Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
1.6 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
35 |
Pre-Sample Comments: SAND AND SHELL DRILLPAD. This depth comment: CONTAINS ROOTLETS AND ORGANICS. VARIABLY IRON-STAINED. |
1.6 |
2 |
SAND (QUARTZ) |
|
WHITE |
UNCONSOLIDATED |
40 |
VERY CLEAN, MODERATELY WELL-SORTED QUARTZ SAND. WATER TABLE AT 2FT. BLS. |
2 |
4 |
NO SAMPLE |
|
|
|
|
WET SAND, DROPPED OUT OF AUGERS. |
4 |
11.4 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
30 |
BED AT 10.8 - 11.4 CONTAINS 6-8% IRON AND IS SLIGHTLY CEMENTED. |
11.4 |
14 |
SAND (QUARTZ) |
|
MODERATE BROWN |
UNCONSOLIDATED |
35 |
|
14 |
17 |
SAND (QUARTZ) |
|
DUSKY BROWN |
POOR |
35 |
|
17 |
25 |
SAND (QUARTZ) |
|
MODERATE BROWN |
UNCONSOLIDATED |
40 |
|
25 |
30 |
SAND (QUARTZ) |
|
DUSKY BROWN |
UNCONSOLIDATED |
40 |
ALTHOUGH GENERALLY IRON-STAINED, UNIT CONTAINS 10-15% COARSE, ROUNDED, UNSTAINED QUARTZ SAND. |
30 |
35 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
|
LIKELY CONTAINS INTERBEDDED MEDIUM-COARSE ROUNDED QUARTZ SAND AND SLIGHTLY IRON-CEMENTED VERY FINE TO MEDIUM QUARTZ SAND. |
35 |
37 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
45 |
GENERALLY CLEAR QUARTZ SAND WITH INTERBEDS OF IRON-CEMENTED VERY FINE QUARTZ SAND. |
37 |
40 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
|
40 |
AUGER BLADE SAMPLE FROM 39 FT. CONTAINED 10% WHITE SILT (NONCALCAREOUS). CONTAINS SOME IRON-CEMENTED GRAINS. |
40 |
45 |
SAND (QUARTZ) |
|
LIGHT GRAY |
UNCONSOLIDATED |
40 |
CLEAN WELL-SORTED SAND WITH (REWORKED?) CRAB SHELL FRAGMENT, SHARK TOOTH AND OPERCULUM. TRACE ROUNDED LIMESTONE FRAGMENTS. BASE OF UNDIFFERENTIATED SURFICIAL DEPOSITS. |
45 |
47 |
SAND (QUARTZ) |
|
LIGHT GRAY |
UNCONSOLIDATED |
40 |
CONTAINS INCREASED PERCENT OF ROUNDED LIMESTONE FRAGMENTS AND A SMALL PERCENT OF LEACHED ROUNDED PHOSPHATIC SAND. TOP OF HAWTHORN DEPOSITS. |
47 |
51 |
SAND (QUARTZ) |
|
MODERATE GRAY |
UNCONSOLIDATED |
45 |
QUARTZ SAND WITH SUBSTANTIAL PERCENT OF WORN LIMESTONE FRAGMENTS AND INTERBEDDED CALCILUTITE. PHOSPHATE IS BOTH LEACHED AND UNLEACHED. |
51 |
55 |
SAND (QUARTZ) |
|
DARK GRAY |
UNCONSOLIDATED |
45 |
COARSE, WELL-ROUNDED PHOSPHATE-RICH QUARTZ SAND. CALCILUTITE TRACES MAY PROVIDE SLIGHT INSITU CEMENTING OF UNIT. BOTTOM OF SURFICIAL AQUIFER SYSTEM. |
55 |
60 |
MICRITE |
|
DARK GRAY |
POOR |
18 |
UPPERMOST CARBONATE. RICH IN ROUNDED QUARTZ, PHOSPHATIC SANDS. TOP OF INTERMEDIATE AQUIFER SYSTEM. |
60 |
65 |
PHOSPHATE |
|
DARK GRAY |
POOR |
|
A CONCENTRATION OF ROUNDED PHOSPHATE GRANULES (4MM) WITH LESSER CALCILUTITE MATRIX. |
65 |
70 |
MICRITE |
|
MODERATE DARK GRAY |
POOR |
14 |
CLAYEY CALCILUTITE WITH MUCH PHOSPHATIC SAND. |
70 |
77 |
MICRITE |
|
OLIVE GRAY |
POOR |
|
VERY CLAYEY CALCILUTITE. CLAY IS DISSEMINATED AND AS STREAKS. |
77 |
82 |
CLAY |
|
LIGHT OLIVE GRAY |
MODERATE |
|
VARIABLY CALCAREOUS CLAY CONTAINING SAND STRINGERS AND BURROW FILL. |
82 |
85 |
MICRITE |
|
LIGHT OLIVE GRAY |
MODERATE |
16 |
|
85 |
91 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
UNIT GRADES SOFTER WITH DEPTH. VARIABLY PHOSPHATIC. CLAY IS IN STREAKS, BLEBS, AND DISSEMINATED. A FEW 1-2 CM PHOSPHATE CLASTS. CONTAINS HARDER ALTERED OR DOLOMITIC INCLUSIONS. |
91 |
93 |
MICRITE |
|
PALE OLIVE |
POOR |
|
SOFT VERY CLAYEY PHOSPHATIC CALCILUTITE. |
93 |
96.5 |
NO SAMPLE |
|
|
|
|
PROBABLY PHOSPHATIC AND QUARTZ SAND (POORLY CONSOLIDATED). |
96.5 |
101.3 |
CLAY |
|
DARK GREENISH GRAY |
MODERATE |
|
UPPER 1-5 FT. CONTAINS THIN INTERBEDS OF SOMEWHAT CALCAREOUS PHOSPHATIC SANDY OLIVE CLAY. 98 - 101.3 FT IS PURE DARK GREEN CLAY. |
101.3 |
103 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
VERY CLAYEY PHOSPHATIC CALCILUTITE. CLAY IS DISSEMINATED IN MATRIX AND ALSO AS INFILL AROUND ROUNDED CLASTS OF PHOSPHATIC CALCILUTITE. |
103 |
107 |
MICRITE |
|
YELLOWISH GRAY |
POOR |
12 |
SEMI-SOFT PHOSPHATIC CLAYEY CALCILUTITE WITH MINOR LIMESTONE STRINGERS AND BIVALVE CASTS. A RESIDUUM? UNIT RUBBELIZED ON CORING. BOTTOM OF PEACE RIVER FORMATION. |
107 |
113.2 |
MICRITE |
|
VERY LIGHT GRAY |
MODERATE |
16 |
TOP OF A VERTICALLY PERSISTENT LIMESTONE SECTION WITH LOWER PERCENT OF CLAY. TOP 1 FT. OF UNIT SHOWS INFILL OF QUARTZ AND PHOSPHATIC SAND (IN DESICCATION CRACKS?). THIN, MUDDY LENSES 108 - 110 FT. MORE VERY FINE PHOSPHATE 111 - 113 FT. AND SMALL MOLDS 111 - 113 FT. |
113.2 |
115 |
MICRITE |
|
LIGHT GRAY |
MODERATE |
18 |
VARIEGATED DARK AND LIGHT GRAY. DARKER SECTIONS ARE HARDER AND MAY BE DOLOMITIC. STARFISH ARM MOLD AT 113.9 FT. |
115 |
115.5 |
CHERT |
|
MODERATE DARK GRAY |
GOOD |
|
|
115.5 |
118 |
MICRITE |
|
VERY LIGHT GRAY |
MODERATE |
14 |
CONTAINS SOFT CLAYEY STREAKS AND INFILLED BURROWS. |
118 |
123.1 |
CALCARENITE |
|
YELLOWISH GRAY |
GOOD |
16 |
|
123.1 |
125.5 |
MICRITE |
|
LIGHT GRAY |
GOOD |
8 |
VERY HARD, FEATURELESS. DOLOMITIC? |
125.5 |
128.5 |
MICRITE |
|
MODERATE LIGHT GRAY |
MODERATE |
14 |
|
128.5 |
133.2 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
16 |
|
133.2 |
138.2 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
CLAYEY CALCILUTITE IRREGULARLY BEDDED WITH OR INFILLED AROUND QUARTZ - PHOSPHATIC SANDY CALCILUTITE. |
138.2 |
143 |
MICRITE |
|
LIGHT OLIVE GRAY |
POOR |
10 |
CONTAINS SOME SOFTER BEDS. |
143 |
160 |
MICRITE |
|
LIGHT OLIVE GRAY |
MODERATE |
12 |
UNIT BECOMES SLIGHTLY LESS CALCAREOUS AND MORE CLAYEY AND QUARTZ SANDY BELOW 150 FT. CHERT INCLUSION AT 151.8 FT. |
160 |
163 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
10 |
IRREGULARLY BEDDED OR INFILLED OLIVE CLAY AND CLAYEY QUARTZ-PHOSPHATE SANDY CALCILUTITE. RUBBLY. |
163 |
168.2 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
12 |
DISSEMINATED AND INTERBEDDED CLAY FACTION. CHERT AS INCLUSIONS AT 163 FT. AND 164.5 FT. |
168.2 |
175.5 |
CLAY |
|
LIGHT OLIVE GRAY |
MODERATE |
|
A CLEAN WAXY OLIVE CLAY CONTAINING SOME VEINLETS OF VERY FINE ORGANIC SAND OR DARK MINERAL. |
175.5 |
188 |
MICRITE |
|
LIGHT OLIVE GRAY |
MODERATE |
15 |
CLAY IS DISSEMINATED AND AS INFILL. CHERT INCLUSION AT 181 FT. DOLOMITIC LENSES AT 184 FT., 185 FT. |
188 |
191 |
SANDSTONE |
|
LIGHT OLIVE GRAY |
POOR |
10 |
QUARTZ SANDSTONE, ABUNDANT PHOSPHATIC SAND AND GRAVEL. NUMEROUS CALCAREOUS AND PHOSPHATIC FOSSILS, SHELLS AND TEETH IN CALCAREOUS CLAY MATRIX. |
191 |
193 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
5 |
|
193 |
194.3 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
MODERATE |
3 |
DOLOSTONE, LITTLE QUARTZ. PHOSPHATIC SAND. FEWER FOSSILS. |
194.3 |
198.2 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
MODERATE |
3 |
|
198.2 |
199.5 |
DOLOMITE |
|
YELLOWISH GRAY |
POOR |
2 |
|
199.5 |
204.7 |
CLAY |
|
LIGHT OLIVE GRAY |
MODERATE |
1 |
CLAY WITH INTERBEDDED FORAM FRAGMENTS, SOME INTERBEDDED DOLOSTONE AND SOME QUARTZ AND PHOSPHATIC SAND. |
204.7 |
210.8 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
2 |
|
210.8 |
217 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
GOOD |
2 |
|
217 |
218 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
2 |
CLAY, DOLOMITIC, ABUNDANT PHOSPHATIC GRAVEL. |
218 |
233 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
5 |
|
233 |
233.9 |
CLAY |
|
YELLOWISH GRAY |
MODERATE |
2 |
|
233.9 |
234.6 |
CLAY |
|
YELLOWISH GRAY |
POOR |
2 |
|
234.6 |
238 |
CLAY |
|
YELLOWISH GRAY |
POOR |
2 |
|
238 |
246.9 |
CLAY |
|
YELLOWISH GRAY |
POOR |
1 |
|
246.9 |
248.4 |
CLAY |
|
YELLOWISH GRAY |
POOR |
1 |
CLAY, CALCAREOUS, PHOSPHATIC SAND AND GRAVEL. SOME QUARTZ SAND. MOLLUSK FRAGMENTS ARE CALCAREOUS. |
248.4 |
263 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
1 |
|
263 |
267.8 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
CALCARENITE, SOFT, FOSSILIFEROUS (SORITES-FORAM), INTERBEDDED CLAY, PHOSPHATIC SAND AND GRAVEL, MINOR QUARTZ SAND. |
267.8 |
269 |
CLAY |
|
YELLOWISH GRAY |
POOR |
2 |
|
269 |
270.1 |
DOLOMITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
DOLOSTONE, FRACTURES, SOME CLAY INFILLED, INTERBEDDED PHOSPHATIC SAND AND GRAVEL, MOLDIC. |
270.1 |
278 |
CALCARENITE |
|
YELLOWISH GRAY |
POOR |
8 |
|
278 |
280 |
MICRITE |
|
WHITE |
MODERATE |
5 |
|
280 |
283.4 |
CLAY |
|
DARK GREENISH GRAY |
POOR |
2 |
CLAY, GREEN, INTERBEDDED. |
283.4 |
284.3 |
CALCARENITE |
|
WHITE |
MODERATE |
5 |
|
284.3 |
292.8 |
CALCARENITE |
|
WHITE |
MODERATE |
5 |
|
292.8 |
294.1 |
CLAY |
|
WHITE |
POOR |
1 |
|
294.1 |
296.8 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
3 |
|
296.8 |
298 |
CALCARENITE |
|
GRAYISH BROWN |
POOR |
4 |
CALCARENITE, SANDY, VERY WEATHERED MOLLUSK FRAGMENTS. |
298 |
298.8 |
CLAY |
|
OLIVE GRAY |
POOR |
1 |
|
298.8 |
303.8 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
3 |
|
303.8 |
308.8 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
1 |
CALCILUTITE, VERY HARD, NUMEROUS FILLED IN MOLDS-SOME CALCITE REPLACED. SOME ORGANICS. |
308.8 |
313 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
|
313 |
333 |
CALCARENITE |
|
|
POOR |
10 |
CALCARENITE, VERY CLEAN, VERY MINOR ORGANICS, POORLY INDURATED SUWANNEE LIMESTONE. |
333 |
341 |
CALCARENITE |
|
|
MODERATE |
10 |
CALCARENITE, CREAM-COLORED, VERY CLEAN, FEW INTERBEDDED MINERALS, TYPICAL SUWANNEE LIMESTONE CORE. |
341 |
348.6 |
MICRITE |
|
|
UNCONSOLIDATED |
3 |
|
348.6 |
353 |
MICRITE |
|
|
MODERATE |
3 |
|
353 |
373.3 |
CALCARENITE |
|
|
MODERATE |
3 |
|
373.3 |
377 |
CALCARENITE |
|
|
MODERATE |
10 |
|
377 |
382.5 |
MICRITE |
|
|
MODERATE |
3 |
|
382.5 |
390.5 |
CALCARENITE |
|
|
MODERATE |
5 |
CALCARENITE, FRACTURED, RUBBLE. SOME INTERBEDDED GREEN CLAY. |
390.5 |
402.1 |
CALCARENITE |
|
|
MODERATE |
10 |
CALCARENITE, MOLDIC, NUMEROUS MOLLUSK MOLDS. APPEARS VERY PERMEABLE. |
402.1 |
403 |
MICRITE |
|
|
UNCONSOLIDATED |
2 |
|
403 |
405 |
CLAY |
|
|
POOR |
1 |
|
405 |
413 |
MICRITE |
|
|
POOR |
3 |
CALCILUTITE, RUBBLE. LARGE DOLOMITIC CHERT NODULE AT 412 FT. |
413 |
418 |
CLAY |
|
|
UNCONSOLIDATED |
1 |
|
418 |
419 |
CALCARENITE |
|
|
POOR |
5 |
|
419 |
422.6 |
CLAY |
|
|
MODERATE |
2 |
|
422.6 |
429 |
CALCARENITE |
|
|
POOR |
5 |
|
429 |
433 |
CLAY |
|
|
POOR |
2 |
|
433 |
438.5 |
CALCARENITE |
|
|
POOR |
10 |
CALCARENITE, MOLDIC, INTERBEDDED CLAY LENSES. SOME DOLOSTONE. |
438.5 |
478.1 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
15 |
CALCARENITE, MOLDIC, HIGHLY PERMEABLE, POSSIBLE FAULT SURFACE AT 447.5 FT. |
478.1 |
482.6 |
CLAY |
|
WHITE |
UNCONSOLIDATED |
2 |
|
482.6 |
489 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
10 |
|
489 |
493 |
CLAY |
|
WHITE |
UNCONSOLIDATED |
2 |
|
493 |
518.6 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
10 |
CALCARENITE, FOSSILIFEROUS, MOLDIC. SOME UNCONSOLIDATED CALCAREOUS CLAY LENSES. |
518.6 |
523.6 |
CLAY |
|
WHITE |
UNCONSOLIDATED |
1 |
|
523.6 |
535 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
5 |
|
535 |
568 |
CLAY |
|
WHITE |
UNCONSOLIDATED |
2 |
CLAY, CALCAREOUS, INTERLAYERED WITH CALCARENITE LENSES. |
568 |
576 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
CALCARENITE, INCREASING ORGANICS CONTENT, INTERBEDDED GRAY CLAY LENSES. VERY WEATHERED. |
576 |
593 |
CLAY |
|
LIGHT GRAY |
POOR |
1 |
|
593 |
620.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
CALCARENITE, FOSSILIFEROUS, VERY WEATHERED, INTERLAYERED WITH CALCAREOUS CLAY ZONES. |
620.5 |
623 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
623 |
639 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
6 |
INTERBEDDED GRANULAR VERY FINE CALCARENITE AND POORLY INDURATED GRAINY CALCILUTITE. MAY DISPLAY FINING-UPWARD SEQUENCES. ORGANIC SPECKS AND ALTERED CALCARENITE GRAINS ARE COMMON. |
639 |
640 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
24 |
|
640 |
644.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
16 |
GRANULAR VERY FINE CALCARENITE, FAINTLY CROSS-BEDDED WITH SLIGHTLY ALTERED LAMINAE. ORGANIC SPECKS COMMON. |
644.5 |
662 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
22 |
INTERBEDDED FINE SKELETAL/GRANULAR PACKSTONE AND POORLY CONSOLIDATED GRAINY CALCILUTITE. HARD, THIN CALCILUTITE STRINGERS AT 659 FT. VARIABLY PERMEABLE. |
662 |
668.5 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
VARIABLY HARD, VARIABLY MOLDIC. |
668.5 |
674.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
VERY FINE CALCARENITE. |
674.5 |
678 |
MICRITE |
|
WHITE |
POOR |
12 |
CHALKY, POOR TO MODERATELY INDURATED. (OCALA TYPE?) |
678 |
683 |
NO SAMPLE |
|
|
|
|
CUTTINGS COLLECTED THROUGH INTERVAL SUGGEST POORLY INDURATED VERY FINE CALCARENITE, BUT MAY CONSIST OF PREVIOUS CHALKY CALCILUTITE. |
683 |
686 |
SHELL |
|
LIGHT GRAY |
POOR |
40 |
PERMEABLE BED OF RECRYSTALLIZED OYSTER SHELL WITH INTERBEDS OF POORLY PERMEABLE, WHITE, POOR TO MEDIUM INDURATED CALCILUTITE. (OCALA TYPE?). |
686 |
687 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
MOLLUSK MOLDS AND CASTS IN HARD SOMEWHAT RECRYSTALLIZED LIMESTONE. SOME RECRYSTALLIZED OYSTER SHELLS. SUWANNEE-TYPE LITHOLOGY. |
687 |
708.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
OCALA TYPE LITHOLOGY ALTHOUGH TRACES OF MOLLUSK MOLDS. VERY FEW LEPIDOCYCLINA NEAR BOTTOM OF INTERVAL. |
708.5 |
713.8 |
CALCARENITE |
|
VERY PALE ORANGE |
POOR |
10 |
|
713.8 |
717.9 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
10 |
|
717.9 |
743 |
CALCARENITE |
|
VERY PALE ORANGE |
POOR |
10 |
VERY WEATHERED LEPIDOCYCLINA FRAGMENTS. ALSO MOLLUSK MOLDS. |
743 |
748 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
5 |
VERY FINE-GRAINED, NEARLY WHITE IN COLOR. VERY WEATHERED. |
748 |
754 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
10 |
|
754 |
783 |
CALCARENITE |
|
VERY PALE ORANGE |
POOR |
5 |
VERY FINE-GRAINED NUMEROUS FORAMS. VERY WEATHERED. |
783 |
788 |
SILT |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
20 |
|
788 |
793.5 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
3 |
|
793.5 |
832 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
VERY FINE CALCARENITE WITH MUCH CALCILUTITE MATRIX. VARIABLE CONCENTRATION OF NUMMULITES AND LEPIDOCYCLINA CRYSTALLINE SKELETONS (10-30% OF UNIT). |
832 |
834 |
MICRITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
THIN BED CONTAINS MINOR CLAY FRACTION. TIGHT. FEWER NUMMULITES AND LEPIDOYCLINA. |
834 |
852 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
SIMILAR TO INTERVAL NEAR 832. 10-30% NUMMULITES AND LEPIDOCYCLINA SKELETONS (CRYSTALLINE). |
852 |
855.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
10 |
SOME FAINT BANDING. CRYSTALLINE NUMMULITES AND LEPIDOCYCLINA SKELETONS. A FEW GRAY DOLOMITIC(?) SKELETONS INCORPORATING ORGANIC SPECKS. |
855.5 |
863.5 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
14 |
GENERALLY 15-25% SKELETAL FRAGMENTS (NUMMULITES AND LEPIDOCYCLINA). TRACES OF IRREGULAR GRAY BANDING IN MATRIX. |
863.5 |
878 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
16 |
SIMILAR TO PREVIOUS INTERVAL BUT CONTAINS 2% ALTERED (DOLOMITIC?) SKELETAL FRAGMENTS. ALTERED FRAGMENTS OFTEN CONTAIN ORGANIC SPECKS. |
878 |
883 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
12 |
UNIT CONTAINS LESS FORAMS. FAINT GRAY BANDING MAY INDICATE MINOR DOLOMITIZATION. |
883 |
901 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
16 |
CONTAINS CRYSTALLINE FORAM TESTS (LEPIDOCYCLINA AND NUMMULITES) IN CONCENTRATIONS OF 20-35%. APPROXIMATELY 1-2% OF FORAMS ARE ALTERED TO GRAY COLORED. |
901 |
908 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
12 |
FORAM SKELETONS ARE CHALKIER AND COMPOSE APPROXIMATELY 10-20% OF UNIT. MOSTLY LEPIDOCYCLINA. ROCK MATRIX DARKENS SLIGHTLY. |
908 |
928 |
CALCARENITE |
|
YELLOWISH GRAY |
MODERATE |
5 |
VERY LARGE FORAMS, LEPIDOCYCLINA COMPRISING 25% OF MATRIX. |
928 |
932.5 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
5 |
FEWER LARGE FORAMS, MATRIX GRAINS FINER, BECOMING OOLOMITIC. |
932.5 |
934 |
LIMESTONE |
|
YELLOWISH GRAY |
GOOD |
3 |
SLIGHTLY LARGER GRAIN SIZE, NUMMULITES INCREASING, DARKER. |
934 |
939.5 |
DOLOMITE |
|
YELLOWISH GRAY |
POOR |
5 |
|
939.5 |
941.2 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
3 |
|
941.2 |
944 |
MICRITE |
|
YELLOWISH GRAY |
POOR |
3 |
|
944 |
949 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
3 |
|
949 |
959 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
3 |
CALCILUTITE, VERY FINE-GRAINED, DOLOMITIC, NUMEROUS NUMMULITES, FEWER LEPIDOCYCLINA. |
959 |
965.5 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
GOOD |
15 |
DOLOSTONE, CRYSTALLINE, NUMEROUS MOLDS. APPEARS HIGHLY PERMEABLE. |
965.5 |
966 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
5 |
|
966 |
968 |
CLAY |
|
WHITE |
UNCONSOLIDATED |
3 |
CALCAREOUS CLAY, UNCONSOLIDATED. |
968 |
969.5 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
3 |
DOLOSTONE, HARD LENS, GRADES INTO A CALCAREOUS CLAY. |
969.5 |
970 |
CLAY |
|
YELLOWISH GRAY |
POOR |
2 |
|
970 |
974 |
CALCARENITE |
|
VERY PALE ORANGE |
POOR |
15 |
|
974 |
976 |
CLAY |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
2 |
|
976 |
981.4 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
GOOD |
20 |
DOLOMITE, CRYSTALLINE NUMEROUS ECHINOID MOLDS, CASTS AND FRAGMENTS. TOP OF AVON PARK FORMATION AT 976 FT. BLS. |
981.4 |
988 |
CALCARENITE |
|
VERY PALE ORANGE |
GOOD |
25 |
CALCARENITE, SOME INTERBEDDED DOLOSTONE, NUMEROUS LIMESTONE AND CALCITE ECHINOID MOLDS. |
988 |
992 |
CALCARENITE |
|
VERY PALE ORANGE |
GOOD |
30 |
CALCARENITE, VERY FOSSILIFEROUS, NUMEROUS ECHINOID MOLDS. MATRIX IS MADE UP OF FORAM AND ECHINOID FRAGMENTS. APPEARS HIGHLY PERMEABLE. |
992 |
996 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
5 |
|
996 |
1027 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
20 |
SOME ROUNDED CLASTS OR LENSOIDS OF CALCILUTITE. |
1027 |
1030 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
12 |
|
1030 |
1033 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
16 |
|
1033 |
1034.5 |
MICRITE |
|
YELLOWISH GRAY |
GOOD |
8 |
VERY WELL INDURATED, IRREGULARLY BANDED BED CONTAINING THIN ORGANIC PARTINGS. ORGANIC LAMINAE AT TOP. |
1034.5 |
1038.5 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
16 |
|
1038.5 |
1042.5 |
CALCARENITE |
|
GRAYISH ORANGE |
MODERATE |
18 |
GRAINY FINE-GRAINED CALCARENITE WITH THIN INTERBEDS OF GRAINY CALCILUTITE. |
1042.5 |
1048 |
CALCARENITE |
|
GRAYISH ORANGE |
MODERATE |
26 |
HARD, BRITTLE MODERATELY WELL-SORTED PELLETAL GRAINSTONE. END OF CORE. |
1048 |
1058 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
18 |
FINE-GRAINED CALCARENITE WITH LESSER INTERBEDS OF LIMESTONE AND GRANULAR DOLOSTONE. LOW PERMEABILITY. SOMEWHAT SOFT. INITIAL GROUP OF CUTTINGS DESCRIPTION IS FROM PERMANENT AVON PARK MONITOR. CEMENT FRAGMENTS ARE SEEN IN THE CUTTINGS IN MODERATE CONCENTRATIONS THROUGH 1090 FT. |
1058 |
1070 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
14 |
|
1070 |
1120 |
CALCARENITE |
|
GRAYISH ORANGE |
MODERATE |
20 |
GRANULAR CALCARENITE. DICTYOCONUS. NOT A BIG WATER PRODUCER. UPPER 10 - 20 FT. ARE SOFTER, SLIGHTLY FINER GRAINED THAN REST. |
1120 |
1130 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
16 |
SOMEWHAT HARDER THAN CALCARENITES ABOVE. 1125 - 1130 FT. IS VERY FINE-GRAINED. |
1130 |
1133 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
NO APPARENT WATER PRODUCTION FROM BED. |
1133 |
1145 |
CALCARENITE |
|
GRAYISH ORANGE |
MODERATE |
20 |
VERY GRANULAR SKELETAL CALCARENITE. DICTYOCONUS. DOLOMITE IS PROBABLY FALLING FROM OVERLYING BED. |
1145 |
1156 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
14 |
CALCILUTITIC LIMESTONE WITH LESSER AMOUNTS FINE CALCARENITE. |
1156 |
1182 |
CALCARENITE |
|
VERY PALE ORANGE |
MODERATE |
18 |
FINE TO VERY FINE-GRAINED CALCARENITE. TRACE AMOUNTS OF GRAY LIMESTONE. |
1182 |
1190 |
LIMESTONE |
|
LIGHT GRAY |
MODERATE |
14 |
DOLOMITIC PERCENT IS AS TRACE DOLOMITE GRAINS. |
1190 |
1207 |
CALCARENITE |
|
GRAYISH ORANGE |
MODERATE |
20 |
GRANULAR CALCARENITE. CONTAINS DOLOMITIC GRAINS. DICTYOCONUS. NOT MUCH PERMEABILITY. |
1207 |
1218 |
LIMESTONE |
|
LIGHT GRAY |
MODERATE |
16 |
GRAY CALCILUTITIC LIMESTONE WITH SUBEQUAL BEDS GRANULAR SKELETAL CALCARENITE. |
1218 |
1228 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
30 |
HARD, DARK CRYSTALLINE DOLOMITE. UNIT/SEQUENCE OF DOLOSTONE BEDS MAKES SUBSTANTIAL WATER. TOP OF AVON PARK FRACTURED DOLOSTONES. |
1228 |
1247 |
DOLOMITE |
|
LIGHT OLIVE GRAY |
GOOD |
35 |
OLIVE-COLORED CRYSTALLINE DOLOSTONE WITH SOME BROWN (ORGANIC?) STREAKING. WATER PRODUCER. |
1247 |
1307 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
35 |
BROWN DOLOSTONE. SHOWS SMALL AMOUNTS RECRYSTALLIZATION ON CUTTINGS. SOME DARK STREAKING. |
1307 |
1344 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
35 |
HARD BROWN VERY FINE-GRAINED DOLOSTONE. SOME ORGANIC COATINGS ON CUTTINGS. PRODUCES FETID ODOR ON PUMPING. TRACES OF OXIDE IRON SPECKS. |
1344 |
1359 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
|
|
1359 |
1370 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
|
|
1370 |
1380 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
|
ORGANICS ARE AS STREAKS, SPECKS, AND INTERSTITIAL. |
1380 |
1421 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
INTERBEDDED MICROCRYSTALLINE VERY FINE-GRAINED CALCAREOUS DOLOSTONE AND SLIGHTLY ORGANIC VERY FINE-GRAINED DOLOSTONE. SOME OF ORGANIC UNIT APPEARS TO BE BRECCIATED OR CONTAINS RIP-UP CLASTS. MINOR SECONDARY QUARTZ IN VUGS. |
1421 |
1431 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
|
|
1431 |
1441 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1441 |
1451 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1451 |
1484 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1484 |
1499 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1499 |
1506 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
|
SUBEQUAL INTERBEDS OF TAN, CRYSTALLINE DOLOSTONE AND CREAM-COLORED CALCAREOUS ORTHOCRYSTALLINE DOLOMITE. |
1506 |
1514 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1514 |
1525 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
|
GOLDEN TAN VERY FINE-GRAINED DOLOMITE WITH LESSER INTERBEDDED PALE CALCAREOUS ORTHOCRYSTALLINE DOLOSTONE. FREQUENT QUARTZ PSUEDOMORPHS AFTER RHOMBIC DOLOMITE. |
1525 |
1540 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
|
1540 |
1556 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
INTERBEDDED GOLDEN BROWN VERY FINE GRANULAR DOLOMITE AND ORGANIC STREAKED/SPECKED CALCAREOUS PALE DOLOSTONE. QUARTZ PSUEDOMORPHS AFTER RHOMBIC DOLOMITE ON SURFACES OF THE PALE DOLOSTONE. |
1556 |
1560 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
|
GRANULAR CALCAREOUS DOLOMITE WITH MUCH SECONDARY QUARTZ. |
1560 |
1575 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
CRYSTALLINE LIGHT BROWN DOLOMITE. GRAY AND CREAM-COLORED CALCAREOUS FRAGMENTS (MORE IN UPPER 5 FT.). |
1575 |
1595 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
|
CRYSTALLINE GOLDEN BROWN DOLOMITE WITH MINOR SECONDARY QUARTZ AND ORGANIC COATINGS. |
1595 |
1623 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
12 |
CALCAREOUS DOLOSTONE. LIGHTLY BUT VARIABLY SPECKLED WITH ORGANICS. MINOR VUG-FILL, VEINLETS, AND EUHEDRAL SURFACE COATINGS OF QUARTZ. |
1623 |
1633 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
12 |
COMPACT VERY CALCAREOUS DOLOSTONE. |
1633 |
1638 |
CALCARENITE |
|
GRAYISH ORANGE |
GOOD |
15 |
VARIABLY DOLOMITIC CALCARENITE WITH MINOR AMOUNTS OF QUARTZ AS VEINLETS AND DRUSY COATINGS. |
1638 |
1660 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
15 |
|
1660 |
1665 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
12 |
CALCAREOUS DOLOSTONE CONTAINING DRUSY QUARTZ ON SOME SURFACES. LAMINATED ORGANICS IN SOME OF THE DOLOSTONE. |
1665 |
1686 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
15 |
CALCAREOUS DOLOSTONE. DOME ORGANIC LAMILLAE. |
1686 |
1701 |
MICRITE |
|
VERY PALE ORANGE |
MODERATE |
12 |
MODERATELY INDURATED DOLOMITIC CALCILUTITE. TRACE AMOUNTS ORGANIC LAMELLAE. DREDGING ZONE. LOW PERMEABILITY RESPONSE DURING DRILLING. |
1701 |
1742 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
CALCAREOUS DOLOSTONE, VARIABLY GRANULAR INTERBEDDED WITH OOLOMITIC VUGULAR CALCARENITE. SOME ORGANIC VARVES. |
1742 |
1765 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
INTERBEDDED PALE CALCILUTITIC DOLOMITE, DOLOMITIC CALCARENITE WITH INTERSTITIAL CALCITE, AND ORGANIC-RICH DOLOMITIC CALCARENITE. MINOR BLACK CHERT AT 1765 FT. |