U.S. Geological Survey Home AASG Logo USGS HOME CONTACT USGS SEARCH USGS
National Geologic Map Database
Geologic Unit: Cotui
Search archives
Map showing publication footprint
  • Usage in publication:
    • Cotui Limestone*
  • Modifications:
    • Principal reference
    • Revised
  • AAPG geologic province:
    • Caribbean region
Publication:

Volckmann, R.P., 1984, Upper Cretaceous stratigraphy of southwest Puerto Rico; a revision, IN Stratigraphic notes, 1983: U.S. Geological Survey Bulletin, 1537-A, p. A73-A83.


Summary:

The names San German Formation and its Cabo Rojo Agglomerate Member are here abandoned. The Cotui Limestone Member of the San German is here raised to formation rank as the Cotui Limestone. The rocks of the San German are assigned to the Cotui, the Lajas Formation, and the Sabana Grande Formation. The Cotui overlies the Lajas Formation with slight disconformity; conformably underlies the Sabana Grande Formation. Age is latest early Campanian through Maastrichtian. Brujo Limestone of Mattson (1960) is lithologically identical to and laterally continuous with the Cotui and is here abandoned; its rocks are assigned to the Cotui.
Type locality: exposures in Barrio Cotui along Road 314, 1.25 km south of Sabana Eneas, 350 m northeast and 150 m southwest of the intersection of Road 314 with an unnumbered road from the south.

Source: Modified from GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Cotui Limestone*
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Caribbean region
Publication:

Krushensky, R.K., 2001, Geologic map of Puerto Rico with correlation chart and map unit descriptions, IN Bawiec, W.J., and others, Geology, geochemistry, geophysics, mineral ccurrences, and mineral resource assessment for the Commonwealth of Puerto Rico: U.S. Geological Survey Open-File Report, OF-98-38, scale 1:100,000


Summary:

The Cotui Limestone occurs in southwestern Puerto Rico and consists of massive limestone with a local basal conglomerate containing clasts of lava from the underlying Lajas Formation. Maximum thickness is 75 meters. The Cotui is of Late Cretaceous age.

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).