Fox Hills Formation

Geologic formation in the Great Plains of North America From Wikipedia, the free encyclopedia

The Fox Hills Formation is a Cretaceous geologic formation in the northwestern Great Plains of North America. It is present from Alberta on the north to Colorado in the south.

Unit ofMontana Group (MT, ND)
Sub-unitsFairpoint member (SD),
Trail City member (ND, SD),
Timber Lake (ND, SD),
Lincoln member (CO), etc.
UnderliesLance (WY)/Hell Creek (MT)[1]
Laramie Formation (CO)
Quick facts Type, Unit of ...
Fox Hills Formation
Stratigraphic range: Late Cretaceous, Maastrichtian
A ridge capped by a sandstone bed of the Fox Hills Formation west of Limon, Colorado
TypeGeological formation
Unit ofMontana Group (MT, ND)
Sub-unitsFairpoint member (SD),
Trail City member (ND, SD),
Timber Lake (ND, SD),
Lincoln member (CO), etc.
UnderliesLance (WY)/Hell Creek (MT)[1]
Laramie Formation (CO)
OverliesPierre (USA)/Bearpaw (CAN)[1]
Lewis Shale (WY, MT)[1]
Thickness75-225 feet
Lithology
PrimarySandstone
OtherShale
Location
RegionAlberta, Colorado, Montana, North Dakota, South Dakota and Wyoming
CountryUnited States/Canada
Type section
Named forFox Hills between Cheyenne and Moreau Rivers, South Dakota
Named byMeek and Hayden[1]
Year defined1862[1]
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Fossil remains of dinosaurs, including tyrannosaurs, as well as large marine reptiles, such as mosasaurs, have been recovered from the formation.[2]

Lithology

The Fox Hills Formation consists of marginal marine yellow to grey sandstone with shale interbeds.[1][3] It was deposited as a regressive sequence of barrier islands during the retreat of the Western Interior Seaway in Late Cretaceous time. [4] In its eastern extent, the formation is underlain by the marine Pierre Shale in the United States and by the equivalent Bearpaw Formation in Canada, while in western ranges in Montana and Wyoming it overlies the Lewis Shale. The Fox Hills is overlain by continental sediments of the Laramie Formation in Colorado and the Lance Formation in Wyoming, the latter being the equivalent of the overlying Hell Creek Formation in Montana.[1]

Fossil content

Plants

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
More information Taxa, Species ...
TaxaSpeciesLocalityMaterialNotesImages
Marmarthia M. johnsonii Belongs to Lauraceae, similar to Lindera.[5]
Mesocyparis M. borealis Belongs to Cupressaceae, similar to Thuja.[5]
Nilssoniocladus N. comtula A Cycaceoid.[5]
N. yukonensis [5]
Paloreodoxites P. plicatus Incertae sedis, a palm-like monocot.
Rhamnus R. salicifolius Similar to R. caroliniana.[5]
Zingiberopsis Z. magnifolia Belongs to Zingiberaceae, related to Alpinia.[5]
Cornus C. sp A Dogwood.[5]
Cercidiphyllum C. ellipticum A katsura.[5]
Asimina A. knowltonia A pawpaw.[5]
Paranymphaea P. hastata A water lily.[5]
Platanites P. marginata A sycamore (plane tree).
Metasequoia M. sp A Dawn redwood.[5]
Glyptostrobus G. sp A Swamp Cypress.[5]
Taxodium T. olrikii A bald cypress, also found in Hell Creek.[5][6]
Osmunda O. hollicki A royal fern.[5]
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Mollusks

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
More information Taxa, Species ...
TaxaSpeciesLocalityMaterialNotesImages
Palaeocypraea[7] P.squyeri
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See also

References

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