FLORIDA GEOLOGICAL SURVEY


 F P EXPLANATION
 S F Number mcates depth to the top Norml fault
 of he Ocala Lnsbone in feet -u U=Upthrown side; D=D nlhfrown side
 below mean sea level
 Contour represents the top of the
 S -"- Ocala L nefoe an feet below Nolte All data from electric logs
 mean sea level. Cctour iterval I00 feet.
 SI I I I I 6I ,,,,
 0- 0 1 2 3 4 5 6 7 9 I Om1 Geolc/ by 0 T Marsh

 Figure 9. Map of Escambia and Santa Rosa counties showing contours on top of
 the lower limestone of the Floridan aquifer.



 AQUICLUDES

 Aquicludes within the sand-and-gravel aquifer.-As shown by the
geologic section along the Perdido River in Escambia County (fig. 8),
the sand-and-gravel aquifer contains discontinuous layers and lenses of
clay and sandy clay. The clay strata range in thickness from a few inches
to several tens of feet. For example, the clay bed mined by the Taylor
Brick and Tile Co., Inc., of Molino in Escambia County is about 50 feet