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

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A<br />

Layer 1<br />

EXPLANATION<br />

<strong>Central</strong> <strong>Valley</strong> boundary<br />

Percentage of coarse-grained<br />

material > is greater than.<br />

0 to 10<br />

>10 to 20<br />

>20 to 30<br />

>30 to 40<br />

>40 to 50<br />

>50 to 60<br />

>60 to 70<br />

>70 to 80<br />

>80 to 90<br />

>90 to 100<br />

7,263 wells have logged data<br />

Wells having logged data<br />

11<br />

Western<br />

Sacramento<br />

0 50 100 Miles<br />

0 50 100 Kilometers<br />

Layer 1<br />

L<strong>and</strong> surface<br />

Not in model<br />

10<br />

Redding<br />

20<br />

Tracy/Delta-<br />

Mendota<br />

Enlarged area<br />

shown<br />

on figure 14<br />

12<br />

Eastern<br />

Sacramento<br />

21<br />

Westside<br />

22<br />

Northern<br />

San Joaquin<br />

Shaded relief derived from U.S. Geological Survey<br />

National Elevation Dataset, 2006. Albers Equal Area Conic Projection<br />

23<br />

Chowchilla-<br />

Madera<br />

Well locations<br />

24<br />

Kings<br />

Hydrogeology 31<br />

30<br />

Tulare/Kern<br />

Enlarged area<br />

shown<br />

on figure 14<br />

Figure A12. Kriged distribution of coarse-grained deposits for layers 1, 3, Corcoran Clay, 6, <strong>and</strong> 9 of the groundwater-flow model. Inset<br />

shows distribution of wells used in that depth interval.

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