Santa Clara basalt. Named as seventh (and youngest) in a series of Quaternary formations in area. Santa Clara basalt and Bandelier rhyolite (new) tuff locally overlie Puye formation (new).
Occurs in Abiquiu quadrangle, Rio Arriba Co., north-central NM.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Santa Clara Pumice Bed of Bandelier Rhyolite of Tewa Group. Occurs at base of "middle" member of Bandelier Rhyolite, locally in Jemez Mountains, Bandelier National Park, Los Alamos County, New Mexico. Consists of pumice and pumice gravel. Thickness up to 100 feet. Is an apron of explosive rhyolite debris which nearly surrounds the eroded older "Chicoma" volcanics. Age is Pleistocene.
[GNU remark (USGS DDS-6; Denver GNULEX, June 1, 1987): Santa Clara Pumice Bed probably not a good unit. Not used by anyone else.]
Source: Modified from GNU records (USGS DDS-6; Denver GNULEX).
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