The Pleasanton Fault is a seismically active geological structure in Alameda County and Contra Costa County, California, USA. The existence of the fault is disputed as geotechnical reports have found no evidence for its existence.

Relation to hydrological features

All the streams draining Livermore Valley merge above the Bernal Subbasin and then leave the subbasin and the valley as the

Arroyo de la Laguna Arroyo de la Laguna is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed March 15, 2011 southward-flowing stream in Alameda County, California, United States which originates at the con ...

. Groundwater 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 City of Pleasanton. This consequence arises because any movement of groundwater in the southern section is essentially parallel to the Pleasanton Fault.Earth Metrics Incorporated, ‘'Environmental Site Assessment for the Hopyard Village Shopping Center, Pleasanton, California'‘, May 24, 1989

References

External links

Bulletin of the Seismological Society of America; December 1971; v. 61; no. 6; p. 1795-1799; 1971 Seismological Society of America, NATIONAL CENTER FOR EARTHQUAKE RESEARCH U. S. GEOLOGICAL SURVEY, MENLO PARK, CALIFORNIA
Seismic faults of California Geology of Alameda County, California Geology of Contra Costa County, California Livermore Valley Geography of Pleasanton, California Livermore, California Geography of the San Francisco Bay Area {{ContraCostaCountyCA-geo-stub

Relation to hydrological features

See also

References

External links