Aguadilla limestone shown on correlation chart as subdivision of Arecibo formation. Overlies Lares limestone, underlies Quebradillas limestone. Age is Oligocene. Maury (1919b) changed age to early Miocene.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Sediments ranging from coarse bouldery gravel through sand, silt, clay, and marl to pure limestone, characterized by rapid lateral changes in lithology and intergrading both horizontally and vertically, are named the Rio Guatemala group. The San Sebastian formation represents the first interval of clastic deposition; the Lares limestone represents biohermal areas; and the Cibao marl with its Guajataca member represents the second interval of clastic deposition. Maximum thickness is 700 m. Unconformably overlies rocks of Late Cretaceous age; conformably underlies Aguada limestone. Age is Tertiary.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Lares Limestone occurs on the north coast of Puerto Rico and consists of calcilutite, locally, and hard calcilutite interbedded with chalky limestone and calcareous clay. Maximum estimated thickness is 270 meters. The Lares is of late(?) Oligocene age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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