The Cibuco Formation, here named, consists of massive conglomerate in the lower part grading upward into thinner bedded conglomerate and volcanic clastic rocks. Lower contact is hidden by faulting; underlies and interfingers with lower beds of the Carreras Siltstone. Age is same as Carreras, Late Cretaceous or early Tertiary.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Cibuco Formation occurs in central Puerto Rico and consists of conglomerate with interbedded volcanic sandstone, siltstone, and tuff. Maximum known thickness is 2000 meters. The Cibuco is of Late Cretaceous(?) and Paleogene(?) age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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