Most complete section occurs below summit of Warren Peak [Warren Peak 7.5' quad, Modoc Co, CA]. Here 7 flows are composed of 300-ft thick andesite flow succeeded by 6 thin basalt flows. Uppermost flow is diktytaxitic and gray in color and can be traced down to vicinity of US HWY 395; it does seem to be continuous from Warren Peak down to table land north of Likely, CA (probably an example of a flood basalt). This flow is the Warner basalt of Russell (1928). Flows of this nature were named "Mesa Basalt" by Merriam (1910). Duffield [personal commun.] reports whole-rock K-Ar age of about 5 Ma on flow. Age of unit in study area (Warner Mountains) given as Tertiary.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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