BA.r1.". :0 Nrr FiCAMPA C*I Nr AAJT.1 SAY A A P CCOh0,fr I :0U.Ir fA ;, '
 ,ASll A &a AI I IA i

 0- OAP Ili -L 0
 SAN 0 ANiD -- GRAVEL AQUIFER Yea 000
2 00- .-- ... .......... 2.00
60020
 000 M C~ N~ ~ ...-...........Dc
 400F 400
 6- 000 150




 240
 800- Y eOO
 1000 C( E AOLFR uIFFRi~lo
 S12600
14 00- NQIIAI o200
 M30t 0 r 0014
 41500iiAN AWUFER
 leoo O,,LtOE 5a J OIAS OFN F LOR10N 10
t,2000- jp? L~C 00
 t~2OWLVER C~Y2200

 2600i~LE: 20
 2800.-21BO
 3000-i
 y I;ie a to s r 3000
WOO-anr


 EXPLANATION
 LInqI' at I soila 11 miles
V4nPIrhcal gaqq..afn aaut 52 tinns
-UMneformity


 Well inclane dl?0 ton4 ci
 1.01cna along lstre cd beai


 0 0 20 30miles
 Map rsnownq COi,,c aof cross uthan R-*R

Figure 7. Geologic section along the Gulf Coast from Mobile Bay to the Choctaw-
 hatchee River showing aquifers and aquicludes.


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