| Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
| 0 |
1.5 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
|
ORGANICS AND PLANT REMAINS DECREASE WITH DEPTH. |
| 1.5 |
7.8 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
POOR |
|
CLAY VARIES 2-15%. CLAY CONCENTRATED IN LENSES. CLAY IS ORGANIC RICH. HYDRAULIC CONDUCTIVITY TESTED AT 7.5'. AVERAGE K: 7.79E-04 CM/SEC OR 2.21E+00 FT/DAY. |
| 7.8 |
9.8 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
POOR |
|
INTERVAL WAS PUMPED. CLAY VARIES 1-5%. CLAY CONCENTRATED IN BLEBS. |
| 9.8 |
11 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS BAILED. |
| 11 |
12.5 |
SAND (QUARTZ) |
|
|
|
|
INTERVAL WAS BAILED. |
| 12.5 |
13.5 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS BAILED. |
| 13.5 |
16.3 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
POOR |
|
INTERVAL WAS BAILED. SOME CLAY IS CONCENTRATED IN BLEBS. |
| 16.3 |
18.3 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS BAILED. SOME CLAY IS CONCENTRATED IN BLEBS. |
| 18.3 |
18.8 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
|
A FEW BLEBS OF ORGAINC RICH CLAY. HYDRAULIC CONDUCTIVITY TESTED AT 18.5'. AVERAGE K: 1.36E-03 CM/SEC OR 3.86E+00 FT/DAY. |
| 18.8 |
20.5 |
SAND (QUARTZ) |
|
VERY LIGHT GRAY |
POOR |
|
INTERVAL WAS BAILED. SOME ORGANIC RICH CLAY IN BLEBS. |
| 20.5 |
23.5 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
|
INTERVAL WAS BAILED. |
| 23.5 |
26 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. |
| 26 |
29.5 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS PUMPED. LAYER OF ORGANIC RICH CLAY NEAR BASE OF INTERVAL. |
| 29.5 |
32.5 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. |
| 32.5 |
34 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. |
| 34 |
35.8 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS PUMPED. SOME CLAY IN BLEBS. |
| 35.8 |
38.5 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
POOR |
|
INTERVAL WAS PUMPED. SOME CLAY IN BLEBS. |
| 38.5 |
41 |
SAND (QUARTZ) |
|
VERY PALE ORANGE |
POOR |
|
INTERVAL WAS PUMPED. CLAY MOSTLY IN BLEBS. |
| 41 |
43 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
POOR |
|
CLAY AND ORGANICS CONCENTRATED IN BLEBS AND LENSES. |
| 43 |
45.5 |
SAND (QUARTZ) |
|
LIGHT GRAY |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. CLAY IS IN SMALL BLACK BLEBS. |
| 45.5 |
47 |
SAND (QUARTZ) |
|
GRAYISH BROWN |
UNCONSOLIDATED |
|
POOR SAMPLE RECOVERY. NO VIABLE HYDRAULIC CONDUCTIVITY SAMPLE RECOVERED. |
| 47 |
48.5 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
|
|
| 48.5 |
50 |
SAND (QUARTZ) |
|
LIGHT GRAY |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. HYDRAULIC CONDUCTIVITY TESTED AT 48.5'. AVERAGE K: 4.96E-03 CM/SEC OR 1.41E+01 FT/DAY. |
| 50 |
51 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
|
|
| 51 |
51.5 |
SAND (QUARTZ) |
|
YELLOWISH GRAY |
POOR |
|
|
| 51.5 |
52.5 |
NO SAMPLE |
|
|
|
|
|
| 52.5 |
55.5 |
SAND (QUARTZ) |
|
VERY LIGHT GRAY |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. CLAY IS IN BLEBS. |
| 55.5 |
58 |
SAND (QUARTZ) |
|
|
|
|
INTERVAL WAS PUMPED. |
| 58 |
60.5 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
UNCONSOLIDATED |
|
INTERVAL WAS PUMPED. |
| 60.5 |
66 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
UNCONSOLIDATED |
|
PUMPED SAMPLE (CUTTINGS) MOST SAMPLE RECOVERED IS SLIGHTLY SHELLY SAND WITHOUT MATRIX. SOME RECOVERED AS CLASTS OF CLAYEY SHELLY SAND-PROBABLY THE ACTUAL LITHOLOGY. |
| 66 |
69 |
SAND (QUARTZ) |
|
LIGHT OLIVE GRAY |
POOR |
|
INTERVAL WAS PUMPED. ABUNDANT CLASTS OR BLEBS OF CLAYEY SHELLY SAND RECOVERED-PROBABLY THE ORIGINAL BULK LITHOLOGY. |
