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Front Cover 1 Front Cover 2 Title Page Page i Page ii Letter of transmittal Page iii Table of Contents Page iv Page v Page vi Abstract Page vii Page viii Main Page 1 Page 2 Page 3 Page 4 Page 5 Page 6 Page 7 Page 8 Page 9 Page 10 Page 11 Page 12 Page 13 Page 14 Page 15 Page 16 Page 17 Page 18 Page 19 Page 20 Page 21 Page 22 Page 23 Page 24 Page 25 Page 26 Page 27 Page 28 Page 29 Page 30 Page 31 Page 32 Page 33 Page 34 Page 35 Page 36 Page 37 Page 38 Page 39 Page 40 Page 41 Page 42 Page 43 Page 44 Page 45 Page 46 Page 47 Page 48 Page 49 References Page 50 Page 51 Page 52 Page 53 Page 54 Appendix Page 55 Page 56 Page 57 Page 58 Page 59 Page 60 Page 61 Page 62 Back Cover Page 63 Page 64 |
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STATE OF FLORIDA DEPARTMENT OF ENVIRONMENTAL PROTECTION Virginia B. Wetherell, Secretary DIVISION OF ADMINISTRATIVE AND TECHNICAL SERVICES Nevin Smith, Director FLO.RIDA EOLOGI LSU VE Walter S chmrd, .tate.Geoog/st dv/ ef ,. -- / ., INFORMATION CIRCULAR NO, 111 . 1994 AND 1995 FLORIDA pETRpLEUM! \.O PRODUCTION AND EXPLORATION .. -. By ,:.,-Jacqueline' M. Lloyd / 1 '- ; *: } . Published for the FLORIDA GEOLOGICAL SURVEY Tallahassee 1997 STATE OF FLORIDA DEPARTMENT OF ENVIRONMENTAL PROTECTION Virginia B. Wetherell, Secretary DIVISION OF ADMINISTRATIVE AND TECHNICAL SERVICES Nevin Smith, Director FLORIDA GEOLOGICAL SURVEY Walter Schmidt, State Geologist and Chief INFORMATION CIRCULAR NO. 111 1994 AND 1995 FLORIDA PETROLEUM PRODUCTION AND EXPLORATION By Jacqueline M. Lloyd Published for the FLORIDA GEOLOGICAL SURVEY Tallahassee 1997 Printed for the Florida Geological Survey Tallahassee 1997 ISSN 0085-0616 ii LETTER OF TRANSMITTAL Florida Geological Survey Tallahassee Governor Lawton Chiles Florida Department of Environmental Protection Tallahassee, Florida 32301 Dear Governor Chiles: The Florida Geological Survey, Division of Administrative and Technical Services, Department of Environmental Protection, is publishing "1994 and 1995 Florida Petroleum Production and Exploration" as its Information Circular 111. This information is useful to the state and to the oil and gas industry in planning wise development and conservation of Florida's oil and gas resources. Respectfully yours, Walter Schmidt, Ph.D., P.G. State Geologist and Chief Florida Geological Survey TABLE OF CONTENTS Page Abstract ...................................................................................... vii Acknowledegments............................................................................. vii Introd uctio n ....................................................................................... 1 1994 and 1995 Production ................................................................... 1 1994 and 1995 Onshore Drilling Activity............................................... 10 Proposed Everglades Exploration ........................................................... 10 Offshore Drilling Activity...................................................................... 1 2 Exploratory Drilling in State W aters.............................................. 12 Exploratory Drilling in Federal W aters, Offshore Florida................... 16 1994 and 1995 Geophysical Exploration Activity.................................... 17 Florida Oil Field Descriptions................................................................. 17 North Florida Oil Field Summaries ................................................ 20 Introduction ..................................................................... 20 Bluff Springs Field............................................................. 20 McDavid Field .................................................................. 22 Jay Field .......................................................................... 26 Coldwater Creek Field ....................................................... 26 Blackjack Creek Field......................................................... 28 Mt. Carmel Field ............................................................... 30 McLellan Field .................................................................. 30 Sweetwater Creek Field..................................................... 33 South Florida Oil Field Summaries ................................................ 35 Introduction ..................................................................... 35 Lehigh Park Field............................................................... 35 Townsend Canal Field ....................................................... 37 West Felda Field ............................................................... 37 Mid-Felda Field ................................................................. 39 Sunoco Felda Field ............................................................ 39 Corkscrew Field ................................................................ 40 Lake Trafford Field ............................................................ 40 Sunniland Field ................................................................. 43 Seminole Field .................................................................. 45 Bear Island Field ............................................................... 45 Pepper Hammock Field ...................................................... 47 Baxter Island Field............................................................. 47 Raccoon Point Field........................................................... 47 Forty Mile Bend Field......................................................... 47 References ...................................................................................... 50 ILLUSTRATIONS 1. South Florida oil field location m ap................................................. 2 2. Stratigraphic nomenclature, Upper Jurassic to Lower Cretaceous, south Florida ............................................................................... 3 3. Northwest Florida oil field location map .......................................... 4 4. Stratigraphic nomenclature, Middle Jurassic to Lower Cretaceous, north est Florida ......................................................................... 5 5. Oil and gas production, 1943 through 1995.................................... 6 6. Jay field and statewide oil production comparison, 1970 through 19 9 5 ........................................ ....... ........ .. ......... ....... ... .......... 8 7. 1993, 1994, and 1995 oil production comparison for active Florida oil fields, excluding Jay field.............................................................. 9 8. Updated map of 1992 and 1993 exploration wells........................... 11 9. Exploration wells, Florida state waters, including Coastal Petroleum's proposed exploratory well locations................................................ 13 10. 1994 and 1995 geophysical exploration activity.............................. 14 11. Mesozoic structural features in Florida and offshore ......................... 1 5 12. Exploration wells and historic leases, federal waters, offshore Florida... 18 13. Bluff Springs and McDavid fields structure map, top of Smackover Form ation ........................................... .................................... .... 2 1 14. Geophysical log correlation, Bluff Springs and McDavid fields............ 23 15. M cDavid field production curve...................................................... 25 16. Jay field structure map, top of Smackover Formation ....................... 27 17. Blackjack Creek field structure map, top of Smackover Formation ...... 29 18. Mt. Carmel field structure map, top of Norphlet Sandstone ............... 31 19. McLellan and Sweetwater Creek fields well location map.................. 32 20. Geophysical log correlation, McLellan field ...................................... 34 21. Lehigh Park field structure map, top of Sunniland Formation.............. 36 22. Sunoco Felda, West Felda, and Mid-Felda fields structure map, top of Sunniland Form ation..................................................................... 38 23. Corkscrew field structure map, top of Sunniland Formation............... 41 24. Lake Trafford field structure map, top of rubble zone, Sunniland Form ation ................................................................................... 4 2 25. Sunniland field structure map, top of Sunniland Formation ................ 44 26. Bear Island field structure map, base of anhydrite in Upper Sunniland Form ation ................................................... ................................ 4 6 27. Raccoon Point field structure map, top of Sunniland porosity ............ 48 APPENDICES 1. Florida oil field discovery well data................................................. 55 2. 1994, 1995 and cumulative production data................................... 56 3. 1994 and 1995 field well statistics.................................................. 57 4. 1994 and 1995 field wells drilled .................................................. 58 5. Exploratory well drilled in 1993; completion report received in 1994.... 58 6. Oil exploration wells drilled in Florida state waters ........................... 59 7. 1994 and 1995 geophysical exploration activity.............................. 61 8. Florida oil and gas reserve estimates .............................................. 62 ABSTRACT Florida oil production began to decline in 1979 and generally has continued to do so; however, production increased by eight percent from 1993 to 1994. Production then declined by six percent during 1995. Two of the south Florida oil fields (Sunoco Felda and Sunniland) are nearing the end of their production history. The last reported production from Sunniland field was in 1991 and the last reported production from Sunoco Felda field was in 1992. Exploration activity during 1994 and 1995 was very limited. There were no exploratory wells drilled, however, one well which was completed in 1993 is included in this report because the completion report was received in 1994. This Santa Rosa County well was plugged and abandoned as a dry hole. Geophysical exploration during 1994 and 1995 covered only 22.5 miles of seismic lines in the Florida panhandle, 20.3 miles of seismic lines in south Florida, and 102 miles of gravity survey in south Florida. In addition to this completed geophysical exploration, a permit application was pending for an extensive offshore seismic, gravity, and magnetic survey. A similar area was covered by an approved permit during 1992/93 but the permit expired with only minimal magnetic exploration having been conducted. This exploration would potentially explore a dense grid off Florida's Gulf coast extending from offshore of Apalachicola, Franklin County to offshore of Naples, Collier County. One exploratory well was being drilled in federal waters off Florida at the close of 1995. This well .will be the fourth drilled in the Destin Dome area by Chevron. Two of the previously drilled wells were classified by the federal government as producible Norphlet gas discoveries. A summary of offshore exploratory drilling is included in this report, as well as descriptions of each of Florida's 22 oil fields. The descriptions include discovery data, geologic information, and production totals. ACKNOWLEDGEMENTS Several Florida Geological Survey staff members contributed to this report. Special recognition goes to Jim LeBar, Petroleum Engineer with the FGS Oil and Gas Section, for his significant contributions. Jim updated several field structure maps, compiled production statistics, and provided historical and current information on field development, production and exploration. Don Hargrove and Ed Garrett assisted in using and interpreting well and geophysical permit files. Ed Garrett, Jim LeBar, Tom Scott, Walt Schmidt, Deborah Mekeel and Ed Lane reviewed the manuscript and suggested improvements. Jim Jones and Ted Kiper provided base maps, reviewed and suggested improvements to the graphics, and drafted some of the original figures which were updated from earlier petroleum reports. Kim Staubinger (Accounting Systems Analyst, Florida Department of Revenue) provided oil and gas severance tax data. Information Circular 111 1994 AND 1995 FLORIDA PETROLEUM PRODUCTION AND EXPLORATION By Jacqueline M. Lloyd, P.G. #74 INTRODUCTION There are two major oil producing areas in Florida. One is the Sunniland trend in south Florida and the other is the Jay trend in the western panhandle area. The Sunniland trend includes 14 oil fields; the western panhandle includes eight. Appendix 1 lists the discovery well data for these fields. South Florida production began with Florida's first oil discovery at Sunniland field in September, 1943. Of the 14 south Florida oil fields, seven are active, three are temporarily shut- in, and four are plugged and abandoned. These fields are oriented along a northwest-southeast trend through Lee, Hendry, Collier, and Dade Counties (Figure 1). This trend has become known as the Sunniland trend. Production is principally from rudistid reefs found in the upper one hundred feet of the Lower Cretaceous Sunniland Formation (Figure 2). Depth to Sunniland production averages about 11,500 feet. Production in the western panhandle began with the discovery of Jay field in June, 1970. The eight panhandle oil fields are located in Escambia and Santa Rosa Counties, Florida (Figure 3). Five fields are active and three are plugged and abandoned. Production is from Upper Jurassic Smackover Formation carbonates and Norphlet Sandstone sands (Figure 4). Depth to Jurassic production averages approximately 15,000 feet. 1994 AND 1995 PRODUCTION Appendix 2 lists 1994, 1995, and cumulative production statistics for each of Florida's oil fields including oil, gas, and water production data. Appendix 3 lists 1994 and 1995 field well statistics including the number of production, injection, shut-in, and temporarily abandoned wells for each field. Florida oil production peaked at 47.5 million barrels in 1978. Production began to decline in 1979 and generally has continued to do so since then (Figure 5). Total oil production for 1994, however, was 6,073,038 barrels, up eight percent from 1993. Oil production then decreased by six percent during 1995 for a 1995 total of 5,681,618 barrels. Total gas production increased five percent in 1994 and decreased 15 percent in 1995. Gas production totals were 8,446,904 thousand cubic feet (MCF) in 1994 and 7,171,557 MCF in 1995. The production increase northwest short term increase in in 1994 was due to an in production in both Florida and south Florida. Florida Geological Survey EXPLANATION ACTIVE OIL FIELD INACTIVE OIL FIELD LOCATION 0 10 20 MILES 0 10 20 30 KILOMETERS Figure 1. South Florida oil field location map Information Circular 111 STAGE ' 4 l ','',' ,1.1vvvv vvv.Vlv 0 <>L - 108 - - 115 - 125 - -130 -135 - 140 GROUPS AND FORMATIONS I LITHOLOGY RATTLESNAKE HAMMOCK FORMATION zo LAKE TRAFFORD FORMATION / 0 SUNNILAND FORMATION I' I PUNTA GORDA ANHYDRITE ABLE MEMBER 0 C Z I I I' W TWELVE MILE I I MEMBER I S^_____ IIIIIII I -J WEST FELDA SHALE PUMPKIN BAY FORMATION vyvvvv.vvvyvvv I Ivv vv vv v __) __ J '! L BONE ISLAND FORMATION I vy WOOD RIVER FORMATION ---I -J __________________________________________________ APTIAN BARREMIAN HAUTERIVIAN VALANGINIAN BERRIASIAN I LIMESTONE U P DOLOMITE U CLASTICS 17771 ''''V SHALE ANHYDRITE Figure 2. Stratigraphic nomenclature, Upper Jurassic to Lower Cretaceous, south Florida. BROWN DOLOMITE ZONE BASAL CLASTICS FGS060491 ,VVVVVVVVVVVVVVV v-.--,.-.;-v. I I I I I I '1 1 1 1 II I I I I I -7-- ---7----- ///// TITHONIAN Florida Geological Survey R33W1 R32W4 R31W/ SCALE 10 20 10 0 30I 10 20 30 MILES R30W R29W R28W R27V R26W Sqk MT. CARMEL FIELD I 4 McLELLAN 4 FIELD z F FIELD\ BLACKJACK I 9 CREEK FIELD - SANTA ROSA COUNTY S IZ MILTOIN PENSACOLA ~1 GS 0491 FGS010491 Figure 3. Northwest Florida oil field location map. EXPLANATION O ACTIVE OIL FIELD 0 INACTIVE OIL FIELD Information Circular 111 SYSTEM LOWER CRETACEOUS 140 1 145 - UPPER JURASSIC - 155 - - 160 ----..--- MIDDLE JURASSIC STAGE GRO BERRIASIAN I TITHONIAN UPPER KIMMERIDGIAN LOWER KIMMERIDGIAN UPS AND FORMATIONS COTTON VALLEY GROUP UNDIFFERENTIATED HAYNESVILLE FORMATION BUCKNER MEMBER (LOWER HAYNESVILLE FORMATION) SMACKOVER FORMATION OXFORDIAN I NORPHLET SANDSTONE CALLOVIAN LOUANN SALT LITHOLOGY ---- -- - "' I. r. '. ... . .. /. .. ^rT 7 .." r^/ ../ .. '..'.: ".' "' .. ~ / / '. SILTSTONE DOLOMITE ANHYDRITE I CONGLOMERATE SSALT LI]J FGS070491 Figure 4. Stratigraphic nomenclature, Middle Jurassic to Lower Cretaceous, northwest Florida. SANDSTONE LIMESTONE CLASTICS Florida Geological Survey YEAR -U- Oil -+- Gas FGS020197 Figure 5. Oil and gas production, 1943 through 1995. Information Circular 111 The increase in south Florida oil production was most likely due to field or well-specific management (Ed Garrett, Professional Geologist, Florida Geological Survey, personal communication, 1996). The general trend, however, will probably continue to be a declining trend, with two of the south Florida oil fields recently at or near the end of their production history. The last reported production from Sunniland field was in 1991, while the last reported production from Sunoco Felda field was in 1992. All producing wells at Sunoco Felda have been plugged and abandoned. In addition, the single producing well at Lake Trafford field has been periodically shut-in due to mechanical problems and has been producing only sporadically since March 1988. Finally, the operator of Pepper Hammock field has proposed that the field's single well be plugged and abandoned because it is non-commercial (Jim LeBar, Petroleum Engineer, Florida Geological Survey, personal communication, 1996). The Jay field was discovered in 1970 and reached peak production in 1978. It accounts for about 68 percent of the 1994 oil production total, about 67 percent of the 1995 total, and about 70 percent of the cumulative total. Figure 6 graphically compares statewide annual oil production with Jay field annual oil production for 1970 through 1995, clearly showing Jay field's dominance in Florida oil production trends. The Jay field production curve is typical of oil fields produced with tertiary recovery methods (David Curry, Oil and Gas Section Administrator, Florida Geological Survey, personal communication, 1992). Production has generally leveled off since 1987 (Figure 6). This agrees with the projections made by Christian et al. (1981) in their discussion of tertiary recovery estimates for Jay field. They estimated that tertiary recovery would be terminated in 1996, followed by rapid decline to depletion in about 2004. However, this type of level production is difficult to project because it depends, not only on enhanced recovery methods, but also on the price per barrel of oil. Current projections by Jim LeBar (Petroleum Engineer, Florida Geological Survey, personal communication, 1 996) predict production through 2010. Figure 7 is a histogram comparing 1993, 1994, and 1995 oil production for all Florida oil fields except the Jay field. Jay field data would obscure the information for all other fields since its production for 1993 was more than six times greater than that of Raccoon Point field, the next most productive field in Florida during 1993. Northwest Florida production increased by five percent from 1993 to 1994 and decreased by ten percent from 1994 to 1995. South Florida production increased by 22 percent from 1993 to 1994 and by four percent from 1994 to 1995. Oil and gas severance taxes collected for 1994 and 1995 totaled 7.3 million dollars and 7.7 million dollars, Information Circular 111 ^9 1993 1994 1995 1 2 3 4 5 6 7 8 9 1( ACTIVE FLORIDA OIL FIELDS EXCLUDING JAY FGS020397 Figure 7. 1993, 1994, and 1995 oil production comparison for active Florida oil fields, excluding Jay field. Florida Geological Survey 1- 30 25 ' 20 70 72 74 76 78 80 82 84 86 88 90 92 94 YEAR -*- Statewide -I- Jay Field FGS020297 Figure 6. Jay field and statewide oil production comparison, 1970 through 1995. Florida Geological Survey respectively (Kim Straubinger, Accounting Systems Analyst, Florida Department of Revenue, written communication, 1996). Florida currently ranks nineteenth in crude oil production for the nation (World Oil, 1996). 1994 AND 1995 ONSHORE DRILLING ACTIVITY There were no new development wells completed during 1994; only one development well and its sidetrack were completed and abandoned in 1995 (Appendix 4). The original well was drilled in Mt. Carmel field in Santa Rosa County to a total depth of 15,077 feet below MSL and encountered the Smackover Formation at 14,871 feet below MSL and the Norphlet Sandstone at 15,125 feet below MSL. The well had an oil show, however, it was directionally drilled beyond the limits of the permitted irregular drilling unit, and thus had to be sidetracked to a permitted bottom hole location (Jim LeBar, Petroleum Engineer, Florida Geological Survey, personal communication, 1996). The sidetrack well reached a total depth of 1 5,169 feet below MSL and drilled into the Smackover at '14,822 feet below MSL and the Norphlet at 15,076 feet below MSL. The well is in the process of being plugged and abandoned as a dry hole. There were no exploratory wells drilled during 1994 and 1995, however, a well drilled in 1993 is included in this report because it was not reported on until 1994 and was excluded from the previous biennial report on petroleum activities (Lloyd, 1994). This well was drilled in Santa Rosa County, about four miles south of Blackjack Creek field (Appendix 5, Figure 8). The well was drilled to a total depth of 16,414 feet below MSL and encountered the Smackover Formation at about 15,959 feet below MSL and the Norphlet Sandstone at about 16,314 feet below MSL. There were no oil or gas shows in either the Smackover or the Norphlet and the well was plugged and abandoned as a dry hole. PROPOSED EVERGLADES EXPLORATION As discussed in the 1992/93 report (Lloyd, 1994) on petroleum activity in Florida, Shell Western had proposed drilling a wildcat well on the Miccosukee Indian Reservation located within the Everglades in south Florida. At the end of 1993, the Bureau of Land Management was in the process of finalizing the Environmental Impact Statement (EIS) for the proposed exploration and an announcement of the federal "record of decision" was expected in summer 1994. On August 1, 1994 Shell Western officially withdrew its application to drill this exploratory well. Following the withdrawal, the Miccosukee Tribe announced that it intends to make an effort to find others interested in pursuing exploration of the Reservation's mineral potential. Information Circular 111 2.5 TIMES ENLARGEMENT LEGEND APPROXIMATE WELL LOCATION P-280 FLORIDA PERMIT NUMBER A WELL COMPLETED IN 1993, ', 9- NOT REPORTED UNTIL 1994 p-1275- - -vD SCALE 0 50 100 150 MILES I I I 0 80 160 240 KILOMETERS , FcGS0204q' Figure 8. Updated map of 1992 and 1993 exploration wells. There were no new exploration wells drilled during 1994 or 1995. Florida Geological Survey The drill site would have been on Indian land north of Interstate 75 and just west of the L-28 canal in Broward County. The well was to be directionally drilled with the bottom of the hole located beneath one of south Florida's protected water conservation areas. The proposed location was about 12 miles northeast of Raccoon Point oil field which produces from the Cretaceous Sunniland Formation (Figure 2) at about 11,375 feet below mean sea level (MSL). Raccoon Point field is currently the southeastern-most producing field in the Sunniland trend (Figure 1). OFFSHORE DRILLING ACTIVITY State ownership of the continental shelf off Florida extends three miles into the Atlantic Ocean and about 10.4 miles (three marine leagues) into the Gulf of Mexico. The federal government controls resources beyond these state boundaries out to 200 miles. The Outer Continental Shelf (OCS) is a jurisdictional term that describes the offshore area which is under control of the federal government. "Federal waters," in this context, does not refer to ownership, but rather to responsibility (Johnson and Tucker, 1987). Exploratory Drilling in State Waters A total of 19 wells were drilled in Florida state waters between 1947 and 1983 (Appendix 6 and Figure 9). Effective July 1992, all drilling activity was prohibited in Florida state waters (Lloyd and Ragland, 1991), except for within pre-existing lease areas. Only one company, Coastal Petroleum, has pre-existing mineral-rights leases in Florida state waters. Coastal has held leases since 1947 for an area extending from Apalachicola Bay to Naples. The leases originally included all acreage within state waters extending out to 10.4 miles offshore. The leases were renegotiated in 1975, leaving Coastal with full lease rights from 7.4 to 10.4 miles and partial lease rights within the remaining portion of the original lease area. The outer lease area is shown as the offshore shaded area on Figure 10 (this coincides with the company's proposed geophysical exploration area). The information obtained from the 19 wells that were drilled in state waters prior to the ban may be useful in future decisions concerning offshore exploration and development in federal waters. The 19 offshore wells tested three different potential oil horizons. Ten of the wells were within the south Florida Basin (off Charlotte and Lee Counties and off the Florida Keys, Monroe County, Figures 9 and 11) and targeted the Lower Cretaceous. The six wells drilled off the Florida panhandle sought to extend the onshore (and offshore Alabama) Jurassic production (Figures 3 and 9). The remaining three wells drilled off the northern portion of the Gulf coast (Permits 304, 382 and 383) were Cretaceous or possibly Paleozoic tests (Applegate and Lloyd, 1985). Information Circular 111 P-251 17qa * 7.479 1983 1956 P- 7,( 19 LEGEND APPROXIMATE P-280 FLORIDA PERM TOTAL DEPTH FEET BELOW I 1959 WELL COMPLEX A COASTAL PETF EXPLORATORY SCALE 0 50 100 0 80 160 1968 WELL LOCATION IT NUMBER OF WELL, MSL TION DATE ?OLEUM'S PROPOSED WELL LOCATIONS 150 MILES 240 KILOMETERS 240 KILOMETERS Figure 9. Exploration wells, Florida state waters, including Coastal Petroleum's proposed exploratory well locations. P-375-- 12,910 1967 P-297 12.560 1961 15,432 1947 FGS021697 Florida Geological Survey LEGEND PERMITTED AND SURVEYED PERMITTED; SURVEY IN PROGRESS APPLICATION PENDING SCALE 0 50 100 150 MILES 0 80 160 240 KILOMETERS FGS020697 Figure 10. 1994 and 1995 geophysical exploration activity. b Information Circular 111 0 50 100 150 0 80 160 240 FGS120692 Figure 11. Mesozoic structural features in Florida and offshore (after Applegate, 1987). Florida Geological Survey As shown in Appendix 6, only one of the wells drilled in state waters had a significant oil show. A drill stem test of the Gulf Oil-Florida State Lease 826-Y (Permit 275), located near the Marquesas Keys off Monroe County, recovered 15 barrels of 22 A.P.I. gravity oil and 14.1 barrels of saltwater from the Lake Trafford (?) Formation. Another well, which was drilled in federal waters near the Marquesas, tested black saltwater in the Lake Trafford and Sunniland Formations and in the Brown Dolomite Zone of the Lehigh Acres Formation (Applegate and Lloyd, 1985). Exploratory Drilling in Federal Waters, Offshore Florida The first federal oil and gas lease sale off Florida was conducted in May, 1959 off the Florida Keys in what is now the Straits of Florida Planning Area. Ten additional OCS lease sales have occurred since then; seven in the Eastern Gulf of Mexico Planning Area and three in the South Atlantic Planning Area. There have been no sales in the Straits of Florida Planning Area off Florida since the 1959 sale. The last lease sale in the South Atlantic Planning Area off Florida was Sale 78 in July, 1983. Leases in the Eastern Planning Area are shown on Figure 12. The two most recent lease sales off Florida were in the Eastern Planning Area. They were Sales 79 and 94, held in January, 1984 and January, 1985, respectively. Lease sales 79 and 94 are discussed in Applegate and Lloyd (1985) and Lloyd and Applegate (1987). The State of Florida has responded to the public's environmental concerns by objecting to future lease sales and exploration in federal waters off the Florida coast. In response to these concerns, the federal government excluded all areas originally proposed off the Florida coast in Eastern Planning Area Sale 116, held in November 1988. The federal government also agreed to pay nine oil companies a total of $200 million for 73 leases off the Florida coast south of 260north latitude (Pulley Ridge and Howell Hook areas, Figure 12). This settlement permanently excludes the southwest Florida area from petroleum exploration, but does not affect. the area off Florida's panhandle. Florida's Governor Lawton Chiles has said that he will continue to fight for protection of the remainder of the Florida Gulf coastline and is pressing for a permanent 100-mile wide buffer zone around the entire Florida coastline. The 100-mile buffer will be excluded from the next Minerals Management Service five-year (1997-2002) lease plan. At the close of 1995, Chevron was in the process of drilling an exploratory well in the Destin Dome area, 26 miles south of Pensacola, Florida (Block 57, Figure 12, map location code 40). Chevron has successfully drilled two producible Norphlet wells in this area (Block 56, Figure 12, map location code 32) (Lloyd, 1992). In addition to the two Chevron wells, the Amoco-8338 well, Information Circular 111 which was completed in Destin Dome block 111 in 1987, was also a Norphlet discovery described by Gould (1989) as a producible field (Figure 12, map location code 31). This was the first commercial discovery in the Eastern Gulf of Mexico Planning Area (Gould, 1989). These discoveries extend the offshore Norphlet gas trend (which is highly productive off Mobile Bay, Alabama) seaward and eastward from the Mobile map area of the Central Gulf of Mexico Planning Area, offshore Alabama, into the Florida offshore. In addition to these Norphlet gas discoveries, another Amoco well drilled in DeSoto Canyon, Block 133 (Figure 12, map location code 38) was apparently judged to be producible from a Miocene fan deposit (depth to producing horizon is not known). The location is approximately 100 miles south of the Florida-Alabama border; it is not known whether this will spur further interest in federal waters off Florida in this area. 1994 AND 1995 GEOPHYSICAL EXPLORATION ACTIVITY Geophysical exploration during 1994 and 1995 included 102 miles of gravity survey and 42.8 miles of seismic survey. Appendix 7 summarizes the data for the three permits covering these areas. The gravity survey was completed in Highlands County (Figure 10) in an area northeast of the Sunniland producing trend. Of the 42.8 miles of seismic survey, 22.5 miles were located in Santa Rosa County southeast of the known Smackover production. The remaining 20.3 miles were located in south Florida in Lee, Hendry and Collier Counties within the Sunniland producing area. An additional permit application was pending at the end of 1995 which included an extensive offshore area. This application includes seismic, gravity, and magnetic surveys of a dense grid off of Florida's Gulf coast extending from offshore of Apalachicola, Franklin County to offshore of Naples, Collier County (Figure 10). The permit application is incomplete at this time and does not provide seismic mileage or gravity/magnetic survey details. The same area was permitted for exploration in July 1992, however, the permit expired in July 1993 with minimal activity (magnetometer survey off Franklin and Gulf Counties) reported to the Department of Environmental Protection. FLORIDA OIL FIELD DESCRIPTIONS Applegate and Lloyd (1985) and Lloyd (1991) provide a brief history of each of Florida's oil fields including discovery data, geologic information, and production totals. Structure maps were presented whenever possible. These publications are now out-of- print; therefore, this information is summarized again and presented in this report. Fields are discussed in approximate geographic order from Florida Geological Survey SCALE Figure 12. Exploration wells and historic leases, federal waters, offshore Florida (Gould, 1989). Information Circular 111 MAP LOCATION CODES AND WELL DATA FOR FIGURE 12 LEASE NO. MAP OR FLORIDA PLUGGED& TOTAL PLANNING LOCATION MAP BLOCK PERMIT WELL ABANDONED DEPTH AREA CODE AREA NUMBER NO. (P-) OPERATOR NO. (1) DATE (FT.) EASTERN 1 Destin Dome 162 2486 Exxon 1 1974 10,930 GULF OF 2 Destin Dome 118 2492 Exxon 1 1974 7,075 MEXICO 3 Florida Middle Ground 252 2516 Texaco 1 1975 15,663 PLANNING 4 Destin Dome 166 2490 Fina 1 1975 17,608 AREA (21 5 St. Petersburg 7 2527 Shell 1 1975 18,443 1 Destin Dome 162 2486 Exxon 2 1975 10,418 2 Destin Dome 118 2*492 Exxon 2 1975 7,507 6 St. Petersburg 100 2523 Texaco 1 1975 17,388 7 Destin Dome 250 2472 Exxon 1 1975 6,634 8 Destin Dome 207 2480 Exxon 1 1975 4,800 1 Destin Dome 162 2486 Exxon 3 1975 17,938 9 Destin Dome 360 2468 Gulf 1 1975 20,988 10 The Elbow 566 3344 Mobil 1 1977 15,865 11 Destin Dome 617 2463 Chevron 1 1977 10,513 12 Destin Dome 31 2502 Amoco 1 1977 18,338 13 Destin Dome 529 3888 Shell 1 1980 20,450 14 Charlotte Harbor 144 3906 Gulf 1 1981 11,362 15 Charlotte Harbor 672 3917 Tenneco 1 1981 11,302 16 Charlotte Harbor 265 3912 Shell 1 1981 12,362 17 The Elbow 915 3341 Mobil 1 1981 18,128 18 Vernon Basin 654 3903 Mobil 1 1981 10,768 19 Charlotte Harbor 628 3915 Mobil 1 1981 1,270 20 Pensacola 973 3886 Mobil 1 1981 23,264 21 Charlotte Harbor 188 3909 Odeco 1 1981 11,360 22 Destin Dome 563 3890 Sohio 1 1982 21,068 23 Destin Dome 160 6417 Shell I TA 1985 7,764 24 Pensacola 948 6391 Sohio 1 1985 18,958 23 Destin Dome 160 6417 Shell 2 1985 16,953 25 Gainesville 707 6456 Sohio 1 1985 15,941 26 Destin Dome 284 6428 Exxon 1 1985 17,500 27 Destin Dome 422 6438 Chevron 1 1985 22,222 28 DeSoto Canyon 512 6472 Shell 1 1986 12,300 29 Charlotte Harbor 622 4950 Shell 1 1986 10,550 30 Florida Middle Ground 455 8363 Tenneco 1 1986 12,401 24 Pensacola 948 6391 Tenneco 2 ST 1987 19,200 31 Destin Dome 111 8338 Amoco 1 1987 19,240 32 Destin Dome 56 6406 Chevron I TA 1988 22,572 24 Pensacola 948 6391 Tenneco 2 TA 1988 19,200 33 Pensacola 996 6396 Texaco 1 1988 17,910 34 Destin Dome 1 6397 Gulfstar 1 TA 1989 2,000 35 Destin Dome 2 6398 Gulfstar 2 TA 1989 1,800 36 Pensacola 881 6390 Gulfstar 1 TA 1989 2,700 37 Destin Dome 167 6420 Chevron 1 1989 17,128 32 Destin Dome 56 6406 Chevron 2 1990 22,840 38 DeSoto Canyon 133 10444 Amoco 1 1993 12,564 39 Destin Dome 97 8336 Chevron 1 1994 24,084 40 Destin Dome 57 6407 Chevron 1 TA 1996 22,811 SOUTH 1 NH 17-5 208 3686 Tenneco 1 1979 7,754 ATLANTIC 2 NH 17-5 427 3695 Tenneco 1 1979 7,472 PLANNING 3 NH 17-2 913 3664 Getty 1 1979 7,000 AREA (3) 4 NH 17-2 1005 3671 Transco 1 1979 11,635 5 NH 17-5 472 3699 Exxon 1 1979 7,578 6 NH 17-5 564 3705 Exxon 1 1980 12,863 7 NH 17-5 387 N.A. Ocean Prod. GE-1 1977 13,254 STRAITS OF 1 NG 17-10 44 P-296 Gulf 1 1961 4,686 FLORIDA 2 NG 17-10 46 P-290 Gulf 1 1961 7,871 PLANNING 3 NG 17-10 28 P-284 Gulf 1 1960 15,294 AREA (3) 1. TA Temporarily Abandoned; ST = Sidetrack Well. 2. Data from Gould, 1989; Andy Petty, MMS, personal communication, 1992 and 1996; S. M. Fury, Chevron, personal communication, 1996. 3. Data from Karpas and Gould, 1990. Florida Geological Survey north to south and west to east (Figures 1 and 3). More detailed information is presented for the five oil fields discovered since 1985. These are Bluff Springs, McDavid, Coldwater Creek, and McLellan fields in north Florida and Corkscrew field in south Florida. North Florida Oil Field Summaries INTRODUCTION Production in north Florida began with the discovery of Jay field in June, 1970. There are now eight panhandle oil fields located in Escambia and Santa Rosa Counties, Florida (Figure 3). Five fields are active and three are plugged and abandoned. Production is from Upper Jurassic Smackover Formation carbonates and Norphlet Sandstone sands (Figure 4). Jay field is located within a trend which extends through Escambia and Santa Rosa Counties in Florida, and Escambia County, Alabama. Other fields within the trend include Mt. Carmel, Coldwater Creek, and Blackjack Creek fields in Florida and Fanny Church, Flomaton, and Big Escambia Creek fields in Alabama. The fields are located along a normal fault complex which rims the Gulf Coast through Alabama, Mississippi, Louisiana, Arkansas, and Texas (Moore, 1984). Bluff Springs and McDavid fields are located west and southwest of the Jay trend in an area known to be underlain by Louann Salt, with seismic studies indicating salt-induced fault structures in the overlying formations (Lloyd and Applegate, 1987). The remaining two north Florida oil fields, McLellan and Sweetwater Creek, are located east of the Jay trend, near the approximate updip limits of the Smackover Formation (Lloyd, 1989; Applegate et al., 1978; Ottman et al., 1973 and 1976) and could be the result of stratigraphic pinchouts. They are also located within the area known to be underlain by the Louann Salt and may have salt-related trap structures. Current data does not reveal which trapping mechanism produced the Smackover reservoirs for these fields. BLUFF SPRINGS FIELD Bluff Springs field was discovered on March 25, 1984 and was plugged and abandoned in 1991 after producing a total of 242,000 barrels of oil solely from the discovery well (Appendices 1 and 2). The discovery well, the Stone Petroleum Corp. St. Regis Paper Co. number 29-4 (permit 1125), was a rank wildcat located in Section 29, Township 5 North, Range 31 West, Escambia County. It is approximately 10 miles west-southwest of Jay field and approximately four miles southeast of the nearest previously drilled wildcat, permit 1177 (Figures 3 and 13). This area, west and southwest of Jay, is known to be underlain by Louann Salt, with seismic studies indicating salt- induced fault structures in the overlying formations (Lloyd and Applegate, Figure 13. Bluff Springs and McDavid fields structure map, top of Smackover Formation (after Hughes Eastern Corporation, 1988). 21 Florida Geological Survey 1987). Seismic data has been interpreted by Hughes Eastern Corporation (1988) to indicate several small structures in a northwest-to- southeast trend in this specific area. The discovery well produced 477 barrels of oil and 170 barrels of saltwater per day. Oil gravity was 57.00 A.P.I. Production was from Jurassic-age Smackover Formation dolostones from -16,154 to -16,161 feet MSL. These dolostones are dark brownish-gray to brownish-black, fine grained, microcrystalline, and show evidence of recrystallization from originally oolitic and possibly pelletal faces (Lloyd, 1986; Lloyd and Applegate, 1987). The offset well, permit 1136 (Stone Petroleum Corporation St. Regis Paper Company number 29-3) was drilled about one-half mile northwest of the discovery well (Figure 13). The Smackover Formation was encountered at -16,171 feet MSL, structurally 17 feet lower than in the discovery well (Figure 14). The well produced only saltwater from two thin zones (-16,182 to -16,185 feet MSL and -16,192 to -16,195 feet MSL; Figure 14) within the upper Smackover. Core analysis by Location Sample Service, Inc. (LSS), Jackson, Mississippi, yielded mean porosity estimates for these zones of 11.4 and 8.4 percent, respectively. LSS found a trace of oil in one sample at -16,185 feet MSL. This well may be located too low on the structure. Alternatively, as shown on the structure map (Figure 13) drawn by Hughes Eastern Corporation (1988; based on geophysical and well data), Hughes believes there may be a permeability barrier between the discovery well and this well. Ownership of the discovery well transferred to Hughes Eastern Corporation in 1985. Permits were issued to Hughes Eastern to drill two additional offsets, one east and one southeast of the discovery well (permits 1204 and 1205, Figure 13). Permit 1204'was completed in August 1986. The Smackover was again found at a structurally lower position (Figure 14), this time 44 feet lower. Two zones of saltwater production were also encountered (-16,208 to -16,211 feet MSL and -16,215 to -16,233 feet MSL; Figure 14). LSS core analysis yielded mean porosity estimates of 23.9 and 13.6 percent, respectively, and no indications of oil. As interpreted by Hughes Eastern Corporation (1988) (Figure 13), the Smackover in this well is below the probable oil-water contact. The third offset, permit 1205, was not drilled. The location for permit 1205 is actually closer to McDavid field (discussed below) and is outside the potential productive limits drawn by Hughes Eastern Corporation (1988) (Figure 13). McDAVID FIELD McDavid field was discovered on June 14, 1988 with the first production test of the discovery well, the Hughes Eastern Corp. Walker-Baley number 34-2 (permit 1230, Appendix Information Circular 111 Nr M C'. .1 'L[ Figure 14. Geophysical log correlation, Bluff Springs and McDavid fields. Florida Geological Survey 1). This field was also plugged and abandoned in 1991 after producing solely from its discovery well. McDavid field produced a total of 150,000 barrels of oil (Appendix 2). The discovery well is located in Section 34, Township 5 North, Range 31 West, Escambia County (Appendix 1). It is about one and one-half miles southeast of the Bluff Springs discovery well (Figures 3 and 13). As discussed above for Bluff Springs field, this area, west and southwest of Jay, is known to be underlain by Louann Salt, With seismic studies indicating salt-induced fault structures in the overlying formations (Lloyd and Applegate, 1987). Seismic data has been interpreted by Hughes Petroleum Corp. (1988) (Figure 13) to indicate several small structures in a northwest to southeast trend in this specific area. The discovery well produced 235 barrels of oil per day and no saltwater. Oil gravity was 53.80 A.P.I. Production was from Jurassic-age Smackover Formation dolostones from -16,075 to -16,089 feet MSL. These dolostones were described by LSS as gray to dark gray, sucrosic to granular, with poor to fair porosity and permeability. Examination of core chips with a binocular microscope concurs with this description. Core analysis by LSS yielded a mean porosity estimate of 15.9 percent for this zone. Geophysical log analyses by Charles Tootle (Professional Engineer, Florida Geological Survey, personal communication, 1988) yielded a mean porosity estimate of 12.8 percent, an original oil in place estimate of 4,987,347 barrels, and a recoverable oil estimate of 498,736 barrels (Appendix 8). The first offset, permit 1234 (Hughes Eastern Corporation Jones Estate number 34-1) is located about one-half mile southeast of the discovery well (Figure 13). The offset was completed in June 1989. The Smackover Formation was encountered at -16,099 feet MSL, structurally 24 feet lower than in the discovery well (Figure 14). The structure map (Figure 13) was drawn prior to the time this well was drilled. As shown on the map, Hughes Eastern Corporation expected to encounter the Smackover at about -16,050 feet MSL in this well. Based on the actual depth (-16,099 feet MSL), the McDavid structure is probably smaller than that shown. The productive limit expected by Hughes is still below this depth (at about -16,200 feet, Figure 13); however, analysis of geophysical logs from this well indicate that the oil-water contact may actually be at about -16,102 feet MSL (Joel Duncan, professional geologist, Florida Geological Survey, personal communication, 1991). In addition, production from the discovery well appears to have peaked around December 1988 and may have depleted this small structure enough to move the potential productive limits above the level of the Smackover in the offset (Figure 15) (Joel Duncan, professional geologist, Florida Geological Survey, personal communication, 1991). Information Circular 111 MONTH/YEAR -i- Oil -- Water FGS160491 Figure 15. McDavid field production curve. Florida Geological Survey JAY FIELD Jay field was discovered in June, 1970, by the drilling of the Humble St. Regis number 1 (permit 417) in Section 43, Township 5 North, Range 29 West, Santa Rosa County (Figures 3 and 16 and Appendix 1). The well produced from the Smackover Formation from -15,264 to -15,318 feet MSL. The initial production test yielded 1,712 barrels of 50.70 A.P.I. gravity oil and 23 barrels of saltwater per day. Jay field is located within the "Jay trend" of Escambia and Santa Rosa Counties, Florida and Escambia County, Alabama (discussed in north Florida oil fields introduction above). The northern extension of Jay, in Escambia County, Alabama, is the Little Escambia Creek (LEC) field. Oil accumulation at Jay is within an asymmetric anticline with the fault complex forming the eastern barrier to oil migration (Figure 16) (Applegate and Lloyd, 1985). The northern limit of Jay field is a porosity barrier in Alabama where the lithology changes from porous dolostone to dense, micritic limestone. The porosity at Jay field is due to dolomitization of the pelletal grainstones in the upper, regressive section of the Smackover Formation. Dolomitization, fresh water leaching, and an anhydrite cap rock (Buckner Member of the Haynesville Formation, Figure 4) have formed a complex, extensive reservoir. Numerous analyses of the Jay area Smackover Formation, including comparisons with modern carbonate environments, have been made in attempts to understand this complex reservoir (Ottman et al., 1973 and 1976; Sigsby, 1976; Mancini and Benson, 1980; Lomando et al., 1981; Vinet, 1984; Moore, 1984; Bradford, 1984; Lloyd et al., 1986). Despite the complexity of the Jay field Smackover Formation reservoir, exploration and development of the field have been extremely successful. Core analyses were combined with bottom hole pressure data, porosity log information, and other geologic data to arrive at a highly successful reservoir management program (Shirer et al., 1978; Langston et al., 1981; Langston and Shirer, 1985). As of December 1995, Jay field was producing from a total of 51 wells, 32 wells were temporarily shut- in, and there were 28 injection wells (Appendix 3). Cumulative production for Jay field, as of the end of 1995, was 387,815,585 barrels of oil (Appendix 2). COLDWATER CREEK FIELD Coldwater Creek field was discovered on June 4,. 1988. The discovery well was a reentry of a Smackover wildcat. The original permit was issued to Inexco Oil Company (permit 1173). The location is about two miles east of the southern portion of Jay field in Section 26, Township 5 North, Range 29 West, Santa Rosa County (Figure 3). Inexco began drilling Information Circular 111 JAY FIELD ESCAMBIA AND SANTA ROSA COUNTIES, FLORIDA STRUCTURE MAP TOP OF SMACKOVER- NORPHLET OIL POOL R 30W O4 R 29W 911 ALABAMA 4- s 30 2 F L 0 R D A ,&,',* ,9 , S15 977r I 3 0 -150 3 D sa 061N25 14 95 40 U- 4 -l42 149.53 4 9o I s -1 4 8 4l-s75/ 411 \0 4 52 Ia 20 4 o \\ 52s PERMIT NUMBER s +5, 2o 22 DEPTH BELOW MSLOj .....1, 470 PRODUCER 2\ 2r 23 D DRY HOLE 24 N\ ABANDONED PRODUCER \ \ 1 1 25 -152 5 2 00 WATER INJECTION WELL OIL/WATER CONTACT. 1974 ooa a 25 1 $i R 30 W R 29 W ; SCALE 0 0.5 1 2 MILES 1 1 2 KILOMETERS D\ * Figure 16. Jay field structure map, top of Smackover Formation (after Jay-LEC Fields Unit Geological Committee, 1974). S^ ^ ^ ^ ^ KLO E ER ________________^_______0__73^ ' Figure~ ~~~~~~~~6 116. 0a"il tutr atpo makvrFrain(fe a- Florida Geological Survey in November, 1985. They drilled the well to a total depth of -15,407 feet MSL, logged the well, and recommended plugging and abandonment. The top of the Smackover Formation had been encountered at -14,969 feet MSL; the Norphlet Sandstone at -15,331 feet MSL. Side wall core analyses by Location Sample Service, Inc. (Jackson, Mississippi) indicated a potential oil productive zone from -14,985 to -15,016 feet MSL. Mean porosity of the zone was about 14.8 percent. Analysis of the same interval by Charles Tootle yielded a mean porosity of about 12 percent, an original oil in place estimate of 2,080,107 barrels, and a recoverable oil estimate of 312,016 barrels (Appendix 8). Louisiana Land and Exploration Company (LL&E) took over operations on January 10, 1986 and plugged and abandoned the well. Bruxoil, Inc. then took over responsibility for the well. They conducted a geophysical survey across the area (geophysical permit G- 70-86; see Lloyd, 1989). The stated purpose was to determine whether to reenter the existing well or drill at a new location. They decided not to reenter the well and have not submitted any permit applications to drillJrinthe vicinity. In 1987, Red Rock Oil and Minerals Corporation received permit 1220 (Appendix 1) to reenter the well. They completed redrilling on May 24, 1987 and ran the first production test on June 4, 1988. This test yielded 152 barrels per day of 46.50 A.P.I. gravity oil and 280 barrels per day of saltwater. In a retest on December 27, 1988, the well flowed 259 barrels per day of 46.50 A.P.I. gravity oil with no saltwater production. Production is from the zone discussed above, from -14,984 to -15,006 feet MSL in the Smackover Formation. Judging from the field's location within the Jay trend, it appears that reservoir formation may have been structurally related to the Foshee Fault System; however, a single well does not yield sufficient information to test this hypothesis. No additional wells have been drilled at Coldwater Creek field. Cumulative production, as of December 1995 from Coldwater Creek field was 80,068 barrels of oil from this single well (Appendix 2). BLACKJACK CREEK FIELD The Blackjack Creek field discovery well was the Humble Oil and Refining Company St. Regis Paper Company number 13-3 well (permit 523) drilled in Section 13, Township 4 North, Range 29 West, Santa Rosa County, about eight miles southeast of Jay field (Appendix 1, Figures 3 and 17). The well was completed February 14, 1972, as a producer in the Norphlet Sandstone from -15,965 to -15,975 feet MSL. Initial production was 371 barrels of 51.30 A.P.I. gravity oil and 4.5 barrels of saltwater per day. Due to limited productivity and water production from the Norphlet Information Circular 111 FGS020997 Figure 17. Blackjack Creek field structure map, top of Smackover Formation (after Blackjack Creek Geological Committee, 1974, modified by Jim LeBar, Petroleum Engineer, Florida Geological Survey, personal communication, 1996). Florida Geological Survey Sandstone, the well was recompleted as a Smackover Formation producer from -15,633 to -15,743 feet MSL. The initial production test from the Smackover, on January 22, 1975, yielded 1,428 barrels of 51.20 A.P.I. gravity oil and no saltwater. Blackjack Creek field now produces primarily from oolitic dolostones of the Smackover Formation (Applegate and Lloyd, 1 985) A single well, permit 1080 (Figure 17), produces from the Norphlet Sandstone. The trapping structure is an anticline located on the downthrown, southwest side of the regional Foshee Fault System (Figure 17). Similar to Jay field, Blackjack Creek has been carefully cored and analyzed to achieve a successful reservoir management and development program. Cumulative production for Blackjack Creek field was 56,805,223 barrels through December 1995 (Appendix 2) Of this total production, 578,533 barrels were produced from the Norphlet Sandstone and 56,226,690 barrels were produced from the Smackover Formation. Through January 1996, 18 producing wells and seven dry holes had been drilled at Blackjack Creek. Ten wells were actively being produced as of December 1995 (Appendix 3). MT. CARMEL FIELD Mt. Carmel field was discovered in December 1971 by LL&E. The discovery well was the LL&E Finley Heirs number 39-3 (permit 504), located about one mile east of Jay field in Section 39, Township 5 North, Range 29 West, Santa Rosa County (Appendix 1, Figures 3 and 18). Initial production was 1,440 barrels of 470 A.P.I. gravity oil per day with no saltwater. Mt. Carmel field is separated from Jay field by the Foshee Fault System (Figure 18) Mt. Carmel field produces both oil and gas from the Smackover Formation and the Norphlet Sandstone. Complex reservoir geometry has apparently made development of this field more difficult. As of January 1996, three producing wells and 12 dry holes had been drilled at Mt. Carmel field. There is currently one producing well in the Mt. Carmel field. As of the end of 1995, the field had produced 4,770,745 barrels of oil (Appendix 2). McLELLAN FIELD McLellan field was discovered on February 15, 1986, with the initial testing of the Exxon Corporation - State of Florida number 33-1 (permit 1194, Appendix 1, Figures 3 and 19). The well is located about 3.25 miles north of the abandoned Sweetwater Creek field in Section 33, Township 6 North, Range 26 West, Santa Rosa County. An initial flowing test of the discovery well produced 1 52 barrels of 410 A.P.I. gravity oil per day and no saltwater. Production is from Smackover Formation dolostones from -13,827 to -13,845 feet MSL (Figure Information Circular 111 FGS021097 Figure 18. Mt. Carmel field structure map, 1974). top of Norphlet Sandstone (after Miller, Florida Geological Survey ALABAMA FLORIDA 29 5 P175 8 1 0 1 MI 1.6 0 1.6 KM SCALE EXPLANATION 1136 PERMIT NUMBER -16176 DEPTH 0 PRODUCER 4- DRY HOLE - S P12260 -13773 P153 0 P1194 -13815 - - * P1206 -13788 R26W R25W 25 I 36 T 6 N T 5 N T5N * P881 -14045 4- P890 -14071 22 d (.) 01 23 24 Z Figure 19. McLellan and Sweetwater Creek fields well location map. McLELLAN FIELD 6 7 SWEETWATER CREEK FIELD Information Circular 111 20). Core analysis of a potential oil and gas productive zone from -13,819 to -13,845 feet MSL by Core Laboratories, Inc. (Dallas, Texas) indicated a mean porosity of 12.3 percent. The analysis showed additional oil and gas production potential between -13,854 and -13,863 feet MSL. Mean porosity is about 15 percent for this zone. Both of the analyzed zones contained dark, fine grained, microcrystalline dolostones with vuggy porosity. McLellan field is located within the area known to be underlain by the Louann Salt and may have a salt- related trap structure. It is also located within a few miles of the approximate updip limits of the Smackover Formation (Lloyd, 1989; Applegate et al., 1978; Ottman et al., 1973, 1976); thus, the trap could be a stratigraphic pinchout. Current data does not reveal which trap mechanism produced the Smackover reservoir for this field. The first offset and confirmation well for the field was the Exxon Corporation State of Florida number 34-2 (permit 1206). It is located about one-half mile east of the discovery well (Figure 19). It was tested on March 9, 1987 and flowed 641 barrels of 43.40 A.P.I. gravity oil and 24 barrels of saltwater per day. The Smackover Formation was encountered at -13,788 feet MSL, 27 feet higher than in the discovery well (Figure 20). Production is from the Smackover Formation from -13,797 to -13,847 feet MSL. Core analysis by All Points, Inc. (Houston, Texas) yielded a mean porosity of 11.5 percent for the productive zone. A second offset to the discovery well, Exxon Corporation State of Florida number 28-4 (permit 1226) was drilled about one-half mile north of the discovery well (Figure 19). During initial production tests, in February 1988, the well flowed 154 barrels of oil (gravity not reported) and 171 barrels of saltwater per day. The Smackover was encountered 42 feet higher in this well than in the discovery well (Figure 20), indicating a fairly steep gradient between these wells. This second offset well has since been converted to a salt water disposal well. As of December 1995, production for McLellan field was from the two remaining wells and totaled 351,617 barrels of oil (Appendix 2 and 3). SWEETWATER CREEK FIELD Sweetwater Creek field was discovered on April 22, 1977, with the successful flow test of the Houston Oil and Minerals Corporation W. M. Stokes number 15-2 well (permit 881, Appendix 1, Figures 3 and 19). The well is located in Section 15, Township 5 North, Range 26 West, Santa Rosa County. In the initial test the well produced 624 barrels of 43.50 A.P.I. gravity oil and only a trace of saltwater from a Smackover limestone interval from -14,044 to -14,085 feet MSL. This test data spurred rumors that a "new Jay" field had been discovered. Rumors proved to be false and an Florida Geological Survey KO CD oJ 0U 0^ I^ Figure 20. Geophysical log correlation, McLellan field. . O- 0 E E>. 00 0 oC 0 Information Circular 111 offset drilled in 1978 to the south of the discovery well was dry (permit 890, Figure 19). Core analyses of the Smackover Formation in the offset well by Core Laboratories, Inc. (Dallas, Texas) indicated very fine crystalline, gray brown limestone and dolostone, with low porosity and permeability, and potential for only saltwater production. The field produced a total of 13,695 barrels of oil during its entire lifetime (Appendix 2). The discovery well was the only producer at Sweetwater Creek field and was plugged and abandoned in December 1980, after it began producing 100 percent saltwater. South Florida Oil Field Summaries INTRODUCTION South Florida oil production began with Florida's first oil discovery at Sunniland field in September, 1943. There are now 14 oil fields in south Florida, oriented in a northwest- southeast trend through Lee, Hendry, Collier and Dade Counties (Figure 1). Of these 14 Sunniland trend oil fields, seven are active, three are temporarily shut-in, and four are plugged and abandoned. Reservoirs found along the Sunniland trend are composed of localized buildups of organic debris into mounds or pods which formed porous grainstones within the upper Sunniland Formation (Figure 2). The fauna which make up these bioherms include rudistids, algal plates, gastropods, and foraminifera. Dolomitization has enhanced the porosity of these grainstones. The grainstones grade laterally into nonporous, miliolid-rich mudstones (Means, 1977; Mitchell- Tapping, 1984, 1985, and 1986). These miliolid mudstones often provide the trapping mechanism for these reservoirs. The exception to the above general description of south Florida oil fields is Lake Trafford field. Lake Trafford produces oil from a fractured limestone in the lower Sunniland Formation (Means, 1977). LEHIGH PARK FIELD The discovery well for the Lehigh Park field was the Exxon Consolidated Tomoka number 22-4 (permit 712) drilled in Section 22, Township 44 South, Range 26 East, Lee County (Appendix 1, Figures 1 and 21). This is the most northwesterly field in the Sunniland trend. The discovery well was completed on July 30, 1974, in the -11,349 to -11,354 foot MSL interval of the Sunniland Formation. Initial production was 490 barrels of 27.60 A.P.I. gravity oil and 48 barrels of saltwater per day. This well was later abandoned and a deviated well (permit 712A) was drilled at the same surface location to produce higher on the structure. A total of nine dry holes were drilled to delineate this field. All of the producing wells were directionally drilled because bottom hole locations are beneath the town of Lehigh Acres. Florida Geological Survey LEHIGH PARK FIELD LEE COUNTY, FLORIDA STRUCTURE MAP TOP OF SUNNILAND FORMATION SCALE 0 0.5 1 MILE 0 1 KILOMETER EXPLANATION 34 35 -11310- 525 PERMIT NUMBER T 44 s -15250 DEPTH T 45 s I PRODUCER DRY HOLE A SALT WATER DISPOSAL Figure 21. Lehigh Park field structure map, top of Sunniland Formation (after Ferber, 1985) Information Circular 111 Figure 21 is a structure map of the top of the Sunniland Formation (Ferber, 1985) at Lehigh Park field. The reservoir appears to be typical of the south Florida Sunniland trend fields, a leached limestone bioherm. Core analysis by R. E. Laboratories, Inc. (Dallas, Texas) yielded an average porosity of 19.7 percent for the Sunniland Formation from -11,337 to -11,364 feet MSL. They described this interval as a tan to brown, fossiliferous, partially dolomitized limestone. One well was actively producing, and production totaled 5,462,076 barrels of oil at the end of December 1995 for this field (Appendices 2 and 3). TOWNSEND CANAL FIELD Townsend Canal field is located in Section 2, Township 45 South, Range 28 East, Hendry County, approximately three miles north of Mid- Felda field, within the Sunniland trend (Figure 1). It was discovered on June 27, 1982, with the first production test of the Natural Resources Management Corporation A. Duda & Sons number 2-3 well (permit 1070). The test produced 160 barrels of 28.40 A.P.I. gravity oil and 42 barrels of saltwater per day. Production is from the Sunniland Formation between -11,363 and -11,368 feet MSL (Appendix 1). One well was producing at Townsend Canal field at the end of 1995 (Appendix 3). Production totaled 526,420 barrels of oil at the end of 1995 (Appendix 2). WEST FELDA FIELD West Felda field was discovered on August 2, 1966, with the drilling of the Sun Red Cattle number 21-3 well (permit 371) in Section 21, Township 45 South, Range 28 East, Hendry County. The filed now extends into Lee County (Appendix 1, Figures 1 and 22). The first production test yielded 56 barrels of 24.60 A.P.I. gravity oil and 148 barrels of saltwater per day from the -11,437 to -11,440 foot MSL interval of the Sunniland Formation. The field is mainly a stratigraphic trap; however, structural closure is more evident than at Sunoco Felda field (Figure 22). The main producing unit has a composition typical of the south Florida Sunniland trend fields (Means, 1977; Mitchell-Tapping, 1986). Means (1977) summarized the reservoir characteristics for West Felda field as follows: average pay thickness of 17 feet, average porosity of 20 percent, average water saturation of 35 percent, A.P.I. oil gravity of 260, and average daily oil production of 4,600 barrels. Values indicate improved reservoir quality over Sunoco Felda field. Means (1977) believed that the reservoir quality was improved because West Felda field "experienced higher energy and more-normal marine conditions" than did Sunoco Felda field. Alternatively, Mitchell-Tapping (1986) considered the energy levels Florida Geological Survey o.2 o g "------"- R - I- U- -" ,- \ o s5 --- --\ zo I0 O~ / N S / Z 1o < U z 3 -J Ui Z. I I-4 oz Sun ilan Formation sA s--Ji 3.. OZ 8^. 3 *j." R'y Y Q0U _ji Lz M -2 1 ^A' 0 (n7 u0 N 2 i O /3I\1Ol F 2W/.,Mfr u n Formtio /^_^ J--o^^1g- \ --7 t^ l ^^;F \\ Y- / / /" ^^ /f ^s^J N' A; kUNnoa !I H 18^ 4 AINA03 83'd 1 1103 ^ mN-o5 3-317 LZ V -? ^. 3^\ -2: 7 ?1"" 3 '- ~^ *: INZS / r 1 Figure 22. Sunoco Felda, West Felda, and Mid-Felda fields structure map, top of Sunniland Formation. Information Circular 111 topographically higher" at West Felda field. At the end of December 1995, six wells were producing at West Felda field and cumulative production totaled 43,301,266 barrels of oil (Appendices 2 and 3). MID-FELDA FIELD The Mid-Felda field discovery well was the R. L. Burns Red Cattle number 27-4 (permit 904) in Section 27, Township 45 South, Range 28 East in Hendry County, Florida (Appendix 1). The well was completed in the -11,433 to -11,437 foot MSL interval of the Sunniland Formation on October 13, 1977. An initial production test on October 24, 1977 yielded 281 barrels of 260 A.P.I. gravity oil and 53.6 barrels of saltwater per day (Appendix 1). The well is located on a small subsurface feature between West Felda field and Sunoco Felda field (Figure 22). Samples from the producing zone show a partially dolomitized fossil hash with about ten feet of oil staining. Geophysical log analysis indicated approximately 20 percent porosity for an eight-foot interval (Applegate and Lloyd, 1985). At the end of 1995, two wells were actively producing (Appendix 3). Cumulative production, as of the end of December 1995 was 1,484,994 barrels of oil (Appendix 2). SUNOCO FELDA FIELD The Sunoco Felda-field, located in Hendry and Collier Counties, was discovered in July 1964 by Sunoco, when they drilled the discovery well (Appendix 1). The well (the Sun Red Cattle number 32-1; permit 315) is located in Section 32, Township 45 South, Range 29 East. Sunoco Felda was the second commercial oil field discovered in Florida and was discovered 21 years after the first commercial discovery (Sunniland field). Forty Mile Bend field was discovered in 1954 but turned out to be non- commercial and was abandoned in 1956. The Sunoco Felda discovery well location was based on a combination of subsurface and seismic data (Tyler and Erwin, 1976). In an initial pumping test in November 1964, the discovery well produced 427 barrels of 25.40 A.P.I. gravity oil and 11 barrels of saltwater per day. Production is from the Sunniland Formation from -11,417 to -11,430 feet MSL from a leached limestone bioherm. The faunal composition of the bioherm is somewhat typical of the Sunniland reservoirs (as described in the south Florida oil fields introduction above) (Means, 1977; Mitchell-Tapping, 1986). Mitchell-Tapping (1986) observed faunal differences at Sunoco Felda field which indicated formation in "the shallow lagoonal zone of the back- reef environment." The reservoir has a permeability barrier to the northeast Florida Geological Survey "the shallow lagoonal zone of the back- reef environment." The reservoir has a permeability barrier to the northeast which prevents migration of the oil up- dip (Tyler and Erwin, 1977). Means (1977) summarized the reservoir characteristics of Sunoco Felda field. These include an average pay zone thickness of 11 feet, average porosity of 18 percent, average water saturation of 50 percent, A.P.I. oil gravity of 250, and average daily oil production of 1,700 barrels. The last reported production from Sunoco Felda field was in August, 1992 and all producing wells have been plugged and abandoned. The total production for this field was 11,528,000 barrels of oil (Appendix 2). CORKSCREW FIELD Corkscrew field was discovered on November 10, 1985 with an initial swab test of the R. K. Petroleum Rex Properties number 33-2 (permit 1170, Appendix 1). Corkscrew field is located about two and one-half miles north and slightly west of the one-well Lake Trafford field in Collier County, Florida (Figures 1 and 23). In its initial test, the discovery well produced 435 barrels of 250 A.P.I. gravity oil per day with no saltwater. Production was from open hole in the Sunniland at -11,502 to -11,520 feet MSL. Core analysis by Analytical Logging, Inc. (Ft. Myers, Florida) indicated an oil producing zone from -11,506 to -11,515 feet MSL. The zone was described as a "fossil-hash" of dolomitic limestone with an average porosity of 15.25 percent. This description, and the small closed structure drawn by LeBar (Petroleum Engineer, Florida Geological Survey, personal communication, 1996) (Figure 23), are again consistent with a bioherm formation for the reservoir. Two successful offsets have been drilled at Corkscrew field (Figure 23, permits 1199 and 1201 A) (Lloyd, 1989). In addition, permit 1243C, a reentry and sidetrack of the Permit 1224 (a dry hole), was completed as a producer in 1993, but was ultimately deemed non-commercial. Corkscrew field's total oil production as of January 1, 1996 was 966,703 barrels (Appendix 2). LAKE TRAFFORD FIELD Lake Trafford field was discovered by Mobil Oil Corporation on the Baron Collier Jr. lease in Section 9, Township 47 South, Range 28 East in Collier County (Figures 1 and 24). The discovery well (permit 401) was completed on March 30, 1969 (Appendix 1). During initial production tests the well pumped 118 barrels of 25.60 A.P.I. gravity oil and 78 barrels of saltwater per day. Production was from the Sunniland Formation from -11,830 to -11,892 feet MSL. The well was later squeeze cemented to shut off water from above the perforations. The well is unique in south Florida in that it has not produced water since that time. Information Circular 111 Figure 23. Corkscrew field structure map, top of Sunniland Formation (mapped by J. LeBar, petroleum engineer, Florida Geological Survey, 1996, personal communication). Florida Geological Survey LAKE TRAFFORD FIELD COLLIER COUNTY, FLORIDA STRUCTURE MAP TOP OF THE RUBBLE ZONE (LOWEST ZONE IN THE z z SUNNILAND FORMATION) 0 0 . -.. c- u ... 1224 U/ ,36 /> 2827 -1 28 2729 S11734 SCALE 0 1 MILE nN \- 0 I 0 1.6 KILOMETER EXPLANATION 525 PERMIT NUMBER -15250 DEPTH BELOW MSL PRODUCER DRY HOLE -N-- FGS021597 Figure 24. Lake Trafford field structure map, top of rubble zone, Sunniland Formation (lowest zone in Sunniland Formation, mapped by J. LeBar, petroleum engineer, Florida Geological Survey, 1996, personal communication). LEE COLLIER Information Circular 111 Lake Trafford field is also unique in south Florida as the only field which produces oil from a fractured limestone in the lower Sunniland Formation (Means, 1977). This producing horizon has been described as an argillaceous, burrowed, limestone "rubble." Figure 24 is a structure map on top of this "Rubble Zone" as mapped by Jim LeBar (Petroleum Engineer, Florida Geological Survey, personal communication, 1996). The combination of burrowing and fracturing was believed to be responsible for the development of producible permeability and porosity (Jim Richter, Mobil Oil Corporation, personal communication, in Applegate and Lloyd, 1985). Offsets drilled northwest and south of the discovery well were dry holes. The discovery well remains the single producing well for Lake Trafford field. The well has been periodically shut-in due to mechanical problems and has been producing only sporadically since March 1988. This well is still capable of producing substantial reserves if the mechanical problems can be solved (Jim LeBar, Petroleum Engineer, Florida Geological Survey, personal communication, 1996). The last reported production was during 1992. Total oil production for this field, as of January 1996, was 278,000 barrels (Appendix 2). SUNNILAND FIELD In September 1943, Humble Oil and Refining Company discovered Sunniland field in Collier County, Florida (Appendix 1, Figures 1 and 25). This was the first commercial oil discovered in Florida. The discovery well was the Humble Oil and Refining Company Gulf Coast Realties number 1 (permit 42) located in Section 29, Township 48 South, Range 30 East. The well was completed in an open hole interval between -11,568 and -11,592 feet MSL. Initial production was 97 barrels of 260 A.P.I. gravity oil and 425 barrels of saltwater per day by pumping. The well was drilled on a prospect outlined by magnetic, gravity, seismic, and core data. Production in the field is from various porous zones in rudistid mounds in the upper 60 feet of the formation. Mitchell-Tapping (1985) described the producing horizon as consisting of leached rudist and algal particles together with pellets and foraminifers. Mitchell-Tapping's (1985) study of Sunniland, Bear Island, and Forty Mile Bend fields concluded that the depositional environment of these fields was that of a tidal shoal with a landward (east-northeast) mud-flat area and a seaward (west-southwest) shallow-water back-reef area. The structure map (Figure 25) for the Sunniland field shows a northwest- southeast trending dome that formed as these rudistid beds grew with slowly-rising sea level during the Lower Cretaceous. The dome is about four miles long and two miles wide with closure of about 40 feet. Twenty-six producing wells and ten dry holes have been drilled at Florida Geological Survey Figure 25. Sunniland field structure map, top of Sunniland Formation. Information Circular 111 Sunniland field. After producing oil for over 50 years, increased saltwater production has forced abandonment of Sunniland field. All but two of the producing wells have been plugged and abandoned. It is unlikely that the remaining two wells (which are shut-in) will produce any additional oil (Jim LeBar, Petroleum Engineer, Florida Geological Survey, personal communication, 1996). The oil production total for Sunniland field, as of January 1996, was 18,445,000 barrels of oil (Appendix 2). SEMINOLE FIELD The discovery well for the Seminole field was the Weiner-Oleum Corporation well number 12-1 (permit 662) in Section 12, Township 48 South, Range 32 East, Hendry County (Appendix 1, Figure 1). The well was completed in the -11,379 to -11,384 foot MSL interval of the Sunniland Formation on November 14, 1973. Initial production was 26 barrels of 25.40 A.P.I. gravity oil and eight barrels of saltwater per day. This three-well oil field was abandoned in 1978 after producing a total of 85,000 barrels of oil (Appendix 2). BEAR ISLAND FIELD Bear Island field was discovered on December 5, 1972, with the completion of the Exxon Gulf Coast Realties number 2-4 well (permit 563) in Section 2, Township 49 South, Range 30 East (Appendix 1, Figures 1 and 26). The field is located about two miles southeast of Sunniland field. The discovery well pumped 132 barrels of 260 A.P.I. gravity oil and 545 barrels of saltwater per day from perforations between -11,558 and -11,564 feet MSL in Sunniland carbonates. The structure map of Bear Island field (Figure 26) indicates a northwest- southeast trending dome about 4.5 miles long and 2.5 miles wide with a closure of about 55 feet. Mitchell- Tapping (1985) found this field to have the same faunal assemblage as Sunniland field; his conclusion concerning the general depositional environment is listed above in the description of Sunniland field. Despite the generally similar origin, Mitchell- Tapping (1985) found Bear Island field to be lithologically different from Sunniland field. Most of the Sunniland Formation at Bear Island field is dolomitized and is more leached than at Sunniland field. Anhydrite and some secondary dolomitization has reduced the effective permeability in some sections. Dolomitization in the lower units of the upper Sunniland, however, enhanced both porosity and permeability (Mitchell-Tapping, 1985). A total of 25 producing wells have been drilled at Bear Island field; five of these were active at the end of 1995 (Appendix 3). Total oil production, through December 1995, was 11,318,991 barrels (Appendix 2). Florida Geological Survey Figure 26. Bear Island field structure map, base of anhydrite in Upper Sunniland Formation (after Bear Island Geological Committee, 1978). Information Circular 111 PEPPER HAMMOCK FIELD Pepper Hammock was discovered on September 28, 1978. The discovery well, the Exxon Corporation Collier Company number 23-1 well (permit 897), is located in Section 23, Township 29 South, Range 30 East, approximately one and one-half miles south of Bear Island field (Appendix 1, Figure 1). The initial production test yielded 20 barrels of 270 A.P.I. gravity oil and 206 barrels of saltwater per day. Production was from Sunniland limestones between -11,586 and -11,590 feet MSL. The discovery well is the only well at Pepper Hammock and is shut-in. A total of 323 barrels of oil were produced before the well was shut-in in October 1978 (Appendix 2). BAXTER ISLAND FIELD Baxter Island field is a one-well, abandoned field located approximately eight miles southeast of Bear Island field (Figure 1). The single producer and discovery well was the Diamond Shamrock Gerry Brothers Ltd. number 31-3 well (permit 865) located in Section 31, Township 49 South, Range 32 East, Collier County (Appendix 1). In its initial production test on August 11, 1977, the well pumped 35 barrels of 22.40 A.P.I. gravity oil and 220 barrels of saltwater per day. Production was from the Sunniland Formation from -11,482 to -11,485 feet MSL. The field produced a total of 1,859 barrels of oil before the well was shut-in in 1978 (Appendix 2). The well was plugged and abandoned on January 12, 1980. RACCOON POINT FIELD Raccoon Point field is the southeastern-most active field in the Sunniland trend (Figure 1). Its discovery well was the Exxon -Oleum Corporation number 33-4 (permit 829) drilled in Section 33, Township 51 South, Range 43 East, Collier County (Appendix 1, Figure 27). Initial production was from the -11,371 to -11,375 foot MSL interval of the Sunniland Formation. In a production test on June 20, 1978, the well pumped 57 barrels of 23.30 A.P.I. gravity oil and 845 barrels of saltwater per day. Figure '27 indicates a structure similar to other Sunniland producing fields. At the end of 1995, six wells were actively producing (Appendix 3). Oil production totaled 8,569,027 barrels at the end of December 1995 (Appendix 2). FORTY MILE BEND FIELD Commonwealth Oil Company drilled the Wiseheart State Board of Education number 1 wildcat (permit 167) in Section 16, Township 45 South, Range 35 East, Dade County. It was located 50 miles southeast of Sunniland field (Appendix 1, Figure 1). The well was completed in the -11,298 to -11,315 foot MSL interval of the Sunniland Formation and was initially Florida Geological Survey Figure 27. Raccoon Point field structure map, top of Sunniland Formation porosity (after Raccoon Point Geological Committee, 1993). Information Circular 111 tested on February 5, 1954. In this initial test, the well pumped an estimated 76 barrels of 21.30 A.P.I. gravity oil and 96 barrels of saltwater per day. Core examination (Applegate and Lloyd, 1985) in the open interval showed a partially to fully oil-saturated, finely crystalline dolostone and limestone with pin-point porosity, which did not appear to be commercial. The second well in the Forty Mile Bend field, the Gulf Oil State of Florida number 1 well (permit 182), was also completed in 1954. The well is located about three and one-quarter miles east of the discovery well (Figure 1). It was completed as a pumping well in the -11,309 to -11,316 foot MSL interval of the Sunniland Formation. Initial production was 112 barrels of 21.70 A.P.I. gravity oil per day. Water production was not tabulated. The distance between the two wells comprising Forty Mile Bend field indicate that they probably did not produce from the same reservoir. Mitchell-Tapping (1985) studied the fauna and lithology of Sunniland, Bear Island, and Forty Mile Bend fields. His description of the depositional environment for these fields is discussed above in the Sunniland field description. He found the lithology and fauna at Forty Mile Bend to be similar to that of Sunniland field, except for the presence of anhydrite in the pore space and an increase in the dolomite content. Low oil gravity and low porosity and permeability in the Sunniland at both well locations made this field non- commercial. In addition, a half-inch hole was found in the casing of the Gulf well (permit 182) at -10,027 feet MSL. This could have caused excessive water flow, and thus shortened the productive life of this well. Both of the Forty Mile Bend wells were abandoned in 1956, after producing only 32,888 barrels of oil in about 17 months in 1954 and 1955 (Appendix 2) (Gunter, 1955 and 1956). REFERENCES Applegate, A. V. and Lloyd, J. M., 1985, Summary of Florida petroleum production and exploration, onshore and offshore, through 1984: Florida Geological Survey Information Circular no. 101, 69 p. Pontigo, F. A., Jr., and Rooke, J. H., 1978, Jurassic Smackover oil prospects in the Apalachicola embayment: Oil and Gas Journal, January 23, 1978, v. 76, no. 4, p. 80-84. Winston, G. 0., and Palacas, J. G., 1981, Subdivision and regional stratigraphy of the Pre-Punta Gorda Rocks lowermostt Cretaceous-Jurassic?) in south Florida: Supplement to Transactions of the Gulf Coast Gulf Coast Association of Geological Societies, v. 31, p. 447-453. Bear Island Geological Committee, 1978, Bear Island field structure map, Exxon Corporation Sunniland oil pool report: Florida Department of Natural Resources Hearing no. 40. Blackjack Creek Geological Committee, 1974, Blackjack Creek field unit, Exhibit M-1: Florida Department of Natural Resources Hearing no. 38. Bradford, C. A., 1984, Transgressive-regressive carbonate of the Smackover Formation, Escambia County, Alabama: in Ventress, W. P. S., Bebout, D. G., Perkins, B. F., and Moore, C. H. (editors), The Jurassic of the Gulf Rim: Proceedings of the third annual research conference, Gulf Coast Section, Society of Economic Paleontologists and Mineralogists Foundation, p. 27-39. Christian, L. D., Shirer, J. A., Kimbel, E. L., and Blackwell, R. J., 1981, Planning a tertiary oil-recovery project for Jay/LEC fields unit: Journal of Petroleum Technology, v. 33, p. 1535-1544. Ferber, R., 1985, Depositional and diagenetic history of the Sunniland Formation, Lower Cretaceous, Lehigh Park field, Lee County, Florida: Master's thesis, University of Southwestern Louisiana, Lafayette, Louisiana. Gould, G. J., 1989, Gulf of Mexico Update: May 1988 July 1989, U. S. Department of the Interior Minerals Management Service: OCS Information Report, MMS 89-0079, 51 p. Information Circular 111 Gunter, H., 1955, Exploration for oil and gas in Florida, Florida Geological Survey, 1954 Supplement to Information Circular no. 1, 35 p. 1956, Exploration for oil and gas in Florida, Florida Geological Survey, 1955 Supplement to Information Circular no. 1, 31 p. Hughes Eastern Corporation, 1988, McDavid Prospect, Escambia County, Florida, Top Smackover, Geophysical Map: Florida Department of Natural Resources Hearing no. 42. Jay-LEC Fields Unit Geological Committee, 1974, Structure map-top of Smackover- Norphlet oil pool, Exhibit no. G-1: Florida Department of Natural Resources Hearing no. 36. Johnson, P. G. and Tucker, D. L., 1987, The federal Outer Continental Shelf oil and gas leasing program: a Florida perspective, February, 1987: Office of the Governor, Office of Planning and Budgeting, Intergovernmental Unit, 16 p. Karpas, R. M., and Gould, G. J., 1990, Atlantic update: July 1986 June 1990, Outer Continental Shelf oil and gas activities, U. S. Department of the Interior Minerals Management Service: OCS Information Report, MMS 90-0060, 57 p. Langston, E. P., and Shirer, J. A., 1985, Performance of the Jay-LEC field unit under mature waterflood and early tertiary operations: Journal of Petroleum Technology, v. 37, p. 261-268. Shirer, J. A., and Nelson, D. E., 1981, Innovative reservoir management key to highly successful Jay-LEC waterflood: Journal of Petroleum Technology, v. 33, p. 783-791. Lloyd, J. M., 1994, 1992 and 1993 Florida petroleum production and exploration: Florida Geological Survey Information Circular no. 110, 30 p. 1992, 1990 and 1991 Florida petroleum production and exploration: Florida Geological Survey Information Circular no. 108, 31 p. 1991, 1988 and 1989 Florida petroleum production and exploration: Florida Geological Survey Information Circular no. 107, Part I, p. 1-62. Florida Geological Survey 1989, 1986 and 1987 Florida petroleum production and exploration: Florida Geological Survey Information Circular no. 106, 39 p. 1986, Bluff Springs field discovery renews interest in Florida's western panhandle: Oil and Gas Journal, June 30, 1986, v. 84, no 3, p. 105- 108. and Applegate, A. V., 1987, 1985 Florida petroleum production and exploration: Florida Geological Survey Information Circular no. 104, Part I, p'. 1-42. and Ragland, J. M., 1991, Petroleum exploration and development policies in Florida: Response to public concern for sensitive environments: Florida Geological Survey Information Circular no. 107, Part II, p. 63-82. Ragland, P. C., Ragland, J. M., and Parker, W. C., 1986, Diagenesis of the Jurassic Smackover Formation, Jay field, Florida: Gulf Coast Association of Geological Societies Transactions, v. 36, p. 201-211. Lomando, A. J., Jr., Schreiber, C., and Nurmi, R. D., 1981, Sedimentation and diagenesis of Upper Smackover grainstone, Jay-field area, west Florida (abstract): American Association of Petroleum Geologists Bulletin, v. 65, no. 5, p. 950. Mancini, E. A., and Benson, D. J., 1980, Regional stratigraphy of Upper Jurassic Smackover carbonates of southwest Alabama: Gulf Coast Association of Geological Societies Transactions, v. 30, p. 151-165. Means, J. A., 1977, Southern Florida needs another look: The Oil and Gas Journal, v. 75, no. 5, p. 212-225. Miller, J., 1974, Mount Carmel field structure map: Florida Department of Natural Resources Hearing no. 27. Mitchell-Tapping, H., 1984, Petrology and depositional environment of the Sunniland producing fields of south Florida: Gulf Coast Association of Geological Societies Transactions, v. 34, p. 157-173. ,_ 1985, Petrology of the Sunniland, Forty Mile Bend and Bear Island fields of south Florida: Gulf Coast Association of Geological Societies Transactions, v. 35, p. 233-242. Information Circular 111 1986, Exploration petrology of the Sunoco Felda trend of south Florida: Gulf Coast Association of Geological Societies Transactions, v. 36, p. 241-256. Moore, C. H., 1984, The Upper Smackover of the Gulf Rim: depositional systems, diagenesis, porosity evolution and hydrocarbon development: in Ventress, W. P. S., Bebout, D. G., Perkins, B. F., and Moore, C. H. (editors), The Jurassic of the Gulf Rim: Proceedings of the third annual research conference, Gulf Coast Section, Society of Economic Paleontologists and Mineralogists Foundation, p. 283-307. Ottman, R. D., Keyes, P. L., and Ziegler, M. A., 1973, Jay field a Jurassic stratigraphic trap: Gulf Coast Association of Geological Societies Transactions, v. 23, p. 146-157. 1976, Jay field a Jurassic stratigraphic trap: in- Braunstein, J. (editor), North American oil and gas fields: American Association of Petroleum Geologists Memoir 24, p. 276-286. Raccoon Point Geological Committee, 1993, Structure Map Top of Sunniland Porosity, Florida Department of Environmental Protection Order No. 93-1-45: Unitization of Raccoon Point Field. Shirer, J. A., Langston, E. P., and Strong, R. B., 1978, Application of field-wide conventional coring in the Jay-Little Escambia Creek Unit: Journal of Petroleum Technology, v. 30, p. 1774-1780. Sigsby, R. J., 1976, Paleoenvironmental analysis of the Big Escambia Creek-Jay- Blackjack Creek field area: Gulf Coast Association of Geological Societies Transactions, v. 26, p. 258-278. Tyler, A. N. and Erwin, W. L., 1976, Sunoco-Felda field, Hendry and Collier Counties, Florida: in Braunstein, J. (editor), North American oil and gas fields: American Association of Petroleum Geologists Memoir 24, p. 287-299. Vinet, M. J., 1984, Geochemistry and origin of Smackover and Buckner dolomites (Upper Jurassic), Jay field area, Alabama-Florida: in Ventress, W. P. S., Bebout, D. G., Perkins, B. F., and Moore, C. H. (editors), The Jurassic of the Gulf Rim: Proceedings of the third annual research conference, Gulf Coast Florida Geological Survey Section, Society of Economic Paleontologists and Mineralogists Foundation, p. 365-374. World Oil, 1996, Crude output drops again, gas levels off: World Oil, February 1996, v. 217, no.2, p. 69. APPENDIX 1. FLORIDA OIL FIELD DISCOVERY WELL DATA PERFORATIONS DATUM FOR DEPTH OR OPEN HOLE TOTAL DEPTH DISCOVERY PERMIT MEASUREMENTS, DEPTH BELOW BELOW DATUM, PRODUCING DISCOVERY OIL GRAVITY, DATE NO. FIELD COUNTY FT. MSL 11ll DATUM, FT. FT. FORMATION STATUS DEGREES API 9-26-43 42 Sunniland Collier 34 IDF) 11,602-11,626 11,626 Sunniland Pumping 26 2-1-54 167 Forty Mile Bend Dade 24 (DF) 11.322-11,339 11,557 Sunniland Pumping. 21 7-22-64 315 Sunoco Felda Hendry 55 11,472-11,485 11,485 Sunniland Pumpingr 25 8-2-66 371 West Felda Hendry 49 11,486-11,489 11,675 Sunniland Pumping 26 3-30-69 401 Lake Trafford Collier 40 11,870-11,892 11,987 Sunniland Pumping 26 6-15-70 417 Jay Santa Rosa 206 15,470-15,524 15,984 Smackover Flowing 51 & Norphlet 12-19-71 504 Mt. Carmel Santa Rosa 274 15,260-15,280 15,399 Smackover Flowing 47 & Norphlet 2-14-72 523 Blackjack Creek Santa Rosa 157 15,790-15,900 16,235 Smackover Flowing 51 &Norphlet 12-5-72 563 Bear Island Collier 31 11,589-11,595 11,817 Sunniland Pumping 26 11-14-73 662 Seminole Hendry 36 11,415-11,420 11,651 Sunniland Pumping 25 7-30-74 712 Lehigh Park Lee 40 11,389-11,394 11,630 Sunniland Pumping 28 4-22-77 881 Sweetwater Creek Santa Rosa 255 14,299-14,340 14,611 Smackover Pumping 45 8-11-77 865 Baxter Island Collier 30 11.512-11,515 11,823 Sunniland Pumping 22 10-13-77 904 Mid-Felda Hendry 59 11,492-11,496 11,686 Sunniland Pumping 26 6-20-78 829 Raccoon Point Collier 39 11,410-11,414 11,658 Sunniland Pumping 23 9-28-78 897 Pepper Hammock Collier 43 11,629-11,633 11,897 Sunniland Pumping 27 6-27-82 1070 Townsend Canal Hendry 53 11,416-11,421 11,462 Sunniland Pumping 28 3-25-84 1125 Bluff Springs Escambia 178 16,332-16,339 16.800 Smackover Flowing 57 11-10-85 1170 Corkscrew Collier 45 11,547-11,565 11,565 Sunniland Pumping 26 2-19-86 1194 McLellan Santa Rosa 245 14,072-14,090 14,475 Smackover Flowing 41 6-4-88 1220 Coldwater Creek Santa Rosa 166 15,150-15.170 15,407 Smackover Flowing 47 6-14-88 1230 McDavid Escambia 271 16,346-16,360 16,800 Smackover Flowing 54 1. This is usually the kelly bushing elevation; where this is unavailable, drill floor IDF) elevation is given. APPENDIX 2. 1994, 1995 AND CUMULATIVE PRODUCTION DATA (1) CUMULATIVE 1994 PRODUCTION 1995 PRODUCTION PRODUCTION Oil Gas Water Oil Gas Water Oil Gas FIELD (2) (Bbis) (MCFI (BbIs) IBbIs) (MCF) (Bbls) (MBbIs) IMMCF) NORTHWEST FLORIDA Bluff Springs (3) 0 0 0 0 0 0 242 129 McDavid (3) 0 0 0 0 0 0 150 62 Jay (Fla. only) 4,159,336 7,410,410 55,199,267 3,810,967 6,230,813 61.436,742 387,816 505,234 Jay IFla.+Ala.) 4,580,107 8,043,399 60,918,577 4,076,430 6,613,768 67,047,142 Coldwater Creek 32,699 0 116,915 3,404 0 16,753 81 14 Blackjack Creek 354,722 814,154 8,505,848 301,964 738,079 8,595,142 56,805 57,325 Mt. Carmel 20,725 0 160,721 2,737 0 45,557 4,770 4,797 McLellan 24,842 7,888 35,105 17,238 4,560 39,137 352 144 Sweetwater Creek (3) 0 0 0 0 0 0 14 15 Subtotal (4) 4,592,324 8,232,452 64,017,856 4,136,3.10 6,973,452 70,133,331 450,230 567,720 SOUTH FLORIDA Lehigh Park 50,153 6,318 701,074 43,271 6,318 661,097 5,462 559 Townsend Canal 2,590 0 19,578 4,816 0 50,645 527 0 West Felda 353,456 27,934 3,125,074 357,942 28,777 3,283,230 43,301 3,383 Mid-Felda 17,074 0 49,992 10,299 0 91,870 1,485 10 Sunoco Felda (3) 0 0 0 0 0 0 11,598 982 Corkscrew 61,667 0 67,347 47,136 0 59,721 967 0 Lake Trafford 0 0 0 0 0 0 278 0 Seminole (3) 0 0 0 0 0 0 85 0 Sunniland 0 0 0 0 0 0 18,445 1,825 Bear Island 123,877 24,453 458,640 90,125 23,099 275,807 11,319 942 Pepper Hammock 0 0 0 0 0 0 0 0 Baxter Island (3) 0 0 0 0 0 0 2 0 Raccoon Point 871,897 155,747 913,951 991,719 139,911 1,892,882 8,568 1,121 Forty Mile Bend (3) 0 0 0 0 0 0 33 2 Subtotal 1,480,714 214,452 5,335,656 1,545,308 198,105 6,315,252 102,070 8,824 1. Statistics compiled by Jim LeBar, Petroleum Engineer, Florida Geological Survey, Oil and Gas Section. Abbreviations: BbIs Barrels (42 US Gallons) 2. Fields are listed in approximate order from north to south and west to east. MBbis Thousand Barrels 3. Plugged and abandoned oil fields. MCF Thousand Cubic Feet 4. Northwest Florida subtotals use Jay (FL only) data. MMCF Million Cubic Feet -n 0 Ca --, 0) 0 CO CD 0 0) V) C Information Circular 111 APPENDIX 3. 1994 AND 1995 FIELD WELL STATISTICS (1) 1994 1995 Number of Wells Number of Wells FIELD (2) PRO INJ SI TA TOTAL PRO INJ SI TA TOTAL NORTHWEST FLORIDA Jay 43 31 35 0 109 51 27 32 1 111 Coldwater Creek 1 0 0 0 1 0 0 1 0 1 Blackjack Creek 8 10 3 0 21 10 9 2 1 22 Mt. Carmel 1 0 0 0 1 0 0 1 0 1 McLellan 2 0 0 0 2 2 0 0 0 2 Subtotal 55 41 38 0 134 63 36 36 2 137 SOUTH FLORIDA Lehigh Park 1 0 0 0 1 1 0 0 0 1 Townsend Canal 1 0 3 0 4 1 0 1 0 2 West Felda 8 0 15 0 23 6 0 11 2 19 Mid-Felda 1 0 1 0 2 2 0 0 0 2 Sunoco Felda 0 0 4 0 4 0 0 0 0 0 Corkscrew -3 0 0 0 3 3 0 0 0 3 Lake Trafford 0 0 1 0 1 0 '.0 1 0 1 Sunniland 0 0 4 0 4 0 0 2 0 2 Bear Island 6 0 9 0 15 5 0 8 0 13 Pepper Hammock 0 0 1 0 1 0 0 1 0 1 Raccoon Point 5 0 7 0 12 6 0 7 0 13 Subtotal | 25 0 45 0 70 24 0 31 2 57 1. 1994 statistics compiled by Charles Tootle, Petroleum Engineer, Florida Geological Survey, Oil and Gas Section. 1995 statistics compiled by Jim LeBar, Petroleum Engineer, Florida Geological Survey, Oil and Gas Section. 2. Fields are listed in approximate order from north to south and west to east. Abbreviations: PRO Producing Wells INJ -.Injection Wells SI Shut In Wells TA Temporarily Abandoned Wells f' Florida Geological Survey APPENDIX 4. 1994 AND 1995 FIELD WELLS DRILLED Drill Floor Total FIELD Operator-Well Completion Elev., Ft. Depth County Permit No. Name & No. Location (1) Date Above MSL Ft. (2) Comments MT. CARMEL Santa Rosa P-1286 Daniels Corp.- SHL: 980' FWL & 01/29/95 273 MD: 15,370 Top of Smackover: 15,082'. Hendricks 2-1, 1680' FSL TVD: 15,350 Top of Norphlet: 15,310'. No. 2 Sec. 2, Well sidetracked, P-1 286A. T5N, R29W BHL: Not available. (3) Santa Rosa P-1286A Daniels Corp.- SHL: 980' FWL & 03/09/95 273 MD: 15,511 Top of Smackover: 15,164'. Hendricks 2-1, 1680'" FSL TVD: 15,442 Top of Norphlet: 15,418'. No. 2, ST1 Sec. 2, Dry hole, in process of T5N, R29W plugging & abandonment. BHL: 1305' FWL & 1405' FSL Sec. 2, T5N, R29W 1) Directionally drilled well; SHL is surface hole location, BHL is bottom hole location. 2) MD: measured depth, TVD: true vertical depth. 3) Directional survey to total depth not supplied by operator. Hole location at a depth of 14,754' was 1,711' FSL and 587' FWL, Sec. 2, T5N, R29W. APPENDIX 5. EXPLORATORY WELL DRILLED IN 1993, COMPLETION REPORT RECEIVED IN 1994 Drill Floor Total Operator-Well Completion Elev., Ft. Depth County Permit No. Name & No. Location Date Above MSL Ft. Comments Santa Rosa P-1285 Mack Oil Corp.- 1339' FNL & 11/07/93 186 16,600 Target: Smackover Fm. Champion 23-1 1274' FEL Top of Smackover: 16,145'. Sec. 23, Plugged & abandoned T3N, R28W as a dry hole, 11/10/93. Information Circular 111 APPENDIX 6. OIL EXPLORATION WELLS DRILLED IN STATE WATERS (1) Rotary Permit and Lease No. Table Elev. Total Geological Year Well(2) No. Operator and Area County Ft. above MSL Depth, Ft. Significance 1947 P-16 Gulf Oil State of Florida W-1413 Corp. Lease 374 No. 1 Sugarloaf Key Area 1947 P-22 Gulf Oil State of Florida W-972 Corp. Lease 373 No. 1 Big Pine Key Area 1947 P-43 Magnolia State of Florida W-1502 Petroleum Block 5-B No. 1-A Co. St. Vincent Sound 1955 P-232 Gulf Oil State of Florida W-3510C Corp. Lease 826-G No. 1 Florida Bay 1956 P-251 W-4122 HORC State of Florida Lease 833 No. 1 Pensacola Bay 1959 P-275 Gulf Oil State of Florida W-5094 Corp. Lease 826-Y No. 1 Marquesas 1959 P-280 California State of Florida W-5152 Coastal Lease 1011 No. 1 Big Pine Key Area 1959 P-281 California State of FLorida W-5103 Coastal Lease 224-A No. 1 St. George Island Area 1960 P-289 California State of Florida W-5574 Coastal Lease 224-B No. 1 Boca Grande Area 1961 P-292 California State of Florida W-5713 Coastal Lease 1011 No. 2 Marquesas 1961 P-293 California State of Florida W-5654 Coastal Lease 224-A No. 2 South of Alligator Point offshore Monroe offshore Monroe offshore Franklin offshore Monroe offshore Santa Rosa 6,100 Bottomed in Upper Cretaceous(?). 15,455 No porosity in Sunniland Fm. Well bottomed in Pumpkin Bay Fm. Very difficult to correlate this well because of anhydrite development. Structurally very low. 7,019 Bottomed in Lower Cretaceous. 12,631 Well cored from 11,661-12,544' in Sunniland Fm. and Punta Gorda Anhydrite. Encountered some salt stringers in Punta Gorda. Only 60' of dark dense calcilutite in Sunni- land Fm. 7,505 Bottomed in Lower Cretaceous. 15,478 Four drill stem tests: 12,474-1 2,533'(Lake Trafford? Fm.I 12,534-12,544'(Sunniland Fm.) 12,582-12,822'(Sunniland Fm.) 14,642-14,702'(Brown Dolomite Zn.) The 12,474-12,533' test recovered 1 5 barrels of 22 degree API gravity oil and 14.1 barrels of saltwater. Brown Dolomite from 14,650-15,036' was somewhat vuggy. This may be the principal target in this area. Net dolomite estimated at 400'. 6,030 Bottomed in Lower Cretaceous. 7,030 Bottomed in Lower Cretaceous. 14,000 Brown Dolomite: 12,485-12,589'. Estimated net dolomite: 103'. 7,722 Bottomed in Lower Cretaceous. 10,560 Did not encounter Smackover Fm. Bottomed in Eagle Mills Fm. of Triassic age. Diabase found in Eagle Mills. offshore Monroe offshore Monroe offshore Franklin offshore Lee offshore Monroe offshore Franklin 1. Modified from Applegate and Lloyd, 1985. 2. Florida Geological Survey well number for samples (cuttings or core chips). Florida Geological Survey APPENDIX 6 (cont.). OIL EXPLORATION WELLS DRILLED IN STATE WATERS (1) Rotary Permit and Lease No. Table Elev. Total Geological Year Well(2) No. Operator and Area County Ft. above MSL Depth, Ft. Significance 1961 P-297 California State of FloridA W-5785 Coastal Lease 224-B No. 2 Boca Grande Area 1962 P-298 California State of Florida W-5970 Coastal Lease 1011 No. 3 Marquesas 1963 P-304 California State of Florida W-6278 Coastal Lease 224-B No. 3 Honeymoon Island Area 1967 P-375 Mobil Oil State of Florida W-8139 Corp. Lease 224-B No. 1 Boca Grande Area 1967 P-382 Mobil Oil State of Florida W-8304 Corp. Lease 224-A No. 1-A W-SW of Crystal River offshore Lee offshore Monroe offshore Pinellas offshore Charlotte offshore 22 Citrus 1967 P-383 Mobil Oil State of Rorida offshore 25 W-8305 Corp. Lease 224-A No. 1-B Levy Cedar Key Area 1968 P-387 Mobil*Oil State of Florida offshore W-8487 Corp. Lease 224-A No. 1-C Franklin Little St. George Island Area 1983 P-1097 Getty Oil State of Florida W-15391 Company Lease 2338 No. 1 East Bay offshore Santa Rosa 12,600 There is an estimated 40' of dolo- mite in the 12,445-12,560' Brown Dolomite interval. No evidence of oil staining. Dolomite microcrys- talline to finely crystalline. Core analysis from 11,255-11,625' Sunniland interval showed no permeability, extremely low por- osity, and no oil. 12,850 Bottomed in Punta Gorda Anhydrite. No shows of oil and no porosity reported. Drill stem test of the 12.521-12,600' interval tested saltwater. Rebecca Shoals Reef (Paleocene and Upper Cretaceous) present. 10,600 Bottomed in Lower Cretaceous. Very poor samples. No oil shows. Carbonates-clastics below 7,000'. 1 2,931 This well drilled into Pumpkin Bay Fm. at 12,230'. Drilled into basement (rhyolite porphyry) at 1 2,830'. No shows in Sunniland Fm. Brown Dolomite Zone: 11,920-12,000'. Estimated net dolomite: 70'. Poor samples. 6,041 Mixed faces carbonatess, sand- stones, and shales) at 4,325'; Triassic, Eagle Mills at 5,625'; Paldozoic at 5,920'. Very indur- ated shale and siltstone. Some quartzite. Bedding planes verti- cal in this core. No shows and no porosity. 4,735 Mixed faces carbonatess, sand- stones, and shales) at 2,882' in Cretaceous. Predominantly vari- colored unconsolidated sandstone below 4,180'. Highly indurated quartzites and interbedded shales in core (Paleozoic) from 4,720- 4,735'. 14,369 This well encountered Jurassic limestone. First indication of possible Smackover Fm. in Apa- lachicola area. 18,011 Smackover tests at 17,405-17,411' and 17,328-17,411' produced only saltwater. Norphlet Ss. and Louann/ Werner evaporites were very thin. 1. Modified from Applegate and Lloyd, 1985. 2. Florida Geological Survey well number for samples (cuttings or core chips). APPENDIX 7. 1994 AND 1995 GEOPHYSICAL EXPLORATION ACTIVITY GEOPHYSICAL PERMIT EXPIRATION ENERGY SURVEY LENGTH, MI PERMIT COMPANY COUNTY APPROVED DATE STATUS SOURCE APPROVED SURVEYED G-152-93 Universal Seismic Santa Rosa 03-Mar-94 03-Mar-95 Completed Seismic 22.5 22.5 Acquisition Inc. Explosives G-153-93 Triton Energy Highlands 23-Nov-93 23-Nov-94 Completed Gravity 102.0 102.0 Company G-154-95 Calumet Florida Lee, Hendry, 24-Mar-95 23-Mar-96 In Progress Seismic 52.4 20.3 Inc. & Collier Explosives G-155-95 Coastal Offshore Application Airgun and Dense grid: Apalachicola to Naples. Petroleum Pending Gravity/Magnetic Mileage not given in application. Total Miles in Applications: 176.9 144.8 Survey Miles by Area: North Florida: 22.5 22.5 South Florida: 154.4 122.3 APPENDIX 8. FLORIDA OIL AND GAS RESERVE ESTIMATES (1) ORIGINAL OIL REMAINING ORIGINAL GAS REMAINING AVERAGE ORIGINAL ESTIMATE RECOVER- PRODUCED RECOVERABLE RECOVER- PRODUCED RECOVERABLE OIL AVERAGE PRODUC- GAS-OIL OIL IN RECOVERY ABLE OIL THROUGH OIL RESERVES ABLE GAS THROUGH GAS RESERVES GRAVITY, POROSITY, TIVE RATIO, PLACE, FACTOR, IN PLACE, 1-1-96, AS OF 1-1-96, IN PLACE, 1-1-96, AS OF 1.1-96, FIELD (21) A.P.I. PERCENT ACRES SCF/STB BARRELS FRACTION BARRELS BARRELS BARRELS MCF MCF MCF NORTHWEST FLORIDA Bluff Springs (3) 53 19.6 160.00 550 1,300,440 0.19 247,084 241,871 5,213 135,795 128,565 7,230 McDavid (3) 53 12.8 160.00 400 4,987,347 0.10 498,736 150,323 348,413 199,494 61,859 137,635 Jay (FL & AL) 51 14.0 14,414.50 1,277 820,569,503 0.60 492,341,702 419,824,453 72,517,249 628,720,354 547,251,409 81,468,945 Jay (FL only) 51 14.0 13,021.14 1,277 763,129,638 0.60 457,877,783 367,815,585 70,062,198 584,709,929 505,234,204 79,475,725 Coldwater Creek 47 12.1 160.00 500 2,080,107 0.15 312;016 80,068 231,948 156,008 14,012 141,996 Blackjack Creek 48 16.5 5,719.98 954 100,500,000 0.60 60,300,000 56,805,223 3,494,777 57,526,200 57,324,872 201,328 Mt. Carmel 43 9.1 481.28 1,028 17,500,000 0.29 5,075,000 4,770,745 304,255 5,218,140 4,797,292 420,848 McLellan 43 9.0 480.00 430 2,915,540 0.14 412,686 351,617 61,069 177,455 143,494 33,961 Sweetwater Creek (3) 44 11.0 160.00 1,070 624,000 0.10 62,400 13,695 48,705 66,768 14,655 52,113 Subtotal (4) 20,342.40 893,037,072 524,785,705 450,229,127 74,556,578 648,189,789 567,718,953 80,470,836 M SOUTH FLORIDA . Lehigh Park 28 17.7 800.00 100 8,211,707 0.68 5,583,961 5,462,076 121,885 558,396 558,161 235 0C Townsend Canal 28 13.7 640.00 0 4,504,699 0.20 900,940 526,420 374,520 0 0 0 0) West Felda 26 15.0 7,500.00 80 125,802,366 0.35 44,030,828 43,301,266 729,562 3,522,466 3,383,330 139,136 CD Mid-Felda 26 11.9 480.00 10 5,090,419 0.30 1,527,126 1,484,994 42,132 12,726 10,094 2,632 0 0, Sunoco Felda (3) 25 15.0 3,840.00 85 28,946,578 0.40 11,608.631 11,598,196 10,435 984,184 981,827 2,357 0 Corkscrew 26 6.9 480.00 0 1,667.806 0.65 1,084,074 966,703 117,371 0 0 0 . Lake Trafford 26 7.9 160.00 0 7,690,293 0.04 307,612 278,241 29,371 0 0 0 Seminole (3) 25 14.1 480.00 0 2,366,565 0.10 236,657 84,755 151,902 0 0 0 Sunniland 26 15.0 2,080.00 100 37,685,118 0.50 18,842,559 18,445,245 397,314 1,884,256 1,824,628 59,628 c- Bear Island 26 11.9 2,880.00 60 42,811,959 0.35 14,964,184 11,318,991 3,665,193 1,198,735 941,112 257,623 Pepper Hammock 27 15.3 160.00 0 976,713 0.10 97,671 323 97,348 0 0 0 QB Baxter Island (3) 22 19.6 160.00 0 1,276,617 0.10 127,662 1,859 125,803 0 0 0 Raccoon Point 23 13.9 2,400.00 120 42,437,790 0.25 10,609,448 8,569,027 2,040,421 1,273,134 1,121,170 151,964 Forty Mile Bend (3) 21 10.0 320.00 50 1,112,701 0.07 77,889 32,888 45,001 3,894 1,656 2,238 Subtotal 22,380.00 310,581,331 110,019,242 102,070,984 7,948,258 9,437,791 8,821,978 615,813 1. Updated from estimates by Charles H. Tootle in Uoyd, 1994. See Uoyd, 1994 for explanation of methods used to determine reserve estimates. ABBREVIATIONS: MCF Thousand Cubic Feet 2. Fields are listed In approximate order from northwest to southeast. SCF Standard Cubic Feet 3 Plugged and abandoned oil fields. STB Stock Tank Barrels 4. Northwest Florida subtotals use Jay (FL only) data. DISCLAIMER: An attempt was made to present realistic estimates; however, no guarantee or warranty is expressed or implied. Anyone who uses this information does so at their own risk. FLORIDA GEOLOGICAL SURVEY 903 W. TENNESSEE STREET TALLAHASSEE, FLORIDA 32304-7700 ADMINISTRATIVE SECTION Walter Schmidt, Chief and State Geologist Cindy Collier, Administrative Secretary Jessie Hawkins, Custodian Deborah Mekeel, Librarian Sandie Ray, Admin. Asst. GEOLOGICAL INVESTIGATIONS SECTION Thomas M. Scott, Assistant State Geologist Jon Arthur, Petrologist Lance Johnson, Research Assistant Martin Balinsky, Research Assistant Ted Kiper, Cartographer Jim Balsillie, Coastal Geologist Li Li, Research Assistant Clint Barineau, Research Assistant Harley Means, Research Assistant Paulette Bond, Geochemist Tom Miller, Research Assistant Jennifer Branch, Staff Assistant LaMarr Mitchell, Secretary Specialist Ken Campbell, Sedimentologist Spencer Mitchell, Research Assistant Joel Duncan, Sedimentary Petrologist Stephen Palmes, Research Assistant Rick Green, Senior Research Assistant Frank Rupert, Paleontologist Mark Groszos, Research Assistant Frank Rush, Lab Technician Alex Howell, Research Assistant Jim Trindell, Driller Dennis Jensen, Research Assistant Rodger VanLandingham, Asst. Driller Jim Jones, Cartographer Bill Waite, Research Assistant MINERAL RESOURCE INVESTIGATIONS AND ENVIRONMENTAL GEOLOGY SECTION Jacqueline M. Lloyd, Assistant State Geologist Zi-Quiag Chen, Research Assistant Ron Hoenstine, Env. Geologist Adel Dabous, Research Assistant Suvrat Kher, Research Assistant Rodney DeHan, Sr. Research Scientist Jim Ladner, Environmental Geologist Joe Donoghue, Research Associate Ed Lane, Environmental Geologist Henry Freedenberg, Env. Geologist Steve Spencer, Economic Geologist Cliff Hendrickson, Research Assistant Nikki Strong, Research Assistant Deborah Harrington, Research Assistant Candy Trimble, Research Assistant Holly Williams, Research Assistant OIL AND GAS SECTION L. David Curry, Environmental Program Administrator Paul Attwood, Asst. Dist. Coordinator Don Hargrove, Engineer Robert Caughey, District Coordinator Evelyn Jordan, Sec. Spec. Ed Gambrell, District Coordinator Jim LeBar, Professional Engineer Ed Garrett, Geologist Victoria MacFarlan, Sec. Spec. Carolyn Stringer, Secrerary Specialist |
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| MILLISECOND | CLASS.METHOD | MESSAGE |
|---|---|---|
| 0 | sobekcm_page_globals.constructor | |
| 0 | sobekcm_page_globals.constructor | Application State validated or built |
| 0 | sobekcm_database.verify_item_lookup_object | |
| 0 | sobekcm_page_globals.constructor | Navigation Object created from URI query string |
| 0 | sobekcm_database.verify_item_lookup_object | |
| 0 | sobekcm_page_globals.display_item | Retrieving item or group information |
| 0 | sobekcm_page_globals.get_entire_collection_hierarchy | Retrieving hierarchy information |
| 0 | sobekcm_assistant.get_entire_collection_hierarchy | |
| 0 | cached_data_manager.retrieve_item_aggregation | |
| 0 | cached_data_manager.retrieve_item_aggregation | Found item aggregation on local cache |
| 0 | item_aggregation_builder.get_item_aggregation | Found 'all' item aggregation in cache |
| 0 | system.web.ui.page.page_load (ufdc.page_load) | |
| 0 | sobekcm_page_globals.constructor.on_page_load | |
| 0 | html_echo_mainwriter.add_style_references | Adding style references to HTML |
| 0 | html_echo_mainwriter.add_text_to_page | Reading the text from the file and echoing back to the output stream |
| 34 | html_echo_mainwriter.add_text_to_page | Finished reading and writing the file |