Min.Depth(feet) |
Max.Depth(feet) |
Primary Rock |
%PrimaryRock |
Primary Color |
Induration |
%Porosity |
Comments |
10 |
70 |
SAND - SHELL |
|
|
|
|
ANASTASIA FORMATION - LOOSELY CONSOLIDATED SANDY LIMESTONE AND SHELL BEDS |
70 |
126 |
LIMESTONE |
|
|
|
|
TAMIAMI FORMATION - A SANDY AND SLIGHTLY PHOSPHATIC FOSSILLIFEROUS LIMESTONE |
126 |
240 |
CLAY |
|
|
|
|
HAWTHORN GROUP - UPPER PORTION IS A MASSIVE CLAY, LOWER INTERVAL IS SILT, SAND AND CLAY WITH VARYING AMTS OF PHOSPHATE. OVERALL SILTY CHARACTER (DOLOSILT) W/PHOSPHATE, SAND AND SOME CLAY AS ACCESSORY MINERALS |
240 |
380 |
LIMESTONE |
|
|
POOR |
|
OCALA FORMATION - MICRITIC AND BIOGENIC LIMESTONE WITH ABUNDANT BENTHIC FORAMINIFERA INCLUDING OPERCULINOIDES SP., LEPIDOCYCLINA SP. AND GYPSINA GLOBULA. |
380 |
550 |
LIMESTONE |
|
|
|
|
AVON PARK LIMESTONE UPPER INTERVAL. MUCH LIKE THE OCALA GROUP, MICRITIC, SOFT AND BIOGENIC CONTAINING THE GUIDE FOSSIL DICTYOCONUS COOKEI. |
550 |
680 |
DOLOMITE |
|
|
|
|
AVON PARK LIMESTONE LOWER PORTION - MUCH MORE DENSE THAN ABOVE DUE TO THE CRYSTALLINE DOLOMITES INTERBEDDED WITH RECRYSTALLIZED LIMESTONE |
680 |
|
DOLOMITE |
|
|
|
|
LAKE CITY LIMESTONE - PRIMARILY DESE AND ALTERED DOLOMITES WITH INTERBEDS OF MICRITIC AND RECRYSTALLIZED LIMESTONE IN THE UPPER PORTION |