Findings Of Fact DNR is called upon to make a decision concerning the possible issuance of CCCL permits in coastal areas described in Section 161.053, Florida Statutes. The applicant Wiggins has sought such a permit. This application is opposed by Petitioners. Mary Evelyn Wood owns property at 267 South Fletcher Avenue, Fernandina Beach, Nassau County, Florida, which is about a five minute walk from the subject property, according to Ms. Wood. The Wiggins property is at 664 South Fletcher Avenue in the same town and county. The Douglas property is at 649 South Fletcher Avenue. It is located adjacent to the Wiggins property across Fletcher Avenue on the west side and one lot north. The Crim property is at 663 South Fletcher Avenue, directly across that road west of the Wiggins property. The Douglas and Crim properties are also in Fernandina Beach, Nassau County, Florida. Petitioners have expressed their opposition to the grant of a CCCL permit based upon the belief that with construction at the Wiggins property the dune system which fronts the Wiggins property will be adversely impacted and place Petitioners' properties at risk. In this connection Petitioners are concerned about shoreline erosion and flooding of upland properties to include their own. Their attitude is prompted by the history of problems of erosion of the beach in the immediate vicinity where Wiggins and Petitioners have their property, especially related to weather events and maintenance dredging in the St. Mary's River Inlet to facilitate activities at Kings Bay Naval Base. Attempts have been made to mitigate the efforts of that dredging. Petitioners are further disturbed by problems which they have seen with beach front homes referred to as the Caples and Manley properties. The circumstances in those latter two properties are described in greater detail subsequently. Finally, Petitioners are concerned about the cumulative impact associated with the Wiggins project and similar projects which may be forthcoming along the beach front in that vicinity. On March 30, 1989, DNR received an application from Wiggins for a CCCL permit to construct a residential dwelling seaward of the Nassau County Coastal Construction Control Line. DNR determined that Wiggins' original application was incomplete and requested further information from Wiggins by letter dated May 1, 1989. Wiggins submitted all necessary supplementary documents. DNR issued a notice of completeness dated July 10, 1989, notifying Wiggins that this original application had been determined complete as of June 30, 1989. After determining that Wiggins' original application was complete, DNR engineer Robert M. Brantley, Jr. reviewed the application to analyze it for compliance with statutory and rule requirements. In connection with this review, Brantley prepared a memorandum to his supervisor regarding his recommendation for DNR action on the original application. Out of concern that the project proposed by the original application would not minimize adverse impacts on the beach and dune system after the site, Brantley recommended that the structure be moved twenty feet landward, thus requiring a local zoning variance from City of Fernandina Beach right-of-way requirements. On September 21, 1989, DNR issued a final order, "permit NA-148" granting Wiggins' original application as modified pursuant to Brantley's recommendation to require siting of the dwelling structure twenty feet landward. This constituted proposed agency action on the permit request. Petitioners were determined to have failed to allege injury to their substantial interests sufficient to grant them standing to challenge proposed permit NA-148, and their petition was dismissed. Wiggins was denied the local zoning variance from the twenty foot right-of-way setback contemplated by proposed permit NA-148. Petitioners appeared at the variance hearing and opposed the variance. After denial of the zoning variance required by proposed permit NA- 148, Wiggins contacted Brantley to ask for "reconsideration" of permit NA-148. Wiggins' request was treated by DNR as an application for modification of proposed permit NA-148. After review the application as modified was determined to be complete and a letter to that effect was issued by DNR on May 10, 1990. The modified application sited the dwelling in the same location as the original application, but with several improvements to satisfy DNR. This application as modified deleted the condition of proposed permit NA-148 allowing any excavation, as clarified at hearing; deleted the condition of proposed permit NA-148 allowing understructure parking (including the deletion of a condition allowing a concrete slab or impermeable surface), and committed the permittee to maintain the frontal dune and encumber the lot with a covenant requiring the present and future owners of the project site to maintain the dune integrity. Additionally, the seaward deck of the project structure was reduced from eight feet to six feet and the direction of stairs on the exterior of the structure was adjusted. On June 11, 1990, DNR issued a final order "Permit NA-148 M1" with the aforementioned changes incorporated. This constituted proposed agency action about which the dispute has been joined. The project site, described as lot 5, block 8, Ocean City subdivision, Fernandina Beach, Nassau County, Florida (WE 1, 3) is an oceanfront lot crossed by a well vegetated, single ridge frontal dune. The crest of the dune is located approximately 127 feet seaward of the Nassau County CCCL. It is approximately three to four feet above the existing grade with an elevation of 14 feet NGVD. The project site is located on the northern one-third of Amelia Island. As alluded to before, the northern one-third of Amelia Island has experienced erosion since the turn of the century when the St. Marys River entrance channel was stabilized by jetties. Such erosion continues and will continue as long as the St. Marys River channel jetties interrupt the natural southern transport of sand and routine maintenance dredging is conducted. Over the last twenty years, in acknowledgment of the erosion resulting from the increased frequency of maintenance dredging of the St. Marys River navigational channel, the project site has benefited from federally-funded beach renourishment projects which have deposited beach-quality spoil on two or three occasions. Material from the most recent renourishment project is still in the area of the project site. A granite revetment was built along the shoreline on the property following the destruction brought by Hurricane Dora in 1964. Further improvements to the revetment were made in the mid-1970s. The revetment protects the uplands and has acted like a sand fence to catch sand on its landward side and promote the buildup of the dune on that side. Since at least 1979, the dune ridge which parallels the property frontage has built up behind the rock revetment line. Currently, the revetment is covered by sand. The revetment would stabilize the shoreline in the event of major shore erosion. Deposition and accumulation of beach material on the seaward side of the revetment has occurred on this site as well, due to the renourishment project. Such accumulation improves the protection of the revetment system in that the accumulated sand acts as a sacrificial buffer to erosion. If that buffer is removed, the revetment then offers its protection against erosion. The revetment is located in approximately the same position as an established erosion control line. An established line of construction, including projects permitted by DNR has occurred landward of the erosion control line. As proposed, permit NA-148 M1 would site the project dwelling structure landward of the erosion control line and the permitted line of construction. The single ridge dune on the project site provides protection for upland property from flooding attributable to wave runup during astronomical high tides and storms called northeasters. The next structure north of the project site is a single family dwelling located 210 feet from the project and constructed pursuant to CCCL permit number NA-32. This is the Caples house. The next structure south of the project site is a single family dwelling located 300 feet from the project site and constructed pursuant to CCCL permit number NA-28, the Manley house. No dune crest or ridge or significant topographic feature exists under either the Caples house or the Manley house. The sand forming such crest, ridge, or feature has been removed. The seaward pilings of the Caples and Manley houses had been placed in the frontal dune. Erosion in the vicinity of the Caples and Manley houses has affected adjacent properties. Two lots north of the Caples house, no topographic feature or dune crest exists due to the presence of a parking lot servicing a private business. Approximately one lot south of the project site, midway between the project site and the Manley house, no topographic feature or dune crest exists due to the presence of a street end or public parking area. The northern part of Amelia Island is subject to occasional flooding due to the previously described astronomical high tides or northeasters. The properties owned by Petitioners Crim and Douglas have been subjected to upland flooding by ocean water which probably entered through lower elevations including through the dune breach created by the parking lot north of the Caples house, through the dune breach at the street end of parking area between the project site and the Manley house, or thorough the dune breach beneath the Caples house. Such flooding may occur with every northeaster. The Caples house and the Manley house were permitted by DNR prior to legislative authorization for the requirement of restrictive covenants in connection with CCCL permitting. The permits for the Caples and Manley houses contained no provision requiring the owner of such properties to maintain the dune on those sites. As each of the Respondents' experts testified at hearing, construction pursuant to proposed permit NA-148 M1 will not make Petitioners' property more susceptible to flooding, tidal flow and windstorm damage, because the project site will be encumbered with a covenant requiring the property owner to maintain the elevation and contours of the frontal dune. The Petitioners proffered no expert testimony on this issue to the contrary. Respondents' experts opinions are accepted. The imposition on an oceanfront parcel of a covenant which requires that dune contours be maintained, such as the one required by Condition 11 of proposed permit NA-148 M1, provides owners of property upland of such parcel with a greater level of protection than they have presently in the absence of any covenant or requirement placing such an obligation upon the owner of the project site. The seaward tow of the dune on the project site is approximately 145 feet seaward of the control line. The beach in this area is located between the seaward toe of the dune and the mean high water line. Such area is sometimes referred to as the public right-of-way on the beach. As each of the Respondents' experts testified at hearing, and as accepted, the proposed structure does not extend beyond the seaward toe of the dune and thus does not infringe on the area between the seaward toe of the dune and the mean high water line. The Petitioners proffered no expert testimony on this issue to the contrary. The impacts on a beach and dune system associated with a dwelling structure may occur from four types of events: construction, windblown sand and recharge, localized erosion from a high frequency storm event, and erosion in a design storm event. During construction of the project dwelling structure, installation of a pile foundation into the dune would result in the disturbance of the dune and vegetation on the site, including vegetation which stabilizes the dune where the pilings are placed and under the structure itself. The seaward pilings of the dwelling structure permitted by NA-148 M1 would be located approximately 128 feet seaward of the CCCL and thus will be located in the crest of the dune ridge which traverses the project site. This is a most disadvantageous placement. However, it will not be necessary to take out a section of the dune in the installation of the piles. Impacts to vegetation on the seaward side of the dune should be minimal in front of the structure and non existent in other parts of the dune located at the Wiggins parcel. Proposed permit NA-148 M1 contains conditions which require protection of the site and adjoining properties during construction, including the requirement for a preconstruction conference between a representative of the permittee and DNR. Construction fencing or sand fences are generally required by DNR pursuant to such a conference. However, a condition of proposed permit NA-148 which required a construction fence on the seaward side of the structure was made obsolete by and deleted in proposed permit NA-148 M1. The condition required a construction fence on the seaward side of the permitted structure to protect the dune. Under proposed permit NA-148, the structure would have been located landward of the dune. Proposed permit NA-148 M1 sites the structure on top of the dune negating the utility of the sand fence. The department will monitor and exercise supervisory authority over the project during construction. Upon completion of construction, proposed permit NA-148 M1 contemplates that the dune system on the project site be returned to preconstruction condition with the exception of vegetation where the piles were placed and under the structure. A structure located in a beach or dune system may affect the beach or dune system by affecting wind currents across the property. The dune system is recharged by windblown sand and the proximity of the structure to the dune may tend to have some adverse effect on that process. However, such a structure may also act as a "sand fence" and allow windblown sand to accumulate beneath it. Whatever the outcome with windblown movement of sand, the applicant must maintain the integrity of the dune in furtherance of the covenant. The presence of a structure in a beach or dune system may have localized impacts on the beach and dune system during a storm event. A pile foundation structure would increase scour and erosion about its pilings and have an impact equal to approximately twice the diameter of the pile. As example a 12" pile would cause approximately two feet of erosion. The pilings here are 10" diameter piles. In effect such "washtub" erosion reaches an equilibrium point at which it does not continue to get wider or deeper and can fill back in under varying seasonal conditions. A structure in the beach or dune system would have an impact on the beach and dune system during a design or major storm event. The design storm event is the 100 year storm event. In such a storm event, the most impactive type of structure is one with a rigid monolithic slab. An example of such a structure is a slab-on-grade dwelling structure with spread footer foundations. The Wiggins structure, a pile foundation dwelling, is designed to minimize impacts in the major storm event. The principal impacts of the structure proposed through the modified application related to the beach and dune system would be the impact on day-to- day recharge of the dune system by windblown sand and possible inhibition of dune reformation after an event which eroded the entire dune line. Condition 11 of proposed permit NA-148 addresses those impacts, namely it calls for promoting the integrity of the dune and the maintenance of the contours of the dune whatever the contingency. That is to say, Condition 11 requires Wiggins and, by restrictive covenant, future owners of the project site, to maintain the topography of the dune and to restore the dune to preconstruction conditions if it is damaged by or destroyed by wind, erosion, or during a storm event. Condition 11 also requires that salt-resistant vegetation indigenous to Florida's beaches and dunes be maintained in perpetuity and restored to preconstruction conditions if damaged by or destroyed by wind, erosion, or during a storm event, except where pilings are placed and under the dwelling. Revegetation of the dunes is a very viable option. Typically, the plants for revegetation are sea oats, and they are very hardy. If planted and given water for about the first three months thereafter, they will grow right along. Sea oats propagate through their roots. Their root systems contribute to the stability of the dune. The vegetative cover of the dune traps sand, assists in the accumulation of sand blown across the beach into dunes, and thus helps to maintain the dune topography. Again, Condition 11 does not require the owner of the project site to maintain vegetation underneath the structure on the landward face of the dune. The condition does require the dune itself to be maintained beneath the structure. Vegetation on the seaward side or face of the dune and in the side yards and areas of the dune not covered by the structure must be maintained. Vegetation on the seaward side of the dune plays the most important or critical part in the accumulation of the sand and maintenance of dune topography. The performance of Condition 11, both in maintenance of vegetation and dune contours where contemplated is feasible. Replanted vegetation should be used first to lend dune stability and integrity and should be successful. In the event that the method does not adequately provide the necessary dune aggregate or webbing to hold the dune together, artificial means such as sand fencing, geosynthetic geotextiles, webbing materials, or a slurry of biodegradable composite jell, may be used to provide such stability. Since 1985, DNR has used a dune maintenance condition in connection with other CCCL permits, and has had success with that policy. DNR has a mechanism in place to enforce Condition 11. A project site, such as permit NA-148 M1, encumbered by a covenant to maintain dune topography, such as Condition 11, will be entered in the DNR computer system as part of a master report of similar such covenanted properties. This report would have a "check date" column. That column might require that a site be reviewed every six months, for example. At the six month anniversary, the field inspector for the project area would get a notice instructing him to check the compliance of the site. He would do so and file a report with the DNR engineer responsible for the project. The engineer would file the report and set the next compliance check date. The occurrence of a major storm event in a project area would cause the Department to perform post-storm compliance survey on all projects in the affected areas. As each of the Respondents' experts established at hearing, proposed permit NA-148 M1 adequately address the concerns of DNR as contained in Brantley's analysis of the project and minimizes adverse impacts to the beach and dune system. The Petitioners proffered no expert testimony on this issue to the contrary. The primary concern relating to the cumulative effect of the project is also related to the project structure's impact on the frontal dune, namely the inhibition of dune recharge from windblown sand and its rebound after a storm event. As each of the Respondents' experts established at hearing, the conditions of proposed permit NA-148 M1 reduce or eliminate concerns regarding the cumulative effects of similar projects. With Condition 11, being universally required in the future the cumulative effect of projects similar to the project permitted by proposed permit NA-148 M1 would be tolerable. The cumulative impacts of projects similar to the Wiggins project, if subject to the same permit conditions, will not threaten the beach and dune system and may in fact provide additional protection to the upland structures because of requirements to restore and maintain existing conditions as necessary. The Petitioners proffered no expert testimony on this issue to the contrary. As the Respondents' expert witnesses established at hearing the project as modified is in compliance with all requirements of Chapter 16B-33, Florida Administrative Code, and Chapter 161, Florida Statutes. The Petitioners proffered no expert testimony on this issue at hearing to the contrary.
Recommendation Having considered the foregoing findings of fact, conclusions of law, the candor and demeanor of the witnesses, and the pleadings and arguments of the parties, it is, therefore, recommended that proposed permit NA-148 M1 be issued by DNR to Wiggins subject to all its conditions. RECOMMENDED this 18th day of February, 1991, in Tallahassee, Florida. CHARLES C. ADAMS, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 18th day of February, 1991. APPENDIX TO RECOMMENDED ORDER, CASE NO. 90-4992 The following discussion is given concerning the fact proposals of the parties: Petitioners' Facts Paragraphs 1 and 2 are subordinate to facts found. Paragraph 3 is not necessary to the resolution of the dispute. Paragraph 4 is subordinate to facts found. Paragraph 5 is not necessary to the resolution of the dispute. Paragraphs 6 through 8 and the first sentence of Paragraph 9 are subordinate to facts found. The remainder of Paragraph 9 is contrary to facts found. The first sentence of Paragraph 10 is subordinate to facts found. Concerning the second sentence, while it is recognized that the placement of the piles in the dune crest is problematic, Condition 11 to the permit provides necessary remedial response. Paragraph 11 is subordinate to facts found as is the first sentence of Paragraph 12. The remaining sentences in Paragraph 12 are addressed by Condition 11. Paragraphs 13 through 19 are subordinate to facts found. Paragraphs 20 and 21 are contrary to facts found. Paragraph 22 is not necessary to the resolution of the dispute. Concerning Paragraph 23, whatever erosion occurs Condition 11 will require the applicant to rectify the situation. As to Paragraph 24, although it has not been necessary to test the nature of the maintenance covenant act after a storm event, nothing suggests that it would not be a viable requirement following such an eventuality. Paragraph 25 is subordinate to facts found. Paragraph 26 is contrary to facts found. DNR's Facts Paragraph 1 through 8 are subordinate to facts found. Paragraph 9 and 10 are discussions in law. Paragraphs 11 through 15 are subordinate to facts found. Paragraph 16 is not necessary to the resolution of the dispute. Paragraphs 17 through 30 are subordinate to facts found. The first sentence to Paragraph 31 is contrary to the impression of the importance of the dune in question. The second sentence in Paragraph 31 is subordinate to facts found. Wiggins' Facts Paragraphs 1-54 are subordinate to facts found. COPIES FURNISHED: Tom Gardner, Executive Director Department of Natural Resources 3900 Commonwealth Boulevard Mail Station #10 Tallahassee, FL 32399-3000 Granville C. Burgess, Esquire 301 1/2 Centre Street Post Office Box 1492 Fernandina Beach, FL 32034 Brian F. McGrail, Esquire Department of Natural Resources 3900 Commonwealth Boulevard Mail Station #10 Tallahassee, FL 32399-3000 T. R. Hainline, Jr., Esquire Andrew Keith Daw, Esquire Rogers, Towers, Bailey, Jones & Gay 1300 Gulf Life Drive Jacksonville, FL 32207
The Issue The issue for determination at the final hearing was whether the Petitioner Blaha possessed the requisite standing to maintain this action and if so, whether the Applicant Aquarina Developments, Inc., established by a preponderance of the evidence entitlement to a permit from the Coastal Construction Control Line ("CCCL") which would authorize construction of the following: (1) twelve above-ground balconies extending five feet over the CCCL; (2) two roof overhangs extending approximately one foot over the CCCL; (3) two dune walkovers and four decks providing elevated beach access; and (4) a temporary fence extending no more than five feet beyond the CCCL. At the final hearing, the Respondent Aquarina Developments, Inc., (hereafter "Aquarina" or "Applicant") offered Respondent's Exhibits 1-16, which were admitted into evidence. Edward Fleis, Howard J. Teas, Bert Leltz and Ross Witham testified on behalf of the Respondents. Peter Pritchard, Rob Lee and Georges Blaha testified for the Petitioner. Additionally, public comment was taken as provided at Section 120.57(1)(b)(4), Florida Statutes. A Proposed Recommended Order has been submitted by the Respondent Aquarina Developments, Inc. To the extent that the proposed findings submitted by Respondent are not reflected in this Order, they are rejected as unsupported by the weight of credible evidence or as being immaterial to the results reached.
Findings Of Fact By application No. 775-020.61 filed on July 1, 1981, Respondent Aquarina requested a coastal construction permit for construction of portions of twelve cantilevered balconies, two roof overhang sections, a temporary construction fence, four elevated wooden decks, and two dune crossovers, all seaward of an established coastal construction control line ("CCCL") in Brevard County, Florida. The purpose of the proposed structures is to enhance utilization of the beach by residents of Aquarina's PUD located between the Atlantic Ocean and Mullet Creek, a tributary of the Indian River in South Brevard County, while at the same time inhibiting the deleterious effects of unrestrained pedestrian and vehicular access across the beach dune on the property. Respondent Aquarina's project is located on the barrier islands separated from the mainland by the Indian River, thirteen miles south of Melbourne and five miles north of Indian River County. Aquarina proposes to develop a condominium community approved as a PUD by Brevard County, with a projected population of 3,400 persons including 1,600 residential units, a commercial area, and 500 hotel rooms. The project includes at least two condo- mini urn buildings located entirely landward of the CCCL except for the following specific portions: Twelve cantilevered balconies ex- tending approximately five feet beyond the CCCL but not touching the ground; Two roof overhang sections extending approximately one foot beyond the CCCL; Two beach-dune walkover structures to be constructed a maximum of seventy- five feet seaward of the CCCL, which are to provide controlled beach access; Four elevated wooden observation decks constituting integral parts of the walkover structures; A temporary construction fence extending no more than five feet beyond the CCCL. On or about November 20, 1981, the Department indicated its intent to recommend to the Executive Director the issuance of the Applicant's coastal construction permit. After the granting of a requested extension of time, Petitioner Blaha filed objections and a Petition for the Initiation of Formal Proceedings under Section 120.57, Florida Statutes. The Petition raised three issues: Whether construction of the proposed minor structures seaward of the CCCT would harm sea turtles inhabiting the area at issue; Whether a new CCCL should have been set based on changing conditions in the area; Whether the additional shading caused by the proposed structures would harm the dune vegetation system. At the beginning of the hearing, the Hearing Officer heard argument and received evidence on the issues raised by the Motions to Dismiss filed by the Department and the Applicant. The Respondent's Motions raised three issues: Whether the Petitioner had standing to initiate this cause; Whether the alleged impact that the Applicant's proposed coastal construction would have on sea turtles lies within the jurisdiction of the Department and the Hearing Officer under Chapter 161 of the Florida Statutes; and Whether the exact configuration of the CCCL is a proper subject for consi- deration at a hearing challenging the proposed issuance of a coastal construction permit. Petitioner Blaha admitted that he did not live on the beach at issue and in fact lived on the west side of State Road A1A, three miles to the north of the Applicant's proposed project. The Petitioner stated that he was the Director of the Space Coast Branch of Friends of Animals, an environmental organization concerned about wildlife, although not representing the organization in this proceeding, and that he had a general interest in protecting the beach from erosion, a problem affecting everyone on the barrier island. In response to the argument that Petitioner Blaha had no special interest differing in kind from the interests of the general public, the Petitioner alleged that he runs on the beach and observes the sea turtles, arguing that this evinces a more than average interest in protecting the beach and its wildlife. The Hearing Officer also heard argument on whether the Department has jurisdiction to consider potential impacts on the nesting habitats of sea turtles from proposed coastal construction, under Chapter 161, Florida Statutes. Petitioner Blaha urged that although Section 161.053, Florida Statutes and the rules promulgated thereunder do not address sea turtles and their protection, the statute should be so interpreted. The Department responded that any jurisdiction it may have over sea turtles would be reposited in its Marine Resource Division, not in the permitting procedures for a coastal construction permit. In addition, federal laws protect endangered sea turtles, and the federal government has primary jurisdiction over the regulation of the nesting habitats of such sea turtles. Similarly, the Applicant and the Department pointed out that the Petitioner's criticism of the placement of the present CCCL falls outside the scope of a hearing on the issuance of a coastal construction permit, since Section 120.54, Florida Statutes provides for rulemaking proceedings for those attempting to change a rule established CCCL and Rule 16B-33.10, Florida Administrative Code, contains provisions for CCCL revisions or modifications on application of a riparian owner of property at or on the CCCL. Petitioner Blaha is not a riparian property owner and this was not a proceeding under Section 120.54, Florida Statutes. Respondent Aquarina established that it had taken and would continue to take all reasonable actions necessary to ensure the protection of sea turtles that inhabit the site through public relations campaigns and public advertisements to educate the public and especially the residents of the PUD and through architectural design efforts and dareful construction practices that will limit the impact of the proposed development on sea turtles and their nesting habitats. Moreover, to the extent that the development might have an impact on sea turtles, the source of the impact would not primarily be the structures at issue in these proceedings, but the buildings, parking lots, and other human habitation lying landward of the CCCL. The proposed temporary construction fence to be placed five feet beyond the CCCL will help conserve the dunes by limiting the potential impact of construction, and the Respondent Aquarina has agreed to restore that affected area to its natural state upon the completion of construction. Most importantly, the proposed dune crossovers will protect the dunes from the destruction that is occurring in the dunes to the north of the project and on the project site itself because of unrestrained pedestrian and vehicular traffic over and/or through the dunes and the accompanying destruction of dune vegetation in those areas. The dune crossovers are wooden walkways on raised pilings designed to have as little contact with the dunes as possible, with railings to restrain pedestrians from straying away from this direct access from the condominiums to the beach. The crossovers will make it unnecessary and undesirable for residents and visitors to create alternative foot paths through the heavy dune vegetation to the beach. Coupled with the educational program already being implemented by Aquarina, the dune crossovers should help to conserve the dunes. The Respondent Aquarina established that the incremental shading caused by the proposed roof overhangs extending about one foot beyond the CCCL and the cantilevered balconies extending approximately five feet beyond the CCCL would not significantly add to the shading from the buildings themselves, which lie entirely landward of the CCCL. The evidence showed that even the impact of the shading from the landward buildings would have no significant impact on the dune vegetation system or increase the rate of erosion or deterioration of the dune. See Rule 16B-33.02(23)(b), Florida Administrative Code. The additional impact from the minor structures for which the Respondent Aquarina seeks its permit should be minimal.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED: That the Respondent Department of Natural Resources, through its Executive Director, grant the requested construction control permit to the Applicant Aquarina Developments, Inc., subject to the conditions stated in the proposed permit (No. BE-80), the draft of which was attached to the Department's letter of November 20, 1981, notifying Petitioner Blaha of the Department's intent to issue the requested permit. DONE and ORDERED this 25th day of October, 1982, in Tallahassee, Florida. SHARYN L. SMITH, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 ApA1Achee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 25th day of October, 1982. COPIES FURNISHED: Georges Blaha 280 Flamingo Drive Melbourne Beach, Florida 32951 Deborah A. Getzoff, Esquire Assistant Department Attorney Department of Natural Resources 3900 Commonwealth Boulevard Tallahassee, Florida 32303 Clifford A. Schulman, Esquire GREENBERG TRAURIG ASKEW HOFFMAN LIPOFF QUENTEL & WOLFF, P.A. 1401 Brickell Avenue Miami, Florida 33131 Henry Dean, Esquire General Counsel Department of Natural Resources 3900 Commonwealth Boulevard Tallahassee, Florida 32303 Elton Gissendanner, Executive Director Department of Natural Resources 3900 Commonwealth Building Tallahassee, Florida 32303
Findings Of Fact After DNR issued a cease and desist order to Petitioner, forbidding further construction on his Walton County lot seaward of the coastal construction control line, he applied for an after-the-fact permit authorizing work to go forward on a three-story ten-unit condominium, which would occupy some 95 percent of the width of his lot, and extend 34 feet seaward of the coastal construction control line. Petitioner's Exhibit No. 1. DNR staff stated the following, in recommending denial: There presently exists over 160 feet of property located landward of the control line in which the proposed structure could be sited. The staff is concerned that the proposed encroachment is not justified, nor considered necessary for reasonable use of the property. In addition, staff is concerned about the potential cumulative effects of siting major structures seaward of the control line along this section of the coast, which contains a number of undeveloped lots, as well as redevelopable lots. The cumulative impact of such construction will result in significant disturbance and damage to well-established, mature vegetation and eventual destabilization of the coastal barrier dune ridge. Also, the proposed encroachment and shore-parallel site coverage will have an adverse impact on the natural recovery processes of the beach/dune system following the impact of a major storm event. The proposed building is not designed in accordance with the standards set forth in Subsections 16B-33.05(6) and 16B-33.07(1) and (2), Florida Administrative Code. File number WL-183 ATF has been assigned. . . . RECOMMENDED DENIAL, ASSESMENT OF A CIVIL FINE OF FIVE THOUSAND DOLLARS ($5,000) AND REQUIRING REMOVAL OF THE EXISTING UNAUTHORIZED CONSTRUCTION SEAWARD OF THE COASTAL CONSTRUCTION CONTROL LINE. Petitioner's Exhibit No. 1. The "reference [to] the extensive site coverage was not only the shore parallel site coverage, but also included the proposed encroachment seaward of the control line." (T. 18). DNR staff opposes construction on Mr. Hill's lot of a habitable structure seaward of the control line. (T. 19, Petitioner's Exhibit No. 2, pp. 12 and 13). Petitioner Hill timely instituted formal proceedings on his application, WL-183 ATF, and Case No. 85-2455 is still pending. Shore Parallel Site Coverage Since October of 1983, in processing coastal construction permit applications, DNR has taken into account "shore parallel site coverage," i.e., DNR staff have considered the relationship between lot width and the width of any structure proposed to be built fronting the water, seaward of a coastal construction control line. A succession of waterfront buildings stretching the entire width of their respective lots walls off the foreshore from more landward dunes. "[I]f you cover an extensive portion of the beach in the shore parallel direction, you tend to she[a]r off the upland area from the beach area and limit and inhibit the natural recovery processes of the dune system." (T. 15) With respect to Petitioner's proposed project and any other of this size and shape planned this far down on a similarly platted, developed and configured beach, DNR engineers put the maximum acceptable width of the structure at 50 to 60 percent of the lot's gulf frontage. Petitioner's Exhibit No. 2, p. 23; T. 20, 22, 32, 35. DNR has no written policy limiting the width of structures built seaward of the coastal construction control line. Although DNR endeavors to treat similar sites similarly, sites vary significantly and different widths may be allowed on similar sites when structures with different depths are planned. Petitioner's Exhibit No. 3, pp. 9-13. In its post-hearing memorandum in support of Petitioner's rule challenge to DNR's non-rule policy regarding side setbacks, Petitioner quotes the following: Q: Would you generally recommend this 50 to 60 percent shore-parallel site coverage for other types of similarily situated lots, either on the same beach or on other beaches in Florida? A: The reference 50 to 60 percent is something we would feel comfortable with in certain areas of the beach that have similar characteristics and existing--similar situations regarding existing development, potential for redevelopment, stability of the dune area, and things of that nature. It certainly wouldn't apply--those figures wouldn't apply to all areas of the Florida coastline. [Deposition of Brett Moore, September 10, 1985, pp. 16-17.] Q: But for, say, a similarly situated beach, maybe you would try to get people to move toward that time of width without specifically telling them that that's the width of coverage that you desire. A: For the two areas I mentioned, I feel that something in the vicinity of 60 percent site coverage would be acceptable to the staff, and that's what I would tell people if someone proposed a project in that area today. [Deposition of Brett Moore, p. 27.] A: Given that amount of encroachment on the dune, I feel that a reasonably acceptable shore-parallel coverage, given that shore- normal coverage, that would not have a significant adverse impact, would probably be between zero percent coverage and thirty percent coverage. In terms of what we would recommend, generally, in what kind of dune encroachment of a major structure, approximately a thirty-foot width, or about fifty percent coverage would probably be acceptable in terms of the impact to the dune and the recovery potential following a major storm event. Q: Okay. Did you--so fifty percent would probably be okay by your lights; is that a fair characterization of that statement you just made? A: Yeah, I could recommend a fifty percent coverage there, . . . In terms of what I would recommend for a site like that with that kind of encroachment with a major structure on the dune, I would recommend approximately fifty percent coverage. Q: What about for a similar type of beach, not one down in Charlotte County or any place like that, but let's just say a similar type of beach somewhere in the panhandle, same relative dimensions, topography and the like? A: So for the same---for the same site, I would recommend the same. [Deposition of Ralph Clark, pp. 10-11.] At 2-3. Neither this evidence nor any other adduced at hearing proved the existence of an agency statement of general, statewide application purporting in and of itself to have the direct and consistent effect of law. It is DNR's policy to treat similarly situated landowners similarly and to consider cumulative impact. The parties proposed orders contain proposed findings of fact which are addressed by number in an appendix to this final order.
Findings Of Fact On 24 July 1979 the Board of County Commissioners of Palm Beach County adopted Resolution R-79-887 petitioning the TIITF to establish an erosion control line (ECL) extending from South Lake Worth Inlet to the northern city limits of Delray Beach in conjunction with a beach restoration project in the same area. The project as then proposed encompassed extension of the south jetty at the Inlet 170 feet, construction of eight groins at 400-foot intervals commencing just south of the Inlet, and widening the beaches by 500 feet with 150 feet above the mean high water and 350 feet below mean high water, for a distance of approximately 4.8 miles. The restoration project is proposed to be accomplished with sand from a borrow area located approximately one-half mile off shore. The project is designated "Ocean Ridge-Briny Breezes" beach restoration project. SLWID objected to the project and, following conferences between Palm Beach County, SLWID and DNR the County amended its project to exclude property owned by SLWID from the ECL and beach restoration projects with the restoration of the beach to commence 300 feet south of the Inlet and continue for 2.6 miles to the town of Briny Breezes. Extension of the jetty and installation of groins were deleted. Palm Beach County's proposed beach restoration project was authorized by the U.S. Congress and the U.S. Army Corps of Engineers in House Document 164 (Exhibit 5). The proposed "Ocean Ridge-Briny Breezes" beach restoration project was designed in accordance with the criteria set forth in Exhibit 5. The project is designed to restore the severe beach erosion that has occurred in the 2.6-mile project area and to provide the affected uplands protection against the ten-year design storm event. The ten-year design storm event implies a 3.8-foot storm surge with up to eight-foot waves superimposed thereon. The proposed ECL has been surveyed by Palm Beach County along the mean high water line in the proposed area. Over 60 percent of the ocean front property owners have approved the establishment of the ECL in conjunction with a beach restoration project by executing letters of consent. Following notice by DNR a public hearing was held on February 13, 1980, to receive evidence relative to the necessity and propriety of the proposed beach restoration project and the proposed location of the ECL. The Hearing Officer's report (Exhibit 28) concluded that there is a definite need to restore the proposed area where severe beach erosion has occurred and the establishment of the ECL would accomplish the purpose stated in Section 161.161, Florida Statutes. Approval of the project was recommended. The staff of DNR approved the project and prepared the agenda item for the next meeting of the TIITF in which this project was to be considered for final approval. Prior to this meeting of the TIITF, SLWID filed its initial Request for Formal Proceeding and the item was removed from the TIITF agenda and referred to the Division of Administrative Hearings. The beach erosion in the project area has been documented by Palm Beach County, DNR and the U.S. Army Corps of Engineers. Much of the erosion in the northernmost mile of the project has involved the beach above high water, as well as the offshore beach, while the erosion in the southern 1.6 files of the project has predominantly been offshore. During the period 1955-1981 approximately 1.6 million cubic yards of sand has been lost in the project area. Beach erosion determinations are made by calculating both onshore and offshore changes in the beach profile. Significant offshore erosion will lead to onshore beach recession by storm-generated waves. A gradually sloping beach is a natural absorber of wade energy and the most effective. Since maximum wave height is a function of the depth of the water, waves rapidly dissipate when they reach shoal water. With offshore erosion and the resulting deeper water near the shore, incoming waves can be higher and will impact on the upland area with greater force than would occur with a gradually sloping beach. There is a net annual littoral drift of 200,000 cubic yards of sand southward in the project area. Prior to the construction of the Inlet this drift replaced sand lost during storms, thus creating a dynamic beach which receded and was augmented from time to time. The installation of the jetties disrupted this littoral flow and caused the sand to build up on the beach north of the jetty while starving the beach south of the jetty. This problem was partly corrected by the erection of a sand transfer plant on the north jetty which pumped some of this sand across the Inlet to the beach south of the Inlet. The sand transfer plant was not operated during WWII due to the fuel shortage and severe erosion occurred in the project area. Following WWII the sand transfer plant was replaced in operation, sand was dredged from the Inlet and deposited on the beach south of the Inlet and the beach in the project area was largely restored. In 1967 the north jetty at the Inlet was extended and the sand transfer plant was moved eastward some 130 feet. This plant is a fixed plant consisting of a suction line on a boom which dredges sand to be pumped south of the Inlet only from the area that can be reached by the boom. Although capacity of the plant is adequate to pump the sand needed to replace in the project area that sand intercepted by the jetty, due to the limitation of the plant to reach a larger area there is insufficient sand available for the plant to pump to capacity. As a result, even if the plant operated all the time and there was sand available to pump, there would still be a net loss of sand in the project area (Exhibit 21). During recent winter storms property-threatening beach erosion has occurred to beach property in the project area. Some of the property owners have erected bulkheads and seawalls and others are proceeding with plans to do so. In some places in the north portion of the project area there is no exposed beach at high water. In the southern portion of the project area the offshore erosion will, if left to continue, result in severe damage and loss of upland beach if impacted with seas commensurate with a ten-year design storm event. This erosion, both on and offshore, will, if uncorrected, result in a calculated total of 134 feet of beach recession for the ten-year design storm event. This could result in the inundation of S.R. A1A, which runs near the beach in the northern portion of the project area. S.R. A1A is the primary north-south highway east of the Intracoastal Waterway and the evacuation route to the bridges to the mainland in the event evacuation of the beach is necessary in a hurricane situation. The proposed beach restoration project is designed to replace sand lost offshore and onshore erosion in the the project area and provide a sloping beach to absorb wave impact. It will not accelerate erosion. The proposed restoration of the beach will protect property and structures in the project area against the forces associated with a ten-year design storm event. Addition of the 1.5 million cubic yards of sand in the project area will result in some sand infiltration of the Inlet. This was calculated at 8,000 cubic yards the first year, 6,000 cubic yards the second year and 4,000 cubic yards per year thereafter. This will result in insignificant shoaling in the Inlet but will require infrequent maintenance dredging. It will not adversely impact the tidal prism in the Inlet or materially increase the maintenance of the Inlet. Heavy storms result in immediate loss of sand from the upland beach. Most of this sand is deposited in the offshore beach and is returned to the upland beach by the normal action of waves and tides. Approximately ten percent of the sand so removed from the upland beach is not returned but is lost.
The Issue The ultimate issue is whether the Applicant, Florida-Georgia Venture Group, is entitled to development orders for its proposed development of regional impact, Hunter's Ridge, in Flagler County and the City of Ormond Beach, Florida.
Findings Of Fact The Petitioner is Florida-Georgia Venture Group, 402 Clifton Avenue, Holly Hill, Florida 32117, and its authorized agent is Thomas L. Durrance, Managing Partner. The Hunter's Ridge project lies within the jurisdiction of both the Northeast Florida Regional Planning Council (NEFRPC) and the East Central Florida Regional Planning Council (ECFRPC) and underwent concurrent review. The Hunter's Ridge project as proposed in this proceeding is a proposed planned unit development located in the unincorporated area of Flagler County and in the City of Ormond Beach on approximately 5,037 acres. The portion of the Hunter's Ridge project located in the unincorporated area of Flagler County consists of approximately 3,800 acres, of which 1,940 acres will be preserved as conservation area. The portion to be developed in the unincorporated area of Flagler County is approximately 1,860 acres, consisting of 1,702 residential units, plus commercial, recreational, and other uses. The portion of the Hunter's Ridge project located in the City of Ormond Beach consists of approximately 1,237 acres, of which 327 acres will be preserved as conservation area. The portion of the property in Ormond Beach to be developed is approximately 910 acres, consisting of 982 residential units, plus commercial, recreational, and other uses. Of the residential units to be developed in the City of Ormond Beach, 109 residential units were approved by the Department of Community Affairs (DCA) under a preliminary development agreement. The Board of County Commissioners of Flagler County held a public hearing on the DRI/ADA on July 13, 1989, which was continued to October 12, 1989, to November 2, 1989, to January 11, 1990, and to January 25, 1990. On January 25, 1990, the Board of County Commissioners of Flagler County passed and adopted a Development Order for the Hunter's Ridge DRI, which Development Order was recorded in Official Records Book 0423, Page 0669 through 0728, Public Records of Flagler County, Florida. The City Commission of the City of Ormond Beach held a public hearing on the DRI/ADA on August 15, 1989, which was continued to September 5, 1989, to September 19, 1989, to October 3, 1989, to October 17, 1989 and to January 30, 1990. At the public hearing on January 30, 1990, the City of Ormond Beach adopted Resolution 90-20 denying the DRI/ADA for the portion of the Hunter's Ridge DRI located in the City of Ormond Beach. The DCA, pursuant to Section 380.07, Florida Statutes, and Rules 42- 2.002 through 42-2.011, Florida Administrative Code, timely filed a Notice of Appeal and Petition for Administrative Hearing with the Florida Land and Water Adjudicatory Commission (FLWAC), whereby DCA appealed the Development Order adopted by the Board of County Commissioners of Flagler County. The Applicant, pursuant to Section 380.07, Florida Statutes, and Rules 42-2.002 through 42-2.011, Florida Administrative Code, timely filed a Notice of Appeal and Petition for Administrative Hearing with FLWAC, whereby the Applicant appealed the denial of approval by Ormond Beach. This cause came before FLWAC on May 22, 1990, for consideration of the Appeals and the Petitions for Administrative Hearing; FLWAC ordered that this matter be forwarded to Division of Administrative Hearings (DOAH) for assignment of a hearing officer and further proceedings. At the Administrative Hearing conducted by DOAH, on December 5-7, 1990, the Applicant amended its DRI/ADA to reduce the size of the project and to reallocate land uses, densities, and other components of the project. The current scope of the project is reflected in Florida-Georgia Exhibits 1-5, 9, and 14. As amended by the Applicant, the proposed project now consists of the following uses in Flagler County: 11.61 acres of Village Retail Office; 5.71 acres of Village Office; 16.68 acres of Light Industrial; 197.18 acres of Village Services/Recreational; 90.89 acres of Parks and Schools; 64.52 acres of Multi-Family Residential (with Upland Buffer); 259.34 acres of Wetlands; 146.93 acres of Roads, Drainage, and Retention; 52.90 acres of Lakes; 130.00 acres of Golf Course; 57.25 acres of Utility Easement; and 130.00 acres of Single Family Residential. The total number of dwelling units permitted in the County is 220 townhouses and villas and 145 apartments and condominiums. As amended by the Applicant, the proposed project now consists of the following uses in the City: 192.00 acres of Village Services/Recreational; 30.61 acres of Parks and Schools; 14.51 acres of Multi-Family Residential (with Upland Buffer); 174.54 acres of Wetlands; 110.95 acres of Roads, Drainage, and Retention; 28.65 acres of Lakes; 17.32 acres of Utility Easement; and 341.42 acres of Single Family Residential (with Upland Buffer). The total number of dwelling units permitted in the City are 932 single family units and 50 townhouses and villas. Generally speaking, the portions of the development within the County which are to be developed are in Township 41 South, Range 31 East, Section 22 and the east half of Section 21; Section 15 and the east half of Section 16, with the exception of a golf course in Section 15, constitute an area that, if it is to be developed in the future, will require a substantial deviation approval from all concerned agencies. Pursuant to stipulation of the Applicant and Flagler County, an area approximating Section 15 and the east half of Section 16 will be redesignated under the Flagler County Comprehensive Plan as Agricultural, with a permitted residential density of not more than one unit per five acres. Pursuant to stipulation, Sections 17 and 20 and the west halves of Sections 16 and 21, along with most of the portions of Sections 29 and 30 north of State Road 40, will be deeded to a public or public interest agency, with the Applicant retaining the right to conduct silviculture with best management practices except in those wetland areas of the property designated for conservation. The parties, with the exception of Citizens, have stipulated that Florida-Georgia Exhibit 5 constitutes the necessary affordable housing conditions for the project. The affordable housing provisions of the proposed project are consistent of the requirements of Chapter 380, Florida Statutes, Rule 9J-2, Florida Administrative Code, and the State Comprehensive Plan. The affordable housing conditions adequately address affordable housing needs of the project consistent with all local government, state, and regional requirements and regulations. The Applicant, the Florida Audubon Society, Flagler County and the City of Ormond Beach, have stipulated that the conditions contained in their Joint Stipulation, filed as Florida-Georgia Exhibit 9 satisfactorily resolve all issues concerning wetlands, wildlife habitat, and endangered species. The soils on the project will support the proposed development. During review of the DRI/ADA by the RPCs, Volusia County submitted comments and recommendations to ECFRPC. The comments and recommendations of Volusia County were considered by ECFRPC when it adopted its recommended conditions of approval. The conservation area proposed by the Applicant represents a significant contribution to conservation and wildlife. The proposed Development Orders and Conditions of Approval adequately address the regional impacts of the project on the environment and natural resources. The proposed Development Orders and Conditions of Approval include measures intended to address impacts upon, and to protect, the Little Tomoka River. The proposed Development Orders and Conditions of Approval provide for preservation and conservation of wetlands. The proposed Development Orders and Conditions of Approval provide flexibility for protection of environmentally sensitive areas. The proposed plan of development reflects a development that provides adequate environmental protection. The proposed project will have no adverse environmental impacts in the City of Ormond Beach. The proposed Development Orders and Conditions of Approval provide protection for the Little Tomoka River, preventive measures regarding stormwater discharge and stormwater treatment, and mitigative, water quality treatment methods in the surface drainage system, if any degradation is found at a later date. The proposed Conditions of Approval require that all construction within the project be protected against flooding. The project has sufficient safeguards to prevent construction within flood prone areas. Minimum floor elevations for flood plain purposes will be controlled by FEMA flood plain designations and by local rules and regulations, and will be established on a case by case basis for the Hunter's Ridge project. The proposed Conditions of Approval addressing transportation impacts and facilities are consistent with the provisions of Chapter 380, Florida Statutes, with the provisions of Rule 9J-2, Florida Administrative Code, and with the State Comprehensive Plan. The proposed Conditions of Approval ensure that the Hunter's Ridge project will not have an adverse impact on regionally significant roadways, including State Road 40. The proposed Conditions of Approval will ensure that the regional highway network will function at the desired level of service during the project buildout. The proposed Conditions of Approval are consistent with the provisions of Section 380.06(12), Florida Statutes, relating to transportation impacts. The proposed Conditions of Approval adequately address the transportation concerns of Flagler County. The proposed Conditions of Approval adequately address the transportation impacts on the City of Ormond Beach. The proposed Conditions of Approval dealing with public facilities are consistent with the provisions of Chapter 380, Florida Statutes, consistent with the provisions of Rule 9J-2, Florida Administrative Code, and consistent with the State Comprehensive Plan. If the conditions for providing public facilities are not met by the Applicant, development must cease. The proposed Conditions of Approval dealing with public facilities are consistent with the concurrency requirements of Chapter 380, Florida Statutes. The proposed Development Orders and Conditions of Approval adequately address the regional impacts of the project on public services and facilities. The proposed plan for development of the Flagler County portion of the project provides for all required public facilities and services. The Applicant will have to subsidize any deficits in providing public services. The Applicant has agreed to make contributions intended to assist Flagler County in providing public services to residents of areas outside of the Hunter's Ridge project. Solid waste is not an issue in Flagler County. The proposed Conditions of Approval for the Flagler County portion of the project provide three options for wastewater treatment. The proposed Conditions of Approval for the Flagler County portion of the project require that the project must stand on its own and must provide water supply and wastewater treatment without cost to the rest of the residents of Flagler County. The Flagler County portion of the project requires 1,200 to 1,500 dwelling units to provide a self-contained, self-supporting, self-sufficient development which will not require subsidy by other Flagler County taxpayers. The good mix of land uses contained in the proposed plan for development will help the tax base of Flagler County and avoid a deficit during the buildout of the project prior to construction of 1,200 to 1,500 dwelling units. The tax base, the values, and the assessments for the proposed project will provide sufficient funds to support the development. The proposed Conditions of Approval for the Flagler County portion of the project provide for voluntary contributions by the Applicant in excess of what is required by local ordinance. The dedication and donation of the golf course and conservation areas to Flagler County are voluntary contributions by the Applicant. The Ormond Beach portion of Hunter's Ridge project will not require a separate police patrol zone. The Ormond Beach Police Department can provide acceptable response times for the portions of the project within the City. The public safety site to be dedicated by the Applicant will benefit the City and the Police Department and will be helpful in rendering public safety services to the citizens of Ormond Beach. The Ormond Beach portion of Hunter's Ridge project will provide needed revenue to provide needed Police Department services. The Ormond Beach Police Department can adequately provide public safety services for the Hunter's Ridge area and respond to public safety needs within a reasonable amount of time. The City of Ormond Beach is capable of providing potable water service to the project. Impact fees generated by the project will be sufficient to fund water supply and wastewater capital facilities needed to serve the project. The City has adopted the West Ormond Plan to provide utilities to the Hunter's Ridge project. The Applicant has dedicated to the City a westerly wellfield site which will be needed for the entire city in the future, even if the Hunter's Ridge project is not developed. The City of Ormond Beach does not lose money on water and sewer fees. If the homes built in the Ormond Beach portion of the Hunter's Ridge project approximate the assessed values of existing homes within the city, there will be no revenue strain on the operating budget of the City of Ormond Beach. The average sale price for homes in the Hunter's Ridge project will be higher than the current average sale price within the City of Ormond Beach. The Hunter's Ridge project will not place an economic strain on the City of Ormond Beach. Future growth in the City of Ormond Beach will pay for itself in terms of capital needs. The fiscal problems of the City of Ormond Beach are not unique, but are similar to those occurring throughout the state. Increased property values from the Hunter's Ridge project will help the city's fiscal problems in the long run. The City of Ormond Beach has a great deal of ad valorem capacity to meet service needs and operating budgets. The Hunter's Ridge DRI will make significantly more contributions to public services and facilities than traditional subdivisions. The reduced project as proposed for approval in this proceeding contributes a greater amount of money toward public facilities. The public safety site to be dedicated in the Ormond Beach portion of the project is adequate to serve the fire fighting needs of the project and the surrounding areas. The public safety site to be dedicated in the Ormond Beach portion of the project gives the city flexibility in providing fire fighting services if the road network connecting the project with Shadow Crossings and Breakaway Trails is in place and will enable the city to better serve Shadow Crossings and Breakaway Trails. The roadway network for the Hunter's Ridge project will provide interconnections with Shadow Crossings and Breakaway Trails for the provision of police, fire, and emergency services. The Hunter's Ridge project will have no impact on solid waste in the City of Ormond Beach. The Hunter's Ridge project will have no impact on the vehicular needs of the City of Ormond Beach Department of Public Works. The Hunter's Ridge project will have no adverse impact on road maintenance in the City of Ormond Beach. The proposed Hunter's Ridge DRI is consistent with the requirements of Chapter 380, Florida Statutes, the requirements of Rule 9J-2, Florida Administrative Code, and the requirements of the State Comprehensive Plan. The Hunter's Ridge DRI meets all regional requirements. The Hunter's Ridge DRI does not represent "leap frog development," nor does it constitute "urban sprawl." The density of 982 dwelling units for the Ormond Beach portion of the Hunter's Ridge project is consistent with the State Comprehensive Plan and the requirements of Chapter 380, Florida Statutes. Reducing the density proposed for the Ormond Beach portion of the project from 982 residential units to 882 residential dwelling units would not necessarily be considered an improvement to furthering the plan concept. The Hunter's Ridge DRI is consistent with the plans and policies of the Regional Planning Councils. As to the portions within Flagler County, the Hunter's Ridge DRI: Is consistent with the provisions of Chapter 380, Florida Statutes; Is beneficial to Flagler County; Is consistent with the Flagler County Comprehensive Plan; Is consistent with the NEFRPC report and recommendations; Is superior to existing zoning; Provides better development and more planning opportunities than non- DRI approaches to development; and, Provides adequate controls for the development of Hunter's Ridge. The Ormond Beach portion of the project: Is consistent with the provisions of Chapter 380, Florida Statutes; Is consistent with the Ormond Beach Comprehensive Plan and all City ordinances and regulations; Adequately mitigates against adverse impacts through the Conditions of the proposed Development Order. To the extent that the opinions of some witnesses, primarily Mr. Grace and Mr. Shearer, have not been adopted in these Findings of Fact, they are deemed to be unreliable or lacking in substantial weight or persuasive value.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Florida Land and Water Adjudicatory Commission enter a Final Order and therein: Adopt the development order with conditions as set forth in the Joint Stipulation of Florida-Georgia Venture Group and the City of Ormond Beach. Adopt the development order with conditions as set forth in the Joint Stipulation of Florida-Georgia Venture Group and Flagler County. DONE and ENTERED this 21st day of March, 1991, in Tallahassee, Florida. DIANE K. KIESLING Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 21st day of March, 1991. APPENDIX TO THE RECOMMENDED ORDER The following constitutes my specific rulings pursuant to Section 120.59(2), Florida Statutes, on the proposed findings of fact submitted by the parties in this case. Specific Rulings on Proposed Findings of Fact Submitted by Florida-Georgia Venture Group Each of the following proposed findings of fact is adopted in substance as modified in the Recommended Order. The number in parentheses is the Finding of Fact which so adopts the proposed finding of fact: 1-5(1-5); 12-14(6-8); 16- 19(9-12); 20(18); 22-25(19-22); 27-38(23-34); 40-89(35-83); 91(84); 92(85); 94(86); 97(87(; and 98(88). Proposed findings of fact 26, 39, 90, 93, 95, and 96 are subordinate to the facts actually found in this Recommended Order. Proposed findings of fact 6-11 and 21 are unnecessary. Proposed finding of fact 15 is irrelevant. Specific Rulings on Proposed Findings of Fact Submitted by Department of Community Affairs Each of the following proposed findings of fact is adopted in substance as modified in the Recommended Order. The number in parentheses is the Finding of Fact which so adopts the proposed finding of fact: 8-12(13-17). Proposed findings of fact 1, 2, and 13-17 are subordinate to the facts actually found in this Recommended Order. Proposed findings of fact 3-7 are unnecessary. Specific Rulings on Proposed Findings of Fact Submitted by the City of Ormond Beach 1. Proposed findings of fact 1, 8, 10-17, 21, 33-36, 38-40, 43, 46, and 49 are subordinate to the facts actually found in this Recommended Order. Proposed findings of fact 2-7, 19, 20, 22, 23, 37, 47, 48, and 50 are irrelevant. Proposed findings of fact 9, 18, 24-32, 41, 42, 44, 45, 51, and 52 are unsupported by the credible, competent and substantial evidence. Specific Rulings on Proposed Findings of Fact Submitted by the Citizens for Ormond Beach 1. Proposed findings of fact 7, 9-11, 13-19, 21-25, 35, 47, and 49-52 are subordinate to the facts actually found in this Recommended Order. Proposed findings of fact 8, 12, 20, 26-32, 34, 42, and 57 are irrelevant. Proposed findings of fact 33, 36-39, 43-46, 48, and 53-56 are unsupported by the credible, competent and substantial evidence. Proposed findings of fact 1-6, 40, and 41 are unnecessary. COPIES FURNISHED: J. Doyle Tumbleson, Attorney at Law Kinsey Vincent Pyle Professional Association 150 South Palmetto Avenue, Box A Daytona Beach, FL 32114 Fred S. Disselkoen, Jr. Attorney at Law City of Ormond Beach Post Office Box 277 Ormond Beach, FL 32175-0277 Gerald S. Livingston Attorney at Law Post Office Box 2151 Orlando, FL 32802 Timothy Keyser, Attorney at Law Post Office Box 92 Interlachen, FL 32148 Jonathan Hewett Attorney at Law Central Florida Legal Services, Inc. 216 South Sixth Street Palatka, FL 32177 David Russ, Senior Attorney Julia Johnson, Attorney Department of Community Affairs 2740 Centerview Drive Tallahassee, FL 32399-2100 Charles Lee Senior Vice President Florida Audubon Society 1101 Audubon Way Maitland, FL 32751 Linda Loomis Shelley Attorney at Law Dixon, Blanton & Shelley 902 North Gadsden Street Tallahassee, FL 32303 Noah McKinnon Attorney at Law 595 West Granada Avenue Ormond Beach, FL 32075 Douglas M. Cook, Director Planning and Budgeting Florida Land and Water Adjudicatory Commission Executive Office of the Governor The Capitol, PL-05 Tallahassee, FL 32399-0001
The Issue The issue is whether the Department of Environmental Protection should approve Petitioner’s application for a coastal construction control line permit.
Findings Of Fact Stipulated Facts2 Petitioner, Beach Group Investments, LLC (Beach Group), is a limited liability corporation under Florida law. Its address is 14001 63rd Way North, Clearwater, Florida 33760. On December 19, 2005, Coastal Technology Corporation (Coastal Tech) on behalf of Beach Group submitted to the Department an application for a CCCL permit pursuant to Chapter 161, Florida Statutes, to construct 17 luxury townhome units in two four-story buildings, a pool, a dune walk-over, and ancillary parking and driveway areas (hereafter “the Project”). The Department designated the application as File No. SL-224. The property on which the Project is proposed (hereafter “the Property”) is located between the Department's reference monuments R-34 and R-35, in St. Lucie County. The Property’s address is 222 South Ocean Drive, Fort Pierce, Florida. The Property is located seaward of the CCCL line established in accordance with Section 161.053, Florida Statutes, and Florida Administrative Code Rule Chapter 62B-33. On April 21, 2006, the application was determined to be complete. By letter dated June 5, 2006, the Department notified Beach Group that the Project appeared to be located seaward of the 30-year erosion projection of the seasonal high water line (SHWL), and that in accordance with Section 161.053(6), Florida Statutes, the staff could not recommend approval of the Project since major structures are seaward of the estimated erosion projection. By letter dated July 7, 2006, and subsequent submittals, Beach Group requested a waiver of the 90-day time period for processing completed applications pursuant to Chapter 120, Florida Statutes, until October 31, 2006. On August 30, 2006, Beach Group submitted a certified engineering analysis of the 30-year erosion projection of the SHWL for the Department's consideration pursuant to Florida Administrative Code Rule 62B-33.024(1). Beach Group's analysis determined that the proposed major structures associated with the Project were located landward, not seaward, of the 30-year erosion projection. The Department also performed its own 30-year erosion projection of the SHWL, and determined that the proposed major structures were located seaward, not landward, of the 30-year erosion projection. The Department asserts that the proposed structures are located between 87 feet and 68 feet seaward of the Department's determination of the 30-year erosion projection. The Department disagreed with Beach Group's analysis because the analysis appeared to be inconsistent with Section 161.053(6), Florida Statutes, Florida Administrative Code Rule 62B-33.024, and the Department's own analysis. The Property is located just south of the Fort Pierce Inlet, and landward of a federally maintained beach restoration project that had approximately 14 years of life remaining under the existing Congressional authorization when the permit was submitted to the Department. By proposed Final Order dated November 1, 2006, the Department provided to Beach Group notice of its intent to deny the permit application. The proposed Final Order was received by Beach Group on November 8, 2006. Beach Group's petition for hearing was timely filed with the Department. Since the Department proposes to deny Beach Group's CCCL permit application, its substantial interests are clearly at issue, and it has standing to maintain this proceeding. On December 11, 2006, the Department issued an environmental resource permit for the Project. The Department denied Beach Group’s permit application because the Project extends seaward of the 30-year erosion projection calculated by the Department and because the Project’s impacts to the beach-dune system had not been minimized. The permit was not denied on the basis of the existence, or absence, of a line of continuous construction in the vicinity of the Project. The 30-year Erosion Projection (1) Background Fort Pierce Inlet (hereafter “the inlet”) was constructed by the Army Corps of Engineers in the 1920’s. The channel of the inlet is protected by two jetties that extend several hundred feet into the Atlantic Ocean. The jetties act as a barrier to the littoral transfer of sand from the north to south that would otherwise occur along the beach in the vicinity of the Property. The jetties cause accretion on the beach to the north of the inlet and erosion of the beach to the south of the inlet. The inlet channel beyond the jetties also restricts the littoral transfer of sand in the area. The deepening and widening of the channel in 1995 likely contributed to the increased erosion observed south of the inlet in recent years. The beach to the south of the inlet, including that portion on the Property, is designated as a “critically eroded beach” by the Department. The inlet is the primary cause of the erosion. Congress first authorized beach nourishment south of the inlet in 1965. That authorization expired in 1986. Congress “reauthorized” beach nourishment south of the inlet in 1996. That authorization expires in 2021, but St. Lucie County has requested that the authorization be extended for “another 50 years.” The first “major” beach nourishment south of the inlet occurred in 1971. Subsequent “major” nourishments occurred in 1980, 1999, 2003, 2004, and 2005. Another “major” nourishment is planned for 2007. There was a “moderate” nourishment of the beach in 1995, which included the placement of geotextile groins on the beach just to the north of the Property. “Small” nourishments occurred in 1973, 1978, 1987, 1989, 1990, 1992, 1994, 1997, and 1998. Cumulatively, the nourishments that occurred between the “major” nourishments in 1980 and 1999 involved approximately 419,000 cubic yards of sand, which is more than the volume involved in several of the “major” nourishments. Beach nourishment south of the inlet has been an ongoing effort since it started in 1971. The more persuasive evidence establishes that the nourishment project that is authorized through 2021 is a continuation of the project started in 1971 rather than a separate and distinct project. Various erosion control efforts have been used south of the inlet in conjunction with the beach nourishment efforts. For example, geotextile groins (which are essentially massive sandbags) have been installed and removed on several occasions since the mid-1990’s in order to “temporarily stabilize the shoreline until such measures could be taken to design, permit and construct a long-term solution”; concrete rubble and other riprap has been placed on the beach over the years (without a permit from the Department) to protect upland structures from erosion; and a "spur jetty" was constructed on the south jetty in an effort to reduce erosion south of the inlet. These efforts have not slowed the pace of the erosion or minimized the need for beach nourishment south of the inlet. Indeed, the need for and frequency of “major” nourishments south of the inlet have increased in recent years. Beach erosion south of the inlet will continue to be a serious problem so long as the inlet exists and the jetties remain in place. There is no reason to expect that the inlet or the jetties will be removed in the foreseeable future and, as a result, beach nourishment south of the inlet will continue to be necessary. The Department has recognized the need for continuing nourishment of the beach south of the inlet, as reflected in both the Strategic Beach Management Plan for the St. Lucie Beaches and the Ft. Pierce Inlet Management Study Implementation Plan. Those plans acknowledge the long-term need for continued nourishment of the beach at a rate of at least “130,000 cubic yards on an average annual basis.” The plans do not, however, guarantee that future beach nourishment in the area will occur at that, or any, rate. (2) Rule Methodology Florida Administrative Code Rule 62B-33.024 contains the methodology for determining the 30-year erosion projection, which is the projected location of the SHWL 30 years after the date of the permit application under review. Where, as here, the beach at issue is subject to an ongoing beach nourishment project, the methodology requires consideration of “pre-project” conditions -- i.e., the conditions that existed before the beach nourishment efforts started -- because those conditions are used to project how the beach will migrate landward in the periods over the next 30 years when there may not be any beach nourishment activity. The coastal engineering experts presented by the parties -- Michael Walther for Beach Group and Emmett Foster for the Department -- used essentially the same methodology to determine the location of the 30-year erosion projection. However, the variables that they used in each step of the methodology differed. Step 1: Locate the Pre-Project MHWL The first step in determining the 30-year erosion projection is to locate the pre-project MHWL. If a pre-project erosion control line (ECL)3 has been established in the area, it is to be used as the starting-point for the determination of the 30-year erosion projection. Otherwise a pre-project survey of the MHWL is to be used as the starting-point. Mr. Walther used a 1997 ECL as the starting point for his analysis. Mr. Foster used a March 2002 survey of the MHWL as the starting point for his analysis because he did not consider the 1997 ECL to be an appropriate pre-project ECL. The March 2002 survey of the MHWL is not itself an appropriate starting point for the analysis. The survey is not a “pre-project” survey, no matter how the project is defined; the survey occurred more than 30 years after the nourishments started in 1971, and three years after the first “major” nourishment pursuant to the Congressional reauthorization of the project. Moreover, as discussed below, there is an appropriate pre-project ECL in the area. There are two lines that might be considered to be a pre-project ECL in this case -- (1) the ECL established in 1997, and (2) the South Beach High Tide Line (SBHTL) established in 1968. The 1997 ECL was established based upon a survey of the MHWL performed on May 5, 1997. The survey occurred two years after a “moderate” beach nourishment and the placement of the geotextile groins on the beach. There was also a “small” nourishment in 1997, but the record does not reflect whether that nourishment occurred before or after the survey. The SBHTL was established based upon a survey of the MHWL between 1966 and 1968, prior to the initial nourishment of the beach south of the inlet. It is approximately 65 feet landward of the 1997 ECL. The SBHTL is the functional equivalent of an ECL, and it roughly corresponds to the “best fit line” for the March 2002 survey used by Mr. Foster as the starting point for his determination of the 30-year erosion projection in this case. The Department contends that the 1997 ECL is not based upon a “pre-project” survey of the MHWL because the applicable beach restoration project south of the inlet began in the 1970’s and has been ongoing since that time. Beach Group contends that the applicable project is the current one that is authorized through 2021, and that the 1997 survey preceded the start of the nourishments authorized by that project. The Department has used the 1997 ECL as the starting- point for determining the 30-year erosion projection in several prior permits in the vicinity of the Project,4 and in an April 9, 1999, memorandum discussing the 30-year erosion projection in the vicinity of monuments R-35 and R-36, Mr. Foster stated that “the ECL represents the pre-project [MHWL].” Mr. Foster no longer considers the 1997 ECL to be the appropriate pre-project MHWL for purposes of determining the 30- year erosion projection south of the inlet. He testified that had he been aware of “the complete background” of the 1997 ECL and the extent of the nourishments in the 1980’s and 1990’s, he would have brought the issue to the Department’s attention so that the Department could consider whether the 1997 ECL or “an earlier prenourishment line” was the appropriate pre-project MHWL. Although it is a close question, the more persuasive evidence presented at the final hearing establishes that the 1997 ECL is not an appropriate pre-project MHWL because the applicable “project” includes the beach nourishment efforts started in 1971 that have continued through the present, even though those efforts were intermittent at times. Thus, the appropriate starting point for determining the location of the 30-year erosion projection is the SBHTL, not the 1997 ECL used by Mr. Walther or the March 2002 MHWL survey used by Mr. Foster. Step 2: Locate the Pre-Project SHWL The second step in determining the 30-year erosion projection is to determine the location of the pre-project SHWL. Mr. Walther located the pre-project SHWL 26.4 feet landward of the 1997 ECL. That is the surveyed distance between the MHWL and SHWL in June 2005. Mr. Foster located the pre-project SHWL at the most landward location that the SHWL was surveyed in March 2002. The line is between 50 and 75 feet5 landward of the “best fine” line used by Mr. Foster as the pre-project MHWL, and it is as much as 25 feet landward of the surveyed location of the SHWL in some areas. Mr. Foster used “an average [of] 50 feet” as the MHWL- to-SHWL distance in his analysis of several prior permits in the vicinity of the Project.6 Mr. Foster testified that the distance between the MHWL and SHWL in this area varies “from the 20s in the immediate post-nourishment situations . . . all the way up to 70-some feet” and that the “the averages gravitate towards 40 feet.” Consistent with that testimony, the distance between the surveyed locations of the MHWL and SHWL depicted on Department Exhibit 6 is approximately 40 feet, on average. The MHWL-to-SHWL distance calculated by Mr. Walther is not a reasonable projection of the pre-project distance because it was based upon survey data taken immediately after a “major” beach nourishment when the shoreline was unnaturally steep and, hence, not representative of “pre-project” conditions. The SHWL located by Mr. Foster is also not a reasonable projection of the pre-project SHWL because it was based upon a March 2002 survey (which is clearly not "pre- project"); because it used the most landward surveyed location of the SHWL rather than a “best fit” line or an average of the distances between the surveyed MHWL and SHWL; and because it runs across areas of well-established dune vegetation. In sum, the MHWL-to-SHWL distance calculated by Mr. Walther (26.4 feet) is too low, whereas the distance resulting from Mr. Foster's siting of the SHWL based on the March 2002 survey (50 to 75 feet) is too high. Those distances are essentially endpoints of the range observed in this area, as described by Mr. Foster. A more reasonable estimate of the pre-project MHWL-to- SHWL distance is approximately 40 feet. See Findings 51 and 52. Thus, the pre-project SHWL is located 40 feet landward of and parallel to the SBHTL. That line is not depicted on any of the exhibits, but on Petitioner’s Exhibit 37, it roughly corresponds to a straight line between the points where the red- dashed line intersects the Property’s north and south boundaries. Step 3: Calculate the Erosion Rate The third step in determining the 30-year erosion projection is to calculate an erosion rate. The erosion rate used by Mr. Foster was -7 feet per year (ft/yr). That rate was calculated based upon an average of the shoreline change data for monument R-35 for the period from 1949 to 1967. The rate would have been higher had Mr. Foster averaged the rates for the nearby monuments.7 The erosion rate used by Mr. Walther was -4.9 ft/yr. That rate was calculated based upon an average of the shoreline change data for monuments R-34 to R-39 over the period of 1930 to 1968. An erosion rate of -7 ft/yr south of the inlet was referenced in permit applications submitted by Mr. Walter’s firm, Coastal Tech, for several shore protection structures south of the inlet; was used by Mr. Foster in his review of several prior CCCL permit applications south of the inlet; and was included in reports on the inlet prepared by the Army Corps of Engineers over the years. An erosion rate of -3.3 ft/yr was used and accepted by the Department in its review of another permit application in the general vicinity of the project.8 That erosion rate was based upon data from the period of 1972 to 1994, which is after the beach nourishment started south of the inlet. It is not entirely clear why Mr. Foster chose to use a data set starting in 1949, particularly since his report stated that the “1928-30 survey already shows significant erosion occurring south of the inlet.” His testimony did not adequately explain the choice of that data set. The use of a longer data set is typically more appropriate when calculating a historical rate. In this case, however, the use of the shorter period of 1949-68 is reasonable because the 1930-49 erosion rate was considerably lower than the 1949-68 rate,9 which has the effect of skewing the erosion rate calculated for the longer period of 1930-68. The higher erosion rate calculated by Mr. Foster also better takes into account the increased frequency of the nourishments in recent years as well as the continued need for shore stabilization in the area. In sum, the higher erosion rate of -7 ft/yr calculated by Mr. Foster using the 1949-68 data set better reflects the historical post-inlet, pre-nourishment erosion rate than does the lower erosion rate calculated by Mr. Walther. Step 4: Determine the Remaining Project Life The fourth step in determining the 30-year erosion projection is to determine the “remaining project life” of the “existing” beach nourishment project. It was stipulated that there are 14 years remaining until the currently authorized federal beach restoration project expires. It is reasonable to expect that beach nourishment south of the inlet will continue well beyond the expiration of the current federal project, but there were no other funded and permitted projects in place at the time Beach Group’s permit application was filed. Potential future beach nourishment projects are not considered “existing” under the rule methodology in Florida Administrative Code Rule 62B-33.024 unless they are funded and permitted at the time the application at issue is filed. Mr. Walther used the 14-year remaining life of the existing federal project in his calculation of the 30-year erosion projection, as did Mr. Foster. The “remaining project life” applicable to this case is 14 years, notwithstanding the likelihood of continued beach nourishment in the area beyond the expiration of the existing project. Step 5: Calculate the 30-year Erosion Projection The final step in determining the location of the 30- year erosion projection is a calculation using the variables determined in the previous steps. The calculation is as follows: first, the remaining project life determined in step four is subtracted from 30; then, that result is multiplied by the erosion rate determined in step three to get a distance; and, finally, the SHWL is moved that distance landward of its pre-project location determined in step two. Subtracting the remaining project of 14 years from 30 equals 16 years. Multiplying 16 years by the erosion rate of -7 ft/yr equals 112 feet, which means that the 30-year erosion line is located 112 feet landward of the pre-project SHWL (or 152 feet landward of the SBHTL). That line is not depicted on any of the exhibits, but it roughly corresponds to a straight line than runs across the Property parallel to the SBHTL just landward of the “conc. pad” and “existing conc. Pile caps (typ)” shown on Petitioner’s Exhibit 37. The line is 25 to 30 feet seaward of Mr. Foster’s 30-year erosion projection depicted on that exhibit. (3) Ultimate Finding Regarding the Location of the Proposed Structures in Relation to the 30-year Erosion Projection The Project includes major structures seaward of the 30-year erosion projection, as determined above. Impacts of the Project on the Beach-Dune System The Project includes 17 luxury town home units in two four-story buildings, a pool and spa, landscaping, and an elevated dune walkover. The units will range from 2,700 to 4,400 square feet of living space and are projected to be offered for sale in the $1.5 to $2.5 million range. Beach Group’s principal, Harold Seltzer, testified that the Project is sited as far landward as possible to allow for the development of all 17 units while still complying with the local setback and height restrictions; that the Project’s financial viability depends upon it being developed as proposed; and that the Project cannot be redesigned and remain financially viable. The CCCL permit application included a letter from the City of Ft. Pierce confirming that the Project is consistent with the applicable local development codes. Mr. Seltzer testified that the Project’s local development approvals expired in September 2006 because the CCCL permit had not been issued, and that Beach Group is having to go back through the local permitting process. The seaward extent of the Project is the 1978 CCCL, which is approximately 250 feet seaward of the current CCCL. The buildings on the adjacent properties are also located on the 1978 CCCL. The Project does not extend further seaward than the nearby development, including the structures authorized by the Department in File Nos. SL-162 and SL-173.10 The seaward boundary of the Property is the SBHTL. That line is approximately 295 feet landward of the MHWL established in June 2005, and as noted above, it is approximately 65 feet landward of the ECL established in 1997. The adjacent properties are developed with multi-story residential buildings. There is a densely vegetated dune feature in front of the building to the south of the Property. There is some vegetation, but no discernable dune in front of the building to the north of the Property. The Property as a whole is sparsely vegetated, but there are areas of “prolific vegetation” on the Property. The seaward extent of the vegetation on the Property roughly corresponds to the location of the 1978 CCCL. There are several mature sea grape clusters in the vicinity of that line. The beach in front of the Property is devoid of vegetation. It has a steep slope immediately landward of the water line; a wide (approximately 270 feet) expanse of relatively flat beach; and a gently sloping dune feature that starts just landward of the Property’s seaward boundary, crests approximately 30 feet farther landward, and then gradually slopes downward across the Property all of the way to State Road A1A. The dune feature on the Property is the frontal dune. It is the first mound sand located landward of the beach that has sufficient vegetation, height, continuity, and configuration to offer protective value. The crest of the frontal dune is seaward of the vegetation line on the Property, and ranges in height from +9.7 to +12.2 feet NAVD.11 The seaward toe of the dune is shown on the topographic survey for the Property at elevations ranging from +7.27 to +7.85 feet NAVD. Similar elevations occur on the landward side of the dune crest, just landward of the 1978 CCCL. The vegetation on the Property extends landward of the 1978 CCCL and landward of the line shown on the topographic survey of the Property as the “approximate location of sparse grass and ground cover.” The landward extent of the vegetation does not in and of itself define the landward extent of the dune; changes in the slope of the ground must also be considered. The more persuasive evidence establishes that the landward toe of the frontal dune is landward of the 1978 CCCL, but not as far landward as suggested by Department witness Tony McNeal.12 The landward toe of the dune on the Property is best defined by the elevations landward of the dune crest similar to the elevations shown for the seaward toe of the dune. The Project extends into the frontal dune on the Property, and it will requires minor excavation of the frontal dune, primarily in the area of the proposed pool. All aspects of the project, except for the proposed dune walkover, will be landward of the crest of the frontal dune and the mature sea grape clusters located on the dune. There will be no net excavation on the Property as a result of the Project. The sand excavated for the pool will be placed on-site, and additional beach-compatible sand will be used as fill for the site. Overall, the Project will result in the net placement of approximately 66 cubic yards of sand on the Property. The proposed structures will be elevated on piles, which will allow the beach-dune system to fluctuate under the structures during storm events. The finished floor elevation of the proposed structures is approximately +8 feet NAVD, which is slightly higher than the elevations associated with the toes of the frontal dune. The Project will not destabilize the frontal dune, even though it will encroach into the dune. The impacts of the Project on the beach-dune system will be mitigated by the placement of additional sand into the beach-dune system, as described above. The Project’s impacts will be further mitigated by the enhancements to the frontal dune described in the permit application. Mr. Walther testified that the frontal dune on the Property could “very easily” be enhanced to be of comparable height and magnitude of the dunes on the adjacent properties. The permit application proposes enhancements to the frontal dune as part of the Site Landscaping Plan for the Project. The proposed enhancements include increasing the crest of the dune to a height of +15 feet NAVD, and extensive planting of the dune with sea grapes, beach morning glories, and sea oats. The plantings would extend from the 1978 CCCL to the seaward toe of the existing frontal dune. The dune enhancements proposed in the permit application should be included as a specific condition of the CCCL permit for the Project, if it is approved.
Recommendation Based upon the foregoing findings of fact and conclusions of law, it is RECOMMENDED that the Department issue a final order denying Beach Group’s application for a CCCL permit. DONE AND ENTERED this 19th day of April, 2007, in Tallahassee, Leon County, Florida. S T. KENT WETHERELL, II Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 19th day of April, 2007.
The Issue The issue to be resolved in this proceeding concern whether the Respondents, the permit applicants, Daniel and Doris Wentz, are entitled to a Coastal Construction Control Line Permit allowing them to build a single-family home seaward of the coastal construction control line on Cape San Blas in Gulf County, Florida.
Findings Of Fact Daniel G. and Doris Wentz (Applicants) own property on Cape San Blas, Gulf County, Florida, between department monuments R-93 and R-94. The property is 65 feet wide and extends to the mean high water line of the Gulf of Mexico. When it was plated in 1980, the property was some 350 feet deep between the landward eastern-most boundary and the waterward or western-most boundary, which is at the mean high water line (MHWL) of the Gulf. About 47 percent of the property's total depth has eroded since that time, such that some 90 feet of the property, by 65 feet wide, lies landward of the crest of the artificial berm at issue. The proposed house will be built 20 feet from the landward rear property boundary (east boundary). The applicants propose to construct a pile-supported, single-family dwelling on that property with a wooden deck, pervious parking area, landward of the dwelling, a concrete slab under the dwelling and a septic tank and drain field to the southeast side of the dwelling. All these structures and improvements are seaward of the coastal construction control line established for Gulf County. The landward side of the dwelling to be located 20 feet seaward of the eastward or landward boundary of the property, cannot be located more landward or eastward due to local government set-back line requirements. The dwelling complies with all applicable department structural requirements. It is piling-supported and the lowest structural member is located above the department's design elevation. It meets all applicable wind load, wave, hydro-static and hydro-dynamic load requirements associated with a "100 year storm" event. The proposed dwelling would comply with all pertinent local set-back requirements, building code requirements and Gulf County growth management plan requirements. A permit has been issued authorizing construction of the septic tank and drain field, by Gulf County. "Freedom" Procedural Background This controversy originally arose when a prior owner of the property, Richard Price, submitted an application for a Coastal Construction Control Line Permit authorizing construction of a single family dwelling on the above-referenced parcel of property. That application was submitted on December 20, 1999, and on February 9, 2000, the new owners of the property, the Wentzes, submitted a similar application. The Department's Division of Water Resource Management and Office of Beaches and Coastal Systems requested the Florida Fish and Wildlife Conservation Commission (Commission) through its office of Environmental Services, to review the applicants' plans for the proposed house with a view to deciding whether the project would result in a take of marine turtles due to habitat destruction or similar considerations. The DEP, by policy, will not issue a coastal construction control line permit in the absence of such review or if commission review determines the project would result in a "take" with regard to marine turtles. On March 14, 2000, Bradley Hartman of the Commission's office of Environmental Services responded to the Department's request by stating that the project would result in a take of marine turtles through interference with breeding behaviors, as envisioned in Section 370.12(1)(c), Florida Statutes, and that therefore the application should be denied. On May 25, 2000, Director Hartman again wrote to DEP responding to a request for commission review of revised plans by the applicant, which showed that the dwelling would be proposed be located approximately 25 feet landward on the "frontal dune". The Commission again took the position that the revised project would constitute a "take" of marine turtles as well. Thereafter on May 30, 2000, the administrator of DEP's bureau of Beaches and Wetland Resources issued an assessment recommending denial of the applicants' application because it would constitute a "take" of marine turtles. The Department's position to initially choose to deny the permit application was also based on the fact that it believed that the proposed dwelling would be built upon the frontal dune on the property and beach system. Thereafter, on July 18, 2000, Director Hartman of the Commission notified DEP that the applicant had presented a plan to restore a dune on the property and moved the proposed dwelling to a more landward location. Director Hartman's letter thus stated that if both of these events occurred there would be no "take" of marine turtles. On June 27, 2002, DEP Administrator Anthony McNeil prepared an amended assessment of the applicants' pending project wherein he recommended granting the permit. The change in recommendation was based upon a March 2002 survey showing that a man-made dune had been constructed on the property "approximately 20 feet wide between he seaward and landward toes and has a crest elevation of plus 16.0 feet (NGVD)" or (National Geodetic Vertical Datum). The Department noticed issuance of the coastal construction control line permit (permit) on July 3, 2002. It had changed its position to a grant posture because the Department decided that the man-made dune satisfied the requirements so as to be considered a "frontal dune." If it were not considered a frontal dune (by complying with the relevant statutory qualities a frontal dune must have) the Department would be denying issuance of a permit, in accordance with Section 161.053, Florida Statutes. Description of Subject Property Five aerial photographs showed the applicants' two lots and the adjacent, upland, five-unit complex. The Petitioners own and reside in the northern-most unit, which is the unit appearing on the left side of their condominium building in the aerial photographs in Petitioners' exhibit three. The lot which is the subject of the proceeding is the northern-most lot of the applicants' two adjacent lots. It is immediately seaward of the Petitioners' condominium or townhouse unit. See Petitioners' Exhibit Three in evidence. The Northern boundary of the property is the boardwalk shown on the aerials. The only densely vegetated area, which includes woody species on the property, is where the proposed home would be built. That is the highest point on the subject property or approximately 14 to 15 feet NGVD. A second heavily vegetated area shown on the area photographs is not on the subject project and not at issue. The eastern-most portion of the proposed dwelling is 20 feet from the eastern most or landward property line of the applicants' lot. The roof provides an overhang for the entire house including the porch and the septic tank and drain field would be located southeast of the house on the same lot. An artificial berm or man-made dune was constructed on the property by the applicant on or about March 18, 2002. The property extends to about 90 feet behind or landward of the artificial berm or dune and the property is 65 feet wide. The house would be placed 20 feet seaward from the eastern-most or landward boundary of the subject lot, based upon requirements of the local government set-back from the easement along the eastern boundary of the property. Erosion of Beach and Dunes DEP survey monument, R-94, is about 150 feet from the property. The property is thus close enough from an engineering perspective that it is essentially subject to the same physiographic changes which are occurring in the vicinity of monument R-94. Survey data gathered by the State at the monument since 1973 creates an historical profile of the shoreline and the immediate vicinity of the property, including the subject property. Because of the progressive erosion of the local beach system since 1973, the DEP has been forced to relocate monument R-94 three times. All survey data at the monument has been adjusted so that it can be reliably compared over the period of record. The historical survey data at R-94 allows for reliable engineering estimates of shoreline change at this location. The shoreline of the property has exhibited an extremely high erosion rate over the years as to both the MHWL and the upland dune. On an eroding beach such as this one, dunes do not build up, but rather are lost as the MHWL recedes in a landward direction. A 1993 DEP aerial photo shows a home in the immediate vicinity of monument R-94 and seaward of the subject property. See Petitioner's Exhibit 15 in evidence. A 1998 aerial of that same area reveals that the house is no longer there. It was destroyed by Hurricane Opal in 1996 and ensuing erosion. If it were still there the house would be seaward of the present day MHWL. During the five year period from 1993 to 1998 the MHWL at R-94 monument receded 120 feet landward. From January 1998 to October 2002, the MHWL has receded another 50 feet. The shoreline in the vicinity of and including the subject property has eroded over a long period of time at a rapid rate such that it has actually eroded back into the piney flat woods ecological zone. There are numerous pine tree stumps on the active beach and surf zone. Indeed the whole Cape San Blas land form is retreating and rotating to the eastward. The seaward-most dune formations presently have mature pines growing on them, indicating a shoreline receding at such a rapid rate that it has progressed well into different vegetative eco- systems. The Cape San Blas spit has a north-south orientation of its shoreline, unlike any other orientation along most of the northern Gulf Coast mainland or barrier island land forms, which generally lie in a more east and west orientation. This orientation of Cape San Blas spit makes the shoreline more susceptible to wave energy and recession from being struck by waves at an angle rather than head-on or at a near perpendicular approach. Thus the Cape San Blas spit is more highly erosional. The beach in the vicinity of and including the subject property is moving backward and through the historical upland dune ridges. These historical dune ridges are not parallel to the present day shoreline orientation, but rather are at an angle, or more or less diagonal to the present day shoreline. Resultingly, there are sections of historical dunes which are on the existing beach front with gaps between them because they each represent the ends, on the beach, of separate historic dune ridges. The Frontal Dune A frontal dune is defined in Section 161.053(6)(a)(1), Florida Statutes, to be "the first natural or man-made mound or bluff of sand which is located landward of the beach and which has sufficient vegetation, height, continuity and configuration to offer protective value." There is no dispute that a frontal dune must provide protective value to upland property. The most densely vegetated area on the property, which includes woody species, is part of the natural frontal dune. That is, the dune existing at approximately a height of 14 feet NGVD upon which the subject house is proposed to be built. The property is extremely prone to erosion by any source of elevated wave energy and, in particular, that associated with tropical depressions or storms moving through the Gulf. The destruction of one-half of the man-made dune on the applicants' property about six months after its construction, by Tropical Storm Isadore in late September 2002, illustrates this point. That storm actually made landfall in the vicinity of Biloxi, Mississippi, approximately 200 miles west of the subject property. The storm, however, eroded a total of about 30 feet of beach at the property. The annual storm activity in the area of monument R-94 has sufficient wave energy to cause significant beach erosion at the property. According to DEP, when the artificial dune was constructed it was about 20 feet wide from the landward toe to the seaward toe and crested at approximately 16 feet in height. On September 12, 2002, the peak was about 15 feet. After Tropical Storm Isadore, the berm was half as wide. The entire forward or waterward slope of the original man-made dune had mostly eroded away leaving a sheer scarp or bluff. After Tropical Storm Isadore the dune crested at about nine to 14 feet. The return frequency of storm effects from distant storms, like those of Isadore at the subject property is about one to two-year frequency. This means that during an average year the remainder of the man-made dune at this location likely will be obliterated. The shoreline at the property as measured at monument R-94 has progressively receded landward since 1973. There is no history of episodic accretion or expansion of the shoreline; instead, the survey data uniformly indicates, for R-94, that there is a constant landward recession of the beach and dune face, due to continuous erosion. The seaward-most dune bluff in existence at hearing was the eroded face of the man-made dune. Half of that berm has disappeared due to erosion only short few months after it was constructed and in March 2002. The duration of the man-made dune on the property can be determined by calculating the documented recession rate of the dune formation historically located in the vicinity of the property. Application of this recession rate will reveal the likely life of the man-made dune and determine its potential protective value. Mr. Walther, the engineer who designed the berm, acknowledged that, indeed, the berm will eventually be eroded by storm events and might be obliterated within a year. Measurement by survey of the dunes at R-94 indicates that they have historically receded at a far greater rate than the MHWL. This is because the sand eroded from the dune line served to nourish the active beach face where the MHWL is located, so that it recedes landward at a slower rate than the dune line itself. Using the survey data for DEP monument R-94, the MHWL recession rate was calculated at seven feet per year. The dune recession rate landward at R-94 however is approximately 13 feet per year. The width of the remaining man- made dune is about 10 to 15 feet. Therefore, the dune recession rate calculated and in evidence, shown by witness Olson, illustrates that the remaining portion of the man-made dune will likely be lost to erosion in a year or a little more. That calculation and opinion is more persuasive and is accepted. The dune recession at R-94 was estimated using a 10 foot contour line. Any contour elevation number that reasonably represents the face of the eroding bluff of the artificial dune could be used. The result would be basically the same, that the house proposed to be constructed by the applicants' will be intercepted by the bluff line in less than three years, since the proposed dwelling is set back 31 feet from the seaward face of the artificial dune. Given a dune recession rate of 13 feet per year and taking into account that the man-made dune was constructed in March of 2002, it has been shown that the proposed dwelling will be most likely located on the active beach within five years. It will be subject to wave action on almost a daily basis. In ten years the limits of erosion would exceed the home and will reach the townhouses, including the Petitioners' townhouse, landward of the proposed dwelling. The applicants' proposed dwelling will be then totally stranded on the beach or destroyed, as shown by the testimony of expert engineer Eric Olson, which was unrefuted and is accepted. The seasonal high waterline (SHWL) will be at the proposed home in about 6.6 years from October of 2002. This finding is calculated by dividing the distance the house lies from the 2002 seasonal high waterline (46 feet) by seven feet per year, the erosion rate. That will mean that waves will run under the house on a daily basis within five years from October 2002. By that time there will be a sandy beach under the house back to the ten foot contour line. The dune recession rate provides a more reliable estimate of the maximum erosion limits at the property than does the SHWL. SHWL is intended to define the back portion of the day to day dynamic beach for most beaches in Florida. However, for Gulf County where this property is located, the elevation of the SHWL is not as good an indicator of the back portion of the beach because the local tides are mixed, i.e., two equal or near equal tides do not occur at this location on a daily basis and accordingly the elevation of mean high water or MHW, upon which the SHWL is based, is lower than the actual high water experienced. A more realistic indicator of erosion for this site is therefore the documented dune recession rate which was used to calculate the expected life of the man-made dune. The residential structure proposed will thus be completely on the active beach in a little over five years. That is, substantially before the 30-year period which statutorily defines the erosion line beyond which or seaward of which most construction is prohibited, except for single family residences under the exceptional circumstances provided in the statutes and rules addressed and at issue herein. Ten years hence, the SHWL will be under two-thirds of the home and the ground level of the house at the SHWL will be about plus 2.8 feet above sea level. Artificial Dune Characteristics The man-made dune lacks continuity. It is most vulnerable to wave and water penetration at its northerly terminus where it ends near the boardwalk and near the property line. It is not part of a contiguous dune system. The berm's flank or end-point will be the focal point of waive penetration and accelerated erosion due to the low elevation above the MHWL or SHWL, as the case may be, at that point. Due to the lack of continuity of the artificial dune, it will tend to collapse from its northerly end. There is not a dip in the dunes system between the property and the adjacent lot to the north which would still render it a continuous dune system. Instead there is no dune at all at that point. There is a gap in the system which has been caused over time by waves or tides, as well as the fact that the beach had eroded into the remnant dunes located in the piney flat woods area of Cape San Blas at the vicinity of and on the property. The shorter the dune is the easier it is for water to get around it and for wave action to destroy it. The man-made dune is 65 feet long. The short length of the artificial dune means it can not provide much protective value. Its expected effective life will be short, as demonstrated by Mr. Olson's opinions which are accepted. Prior to the construction of the man-made dune, as shown in the original site profile in the application, there was a natural grade from the water to the natural frontal dune. As a result of Tropical Storm Isadore the man-made dune has sharp escarpment on its waterward side and less height. Due to Tropical Storm Isadore, the man-made dune lost half its planted vegetation. The October 2002 aerial photographs contained in Petitioner's Exhibits 3 and 12A reveal that the remaining berm vegetation is sparse. Before Hurricane Opal struck in 1996 there was a large continuous dune formation, including a 15-foot high dune on the property near where the remainder of the man-made dune is now located. Hurricane Opal totally eroded that dune. It has not since rebuilt or restored. After Opal, and before the applicant constructed the man-made dune, the beach gently sloped to the naturally heavily vegetated dune on the 14-foot contour line. Opal had completely destroyed the more seaward dune that was on the property leaving no discernible mound of sand in that location. The heavily vegetated dune that still exists at the rear portion of the property is what protected the townhouses during Hurricane Opal. This is presently the only dune remnant on the property providing protective value to upland properties and structures. It is the natural frontal dune upon which the proposed home is proposed to be built. The proposed home will not be landward of that natural frontal dune. It will be built on top of that dune and its construction will somewhat lower the elevation of that dune by excavation to place the concrete slab and parking area which will exist under and landward of the house. This natural frontal dune crests at the present time, at about 14-15 feet and continues across the property and onto adjacent lots. The project when originally proposed in early 2002 could not be approved by the Department because the dwelling was to be situated on the frontal dune (the natural frontal dune). This view was memorialized in the DEP memo of January 8, 2002, in evidence as Petitioners' Exhibit 22 wherein it was provided: "staff advised the applicant representatives that review of its recent submittals it still considered the proposed structure as being not landward of the frontal dune, and therefore ineligible for a permit." In order to attempt to comply with the statutory requirements that the proposed dwelling be sited landward of the frontal dune, the applicant constructed the man-made dune seaward of the natural frontal dune, at the suggestion of the DEP administrator and ultimately with a DEP permit authorizing such construction. "Significant Adverse Impact" Assessment Rule 62B-33.005(3)(A), Florida Administrative Code The location of the proposed house appears to be an elevation of 12 to 13 feet above sea level. In 10 years when the proposed structure will be completely stranded in the water with no dune under it, 10 feet of the sand supporting the pilings will be gone. That will adversely affect the structural integrity of the house and the septic system will inoperable and exposed, possibly contaminating the surrounding beach-dune system. Vegetation Issue Rule 62B-33.005(4)(A), Florida Administrative Code Construction of the house will require removal of most of the dense vegetation atop the true frontal dune to make way for a concrete slab which will provide a parking area under the proposed home. The vegetation presently deters wind-borne erosion. A loss of vegetation and displacement of part of the dune by grading for the slab and the house will tend to destabilize the dune and diminish its protective ability for adjacent upland structures and property, including the Petitioners' property and residence. The natural frontal dune and related vegetation is what protected the Petitioners' townhouse during Hurricane Opal. Because construction of the proposed house will remove substantial vegetation and sand to make way for the slab, even if the sand is retained on the project site, in order to provide for under story parking, the protection presently afforded by the natural frontal dune will be diminished. Disturbance Of In Situ Sandy Soils Rule 62B-33.005(4)(B)(C), Florida Administrative Code The proposed house will be built on the highest point on the property which is presently at about 14 to 15 feet above sea level. Construction of the home will provide displacement or excavation of a portion of the sand atop the natural frontal dune in order to make way for the parking garage concrete slab under the home. Structure-Induced Scour Rule 62B-33.005(4)(D), Florida Administrative Code Subsequent to the recession of the shoreline the house may act similar to a groin feature, thereby somewhat accelerating localized erosion, particular upon the dune upon which it will be built. As the slab under the house is undermined its debris will increase the erosive impact of wave action on the beach system and nearby upland structures. Wind And Water-Borne-Missiles Rule 62B-33.005(4)(E), Florida Administrative Code When the existing shoreline recedes and the proposed home is on the active beach, it will pose a risk to upland structures, including the Petitioners' townhomes. The proposed home will then be only about 50 or 60 feet from the Petitioners' upland townhomes. The dune upon which the house would be built is the only natural feature which presently provides protection to the Petitioners' homes. During storms, portions of the structured part of the proposed home could be blown into upland structures. The air- borne missiles will include such things as stairways, garage doors and lower walls all of which are designed to be expendable. The proposed home was certified to withstand a 100 year storm. Consequently, that might dictate that with the wind loading it is certified to withstand, wind-borne missiles might be unlikely. However, the 100-year storm certification assumed that the home would be located on the upland at or above elevations of plus 10 feet and not on the active beach. The forces of the 100-year storm would be exaggerated when the dune is eroded away and the house is on the active beach. As the shoreline of the property recedes, deeper water will be below the proposed home, thereby creating a greater freeboard for storm surge elevation and more damage to the home from the higher waves. The size of a storm wave is proportional to the depth of water below the structure during the 100-year storm event. During and after Hurricane Opal in 1996, debris from the house that formerly was 200 to 300 feet seaward of the applicants' proposed home damaged the Petitioners' townhome and other units in that complex. The Petitioners' have had to pick up debris from that home for six to seven years following Hurricane Opal. The same thing will happen with projectiles or parts from the applicants' proposed home, but even more damage is likely since the home will be constructed only 50 to 60 feet away from the Petitioner's townhomes and directly seaward of them. Line Of Construction Rule 62B-33.005(7), Florida Administrative Code There is not a uniform and continuous line of construction associated with the siting of the proposed home. Impact To Marine Turtles Issue Adult female loggerhead and green turtles nest on the beaches of Cape San Blas. The vast majority of nesting adults are loggerheads. The marine turtle nesting season begins about May 1st of each year and ends October 31st. Female turtles come on the beach between the beginning of May and the middle of August to lay eggs. The eggs hatch between July and October. The Department approved the lighting plan for the Wentz dwelling designed to protect against adverse effects on marine turtles when they are nesting at night. That plan meets applicable rule requirements. Exterior lighting associated with the dwelling will not adversely affect marine turtles. The area where the dwelling will be located is not precisely marine turtle nesting habitat. There is no evidence that the area landward of the location of the present artificial dune has been used for nesting. Nesting data for the 2000, 2001, and 2002, nesting seasons for a six-mile beach segment, including the beach adjacent to the subject property, indicates that only one nest (nest number 51) was laid immediately adjacent to the property over that three-year period (not directly on the property). It was laid seaward and near the western end of the man-made dune. It is highly unlikely that a turtle would nest in the area of the dwelling. The area landward of the scarp of the man-made dune, which includes the location of the dwelling, is not viable marine turtle nesting habitat. This is primarily because it is currently a vegetative area and turtles do not typically venture to any extent into a vegetative area to dig their nest and lay eggs. It is landward of the scarp or bluff on the man-made dune, which is difficult for turtles to climb over. The scarp on the seaward face of the man-made dune varies between 9 and 14 feet in height, dropping off to essentially no scarp or one and one-half feet on its northward end. It would largely prevent marine turtles climbing over and nesting landward of the man-made dune scarp with the possible exception of the gap, referenced above, at the northward end of the man- made dune on or about the property boundary. The boardwalk which goes seaward from the Petitioners' townhomes at that point, would, however, to a great extent prevent sea turtles from migrating landward of the line of the artificial dune scarp. Based on the 2000-2002 nesting data for Cape San Blas, the vast majority of Marine turtle nests are laid waterward of the vegetation line. More specifically, 48.4 percent of the nest were laid within the area 10 seaward of the vegetation line near the toe of the frontal dune, while another 37.5 percent were laid further waterward of the frontal dune. Thus approximately 85 percent of the nests are waterward of the vegetation line. Consequently, the vast majority of any nests that might be laid on the property in question would be seaward of the vegetation line and the toe of the man-made dune (or scarp-face) and not in the upland vegetated area of the dune system where the house would be located. The dwelling is well landward of that vegetation line. In terms of survival, the best place and the location preferred by marine turtles, for the placement of eggs is at or near the toe of the frontal dune. The survivorship of nests landward of the vegetation line is low, due in part to predation. The likelihood that a marine turtle will nest within the 65-foot wide property is very low. Based on nesting density data for Cape San Blas and the width of this property, only 0.52 nests within the 65-foot wide property would be expected on a yearly basis. That translates to about one nest every two years. The likelihood that a nest would be laid within the property boundaries and landward of the vegetation line is considerably lower. Based on the same nesting data and the fact that 86 percent of the nests are laid waterward of the vegetation line, a nest landward of the vegetation line on the property would be expected statistically only about once every 13.5 years. Based on nesting data only one green turtle nest every 100 years would statistically be expected to be on the property. Even though the northwest end of the man-made dune is much lower than the remainder of the dune, it is unlikely a nesting adult would be able to nest in the area of the proposed dwelling by gaining access through this lower area. Approximately 91.4 percent emerging nesting adult turtles follow a straight path up the beach. Thus, turtles emerging on either side of that low spot would not veer to that low spot to seek a place to nest. Furthermore the boardwalk is located at the low spot and would act as a barrier that would prevent turtles from nesting landward of the man-made dune in the area of the low spot. The area behind the man-made dune is insignificant in comparison to the nesting habitat on Cape San Blas generally, within the nest survey area encompassed by the Petitioners' witness Martha Pridgeon. There are more than 3,168,000 square feet of nesting habitat within the Cape San Blas survey area, while the area on the property behind the man-made dune is approximately 3,900 square feet, which is well less than 0.1 percent of the nesting habitat within the survey area. Turtle nesting densities in southeast Florida are 64 times greater than on the beaches of northwest Florida, including Gulf County. Turtle nesting in northwest Florida is a relatively minor component of statewide nesting density. In the 1999 nesting season, there was approximately 81,000 loggerhead nests in Florida. Based on average clutch size, that would mean approximately 9,480,000 eggs were laid in Florida that year, by loggerheads at least. Given that only one nest would be anticipated on this property every two years, the number of eggs that might be laid on the property is inconsequential. Even if a nesting turtle encounters the dwelling, the encounter may well result in a false crawl. However, approximately 48 percent of nesting emergences by turtles result in false crawls. False crawls do not injure the turtle and are considered normal behavior. If eggs were deposited near the dwelling, any alteration of sex ratios in the hatchlings due to shading of the nest would be inconsequential in view of the 9,000,000 eggs laid in Florida each year. Moreover, if a nest was deposited near the dwelling it could be relocated to avoid any potential harm since nests are routinely, successfully moved to avoid harmful conditions. Adverse impacts to turtle eggs do not play a critical role in turtle survival. Rather, the nesting female is the critical link. Egg mortality is naturally very high. The survival strategy of marine turtles is to lay a large number of eggs. Even if the dwelling caused the loss of one nest every two years that loss would be insignificant. The loss of nests due to natural conditions on Cape San Blas is not unexpected or unusual. For example all remaining nests, at least 21, were destroyed during the 2002 nesting season by Tropical Storm Isadore. In that same year, at least six nests were destroyed by predators on Cape San Blas in the area of the subject property. Construction and use of the dwelling would not actually kill or injure a marine turtle, nor would it impair essential behavioral patterns of marine turtles. Construction and use of the dwelling would not impair the feeding or sheltering of marine turtles. Construction and use of the dwelling would not impair turtle breeding. Construction and use of the dwelling would not cause significant habitat modification or degradation that would actually kill or injure a marine turtle. In summary, the preponderant evidence does not establish that a take of marine turtles caused by significant habitat modification, degradation or any of the other reasons found above will occur.
Recommendation Having considered the foregoing Findings of Fact and Conclusions of Law, the evidence of record, the candor and demeanor of the witnesses, and the pleadings and arguments of the parties, it is, therefore, RECOMMENDED that a final order be entered by the Department of Environmental Protection denying the applicants' application for a permit pursuant to Section 161.053, Florida Statutes, for construction seaward of the coastal construction control line in Gulf County, Florida. DONE AND ENTERED this 5th day of June, 2003, in Tallahassee, Leon County, Florida. P. MICHAEL RUFF Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 5th day of June, 2003. COPIES FURNISHED: Kenneth G. Oertel, Esquire Patricia A. Renovitch, Esquire Oertel, Hoffman, Fernandez & Cole, P.A. 301 South Bronough Street, Fifth Floor Tallahassee, Florida 32301 Charles T. Collette, Esquire Department of Environmental Protection Office of General Counsel 3900 Commonwealth Boulevard, Mail Stop-35 Tallahassee, Florida 32399-3000 Thomas G. Tomasello, P.A. 1107 Terrace Street Tallahassee, Florida 32303 Teri L. Donaldson, General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop-35 Tallahassee, Florida 32399-3000 Kathy C. Carter, Agency Clerk Office of the Attorney General Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Stop-35 Tallahassee, Florida 32399-3000
The Issue The issue for determination is whether Petitioners are eligible for a permit, pursuant to Section 161.053, Florida Statutes, for construction seaward of the Coastal Construction Control Line in Broward County, Florida.
Findings Of Fact On November 30, 1993, Vander Ploeg and Associates, Inc., on behalf of Paul Leto, Richard Meyer, and Berta Anderes (Petitioners) submitted an application to the Florida Department of Environmental Protection (Respondent) for a permit to perform construction on their property seaward of the Broward County Coastal Construction Control Line. Respondent deemed their application complete on April 18, 1994. Petitioners proposed construction will be seaward of the Coastal Construction Control Line. The proposed construction will occur on two adjacent lots in Broward County. Petitioner Leto is the owner of one of the lots described as Lot 19, Block 196, Hollywood Central Beach, Plat Book 4, Page 20, Public Records of Broward County. Petitioners Meyer and Anderes are the owners of the other lot described as Lot 20, Block 196, Hollywood Central Beach, Plat Book 4, Page 20, Public Records of Broward County. Petitioner Leto purchased his lot in September 1992 and Petitioners Meyer and Anderes purchased their lot in March 1993. The lots were platted in or around the 1920's. Both lots are seaward of the seasonal high water line, on a sandy beach with no frontal dune structure. They are bordered by the Atlantic Ocean on the eastern most side and by a roadway (Surf Road) which is immediately adjacent to the lots on the western most side and landward of the lots. Approximately 200 feet north of the lots is an existing structure and approximately 800 feet south of this first existing structure is another existing structure. Petitioners topographical survey, which was submitted to Respondent in December 1993, showed that Lots 19 and 20, each measured 40 feet in a shore parallel direction and 80 feet in a shore normal direction, i.e., perpendicular to the shoreline. The proposed structure will be located directly on the sandy beach. The City of Hollywood, Florida has granted Petitioners a variance. Further, the proposed construction complies with the rules, zoning regulations, and ordinances of the City of Hollywood. Petitioners' application requests a permit for the construction of a single-family residence on the lots, which will house two families. However, the proposed construction is for a duplex, not a single-family residence. Petitioners are willing, and agreeable, to changing the design of the proposed structure to comply with Respondent's specifications for a single- family residence. Additionally, the proposed construction includes a riprap which will also be located on the sandy beach. A riprap is typically used for protective armoring. No structure presently exists for the riprap to protect. Furthermore, the riprap proposed by Petitioners is not adequately designed as a coastal protection structure, and if the proposed single-family residence is modified in accordance with Respondent's specifications, the proposed modified single-family residence would not be eligible for coastal armoring. The riprap structure is not an integral part of the structural design. Petitioners are willing, and agreeable, to eliminating the riprap structure. No other issues exist as to the structural integrity of the design of the proposed project. The lots on which the proposed structure will be located are a part of the beach-dune system. The natural function of the beach provides protection to upland property. The lots on which the proposed structure will be located are subject to normal storm-induced erosion. Tide and wave forces will impact the proposed structure during storms of minor intensity, including five-year storms. The proposed structure will induce greater erosion on the lots as a result of scour due to the interaction of the storm waves and currents with the proposed structure. During the storm, the normal storm-induced erosion combined with the scour erosion will form a breach or depression in the subject property. In turn, the upland property will be exposed to greater tide and wave forces, increasing the risk of erosion and damage to the upland property. The subject lots and surrounding properties have been subjected to unnatural forces which have added to the erosion. The Port Everglades inlet has inhibited the natural downdrift of sand. The City of Hollywood's beach maintenance division has been regularly pushing sand seaward and in the process, breaking down natural forming cliffs. Even though these unnatural forces are capable of being eliminated, the normal storm-induced erosion and the scour erosion would still exists. The existing developed structures to the north and south of the subject lots appear to create a reasonably uniform line of construction. However, the developed structures have been unduly affected by erosion. The proposed structure will be located within this line of construction. During a major storm along the shoreline, waves remove sand from the beach and dune area and deposit the sand in an offshore bar. After the major storm, a recovery of the beach and dunes takes place. Normal wave activity carries the sand from the offshore bar back to the beach, and the sand is then carried landward by winds and is caught and trapped by dune vegetation; thereby reforming a dune. Constructing the structure as proposed will not locate the structure a sufficient distance landward of the beach-dune system. As a result, the proposed structure will interrupt natural fluctuation in the shoreline and not preserve the natural recovery following the storm-induced erosion. The cumulative impact on the beach-dune system by the proposed structure would be severe, i.e., the effects on the beach-dune system by repeating this same proposed structure along the subject shoreline would be severe. There would be structure-induced scour and general degradation of the beach-dune system. Additionally, the recovery potential of the subject area following a major storm event would be threatened. Over the years, the beach of the subject property has been subjected to a re-nourishment project consisting of pumping sand from offshore. This method of re-nourishment may have negatively impacted the sand bar system immediately offshore affecting the hindrance of erosion. A sand bar system immediately offshore softens wave action on the shore and aids in inhibiting erosion. The proposed structure will hinder lateral public beach access. Currently, lateral beach access exists along the beach between the existing northern developed property and the existing southern developed property. The proposed structure will be located on the sandy beach, and the seaward face of the proposed structure will be within approximately one foot of the wet sand beach. At times, the proposed structure will be surrounded by water on at least three sides. No alternative beach access would be available. The proposed riprap will also be located on the sandy beach and will further hinder lateral public beach access. 2/ Loggerhead turtles, which are nesting marine turtles, engage in nesting activities along the stretch of beach where the subject property is located. They are a threatened species, i. e., close to extension. Although they do not nest every year, the turtles usually provide several nests in a single year. Typically, one hundred eggs comprise a turtle nest. In 1992, approximately 2,221 loggerhead turtle nests were in Broward County, with 22 of these nests located within 1,000 feet of the subject property. Turtle nesting efforts have been observed in the beach area of the subject property. One nest was found within the subject property. Structures located on the sandy beach interfere with marine turtle nesting habits. If female turtles make contact with the structures, they often abort nesting attempts, which results in false crawls. Repetitive false crawls harms successful nesting, which may cause malformed egg chambers, impacting the successful incubation of the nest. Also, interaction with a structure can cause injury or death to a female turtle attempting to nest. Additionally, urbanization activity and lighting on the beach deter nesting. A loss of marine turtle nesting habitat will result if the proposed structure is constructed. Also, armoring, such as the proposed riprap, can result in nests being placed more seaward. 3/ Consequently, the nests would be threatened with tidal inundation, which would affect the mortality of the nest itself. As one nest has been located within the subject property, at least one nest or crawl per year would be affected by the proposed structure. Within 30 years, the proposed structure will be seaward of the seasonal high water line. The location of the proposed structure is seaward of the 30-year erosion projection for the subject property. Beach Defense Fund, Inc. (Intervenor) presented no evidence to show that its interest is different than the public at large and that it has substantial interest separate and apart from the public.
Recommendation Based on the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that the Department of Environmental Protection enter a final order denying the application of Paul Leto, Richard Meyer, and Berta Anderes for a permit, pursuant to Section 161.053, Florida Statutes, for construction seaward of the Coastal Construction Control Line in Broward County, Florida. DONE AND ENTERED this 31st day of May, 1996, in Tallahassee, Leon County, Florida. ERROL H. POWELL, Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 31st day of May, 1996.
The Issue Whether the Petitioners have standing to initiate this proceeding? Whether the Intervenors have standing to intervene? Whether the Department should enter a final order that issues the JCP and the Variance?
Findings Of Fact The Parties The Sherry Petitioners and Their Property David and Rebecca Sherry, husband and wife, are the leaseholders of "Apartment No. 511 [a condominium unit] of Surf Dweller Condominium, a condominium with such apartment's fractional share of common and limited elements as per Declaration thereof recorded in Official Records . . . of Okaloosa County, Florida." WD Ex. P-8, Bates stamped PET7157. Their address is 554 Coral Court, #511, Fort Walton Beach, Florida 32548. The Sherrys leased their condominium unit in May 2002 in anticipation of it being their retirement home. After retirement, "towards the end of 2005," WD tr. 840, the unit became their permanent residence. They chose their home after an extensive search for the best beach in America on which to reside. The couple toured the Gulf Coast of Florida, the Keys and the Atlantic seaboard from South Florida into the Carolinas. Both explained at hearing why they picked the Panhandle of Florida in general and selected the Surf Dweller Condominium in particular as the place that they would live during retirement. Mr. Sherry testified: This particular area we chose because of the beach quality. Quite frankly, . . . I was surprised when I first saw the place . . . the really stunning quality of it. The sand is absolutely beautiful. The water has that clear green hue. You can walk off shore and it just looks great. There isn't any other place like it in the Continental US that I've ever seen. WD Tr. 841. Mrs. Sherry elaborated about the reasons for their choice to reside on the beach adjacent to the Surf Dweller and their enjoyment of the beach in the Okaloosa Island area of Santa Rosa Island. "We moved here for the quality of the beach, the sugar white sand." Tr. 936, Case No. 10-0515 (emphasis added). She explained that both she and her husband walk or run the beach daily. Mr. Sherry always runs; Mrs. Sherry's routine is to walk and run alternately. There are other distinctions in their daily traverses over the sugar white sand of Okaloosa Island. Mr. Sherry sometimes runs in shoes. As for Mrs. Sherry, however, she professed, I always run barefoot. I always walk barefoot and I take longer walks than he does. He runs the whole Island. I walk the whole Island and I run 3 miles at a time of the Island. So, that's the difference in the way we use [the beach.] Id. Mrs. Sherry described her activities on the beach more fully and how she enjoys it: I . . . swim. I surf on the skim board, float out in the water . . . I help Dave fish, we crab, . . . all sorts of things like that for recreation. Pretty much a beach person. I sit down on the beach under an umbrella with a lot of sunscreen. * * * I've always run barefoot. That's the reason [we chose the beach next to the Surf Dweller], it's not only the quality of the sand, [it's also] the fact that it's so soft because as I've aged, my husband and I have both been running for 30 years. He's in much better shape. I can still run barefoot and I can do a good pace, but if I've got shoes on, it's not nearly as much fun and I don't do nearly as much of it. So, to me, being able to have the squeak [of the sand underfoot], which you don't have with the restored sand is a big deal and having to wear shoes is a big deal. I really like to . . . [cross the beach] barefoot. WD Tr. 939. I actually think the project will impact me, at least, as much as my husband, David . . . my husband is . . . involved with . . . being board president of the Surf Dweller[.] I spend at least as much time as he does on the beach. And the way our furniture is arranged in the unit, it's so that when I'm in the kitchen, I bake the cookies, I see the beach, when I'm at the computer I can see the beach. I've got all the best views. So, I think I'm . . . extremely involved with it. It's the first thing I see in the morning; it's the last thing I see at night and I'm down there every morning. In fact, I was on the beach this morning before we came in . . . I don't miss my morning walk. Tr. 950, 10-0515. The Surf Dweller Condominium is located in Block 5 of Santa Rosa Island, Okaloosa County, on real property that was deeded to the County by the federal government and then subsequently leased out by the County under long-term leases. The legal description of the Surf Dweller Condominium is: LOTS 257 TO 261, INCLUSIVE, LOTS 279, 280, 281, BLOCK 5, SANTA ROSA ISLAND, PLAT BOOK 2, PAGE 84, OKALOOSA COUNTY. WD Ex. P-8, PET7158. Block 5 of Santa Rosa Island is subject to Protective Covenants and Restrictions adopted by the Okaloosa Island Authority in 1955 and recorded in the Official Records of the County at BOOK 121, PAGES 233-250. See WD County Ex. 13. The Protective Covenants and Restrictions set up four classifications of areas denominated as Zones B-1 through B-4. See id., Part B: Areas of Application, at BOOK 121 Page 235. Block 5 of Santa Rosa Island is in Zone B-2, "Apartment, Hotel Court and Hotel Areas." Id. at BOOK 121 PAGE 236. Part F of the Protective Covenants and Restrictions, provides, in part, Beach Protection * * * The beaches, for 300 feet inland from mean water level (or to the dune crest line, whichever is the greater distance), are under strict control of the Authority . . . One hundred fifty feet inland from the mean water line, in front of all B1 and B2 Areas, will be public beaches. The next 150 ft. inland will be private beaches as set out on subdivision plats . . . WD County Ex. 13, at page marked "BOOK 121 PAGE 242." The Surf Dweller Condominium Property, lying between reference monuments R-6 and R-7, does not extend as far south as the mean high water line ("MHWL") of the Gulf of Mexico. From testimony provided by Mr. Sherry, see below, it appears that the Surf Dweller Condominium Property is deeded to the border with the beaches governed by Part F of the Protective Covenants and Restrictions. Mr. Donovan and His Property John Donovan is the leaseholder of "APARTMENT NO. 131 AND APARTMENT NO. 132, OF EL MATADOR, A CONDOMINIUM AS PER DECLARATION THEREOF, AS RECORDED IN . . . THE PUBLIC RECORDS OF OKALOOSA COUNTY, FLORIDA." WD Ex. P-7, PARTIAL ASSIGNMENT OF SUBLEASE, Bates stamped PET7067. The address of the El Matador is 909 Santa Rosa Boulevard, Fort Walton Beach, Florida 32548. Mr. Donovan is not a resident of the State of Florida. His primary residence is in the State of Georgia. Mr. Donovan described in testimony his use and the use of his family of the beach seaward of El Matador and other parts of the Okaloosa Island area of Santa Rosa Island: I've . . . got to walk [for reasons of health] and I do walking every day I'm down here[.] I get all the way down to East Pass. I don't get down there every day, but I get down there a lot. My sons and my one grandchild take great pleasure in fishing off there, right at the end where the East Pass is right from the surf. * * * I swim. I don't swim probably as much as my co-petitioners [the Sherrys], but I'm sure I go out further. And I don't surf like David [Sherry] does but my grandchild would never tell me that I don't. I run as much as I can. Not as much as I used to. We also take long walks. WD Tr. 973-4. In a plat of El Matador Condominium introduced into evidence as part of Exhibit P-7, El Matador is described as: A CONDOMINIUM OF LOTS 557 THROUGH 590 INCLUSIVE, BLOCK 9 AND THE INCLUDED PORTION OF PORPOISE DRIVE THEREOF SANTA ROSA ISLAND A SUBDIVISION OF BLOCK 9 A RESUBDIVISION OF BLOCK 8 AS RECORDED IN PLAT BOOK 2, PAGE 190, PUBLIC RECORDS OF OKALOOSA COUNTY, FLORIDA Exhibit P-7, last page (un-numbered). Block 8 of Santa Rosa Island (like Block 5 in which the Surf Dweller Condominium is located) is also in Zone B-2 set up by the Protective Covenants and Restrictions. Block 8, just as Block 5, is governed by Part F, Beach Protection, of the Protective Covenants and Restrictions that places the beaches, for at least 300 feet inland, of the segment of Santa Rosa Island to which Block 8 is adjacent under the strict control of the County and makes the first 150 feet inland from the MHWL "public beaches." County WD 13, at page marked "BOOK 121 PAGE 242." El Matador Condominium is between reference monuments R-1 and R-2. It is not deeded to the MHWL of the Gulf. The plat in County Exhibit 13 shows the southern edge of the El Matador condominium property to be adjacent to the "FREEHOLDERS BEACH," see Exhibit P-7, last page (un-numbered), that is, to the edge of the area of the private beach designated under the "Beach Protection" provision of the Protective Covenants and Restrictions. The public beach designated by the same provision is seaward of the private beach. Concerns of the Sherrys and Mr. Donovan The Surf Dweller Condominium Property that serves the Sherrys' condominium unit and the El Matador Condominium Property that serves Mr. Donovan's condominium unit are along the segment of the beaches and shores of Okaloosa County that will be restored by the Okaloosa Island Project. The Sherrys and Mr. Donovan initiated this proceeding because they are opposed to the Okaloosa Island Project. One of the grounds for their opposition concerns the Project's borrow area to be used as a source of sand. It is offshore but relatively close to the beach immediately landward of the Sherry and Donovan condominium units. The Sherrys and Mr. Donovan presented evidence that the borrow area is sited and situated in such a way that once dredged it will cause impacts to the shoreline of Okaloosa Island. The impacts, they believe, in turn will affect their use and enjoyment of the beach. Mr. Donovan is concerned about the erosion and turbidity impacts that dredging the borrow site which serves the Project could have on the Gulf and the beach. Erosion would change his view of the beach from the window of his condominium unit and aggravate a scalloping of the shore. The unevenness of the scalloped surface would cause him difficulties in his walks. He is concerned that turbidity could attract sharks which would make it unsafe for him to swim. Most importantly to him, the change in the beach and shoreline along the El Matador Condominium property contemplated by the Draft JCP could deter his family members (his grandchild included) from visiting him and vacationing at his unit in the El Matador Condominium. The Sherrys and Mr. Donovan have other concerns about the Project. For example, they believe that the sand used in the restoration will not be compatible with Okaloosa Island's "sugar white" sand. They also are concerned about the impact that placement of the sand will have on their view, their walks and their runs and the many ways in which they use and enjoy the beach. Furthermore, they presented evidence that the cost of the Project will outweigh its benefit. The Intervenors Intervenors John Dezzutto and Thomas Wilson own condominium units 102-D and 101-B in the Seaspray Condominium located at 1530 Miracle Strip Parkway, Fort Walton Beach, Florida 32548. At its southern boundary the property that is subject to the declaration of condominium that created the Seaspray Condominium (the "Seaspray Condominium Property") is deeded to the MHWL. Hence, the Seaspray Condominium Property is considered to be "gulf-front." Intervenor David Wallace owns Unit 502 in the Destin West Beach and Bay Resort Condominium located at 1515 Miracle Strip Parkway, Fort Walton Beach, Florida 32548. Similar to the Seaspray Condominium, at its southern boundary the property that is subject to the declaration of condominium that created the Destin West Beach and Bay Resort Condominium (the "Destin West Beach and Bay Resort Condominium Property") is deeded to the MHWL. The property, therefore, is considered to be "gulf- front." The Seaspray Condominium Property and the Destin West Beach and Bay Resort Condominium Property overlap the beaches that are to be restored by the Project. If the County is to restore the area of the beach that is on the condominium properties of the two condominiums in which the Intervenors own condominium units, it will need to heed the advice of General Condition Six in the Draft JCP which is interpreted by the Department as a warning against trespass as well as provide authorization for such use from the property owner as required by the Draft JCP. The County and the Department Okaloosa County is a political subdivision of the State of Florida and the applicant for the JCP and the Variance. The Department is the state agency responsible for administration of the state's regulatory authority as found in Part I of the Beach and Shore Preservation Act, chapter 161, Florida Statutes, and in particular, for the issuance of permits required by section 161.041 and the concurrent processing of "joint coastal permits" as allowed by section 161.055. It also serves as staff to the Board of Trustees of the Internal Improvement Fund and in that capacity handles the processing and issuance of SSL Authorizations. Okaloosa Island Okaloosa Island is not an island. It is an unincorporated area of Santa Rosa Island. Santa Rosa Island is a barrier island that runs along much of the coast of the Panhandle of Florida. As explained by Mr. Clark at the final hearing, one is "in" Okaloosa Island while being "on" Santa Rosa Island. Okaloosa Island was conveyed to the County by the federal government and then leased by the County under long-term leases. The Surf Dweller and El Matador Condominium Properties (with units that belong to the Sherrys and Mr. Donovan, respectively), are in Okaloosa Island. Some of the other leaseholders in Okaloosa Island opted to have their leases converted to ownership of the leased property in fee simple. The Surf Dweller and El Matador Condominium Properties remain under long-term leases. Dry Beach Adjacent to Surf Dweller and El Matador Beginning with Hurricane Opal in 1995, the beaches and shores adjacent to the Surf Dweller and El Matador Condominium Properties were seriously damaged. Nonetheless, there is a significant stretch of dry beach between the Surf Dweller and El Matador condominium properties and the MHWL of the Gulf. In the case of the Surf Dweller Property, Mr. Sherry estimated the width of the beach between the condominium property and the MHWL to be 300 feet. See his testimony quoted, below. The MHWL of the Gulf of Mexico is a dynamic line, subject to constant change from the natural influences of the coastal system. Whatever effect its ever-changing nature might have on the width of the beaches between the MHWL and the Surf Dweller and El Matador condominium properties, at the time of hearing, there existed a 150 foot-wide stretch of beach water- ward of the two condominiums that the public has the right to occupy and use. David Sherry confirmed as much when he related the actual practice by the public in using it and the response that public use generated from him and his wife in the following colloquy on cross-examination by Mr. Hall for the County: Q If someone . . . crosses Santa Rosa Boulevard and utilizes this access[-]way that's marked on the map that you identified earlier, do they have the right to utilize any of the portion of [the private beach] of that 150-foot portion in front of your condominium? A . . . [N]o, they wouldn't have the right to do that. Q . . . [D]o they have the ability to set up an umbrella or place their towel within that 150-foot area [of private beach] in front of your condominium? A In that area, no. In the area south of that [the public beach] , which is where everyone actually sets up and wants to set up, in that area south, people set up and we don't have any problem with that. We let people do it -- Q On [the] public beach[.] A On the public beach they're perfectly free to do that. * * * Q I believe your testimony today, based on your GPS calculations, was that you have 300 feet of dry sand beach . . . running from the boundary of the condominium to the edge of the Gulf of Mexico; is that correct? A Essentially, from the building to the Gulf of Mexico. * * * Q So, 300 feet, roughly, from the boundary of the Surf Dweller Condominium common area down to the waterline? A Correct. Q So, there would be enough room today, based on the language of the restrictive covenants to have . . . 150 feet of public beach and then the 150 feet of Freeholders Beach as designated on the plat [in County Exhibit 13] now? A Much like it was in 1955 [when the Protective Covenants and Restrictions were adopted and recorded], yes. WD Tr. 891-3 (emphasis added). Since the first 150 feet of beach landward of the MHWL under the Protective Covenants and Restrictions is "public beach," there is no doubt that there is a stretch of beach between the Surf Dweller Condominium and the MHWL that is public beach, and it has a width of 150 feet. From aerial photographs introduced into evidence, the same finding is made with regard to beach that is public between El Matador and the MHWL of the Gulf. Mr. Donovan testified that his leasehold interest in his units at El Matador along with the interests of the other El Matador condominium unit leaseholders included 150 feet of private beach landward of the 150 feet of public beach adjacent to the MHWL of the Gulf of Mexico. His lawyer, moreover, advised him not to convert his leasehold interest into a fee simple ownership in order to protect his interest in access to the private beach designated by the Protective Covenants and Restrictions. See WD Tr. 986-87. Opal and Okaloosa Island Beaches Today Hurricane Opal made landfall near Pensacola in October 1995. Prior to Hurricane Opal, the shoreline in Okaloosa Island had been stable. The width of the vegetated and upper berm and dune systems had been about 175 feet and the un- vegetated beach seaward of the dune system about 100 feet wide. Upland development was protected from storm surge and wave action by a good 285-foot width of dune system and beach. Opal devastated much of the Florida Panhandle. Okaloosa Island was not spared. The shoreline of Okaloosa Island both advanced and retreated. The western half of Okaloosa Island (west of R-8) showed shoreline recession, that is, the shoreline on the western half retreated landward. The shoreline on the eastern half (east of R-8) advanced water-ward. The dune system, however, was destroyed. From the point of protection the beaches and the dune system offer upland development, moreover, the advance of the beaches in the eastern half of Okaloosa Island did not offset the damage done from volumetric reduction of the sand that the eastern half of Okaloosa Island suffered. As for Okaloosa Island as a whole, the area lost considerable sand volume. Opal's damage to Okaloosa Island, in sum, consisted of substantial loss of sand volume, significant deflation of beach profile and erosion of the dune and beach system throughout the area. After Opal, the general trend along Okaloosa Island was recession. Based on an overall average, the recession measured about minus 7 feet per year. See OI Tr. 561. The Okaloosa Island shoreline moved toward upland development. Despite the general retreat of the shoreline, in some areas of Okaloosa Island, the beaches appear to the untrained eye to be healthy because they are usable and quite wide. But even at their widest points, Okaloosa Island beaches are "very low and flat" OI tr. 562. The only dunes (where there are any at all) are "insignificant manmade dunes," id., that do not protect upland development. In short, Okaloosa Island is in need of coastal protection. It is "completely vulnerable to the impact of a storm surge or waves from, not only a hurricane, but lesser storms . . . ." OI Tr. 536. Critically Eroded Shoreline Florida Administrative Code Chapter 62B-36 governs the Beach Management Funding Assistance Program. It contains the following definition of "Critically Eroded Shoreline": "Critically Eroded Shoreline" is a segment of shoreline where natural processes or human activities have caused, or contributed to, erosion and recession of the beach and dune system to such a degree that upland development, recreational interests, wildlife habitat or important cultural resources are threatened or lost. Critically eroded shoreline may also include adjacent segments or gaps between identified critical erosion areas which, although they may be stable or slightly erosional now, their inclusion is necessary for continuity of management of the coastal system or for the design integrity of adjacent beach management projects. Fla. Admin. Code R. 62B-36.002(4) (the "Critically Eroded Shoreline Definition"). The Department determines whether upland development, recreational interests, wildlife habitat or cultural resources are threatened or lost based on a 25-year storm event. In 2005, the Department designated the area subject to the Okaloosa Island Project as having a "critically eroded shoreline." The designation was in accordance with the Critically Eroded Shoreline Definition and based on post-storm vulnerability after Hurricane Ivan which made landfall in the United States in September of 2004. An investigation was conducted in Fall 2008 to update the designation in response to a request from the County. The investigators concluded that there had been erosion, including deflation and recession of the dune and beach, to such an extent that upland properties and development were threatened between R-1 and R-8.5 and R-12 and R-13. The shoreline in the area between R-8.5 and R-12 (the "Gap Segment") standing alone did not meet the requirements for designation as critically eroded. Nonetheless, the Gap Segment was designated as having a critically eroded shoreline for continuity of management of the coastal system and to facilitate management of the adjacent beached in order to maintain the integrity of the Project's design. The same is true of the segment of the Project east of R-13, that is, from R-13 to R-15. ("Continuity of management and maintenance of a project's design integrity" is a basis for designating a shoreline to be critically eroded under the Department's rule.) Were the Gap Segment to be excluded from the Project, fill placed by the restoration effort in the adjacent, restored areas would collapse into it over time. The restored areas would not remain stable and the restoration effort would be defeated, diminished or endangered. That upland areas in the Gap Segment might not be threatened by a 25-year storm does not mean that restoration is not a useful activity for the segment. To the contrary, the upland areas alongside the Gap Segment will benefit from the Project. While the upland areas adjacent to the Gap Segment's shoreline may not be threatened by less damaging higher- frequency storms, they are "definitely threatened by a 50 or 100-year storm event and are in need of the project from that standpoint." OI Tr. 557. Genesis of the County's Efforts Following the designation by the Department of the shoreline subject to the Project as critically eroded, the County began to consider beach restoration in Okaloosa Island. The efforts gained momentum when the County entered an inter- local agreement with the City of Destin in 2006. The agreement provided that the Tourist Development Council (the "TDC") would be the lead agency in all beach restoration issues. The County chose the shoreline now subject to the Project for restoration because of the Department's designation of it as critically eroded. The Project The Project calls for the placement of 940,000 cubic yards of beach quality sand along a 2.8 mile stretch of shoreline. The shoreline is between the Department's reference markers R-1 and R-15 on Santa Rosa Island in an unincorporated area of the County known as Okaloosa Island, Sections 28 through 30, Township 2 South, Range 23 West, in the Gulf of Mexico, Class III Waters. The Project's entire site is situated within the Gulf Islands National Seashore which extends one mile offshore of Santa Rosa Island, the waters of which have been designated by the state as Outstanding Florida Waters ("OFW"). The placement on the beach of the sand (or fill) will create dunes that have the potential to become stable through vegetation, extend the beach seaward roughly two hundred feet, and elevate the beach an average of roughly five and an half feet. The design includes a 40-foot-wide dune crest at an elevation of 14 feet NAVD, a 60-foot wide backberm at 8.5 feet NAVD, and a variable width berm at 5.5 feet NAVD. The dune will transition into the backberm at a 1:4 (vertical:horizontal) slope; the backberm will transition into the berm at a 1:10 slope; and the berm will transition into the existing sea bottom at a 1:10 slope. In areas where the landward edge of the dune crest does not tie into the existing dune, the landward dune face will merge into the existing topography at a 1:4 slope. The fill for the Project will be dredged from an offshore borrow area. The Project includes the removal of sand placed on Okaloosa Island beaches in 2006. Referred to at hearing as "brown sand," see OI tr. 1668, Case No. 10-2468, the sand had been hauled in from an upland source by truck rather than being from an offshore borrow area as contemplated by the Draft JCP. The brown sand is not the same color as the "sugar white" sand on Okaloosa Island's beaches. It is being removed because it is not compatible on the basis of color with the sand on the beach. The ECL Morgan and Eklund, Inc., Professional Survey Consultants (the "ECL Surveyors"), prepared a document dated October 30, 2008, entitled "MEAN HIGH WATER LINE SURVEY AND PROPOSED OKALOOSA ISLAND EROSION CONTROL LINE FOR FDEP RANGE MONUMENTS R-1 TO R-16 OKALOOSA COUNTY, FLORIDA," see WD County Ex. 7. The document was referred to at hearing by Mr. Trudnak as the "Erosion Control Line drawings for the Okaloosa Island Project." WD Tr. 261. (The document, WD County Exhibit 7, will be referred to in this order as the "Proposed ECL Drawings.") The Proposed ECL Drawings show that a survey of the MHWL survey between R-1 and R-16 was conducted on September 16, 2008. As would be expected, the MHWL depicted on the Proposed ECL Drawings is not a straight line. For the most part, it meanders across the drawings with sections where the line comes to "points" that protrude seaward. For example, one prominent point would be at the end of a perpendicular line (that does not appear on the Proposed ECL Drawings) drawn seaward across the dry beach from a point (also not on the Proposed ECL Drawings) on Surf Dweller Condominium Property. See WD County Ex. 7, Case No. 10-2468. The Proposed ECL Drawings depict three other lines, entitled "LANDWARD LIMITS OF CONSTRUCTION," "POST CONSTRUCTION MEAN HIGH WATER LINE," and "SEAWARD LIMITS OF CONSTRUCTION," all of which are predominately straight lines. On April 21, 2010, the Board of Trustees of the Internal Improvement Fund by resolution (the "Resolution") "approved, adopted and certified for the purposes prescribed by Sections 161.141 through 161.211, Florida Statutes," OI Petitioners' Ex. 22, the Okaloosa Island Project ECL "particularly described in Exhibit A." Id. Exhibit A begins with the legal description of the ECL and ends with drawings entitled "OKALOOSA 001-016 EROSION CONTROL LINE OKALOOSA COUNTY, FLORIDA" (the "Approved ECL Drawings"). With a few exceptions (dates and titles) immaterial to this proceeding, the Approved ECL Drawings are identical to the Proposed ECL Drawings. The Seaward Limit of Construction Line is water-ward of the Post Construction MHWL, both of which are well water-ward of the MHWL set in September 2008. Generally, the width from the Seaward Limit of Construction Line to the Landward Limit of Construction Line on the drawings is about 400 feet. The Landward Limit of Construction The Landward Limit of Construction Line in much of the Proposed and Adopted ECL Drawings is over dry beach which, although under the strict control of the County, was declared to be "private" by the County's Protective Covenants and Restrictions. As its name suggests, the Landward Limit of Construction Line was expected by the ECL Surveyors to be the landward edge of the sand fill placed during construction of the Project. As explained by Mr. Trudnak at hearing, the line is "the back of the dune. So, it is the landward most point where sand will be placed." OI Tr. 270. But Mr. Trudnak explained further that the Landward Limit of Construction Line on the Proposed ECL Drawings (and therefore, on the Approved ECL Drawings as well) would not, in fact, be the actual landward- most point of sand placed during the construction phase of the restoration. Rather, the landward-most point where sand would be placed would be significantly waterward of the Landward Limit of Construction Lines on the drawings. Mr. Trudnak offered several reasons for his position. The Landward Limit of Construction Lines on the drawings are straight lines which is not consistent with what will happen when the construction is actually undertaken. Furthermore, a new limit of construction line will be determined when construction plans are submitted prior to the issuance by the Department of a Notice to Proceed, subsequent to the issuance of a JCP. The ECL Surveyors whose Proposed and Approved ECL Drawings contain the straight Landward Limit of Construction Lines that are too landward were not retained to produce drawings for construction plans. The line on the construction plans, when developed, will be much more seaward than the line on the Proposed and Approved ECL Drawings. The County intends, moreover, to construct the Project so that the landward limit of construction falls inside the 150 feet of public beach immediately waterward of the ECL, much further seaward of the Landward Limit of Construction Lines on the Proposed and Approved ECL Drawings. It is reasonable to expect that the County will be able to carry out its intention. See Okaloosa County Exs. 20 and 21, Case No. 10-2468 and Mr. Trudnak's testimony at OI Tr. 181. To the west of a point relatively close to R-12, that is, from R-1 to roughly R-12, the Project can be built on "public" property, that part of the beach declared by the Protective Covenants and Restrictions to be public and controlled by the officials of Okaloosa County or owned by the federal government as part of Eglin Air Force Base. The same is not true of the property to the east of a point just west of R-12. With the exception of the beach adjacent to Newman Brackin Wayside Park (see OI Joint Ex. 2B, sheet 4 of 4 and OI DEP 24), the property east of the federally owned Eglin property is privately owned to the MHWL. If the County does not get authorization from the owners of this private property to conduct restoration activities on the property, the property "would have to be skipped." OI Tr. 188. That would leave two gaps with no restoration landward of the MHWL: the eastern-most end, from roughly R-13.8 to R-15, and a gap from roughly R-11.9 to R-12.9. "Skipping" private properties in the event of a refusal of consent by the owners to use the property during construction would not mean that the Project should be abandoned. The Project could be fully constructed where consents were not required. Where necessary consents were not obtained, the Project could still be constructed below the MHWL. Thus, the project could be constructed over its entire proposed length from R-1 to R-15; east of R-12, however, the Project would not be at its proposed width along the entire length. Some sand from the areas that are restored fully would be transported to the private properties not restored above the MHWL. The Project width in the fully restored segments adjacent to the gaps would be diminished. The beach width in the eastern part of the Project will be narrower than if the private consents had been obtained and the eastern beach fully restored. If the Project's proposed width is narrowed in parts by lack of consents, the Project will not be as effective had the consents been obtained. Nonetheless, the Project will still provide protection over its entire length from surges and damaging wave action produced by tropical storms. Project Construction The Project's Construction is intended to be facilitated by hopper dredge. The dredge excavates at a borrow site. A ship brings the excavated material to the beach fill site where it is discharged by pipe onto the beach. The pipeline runs perpendicular to the shore and extends about a quarter of a mile offshore. The contractor normally fences off a work zone that is about 500 feet wide. The work zone moves along the beach as construction progresses. "[I]n that work zone, there is a lot of heavy equipment that moves the sand around . . . looking at the Project . . . [from] an aerial view, roughly half the sand will be placed seaward and half the sand . . . landward of . . . [the] Mean High Water Line." WD Tr. 139. The Project's construction template or "the shape of the beach when it[']s constructed," id., consists of a dune, a backberm and a wide variable berm. Over the first several months following the Project's construction, a calibration process takes place. About half of the berm erodes and deposits offshore in a near shore sand bar. The near-shore bar acts as a wave break. It dissipates wave energy during storms. A healthy near-shore bar provides significant storm protection. The Project will provide protection from a 50-year storm. Selection of the Sand Source: Borrow Area OK-A The engineers of the Project, ("Taylor Engineering," the "Project's Engineers" or the "Engineers") examined the Gulf's underwater expanse from Santa Rosa County to Walton County seaward to Federal waters. The search for a sand source included a reconnaissance phase and a detail phase investigation of geophysical and geotechnical data. After exhaustive study, two potential borrow areas were identified: a "far-shore" site and a "near-shore" site. The far-shore site is eight miles offshore and about a mile east of East Pass and is designated "OK-B." The near-shore site, three miles west of East Pass and centered about a mile and a quarter from the shores of the Okaloosa Island part of Santa Rosa Island, is designated "OK-A." With its edge within the designated Outstanding Florida Water boundary of the Gulf Islands National Seashore Park, OK-A is within a relic ebb tidal delta in water depths of -36 to -51 feet, NGVD. Approximately 1.7 miles wide from east to west and approximately 0.9 miles wide north to south, it covers approximately 700 acres. At its landward-most side, it will be dredged 10 feet into the existing bottom. Reference in documents of Taylor Engineering and the County to OK-A as the "near-shore site" does not mean it is located in the "nearshore" as that term is used in coastal geology. The coastal geologic term "nearshore" refers to the zone from the shoreline out to just beyond the wave breaking zone. See WD Tr. 513. Borrow Area OK-A is well beyond the nearshore. It is clearly located "offshore," in "the relatively flat zone that is located from the surf breakers seaward out to the outer limits of the continental shelf." OI Tr. 513. It is referred as the near-shore site by Taylor and the County to distinguish it from OK-B which is farther offshore and therefore was referred to as the "farshore site." The two sites, OK-A and OK-B, were selected for comparative review on three bases: sand quality; financial impact; and dredging impacts. Sand quality is "the number one criteri[on]." WD Tr. 143, 10-0515. It involves grain size, soil and shell content, sand color and size of material in the sand, including large shells. See OI Sherry 138. Financial impact is determined mainly by distance; the farther from the construction site, the more expensive to transport the sand. If the borrow area is close enough to shore, a Borrow Area Impact Analysis is conducted. An impact analysis was not conducted for OK-B. The Engineers assumed on the basis of its 8-mile distance from shore that it would not impact the shoreline. The assumption was a reasonable one. Impacts to the shoreline or beach from the dredging of OK-B are unlikely. A Borrow Area Impact Analysis was conducted of OK-A. The quality of the sand in OK-B was similar to that of OK-A but OK-A's "was slightly better." WD Tr. 144. The slight difference was not a significant factor in the determination that OK-A should be selected. The main factor in favor of OK-A was distance. Because it is so much closer to the Project than OK-B, use of OK-A "substantially reduces the cost of construction" id., compared to OK-B. Taylor Engineering (and ultimately the County) selected OK-A as the sand source. The selection process included a sand source investigation by Taylor. Taylor Engineers' final report on sand source was released in October 2009. The report shows that in OK-A, the southeast corner of the area "seemed to contain a lesser quality sand than the borrow area as a whole and in terms of color." WD Tr. 145. Sand from the southeast corner of OK-A, nonetheless, was used in two beach restoration projects, both on Eglin Air Force Base property. Those projects were denominated A-3 and A-13. See further findings, below. The selection of OK-A was supported by Taylor Engineering's OK-A Borrow Area Impact Analysis. Borrow Area Impact Analysis An Okaloosa County Sand Search Borrow Area Impact Analysis was prepared by Taylor Engineering for the Joint Coastal Permit Application and released in July 2008. Aware that dredging the borrow site could affect both wave climate and current (the swift flow of water within a larger body of water), Taylor examined the impact of dredging the OK-A Borrow Area for those effects in the borrow area vicinity. The ultimate purpose of the Borrow Area Impact Analysis, however, was larger. It was to determine the changes to wave and current climate for impact to the beach, such as erosion. An increase in wave height, for example, would increase erosion. Two numerical modeling efforts were conducted. The first, called STWAVE, documents the impacts to wave climate. The second, ADCIRC, analyzes the effects of the dredging on currents. The STWAVE model requires wave characteristics as input. Taylor Engineering used "a 20-year hindcast of wave data from a WIS station located directly offshore in deep water. Under STWAVE modeling, impacts were examined for normal conditions and then 'under a 100-year storm condition.'" WD Tr. 149. The basis was the 100-year storm data from Hurricane Opal. The impacts of bottom friction were ignored, a common practice in applications like the County's JCP application that involves work on the open coast with a uniform sandy bottom. As Mr. Trudnak put it: When you use . . . wave monitoring devices, you're trying to calibrate a model for the effects of bottom friction. And when the borrow area is this close to shore [as in the case of OK-A], . . . the propagation of distance of the waves is relatively short. And when you have a uniform sandy bottom you don't expect the impacts of bottom friction to be significant. So . . . in applications like [Okaloosa County's for the Western Destin Project], you ignore the effects of bottom friction. WD Tr. 150. The analysis assumed that all of the sand in the borrow area would be removed when, in contrast, "the borrow site usually contains 50 percent more sand than what the Project requires on the beach." WD Tr. 152. Borrow Area OK-A is intended to serve five beach restoration projects in all. Three are completed: the two projects on Eglin Air Force Base and the Emergency Holiday Isle Project. The remaining two are the Western Destin Project and the Okaloosa Island Project. These five projects require 4.7 million cubic yards of sand of the nearly 7 million cubic yards of sand available in OK-A. The impact analysis, therefore, was conservative in that it predicted more impact than would actually occur because significantly less sand would be removed from the site than was factored into the STWAVE modeling. With regard to normal conditions, the STWAVE modeling led to the conclusion that impacts from the permitted activities associated with the borrow area would be negligible. Under storm wave conditions, the STWAVE modeling showed "a certain wave angle or direction that increased the wave height." WD Tr. 151. The increase in wave height, however, was far enough offshore so as to never affect the "actual breaking wave height on the beach." Id. The modeling results enabled Taylor Engineering to conclude "that the borrow area did not have a potential to cause any impacts whatsoever." WD Tr. 152. (emphasis added). ADCIRC is a state-of-the art hydrodynamic model that simulates tidal currents. Taylor Engineering conducted the ADCIRC modeling to analyze effects on the tidal currents and circulation in and around East Pass that would be caused by dredging the borrow area. Just as in the case of STWAVE, ADCIRC modeling showed that the impact of dredging the borrow area would be negligible whether in normal or "storm" conditions. Upland Private Property Of the properties along the 2.8 miles of shoreline to be restored, six are deeded to the MHWL. The six are the properties of Eglin Air Force Base, the Sheraton Hotel, the Gulfarium, the Ramada Hotel, Destin West Beach and Bay Resort Condominium, and Seaspray Condominium. These properties are all located in the eastern part of the Project, from R-11.3 to Beasley Park at the east terminus of the Project. Intervenor Wallace and his wife Sondra S. Wallace were deeded Condominium Unit 502 in the Destin West Beach and Bay Resort-Gulfside by a Special Warranty Deed executed by Tolbert Gulfside Development Company on March 7, 2003. See OI Petitioners' 112. The Condominium Property associated with Destin West Beach and Bay Condominium extends to the MHWL of the Gulf of Mexico. The Parcel ID Number on the Special Warranty Deed is 00-2S-24-2185-0015-0030 (Parent Parcel). Id. A quitclaim deed admitted into evidence as OI County Exhibit 22 bears the same Parcel ID Number but without reference to "(Parent Parcel)." The grantor of the quitclaim deed is Okaloosa County and the grantee is Tolbert Enterprises, Inc. The deed contains the following language: IT IS THE EXPRESS intent of the Grantor that its reversionary estate in that portion of the original leasehold estate from the Okaloosa County and/or Okaloosa Island Authority which the Grantee now owns in the subject premises shall be merged with such present leasehold interest now owned by the Grantee, subject, however to such terms and conditions contained in the 1963 quitclaim deed of record from the United States of America to the Grantor and all Protective Covenants previously imposed of record on the above land by Okaloosa County or its agent, Okaloosa Island Authority, and by acceptance of this deed, Grantor acknowledges the validity of such Protective Covenants and Restrictions (with the term "owner" being substituted for "leaseholder" or "lessee" therein where appropriate), which are hereby reimposed. OI County Ex. 22 (emphasis in original). Whether the Protective Covenants and Restrictions apply to all of the six properties so that the first 150 feet landward of the MHWL is "public beach" under the "strict control of the County" is a question that cannot be decided on the state of this record. But it appears from the quitclaim deed that constitutes OI County Exhibit 22 that the County took pains when it conveyed the Okaloosa Island property subject to the deed to make sure that the grantees under the conveyances were aware of the Protective Covenants and Restrictions and that the County's intention in the conveyances was for the Protective Covenants and Restrictions to survive. For the properties in the Project that are not deeded to the MHWL, the County has control of the beaches through the Protective Covenants and Restrictions. In addition to the documents of record, the County's control is evidenced by seven main public access-ways to the beach along Okaloosa Island, additional smaller access-ways, public use of the access-ways, public parking serving access of the public to the beaches of Okaloosa Island and public use of the dry, sandy portion of the beach in Okaloosa Island. The Application An Application for a Coastal Construction Permit The Application was processed as a joint coastal permit (a "coastal construction" permit under section 161.041). It was not processed as an application for a coastal construction control line ("CCCL") permit. Section 161.041 (the "Shore Protection Statute") and chapter 62B-41 apply to JCPs. Section 161.053 (the "CCCL Statute") and chapter 62B-33 govern CCCL permits. The Department treats its JCP and CCCL permitting programs as independent from each other and as mutually exclusive permitting programs. A project that involves "beaches and shores" construction is permitted under one permitting program or the other but not under both permitting programs. See WD Tr. 424-5. Indeed, when it comes to beach restoration projects (or "shore protection" projects) such as the Western Destin Project, section 161.053(9) of the CCCL Statute provides as follows: "The provisions of this section do not apply to structures intended for shore protection purposes which are regulated by s. 161.041 [the Shore Protection Statute] " The Department interprets section 161.053(9) to exempt the Project from CCCL statutory requirements and the rules that implement the CCCL Statutes so that the only permit the Project requires, in the Department's view, is a JCP. Application Signatures Item 18 of the Application provides a signature line for the County and "the title of the person signing on its behalf." OI Joint Ex. 1, DEP From 73-500 (05/17/07), p. 4 of 9. The Item opens with: "A. By signing this application form, I am applying . . . for the permit and any proprietary authorizations identified above [see findings below related to "written authorizations"], . . . ." Id., (emphasis added). Item 18 also provides "signature lines" for an agent in Section B if the County designates an agent for the processing of the application. Section 18 C of the Application provides a signature line under the following heading: "PERSON AUTHORIZING ACCESS TO THE PROPERTY MUST COMPLETE THE FOLLOWING." There was no signature provided at any point in the application process by any person authorizing access to the property as called for by Item 18C. Joint Ex. 11, Page 4 of 27. The "Written Authorization" Provision Chapter 62B-14 is entitled "Rules and Procedures for Applications for Coastal Construction Permits." The Shore Protection Statutes serves as rule-making authority for every rule in chapter 62B-41. Every rule in the chapter, moreover, implements, among other provisions, one provision or another of the Shore Protection Statute. Rule 62B-41.008 derives its rule-making authority from the Shore Protection Statute and section 161.055(1) and (2). Among the statutory provisions it implements are four subsections of the statute: (1), (2), (3) and (4). Section (1) of rule 62B-41.008 provides, in pertinent part, as follows: A Joint Coastal Permit is required in order to conduct any coastal construction activities in Florida. A person required to obtain a joint coastal permit shall submit an application to the Department . . . The permit application form, entitled "Joint Application for Joint Coastal Permit, Authorization to Use Sovereign Submerged Lands, Federal Dredge and Fill Permit" . . . is hereby incorporated by reference . . . . The application shall contain the following specific information: * * * (c) Written evidence of ownership of any property which will be used in carrying out the project, or authorization for such use from the property owner which is upland of mean high-water, or below mean high water but not sovereign land of the State of Florida. * * * (n) Written authorization for any duly- authorized member of the Department staff to enter upon any property to be used in carrying out the project, for the purpose of evaluating site conditions prior to final processing of the permit application. (emphasis added). Rule 62B-41.008(2) (the "Waiver Provision") lists requirements of rule 62B-41.008(1) which are to be waived by the Department under circumstances described in the Waiver Provision: "Any of the requirements contained in paragraph 62B- 41.008(1)(f), (h), (i), (j), (k), (l), or (m), F.A.C., will be waived if the Department determined that the information is unnecessary for a proper evaluation of the proposed work." In its list of requirements that will be waived under certain circumstance, the Waiver Provision does not include paragraphs (c) or (n). The Application did not contain the "specific information" detailed in paragraphs (c) and (n) of rule 62B- 41.008(1). As of the dates of final hearing, the County had not provided the Department with any written authorizations from the owners of the privately-owned properties within the Project area, including Intervenors. Demonstration of Property Ownership The Application demonstrated that the County owned much of the property subject to the Project. At the time of final hearing, it had permission, of course, to use that property. The County has also obtained the permission of the federal government to use Eglin Air Force Base property that is within the Project area. As for the other property, all privately owned, no written authorizations as of the final hearing had been obtained from the owners despite discussions between them and the County. Despite the clear requirement in rule 62B- 41.008(1)(c), the Department does not usually require that an applicant provide in the application written authorization from owners of upland property to be used in coastal construction projects. The Department might require written authorization in an application for certain coastal construction projects like a groin construction project, see OI tr. 476, or a similar project that involved one or two upland property owners. The typical beach restoration project, however, involves the use of many different upland properties, too many, in the Department's view to require the application to contain the written authorizations of all the owners. The Department justifies departure from enforcing the requirement of rule 62B-41.008(1)(c) in applications for beach restoration for a number of reasons. First, compliance is impractical. Aside from the significant number of signatures that must be obtained, the moment the application is submitted is too early in the process to require written authorization. In beach towns, where most restorations take place, many of the owners are absent and difficult to contact. By the time the restoration begins, the property may have changed hands. Second, the Department's practice is to require the authorizations as a permit condition and for written authorization to be submitted prior to construction, that is, sometime between when the JCP is obtained and the Notice to Proceed with construction is issued. An applicant in possession of a JCP for beach restoration cannot begin construction activities until a Notice to Proceed is issued. The aim of the rule is achieved in a timely manner whether all consents are submitted with an application or not. Aside from practical considerations and safeguards to ensure consent from upland property owners prior to the commencement of construction activities, written authorization in the application is not relevant in the Department's view in a permitting proceeding. Permitting proceedings are not designed to prevent trespass by an applicant. They are designed to consider environmental impacts. With regard to trespass considerations, there are other safeguards. These include the warning to the applicant in General Condition Six of the Draft JCP: 6. This permit does not convey to the Permittee or create in the Permittee any property right, or any interest in real property, nor does it authorize any entrance upon or activities on property which is not owned or controlled by the Permittee. The issuance of this permit does not convey any vested rights or any exclusive privileges. The Draft JCP also contains General Condition Eight: 8. The Permittee, by accepting this permit, specifically agrees to allow authorized Department personnel with proper identification and at reasonable times, access to the premises where the permitted activity is located or conducted for the purpose of ascertaining compliance with the terms of the permit and with the rules of the Department and to have access to . . . copy any records that must be kept under conditions of the permit; to inspect the facility, equipment, practices, or operations regulated or required under this permit; and to sample or monitor any substances or parameters at any location reasonably necessary to assure compliance with this permit or Department rules. Reasonable time may depend on the nature of the concern being investigated. If the applicant conducted construction using upland property without written authorizations from the upland owner, the Department would view the construction to be in violation of the JCP and would bring an enforcement action to halt the construction until written authorization was obtained. There are many opportunities, therefore, to achieve the aim of the rule subsequent to the filing of an application. Lapse in the Application Chapter 62B-49 is entitled, "Joint Coastal Permits and Concurrent Processing of Proprietary Authorizations." Rule 62B-49.005 is entitled, "Application Requirements and Processing Procedures." The following appears in the rule: An application shall be denied if the applicant fails to provide additional information to the Department within six (6) months [the "Six Month Period"] after a written request for such information has been sent to the applicant. However, if the applicant can demonstrate that he or she has been actively working on collecting or developing the requested information, and that additional time will be required to complete their response to the "RAI," the applicant may request up to six (6) additional months to submit their response. Fla. Admin. Code R. 62B-49.005(4). On November 25, 2008, the Department sent its third Request for Information (the "Third RAI") to the County. The Third RAI asked for more information regarding a risk assessment, the permit fee, a biological opinion (the "Biological Opinion") from "Fish and Wildlife," OI tr. 91, and had a question regarding a lighting ordinance. The County did not respond to the Third RAI within six months which expired on May 25, 2009. Nor did it request an extension within the Six Month Period. Mr. Trefilio and others on behalf of the County were in touch with DEP throughout the Six Month Period about various issues concerning the JCP. See OI tr. 90. Mr. Trudnak, for example, in early May, prior to the expiration of the Six Month Period sent an e-mail to DEP personnel to inquire about the permit fee DEP had required because Taylor Engineering believed it was incorrect. The Department did not respond until early June. Taylor Engineering had been "continuously working on the . . . Economic Analysis that addressed the questions that DEP had about the Risk Assessment [and] . . . had been talking to DEP about that." OI Tr. 169-70. Mr. Trudnak corresponded with the Army Corp of Engineers about the Biological Opinion. His hope was that a draft could be timely submitted with the other responses to the RAI. He contacted Ralph Clark and spoke with Jamie Christoff, a Department employee, about its status. But, the County and its agents "were not able to get that done within the six month time frame." OI Tr. 170. On June 3, 2009, Mrs. Sherry wrote an e-mail to Michael Barnett. She asserted that the Application was dormant and had lapsed. She requested that it be denied on the basis of the rule. The next day, an e-mail from Mr. Barnett, Chief of DEP's Bureau of Beaches and Coastal Systems, posed the question to Department personnel, ". . . has there been any verbal or written communication from either the Applicant or their Agent as to when the Department might anticipate a response to RAI #3?" OI Petitioners' Ex. 65, Page 2 of 4. E-mail messages in the file and a conversation with her subordinate, Jamie Christoff, led Dr. Edwards, who was in charge of the processing of the Application, to conclude that the County and its agents had been working on the application during the Six Month Period. After the message from Mrs. Sherry to the Department (and after the expiration of the Six Month Period), Mr. Trudnak requested an extension of time under the rule. The extension was not granted in writing. Dr. Edwards concluded "because there was that active back and forth between the Department and the applicant [during the Six Month Period], there was no need for additional time being granted . . . ." OI Tr. 440. Application Deemed Complete Chapter 62B-49 establishes the joint coastal permit program "by combining the regulatory requirements of the coastal construction program (Section 161.041, F.S.) with the environmental resource (or wetland resource) permit program (Part IV of Chapter 373, F.S.) . . . ." Fla. Admin. Code R. 62B-49.001. The chapter also "provides concurrent review of any activity requiring a joint coastal permit that also requires a proprietary authorization for use of sovereign submerged lands owned by the Board of trustees of the Internal Improvement Trust Fund." Id. Rule 62B-49.003 is entitled "Policy." It provides as follows in pertinent part: Any application submitted pursuant to this chapter shall not be deemed complete . . . until the Department has received all information required for: a coastal construction permit under . . . Chapter 62B- 41, F.A.C.; . . . and Chapters 18-18, 18-20 and 18-21. Fla. Admin. Code R. 62B-49.003(3). Despite the absence in the Application of written authorizations required by rule 62B-41, the clear directive of rule 62B-49.003(3), and the failure of the County to respond in a timely manner to RAI #3 or obtain in writing an extension of the time to respond, the Department deemed the Application complete on December 30, 2009. If Written Authorizations are not Obtained If written authorizations are not obtained from the owners of the six private properties between R-11.3 and the eastern terminus of the Project, the County would have to decide whether and/or how to proceed. If the eastern-most 600 feet of the Project were deleted, for example, the Project could be modified to mitigate the effects of the deletion without much effect on the remainder of the Project. If more of the Project were deleted, it would present more of a challenge to the effectiveness of the Project. In any event, the Project can be completed along its entire length up to the MHWL. The Project may not be at full width where consents are not obtained but it will still provide some storm protection where narrowed. It would also still provide significant protection westward of R- 11.3 all the way to R-1 albeit the closer to R-11.3 the more diminished would be the effectiveness of the Project if the Project is not at full width east of R-11.3. Legislative Declaration of Public Interest Section 161.088, Florida Statutes, bears the catchline, "Declaration of public policy respecting beach erosion control and beach restoration and nourishment projects." It states: Because beach erosion is a serious menace to the economy and general welfare of the people of this state and has advanced to emergency proportions, it is hereby declared to be a necessary governmental responsibility to properly manage and protect Florida beaches fronting on the . . . Gulf of Mexico . . . from erosion and that the Legislature makes provision for beach restoration and nourishment projects . . . . The Legislature declares that such beach restoration . . . projects, as approved pursuant to s. 161.161, are in the public interest; must be in an area designated as critically eroded shoreline, or benefit an adjacent critically eroded shoreline; . . . (emphasis added). Proprietary Public Interest Test Chapter 18-21 governs Sovereignty Submerged Lands Management. Rule 18-21.004 sets out management policies, standards and criteria. It opens as follows: The following management policies, standards, and criteria shall be used in determining whether to approve, approve with conditions or modifications, or deny all requests for activities on sovereignty submerged lands . . . . General Proprietary. (a) For approval, all activities on sovereignty lands must be not contrary to the public interest . . . "Public interest" is defined as: Demonstrable environmental, social, and economic benefits which would accrue to the public at large as a result of a proposed action, and which would clearly exceed all demonstrable environmental, social, and economic costs of the proposed action . . . Fla. Admin. Code R. 18-21.003(51) (the "Proprietary Public Interest Test"). The rule also states that "[i]n determining the public interest in a request for use . . . [of] sovereignty lands . . . , the board shall consider the ultimate project and purpose to be served by said use " Dr. Fishkind, an economist, conducted an economic cost/benefit analysis of the Project and concluded that the economic benefit is between $5.77 and $12.09 million while the cost of the Project is between $16.30 and $21.58 million. The Department did not present an economist to rebut Dr. Fishkind's analysis. The Department takes the position that the Project is in the public interest and meets the Proprietary Public Interest Test because of the declaration by the Legislature in section 161.088. The Department interprets the Legislature's declaration in section 161.088 that beach restoration projects are in the public interest to relieve the County from having to provide evidence that the Project meets the Proprietary Public Interest Test and to relieve the County and the Department from a need to rebut the evidence provided by Petitioners' economist. The Department draws support for its interpretation from language in section 161.091(3). The language makes reference to the declaration in section 161.088 that beach restoration projects are in the public interest. It finds further "that erosion of the beaches of this state is detrimental to tourism, the state's major industry, further exposes the state's highly developed coastline to severe storm damage, and threatens beach-related jobs, which, if not stopped, may significantly reduce state sales tax revenues " § 161.091(3), Fla. Stat. Impacts The depth of OK-A should not exceed -49.4 feet, NGVD, in an area where the depth of the ocean bottom is roughly -40 feet, NGVD. OK-A is relatively wide, at least as compared to an existing borrow area not far away, the borrow area used for beach restoration in western Walton County and eastern Okaloosa County east of the City of Destin (the "Walton Borrow Area"). It is also a shallow borrow area when its depth is measured from the Gulf floor. It is in deeper water than the Walton Borrow Area. These factors make it less likely to cause impacts to the beach than the Walton Borrow Area. Despite the width of OK-A, its relative shallowness measured from the Gulf floor, and its water depth, Dr. Dally, on behalf of the Petitioners, challenged the Taylor Engineering conclusion that there would be no impacts to the beach from the dredging of Borrow Area OK-A. The challenge from Dr. Dally, however, did not detail what the impacts would be or how serious they would be. Instead, Dr. Dally concluded that "not nearly enough study has been conducted of the proposed borrow area to ascertain that there will be no adverse impacts." WD Tr. 633. Dr. Dally's challenge to the conclusion by Taylor Engineering of no impacts to the beach from an excavated OK-A begins with an explanation in general of wave dynamics, sediment transport, and borrow site impacts. Wave Dynamics, Littoral Sediment Transport, and Borrow Site Impacts, Generally General Wave Dynamics "[W]aves in very deep water will start to turn and become more shore parallel in the case of Okaloosa County." WD Tr. 636. As they approach shore, a dynamic process of shoaling and refraction occurs. The waves may also begin to diffract. Shoaling is a growth in height from interaction with the shallow bottom or a shoal. Refraction is a process of alignment of waves with bottom contours. Diffraction is a spreading of waves or the bending of waves or change in wave direction after interaction with emergent structures or submerged features. As the process of shoaling, refraction and diffraction takes place, waves may be affected by bottom friction, depending on ocean bottom conditions. Dr. Dally offered the following description of wave changes as they close in on the face of the beach and interact with the shoreline. The description includes potential impacts of an excavated OK-A on the beaches and shores adjacent to the Surf Dweller and El Matador condominium property: As they pass into the very nearshore . . . they, of course, grow in height. They then break . . . [or] [s]ometimes, as they pass over a [sand]bar, they'll stop breaking. And then begin breaking again when they get right up onto the beach face. Any time you put a bathymetric feature [such as a borrow area] into that otherwise natural system, you affect the wave transformation due to processes dependent upon the character of the perturbation . . . * * * Wave reflection from abrupt bathymetric changes. . . in this case, the landward most . . . notch of the borrow area would be a reflective surface . . . when something has perturbed the wave field like that, defraction [sic] becomes an important process. So, as the waves pass over this proposed borrow area and, especially, over the 10-foot or greater vertical face, they will reflect and begin defraction [sic] so that it becomes a . . . complicated wave field . . . . WD Tr. 636-7. In addition to the perturbation caused by the borrow area there is another factor at work that has the potential to affect the beach along the condominium properties owned by the Sherry Petitioners: sediment transport. Sediment Transport "Sand can move along or away from the beach in two ways." WD Tr. 1141. It can move along the shoreline or it can move offshore. Littoral transport of sediment, a factor important to erosion and accretion, is the movement of sediment, mostly sand, along or parallel to shore. It is caused by the intersection of waves that come ashore at an angle to the shoreline, rather than those that break straight onto the beach. The average net long-term littoral transport in the area of the Project and Okaloosa Island is east to west. The Sherrys and Mr. Donovan own property down-drift from the OK-A site, or to the west. Dr. Young described the beaches down-drift of OK-A at hearing: "Those beaches have, over the . . . last decade or so, been generally stable to accreting. There's a pretty nice beach out there right now." WD Tr. 1143. This area of the Okaloosa County's beaches and shores is the area most likely to be affected by an excavated OK-A if there are, in fact, any impacts to beaches and shores caused by the dredging of the borrow site. Borrow Site Impacts Two processes affecting waves in the Gulf would occur above an excavated OK-A Borrow Area. The first wave process would be "that part of the wave energy will actually reflect and go back out to sea," WD tr. 640, in essence, a scattering effect of the energy. Diffraction at the same time would cause the waves to radiate outwards from the borrow area rather than the waves going straight back out to sea. The second wave process creates the potential for the waves to become "very, very, complicated." WD Tr. 640. They could "trip," that is, the notch in the borrow area could break the waves. "[B]rag scattering" (WD tr. 641) could make the waves deteriorate into shorter period waves. If there are changes in waves, tide level or current, changes will be caused to the beach. As Dr. Dally succinctly put it at hearing, "[the beach] might erode, it might accrete, it might do both," WD tr. 641, by virtue of the presence of an excavated OK-A Borrow Area. If the impact of the excavation of the borrow area were to create shorter period waves, the result generally would be erosion. If the impact created longer period waves which generate water movement deep into the water column the result generally would be accretion. The borrow area has the potential in Dr. Dally's opinion to create both longer and shorter period waves. Wave angle of the waves breaking on the beach also is a factor in beach impacts. But Dr. Dally was unable to predict the impacts of the excavation of OK-A to Okaloosa Island beaches and shores without more study, data and analysis as to what effects a dredged OK-A would have on wave period and wave angle and the concomitant sediment transport. Like Mr. Trudnak, Mr. Clark concluded that OK-A is too far offshore to cause adverse impacts to the beach. If, however, the Project were to utilize a borrow area along the same stretch of the beach but much closer to shore as in the case of the Anna Maria Island Project in which the borrow area was only 1000 feet from the shoreline, erosion impacts could occur on part of the beach. Beneficial impacts in such a case would occur to the beach downdrift of the borrow area. In the Anna Maria Island Project, beaches far enough to the south which were downdrift of the borrow area accreted. The impact to the Sherry and Donovan Properties, both being downdrift of a borrow area located along the same stretch of beach but within 1000 feet of shore and closer in than OK-A, would likely be beneficial. The area of shoreline that would be affected by wave impacts from an excavated OK-A is larger than the area in the immediate shadow zone of the borrow site, that is, a shadow zone perpendicular from the borrow site to the shore. The area affected by wave impacts depends on the angle of the waves. In the Destin area and along Okaloosa Island where the Sherry Petitioners reside, the waves come ashore predominately out of the east. If the waves come ashore along Okaloosa Island at a strongly oblique angle (more directly from the east), "the shadow zone now stretches further to the west and the diffraction pattern . . . increases the size of the shadow zone," WD tr. 680, to a size much larger "than the actual shadow zone of the . . . borrow area." Id. Along these same lines, if there are impacts to the beach caused by a dredged OK-A, the impacts should be greater the closer the beach is to the footprint of a dredged OK-A. Given the predominate tendency of the waves to come from the east along Okaloosa Island, if the beaches alongside both the Surf Dweller Property and the El Matador Property are affected, the beach alongside the Surf Dweller Property will incur the greater impact. Likewise, if beach impacts are incurred by beach alongside only one property or the other, it is much more likely that the beach alongside the Surf Dweller Property will be affected than the beach alongside the El Matador Property. The distance of an offshore borrow area from the shore is critical to the effect of the borrow area on diffraction and wave dynamics. If the borrow area is far off shore, as in the case of the alternative, potential borrow site identified by Taylor Engineering, OK-B, then, as explained by Dr. Dally, diffraction "has a lot of time and a lot of opportunity to smooth the waves out once again and things become uniform when they hit the beach." WD Tr. 645. A borrow area that is closer to the beach has higher potential for creating impacts. Dr. Dally again: "[I]f you move the borrow area closer to the beach, you have this scattering pattern induced by the reflection and the diffraction and refraction that doesn't have time to smooth itself out. And that's when you can really cause impacts to the beach, both accretive and erosive impacts." Id. (emphasis added). The underscored sentence from Dr. Dally's testimony quoted in the previous paragraph was directly addressed in the County's case through Mr. Trudnak's determination that OK-A, although not as far away as OK-B, is far enough away from the beach that it will not cause adverse impacts to the beach. Again, Dr. Dally's testimony, despite the underscored testimony in the previous paragraph, is not that OK-A will, in fact, cause impacts to the beach. His testimony, rather, is the equivalent of a statement that the closer a borrow area is to the beach the more likely that it will have impacts to the beach and that at some point, a borrow area, will be so close to the beach, that adverse impacts will occur. The fact that OK-A is much closer to the beach than OK-B does not mean that an excavated OK-A will cause impacts to the beach. Impacts of an excavated OK-A depend upon OK-A's actual distance from the beach rather than OK-A's distance relative to OK-B's distance. Thus, while it may be determined that the likelihood of impacts to the beach is greater in the case of OK-A than in the case of OK-B, actual impacts from OK-A to the beach (as far as the effect of distance) is a function of OK-A's actual distance from the beach without regard to OK-B's distance from the beach. In addition to Dr. Dally's certitude that there will be impacts to the beach by virtue of the presence of a dredged OK-A, Dr. Dally also took issue with the method by which Taylor Engineering reached the conclusion of no impacts in the OK-A Borrow Area Impact Analysis Report. The OK-A Borrow Area Impact Analysis Generally Mr. Trudnak was part of the Taylor Engineering team that prepared the Borrow Area Impact Analysis Report. Mr. Trudnak was not the only expert to defend the report's conclusion of no impact to the beach. The report was reviewed by Mr. Clark, the Department's expert, who also opined that there would be no impacts. Mr. Clark relied on more than the report for his opinion. He also relied on his extensive experience with beach restoration projects and monitoring data for those projects and visual observation of those projects post-construction. The only numerical data analysis specific to the excavation of the OK-A Borrow Area, however, that the Department used in determining that excavation of OK-A would not have any adverse impacts to the shoreline and coastal systems of Okaloosa Island was the Taylor Engineering OK-A Borrow Area Impact Analysis Report. The Report described its evaluative efforts: [T]his report evaluates two potential dredging templates in terms of their impacts on wave and tidal current patterns during normal and extreme conditions. The evaluation requires analysis of the wave climate and tidal currents before and after the borrow area dredging. The analysis required a balance between minimizing impacts to wave climate and current patterns, and providing acceptable nourishment volumes. STWAVE (Steady-State Spectral Wave Model) simulated normal (average) and extreme (100-year (yr) storm) waves propagating over the baseline and post-dredging bathymetries. ADCIRC hydrodynamic modeling simulated tidal flow over the baseline and post-dredging bathymetries for normal (spring) and extreme (100-yr storm) tide conditions. A comparison of the baseline and post dredging model results established the effects of borrow area dredging on the neighboring shorelines (Destin and Eglin AFB) and the inlet. WD County Ex. 1, Okaloosa County Sand Search Borrow Area Impact Analysis, at 6. Thus, the STWAVE modeling conducted by Taylor as part of the analysis attempted to simulate normal (average) and extreme (100-year storm) waves propagating over the baseline and post-dredging bathymetrics. Taylor Engineering relied on WIS (Wave Information Study) results in performing its STWAVE modeling. WIS data are not measured wave data. Instead, they consist of numerical information generated by specific stations in wind fields in various locations around the Gulf of Mexico. The data are then placed in a model coded to represent the entire Gulf. The WIS station from which data were collected by Taylor Engineering is located approximately 10 miles offshore where the depth is approximately 85 feet. It would have been preferable to have used comprehensive field measurements, that is, data obtained from wave gauges on both sides of the borrow area over enough time to support use of the data, rather than WIS data. Comprehensive field measurements would have produced much more information from which to predict impacts to the beach. As Dr. Dally explained, however, If you don't have [field measurement data], then . . . especially over the long-term . . . a year or more [or] if you're analyzing your beach profile data over a 10 year period, you would like to have . . . wave data to accompany that 10 year period. Generally we don’t and that's when we start relying on models to fill in this missing information. WD Tr. 645-6 (emphasis added). This testimony was consistent with Mr. Trudnak's testimony: the problem with field measurement is that "the useful data that you [get] from [field measurement] gauges is . . . limited to [the] deployment period." WD Tr. 1234. It is not practical to take 10 years' worth of field measurements. As Mr. Trudnak explained: Typically, you would install those gauges for . . . a month or a couple of months . . . you want to use representative conditions . . . you try to pick a winter month and a summer month so you can try to capture those extremes and wave conditions. * * * [W]hen you . . . install those gauges in the field, you have no idea what those conditions are going to be during your deployment period. You can install your wave gauge for a month in the winter but that can be an unusually calm month, it could be an unusually severe month. So, it's really hit or miss, whether you . . . capture representative conditions. Id. (emphasis added). The WIS information utilized is hind-casted. Hind- casting is a method for developing deepwater WIS data using historic weather information to drive numerical models. The result is a simulated wave record. The WIS information utilized includes 20 years of hind-cast information. The purpose of using such a lengthy period of information is that it ensures that representative conditions are captured in the data for purpose of the analysis. Such "lengthy period" information overcomes the concern that there is not enough data to capture representative conditions as in the case of typical field measurement data. For its extreme STWAVE modeling, Taylor relied on WIS information generated during Hurricane Opal in 1995. Analysis of the model results showed negligible impacts on wave height under normal conditions and increased wave height during extreme conditions. Increased wave height during extreme conditions, however, was no closer than 300 feet from the shoreline. The increased wave height and wave angle in storm conditions were far enough offshore that they "never impacted the actual breaking wave height on the beach." WD Tr. 151. The model's prediction of no impacts in wave height on the shoreline due to a dredged OK-A and no change in sediment transport rate by virtue of the presence of a dredged OK-A led Taylor Engineering to conclude that whether in normal or extreme conditions, a dredged OK-A Borrow Area would not cause impacts to the beaches and shores of Okaloosa County. Criticisms of Taylor's STWAVE Modeling Dr. Dally offered four basic criticisms of Taylor Engineering's STWAVE Modeling: a) the model did not account for wave transformation processes caused by bottom friction between the WIS Station (10 miles out in the Gulf) and the OK-A site; b) the model was not calibrated or verified; c) the model did not sufficiently account for wave transformation impacts from the dredging of Site OK-A; and d) Taylor did not plot wave direction results from its STWAVE models or conduct any sediment transport analysis. Mr. Trudnak offered refutations of the criticisms. For example, taking the first of them, wave transformation processes caused by bottom friction between the WIS Station and the OK-A site were not accounted for by Taylor Engineering in its analysis because "most of that distance [between the WIS Station and the OK-A site] is deep water, meaning the waves aren't . . . feeling the bottom so they're not being affected by the bottom friction." WD Tr. 1236. The refutations were not entirely successful. The second of Petitioners' experts, Dr. Young cast doubt on the validity of all modeling no matter how well any particular modeling activity might meet the criticisms leveled by Dr. Dally against Taylor Engineering's effort. Dr. Young accepted Dr. Dally's testimony about why Taylor Engineering's modeling was not sufficient to support an opinion of "no impacts," but he differed with Dr. Dally as to whether coastal engineering models should be utilized to predict impacts to beaches. See WD Tr. 1157. Dr. Dally believes in the benefits of modeling as long as the modeling is conducted properly. Dr. Young does not. It is his opinion that no model produces a projection that is precisely accurate but the essence of his criticism is that "we don't know how wrong the models are." WD Tr. 1159. Models are "incapable of quantifying the uncertainty or how right or wrong that they might be." Id. With regard to the modeling used in Taylor's Borrow Area Impact Analysis, Dr. Young summed up: [W]hen we do this model run, especially with a model that isn't calibrated or verified, we get an answer . . . it's not precisely the right answer, but . . . nobody knows how wrong the answer is. I don't know it, Mr. Trudnak doesn't know and Mr. Clark doesn't know. And that's why being prudent is important and why relying on the monitoring data is critical because the monitoring data is real data. WD Tr. 1160. In contrast to Dr. Young, Dr. Dally, consistent with his faith in models appropriate for the investigation and conducted properly, took another tack in attacking the modeling used by Taylor Engineering. He criticized Taylor Engineering's failure to use a more comprehensive wave transformation model: the Boussinesq Model. Dr. Dally opined that the Boussinesq Model was superior to STWAVE principally because it takes diffraction into account. But Petitioners did not produce any off-shore borrow area impacts analyses which used the Boussinesq Model, and Mr. Trudnak testified that he was unaware of any. See tr. 1233 and 1234. The Boussinesq Model is typically used where diffraction plays the dominant role, that is, within areas like inlets or ports which have structures that will cause wave perturbation. The open coast is not such an area. If not more appropriate than the Boussinesq Model, STWAVE is an acceptable model under the Project's circumstances. When asked about the Boussinesq modeling's application in the context of his testimony that he could not say what would be the impacts of the dredging of the OK-A Borrow Area, their extent or whether they would be adverse, Dr. Dally testified that based on his experience, he was "almost certain," WD tr. 691, that Boussinesq modeling would show impacts to the beach adjacent to the Surf Dweller and El Matador Properties that could be a "type of accretion . . . [that is] momentary . . . due to the propagation of these features as they go up and down the beach." Id. This statement is consistent with Mr. Clark's opinion that if the Project's borrow area were within 1000 feet of shore, the impact of dredging OK-A to the Sherry and Donovan Properties would be beneficial. When asked if the beaches would develop scalloping (sand erosion in some areas and accretion in others), Dr. Dally said, "Right. This [wave transformation process caused by an excavated OK-A borrow area] makes a scalloping." WD Tr. 692. Perhaps the dredging of Borrow Area OK-A would aggravate scalloping along the shores of Okaloosa County but they would not create scalloping of an "un-scalloped" coastal system. Scalloping features in the Okaloosa Island portion of Santa Rosa Island existed at the time of final hearing. In short, Dr. Dally criticized Taylor Engineering's STWAVE modeling. As to the impacts he was sure would occur, he was unable to state whether they would be adverse, beneficial or both. Most importantly to the weight to be assigned his testimony, he was unable to testify as to how significant the impacts would be; one cannot determine from his testimony whether the impacts will be entirely de minimus, see rule 62B- 41.002(19)(c) or whether some could be significant, see rule 62B-41.002(19)(a). Dr. Dally's testimony with regard to the creation by the Project of scalloping did not indicate the significance of that scalloping to the coastal system of Okaloosa County, a system whose ocean bottom, beaches and shores already contain scalloped features. Suppositive impacts that would be caused by the Project to the beaches of Okaloosa County were not the only attack by Petitioners. They also challenged the impact analysis on the basis of the opinion that adverse impacts had been caused to beaches by another beach restoration project and its borrow area not far away: the Walton Project. The Walton Project and Its Borrow Area Completed in the late spring of 2007, the Walton Project placed sand dredged from the Walton Borrow Area on approximately 7 miles of beach in eastern Okaloosa County (East Destin) and western Walton County. Just as in the case of the Western Destin Project, Taylor Engineering performed a borrow site impact analysis for the borrow site used in the Walton Project. Location and Comparison to OK-A The northwest corner of the Walton Borrow Area is roughly 2.75 miles from the northernmost point of the western boundary of the OK-A Borrow Site. See WD Ex. P-13. The area between the eastern-most point of the OK-A Borrow site and the western-most point of the Walton Borrow Area, therefore, is roughly half that distance or 1.375 miles. The northwest corner of the Walton Borrow Area is approximately 0.8 miles offshore; its eastern-most point is roughly one-half mile off-shore. OK-A is larger than the Walton Borrow Area and will have more sand removed. It is also wider, shallow when measured from the Gulf floor, and in deeper water. Nonetheless, because of proximity, Petitioners characterize the two sites as similar. Despite proximity, there are significant differences between the two. A wider, less deeply dredged borrow area would have less impacts than one deeper and narrower. OK-A's location in deeper water makes it less likely to affect waves and current than the Walton Borrow Area. The footprints of the borrow areas are dissimilar. The Walton Borrow Area has an irregular shape. OK-A is in the shape of a rectangle with a uniform dredging depth although "the depth of sand that is dredged will taper off . . . further offshore . . .[s]o that the seaward most edge does not have significant thickness of sand. The maximum cut is towards the northern boundary." WD Tr. 306. The predominately significant difference between the two is the presence on the Gulf floor in the vicinity of the Walton Borrow Area of an ebb shoal: a large deposit of sediment. The ebb shoal exists because of interaction between East Pass and the waves, tides and currents of the Gulf. The Walton Borrow Area is "close to the East Pass ebb shoal . . . and it included the outer flanks of the ebb shoal." WD Tr. 155. It makes the littoral zone for the Walton Project more active than the littoral zone near which OK-A is located. Located a significant distance to the west of the East Pass ebb shoal, OK-A would not interact with its littoral zone in the way the Walton Borrow Area interacts with its littoral zone. Walton Borrow Area Impact Analysis and Monitoring Taylor Engineering's borrow area impact analysis for the Walton Borrow Area was similar to the impact analysis for OK-A in that both consisted of "wave models and hydrodynamic models." WD Tr. 156. The Walton impact analysis showed "one potential impact area about 2,000 feet long [on the beach] just west of East Pass," id., an impact area also described as extending from approximately 3,000 to 5,000 feet west of the westernmost jetty at East Pass. It anticipated that impact would be caused by wave action due to the perturbation resulting from the presence of the dredged Walton Borrow Area. The potential impact was projected by the analysis to be a reduction in the sediment supply to the beaches west of East Pass by 11,000 cubic yards per year. Because of that reduction, DEP included a mitigation condition in the Walton Project permit: placement of 55,000 cubic yards on the impacted beach. As a condition of the Walton Project, Taylor Engineering conducted monitoring of the impacts to the beach from the project in general and in particular from the Walton Borrow Area. At the time of hearing, reports for 2007, 2008, and 2009 had been completed and the engineering firm was working on the 2010 report. Mr. Trudnak described the results from the monitoring through 2008 at hearing. From the period of pre-construction in 2006 through immediate post-construction, the monitoring revealed "a huge volume of erosion." WD Tr. 159. Subsequent analysis from 2007 to 2008 revealed "a huge amount of accretion that actually exceeded the amount of erosion from the previous year." Id. The volumes of erosion and accretion "seemed abnormal." Id. The bottom line, however, of the two years of data is that the early erosion was more than countered by the accretion that occurred into 2008. After describing the impacts in the first two years of monitoring, Mr. Trudnak stressed the importance of what was revealed by additional monitoring. "[M]ore important is the long term trend . . . ." Id. From 2006 through 2009, the monitoring area "as a whole, actually accreted, it gained sand." WD Tr. 160. Determining the impacts to the beach caused by the Walton Project is complicated because of impacts caused by behavior of the beach at the time of construction and earlier. Consistent with the Department's "critically eroded" designations, data from March of 1996 (not long after Hurricane Opal), data from June, 2004 (before Hurricane Ivan) and 2006 pre-construction data showed the shoreline adjacent to the Walton Project Area to have been receding landward at a rapid rate. This "background" erosion is due mainly to the effects of tropical storms. In the wake of the dredging of the Walton Borrow Area it was difficult for Taylor Engineering to determine what impacts were caused by "background" erosion due to tropical storms and what impacts were caused by the dredging of the Walton Borrow Area. In contrast, it is not difficult to determine from monitoring data in the three years after construction of the Walton Project, however, that the beach west of the borrow area has accreted and that this appears to be the long-term trend. WD Tr. 159. Contrary to conclusions Petitioners would have drawn from the evidence presented by their experts, the more comprehensive data indicates that the Walton Project (including its borrow area) is having a beneficial impact on the beaches to the west of the project and its borrow area. Dr. Young opined on behalf of Petitioners that the problem with the OK-A Borrow Area Impact Analysis is that it is based on modeling which is far inferior to "real world" data. His opinion that actual data is superior to data generated by modeling, no doubt, is sound. The only "real world" data that will prove any impacts for sure, whether adverse or beneficial, from a dredged OK-A, however, is after-the-fact monitoring data. Such data is usually obtained annually after the construction of a project or after major storm events. It consists of obtaining near-shore and offshore monitoring profiles and involves determining shoreline changes and volumetric beach changes. In the absence of data from monitoring impacts of a dredged OK-A, Dr. Young opined that the data derived from monitoring the Walton Borrow Area, which showed erosion early after completion of the Project, is superior to the modeling data reviewed by Taylor Engineering in predicting impacts to Santa Rosa Island beaches. There are two problems, however, with Dr. Young's conclusion. First, beach impacts after the dredging of the Walton Borrow Area do not necessarily support similar impacts from a dredged OK-A because the two borrow areas are materially different. Second, the trend revealed by the more comprehensive data gathered in the wake of the dredging of the Walton Borrow Area is that the beach is receiving impacts that are beneficial. Reasonable persons might differ as to the outcome of reasonable assurances with regard to impacts based on the testimony of Mr. Trudnak and Drs. Dally and Young. The balance, however, swings clearly in favor of the applicant in consideration of the testimony of Ralph Clark. Mr. Clark's Review of OK-A Impacts Ralph Clark is a Registered Professional Engineer in Florida. The recent recipient of the Stan Tate Award from the Florida Shore and Beach Preservation Association, a lifetime achievement award for work over the years in beach preservation, and the Murrough P. O'Brien Award from the American Shore and Beach Preservation Association, at the time of hearing, Mr. Clark had worked for 37 years for the State of Florida as a coastal engineer. During his long career, Mr. Clark has worked on the State's two separate regulatory programs in the arena of beach management: a "Wet Beach Program, which is working below Mean High Water and includes projects such as beach restoration" WD tr. 485, and "the more dry beach program which involves construction seaward of Coastal Construction Control Lines and activities landward of Mean High Water . . . ." Id. He has been involved with the Department's Beach Management Program, a grants program for cost-sharing with local governments to develop a long-term comprehensive management plan for the state to solve critical impact problems around Florida which may include erosion. He has conducted or prepared the Critically Eroded Beaches Report every year "going back to the late 1980's" id., and he has "conducted Beach Erosion Studies and Storm Damage Impact Investigations around the State for the past four decades." WD Tr. 486. Specific duties of Mr. Clark's include the review of "scopes of work and project feasibility studies that are provided . . . by the [Department's] Beach Management Section." Id. In this capacity, Mr. Clark conducted the Department's engineering review of the Okaloosa Island Application and additional information related to the Project. On the basis of Mr. Clark's review and his testimony, it is found that "the project is a well designed hurricane protection project that is critically needed to restore the beaches of this beach community of Okaloosa Island " OI Tr. 519. The Project will protect recreational benefits and wildlife habitat in addition to providing necessary storm protection. The placement of 940,000 cubic yard of sand fill as called for by the Draft JCP will provide a significant amount of storm protection from the storm surge and waves of hurricanes or lesser storms that had impacts to the beaches and shores in the Project area. See OI tr. 520. The excavation of the sand from OK-A for the Project along with the excavation of sand from OK-A for all of the other projects the borrow area serves is not expected to have any adverse impacts to the beaches of Santa Rosa Island, including the beaches within the Project area. See WD tr. 488. Mr. Clark's opinions that the Project would be beneficial to the beach and dune system in Okaloosa Island and that the excavation of OK-A is not expected to have adverse impacts have a solid base. His opinions are founded on extensive experience with beach restoration projects over 37 years; extensive experience with coastal processes, coastal morphology, and coastal hydrodynamics; review of the application and supporting information; experience with the Project area and vicinity; extensive experience with coastal storm impacts and beach erosion; and review of roughly three dozen technical documents. Mr. Clark has reviewed 136 beach restoration projects. Of these, 111 were in Florida, six in other states and Puerto Rico, and 19 in countries on every continent in the world other than Asia. But coastal engineering experience in Asia is not missing from Mr. Clark's resume. He has conducted beach erosion control projects and coastal and shore protection projects (as distinguished from beach restoration projects) in that continent as well. Among the "countless number," WD tr. 490, of such projects he has reviewed are ones in the Netherlands, Denmark, Italy, Turkey, Egypt, China, and the Bahamas. Id. The reason his experience extended beyond the State of Florida to nations all over the world is because "the Florida Beach Preservation Program is internationally recognized." Id. The State has received many requests for technical assistance from various world governments. Mr. Clark has also in his time away from his employment with the state served as a consultant to the governments of Mexico, the Cayman Islands, and the Island Nation of St. Bartholomew and the French West Indies. Mr. Clark has investigated the impacts of 83 tropical storms in the Gulf of Mexico. Most investigations have been in Florida but some have been in other Gulf states and along the coast of the country of Mexico. During some of those investigations and while acting as a coastal engineer for the state, Mr. Clark visited the vicinity of Santa Rosa Island 176 times, excluding academic field trips. In his capacity as a state coastal engineer, Mr. Clark provided the Department with detailed damage assessments for each of the eight tropical storms noted in the Consolidated NOI for the Western Destin Project. During his 37 years of service, Mr. Clark has been on numerous task forces, committees and technical advisory groups relating to erosion control and beach management efforts by states along the Gulf and Mexico. Mr. Clark's early reports were used in the development of the state's Strategic Beach Management Plan and he prepared the first "Critically Eroded Beaches in Florida document," WD tr. 494, now electronically available to the public on the Department's website. Mr. Clark performed the "Critically Eroded Shoreline" evaluation for the beaches and shoreline subject to the Project. Storm Protection It is reasonable to expect that hurricanes in the future will have impacts on Okaloosa Island. "Okaloosa Island is completely vulnerable to the impact of a storm surge or waves from, not only a hurricane, but lesser storms and is in need of coastal protection." OI Tr. 536 The best defense against 25-year, 50-year, and 100- year storm events is beach restoration. Comparison to Other Borrow Area Impacts The OK-A Borrow Area is an offshore borrow area. Mr. Clark gave a few examples of other borrow areas that are offshore borrow areas and that are as large as OK-A. These were borrow areas used in the restoration of beaches in Panama City, Delray Beach, Canaveral Shoals, and Anna Maria Island. In addition to Taylor's Borrow Area Impact Analysis Report, Mr. Clark based his opinion on review of monitoring data for the many restoration projects with which he has been involved. Mr. Clark has reviewed borrow area impacts on beach restoration projects that have had adverse impacts. But these projects, typically, were "in inlet ebb tidal deltas of tidal inlets." WD Tr. 518. Located about three miles east of the ebb shoal of East Pass, OK-A is not an inlet-related borrow area. Of the 111 beach restoration projects that Mr. Clark reviewed, there was one that had an off-shore borrow area that adversely impacted the adjacent beach: the Anna Maria Island Project. The Anna Maria Island Borrow Area was located "roughly 1,000 feet off the [adjacent] beach . . . ." WD Tr. 519. In comparison, OK-A "is four to five times further offshore than the Anna Maria Island borrow area." WD Tr. 520. If instead of OK-A, the Project were to use a borrow area as close to the shore as the Anna Maria Island Borrow Area, its impacts to the shoreline would be both adverse and beneficial. The impact to adjacent beach would be erosion, but to the beach to the west of the borrow area the impact would be accretion. Mr. Clark's opinion of no impacts to the beach from dredging OK-A would be entirely different if OK-A had been located in the near-shore zone where "it's a whole different ball game." WD Tr. 532. The location of OK-A, between 4,000 and 5,000 feet offshore is in a zone that is "no problem," that is, it is not in the near-shore and far enough off shore that it will not cause impacts, adverse or beneficial, to the beaches and shores of Okaloosa County. Modeling and Dr. Young's Opinions For all his experience and coastal engineering prowess, Mr. Clark is not an expert in modeling. He relies on others within the Department to evaluate the sufficiency of a model or its methodologies. Mr. Clark did not ask anyone in the Department to evaluate the models used by Taylor Engineering. Dr. Young disagreed with the opinions of Mr. Trudnak and Mr. Clark that there would be no adverse impacts to the beach. He was sure that the dredging of OK-A would cause an adverse impact that would be either erosion or a decrease in the accretion that occurred in recent years along the beaches of Okaloosa Island. Dr. Young also cast doubt on Mr. Clark's experience as support for the opinion that dredging of OK-A would cause no adverse impacts. "Nobody believes there's ever been an adverse impact from a borrow area . . . ." WD Tr. 1206. Dr. Young used the "real world" experience with the Walton Borrow Area to back up that doubt. "[T]he problem is that we're not doing a good job of monitoring this project [the Walton Project] and the problem is convenient interpretation of the monitoring results." Id. Dr. Young's doubt about the value of Mr. Clark's experience was tempered by the reality of beach restoration in contrast to other types of projects whose failure was sudden, dramatic and easily discernible. Dr. Young: [W]hen a bridge collapses, civil engineers converge on that failed project and they learn more from that failure than they could ever learn from a bridge that lasted 30 years. And . . . one of the problems with coastal project design is that never happens. We never have a beach nourishment project that disappears in six months or a borrow area that causes erosion and coastal engineers converge from around the country and say, wow, here's a project that went wrong. And I think that is one of the hurdles that we need to cross in order to do a better job of project design. * * * We have no clear definition of what a failed project is. So, that way you can never have one that fails. And to me, a failed project is one that does not meet the promises made in the design of that project. And a failed project is also one where there are impacts that occur as a result of the project that are not adequately mitigated or anticipated. WD Tr. 1150-1 (emphasis added). When asked the question of whether there is a definition of a failed beach restoration project in the literature or that is generally accepted by the coastal engineering community, see WD tr. 1152, Dr. Young testified, "I have not seen one." Id.. He added, "I would assume they might offer a similar definition [to mine], if the project doesn't work the way we said it would, then we would consider that a failure. But there is certainly not large scale discussion of projects that did not perform as designed." WD Tr. 1152-3. Dr. Young, like Dr. Dally, did not perform any analysis to quantify any degree of erosion or decreased accretion. Nor has he ever performed modeling to analyze borrow area impacts in keeping with his view of the inutility of modeling for accurate prediction of beach impacts. Other Projects Constructed with OK-A Fill The OK-A Borrow Area is the sand source for other projects, several of which have been completed. Of the 7 million cubic yards of sand in OK-A, 1.1 million has been removed for other projects, including two projects on federal property that is part of Eglin Air Force Base, referred to as sites A-3 and A-13 (the "Eglin Projects"), and a small 2600-foot stretch of beach in Destin, referred to as the Holiday Isle Emergency Project. The Eglin Projects The Eglin Projects were completed in May 2010. During the construction phase of the Eglin Projects, hopper loads of OK-A Fill were analyzed on the basis of silt content. "[A] visual shell content analysis and a grain size analysis and color analysis" OI tr. 219, was also conducted on the hopper loads of OK-A Fill. An analysis of carbonate content was not conducted during the construction phase because of expense. Carbonate content analysis was saved for later after "post construction sampling." Id. The Eglin Projects were governed by a Sand Quality Control and Quality Assurance Plan (the "Sand QC/QA Plan") approved by the Department. The Okaloosa Island Project is also governed by a Sand QC/QA Plan. Sand QC/QA Plans The Department requires an application for beach restoration to include a Sand QA/QC Plan by rule: The application shall contain the following specific information: * * * (k) Two complete sets of construction plans and specifications . . . . The plans shall include the following: * * * 4. Permit applications for . . . beach restoration . . . shall include: * * * Quality control/assurance plan that will ensure that the sediment from the borrow sites to be used in the project will meet the standard in paragraph 62B-41.007(2)(j), F.A.C. [the Sand Rule] Fla. Admin. Code R. 62B-41.008(1). The purpose of a Sand QC/QA Plan was explained at hearing by Dr. Koch. It provides an outline of a level of observation and testing that has to be done during construction and post-construction. It provides remediation measures if fill is placed on the beach that is not "beach compatible fill" as defined in the Sand Rule. It is not a method by which the Department obtains reasonable assurance of compliance; reasonable assurance is obtained by the Department through "review of the sediment data." See OI tr. 705. The QC/QA Plan is more like "an insurance policy." Id. If something were to happen that was unexpected or not in compliance with the Sand Rule, the QA/QC Plans ensure that the "dredger is not going to be dredging outside the limits that's . . . outlined in the plan." OI Tr. 706. If non-compatible beach fill "were to be placed on the beach, [the QC/QA Plan] outlines triggers for [remediation] so that [remedial] action can be taken immediately." OI Tr. 707. Application of the Sand QC/QA to Eglin Project A-3 A few of the hopper loads used on Eglin A-3 failed. "One or two had a carbonate content greater than 5 percent. A couple had a grain size that was a millimeter or two under the acceptable range." OI Tr. 220. Given that the hopper used in the Eglin A-3 Project holds 2,500 cubic yards of material and that DEP requires compliance over an area of 10,000 square feet, "sand from one hopper load [that failed] could be blended in with sand from other hopper loads." Id. The remedial measure employed in the Eglin A-3 Project of blending non-compliant fill with good fill did not succeed. Mr. Trudnak offered at hearing that the OK-A Fill used at the Eglin A-3 Project had "a higher percentage of dark material," OI tr. 216, than the fill used in the Emergency Holiday Isle Project and therefore, the sand color in the restored Eglin A-3 Project "is inferior to the [sand color of the restored beach in the Emergency] Holiday Isle Project." Id. The darkness of the material used in the Eglin A-3 Project was confirmed by aerial photography conducted by Dr. Young a month after construction was completed. See discussion, below. Mr. Trudnak attributed the inferior quality of the fill used in the Eglin A-3 Project to the area of OK-A from which it was taken: the southeast and south central portions. Fill taken for the Emergency Holiday Isle Project which Mr. Trudnak opined was superior from the standpoint of color was taken from OK-A's southwest corner. Mr. Trudnak's assessment of the inferior color of the sand placed in the Eglin A-3 Project, however, was not revealed by testing of four post-construction samples taken on May 27, 2010 and tested on June 2, 2010. Those four samples all yielded recorded results for Munsell color at the lightest (and predominate) color assigned to the native beach: 5Y 8/1 or as the post construction testing results admitted into evidence show: "5Y Chroma 1 Value 8." See OI County Ex. 13. These tests results call into question the validity of the tests and other test results of the quality of the sand that is OK-A Fill. Sand Quality Quartz and Carbonate; Native Sand Quartz or Silicon Dioxide, a principal constituent of ordinary sand, is a brilliant, crystalline mineral, occurring in abundance in the earth's crust, most often in a colorless, transparent form. Quartz is usually present in beach sands in high percentages. Like quartz, carbonate also occurs in abundance in the earth's crust and is often present in beach sand. The source of carbonate in beach sand is mainly shells of organisms like clams and scallops. But carbonates that are not from shells also occur in marine environments. These non-shell carbonates may also be constituents of beach sand. The sand on the beaches of Okaloosa Island is predominately quartz and contains an extraordinarily low amount of carbonates. The references to Okaloosa Island beaches as being composed of "sugar white sand" and the beauty of their color which drew the Sherrys to Okaloosa Island is due to their general character as predominately "quartz" beaches to an unusual degree rather than as beaches with a significant amount of carbonate content or other content that would make the color other than "sugar white." As Dr. Young put it in the section of his report which analyzed the carbonate content of OK-A Sand used at A-3, the Eglin East Beach Restoration Project: Okaloosa Island sands are renowned for their unique, mature, quartz composition providing a "dramatic landscape of drifted blinding white sand that often puts northern visitors in mind of snow;" to quote the Walton County Chamber of Commerce website. This project [the Eglin East Project] has replaced that pure quartz sand with beach fill [that] would rank the beach as the highest carbonate content beach on the Panhandle. OI Petitioners' Ex. 40, (un-numbered 5th page). The awareness of the quality and color of Okaloosa Island beaches is accepted by all of the parties to this proceeding. Taylor Engineering, the County's agent, wrote the following in section 3.3 of its Sand Source Investigation Report, entitled "Color Analysis": Residents and visitors cherish the beaches of Okaloosa County for their very white clean sand. Thus, renourishment activity must address maintenance of the native beach sand color. * * * The color analysis determined the Munsell color classification of all the native beach sand samples in Okaloosa County. Taylor Engineering described the majority of them as Munsell Color 5Y8/1 (white) and described several other samples as 5Y 7/1. Notably, the native beach, having been exposed to sunlight and weathering over long periods of time, is lighter in color than in situ potential borrow materials identified in previous sand source investigations . . . . OI Petitioners' Ex. 42 at 16, OKC41283 (emphasis added). In order to ensure that the County's restoration efforts in Okaloosa Island would "address maintenance of the native beach sand color" and other characteristics of the sand native to Okaloosa Island, Taylor and the County made significant effort to comply with the Department's Sand Rule. The Sand Rule Rule 62B-41.007 is entitled "Design, Siting and Other Requirements." Section (1) sets out requirements in general for coastal construction. Section (2) provides special guidelines. Subsection (j) of Section (2) (the "Sand Rule") sets out the guidelines for "beach compatible fill" to be used in coastal construction projects including the beach restoration of the Okaloosa Island Project. The Sand Rule reads as follows: 62B-41.007 Design, Siting and Other Requirements. * * * Coastal construction shall be designed in accordance with established engineering and scientific practice, and the following special guidelines: * * * To protect the environmental function of Florida's beaches, only beach compatible fill shall be placed on the beach or in any associated dune system. Beach compatible fill is material that maintains the general character and functionality of the material occurring on the beach and in the adjacent dune and coastal system. Such material shall be predominately of carbonate, quartz or similar material with a particle size distribution ranging between 0.0062mm (4.0F) and 4.76mm (-2.25F)(classified as sand by either the Unified Soils or the Wentworth classification), shall be similar in color and grain size distribution (sand grain frequency, mean and median grain size and sorting coefficient) to the material in the existing coastal system at the disposal site and shall not contain: Greater than 5 percent, by weight, silt, clay or colloids passing the #230 sieve (4.0F); Greater than 5 percent, by weight, fine gravel retained on the #4 sieve (- 2.25F); Coarse gravel, cobbles or material retained on the 3/4 inch sieve in a percentage or size greater than found on the native beach; Construction debris, toxic material or other foreign matter; and, Not result in cementation of the beach. If rocks or other non-specified materials appear on the surface of the filled beach in excess of 50% of background in any 10,000 square foot area, then surface rock should be removed from those areas. These areas shall also be tested for subsurface rock percentage and remediated as required. If the natural beach exceeds any of the limiting parameters listed above, then the fill material shall not exceed the naturally occurring level for that parameter. Fla. Admin. Code R. 62B-41.007(2)(j) (emphasis added). In compliance with the Sand Rule, the Department seeks to ensure that fill placed on the beach in a restoration project maintains the general character and functionality occurring in the coastal and dune system adjacent to the beach that is the placement site. If a beach is predominately quartz, then the fill should be predominately quartz. The same is true for a beach that is predominately carbonate; the fill to restore that beach should be predominately carbonate. It is the general character and functionality of sand on the beach and the adjacent coastal and dune system where the fill is to be placed that is the baseline against which the Department determines the compatibility of fill. Fill compatible with one beach in Florida is not compatible with all beaches in Florida. Fill that is predominately carbonate, for example, might be compatible with many beaches in the state; it would not be compatible with the predominately quartz coastal and dune systems adjacent to the beaches of Okaloosa Island. OK-A Fill: Not Compatible The environmental functions the Department considered when applying the Sand Rule to this case are nesting habitat for turtles, nesting and foraging habitat for shorebirds and general habitat for beach mice. There may be overlap between the general character of the material at issue and its environmental functionality. Color, a sand characteristic, is a component of the general character of sand. Color can also relate to environmental functionality. It has an effect, for example, on the temperature of the sand which, in turn, determines sex ratios for turtle hatchlings as well as the incubation period for turtle eggs. Sand color, therefore, has an effect on environmental function related to sea turtles. To the extent it affects thermal characteristics of beach sand, color can affect other organisms whose habitat includes beaches. The County and the Department presented evidence that the fill from OK-A ("OK-A Fill") will maintain the environmental functionality on the Project's beaches. The evidence presented by Petitioners to rebut the evidence of the County and Department as to environmental functions or functionality otherwise was insubstantial. The fill from OK-A will maintain the environmental functionality of the Project's placement site. In contrast to environmental functionality, the evidence established that OK-A Fill will not maintain the general character of the native beach subject to the Okaloosa Island Project beach. The finding that the fill will not maintain the general character of the placement site is based on three factors: 1.) carbonate content, 2.) color, and 3.) the presence of 3/4 inch material. Carbonate Content Native Beach Taylor Engineering's Sand Search Investigation Report, see Petitioners' OI 42, Case No. 10-2468, determined the carbonate content of the native beach in Okaloosa Island to be 0.00%. Most beaches in Florida have shell and carbonate content. Carbonate content of "0.00%," therefore, is highly unusual and it underscores the unusual if not unique character of Okaloosa Island beaches. Taylor's determination of "0.00%" carbonate content of the native beach was based on acid digestion tests conducted by Ellis & Associates, a certified laboratory. While there may be other ways of objectively determining carbonate content, acid digestion is the best method. Carbonate content cannot be determined on a percentage basis visually. To arrive at an accurate acceptable percentage, acid digestion is required. See Deposition of Gregory William Stone, Ph.D., at 22. Taylor Engineering conducted tests on 16 sand samples collected by Taylor at four different monuments on the beach and from the adjacent dune system in Okaloosa Island. At R-1 and R- 6, samples were taken at "Mid-Berm," mean high water and mean low water. At R-11 and R-16, samples were taken in areas of dune vegetation, at the dune toe, Mid-Berm, mean high water and mean low water. (Samples were also taken by Taylor in areas of dune vegetation and at the dune toe at R-1 and R-6. These samples were excluded from the analysis by Ellis and Associates because they represented "non-native dune restoration sand trucked in from an upland source." OI Joint Ex. 3G at 2.2). Each of the 16 samples of native beach sand yielded a calcium carbonate content of "0.00%." There was other evidence that indicated that beaches of Okaloosa Island must contain some amount of carbonate, no matter how small, despite Taylor Engineering's testing and analyses that yielded carbonate content at 0.00%. Dr. Stone, the County's witness, testified that in the Okaloosa Island portion of Santa Rosa Island carbonate "is in the swash zone . . . where the waves break, and the water is pushed up and then falls back under gravity." Deposition of Gregory William Stone, Ph.D., at 12. Carbonates from shells are always present in swash zones. Dr. Stone had not conducted carbonate analyses of the native sand and could not testify as to what percentage of Okaloosa Island beach sand is carbonate. During storms, however, large shell fragments are pushed onto the beach. The conflict in the evidence as to the extent to which Okaloosa Island beach sand contains carbonates is resolved by the following. The carbonate content of the native sand is extraordinarily low, at a figure that approaches zero. OK-A Fill Carbonate The persuasive evidence in this case establishes that the carbonate content of OK-A Fill is so much higher than the carbonate content of the sand native to Okaloosa Island beaches that, for this Project, OK-A Fill is not "beach compatible fill," as defined by the Sand Rule. Supportive of the finding is Dr. Young's credible analysis of the OK-A Fill used in the Eglin East Project. The analysis appears in OI Petitioners' Exhibit 40 (marked as "DOAH Case No. 10-2468, Exhibit Sherry 40"), entitled: "Analysis of carbonate content for the Eglin (East) beach nourishment project." Dr. Young acquired 21 random samples of beach sediment in August of 2010 from the Eglin East Project after construction using a sampling grid and ArcGIS. Criticized by the Department because the samples were all taken close to the shoreline and none were taken within the back of the berm to the back of the dune, his methodology for selecting and collecting the samples is found to be reasonable nonetheless. The samples were subjected to standard procedures including "Acid Digestion" for the determination of insoluble residue as an estimate of carbonate content. The data from Dr. Young's "acid digestion/insoluble residue determination," see OI Petitioners' Ex. 40 at 4, show carbonate content to range from as low as 3.89% to as high as 11.81% (using rounded figures). The averaging of the percentage of carbonate content for the 21 samples yields an average carbonate content for OK-A fill of 6.29% (a rounded figure). In addition to Dr. Young's carbonate content results for OK-A fill used in the Eglin East Project, carbonate content acid digestion testing results of OK-A Sand was introduced into evidence as part of the Sand Source Investigation. See OI Petitioners' 42. Table 5.5 of the document, id. at 36, shows that 61 vibracore samples were taken from different locations and different depths at the locations in OK-A. Of the 61 vibracore samples, 24 were subjected to analysis for carbonate content. Several were rejected because they were out of the area to be dredged. The acid digestion tests conducted on Taylor's behalf for the samples selected to be included in the results yielded an average carbonate content of OK-A fill at 3.77%. The carbonate content of OK-A fill, whether measured by Dr. Young or Taylor Engineering, significantly exceeds the carbonate content of seven beaches along the Panhandle of Florida tested for carbonate. These beaches stretch from Perdido Bay in Escambia County to the West to the Walton County 30 A Corridor in the east (with Okaloosa Island being in the middle). The carbonate content in these seven beaches averages 0.6%. The beach with the highest carbonate content of the seven (denominated "Perdido Bay" by Petitioners' Exhibit 3) is located in Escambia County. It is shown to have a carbonate content of 1.4%. Of the seven, the beach with the lowest carbonate content is "Okaloosa Island" at "0." OI Petitioners' 3. The restored beach subject to the Project, therefore, would change from prior to restoration to having either no carbonate content or almost none to being the beach on the panhandle, at least as to its restored portion, with the highest carbonate content by a significant margin. The fill to be used in the Project is not "beach compatible fill" because it will not maintain the general character of the pre-Project sand from the standpoint of carbonate content. 2. Color Unlike the objective testing (acid digestion) that was used to determine the carbonate content of OK-A Fill and sand native to Okaloosa Island, the color of the fill and native sand was determined subjectively. Color determinations were made at various stages in the application process prior to the issuance of the Consolidated NOI. One determination was made when Taylor Engineering conducted an investigation (the "Sand Bleaching Investigation") into how much time it would take for OK-A Fill to lighten up and to what degree it would lighten after it had been excavated and exposed to sunlight and the atmosphere. The investigation led to a report issued in October of 2008 (the "2008 Sand Bleaching Report"). Another determination was made by Ellis and Associates, the laboratory which contracted its work with Taylor. The determinations were reported in a document entitled "Eglin AFB/Okaloosa County/Destin Sand Source Investigation- Okaloosa County, FL" dated October of 2009 (the "2009 Sand Source Report"). Other determinations were made by Department personnel. All of the various color determinations made at the different steps employed the Munsell Color System. The Munsell Color System In Florida, the Munsell System is used to assess the color of beach sand and sand fill used in restoration projects. The Munsell Color System assigns color notations composed of the three dimensions of a color sphere it uses as a model. The three dimensions of the sphere represent hue (five colors of the rainbow and five colors in between each of the five colors), value (lightness), and chroma (saturation or color purity). With regard to hue, Section 3.3 entitled "Color Analysis" of Taylor's Sand Source Investigation Report states, "The hue notation of a color indicates its relation to red, yellow, green, blue and purple." OI Petitioners' Ex. 42 at 16, OKC41283. Hues are identified in Munsell notation by one of ten alphabetical notations that are either a single letter and a number or two letters and a number. The single letter notations indicate the color, "R" for red, "Y" for yellow, "G" for green, "B" for blue and "P" for purple. The double-letter notations are also color notations: "YR" for yellow-red (orange), "GY" for green-yellow, "BG" for blue-green, "PB" for purple-blue, and "RP" for red-purple. The number notation is for one of ten degrees or shades of each hue. The hue that bears a five is not influenced by the adjacent hues. Thus, "5Y" is completely yellow without any influences of "green-yellow" or "yellow-red." The hues that matched the colors of the sand analyzed in this case were either "Y" which stands for "Yellow" or "YR," "yellow-red." The value notation in the Munsell Color System indicates lightness. The Munsell symbols for value span from 0 for absolute black to 10 for absolute white. "Thus, a value of 5 falls visually midway between absolute white and absolute black." Id. The chroma notation "indicates strength or departure from a neutral of the same lightness." Id. The lower the chroma number and the higher the value, the lighter is the color. Munsell color charts used in this case describe a value of 8 and a chroma of 1 to be "white." Thus sand classified as "5Y 8/1" would be a hue of "yellow" that approaches "white" because of value and chroma. Sand classified as "5y 7/1" or 5Y 7/2" as allowed by the permit would not be called "white" but rather, from what appears in Table 1.1 of the Sand Bleaching Investigation Report a grayish shade of "yellow." See OI Joint Ex. 3F at 2. Allowable Color Table 1 of Attachment G to the Application sets out "Sediment Characteristics" as part of the Draft Sand Quality Control and Quality Assurance Plan [the "Draft Sand QC/QA Plan"] for Eglin AFB/Okaloosa Island Beach Restoration Project." OI Joint Ex. 1G. Allowable Moist Munsell Color proposed by the Draft Sand QC/QA Plan for "Native Beach" is "2.5Y 7/1 or lighter." Id., Table 1. For "Borrow Area Acceptable Material Limits," it is "2.5Y 6/2 or lighter." Id. The values of the borrow area were applied for at "6" or lighter because "70 percent of [OK-A] sand has a Munsell value of 7 or lighter and, roughly, 30 percent has value of 6." OI Tr. 362. The moist Munsell colors the Application proposed to be considered as the color of the native beach and acceptable colors for OK-A Fill were not approved by the Department. The Draft JCP set the two, respectively, at "5Y 7/1 - 5Y 8/1" and "5Y 7/2, 2.5Y 7/2, or lighter." OI Joint Ex. 11, last page (un- numbered). A "5Y 7/2" is darker than "5Y 7/1," which in turn is darker than "5Y 8/1," the lightest color assigned by the Draft JCP to the native beach. A "2.5Y 7/2" shares the same value and chroma as a "5Y 7/2" but its hue is not a true yellow; it is of a hue closer to yellow-red (orange) than is the full yellow hue "5Y." Immediately after being dredged, OK-A Fill is darker than the native beach sand. For the time it has been at the bottom of the Gulf, it has not been exposed to natural forces that Taylor hypothesizes to affect the color of the sand on Okaloosa Island's beaches. Native Okaloosa Island beach sand, subject to sun, winds and waves, on the other hand, in Mr. Trudnak's view, has "been in an environment where it's really cleaned up." OI Tr. 212. The Sand Bleaching Investigation conducted by Taylor Engineering concluded that OK-A Fill lightens up once it is dredged and exposed to the elements. Sand Bleaching Investigation Before Taylor prepared its Sand Source Investigation Report that is contained in the Application, it sought to quantify how long it would take to OK-A Fill to lighten and the degree of lightening, if any, after placement on the beach. Taylor's investigation led to a report (the "Sand Bleaching Investigation" and the "Sand Bleaching Report"). See OI Joint Ex. 3F. Forty samples of OK-A fill were kept on the rooftop of a building in Jacksonville and subjected to natural conditions for at least 99 days. The samples were compared to Munsell colors. See the representation of the color of Munsell Hue 5Y in 24 panes on a chart labeled "Table 1.1 Representation of Munsell Colors Used in this Analysis" in the Sand Bleaching Report, OI Joint Ex. 3F, at 2. Values range from 4 to 8 with half steps between each value (4.5 and 5.5, for example) and chromas of 1, 2 and 3. The difference between "5Y 6/1" and "5Y 8/1" is obvious to the human eye. See OI Joint Ex. 3F at 2. The comparison of a sample of sand to Munsell colors and the grading of the sample leading to the assignment of the three Munsell color dimensions do not constitute objective, scientific measurement. Instead, it is merely a visual comparison by the person conducting the test. "[I]t is a subjective test." OI Tr. 237. The grading of the values in Taylor Sand Bleaching Investigation was determined visually by two Taylor employees. As Ms. Naimaster, one of the two Taylor employees testified, "[w]e held the sand up to the book." Naimaster Deposition at 9. Ms. Naimaster did not have any specialized training in use of the Munsell Color System. She was taught how to use the system by the other Taylor employee involved in the grading of the samples, Mr. Hall. Together, the two graded the samples toward the aim of determining the time it took for them to lighten and the degree of lightening. Mr. Hall and Ms. Naimaster reached the conclusion that the majority of the samples taken in the Sand Bleaching Investigation, when exposed to the elements on a Jacksonville rooftop lightened one value, say, "from a Munsell 7 to a Munsell 8 or a Munsell 6 to a Munsell 7." OI Tr. 214. They agreed on most of the comparisons of the samples pre-exposure to the samples post-exposure. When they disagreed, they worked collaboratively: We held the sample up to the book, and he said what he thought, I said what I thought, and we decided together, who was closer. Naimaster Deposition at 11. Mr. Hall, Ms. Naimaster's trainer, was a 27-year old Taylor staff engineer with a Masters of Engineering from Cambridge University in England at the time of his deposition in July 2010. His sole experience with sand bleaching consisted of the work he did that led to the 2008 Sand Bleaching Report. Prior to that work, he had no experience in sand bleaching. Whether quartz sand grains change color when exposed to sun, wind, and water was unknown to Mr. Hall at the time of his deposition. His description of the grading process during the Sand Bleaching Investigation matched Ms. Naimaster's: they agreed on the color selections for the samples "approximately 80 percent of the time; and then on the ones we disagreed, it was fairly quick to come to a consensus." Jonathan Hall DEPO-10- 2468 at 15. The lightening observed by Mr. Hall and Ms. Naimaster did not occur because of a change in the quartz in the samples. It occurred because of changes in the impurities in or on the quartz. Sand Source Grading and Review While anybody can look at a sample of beach sand and compare it to a Munsell color sheet and come up with a subjective determination of the Munsell color dimensions to be assigned, Taylor Engineering relied on a certified laboratory, Ellis and Associates, to conduct the grading of OK-A Fill during the Sand Source Investigation. See OI Tr. 237. The Sand Source Investigation report was also reviewed by Dr. Jennifer Koch, a coastal geologist with the Department, including "the color tests for each of the individual samples." OI Tr. 663. Her review, when it came to color consisted of cross-checking the color data that was provided. Although based on "data" (the samples and the Munsell Color sheets), her review was not conducted using objective standards. It was visual and subjective as she explained: You look at the color information for every individual sample. And then . . . a Vibracore or a portion of borrow area and you kind of look from there. Kind of like creating composites in the same way as you would with sediment data. You look at the overall color and you look at the individual sample color and compare that to what's existing on the beach. OI Tr. 686. Dr. Koch also visited other beach restoration projects to examine OK-A Fill in use. Later, Dr. Koch did her own color testing on samples using the Munsell Color System when she returned to her office. But before she left, Dr. Koch took pictures of the beach restoration in the emergency Holiday Isle project in which OK-A Fill was used. They appear in Department Exhibit 42. The pictures show the fill material to be clearly darker than the native beach sand. Nonetheless, Dr. Koch's assessment of the OK-A Fill used during the Holiday Isle Emergency Project is that "[t]he material was beautiful and it was beach compatible." OI Tr. 703. The Department concluded that the County had provided reasonable assurance that the OK-A Fill material to be used in the Project is beach compatible in every way, including color. The Department's Exhibit 42 establishes that the color of OK-A Fill after placement at Holiday Isle is significantly darker than the native beach. Dr. Young's testimony and other photographs in evidence relate to the color of OK-A Fill more than 100 days after it had been placed on the beach. The testimony and photographs establish that the color of the fill from OK-A is significantly darker than 5Y 8/1, the predominate color of Okaloosa Island native sand, after it has been on the beach for a time long enough to have received the effects of weathering claimed by the Sand Bleaching Investigation Report. The color of the native beach in A-3, one of the Eglin Projects, is rated as 5Y 8/1 or 5Y 7/1, the same as the native beach subject to the Okaloosa Island Project. In Dr. Young's aerials, taken from about 500 feet on June 21, 2010, the line between the restored beach and the native beach is easily seen by their color difference, the fill from OK-A being obviously darker. Sand Source Report Color Conclusions The Sand Source Report states the following: The color analysis determined the Munsell color classification of all the native beach sand samples in Okaloosa County. Taylor Engineering described the majority of them as Munsell Color 5Y 8/1 (white) and described several others samples as 5Y 7/1. Notably, the native beach, having been exposed to sunlight and weathering over long periods of time, is lighter in color than in situ potential borrow materials identified in previous sand source investigations (see Section 2.2). To help establish acceptable borrow material color criteria, the current study evaluated the effects of sun bleaching on sediment color. The color test exposed 40 potential offshore borrow material samples - representing various core borings collected during the detail phase of the investigation (Chapter 5) - to the Florida sun between 12/7/2007 and 3/17/2008 (99 days). Of the 40 samples, 23 began as value 7 and 13 began as value 6. The samples represented various vibracore depths, ranging between 0 ft and 18 ft. The test results, presented in Table 3.5, indicate that all samples with a Munsell value/chroma of 7/1, 7/2, or 7/3 turned white or nearly white (value of 8) due to weathering within 99 days of placement. Approximately 85% of placed sand with a Munsell value/chroma of 6/1, 6/2, or 6/3 lightened in value to at least 7 within that same period. * * * Importantly, the weathering analysis discussed above likely underestimates the level of lightening the beach fill will experience for two reasons. First, the borrow material will undergo a rigorous washing effect through particle abrasion as the sand travels through the dredge pipes during dredge loading and offloading. Second, wind and waves will weather the beach fill. The weathering analysis did not account for such weathering actions. OI Petitioners' Ex. 42, Section 3.3, at 16-17 (emphasis added). The methodology employed in the Sand Source and Sand Bleaching Investigation tests, however, was not scientific. See OI tr. 1424. Explanations The County offered several explanations to minimize the disparity between the quality of sand in OK-A Fill when first placed on the beach and the quality of the sand native to Okaloosa Island. Sand raking is an explanation offered for the low carbonate content of the native sand as determined by Taylor Engineering. "The county has been mechanically cleaning the beaches for close to two decades. Depending upon . . . the season, it's either once every day . . . [or] twice a week . . . [t]hese machines pick up things as small [as] cigarette butts and they've been picking up . . . shells, as well . . . ." OI Tr. 97. The darkness of OK-A Fill used in the Eglin Projects and the darkness of the OK-A Fill in general was attributed by Dr. Stone and Dr. Koch to heavy mineral content. Heavy minerals or iron-bearing minerals occur naturally in Florida Panhandle beach sand and in sand offshore. Dr. Stone's testimony about iron-bearing minerals suggested that OK-A Fill prior to dredging is in an anerobic environment and therefore will lighten when exposed to oxygen in the beach environment was refuted by Dr. Young. As Dr. Young testified, sediments in an anerobic environment are in a reduced form that "tend to look black or gray on the Munsell chart." OI Tr. 1424. Sediments from an anerobic environment are termed "gley," which indicates the presence of reduced iron. The OK-A Fill pumped onto the beach in the Eglin A-3 Project "tend to look more tan or brown, which suggest that the iron in them has . . . been oxidized." OI Tr. 1424-25. Iron imparts much of the color of sediment. If the iron in OK-A Fill has been oxidized prior to excavation, it is not "gleyed." It cannot be expected that it will oxidize and lighten after exposure to air. See tr. 1425 and 1426. As recognized by all parties OK-A Fill at the moment of excavation is darker than the sand native to the beaches of Okaloosa Island. When it is initially placed on the beach, the evidence demonstrates that the rigorous washing effect from particle abrasion as it is piped ashore does not lighten it sufficiently to meet the "whiteness" of the color of the native sand as hoped for by Taylor and the County as the result of their investigations. Aerial photographs of the Eglin A-3 Project taken four weeks after the completion of the project demonstrate "how easily one can . . . delineate the boundaries of the project based entirely on color being assessed at a height of about 400 feet." See OI Petitioners' 8-DDD and 8-GGG. The Eglin A-3 Project was completed at the end of May in 2010. Dr. Young visited the Eglin A-3 site "four or five times," OI tr. 1422, in late June, August and on November 30, 2010. During those visits, including the last visit more than 180 days or six months since completion of the project, he did not observe the OK-A Fill to have "bleached or lightened in color." Id. 3. 3/4 Inch Material Native sand in the beach subject to the Project has little to no material that would be retained on a 3/4 inch sieve. Photographs of OK-A Fill used in the Emergency Holiday Isle Project and at the Eglin A-3 Project were introduced into evidence. They demonstrate the presence in OK-A Fill of an amount of shell material that would not pass through a 3/4 inch sieve much greater than is present on the beach subject to the Project. After the Emergency Holiday Isle Project, an effort was made to remove shells that were in the OK-A Fill deposited on the beach. How much the shell weighed that was removed or how many days of tilling or screening to remove the shells was not established. Mr. Trefilio, the Coastal Management Coordinator acting on behalf of the County "told our contractor to use his professional judgment to basically remove as many shells as possible." OI Tr. 140. Dr. Young' visit to the Eglin A-3 Project and his personal observation establish that the OK-A Fill used at the A-3 site contains a significant amount of shell material that would not be retained on a 3/4 inch sieve. The fill from OK-A already excavated and used in other projects contains material that would be retained on the 3/4 inch sieve in a percentage significantly greater than the percentage of that material on the beach subject to the Project. It is highly likely that any fill taken from OK-A to be used in the Project would contain unacceptably-sized material at significantly greater percentages than on the native beach. Regulatory Public Interest Section 373.414 requires the County to provide reasonable assurance that the activity authorized by the JCP "will be clearly in the public interest" (as opposed to "not contrary to the public interest") since a portion of the OK-A Borrow Area is in an OFW. The statute provides: In determining whether an activity . . . is clearly in the public interest, . . . the department shall consider and balance the following criteria: Whether the activity will adversely affect the public health, safety, or welfare or the property of others; Whether the activity will adversely affect the conservation of fish and wildlife, including endangered or threatened species, or their habitats; Whether the activity will adversely affect navigation or the flow of water or cause harmful erosion or shoaling; Whether the activity will adversely affect the fishing or recreational values or marine productivity in the vicinity of the activity; Whether the activity will be of a temporary or permanent nature; Whether the activity will adversely affect or will enhance significant historical and archaeological resources under the provisions of s. 267.061; and The current condition and relative value of functions being performed by areas affected by the proposed activity. § 373.414(1)(a), Fla. Stat. The Department determined the Project to be clearly in the public interest. In doing so, the Department did not consider the Project's "non-environmental" impacts to the property of others under the authority of Miller v. Dep't of Envtl. Reg., 504 So. 2d 1425 (Fla. 1st DCA 1987). Criterion 1 A distinction is to be drawn between effect on the public health, safety and welfare, on the one hand, and the property of others, on the other hand. The project will not adversely affect the public health, safety or welfare of others. To the contrary it will serve the public health, safety and welfare. The restoration will protect upland structures and property vulnerable to extreme storm events and waves and storm surge should they occur during the life of the Project. The Project will affect the property of the Sherrys and Mr. Donovan by placing sand on the beach waterward of their condominium property that is not beach-compatible fill. The effect is likely to be adverse but to what extent is not established by this record. Criterion 2 The draft permit contains minimization measures during construction to protect endangered and threatened species such as turtles, shorebirds, and mice. The restoration of a critically eroded beach increases the habitat for endangered and threatened species. The environmental assessment developed to address potential impacts to threatened or endangered species, supplemented with literature review of the effects of beach restoration on natural habitat, demonstrates that there will be little to no adverse impacts with the exception of to the benthic infauna communities. Any adverse affects to the benthic infauna communities would be temporary. These communities rebound quickly. The temporary impacts are not considered adverse and they are certainly not significantly adverse. Dr. Robbin Trindell, the Biological Administrator for the State of Florida Management Program, reviewed the Project and concluded that OK-Fill is acceptable for turtle nesting. The conclusion was based on the grain size information submitted by Dr. Stone and from working with the Department's biologists. Criterion 3 The Project will not affect navigation. It is far from inlets and a significant distance from East Pass, which connects Choctawhatchee Bay to the Gulf. The Project may cause erosion, but it may also cause beneficial impacts to the shoreline. Harmful shoaling will not be caused by the Project. Criterion 4 Fishing is not expected to be impacted by the Project. The recreational value of the beach should increase. Marine productivity would not be affected adversely with the exception of the temporary impact to benthic infauna, an impact that would not be adverse in the long term. Criterion 5 The activity will be temporary. Criterion 6 There are no significant historical and archaeological resources in the project area. Criterion 7 The current condition and relative value of functions being performed by the areas affected by the Project will remain the same. It will continue to be a recreational beach adjacent to the Gulf. It will continue to provide habitat to endangered species and wildlife and will provide storm protection. Variance and Conditions The northern boundary of OK-A is within Outstanding Florida Waters ("OFW"). In a letter dated October 14, 2009, Taylor Engineering on behalf of the County requested three variances from rule provisions in chapter 62-4, which governs "Permits," as follows: [W]e request a variance from the provisions of Rule 62-4.244(5)[(c)], F.A.C., to establish a temporary mixing zone greater than 150 meters in an Outstanding Florida Water; a variance from the provisions of Rules 62-4.242(2)(a)2.b., 62-302.700(1), and 62-312.080(3), F.A.C., to establish a maximum allowable turbidity level above background levels for work with an Outstanding Florida Water; and a variance from the thirty-day time period, pursuant to Rule 62-4.242(2)(a)2.b. F.A.C., in which elevated turbidity levels may occur within a mixing zone located in an Outstanding Florida Water. OI Joint Ex. Vol. 3, Ex. 12. Rule 62-4.244(5)(c) which governs "Mixing zones: surface waters" provides: In no case shall the boundary of a dredge and fill mixing zone be more than . . . 150 meters in radius in . . . bodies of water [other than flowing streams], where these distances are measured from the cutterhead, return flow, discharge or other points of generation of turbidity or other pollutants. Rule 62-302.700(1) is in the rule chapter that governs "Surface Water Quality Standards." Entitled "Special Protection, Outstanding Florida Waters, Outstanding National Resource Waters," it provides: It shall be the Department policy to afford the highest protection to Outstanding Florida Waters and Outstanding National Resource Waters. No degradation of water quality, other than that allowed in subsections 62.4.242(2) and (3), F.A.C., is to be permitted in Outstanding Florida Waters and Outstanding National Resource Waters, respectively, notwithstanding any other Department rules that allow water quality lowering. (emphasis added). Rule 62-312.080(3) is in the rule chapter that governs "Dredge and Fill Activities". It provides: "[n]o permit shall be issued for dredging or filling which . . . is within an outstanding Florida Water unless the applicant complies with Section 403.918(2), F.S. (Supp. 1192), and Rule 62-4.242, F.A.C." (emphasis added). Both rules 62-302.700 (an OFW anti-degradation rule) and 62-312.080(3) (an OFW anti-degradation rule applicable to dredging and filling) allow an exception when the applicant complies with rule 62-4.242. Rule 62-4.242(2) sets "standards applying to Outstanding Florida Waters." Subsection (a)2.b of section (2) of the rule reads as follows: (a) No Department permit . . . shall be issued for any proposed activity . . . within an [OFW] or which degrades an [OFW], unless the applicant affirmatively demonstrates that: * * * 2. The proposed activity . . . is clearly in the public interest, and . . . * * * b. the existing ambient water quality within [the OFW] will not be lowered as a result of the proposed activity . . . , except on a temporary basis during construction for a period not to exceed thirty days . . . . [the "Thirty-Day Requirement]. The Department referred to the three variances in its Consolidated NOI as the "Variance" (in the singular rather than the plural). The Department reviewed the request for the Variance under section 403.201(1): Upon application, the department in its discretion may grant a variance from the provisions of this act or the rules and regulations adopted pursuant hereto. Variances and renewals thereof may be granted for any one of the following reasons. There is not practicable means known or available for the adequate control of the pollution involved. Compliance with the particular requirement or requirements from which a variance is sought will necessitate the taking of measures which, because of their extent or cost, must be spread over a considerable period of time. A variance granted for this reason shall prescribe a timetable for the taking of the measures required. To relieve or prevent hardship of a kind other than those provided for in paragraphs (a) and (b). Variances and renewals thereof granted under authority of this paragraph shall each be limited to a period of 24 months, except that variances granted pursuant to part II may extend for the life of the permit or certification. The Department determined that the Variance could be granted to the County for either of the first two reasons, (a) or (b), listed in section 403.201(1). Petitioners do not attack the Variance, however, for failure to meet the requirements of section 403.201(1). Instead, they attack the Variance for failure to satisfy section 120.54(2) [the "APA Variance Statute]: Variances and waivers shall be granted when the person subject to the rule demonstrates that the purpose of the underlying statute will be or has been achieved by other means by the person and when application of a rule would create a substantial hardship or would violate principles of fairness. The APA Variance Statute requires that two elements be met for a variance to be granted pursuant to it: 1.) the purpose of the underlying statute will be or has been achieved by other means; and 2.) violation of fairness (not at issue) or hardship. Hardship Nephelometric turbidity units ("NTUs") in OFWs cannot exceed zero at the edge of the 150-meter radius referenced in rule 62-4.244(5)(c). To keep NTUs at zero outside the 150-meter radius, the County "would have had to almost continually be shutting down . . . .[its hopper] dredge," WD tr. 415, because the turbidity plume created by the hopper dredge's activity would have regularly extended beyond the 150-meter radius. The Variance "allows an anti-degradation allowance of . . . 3 NTU's above background rather than zero NTU's above background at the edge of that mixing zone." WD Tr. 438. Use of a different type of dredge (such as a cutterhead) would not alleviate the need for the Variance for the construction of the Project. A cutterhead dredge is substantially more expensive with regard to both mobilization costs and actual dredging: $15-$20 per cubic yard versus $8 per cubic yard for a hopper dredge. Cutterhead dredges, moreover, do not operate in waves as effectively as hopper dredges. In rough water, "a cutterhead would see much more down time and conditions [could cause] a cutterhead . . . to stop dredging and go into safe harbor into East Pass." WD Tr. 173. The Variance from rule 62-4.244(5)(c), therefore, was needed because the standard-size mixing zone would have created a substantial hardship for the County. Furthermore, the Department had determined that the Project is clearly in the public interest. While the existing ambient water quality within the OFW is likely to be lowered for more than thirty days by the dredging in OK-A, it will not be lowered for more than ninety days, a "temporary" period. It would be a substantial hardship to require the County to meet the mixing zone standards in rule 62-4.244(5((c) and the 30-day requirement in rule 62- 4.242. b. Underlying Statutes: Achievement of Purpose The statutes implemented by the rules covered by the request for the Variance are provisions in either chapter 403 or 373, which control water pollution or protect water resources. No resources in the area, such as hard bottom or sea- grass beds, will be affected by a turbidity plume and an expanded mixing zone. The Department reached the conclusion that the purposes of the underlying statutes would be achieved. The conclusion was based on background knowledge from permitting of borrow areas and beach projects "all over the Panhandle," WD tr. 421, and the data gathered from them including "data from side scan sonar from seismic information all along this area." Id. Included in this background is knowledge of a similar mixing zone of 1,500 meters established for one of the Eglin AFB beach restoration projects which excavated OK-A with a hopper dredge and in which the 1500-meter mixing zone was determined to be appropriate. Independent of the information provided by the County, the decision was founded on the Department's own knowledge that no resources would be impacted by an expanded mixing zone and that there was a comparable project in the area that had been allowed a 1500-meter mixing zone. There were at least two other mitigating factors that the Department entertained as support for its decision. First, because of the difficulty in controlling turbidity in open waters in the Gulf, the 1,500-meter mixing zone established by the Consolidated NOI actually "is on the small side," WD tr. 422, of a mixing zone for the dredging of a borrow area to serve a beach restoration project. Second, 29 NTUs is the maximum turbidity allowed in waters that are not OFW. An extended mixing zone to allow the County to exceed 29 NTUs outside OFW was not granted as part of the variances under the Consolidated NOI. Deepwater Horizon Oil Spill 346. Rule 62B-49.005(16) provides: If site conditions change during the processing of an application to such an extent that the data already provided can no longer be used to determine consistency as provided in this chapter, then the application shall be denied unless the applicant agrees to waive the 90 day time requirements of Chapter 120.60, Florida Statutes, and provides the additional information required to reanalyze the application. After the filing of the Application, malfunction of British Petroleum's Deepwater Horizon offshore oil rig in the Gulf of Mexico led to the Oil Spill, a discharge of a massive amount of oil and natural gas into the Gulf of Mexico. No evidence was presented that showed the Oil Spill had caused impacts to the OK-A Borrow Area. The permit was revised, nonetheless, to add language in the wake of the Oil Spill that requires the County to visually inspect the borrow area prior to construction activity and to analyze sand samples from the borrow area. The County, therefore, plans to send a diver to collect samples to be analyzed for contamination. See WD tr. 175. Prior to the completion of the Emergency Holiday Isle Project, the County hired E-Tech Environmental Consultants to monitor and inspect OK-A. On August 9, 2010, a team of divers investigated the bottom of the borrow area for evidence of oil constituents. "Nothing out of the ordinary was seen on the bottom at the borrow site." OI Tr. 402. The team of divers collected samples at the same time they conducted their visual observation. The samples were sent to Pace Analytical Services in Ormond Beach, Florida, and were received there on August 12, 2010. The results of the analysis showed the presence of no oil constituents. Furthermore, no oil was found in the OK-A Fill pumped onto the beach during the Emergency Holiday Isle Project. A similar inspection, observation, sampling and testing of samples will be conducted prior to the commencement of operation on the Okaloosa Island Project. The QA/QC Plan and the Sand Rule cover foreign material (including oil). The plan and the rule should be sufficient to protect the beaches from oil contamination.
Recommendation Based on the foregoing Findings of Facts and Conclusions of Law, it is recommended that the Department of Environmental Protection issue a Final Order that denies the application of Okaloosa County for issuance of the Joint Coastal Permit for the Okaloosa Island Beach Restoration Project. Denial of the JCP renders the request for the Variance moot. DONE AND ENTERED this 22nd day of September, 2011, in Tallahassee, Leon County, Florida. S DAVID M. MALONEY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 22nd day of September, 2011. COPIES FURNISHED: Gregory T. Stewart, Esquire Nabors, Giblin & Nickerson, P.A. 1500 Mahan Drive, Suite 200 Post Office Box 11008 Tallahassee, Florida 32302 Joseph Alexander Brown, Esquire Hopping Green & Sams 119 South Monroe Street, Suite 300 Tallahassee, Florida 32301 Harry F. Chiles, Esquire Nabors, Giblin and Nickerson, P.A. Post Office Box 11008 1500 Mahan Drive, Suite 200 Tallahassee, Florida 32308 D. Kent Safriet, Esquire Hopping Green & Sams, P.A. Post Office Box 6526 Tallahassee, Florida 32314 Kelly L. Russell, Esquire Department of Environmental Protection The Douglas Building, Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Richard S. Brightman, Esquire Hopping, Green & Sams, P.A. Post Office Box 6526 Tallahassee, Florida 32314 Edward A. Dion, Esquire Nabors, Giblin, & Nickerson, P.A. 208 Southeast Sixth Street Fort Lauderdale, Florida 33301 Walter C. Thompson, Jr. Barkley and Thompson, LC 1515 Poydras Street, Suite 2350 New Orleans, Louisiana 70112 Lea Crandall, Agency Clerk Department of Environmental Protection Douglas Building, Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Herschel T. Vinyard, Jr., Secretary Department of Environmental Protection Douglas Building 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000 Tom Beason, General Counsel Department of Environmental Protection Douglas Building, Mail Station 35 3900 Commonwealth Boulevard Tallahassee, Florida 32399-3000
The Issue The issues to be resolved in this proceeding concern whether the Department of Environmental Protection (DEP) has jurisdiction over the activities encompassed by Permit Application BA-475 (Amended) and, if so, whether issuance of the permit complies with the applicable provisions of Section 161.053, Florida Statutes, and Chapter 62B-33, Florida Administrative Code.
Findings Of Fact Undisputed Facts: The following relevant facts are established by stipulation or admission and are not disputed. The proposed project is landward of the seasonal high waterline within thirty (30) years of December 1996; The project will not interfere with public access; The project will not result in the net excavation of in situ sandy soils seaward of the coastal construction control line (CCCL); Any sandy soil or material excavated for the proposed project seaward of the control line will remain seaward of the control line or setback and be placed in the immediate area of construction; The proposed project complies with the structural provisions of Rule 62B-33.007(2), Florida Administrative Code; The proposed project complies with Rules 62B-33.007(3)(a) through (d) and (f) through (h), Florida Administrative Code. Additionally at hearing, the Petitioners and Intervenor announced that they would not present any evidence on the issue of adverse impacts on marine turtles. Accordingly, impacts on marine turtles are not at issue in this proceeding. Project Description: RHE has proposed constructing a restaurant, pool, deck and stormwater basin within the Boardwalk Beach Resort on Panama City Beach, in Bay County, Florida. The Boardwalk Beach Resort consists of four (4) multi-story hotels with six hundred (600) rooms all together, several pools, boardwalks extending the length of the property and approximately seventeen hundred (1,700) to eighteen hundred (1,800) feet of beach front property. The project site is between Thomas Drive to the north and the Gulf of Mexico to the south. On July 23, 1996, RHE applied to the Department for a CCCL permit to construct, seaward of the interim line established by the emergency Order of October 16, 1995, the restaurant, swimming pool and deck. Part of the proposed deck was located seaward of the coastal construction setback line. On December 9, 1996, the Department issued a permit to RHE to construct the restaurant building with an attached deck fifteen (15) feet landward of the location originally proposed by RHE, as well as for construction of the swimming pool. On December 16, 1996, the Department issued to RHE an Amended CCCL permit authorizing construction of a restaurant building located five (5) feet landward of the location originally proposed by RHE, as well as a deck re-designed so that it would be structurally independent of the restaurant, a swimming pool and a dune enhancement plan which would restore the sandy dune seaward of the pool and restaurant location to its pre-hurricane Opal condition and elevation. The Amended permit would require re-vegetation of the dunes at the site with native plants to secure the dunes from erosion. Both the original and the Amended permits authorized the removal of the stormwater drainage pipe that carried stormwater onto the beach that had caused erosion of the beach near the project area. On January 9, 1997, the Petitioners timely filed a Petition challenging the Department’s decision to issue the Amended permit. On February 7, 1997, the Department established a new CCCL line for Bay County that was farther landward than either the old coastal construction setback line or the interim line established in the October 1995 emergency order. The project authorized by the Amended permit would thus be located entirely seaward of the newly established CCCL for Bay County. As of February 7, 1997, the date the new line was established, RHE had not begun working on the foundation or continued construction above the foundation for any of the structures authorized by the Amended permit. The Department determined that the project did not meet the requirements of Section 161.053(9), and Rule 62B-33.004(1), Florida Administrative Code, so as to qualify for an exemption from complying with the newly established CCCL for Bay County, as the project was not “under construction” at the time the new CCCL was established. The beach and dunes system is wide and the dune system is a significant one, with elevations of fourteen (14) to sixteen (16) feet NGVD, with a wide dune crest. The dry sandy beach in front of the site, even after hurricane Opal struck, remained approximately one hundred twenty-five (125) feet wide. From 1855 to 1934 the shoreline of the site was mildly accretional. Thereafter, until 1955 accretion was less significant, but from 1955 to 1976 became significant. From February 1992 through April 1995, the project site experienced a period of mild erosion. Accordingly the long-term data shows, in essence, that the shoreline is relatively stable at the site. Hurricane Opal caused the dune to erode or retreat landward by approximately a distance of fifteen (15) feet. Hurricane Opal was a major magnitude storm with one hundred twenty-five (125) mile per hour sustained winds and one hundred forty-four (144) mile per hour measured gusts when it came ashore in the vicinity of the proposed site. The dune portion of the proposed site now essentially mimics the pre-Opal conditions. Following hurricane Opal the applicants spent approximately Four Hundred Thousand Dollars ($400,000.00) in dune restoration along the entire shoreline of the resort property, some seventeen hundred (1,700) to eighteen hundred (1,800) feet of shoreline. That dune restoration work was permitted by the Department. There is now little native salt-tolerant vegetation on the site in its natural pre-construction condition. An existing stormwater drainage pipe and catch basin extend onto the beach seaward of the location of the proposed restaurant. The existing pipe and basin have caused erosion of the beach and the sand dune system on the project site. Under the amended permit proposal the stormwater pipe and basin would be removed. All of the proposed structures authorized by the Amended permit would be landward of the pre-Opal coastal construction control line. The proposed pool will be located landward of the dune crest and fifty-five (55) feet landward of the toe of the dune. The proposed restaurant would also be located landward of the dune crest and two hundred five (205) feet landward of the mean high waterline. The original design of the project was for a much larger, three story restaurant. The original pool design called for a one hundred twenty foot pool extending from in front of the Comfort Inn to beneath the proposed restaurant, in effect being located on the first floor of the restaurant. At DEP’s request the size of the pool was reduced by fifty percent (50%) and it was relocated into the shadow of the Comfort Inn next door so that it will no longer serve as an integral part of the restaurant. Pool depths were also reduced to three (3) feet at DEP’s request. The pool, at DEP’s request, will now be constructed of Gunnite concrete material and will be frangible, that is, it will be designed to break up in storm-surge or storm-waves. This will serve to decrease the erosion which could be caused by storm-waves flowing over and around the pool structure. The same is true of the restaurant deck, which at DEP’s request has been re-designed to be separate from the restaurant and also designed to fail in storm conditions. The frangibility of the deck, as now proposed, will retard erosion during storm conditions, as the stormwater or waves will demolish the deck and remove it rather than scouring the sand dune around it. The Department also requested that the existing stormwater drain pipe and catch basin be removed and such a removal has been made a condition of the subject permit. This will require that the applicant design and build a new stormwater system. The applicant has agreed to this condition and the others referenced above. Vegetation: Construction of the proposed project will not result in the removal or destruction of native vegetation. There is no such vegetation on the site where the construction will take place. Thus, construction of the project will not result in removal or destruction of native vegetation which will either cause de-stabilization of a "frontal, primary or significant dune" or cause a significant adverse impact to the beach and dune system due to increased erosion by wind or water. A special condition of the proposed amended permit requires that the applicant submit a dune enhancement plan for restoration of the dunes seaward of the pool and restaurant to its pre-hurricane Opal condition, including re-vegetation. Such a plan was submitted by the applicant and it includes the planting of sea oats on one (1) foot centers. The planting of sea oats as part of the dune enhancement plan will constitute a significant improvement to the native vegetation situation at the site. Disturbance of Sandy Soils: The project will not result in the removal or disturbance of in situ sandy soils of the beach and dunes system to such a degree as to have an adverse impact on the system. That is, the existing ability of the system to resist erosion during a storm will not be reduced. The proposed project will not result in the removal or disturbance of in situ sandy soils of the beach and dune system to such a degree as to cause adverse impact to those systems by lowering existing levels of storm protection to upland properties and structures. All the sandy material excavated for the pool and the stormwater basin will be placed seaward of these structures on the dune in the immediate area of the construction and seaward of the CCCL. The additional sand to be placed on the dune as part of the dune enhancement plan will, in fact, enhance the ability of the system to resist erosion during the storm. The ability of the dune to resist storm erosion is primarily a function of the quantity of sand within the dune system. The additional sand to be placed on the dune as part of the dune enhancement plan will enhance the protection of upland properties and structures including those of the Petitioners and Intervenor. Excavation of the stormwater basin will not destabilize the dune on the project site. The applicant is moving the stormwater basin landward by twenty (20) feet which will minimize the potential impacts of the basin on the dune system. The preponderant evidence establishes that the structure of the pool and pool deck will not cause an increase in structure-induced scour of such a magnitude as to measurably affect shoreline change rates. Scour caused by the pool will not significantly interfere with the beach-dune system's ability to recover from a coastal storm. The frangible design of the pool decreases the likelihood that it will cause any scour. It will break up in a storm so that any scour caused by the pool would be minimal. Any scour caused by the pool would not disturb the topography or vegetation such that the coastal system would become unstable or suffer catastrophic failure. Scour would have no measurable effect. The proposed restaurant and deck will not cause an increase in structure-induced scouring during a storm of such a magnitude as to have a significant adverse impact. The restaurant and deck will be constructed on piles. Scouring around piles, in a storm situation, is very localized and insignificant. By constructing the restaurant and deck on piles at the design elevation, storm-surge and storm-waves will pass under the deck and restaurant. The restaurant and deck are located a sufficient distance landward of the beach and frontal dune to permit natural shoreline fluctuations. The structures will be built on pilings and will be elevated above the storm-surge; thus they will not interfere with shoreline fluctuations. The restaurant and deck are located a sufficient distance landward of the beach and frontal dune so as to preserve and protect beach and dune system stability, in terms of the lack of interference with such. Other structures in the area are seaward of the proposed restaurant and deck, including Pineapple Willies Restaurant, located eleven hundred feet to the west. Those structures have not caused instability of the beach during hurricane Opal. Typically, existing structures do not cause instability of the dune systems. The restaurant and deck are located a sufficient distance landward of the beach and frontal dune so as to allow for natural recovery to occur following storm-induced erosion. Natural recovery commonly occurs under pile-supported elevated structures which is not the case with “slab-on-grade” structures which are not elevated. The pool and pool deck will permit natural shoreline fluctuations, will preserve and protect beach and dune stability, and will allow recovery after a storm because they are designed as frangible structures that will fail and disintegrate in a storm situation. Thus they will not appreciably affect the beach-dune system. Line of Construction: Most coastal construction in Bay County extends out to the pre-Opal CCCL while some construction extends beyond it. Throughout Bay County the line of construction is the pre-Opal CCCL. The line of construction is determined by the most seaward extent of similar existing structures in the immediate area of the proposed structure under consideration in a CCCL permit application. The proposed pool is landward of the line of construction determined by existing pools within the boardwalk beach resort. There are a number of existing multi-story structures to the east of the proposed restaurant that are located out to the pre-Opal CCCL. That pattern of construction continues to the east of the proposed restaurant. Approximately one thousand (1,000) feet to the east of the proposed restaurant is an existing multi-story major structure that is built out to the pre-Opal CCCL. The beach in the area of the project is highly developed with commercial and condominium buildings. Within eleven hundred to twelve hundred feet to the west of the proposed restaurant there is another major structure built out to the pre-Opal CCCL. Just beyond that structure are a number of additional major structures, including Pineapple Willie's Restaurant, that are constructed out to the pre-Opal CCCL. The multi-story major structures to the east and west of the proposed structure are within the immediate area of the restaurant. The proposed restaurant is located landward of the line of construction established by these major structures within its immediate area. That line of construction is the pre-Opal CCCL. DEP did not consider major structures more than one thousand (1,000) feet from the proposed restaurant when it determined the line of construction for the restaurant. It is DEP’s policy when reviewing CCCL applications not to consider structures more than one thousand (1,000) feet from a proposed structure when determining the line of construction. The one thousand (1,000) foot limit DEP uses to determine the line of construction is not embodied in a rule. There was no preponderant coastal engineering or other scientific evidence which justifies the one thousand (1,000) foot limit DEP imposes when it determines the line of construction. It was appropriate to consider the existing structures referenced above in assessing the line of construction for this amended permit application and considering those lying just beyond the one thousand (1,000) foot distance, because those existing structures dominate the coastal processees in the region and only lie just beyond one thousand (1,000) feet to the east and twelve hundred (1,200) feet to the west. If the Department had considered the above-referenced existing major structures just beyond one thousand (1,000) feet of the proposed restaurant, it would have been shown that the proposed project was landward of the thus established line of construction. No preponderant evidence was offered to explicate why the one thousand (1,000) foot limit was automatically adhered to in this situation. Moreover, the line of construction is not a prohibition in and of itself but rather is only one of several criteria that must be balanced in determining whether or not to approve a CCCL permit application. Projects have been approved seaward of the line of construction in the past. Minimization The location of the swimming pool at the most practicable landward location, the reduced size of the pool, as well as its frangible design and limited depth, has minimized its impact. The placing of the excavated material in the pool’s immediate area and the restoration of the dune in front of the pool and deck have minimized the impacts of the pool and deck. The construction of the restaurant on pilings with its design elevation above storm-surge and storm-wave elevations, together with locating it behind the dune crest and away from the active beach, has minimized the impact of the restaurant. The deck is on pilings as well, elevated above storm-surge and storm-wave levels. It will be physically separate from the restaurant and its design frangibility (so that it will fail in a storm) results in its impact being minimized. The stormwater basin is located as far landward as practicable. Its location and the placing of the materials excavated for the basin on the dune immediately adjacent to the basin has minimized the impact of the proposed stormwater basin on the beach-dune system. The restaurant, pool, deck, and stormwater system will not have a significant adverse impact to the beach-dune system. The restaurant will not adversely affect exiting shoreline change rates, will not significantly interfere with recovery following a storm, and will not disturb topography or vegetation such that the system will become unstable or suffer catastrophic failure. Cumulative Impacts The proposed project will not have an unacceptable cumulative impact. There are no other proposed similar projects to take into account and a cumulative impact assessment has shown there to be no adverse cumulative impact. No evidence was offered to show that an unacceptable adverse cumulative impact in terms of existing or other proposed projects will result. Positive Benefit The proposed project will have a net positive benefit on the beach-dune system. The removal of the slab-on-grade constructed building will have a beneficial impact because it will reduce the chance of storm erosion to the beach-dune system posed by such structures. The existing stormwater pipe and catch basin which cause erosion would be removed, resolving that erosion problem. Stormwater will now be retained in a new stormwater basin designed to serve 1.7 acres and it will not flow onto the beach for any rainfall event up to a one hundred year design storm. The new stormwater system is designed to recover quickly after a storm event and to treat stormwater. The removal of the stormwater pipe and catch basin, and the installation of the new stormwater basin will have a positive benefit to the beach-dune system. The new stormwater system complies with Special Permit Condition 7. Moreover the applicant will restore the dune seaward of the project to its pre-hurricane Opal condition and will plant sea oats, on one foot centers, throughout the restoration area in accordance with Special Permit Condition 1.8. Such restoration of the dune and vegetation will benefit the beach-dune system. The natural recovery process will take several decades without the placement of sand in the dune restoration project. The dune enhancement plan submitted by the applicant, in order to comply with Special Permit Condition 1.8, exceeds the requirements of that condition since it places more sand on the dunes than necessary to achieve pre-Opal conditions. Testimony of expert witness Michael Walhter, which is accepted, establishes that restored beaches and dunes function much like natural ones in storm events even though they can be somewhat inferior in resistance to storm-surge and waves since the sand is not as compacted at first. This dune enhancement plan, however, exceeds the permit requirements by placing more sand than necessary on the dunes to achieve pre-Opal conditions. The Interim CCCL On October 16, 1995, the DEP issued its emergency Order establishing an interim CCCL for Bay County one hundred feet landward of the pre-Opal CCCL. The Department established that interim line in order to regulate coastal development in the wake of Hurricane Opal. In 1978 the Legislature established criteria to be used by DEP in establishing or re-establishing all CCCL’s. They are thus to be established to define that portion of a beach-dune system subject to severe fluctuations from a one hundred year storm event. At the time of Hurricane Opal, DEP had not re-established the Bay County CCCL using a one hundred year storm event criterion. The interim CCCL for Bay County established by the above-referenced emergency Order did not utilize nor was it based on the statutory one hundred year storm event criterion. All twenty-three (23) other CCCL’s that have been established based on the statutory one hundred year storm event criterion were established by rule. As of January 15, 1997, the applicant had received all governmental approvals necessary to begin construction of the proposed project except for that which is the subject of this proceeding. On January 22, 1997, DEP by letter advised the applicant to cease and desist construction of the project. On February 7, 1997, the Department by rule then taking effect established a new CCCL.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence of record, and the candor and demeanor of the witnesses, it is, therefore, DETERMINED: That the Department of Environmental Protection has jurisdiction over the proposed project and that it is, therefore, recommended that a Final Order be entered granting the Respondent, Resort Hospitality’s CCCL application consistent with the terms and conditions espoused by the Final Order of December 17, 1997, Respondent’s Exhibit 2 and the project plans depicted in Respondent’s Exhibits 3 and 4. DONE AND ENTERED this 30th day of January, 1998, in Tallahassee, Leon County, Florida. P. MICHAEL RUFF Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 Filed with the Clerk of the Division of Administrative Hearings this 30th day of January, 1998. COPIES FURNISHED: Bram D. Canter, Esquire 103 North Meridian Street Tallahassee, Florida 32301 Thomas I. Mayton, Jr., Esquire Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Station 35 Tallahassee, Florida 32399-3000 Thomas G. Tomasello, Esquire 1315 East Lafayette Street, Suite B Tallahassee, Florida 32301 Neil H. Butler, Esquire Butler and Long, P.A. Post Office Box 839 Tallahassee, Florida 32302-0839 Kathy Carter, Agency Clerk Office of General Counsel 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000 F. Perry Odom, Esquire Office of General Counsel 3900 Commonwealth Boulevard Mail Station 35 Tallahassee, Florida 32399-3000
