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In 1851, gold was discovered along the Kern River in the southern Sierra Nevada, and in 1865, oil was discovered in the valley.The Bakersfield area, once a tule-reed-covered marshland, was first known as Kern Island to the handful of pioneers who built log cabins there in 1860.Bakersfield was spared, experiencing minor architectural damage without loss of life.A large aftershock occurred on July 29, and did minor architectural damage, but raised fears that the flow of the Friant-Kern Canal could be dangerously altered, potentially flooding the city and surrounding areas.
Explaining Prehistoric Variation in the Abundance of Large Prey: A Zooarchaeological Analysis of Deer and Rabbit Hunting along the Pecho Coast of Central California. Cotsen Institute Press, University of California, Los Angeles.]The Cross Creek-Diablo Canyon Complex of South Central California: Mid-latitude Pacific Foragers at the Pleistocene-Holocene Boundary. 2.]Another Trans-Holocene Sequence from Diablo Canyon: New Faunal and Radiocarbon Findings from CA-SLO-585, San Luis Obispo County, California. The earthquake, which measured 7.5 on the moment magnitude scale and was felt from San Francisco to the Mexican border, destroyed the nearby communities of Tehachapi and Arvin.The earthquake's destructive force also bent cotton fields into U shapes, slid a shoulder of the Tehachapi Mountains across all four lanes of the Ridge Route, collapsed a water tower creating a flash flood, and destroyed the railroad tunnels in the mountain chain.Aftershocks, for the next month, had become normal to Bakersfield residents, until August 22 at pm a 5.8 earthquake struck directly under the town's center in the most densely populated area of the southern San Joaquin Valley.Four people died in the aftershock, and some of the town's historic structures sustained heavy damage. communities to receive the All-America City Award from the National Civic League.