Imperial Formation

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Imperial Formation
Stratigraphic range:
1.) Canada: Devonian of Paleozoic Era.
2.) California: Pliocene of Cenozoic Era.
TypeTwo separate geologic formations
Underlies Palm Spring Formation (California)
Overlies Ocotillo Formation (California)
Location
Region1.) Northwest Territories,
Canada
2.) Colorado Desert,
Imperial County, California,
United States

The Imperial Formation is the name of two distinct and unrelated geologic formations in North America, of different geologic Eras.

Contents

Separate formations

Canadian Paleozoic Era formation

The older Imperial Formation occurs in the Northwest Territories of Canada. It preserves fossils dating back to the Devonian period of the Paleozoic Era. [1]

Californian Cenozoic Era formation

The younger Imperial Formation occurs in the Colorado Desert, in Imperial County of Southern California. It dates to the ZancleanLower Pliocene stage of the Pliocene Epoch, during the Neogene Period of the Cenozoic Era.

It underlies the Palm Spring Formation, and overlies the Ocotillo Formation. [2]

See also

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The Boas River Formation is a geologic formation in Northwest Territories. It preserves fossils dating back to the Ordovician period.

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The Headless Formation is a geologic formation in Northwest Territories. It preserves fossils dating back to the Devonian period.

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The Hume Formation is a geologic formation in the Northwest Territories, Canada. It preserves fossils dating back to the Devonian period.

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References

  1. Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database" . Retrieved 17 December 2021.; Paleozoic Era Canada.
  2. San Diego State University.edu: "Environments of deposition, Pliocene Imperial Formation, Southeast Coyote Mountains, Imperial County, California"; Bell, Patricia J.; 1980.