Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
10 |
SAND (QUARTZ) |
|
|
UNCONSOLIDATED |
35 |
SOME POORLY CONSOLIDATED LUMPS PRESENT WITH LAMONITE |
10 |
20 |
SAND (QUARTZ) |
|
|
UNCONSOLIDATED |
35 |
|
20 |
30 |
SAND (QUARTZ) |
|
TRANSPARENT |
UNCONSOLIDATED |
35 |
|
30 |
40 |
SAND (QUARTZ) |
|
TRANSPARENT |
UNCONSOLIDATED |
35 |
|
40 |
50 |
SAND (QUARTZ) |
|
TRANSPARENT |
UNCONSOLIDATED |
35 |
|
50 |
60 |
SAND (QUARTZ) |
|
|
|
|
|
60 |
70 |
NO SAMPLE |
|
|
|
|
|
70 |
90 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
12 |
|
90 |
100 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
12 |
|
100 |
110 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
12 |
SOME MORE INDURATED PORTIONS |
110 |
120 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
12 |
|
120 |
130 |
DOLOMITE |
|
|
GOOD |
12 |
HAS APPEARANCE OF TAMPA |
130 |
140 |
DOLOMITE |
|
|
GOOD |
12 |
|
140 |
150 |
DOLOMITE |
|
|
|
|
SAMPLE CONTAINS CONSIDERABLE AMOUNT OF SAND (CAVE) |
150 |
160 |
DOLOMITE |
|
|
|
|
|
160 |
170 |
DOLOMITE |
|
|
GOOD |
12 |
|
170 |
180 |
DOLOMITE |
|
|
GOOD |
12 |
|
180 |
190 |
DOLOMITE |
|
|
|
|
|
190 |
200 |
DOLOMITE |
|
|
GOOD |
18 |
|
200 |
210 |
DOLOMITE |
|
|
GOOD |
18 |
|
200 |
200 |
DOLOMITE |
|
|
GOOD |
20 |
|
210 |
220 |
DOLOMITE |
|
|
|
22 |
|
220 |
230 |
DOLOMITE |
|
|
GOOD |
24 |
|
230 |
240 |
LIMESTONE |
|
|
GOOD |
16 |
|
240 |
250 |
LIMESTONE |
|
|
GOOD |
16 |
WITH ARCHAIS |
250 |
260 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
24 |
|
260 |
270 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
18 |
|
270 |
280 |
DOLOMITE |
|
|
|
|
MUCH LOOSE SAND AND PHOSPHATE GRAVEL IN SAMPLE (CAVE) |
280 |
290 |
LIMESTONE |
|
|
GOOD |
20 |
|
290 |
300 |
LIMESTONE |
|
|
|
|
|
300 |
310 |
LIMESTONE |
|
|
GOOD |
20 |
|
310 |
320 |
LIMESTONE |
|
|
|
|
|
320 |
330 |
LIMESTONE |
|
|
GOOD |
20 |
SAND GRAINS ARE COATED WITH MICRITE, COULD BE CALLED SAND |
330 |
340 |
LIMESTONE |
|
|
|
|
|
340 |
350 |
LIMESTONE |
|
|
GOOD |
20 |
|
350 |
360 |
LIMESTONE |
|
|
|
|
|
360 |
370 |
LIMESTONE |
|
|
GOOD |
20 |
|
370 |
380 |
LIMESTONE |
|
|
|
|
|
380 |
390 |
LIMESTONE |
|
|
GOOD |
20 |
|
390 |
400 |
LIMESTONE |
|
|
|
|
|
400 |
410 |
LIMESTONE |
|
|
GOOD |
15 |
|
410 |
420 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
420 |
430 |
LIMESTONE |
|
|
|
|
|
430 |
440 |
LIMESTONE |
|
|
GOOD |
18 |
|
440 |
450 |
LIMESTONE |
|
|
|
|
WITH CAROPHYTES |
450 |
460 |
LIMESTONE |
|
|
|
|
|
460 |
470 |
LIMESTONE |
|
|
GOOD |
24 |
|
470 |
480 |
LIMESTONE |
|
|
|
|
|
480 |
490 |
LIMESTONE |
|
|
|
|
CEMENT MICROCRYSTALLINE CALCITE |
490 |
500 |
LIMESTONE |
|
|
|
|
WITH COSKINOLINA FLORIDANA |
500 |
510 |
LIMESTONE |
|
|
|
|
WITH DISCORINOPSIS GUNTERI ROTALIA MEXICANA |
510 |
520 |
LIMESTONE |
|
|
|
|
|
520 |
530 |
LIMESTONE |
|
|
|
|
|
530 |
540 |
LIMESTONE |
|
|
|
|
18 PERCENT VERY COARSE FOS.FRAG. MOL. AND ECH. |
540 |
550 |
LIMESTONE |
|
|
|
|
SOME RECRYSTALLIZATION TO MICROCRYSTALLINE CALCITE LESS FORAMS, MORE COARSE MATERIAL |
550 |
560 |
LIMESTONE |
|
|
|
|
|
560 |
570 |
LIMESTONE |
|
|
|
|
|
570 |
580 |
LIMESTONE |
|
|
|
|
|
580 |
590 |
LIMESTONE |
|
|
|
|
|
590 |
600 |
LIMESTONE |
|
|
GOOD |
24 |
|
600 |
610 |
LIMESTONE |
|
|
|
|
|
610 |
620 |
LIMESTONE |
|
|
GOOD |
24 |
|
620 |
630 |
LIMESTONE |
|
|
|
|
|
630 |
640 |
LIMESTONE |
|
|
|
|
|
640 |
650 |
LIMESTONE |
|
|
|
|
|
650 |
660 |
LIMESTONE |
|
|
GOOD |
26 |
ABUNDANT ECH. PLATES, SIMILAR TO CRYSTAL RIVER BUT NO LEPS |
660 |
670 |
LIMESTONE |
|
|
|
|
|
670 |
680 |
LIMESTONE |
|
|
|
|
|
680 |
690 |
LIMESTONE |
|
|
|
|
|
690 |
700 |
LIMESTONE |
|
|
|
|
|
700 |
710 |
LIMESTONE |
|
|
|
|
|
710 |
720 |
LIMESTONE |
|
|
GOOD |
15 |
MOSTLY MICROCRYSTALLINE CALCITE AND SPARRY CALCITE |
720 |
730 |
LIMESTONE |
|
|
|
12 |
|
730 |
740 |
LIMESTONE |
|
|
|
|
|
740 |
750 |
LIMESTONE |
|
|
GOOD |
15 |
|
750 |
760 |
LIMESTONE |
|
|
GOOD |
15 |
|
760 |
770 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
10 |
|
770 |
780 |
LIMESTONE |
|
|
GOOD |
25 |
|
780 |
790 |
LIMESTONE |
|
|
|
|
SOME LEPS |