Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
30 |
LIMESTONE |
|
WHITE |
MODERATE |
25 |
|
30 |
50 |
LIMESTONE |
|
WHITE |
MODERATE |
10 |
|
50 |
80 |
SHELL |
|
WHITE |
UNCONSOLIDATED |
30 |
|
80 |
140 |
LIMESTONE |
|
VERY LIGHT GRAY |
MODERATE |
30 |
|
140 |
170 |
LIMESTONE |
|
MODERATE LIGHT GRAY |
MODERATE |
25 |
|
170 |
210 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
30 |
|
210 |
240 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
30 |
|
240 |
270 |
LIMESTONE |
|
LIGHT OLIVE GRAY |
MODERATE |
25 |
|
270 |
280 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
POOR |
25 |
TOP OF MIOCENE/THE HAWTHORN FORMATION. |
280 |
350 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
350 |
370 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
370 |
410 |
SILT |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
410 |
460 |
SILT |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
460 |
540 |
SILT |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
540 |
630 |
SILT |
|
LIGHT OLIVE GRAY |
POOR |
10 |
|
630 |
710 |
SILT |
|
LIGHT OLIVE GRAY |
POOR |
10 |
SAMPLE 630-640' CONTAINS FRAGMENTS OF SANDY LIMESTONE, POSSIBLE CAVINGS. |
710 |
730 |
LIMESTONE |
|
WHITE |
MODERATE |
25 |
|
730 |
770 |
CLAY |
|
YELLOWISH GRAY |
POOR |
|
|
770 |
790 |
CLAY |
|
YELLOWISH GRAY |
POOR |
|
|
790 |
820 |
CLAY |
|
YELLOWISH GRAY |
POOR |
|
|
820 |
850 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
15 |
|
850 |
870 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
15 |
|
870 |
900 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
|
900 |
920 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
|
|
920 |
940 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
25 |
|
940 |
990 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
990 |
1040 |
LIMESTONE |
|
VERY LIGHT GRAY |
GOOD |
20 |
|
1040 |
1090 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
|
1090 |
1130 |
LIMESTONE |
|
LIGHT GREENISH GRAY |
MODERATE |
25 |
|
1130 |
1160 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
NUMMULITES SP., HETEROSTEGINA SP., LEPIDOCYCLINA SP.; TOP OF UPPER EOCENE/THE OCALA LIMESTONE. |
1160 |
1170 |
NO SAMPLE |
|
|
|
|
|
1170 |
1180 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1180 |
1210 |
LIMESTONE |
|
GRAYISH ORANGE PINK |
MODERATE |
25 |
|
1210 |
1220 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
1220 |
1310 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1310 |
1340 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
1340 |
1370 |
LIMESTONE |
|
PINKISH GRAY |
MODERATE |
20 |
|
1370 |
1380 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1380 |
1410 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS SP., LITUONELLA SP.; TOP OF MIDDLE EOCENE/THE AVON PARK FORMATION. |
1410 |
1430 |
LIMESTONE |
|
WHITE |
MODERATE |
15 |
|
1430 |
1470 |
LIMESTONE |
|
WHITE |
MODERATE |
20 |
|
1470 |
1490 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1490 |
1500 |
LIMESTONE |
|
WHITE |
MODERATE |
15 |
|
1500 |
1520 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1520 |
1550 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
1550 |
1560 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
15 |
|
1560 |
1600 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
1600 |
1620 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
1620 |
1640 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
1640 |
1670 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
10 |
|
1670 |
1680 |
LIMESTONE |
|
WHITE |
GOOD |
10 |
|
1680 |
1700 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
1700 |
1710 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
10 |
|
1710 |
1730 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
20 |
|
1730 |
1740 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
1740 |
1760 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
25 |
|
1760 |
1790 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
1790 |
1810 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
1810 |
1820 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
GRAY DRILLING CEMENT. |
1820 |
1870 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
10 |
|
1870 |
1900 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
MOST OF THE ORIGINAL ALLOCHEMS (CONES, MILIOLIDS AND OTHER FORAMS) REMAIN UNALTERED. |
1900 |
1910 |
LIMESTONE |
|
WHITE |
GOOD |
10 |
|
1910 |
1940 |
DOLOMITE |
|
WHITE |
GOOD |
15 |
|
1940 |
1970 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1970 |
2010 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
2010 |
2040 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
25 |
|
2040 |
2050 |
NO SAMPLE |
|
|
|
|
|
2050 |
2070 |
DOLOMITE |
|
WHITE |
GOOD |
10 |
|
2070 |
2080 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
2080 |
2100 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
25 |
|
2100 |
2110 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
10 |
|
2110 |
2120 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
2120 |
2140 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
25 |
|
2140 |
2150 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
2150 |
2160 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
15 |
|
2160 |
2180 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
CALCAREOUS ALLOCHEMS (CONES AND OTHER FORAMS) IN A DOLOMITE MATRIX. |
2180 |
2200 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
25 |
|
2200 |
2220 |
DOLOMITE |
|
WHITE |
GOOD |
25 |
SOME OF THE CALCAREOUS ALLOCHEMS (CONES AND OTHER FORAMS) REMAIN UNALTERED. |
2220 |
2250 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
2250 |
2260 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
15 |
|
2260 |
2280 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
20 |
A FEW CALCAREOUS ALLOCHEMS (CONES AND OTHER FORAMS) REMAIN UNALTERED. |
2280 |
2300 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
2300 |
2340 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
25 |
TWO DISTINCT COLORS OF DOLOMITE. THE DARKER DOLOMITE SEEMS TO ORIGINATED FROM AN ORGANIC RICH LIMESTONE. SOME OF THE DARK DOLOMITE CRYSTALS GROW ON THE WALL OF A POSSIBLE ROOT TRACE/TUBE. |
2340 |
2390 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
MOST OF THE ALLOCHEMS (CONES AND OTHER FORAMS) REMAIN UNALTERED IN A DOLOMITE MATRIX. TRACE OF DARK BROWNISH BLACK ORGANIC MATERIAL IS NOTED IN THE SAMPLE. |
2390 |
2490 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
2490 |
2520 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
15 |
THERE ARE A FEW UNALTERED CALCAREOUS CONES REMAINING IN THE TOP 10' SAMPLE OF THIS INTERVAL. |
2520 |
2530 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
25 |
|
2530 |
2550 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
20 |
|
2550 |
2610 |
LIMESTONE |
|
PINKISH GRAY |
GOOD |
20 |
|
2610 |
2630 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
|
2630 |
2670 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
ROCK IS PARTIALLY DOLOMITIZED LIMESTONE. |
2670 |
2690 |
DOLOMITE |
|
GRAYISH ORANGE |
GOOD |
20 |
|
2690 |
2730 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
ROCK HAS NOT BEEN COMPLETELY DOLOMITIZED. PART OF THE LIMESTONE, ESPECIALLY ALLOCHEMS, REMAIN UNALTERED. |
2730 |
2750 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
SOME OF THE LIMESTONE REMAIN UNALTERED. |
2750 |
2770 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
|
|
2770 |
2790 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
10 |
ALLOCHEMS ARE MAINLY VERY FINE PELOIDS. |
2790 |
2800 |
CHERT |
|
VERY LIGHT GRAY |
GOOD |
|
|
2800 |
2850 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
10 |
|
2850 |
2880 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
|
|
2880 |
2900 |
CHERT |
|
LIGHT OLIVE GRAY |
GOOD |
|
|
2900 |
2940 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
|
|
2940 |
2970 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
|
TRACE AMOUNT OF GLAUCONITE IS PRESENT. TOP OF THE GLAUCONITE MARKER BED/LOWER EOCENE/THE OLDSMAR FORMATION. |
2970 |
3000 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
|
|
3000 |
3030 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
10 |
|
3030 |
3040 |
CHERT |
|
DARK YELLOWISH BROWN |
GOOD |
|
|
3040 |
3050 |
LIMESTONE |
|
YELLOWISH GRAY |
GOOD |
15 |
|
3050 |
3060 |
LIMESTONE |
|
YELLOWISH GRAY |
GOOD |
|
|
3060 |
3070 |
LIMESTONE |
|
YELLOWISH GRAY |
GOOD |
20 |
GRAINS OF GLAUCONITE SCATTER IN THE LIMESTONE. THIS SAMPLE HAS THE HIGHEST CONCENTRATION OF GLAUCONITE IN THIS WELL. |
3070 |
3090 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
20 |
ALLOCHEMS ARE MAINLY RECRYSTALLIZED FINE PELOIDS AND MILIOLIDS. |
3090 |
3110 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
25 |
|
3110 |
3130 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
3130 |
3150 |
LIMESTONE |
|
WHITE |
GOOD |
20 |
|
3150 |
3200 |
LIMESTONE |
|
WHITE |
MODERATE |
20 |
|
3200 |
3220 |
LIMESTONE |
|
WHITE |
MODERATE |
20 |
|
3220 |
3240 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
|
3240 |
3280 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
|
3280 |
3310 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
20 |
|
3310 |
3350 |
DOLOMITE |
|
MODERATE YELLOWISH BROWN |
GOOD |
25 |
|
3350 |
3390 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
|
3390 |
3410 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
|
LIGHT BROWN COLORED EUHEDRAL DOLOSPARS FILL IN THE VOIDS IN THE DENSE DOLOSTONE. |
3410 |
3440 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
10 |
|
3440 |
3470 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
10 |
|
3470 |
3500 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
|
|