Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
10 |
SAND (QUARTZ) |
|
|
UNCONSOLIDATED |
35 |
|
10 |
20 |
CHALK |
|
|
GOOD |
10 |
|
20 |
30 |
CLAY |
|
VERY PALE ORANGE |
GOOD |
10 |
CHALK IS MIXED WITH THE CLAY MATRIX |
30 |
40 |
CLAY |
|
LIGHT YELLOWISH ORANGE |
GOOD |
10 |
|
40 |
50 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
18 |
ABUNDANT SAND INDICATES CAVING |
50 |
60 |
DOLOMITE |
|
WHITE |
GOOD |
18 |
|
60 |
70 |
CLAY |
|
VERY LIGHT GRAY |
GOOD |
10 |
|
70 |
80 |
DOLOMITE |
|
WHITE |
GOOD |
10 |
|
80 |
90 |
DOLOMITE |
|
|
GOOD |
18 |
|
90 |
100 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
18 |
|
100 |
110 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
18 |
|
110 |
120 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
18 |
|
120 |
130 |
NO SAMPLE |
|
|
|
|
|
130 |
140 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
22 |
|
140 |
150 |
DOLOMITE |
|
YELLOWISH GRAY |
GOOD |
22 |
ABUNDANT SAND, PROBABLE CAVING |
150 |
160 |
CLAY |
|
VERY PALE ORANGE |
|
10 |
|
160 |
170 |
SAND (QUARTZ) |
|
DARK GREENISH GRAY |
UNCONSOLIDATED |
30 |
|
170 |
180 |
SAND (QUARTZ) |
|
|
|
|
|
180 |
190 |
SAND (QUARTZ) |
|
DARK GREENISH GRAY |
UNCONSOLIDATED |
30 |
|
190 |
200 |
SAND (QUARTZ) |
|
DARK GREENISH GRAY |
UNCONSOLIDATED |
29 |
|
200 |
210 |
SAND (QUARTZ) |
|
DARK GREENISH GRAY |
UNCONSOLIDATED |
30 |
|
210 |
220 |
SAND (QUARTZ) |
|
|
|
|
|
220 |
230 |
LIMESTONE |
|
|
GOOD |
23 |
WITH SORITES AND ROTALIA MEXICANA |
230 |
240 |
LIMESTONE |
|
|
|
|
|
240 |
250 |
LIMESTONE |
|
WHITE |
GOOD |
22 |
|
250 |
260 |
LIMESTONE |
|
WHITE |
GOOD |
22 |
|
260 |
270 |
LIMESTONE |
|
WHITE |
GOOD |
22 |
|
270 |
280 |
LIMESTONE |
|
|
|
|
|
280 |
290 |
LIMESTONE |
|
WHITE |
GOOD |
22 |
HARD DENSE LIMESTONE |
290 |
300 |
LIMESTONE |
|
WHITE |
GOOD |
22 |
|
300 |
310 |
LIMESTONE |
|
|
|
|
|
310 |
320 |
LIMESTONE |
|
LIGHT OLIVE GRAY |
GOOD |
21 |
WITH GYPSINA GLOBULA AND ALABAMIA OBTUSA |
320 |
330 |
LIMESTONE |
|
|
|
|
|
330 |
340 |
LIMESTONE |
|
WHITE |
GOOD |
20 |
|
340 |
350 |
LIMESTONE |
|
|
|
|
WITH OPERCULINOIDES SP. |
350 |
360 |
LIMESTONE |
|
WHITE |
GOOD |
20 |
WITH LEPIDOCYLCINA OCALANA |
360 |
380 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
24 |
WITH NUMMULITIES VANDERSTOKI |
380 |
390 |
CALCARENITE |
|
|
|
|
|
390 |
400 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
24 |
|
400 |
420 |
CALCARENITE |
|
|
|
|
|
420 |
430 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
24 |
|
430 |
440 |
CALCARENITE |
|
|
|
|
|
440 |
450 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
24 |
|
450 |
460 |
CALCARENITE |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
24 |
WITH OPERCULINOIDES MOODYSBRANCHENSIS |
460 |
470 |
DOLOMITE |
|
LIGHT GRAY |
GOOD |
22 |
|
470 |
480 |
LIMESTONE |
|
|
GOOD |
23 |
MILLIOLID LIMESTONE |
480 |
490 |
LIMESTONE |
|
|
|
|
WITH DICTYCONUS COOKEI AND SPIROLINA CORYENSIS (UNCONFORMITY) |
490 |
500 |
LIMESTONE |
|
|
GOOD |
23 |
|
500 |
510 |
NO SAMPLE |
|
|
|
|
|
510 |
520 |
NO SAMPLE |
|
|
|
|
|
520 |
530 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
23 |
|
530 |
550 |
LIMESTONE |
|
|
|
|
WITH LITUONELLA FLORIDANA; ABUNDANT DICTYCONUS COOKEI |
550 |
560 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
23 |
|
560 |
570 |
NO SAMPLE |
|
|
|
|
|
570 |
610 |
NO SAMPLE |
|
|
|
|
MILLIOD LMST. SAMPLE IS LIKE CALCAREOUS SAND |
610 |
620 |
NO SAMPLE |
|
|
|
|
|
620 |
670 |
NO SAMPLE |
|
|
|
|
|
670 |
680 |
LIMESTONE |
|
|
GOOD |
21 |
MANY CRYSTAL RIVER FORAMS (POSSIBLE CAVING) |
680 |
690 |
LIMESTONE |
|
|
GOOD |
21 |
|
690 |
700 |
DOLOMITE |
|
WHITE |
GOOD |
22 |
|
700 |
710 |
DOLOMITE |
|
|
GOOD |
23 |
|
710 |
720 |
DOLOMITE |
|
|
|
|
|
720 |
730 |
DOLOMITE |
|
|
GOOD |
23 |
|
730 |
740 |
DOLOMITE |
|
|
|
|
|
740 |
750 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
23 |
|
750 |
760 |
DOLOMITE |
|
DARK YELLOWISH BROWN |
GOOD |
23 |
|
760 |
770 |
DOLOMITE |
|
|
|
|
|
770 |
780 |
DOLOMITE |
|
|
GOOD |
23 |
|
780 |
790 |
DOLOMITE |
|
|
|
|
|
790 |
800 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
23 |
|
800 |
810 |
DOLOMITE |
|
|
GOOD |
21 |
|
810 |
830 |
DOLOMITE |
|
|
|
|
|
830 |
840 |
DOLOMITE |
|
|
GOOD |
22 |
|
840 |
850 |
DOLOMITE |
|
|
|
|
|
850 |
860 |
DOLOMITE |
|
|
GOOD |
22 |
|
860 |
870 |
DOLOMITE |
|
|
|
|
|
870 |
880 |
DOLOMITE |
|
|
GOOD |
22 |
|
880 |
890 |
DOLOMITE |
|
|
|
|
|
890 |
900 |
DOLOMITE |
|
|
GOOD |
22 |
|
900 |
910 |
DOLOMITE |
|
|
|
|
|
910 |
920 |
DOLOMITE |
|
|
GOOD |
22 |
|
920 |
940 |
DOLOMITE |
|
|
|
|
|
940 |
950 |
DOLOMITE |
|
|
GOOD |
22 |
|
950 |
960 |
DOLOMITE |
|
|
GOOD |
23 |
|
960 |
970 |
DOLOMITE |
|
|
GOOD |
23 |
|
970 |
980 |
DOLOMITE |
|
|
GOOD |
23 |
|
980 |
1020 |
NO SAMPLE |
|
|
|
|
|
1020 |
1030 |
DOLOMITE |
|
|
GOOD |
22 |
|
1030 |
1040 |
DOLOMITE |
|
|
|
|
|
1040 |
1050 |
DOLOMITE |
|
|
GOOD |
22 |
|
1050 |
1060 |
DOLOMITE |
|
|
GOOD |
22 |
|
1060 |
1080 |
DOLOMITE |
|
|
|
|
|