The Tesla Fault can be found in the northeastern Diablo Range, California. This fault is only semi-active.
Geology
This fault has been demonstrated to have a
dextral offset of and is closely associated with the Greenville Fault.
[Cotton, W.R., 1972, Preliminary geologic map of the Franciscan rocks in the central part of the Diablo Range, Santa Clara and Alameda Counties, California: U.S. Geological Survey Miscellaneous Field Studies Map MF-343 (Basic Data Contribution 39), 2 sheets, scale 1:62,500]
Mocho Subbasin
The Tesla Fault forms the eastern boundary of the large aquifer known as the
Mocho Subbasin. Some groundwater flow of the Mocho Subbasin occurs across the Tesla fault boundary, but flows are discontinuous below a depth of across the Tesla Fault.
[ Environmental Site Screening Analysis, 2127 Railroad Avenue, Livermore, California, Earth Metrics rpt no. 7785, San Mateo, Ca., Feb. 1989]
See also
External links
