The Rio Bauta Member of the Pozas Formation, here named, consists of dark-gray and bluish-gray calcareous mudstone, siltstone, sandstone, conglomerate, and limestone that crop out in a restricted area of northern Orocovis quadrangle. Unconformably overlies volcanic rocks of the Rio Orocovis Group at the base of the Pozas; gradationally underlies the Blacho Tuff Member of the Pozas. Thickness is 100m. Age is late Santonian through Campanian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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