DBHYDRO	reports

Lithologic Interval Details Well Name X-Coord (feet) Y-Coord (feet) W-17430 506265 1424699 Min. Depth (feet) Max. Depth (feet) Primary Rock % Primary Rock Primary Color Induration % Porosity Comments 0 10 SAND (QUARTZ) PALE BROWN UNCONSOLIDATED 30 RUDDY BROWN COLOR APPEARS TO BE DUE TO IRON STAIN 10 20 SAND (QUARTZ) DARK YELLOWISH BROWN POOR 25 20 40 SAND (QUARTZ) DARK YELLOWISH BROWN POOR 15 40 50 CLAY DUSKY BROWN MODERATE 15 POSSIBLE SAND LAMINATIONS POSSIBLE. POSSIBLE TOP OF MIOCENE HAWTHORN FORMATION 50 70 SAND (QUARTZ) DARK GRAYISH YELLOW UNCONSOLIDATED 30 70 100 SAND (QUARTZ) YELLOWISH GRAY UNCONSOLIDATED 30 MOST OF THE SAMPLE IS MILKY, UNCONSOLIDATED SAND. BUT SOME GRAY, CALCAREOUS, WELL-INDURATED FRAGMENTS (CALCILUTITE) 100 110 LIMESTONE YELLOWISH GRAY POOR 20 110 120 LIMESTONE YELLOWISH GRAY GOOD 13 120 160 LIMESTONE VERY PALE ORANGE POOR 20 160 190 LIMESTONE VERY PALE ORANGE POOR 20 DICTYOCONUS (FIRST). POSSIBLE TOP OF MIDDLE EOCENE AVON PARK FORMATION 190 260 LIMESTONE VERY PALE ORANGE POOR 17 DICTYOCONUS 260 270 LIMESTONE VERY PALE ORANGE UNCONSOLIDATED IDENTIFICATION OF FORAMINIFERA IS UNCLEAR 270 310 LIMESTONE VERY PALE ORANGE UNCONSOLIDATED FRAGMENTS OF DOLOSTONE AMONG CALCILUTITE. THE DOLOSTONE IS EUHEDRAL, DOMINANTLY MEDIUM-GRAINED, WITH RANGE POOR TO MEDIUM 310 320 LIMESTONE VERY PALE ORANGE UNCONSOLIDATED 20 APPROXIMATELY 15% OF FRAGMENTS ARE WELL-INDURATED AND DOMINANTLY RECRYSTALLIZED LIMESTONE. THE REST ARE UNCONSOLIDATED WACKESTONE. MOST OF THE ALLOCHEMS ARE DICTYOCONUS 320 330 LIMESTONE GRAYISH YELLOW UNCONSOLIDATED 17 DOLOSTONE EXISTS AS SEPARATE FRAGMENTS. DICTYOCONUS PRESENT, SOME OF WHICH APPEARS TO BE COOKEI Page generated at: 03-JUL-2024 06:42 EDT

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