DBHYDRO       reports

Lithologic Interval Details

Well Name X-Coord
(feet)
Y-Coord
(feet)
W-10755 445735 930958

Min.
Depth
(feet)
Max.
Depth
(feet)
Primary Rock %
Primary
Rock
Primary Color Induration %
Porosity
Comments
0 5 NO SAMPLE REPORTEDLY A SAND , M-C GRAINED, ORGANIC, WITH NUMEROUS HAIR ROOTS. NO SAMPLE OBTAINED.
5 10 NO SAMPLE FINER GRAINED , LESS ORGANIC.
10 17 SAND (QUARTZ) LIGHT GRAY POOR SAND W/ SHELL FRAGMENTS AND LT. GY CLAY, STICKY, GLOBULAR DUE TO SAND ACCRETION AROUND CLAY FRACTION.
17 21 SHELL UNCONSOLIDATED PRACTICALLY PURE SHELL W/ MINOR QTZ SAND. NUMEROUS CHIONE AND TURRITELLA.
21 30 SHELL POOR MARLY, PROBABLY MORE INDURATED THAN ABOVE.
30 35 CLAY LIGHT GRAY POOR SOMEWHAT MOTTLED WITH TWO THIN SAND LENSES AT 30.5' AND 31'. CALCAREOUS IN UPPER PORTION WITH SOME SHELL FRAGS. PLASTICITY GOOD-EXCELLENT, INCREASING DOWNWARDS WITH DECREASING MACROCARBONATE. SLIGHTLY PHOSPHATIC. NUMEROUS "FORAMS".
35 35.5 CLAY BUT SLIGHTLY LESS PLASTICITY THAN 34-35' INTERVAL. FAIRLY RAPID CHANGE DOWNWARD TO DARKER GRAY. SLIGHTLY BLOCKY.
35.5 37.5 CLAY DARK GREENISH GRAY POOR GOOD PLASTICITY. NON CALCAREOUS.
37.5 39.5 CLAY GREENISH GRAY POOR SLIGHTLY CALCAREOUS AND SOME INCREASE IN PHOS. BUT PLASTICITY REMAINS VERY GOOD.
39.5 45.5 CLAY BUT VERY DARK GRAY AND PRACTICALLY NO CARBONATE.
45.5 52.5 CLAY AS 39.5-45.5'. WITH SOME HIGHLY PHOSPHATIC SAND LENSES BETWEEN 50-51'. LIGHTER GREENISH GRAY IN BOTTOM TWO FEET.
52.5 59.5 CLAY LIGHT GREENISH GRAY POOR AS 35.5-37.5'. BUT LIGHTER GREENISH GRAY, VERY CONSISTENT SECTION, ONLY VARIATION SEEMS TO BE A SLIGHT DARKENING TOWARD LOWER CONTACT.
59.5 64.8 CLAY
64.8 65 PHOSPHATE UNCONSOLIDATED PHOSPHORITE, WITH MOSTLY WELL ROUNDED, FROSTED, SAND GRAINS AND AMBER COLORED SPICULES, SOME FORAMS.
65 66 DOLOMITE MODERATE GRAY MED-DK GRAY MATRIX WITH LIGHTER CARBONATE INCLUSIONS, CONGLOMERATIC, DARK FRACTION 85-90% OF WHOLE, MATRIX APPEARS GLASSY UNDER 30X MAGNIFICATION.
66 67 LIMESTONE MODERATE LS CONGLOMERATE, WHITER INCLUSIONS SUB-ANGULAR TO WELL ROUNDED, BEACH ROCK APPEAREANCE OF OLD EROSION SURFACE, EFFERVESCES VIGOROUSLY IN DILUTE HCL AFTER POWDERING, THEREFORE PROBABLY HIGHLY DOLOMITIZED.

Page generated at: 03-JUL-2024 07:03 EDT

DBHYDRO Menu  |   DBHYDRO Home  |   SFWMD Home  |   User's Guide  |   What's New  |   FAQ |  Comments?