Gracias Formation

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Gracias Formation
Stratigraphic range: Miocene
Type Formation
Underlies Pleistocene basalt
Overlies Padre Miguel Group
Thickness200–300 m (660–980 ft)
Lithology
Primary Sandstone, siltstone, claystone
Other Conglomerate
Location
Coordinates 21°12′N100°42′W / 21.2°N 100.7°W / 21.2; -100.7
Approximate paleocoordinates 21°42′N98°00′W / 21.7°N 98.0°W / 21.7; -98.0
Region Lempira Department
Country Honduras
Type section
Named for Gracias
Named byWilliams & McBirney
Year defined1969
Relief map of Honduras.jpg
Yellow pog.svg
Gracias Formation (Honduras)

The Gracias Formation is a geologic formation in Honduras. The mainly sandstones, siltstones and claystones preserve vertebrate fossils dating back to the Neogene period. [1]

Contents

Description

The Gracias Formation is a sedimentary unit, consisting of sandstone, siltstone, claystone and a few conglomeratic beds. The formation crops out in western Honduras and ranges from 200 to 300 metres (660 to 980 ft) in thickness. The formation overlies the Padre Miguel Group, while it is overlain by Pleistocene basalts. [2] The Padre Miguel Group provided the provenance for the sedimentary material for the Gracias Formation. The clasts in the formation are largely composed of rhyolite, rhyodacite, pumice, vitric ash, quartz, feldspar, and minor biotite fragments. [3]

Fossil content

See also

References

  1. Gracias Formation at Fossilworks.org
  2. N.N., s.a., Informe de Apoyo, A-9
  3. Sánchez Barreda, 1999, p.25
  4. Hulbert, 1988, p.272

Bibliography

Further reading