Named for Frenchie Creek as upper member of 3 of Pony Trail Group. Type section for group designated as Pony Trail Canyon in Frenchie Creek and Pine Valley 15' quads, Eureka Co, NV. Consists predominantly of maroon or black rhyolite and rhyodacite flows. Subordinate rock types include altered green and white flow breccias and scarce volcanic rocks. Thickness at type is about 2500 ft. Overlies Sod House Tuff (new) (Pony Trail Group). Cut by Lower Cretaceous plutons. Assigned Mesozoic age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Frenchie Creek Rhyolite in Cortez Mountains is considered Late Jurassic on basis of 151 +/-3 Ma age on biotite from unit (R.L. Armstrong, written commun., 1972). All three formations in Pony Trail Group, Big Pole Formation, Sod House Tuff, and Frenchie Creek Rhyolite, are now considered Jurassic and probably Late(?) Jurassic age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Mapped in Carlin-Pinon Range area. Rhyolite(?) plug in sec.32 T30N R51E forms extension of plug into this area from Frenchie Creek quad. Age is Late Jurassic based on 151 +/-3 Ma age (R.L. Armstrong, written commun., 1972) and time scale of Harland and others (1964).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Unit geographically extended in Elko Hills as shown on map. Age shown as Jurassic.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Pg. C5-C6; Geol. map of Elko Hills, Elko Co., NV, USGS Misc. Inv. Ser. Map I-2082, 1990. Frenchie Creek Rhyolite. Geographically restricted from the Elko Hills (as mapped by Coats, geol. map of Elko County, Nevada, 1987) and rocks are reassigned to informal unit (rhyodacite of Elko Mountain of Eocene age).
Source: Publication; GNU records (USGS DDS-6; Menlo GNULEX).
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