Central Valley Aquifer, Chapters A and B - MAE Class Websites
Central Valley Aquifer, Chapters A and B - MAE Class Websites Central Valley Aquifer, Chapters A and B - MAE Class Websites
24 Groundwater Availability of the Central Valley Aquifer, California A B 10 S a c r a m e n t o V a l l e y 11 Sacramento River 12 EXPLANATION Textural analysis spatial provinces and domains Number Name 10 11 12 20 21 22 23 24 30 Redding Western Sacramento Eastern Sacramento Tracy/Delta-Mendota Westside Northern San Joaquin Chowchilla-Madera Kings Tulare/Kern Stream or river Orestimba Creek S a n J o a q u i n V a l l e y San Joaquin River 20 22 0 50 100 Miles 0 50 100 Kilometers Shaded relief derived from U.S. Geological Survey National Elevation Dataset, 2006. Albers Equal Area Conic Projection Merced River Bear Creek 21 23 24 Kings River 30 10 11 12 20 21 22 23 24 30 0 50 EXPLANATION Textural analysis spatial provinces and domains Number Name Redding Western Sacramento Eastern Sacramento Tracy/Delta-Mendota Westside Northern San Joaquin Chowchilla-Madera Kings Tulare/Kern Well used for texture analysis 0 50 100 Kilometers 100 Miles Figure A10. A, Central Valley showing groundwater basins and subbasins, groupings of basins and subbasins into spatial provinces and domains for textural analysis. B, Distribution of wells used for mapping texture. C, Count of wells for each depth increment by domains through 1,200 feet. Because less than 1 percent of the logs extend past 1,200 feet, increments below 1,200 feet were not shown. Detailed description of the spatial provinces and domains are in .
C DEPTH TO MIDPOINT OF INCREMENT, IN FEET BELOW LAND SURFACE 0 50 100 150 200 250 300 350 400 450 500 550 600 650 700 750 800 850 900 950 1,000 1,050 1,100 1,150 Selection and Compilation of Existing Well Data - - ated on the basis of the amount of detail in the descriptions - NUMBER OF WELLS USED FOR TEXTURE ANALYSIS EXPLANATION Number of wells, colored by basin Number Name 10 Redding Hydrogeology 25 - - - - 11 12 20 21 22 23 24 30 Western Sacramento Eastern Sacramento Tracy/Delta-Mendota Westside Northern San Joaquin Chowchilla-Madera Kings Tulare/Kern 1,200 0 500 1,000 1,500 2,000 2,500 3,000 3,500 4,000 4,500 5,000 5,500 6,000 6,500 7,000 7,500 Figure A10. Continued.
- Page 1 and 2: GROUNDWATER RESOURCES PROGRAM Groun
- Page 3 and 4: Groundwater Availability of the Cen
- Page 5 and 6: Foreword An adequate supply of grou
- Page 7 and 8: Contents Chapter A Introduction, Ov
- Page 9 and 10: Chapter C Numerical Model of the Hy
- Page 11 and 12: Figures Chapter A Figure A1. Map of
- Page 13 and 14: Figure B12. Map of altitude of the
- Page 15 and 16: Figure C28. Pie chart and histogram
- Page 17 and 18: Conversion Factors Inch/Pound to SI
- Page 19 and 20: Chapter A. Introduction, Overview o
- Page 21 and 22: - - precipitation. -
- Page 23 and 24: 40° 39° 38° 37° 36° 35° Klama
- Page 25 and 26: Texture Model DATA Centralized Geos
- Page 27 and 28: Hydrology Water Well Information Aq
- Page 29 and 30: Table A1. Water-balance subregions
- Page 31 and 32: B Red Bluff 0 50 100 Miles 0 50 100
- Page 33 and 34: Delta and Eastside Streams ).
- Page 35 and 36: for about 30 percent of the annual
- Page 37 and 38: 0 50 100 Miles 0 50 100 Kilometers
- Page 39 and 40: A Coast Ranges Clayey lenses Fault
- Page 41: - the distribution of these pro
- Page 45 and 46: ). The southern part, referred , in
- Page 47 and 48: 3-D Model of Percentage of Coarse-G
- Page 49 and 50: A Layer 1 EXPLANATION Central Valle
- Page 51 and 52: C Layer Corcoran Clay EXPLANATION C
- Page 53 and 54: E Layer 9 EXPLANATION Central Valle
- Page 55 and 56: Geomorphic province— Basin Delta
- Page 57 and 58: San Joaquin Valley ),
- Page 59 and 60: - Water supplied from aquifers
- Page 61 and 62: C Figure A16. Continued. 3.54% 5.45
- Page 63 and 64: CUMULATIVE DEPARTURE OF PRECIPITATI
- Page 65 and 66: CUMULATIVE DEPARTURE OF STREAMFLOW
- Page 67 and 68: 700 500 600 400 200 160 0 50 100 Mi
- Page 69 and 70: B 0 50 100 Miles 0 50 100 Kilometer
- Page 71 and 72: Water Budget per year (
- Page 73 and 74: References Cited 55 -
- Page 75: References Cited 57 - - 2009, at
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C<br />
DEPTH TO MIDPOINT OF INCREMENT, IN FEET BELOW LAND SURFACE<br />
0<br />
50<br />
100<br />
150<br />
200<br />
250<br />
300<br />
350<br />
400<br />
450<br />
500<br />
550<br />
600<br />
650<br />
700<br />
750<br />
800<br />
850<br />
900<br />
950<br />
1,000<br />
1,050<br />
1,100<br />
1,150<br />
Selection <strong>and</strong> Compilation of Existing Well Data<br />
<br />
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<br />
<br />
<br />
<br />
<br />
<br />
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<br />
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-<br />
<br />
-<br />
<br />
ated<br />
on the basis of the amount of detail in the descriptions<br />
-<br />
<br />
NUMBER OF WELLS USED FOR TEXTURE ANALYSIS<br />
EXPLANATION<br />
Number of wells,<br />
colored by basin<br />
Number Name<br />
10 Redding<br />
Hydrogeology 25<br />
<br />
<br />
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-<br />
-<br />
<br />
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-<br />
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-<br />
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<br />
11<br />
12<br />
20<br />
21<br />
22<br />
23<br />
24<br />
30<br />
Western Sacramento<br />
Eastern Sacramento<br />
Tracy/Delta-Mendota<br />
Westside<br />
Northern San Joaquin<br />
Chowchilla-Madera<br />
Kings<br />
Tulare/Kern<br />
1,200<br />
0 500 1,000 1,500 2,000 2,500 3,000 3,500 4,000 4,500 5,000 5,500 6,000 6,500 7,000 7,500<br />
Figure A10. Continued.