The Cambalache Formation, here named, consists of andesitic volcanic breccia, sandstone, and mudstone characterized by altered pumice and perlite. Includes the Toma de Agua Vitrophyre Member, 0 to 50 m thick, at the top of the formation. Vitrophyre is black, vitreous, with columnar jointing. Conformably overlies the Hato Puerco Formation; sharply and conformably underlies the Canovanas Formation. Thickness averages 350 to 450 m, up to 600 m. Age is Late Cretaceous (Turonian) based on fossils.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Cambalache Formation occurs in eastern Puerto Rico and consists of pumiceous volcanic breccia, sandstone, mudstone, and locally, welded ash-flow tuff. Maximum thickness is 600 meters but is typically 350 to 450 meters. The Cambalache is of Late Cretaceous age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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