Teutonia quartz monzonite is named for Teutonia Peak [T9N R13E, Cima Dome 7.5' quad], San Bernardino Co, CA, where typical exposures occur. Extends across southern part of study area, where it exceeds 250 sq mi in area. Consists of holocrystalline, light gray (fresh) to pale reddish-brown (weathered) quartz monzonite [using current classification of igneous rocks the composition is that of a granite.] Composed mostly of feldspar and quartz that range from 5 to 15 mm with sparse plates of biotite. Remainder of rock consists of coarse crystals of pale-reddish or pink orthoclase from 20 to 40 mm in diameter. Age is Late Cretaceous or early Tertiary [on map].
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age of the Teutonia Quartz Monzonite is Late Cretaceous based on isotopic dating (Pb-U).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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