The Camarones Sandstone, here named, was included in the Hato Puerco Tuff by previous writers. Consists of well-bedded, calcareous, dark-gray, thin-bedded tuffaceous siltstone interstratified with tuffaceous wacke and conglomerate. Includes the Mamey Lava Member. Base is indeterminate; interfingers with the Santa Olaya Lava; conformably underlies the Tortugas Andesite. Stratigraphically equivalent to the Rio de la Plata Sandstone. Maximum thickness is 680 m. Age is Late Cretaceous (Coniacian).
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Camarones Sandstone occurs in eastern Puerto Rico and consists of locally carbonaceous volcaniclastic siltstone interbedded with tuffaceous sandstone, and minor volcanic conglomerate, local lava flows. Maximum thickness is 950 meters. The Camarones is of Late(?) Cretaceous age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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