Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
30 |
SAND (QUARTZ) |
|
MODERATE BROWN |
UNCONSOLIDATED |
25 |
|
30 |
100 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
UNCONSOLIDATED |
25 |
|
100 |
140 |
SAND (QUARTZ) |
|
MODERATE BROWN |
UNCONSOLIDATED |
25 |
|
140 |
205 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
UNCONSOLIDATED |
25 |
|
205 |
240 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
UNCONSOLIDATED |
25 |
|
240 |
265 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
UNCONSOLIDATED |
25 |
|
265 |
280 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
UNCONSOLIDATED |
25 |
|
280 |
285 |
SAND (QUARTZ) |
|
PALE BROWN |
UNCONSOLIDATED |
25 |
MIXTURE OF 50-60% COARSE QUARTZ SAND TO GRAVELS AND 30-40% LIMESTONE FRAGMENTS. TOP OF THE HAWTHORN FORMATION. |
285 |
310 |
LIMESTONE |
|
GRAYISH BROWN |
POOR |
20 |
SAMPLE IS SIMILAR TO THE ONE ABOVE BUT HAS MORE LIMESTONE THAN QUARTZ SAND/GRAVELS. ALL THE SAND/GRAVEL COULD BE CAVINGS FROM ABOVE. |
310 |
315 |
LIMESTONE |
|
DARK YELLOWISH BROWN |
POOR |
25 |
|
315 |
320 |
SAND (QUARTZ) |
|
DARK YELLOWISH BROWN |
POOR |
25 |
|
320 |
370 |
LIMESTONE |
|
GRAYISH BROWN |
POOR |
25 |
|
370 |
390 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
390 |
405 |
LIMESTONE |
|
DARK YELLOWISH BROWN |
POOR |
20 |
|
405 |
415 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
415 |
440 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
LEPIDOCYCLINA SP., NUMMULITES SP. TOP OF THE OCALA GROUP. |
440 |
470 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
470 |
500 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
500 |
520 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
30 |
|
520 |
535 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
535 |
590 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
30 |
|
590 |
615 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
30 |
|
615 |
670 |
LIMESTONE |
|
|
|
|
FINE PYRITE CRYSTALS WERE NOTED AT 650'--655'. |
670 |
700 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
700 |
735 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
30 |
|
735 |
795 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
795 |
805 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
805 |
875 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
875 |
900 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
CRIBROBULIMINA SP., SPIROLINA SP., DICTYOCONUS SP. TOP OF THE AVON PARK FORMATION. |
900 |
920 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
920 |
940 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
940 |
945 |
DOLOMITE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
945 |
980 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
980 |
1010 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|
1010 |
1045 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
1045 |
1100 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
1100 |
1115 |
DOLOMITE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
1115 |
1135 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
|
1135 |
1155 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
15 |
|
1155 |
1200 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
25 |
|