Pg. 463 (fig. 2), 466, pl. 1. Cano member of Mesaverde formation. Massive sandstone interbedded in Mancos shale. First massive sandstone characteristic of Mesaverde in area. Thickness increases southward from 25 feet in Arroyo Pinovetito to at least 225 feet southeast of Hogan. [Age is Late Cretaceous.]
[Present only in Tongue Valley, north-central NM.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 611).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
Asterisk (*) indicates published by U.S. Geological Survey authors.
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