Crops out north of outlet of Clear Lake forming Kamiakan Butte and crops out along east side of Indian Creek at west end of Russell Ridge, Yakima Co, WA. 80% of lens-shaped body is amphibolite; is bounded on east and west by fault zones. Shown on geologic sketch map of White Pass region. Intruded by quartz diorite pegmatite dikes up to 4 inches wide on Kamiakan Butte and along Clear Lake fault zone. Has been metamorphosed twice. Age given as pre-Tertiary (although "mapped up to this time as a Tertiary intrusion" p.9).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Described as tectonic lens of interlayered amphibolitic, dioritic, and tonalitic gneiss, hornblendite, and lesser amount of quartz diorite pegmatite, cataclastic orthogneiss and mylonite. Emplaced as solid mass within Russell Ranch Formation. Age of amphibolite-grade metamorphism is about 155 Ma (Mattinson, 1972).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Rocks of Russell Ranch Formation are in fault contact with amphibolitic metagabbros, metadiabases, and gneissose quartz diorites of Indian Creek Gneiss [referring to pre-Cenozoic unit of Ellingson, 1972]. Metamorphic age given as about 155 Ma or Late Jurassic (Mattinson, 1972).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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