This field, 4 miles southeast of Bakersfield, was discovered in 1930 and again in 1933. Production is obtained in the lower Kern River or Chanac and Santa Margarita formations. Structurally the field is faulted monocline. It is 5 miles long and still growing both to the northwest and southeast. It averages 1/4 mile in width, and will probably be 1/2 mile wide when fully developed.

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