Named Oso Canyon Formation. Rocks were formerly mapped as Santa Margarita Formation. Consists of coarse fluviatile sedimentary sequence of beds and intergradations of fanglomerate, conglomerate, sandstone, and siltstone. Maximum thickness is about 5,500 feet. Southwestward, the lower contact is gradational with the underlying Quail Lake Formation (new). Northeastward, Oso unconformably overlies Neenach Volcanic Formation (new) and unconformably overlies Mesozoic granite. Unconformably underlies Meeke Mine Formation (new). Age is late Miocene, based on relationship to Quail Lake Formation.
Named from Oso Canyon. Type section: from contact with Quail Formation 2/3 mi north of west end of Quail Lake, along line N. 20 deg. E. for 2 mi across Oso Canyon to contact with overlying Meeke Mine Formation [La Liebre Ranch and Lebec 7.5-min quadrangles, Los Angeles Co., CA].
Source: Modified from GNU records (USGS DDS-6; Menlo GNULEX).
Oso Canyon Formation of Dibblee (1967) is abandoned. Its rocks are here reassigned to the Santa Margarita Formation.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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