The Barrancas Limestone Member, here named the basal unit of the Magueyes Formation, was described by Briggs and Gelabert (1962) as the limestone unit of formation L. Consists of 60 m of thick-bedded, dark-gray to black, highly fossiliferous, finely crystalline limestone with basal mudstone. Lies with structural conformity on volcanic rocks of formation L, underlies tuffaceous sandstone and siltstone of the Magueyes. Correlates with Torrecilla Breccia and with the Rio Maton Limestone Member of the Robles Formation. Age is Albian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Barrancas Limestone Member of the Magueyes Formation occurs in central Puerto Rico. Member occurs at base of formation and is of Early Cretaceous age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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