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Hanson Creek Formation

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Geologic formation in Nevada, United States
Hanson Creek Formation
Stratigraphic range: Dapingian-Katian (Ibexian-Richmondian)
488–444 Ma PreꞒ O S D C P T J K Pg N
TypeGeologic formation
UnderliesRoberts Mountains Formation
OverliesEureka Quartzite
Thickness350 feet (110 m)
Lithology
PrimaryLimestone
OtherDolomite, sandstone
Location
Coordinates39°00′N 116°00′W / 39.0°N 116.0°W / 39.0; -116.0
Approximate paleocoordinates7°06′S 74°30′W / 7.1°S 74.5°W / -7.1; -74.5
RegionNevada
Country United States
Type section
Named forHanson Creek
Hanson Creek Formation is located in the United StatesHanson Creek FormationHanson Creek Formation (the United States)Show map of the United StatesHanson Creek Formation is located in NevadaHanson Creek FormationHanson Creek Formation (Nevada)Show map of Nevada

The Hanson Creek Formation is a geologic formation in Nevada. It preserves fossils dating back to the Dapingian-Katian (Ibexian-Richmondian in the regional stratigraphy) stages of the Ordovician period.

See also

References

  1. Hanson Creek Formation at Fossilworks.org

Further reading

  • W. C. Sweet. 2000. Conodonts and Biostratigraphy of Upper Ordovician Strata Along a Shelf to Basin Transect in Central Nevada. Journal of Paleontology 74(6):1148-1160
  • G. W. Renz. 1990. Late Ordovician (Caradocian) radiolarians from Nevada. Micropaleontology 36(4):367-377
  • R. J. Elias. 1983. Late Ordovician solitary rugose corals of the Stony Mountain Formation, southern Manitoba, and its equivalents. Journal of Paleontology 57(5):924-956
  • R. J. Ross, Jr., T. B. Nolan, and A.G. Harris. 1980. The Upper Ordovician and Silurian Hanson Creek Formation of central Nevada. United States Geological Survey Professional Paper (1126-A-J)C1-C22
  • R. J. Rose, Jr., T. B. Nolan, and A. G. Harris. 1979. The Upper Ord. and Sil. Hanson Cr. Fm. of central NV. U.S. Geological Survey Professional Paper 1126C
  • R. J. Ross, Jr. 1970. Ordovician Brachiopods, Trilobites, and Stratigraphy in Eastern and Central Nevada. United States Geological Survey Professional Paper 639:1-99


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