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occurs throughout the valley floor portion of the Bernal
Subbasin under conditions ranging from unconfined to confined. There is no inflow of groundwater across the Pleasanton Fault south of the
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Groundwater in the Bernal
Subbasin typically occurs at an approximate depths of 12 to 30 feet (3.7 to 9.1 meters) below ground surface and flows from east to west.
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Projected impacts of injecting reclaimed, reverse osmosis water into the
Livermore-Amador Groundwater Basin
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Evaluation of
Groundwater Resources, Livermore and Sunol Valley, 1974
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moves toward the Bernal
Subbasin, which is bounded on the east by
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144:- westward flowing stream in Livermore and Pleasanton.
150:- groundwater subbasin in the Livermore Valley.
235:Bodies of water of Alameda County, California
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64:, United States. All of the groundwater in
255:Alameda County, California geography stubs
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156:- groundwater basin in Alameda County.
56:located in the southwestern corner of
250:Geology of Alameda County, California
122:Phase I Environmental Site Assessment
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245:Geography of Pleasanton, California
58:Livermore Valley Groundwater Basin
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126:, Report 7952W0.00, May 24, 1989
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183:. You can help Knowledge by
119:Earth Metrics Incorporated,
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177:Alameda County, California
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62:Alameda County, California
37:37.6664306°N 121.8981167°W
76:, and on the west by the
42:37.6664306; -121.8981167
82:Livermore Amador Valley
230:Aquifers in California
179:–related article is a
72:, on the north by the
110:Bonnie, Thomas L.,
86:Arroyo de la Laguna
50:The Bernal Subbasin
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96:City of Pleasanton
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70:Pleasanton Fault
66:Livermore Valley
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28:121°53′53.22″W
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25:37°39′59.15″N
185:expanding it
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92:Groundwater
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224:Categories
154:Niles Cone
74:Park Fault
136:See also
84:via the
54:aquifer
16:Aquifer
116:(2000)
52:is an
175:This
105:Notes
181:stub
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