The Carraizo Breccia, here named, includes rocks previously mapped by Kaye (1959) as Hato Puerco Tuff in the Aguas Buenas quadrangle and is restricted to that quadrangle. Consists of greenish- to reddish-gray porphyritic lava fragments in a fragmental matrix. A tuffaceous siltstone member may represent a tongue of the Guaynabo Formation. Stratigraphic relation to other units is obscure because it is isolated by faults. Maximum thickness is at least 1,400 m. Age is Late Cretaceous.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Carraizo Breccia occurs in eastern Puerto Rico and consists of pumiceous volcanic breccia and subordinate volcanic sandstone and tuffaceous siltstone and tuff. Minimum estimated thickness is 1400 meters. The Carraizo Breccia is of Late Cretaceous age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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