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California aquifers, excerpted from map in Ground Water Atlas of the United States (USGS, 2000): Lavender is "other" for "rocks that generally yield less than 10 gal/min to wells"; dark green-blue (3) are the California coastal basin aquifers, bright-turquoise blue (7) is the Central Valley aquifer system, flat cobalt-blue (1) down south is Basin and Range aquifers
Midway Sunset Oil Field Geologic Cross Section The Lakeview #2 gusher (not the more famous Lakeview #1 gusher), 20 May 1914. While the Midway-Sunset field is a large contiguous area covering more than 30 square miles (80 km 2), it comprises 22 identifiable and separately-named reservoirs in six geologic formations, ranging in age from the Pleistocene Tulare Formation (the most recent ...
Standard Oil Company of California discovered the field in 1912 with the drilling of their Well No. 1, into the Etchegoin pool, to a depth of 2,836 feet (864 m). The well still exists, as Chevron Corp. Well No. 1. Peak production for the field was in 1929, during which 4,535,029 barrels (721,012.0 m 3) of oil were pumped from the ground. [7]
On-site California Historical Marker . California Oil and Gas Fields, Volumes I, II and III. Vol. I (1998), Vol. II (1992), Vol. III (1982). California Department of Conservation, Division of Oil, Gas, and Geothermal Resources (DOGGR). 1,472 pp. Kern River Oil Field information is on pp. 232–233. PDF file available on CD from www.consrv.ca.gov.
The Semitropic Oil Field is an oil and gas field in northwestern Kern County in California in the United States, within the San Joaquin Valley.Formerly known as the Semitropic Gas Field, it was discovered by the Standard Oil Company of California in 1935, and first understood to be primarily a natural gas reservoir; however, in 1956 a much deeper oil-bearing zone was discovered.
Coalinga Oil Field Map Coalinga Anticline Geologic Cross Section An idle oil well along Palmer Road, on Anticline Ridge in the eastern portion of Coalinga Oil Field.. The Coalinga Oil Field is the northernmost of a series of oil fields along anticlines extending along the western margin of the San Joaquin Valley, anticlines which parallel the San Andreas fault and have their origin in ...
The Long Beach field is notable for the thickness and depth of its oil-bearing formations; successively deeper wells continued to find oil even as late as the 1950s, with the deepest well finally hitting the basement rocks of the Catalina Schist at 14,950 feet (4,560 m) below ground surface. [8] [10]
Beverly Hills Oil Field Structure Map. The field is a faulted anticlinal structure with oil trapped by a combination of structural and stratigraphic mechanisms. Bounding the field on the south is the Brentwood-Las Cienegas Fault, and the field ends on the west near the Santa Monica Fault Complex.
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