Unit is named the Camas Valley Member (upper of two) of The Flournoy Formation (new) for exposures in Camas Valley, Douglas Co., OR. Also occurs in Flournoy Valley. Is composed of thin, rhythmically bedded, fine-grained, sandstone and siltstone with some thin limestone layers or limestone concretions. Is 1500 ft thick. Overlies the White Tail Ridge Member (new) of the Flournoy Formation; underlies the Tyee Formation. Age is middle Eocene based on microfossils.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Camas Valley Member of Flournoy Formation of Baldwin (1974) is included in Umpqua Group. [Author discusses reasons for raising rank of Umpqua Formation.]
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Camas Valley Member of the Flournoy Formation of Baldwin (1974) is reassigned as uppermost member (of 4) of Umpqua Formation. [members of Umpqua Formation are not adopted in this paper; Flournoy Formation is not recognized]
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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