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Central Valley Aquifer, Chapters A and B - MAE Class Websites

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A<br />

Coast Ranges<br />

Clayey<br />

lenses<br />

Fault<br />

Marine<br />

deposits<br />

River<br />

Potentiometric surface for the<br />

lower part of the aquifer system<br />

Old saline water<br />

Pumping wells<br />

Slough<br />

-<br />

<br />

<br />

<br />

-<br />

<br />

constitute more than 50 percent of the total thickness of the<br />

<br />

-<br />

2 <br />

<br />

Water<br />

movement<br />

Sierra Nevada<br />

Fresh-water<br />

recharge<br />

Lower part<br />

of the aquifer<br />

system<br />

Upper part<br />

of the aquifer<br />

system<br />

Bedrock<br />

Hydrogeology 21<br />

Figure A9. Pre- <strong>and</strong> post-development of the A, Sacramento <strong>Valley</strong>. B, <strong>Central</strong> part of the San Joaquin <strong>Valley</strong>, California. (Modified<br />

from Belitz <strong>and</strong> Heimes, 1990; <strong>and</strong> Galloway <strong>and</strong> others, 1999).<br />

Water<br />

table<br />

<br />

<br />

<br />

lacustrine deposit (Johnson <strong>and</strong> others, 1968) as much as 200<br />

). This

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