Pg. 21-23, pl. 1. Bennett Creek Breccia. Angular fragments of volcanic and sedimentary rocks embedded in tuff of quartz latite composition. Thickness 0 to 100 feet. Overlies Mojado Fcnmation with angular unconformity in some places and in others rests with erosional unconformity upon Timberlake Fanglomerate (new). Disconformably overlain by Basin Creek Tuff (new). At one locality near head of Bennett Creek formation overlies U-Bar Formation. Age is Tertiary.
Named from exposures south of Bennett Creek, [in N/2 of T. 31 S., R. 18 W.], Walnut Wells quadrangle, Hidalgo Co., southwestern NM.
Source: US geologic names lexicon (USGS Bull. 1350, p. 59).
Age modified from Tertiary to Oligocene on basis of position within a sequence of volcanic rocks that have been dated as Oligocene. Mapped (geologic map) at northern edge of map area, Pedregosa basin.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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