The Canabon Lava Member of the Robles Formation, here named in the Barranquitas quadrangle, consists of grayish-black augite phenocryst lava. Overlies the Las Tetas Lava Member near the top of the Robles. Age is Late Cretaceous.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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