Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
85 |
NO SAMPLE |
|
|
|
|
|
85 |
90 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
CLAY, LIMESTONE, DOLOMITIZED LIMESTONE ALL PRESENT |
90 |
95 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
|
95 |
100 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
FOR SAMPLES 95 AND 100, THE CLAY IS MICRITIC. THERE ARE NOT SEPARATE LIMESTONE AND CLAY PEICES. |
100 |
105 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
105 |
110 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
110 |
115 |
DOLOMITE |
|
LIGHT GRAY |
GOOD |
15 |
|
115 |
120 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
SOME PIECES ARE MUDSTONES OR WACKESTONES |
120 |
125 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
MICRITE PRESENT IN CLAY AND AS FRAGMENTS OF WACKESTONE |
125 |
130 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
130 |
135 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
135 |
140 |
SAND (QUARTZ) |
|
MODERATE LIGHT GRAY |
POOR |
35 |
MOST OF THE CLAY WAS WASHED OUT OF THE CLEAN SAMPLE |
140 |
145 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
30 |
UNWASHED SAMPLE IS A SANDY CLAY, WASHED SAMPLE IS A CLAYEY SAND |
145 |
150 |
PHOSPHATE |
|
MODERATE DARK GRAY |
GOOD |
15 |
|
150 |
155 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
30 |
ROTALIA PRESENT; CLAY, MICRITE, DOLOMITE ALL CLEAN CHUNKS WITHOUT SAND |
155 |
160 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
160 |
165 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
SORITES PRESENT;MOST OF THE SAMPLE IS AT LEAST PARTLY DOLOMITIZED |
165 |
170 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
170 |
175 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
175 |
180 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
180 |
185 |
NO SAMPLE |
|
|
|
|
|
185 |
190 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
190 |
195 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
195 |
200 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
|
200 |
205 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
|
205 |
210 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
210 |
215 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
215 |
220 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
|
220 |
225 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
MOST OF THE SAND IS FINE-VERY FINE GRAINED |
225 |
230 |
CLAY |
|
OLIVE GRAY |
POOR |
15 |
|
230 |
235 |
CLAY |
|
OLIVE GRAY |
POOR |
15 |
|
235 |
240 |
CLAY |
|
YELLOWISH GRAY |
POOR |
15 |
|
240 |
245 |
CLAY |
|
LIGHT OLIVE GRAY |
POOR |
15 |
|
245 |
250 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
250 |
255 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
255 |
260 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
260 |
265 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
265 |
270 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
SORITES PRESENT; THERE ARE A FEW PEICES FULL OF SAND, BUT MOST HAVE VERY LITTLE; ALSO, THESE ROCKS COULD BE CONSIDERED A MUDDY PACKESTONE BECAUSE THEY HAVE SO MANY GRAINS |
270 |
275 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
275 |
280 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
ALMOST A PACKESTONE |
280 |
285 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
|
285 |
290 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
SOME PARTS HAVE AS MUCH AS 50% SAND, WHILE OTHERS CONTAIN ALMOST NO SAND |
290 |
295 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
15 |
VARYING AMOUNTS OF SAND, FROM A SANDSTONE (85% SAND) TO A WACKESTONE WITH <5% SAND; NOT AS BIMODAL AS IT IS GRADATIONAL; ALSO THE CLAY MAY SIMPLY BE CAVINGS |
295 |
305 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
BETWEEN 295 AND 305 THE SAMPLE BECOMES MORE ORANGE, FINER GRAINED AND INCREASES IN GRAIN % |
305 |
305 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
THERE IS EXTRA LOOSE SAND |
305 |
310 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
310 |
315 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
315 |
320 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
320 |
325 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
SOME PIECES IN THIS SAMPLE ARE A VERY SANDY WACKESTONE. MOST ARE NOT |
325 |
330 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
330 |
335 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
335 |
340 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
THIS SAMPLE CONSISTS OF SMALL FRAGMENTS OF PACKESTONE-WACKESTONE, MOSTLY DEVOID OF SAND, AND ABOUT 25% UNCONSOLIDATED SAND. THERE ARE ALSO A FEW FRAGMENTS OF SANDY WACKESTONE |
340 |
345 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
SAMD UNCONSOLIDATED, PROBABLY FROM CAVINGS |
345 |
350 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
FEWER SKELETAL FRAGMENTS, MORE BROKEN |
350 |
355 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
355 |
360 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
360 |
365 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
365 |
370 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
GRAIN SIZE IS MARKEDLY FINER; CHANGE IN FOSSIL ASSEMBLAGE NUMMULITES, LEPIDOCYCLINA PRESENT AND ABUNDANT |
370 |
375 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
NUMMULITES, LEPIDOCYCLINA, SHPAEROGYPSINA PRESENT |
375 |
380 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA PRESENT |
380 |
385 |
NO SAMPLE |
|
|
|
|
|
385 |
390 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
390 |
395 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
NUMMULITES PRESENT |
395 |
400 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
400 |
405 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA PRESENT |
405 |
410 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
410 |
415 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, SPHAEROGYPSINA PRESENT |
415 |
420 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES, SPIROLINA VERONI PRESENT |
420 |
425 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
425 |
430 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
OVER 50 % OF THE SAMPLE IS UNCEMENTED FORAMINIFERA; LEPIDOCYCLINA, NUMMULITES PRESENT |
430 |
435 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
1 |
FOR INTERVALS 430-500, THE MAJORITY OF THE SAMPLE IS LOOSE FORAMINIFERA; THE REST OF THE SAMPLE IS PACKESTONE LEPIDOCYCLINA, NUMMULITES PRESENT |
435 |
440 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
440 |
445 |
NO SAMPLE |
|
|
|
|
|
445 |
450 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
450 |
455 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
455 |
460 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
460 |
465 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
465 |
470 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
470 |
475 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
THERE ARE SOME PIECES OF MEDUIM GRAINED PACKESTONE |
475 |
480 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
480 |
485 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
485 |
490 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
490 |
495 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
495 |
500 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
SHPAEROGYPSINA, LEPIDOCYCLINA, NUMMULITES PRESENT; SMALL AMOUNT OF LOOSE SAND |
500 |
505 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
2 LITHOLOGIES: FINE TO VERY FINE GRAINED PACKESTONE AND MEDIUM GRAINED PACKESTONE; LEPIDOCYCLINA AND NUMMULITES ARE SLIGHTLY LESS ABUNDANT (ABOUT 40% OF SAMPLE) |
505 |
510 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
STILL 2 LITHOLOGIES; LEPIDOCYCLINA, NUMMULITES PRESENT; QUITE A BIT OF LOOSE SAND; SOME SANDY WACKESTONES |
510 |
515 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LOOSE SAND AND SOME SANDY WACKESTONE PRESENT- PROBABLY DUE TO CAVINGS; LEPIDOCYCLINA, NUMMULITES PRESENT |
515 |
520 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
520 |
525 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
MUCH MUDDIER MEDIUM GRAINED PACKESTONE; LEPIDOCYCLINA AND NUMMULITES ABUNDANTLY CEMENTED IN; SAND IS CEMENTED INTO THE PACKESTONE. THIS SAMPLE IS VERY UNLIKE THE PREVIOUS SAMPLES. |
525 |
530 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
A LOT OF LOOSE QUARTZ SAND, BUT IT DOESN'T APPEAR TO BE IN MANY OF THE ROCKS; LEPIDOCYCLINA, NUMMULITES PRESENT |
530 |
535 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
QUITE A BIT OF LOOSE QUARTZ SAND, A LITTLE PHOSPHATE SAND- NEITHER ARE IN THE ROCKS |
535 |
540 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
540 |
545 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS, LEPIDOCYCLINA, NUMMULITES PRESENT |
545 |
550 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
550 |
555 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
555 |
560 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
560 |
565 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS, NUMMULITES PRESENT |
565 |
570 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
NUMMULITES PRESENT |
570 |
575 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
575 |
580 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS, NUMMULITES PRESENT |
580 |
585 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
NUMMULITES PRESENT |
585 |
590 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA PRESENT |
590 |
595 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
NUMMULITES PRESENT |
595 |
600 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
600 |
605 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA CEMENTED INTO ROCK; TWO LITHOLOGIES: ONE FINE GRAINED PACKESTONE, ONE MEDIUM GRAINED PACKESTONE; DICTYOCONUS PRESENT |
605 |
610 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA PRESENT |
610 |
615 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, DICTYOCONUS PRESENT |
615 |
620 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, NUMMULITES PRESENT |
620 |
625 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
LEPIDOCYCLINA, DICTYOCONUS PRESENT; 2 LITHOLOGIES IN 610-625: A MUDDY, FINE GRAINED PACKESTONE AND A MEDIUM GRAINED PACKESTONE; THE MEDIUM GRAINED ONE IS THE MOST ABUNDANT |
625 |
630 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS, NUMMULITES, LEPIDOCYCLINA PRESENT; STILL 2 LITHOLOGIES, BUT NOW THE MUDDY, MEDUIM GRAINED PACKESTONE IS MOST ABUNDANT |
630 |
635 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
635 |
640 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS, SPHAEROGYPSINA PRESENT |
640 |
645 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS PRESENT |
645 |
650 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS PRESENT |
650 |
655 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS PRESENT |
655 |
660 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
DICTYOCONUS PRESENT |
660 |
665 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
DICTYOCONUS, LEPIDOCYCLINA PRESENT |
665 |
670 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
SPIROLINA, LEPIDOCYCLINA, DICTYOCONUS PRESENT |
670 |
675 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
675 |
680 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
680 |
685 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
|
685 |
690 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
690 |
695 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
NUMMULITES, DICTYOCONUS PRESENT |
695 |
700 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
700 |
705 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
705 |
710 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
SPIROLINA, DICTYOCONUS PRESENT |
710 |
715 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
715 |
720 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
720 |
725 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
725 |
730 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
NUMMULITES, DICTYOCONUS PRESENT |
730 |
735 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
735 |
740 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
740 |
745 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
745 |
750 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
LITUONELLA, DICTYOCONUS PRESENT |
750 |
760 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
760 |
770 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
DICTYOCONUS PRESENT |
770 |
775 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
DICTYOCONUS PRESENT |
775 |
780 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
780 |
785 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
NUMMULITES PRESENT |
785 |
790 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
LEPIDOCYCLINA |
790 |
795 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
795 |
800 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
DICTYOCONUS PRESENT |
800 |
805 |
NO SAMPLE |
|
|
|
|
|
805 |
810 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
|
810 |
815 |
DOLOMITE |
|
VERY PALE ORANGE |
GOOD |
15 |
NUMMULITES PRESENT |
815 |
820 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
NUMMULITES PRESENT |
820 |
825 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
DICTYOCONUS PRESENT |
825 |
830 |
DOLOMITE |
|
GRAYISH BROWN |
GOOD |
15 |
DICTYOCONUS PRESENT; NON-DOLOMITIC PARTS ARE A FINE GRAINED PACKESTONE |