Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
0 |
30 |
LIMESTONE |
|
LIGHT YELLOWISH ORANGE |
MODERATE |
25 |
DOMINANTLY RECRYSTALLEZED LIMESTONE: CALCILUTITE MUD CONTENT(25%) INTERVAL 0-10 FEET. |
30 |
40 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
25 |
25% OF SAMPLE CONSISTS OF WELL ROUNDED TO SUB ROUNDED FINE-COARSE GRAINED QTZ SAND. PHOSPHATE IS PRESENT IN WELL CEMENTED RECRYSTALLIZED LIMESTONE WITH QTZ SAND. |
40 |
68 |
LIMESTONE |
|
LIGHT YELLOWISH ORANGE |
GOOD |
15 |
RECRYSTALLIZED LIMESTONE CONSISTING DOMINANTLY OF VERY FINE GRAINED, EUHEDRAL-ANHEDRAL, CALCITE CRYSTALS, SOME OF WHICH FORM FOSSIL MOLDS. RECRYSTALLIZATION, DOMINANTLY HIGH, RANGES FROM VERY LOW TO HIGH IN INTERVAL 50-73 FEET. GASTROPOD MOLDS PRESENT |
68 |
73 |
LIMESTONE |
|
|
|
|
ALSO CONTAINS 25% QTZ SAND NOT OBSERVED IN MATRIX. |
73 |
84 |
LIMESTONE |
|
LIGHT YELLOWISH ORANGE |
MODERATE |
25 |
40% FINE GRAINED QTZ SAND NOT OBSERVED IN MATRIX. DOMINANTLY RECRYSTALLIZED LIMESTONE. |
84 |
92 |
LIMESTONE |
|
LIGHT BROWNISH GRAY |
GOOD |
15 |
QTZ AND PHOSPHATIC SAND OBSERVED IN MATRIX. DOMINANTLY RECRYSTALLIZED LIMESTONE - COARSER GRAINED THAN ABOVE. |
92 |
106 |
LIMESTONE |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
PHOSPHATIC SILT <1%, 3% QTZ SAND NOT OBSERVED IN MATRIX. |
106 |
125 |
SANDSTONE |
|
LIGHT GRAY |
GOOD |
15 |
DOMINANTLY WELL INDURATED SPAR CALCITE CEMENTED SANDSTONES. PHOSPHATIC SILT 1% |
125 |
149 |
SANDSTONE |
|
GRAYISH ORANGE |
GOOD |
15 |
PHOSPHATIC SILT 1%, 60% OF INTERVAL IS UNCONSOLIDATED, POORLY SORTED QTZ SAND. |
149 |
157 |
SAND (QUARTZ) |
|
GRAYISH ORANGE |
GOOD |
25 |
70% OF SAMPLE IS UNCONSOLIDATED POORLY SORTED SAND SIMILAR TO THAT OBSERVED IN ROCK. PHOSPHATE SILT 1%. |
157 |
181 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
30 |
PHOSPHATED SILT 2%, ECHINOID SPINES, PLANKTONIC FORAMS. |
181 |
189 |
SAND (QUARTZ) |
|
LIGHT GREENISH GRAY |
UNCONSOLIDATED |
30 |
ECHINOID SPINES PRESENT. |
189 |
205 |
SAND (QUARTZ) |
|
LIGHT GREENISH GRAY |
UNCONSOLIDATED |
30 |
ECHINOID SPINES PRESENT. |
205 |
213 |
SILT |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
PHOSPHATIC SILT 1% |
213 |
215 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
25 |
THIS SAMPLE IS LABELED FROM 205-215 FOOT DEPTH. QTZ SAND FRACTION IS VERY FINE GRAINED. |
215 |
222 |
NO SAMPLE |
|
|
|
|
|
222 |
254 |
SILT |
|
YELLOWISH GRAY |
POOR |
20 |
ECHINOID SPINES PRESENT. |
254 |
262 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
ECHINOID SPINES PRESENT. |
262 |
278 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
ECHINOID SPINES PRESENT. |
278 |
286 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
20 |
|
286 |
292 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
30 |
ECHINOID SPINES PRESENT, <5% OF SAMPLE IS SPAR CALCITE CEMENTED. WELL ROUNDED QTZ SANDSTONE. |
292 |
300 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
|
300 |
308 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
|
308 |
316 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
30 |
|
316 |
322 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
|
322 |
330 |
SAND (QUARTZ) |
|
DARK YELLOWISH ORANGE |
UNCONSOLIDATED |
25 |
|
330 |
354 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
10% SHELL FRAGMENTS. |
354 |
370 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
20 |
25% OF SAMPLE IS A MODERATELY, WELL INDURATED, CALCILUTITE SANDSTONE. ECHINOID FRAGMENTS COMMON. |
370 |
418 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
ECHINOID FRAGMENTS, 20% SHELL FRAGMENTS, UP TO 10% MODERATELY INDURATED, CALCILUTITE CEMENTED QTZ SANDSTONE. MOST FOSSIL FRAGMENTS ARE RECRYSTALLIZED AND POSSIBLY REWORKED IN THE INTERVAL FROM 394-418. AVERAGE GRAIN SIZE INCREASES TO VERY COARSE GRAINED. |
418 |
448 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
|
448 |
488 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
30% OF SAMPLE IS GREYISH-OLIVE POORLY INDURATED MUDSTONE WITH QTZ SAND AND LITTLE METALLIC SPHERES. |
488 |
512 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
20 |
30% OF SAMPLE IS QTZ SAND SIMILAR TO ABOVE. |
512 |
520 |
LIMESTONE |
|
GRAYISH BROWN |
MODERATE |
20 |
RECRYSTALLIZED LIMESTONE. 35% OF SAMPLE IS MEDIUM-COARSE GRAINED SUBANGULAR QTZ SAND. |
520 |
528 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
|
528 |
536 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
|
536 |
544 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
RECRYSTALLIZED LIMESTONE. |
544 |
602 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
|
602 |
616 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
20 |
|
616 |
632 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
POOR |
25 |
|
632 |
664 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
10% RECRYSTALLIZED SHELL FRAGMENTS. |
664 |
688 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
25 |
|
688 |
696 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
25 |
|
696 |
704 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
704 |
712 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
25% OF SAMPLE RANGE IS PARTIALLY RECRYSTALLIZED. |
712 |
745 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
25 |
20-40% OF SAMPLE IS VERY FINE GRAINED, SUBANGULAR QTZ SAND. |
745 |
755 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
25 |
|
755 |
775 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
|
775 |
785 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
15% RECRYSTALLIZED FOSSIL SHELL FRAGMENTS. |
785 |
805 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
25 |
40% OF SAMPLE IS MEDIUM-COARSE GRAINED, SUBANGULAR QTZ SAND NOT OBSERVED IN MATRIX. 2% PHOSPHATIC SAND(POSSIBLE CAVINGS?) |
805 |
815 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
20 |
QTZ SAND NOT OBSERVED IN MATRIX. |
815 |
825 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
40% OF SAMPLE IS SUBANGULAR, MEDIUM-COARSE GRAINED QTZ SAND NOT OBSERVED IN MATRIX. |
825 |
885 |
LIMESTONE |
|
YELLOWISH GRAY |
POOR |
20 |
QTZ SAND CONTENT RANGES FROM 1-20%. NOT OBSERVED IN MATRIX. |
885 |
924 |
LIMESTONE |
|
VERY PALE ORANGE |
POOR |
25 |
RECRYSTALLIZATION RANGES FROM LOW TO INTERMEDIATE. |
924 |
944 |
LIMESTONE |
|
VERY PALE ORANGE |
MODERATE |
20 |
GASTROPOD MOLDS PRESENT. RECRYSTALLIZATION RANGES FROM NONE TO LOW |
944 |
965 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
UNCONSOLIDATED |
25 |
UNCONSOLIDATED CARBONATE SAND. QTZ SAND NOT IN MATRIX. |
965 |
976 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
POOR |
20 |
15% FRAGMENTS OF RECRYSTALLIZED LIMESTONE. |
976 |
987 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
MODERATE |
20 |
GASTROPOD MOLDS PRESENT. |
987 |
995 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
MODERATE |
20 |
RECRYSTALLIZATION RANGES FROM ZERO TO MEDIUM. |
995 |
1002 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
POOR |
20 |
|
1002 |
1017 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
MODERATE |
20 |
|
1017 |
1045 |
LIMESTONE |
|
LIGHT GREENISH YELLOW |
POOR |
25 |
|
1045 |
1053 |
LIMESTONE |
|
YELLOWISH GRAY |
MODERATE |
20 |
|
1053 |
1065 |
SAND (QUARTZ) |
|
GRAYISH ORANGE |
POOR |
20 |
RECRYSTALLIZED CARBONATE SAND GRAINS. |
1065 |
1140 |
LIMESTONE |
|
GRAYISH ORANGE |
MODERATE |
20 |
INTERVAL FROM 1065-1074 CONTAINS 15% CALCILUTITE CEMENTED LIMESTONE. |