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Thermopolis Shale information


Thermopolis Shale
Stratigraphic range: Late Albian, ~103–98.5 Ma
PreꞒ
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S
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Pg
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TypeFormation
Unit ofColorado Group and Dakota Formation
Sub-unitsUpper Thermopolis Member, Muddy Sandstone Member, Lower Thermopolis Member, "Rusty Beds" Member
UnderliesMowry Shale
OverliesKootenai Formation (Cloverly Formation equivalent)
Thickness320 to 450 feet (100 to 140 m)
Lithology
PrimaryShale
OtherBentonite, Claystone, Lignite, Mudstone, Sandstone, Siltstone
Location
RegionWestern Interior Basin
CountryUnited States
Type section
Named forThermopolis, Wyoming
Named byCharles T. Lupton
LocationBig Horn County, Wyoming
Year defined1916
Coordinates44°32′N 107°59′W / 44.53°N 107.99°W / 44.53; -107.99
CountryUnited States

The Thermopolis Shale is a geologic formation which formed in west-central North America in the Albian age of the Late Cretaceous period. Surface outcroppings occur in central Canada, and the U.S. states of Montana and Wyoming. The rock formation was laid down over about 7 million years by sediment flowing into the Western Interior Seaway. The formation's boundaries and members are not well-defined by geologists, which has led to different definitions of the formation. Some geologists conclude the formation should not have a designation independent of the formations above and below it. A range of invertebrate and small and large vertebrate fossils and coprolites are found in the formation.

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