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Telsitna Formation

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Telsitna Formation
Stratigraphic range: Middle to Late Ordovician
TypeFormation
Unit ofNixon Fork terrane carbonate succession
UnderliesYounger Silurian carbonate and clastic units (locally unconformable)
OverliesNovi Mountain Formation
Lithology
PrimaryLimestone
OtherDolomite, Siltstone
Location
RegionKuskokwim Mountains, Alaska
CountryUnited States
ExtentWest-central Alaska (Nixon Fork terrane)
Type section
Named forTelsitna River region, Alaska
Named byDutro Jr. & Patton Jr. (1982)

The Telsitna Formation is a geologic formation in Alaska. It is part of the older rock record exposed in the Kuskokwim Mountains region, within the Nixon Fork terrane. The formation preserves evidence of an ancient shallow sea that once covered part of Alaska, recording a stage in the early Paleozoic development of the Laurentian northern margin.[1]

The formation consists mainly of carbonate rocks, such as limestone and related sediments that formed in a shallow tropical to subtropical sea. It sits above older Ordovician stratigraphic units and is overlain by younger Paleozoic features, reflecting a long history of changing sea levels and environments in the region.

See also

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References

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  1. J. Thomas Dutro; William W. Patton (1982). "Contributions to Stratigraphy H13" (PDF). Stratigraphic Notes. 13. Washington, D.C.: United States Geological Survey. Archived from the original (PDF) on 2017-02-08.