Fox Hills Formation

E364205

The Fox Hills Formation is a Late Cretaceous geologic unit in the Western Interior of North America, known for its marine to marginal-marine sandstones that record the final retreat of the Western Interior Seaway.

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All labels observed (1)

Label Occurrences
Fox Hills Formation canonical 1

Statements (49)

Predicate Object
instanceOf Late Cretaceous formation
geologic formation
stratigraphic unit
chronostratigraphicPosition Maastrichtian
contains ammonite fossils
bivalve fossils
marine invertebrate fossils
plant fossils
trace fossils
vertebrate fossils
depositionalSetting barrier-island complex
nearshore marine
regressive shoreline system
economicImportance groundwater aquifer in some regions
hydrocarbon reservoir in some basins
environmentOfDeposition deltaic
marginal-marine
marine
shoreface
exposedIn Colorado
Montana
North Dakota
South Dakota
Wyoming
geologicAge Late Cretaceous
hasStratigraphicThickness commonly tens to several hundreds of meters
lithology sandstone
shale
siltstone
locatedIn Canada
North America
United States of America
surface form: United States
namedFor Fox Hills, South Dakota
overlies Pierre Shale
paleogeographicSignificance marks transition from marine to continental deposition in Western Interior
records regression of Western Interior Seaway
partOf Western Interior Basin
records final retreat of the Western Interior Seaway
researchUse study of Cretaceous–Paleogene transition environments
stratigraphicGroup Colorado Group
Montana Group
varies regionally
underlies Frenchman Formation
Hell Creek Formation
Lance Formation
Laramie Formation
Medicine Hat Formation
Scollard Formation
Williston Basin
surface form: Williston Basin Paleocene units

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Hell Creek Formation overlies Fox Hills Formation