Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
10 |
SAND (QUARTZ) |
|
|
UNCONSOLIDATED |
|
|
10 |
20 |
SAND (QUARTZ) |
|
TRANSPARENT |
UNCONSOLIDATED |
|
ABUNDANT ABRAIDED MOLLUSKS FRAGMENTS |
20 |
20 |
LIMESTONE |
|
|
MODERATE |
9 |
|
20 |
30 |
LIMESTONE |
|
|
MODERATE |
9 |
|
30 |
40 |
LIMESTONE |
|
|
|
|
|
40 |
50 |
SAND (QUARTZ) |
|
TRANSPARENT |
MODERATE |
15 |
|
40 |
40 |
DOLOMITE |
|
|
GOOD |
4 |
|
50 |
50 |
LIMESTONE |
|
WHITE |
UNCONSOLIDATED |
|
ABUN. WELLROUNDED NODULES OF CALCITE (RADIATING FROM CENTRAL PT.) |
50 |
60 |
DOLOMITE |
|
|
GOOD |
9 |
|
60 |
70 |
DOLOMITE |
|
|
|
|
|
70 |
90 |
NO SAMPLE |
|
|
|
|
|
90 |
100 |
DOLOMITE |
|
|
GOOD |
9 |
|
100 |
110 |
DOLOMITE |
|
|
|
|
|
110 |
120 |
DOLOMITE |
|
|
|
|
LOCAL VARIATIONS IN SAND AND PHOS. CONC. |
120 |
130 |
DOLOMITE |
|
|
|
|
|
130 |
140 |
DOLOMITE |
|
|
|
|
|
140 |
150 |
DOLOMITE |
|
|
|
|
A LESS CHALK MORE SUCROSIC (SUBHEDRAL DOL.) |
150 |
160 |
DOLOMITE |
|
|
|
|
|
160 |
170 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
4 |
|
170 |
180 |
DOLOMITE |
|
|
|
|
|
180 |
190 |
LIMESTONE |
|
WHITE |
GOOD |
5 |
ARCHAIAS AND SORITES |
190 |
200 |
LIMESTONE |
|
|
|
|
|
200 |
210 |
LIMESTONE |
|
WHITE |
GOOD |
12 |
|
210 |
220 |
DOLOMITE |
|
|
|
|
QTZ. SAND LOCALLY UP TO 50 PERCENT |
210 |
210 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
|
|
220 |
230 |
DOLOMITE |
|
|
|
|
|
230 |
230 |
DOLOMITE |
|
|
|
|
|
230 |
240 |
DOLOMITE |
|
|
|
|
|
240 |
260 |
NO SAMPLE |
|
|
|
|
|
260 |
270 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
|
|
270 |
280 |
DOLOMITE |
|
|
|
|
|
280 |
290 |
SAND (QUARTZ) |
|
TRANSPARENT |
POOR |
17 |
|
290 |
300 |
DOLOMITE |
|
|
MODERATE |
4 |
|
300 |
310 |
LIMESTONE |
|
WHITE |
GOOD |
7 |
|
310 |
320 |
LIMESTONE |
|
|
|
|
|
320 |
330 |
LIMESTONE |
|
|
|
|
|
330 |
340 |
SAND (QUARTZ) |
|
|
POOR |
10 |
|
340 |
340 |
LIMESTONE |
|
|
GOOD |
6 |
|
340 |
350 |
LIMESTONE |
|
|
|
|
|
350 |
360 |
LIMESTONE |
|
|
|
|
ALL SAND CAVINGS |
360 |
380 |
SAND (QUARTZ) |
|
|
MODERATE |
10 |
|
380 |
400 |
SAND (QUARTZ) |
|
|
|
|
|
400 |
410 |
SAND (QUARTZ) |
|
|
|
|
|
410 |
420 |
SAND (QUARTZ) |
|
|
|
|
|
420 |
430 |
SAND (QUARTZ) |
|
|
|
|
|
430 |
440 |
SAND (QUARTZ) |
|
|
MODERATE |
10 |
|
440 |
450 |
SAND (QUARTZ) |
|
|
MODERATE |
10 |
|
450 |
460 |
LIMESTONE |
|
|
POOR |
10 |
|
460 |
470 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
6 |
|
470 |
480 |
LIMESTONE |
|
|
|
|
|
480 |
490 |
LIMESTONE |
|
|
|
|
|
490 |
500 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
8 |
|
500 |
510 |
LIMESTONE |
|
|
|
|
|
510 |
520 |
LIMESTONE |
|
|
|
|
|
520 |
530 |
LIMESTONE |
|
|
|
|
|
530 |
540 |
LIMESTONE |
|
|
GOOD |
10 |
ROTALIA MEXICANA |
540 |
550 |
LIMESTONE |
|
|
|
|
|
550 |
560 |
LIMESTONE |
|
|
|
|
|
560 |
570 |
LIMESTONE |
|
|
|
|
|
570 |
580 |
LIMESTONE |
|
|
|
|
BUT BETWEEN 5 AND 70 PERCENT QTZ. SAND |
580 |
590 |
LIMESTONE |
|
|
|
|
|
590 |
600 |
LIMESTONE |
|
|
|
|
|
600 |
610 |
LIMESTONE |
|
|
GOOD |
9 |
MINOR ORGANIC STAIN |
610 |
620 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
10 |
DISCORINOPSIS GUNTERI SORITES, SPARITE/MICRITE 3/2 |
620 |
630 |
LIMESTONE |
|
|
|
|
|
630 |
640 |
LIMESTONE |
|
|
|
|
|
640 |
650 |
LIMESTONE |
|
|
|
|
10 PERCENT ECHINOID FRAG. |
650 |
660 |
LIMESTONE |
|
|
|
|
|
660 |
670 |
LIMESTONE |
|
|
|
|
|
670 |
680 |
LIMESTONE |
|
|
|
|
|
680 |
690 |
LIMESTONE |
|
|
|
|
|
690 |
700 |
LIMESTONE |
|
|
|
|
|
700 |
710 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
710 |
720 |
LIMESTONE |
|
|
|
|
|
720 |
730 |
LIMESTONE |
|
|
|
|
15 PERCENT LIGHT GRAY FROM ORGANIC STAIN |
730 |
740 |
LIMESTONE |
|
|
|
|
|
740 |
750 |
LIMESTONE |
|
|
|
|
|
750 |
760 |
LIMESTONE |
|
|
|
|
|
760 |
770 |
LIMESTONE |
|
|
|
|
A SLIGHT GRANULAR APPEARANCE |
770 |
780 |
LIMESTONE |
|
|
|
|
SOME ORGANIC STAIN |
780 |
790 |
LIMESTONE |
|
|
|
|
10 PERCENT LIGHT GRAY ORGANIC |
790 |
800 |
LIMESTONE |
|
|
|
|
|
800 |
800 |
DOLOMITE |
|
MODERATE DARK GRAY |
GOOD |
|
|
800 |
810 |
LIMESTONE |
|
WHITE |
GOOD |
15 |
|
810 |
820 |
LIMESTONE |
|
|
GOOD |
8 |
GRANULAR LEPIDOCYCLINA OCALANA AND GYPSINA GLOBULA |
820 |
830 |
LIMESTONE |
|
|
|
|
|
830 |
840 |
LIMESTONE |
|
|
|
|
MOSTLY LEPIDOCYCLINA TESTS |
840 |
850 |
LIMESTONE |
|
|
|
|
|
850 |
860 |
LIMESTONE |
|
|
|
|
MOSTLY NUMMULITES VANDERSTOKI AND OPERCULINOIDES FLORIDENSIS 85 PERCENT |
860 |
870 |
LIMESTONE |
|
|
|
|
|
870 |
880 |
LIMESTONE |
|
|
|
|
|
880 |
890 |
LIMESTONE |
|
|
|
|
|
890 |
900 |
LIMESTONE |
|
|
|
|
|
900 |
910 |
LIMESTONE |
|
|
|
|
|
910 |
920 |
LIMESTONE |
|
|
|
|
|
920 |
930 |
LIMESTONE |
|
|
|
|
|
930 |
940 |
LIMESTONE |
|
|
|
|
|
940 |
950 |
LIMESTONE |
|
|
|
|
|
950 |
960 |
LIMESTONE |
|
|
|
|
|
960 |
970 |
DOLOMITE |
|
DUSKY BROWN |
GOOD |
4 |
|
970 |
980 |
DOLOMITE |
|
|
|
|
|
980 |
990 |
DOLOMITE |
|
|
|
|
|
990 |
1000 |
DOLOMITE |
|
|
|
|
|
1000 |
1010 |
DOLOMITE |
|
|
|
|
|
1010 |
1020 |
DOLOMITE |
|
|
|
|
PREDOMINANTLY DARK YELLOW ORANGE, MORE SUBHEDRAL |
1020 |
1030 |
DOLOMITE |
|
|
|
|
|
1030 |
1040 |
DOLOMITE |
|
|
|
|
|
1040 |
1050 |
DOLOMITE |
|
|
|
|
|
1050 |
1060 |
DOLOMITE |
|
|
|
|
|
1060 |
1070 |
DOLOMITE |
|
|
|
|
PALE YELLOWISH BROWN |
1070 |
1080 |
DOLOMITE |
|
|
|
|
ALL DARK REDDISH BROWN |
1080 |
1090 |
DOLOMITE |
|
|
|
|
|
1090 |
1100 |
DOLOMITE |
|
|
|
|
|
1100 |
1110 |
DOLOMITE |
|
|
|
|
|
1110 |
1120 |
DOLOMITE |
|
|
|
|
|
1120 |
1130 |
LIMESTONE |
|
VERY PALE ORANGE |
GOOD |
8 |
|
1130 |
1140 |
LIMESTONE |
|
|
|
|
CHALKY LIMESTONE AND BROWNISH BLACK DOLOMITE |