Santiago Canyon Tuff. Sample from Carson City area, Lat. 39 deg. 10 min. 33 sec. N., Long 119 deg. 38 min. 11 sec. W., in NE/4 SW/4 sec. 9, T. 15 N., R. 21 E., New Empire 7.5-min quadrangle, Nevada, yielded K-Ar ages of 22.8 +/-0.7 Ma (biotite) and 21.6 +/-0.9 Ma (sanidine). Age is Miocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Named for Santiago Canyon. Type section: exposures at mouth of Santiago Canyon, NW/4 sec.5 T15N R21E, New Empire 7.5' quad, NV. Reference sections: 1) Hackett Canyon sec.9 T15N R21E, New Empire 7.5' quad, 2) hill in W/2 NE/4 sec.20 T16N R20E, Virginia Range, Carson City 7.5' quad, NV. Is simple cooling unit of gray-white to gray sphene-bearing hornblende-biotite quartz latite crystal-vitric tuff. Is over 300 m thick. Disconformably overlies older Tertiary tuffs or unconformably overlies Mesozoic rocks; unconformably underlies Alta Formation. Is late Oligocene or early Miocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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