The Perchas Lava Member of the Rio Orocovis Formation, here adopted by the USGS, consists of massive amygdaloidal pillow lavas and thin lenticular layers of tuff, sandstone, and breccia. Gradationally overlies the Magueyes Member of the Rio Orocovis; unconformably underlies the Avispa Member in the south-central Ciales quadrangle. Thickness is 1,500 m. Age is Turonian(?) to late Santonian(?) or early Campanian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Rio Orocovis Formation redefined Rio Orocovis Group and Perchas Lava Member redefined Perchas Formation. Overlies the Magueyes Formation; conformably underlies the Avispa Formation.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Perchas Formation occurs in central Puerto Rico and consists of pillowed basaltic lava interbedded with basaltic tuff, volcanic sandstone, and minor hyaloclastite breccia. Unit is lithologically similar to the Magueyes Formation. Maximum estimated thickness is 1500 meters. The Perchas is of Cretaceous age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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