Named for Swakane Creek, Entiat Mountains, Chelan quad, Cascade Range, central WA, area of finest occurrence. Consists of complex of remarkably foliated, highly metamorphic rocks, in part sedimentary and in part igneous. Biotite gneiss predominates; also includes granodiorite gneiss, amphibolite, amphibolite schist, marble, mica schist, and serpentine. Unconformably underlies Swauk formation of early Eocene age; intruded by Chelan batholith (probably Late Jurassic age). On basis of comparative metamorphism [with Peshastin formation] age of unit is pre-Ordovician.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Metamorphic age of Swakane Biotite Gneiss given as Late Cretaceous. Protolithic age shown as Precambrian.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Unit is geographically restricted from Lucerne 15' quad [see Cater and Wright (1967 -GQ-647)]. Its rocks in Lucerne 15' quad are reassigned to Skagit Gneiss Complex.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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