Pg. 13, (table 1), 21, pl. 2. Badito quartzite member of Hopewell series. Consists of bluish-gray qnartzite, unquestionably of sedimentary origin. At mouth of Picuris Canyon, it has been converted to quartz-muscovite schist. Age is Precambrian (Proterozoic).
Notable exposures in Picuris area along north side of Bio Pueblo gorge and in a long strip extending from mouth of Picuris Canyon across south and east spurs of Picuris Peak, Taos and Rio Arriba Cos., central northern NM.
Source: US geologic names lexicon (USGS Bull. 1200, p. 191).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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