Named [presumably for Cowlitz River, in order to accommodate a fauna] "seemingly older than typical Tejon [which] may represent a transition from the Martinez to the Tejon --a fauna which as yet is unknown in California. In order to distinguish this [fauna] from the typical Tejon, the term Cowlitz formation is suggested." [no type given] Occurs in southern Lewis Co, WA, east of Little Falls. Composed of sandstone, shale, conglomerate, and subordinate amounts of shaly limestone together with numerous intercalated layers of tuff and basaltic lava. Is at least 500 ft thick; base not exposed. List of megafossils included in report. Age is late Eocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Type section measured in canyon of Olequa Creek between towns of Winlock and Olequa, [a distance of about 8.5 mi in southwestern Lewis Co and northwestern Cowlitz Co, WA]. Thickness at type is 3745 ft. Overlain by Oligocene Keasey formation; basal contact not exposed. Fauna ... "seems to represent the uppermost division of the Eocene ... but may not extend upward to the very top of Eocene time."
Source: GNU records (USGS DDS-6; Menlo GNULEX).
[Cowlitz formation not separately delineated on reconnaissance geologic map]. Exposed along Nehalem River (where it is approximately 950 ft thick) and also exposed along Wolf Creek HWY. Megafossil fauna is sufficient to "separate the Cowlitz fauna from younger faunas". Age is late Eocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Type locality of Cowlitz formation is redefined to include more than 8000 ft of sedimentary and subordinate volcanic rocks exposed along Stillwater and Olequa Creeks as far south as Cowlitz River, southwestern WA. In lower Cowlitz River-eastern Willapa Hills area Cowlitz is subdivided into four closely related, some interfingering members representing different lithofacies of Cowlitz. Members include: Stillwater Creek member (new), Olequa Creek member (new). Goble volcanics member, and Pe Ell volcanics member (new) Fossil lists and petrographic study of volcanic rocks included in report.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age is middle and late Eocene based on foraminifers.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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