Lotta Creek Tuff Member of Franciscan Formation. White crystalithic tuff and interbedded dark-green siliceous shale at headwaters of Lotta Creek. About 900 feet of strata exposed between lower fault contact with Del Puerto Keratophyre Member and upper conformable contact with Knoxville(?) Formation. Though contact is faulted at exposures, regional structural relationships indicate that Lotta Creek rocks directly overlie those of the Del Puerto. Age is Late Jurassic.
Well exposed along headwaters of Lotta Creek in sec. 21, T. 6 S., R. 6 E., Stanislaus Co., central CA.
Source: US geologic names lexicon (USGS Bull. 1350, p. 441).
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