Bearpaw Formation

Bearpaw Formation

The Bearpaw Formation, also called the Bearpaw Shale, is a sedimentary rock formation found in northwestern North America. It is exposed in the U.S. state of Montana, as well as the Canadian provinces of Alberta and Saskatchewan, east of the Rocky Mountains. It overlies the older Two Medicine, Judith River and Dinosaur Park Formations, and is in turn overlain by the Horseshoe Canyon Formation in Canada and the Fox Hills Sandstone in Montana. To the east and south it blends into the Pierre Shale.

A marine formation composed mostly of shale, it represents the last major expansion of the Western Interior Seaway before it completely receded from northwestern North America by the end of the Cretaceous Period. The seaway had previously divided North America in half before orogeny (mountain-building) in the west uplifted the land and forced the seaway to retreat. As the uplift slowed down or ground to a halt in the late Campanian stage, around 74 million years ago, subsidence of the land allowed the seaway to invade once more. This northern expansion is often called the Bearpaw Sea. When the Laramide Orogeny resumed in the early Maastrichtian, the seaway retreated to the south for the final time. Because the sea did not disappear all at once, but instead slowly withdrew to the south, the Bearpaw Formation is superseded by the terrestrial sediments of the Horseshoe Canyon in Canada, while in Montana the Fox Hills Sandstone represents a near-shore marine environment. The Fox Hills too would be replaced by the terrestrial sediments of the Hell Creek Formation in Montana by the late Maastrichtian.

It is famous for its well-preserved ammonite fossils. Other fossils found in this formation include many types of shellfish, bony fish, sharks, rays, birds, and marine reptiles like mosasaurs, plesiosaurs and sea turtles. The occasional dinosaur remains have also been discovered, presumably from carcasses washed out to sea.

External links

* [http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:000966 Bearpaw Formation]
* [http://www.scn.org/~bh162/maas.html Latest Cretaceous Western Interior Seaway]
* [http://www.digitaldreammachine.com/sadrg/formation_bearpaw.html Bearpaw fauna in Alberta]


Wikimedia Foundation. 2010.

Игры ⚽ Поможем написать реферат

Look at other dictionaries:

  • Formation de Bearpaw — La flèche montre la transition entre la Formation de Bearpaw, en dessous, et la Formation de Horseshoe Canyon, au dessus. La Formation de Bearpaw est une formation de roches sédimentaires située dans le nord ouest de l Amérique du Nord. Elle… …   Wikipédia en Français

  • Formation de Horseshoe Canyon — Le canyon Horseshoe. Les bandes noires sont des couches de charbon. Localisation Coordonnées …   Wikipédia en Français

  • Formation de Dinosaur Park — Formation Dinosaur Park dans le Dinosaur Provincial Park en Alberta La Formation de Dinosaur Park (anglais : Dinosaur Park Formation) est une unité géologique du crétacé superieur de l Alberta et du Saskatchewan au Canada. Elle date du… …   Wikipédia en Français

  • Formation de Fox Hills — La Formation de Fox Hills est une formation géologique datant du Crétacé et située dans le nord ouest des Grandes Plaines en Amérique du Nord. On la trouve de l Alberta au nord jusqu au Colorado, au sud. Des restes de fossiles de dinosaures ont… …   Wikipédia en Français

  • Formation de Two Medicine — 48°04′27″N 112°17′58″O / 48.07417, 112.29944 (Two Medicine) …   Wikipédia en Français

  • Dinosaur Park Formation — Stratigraphic range: Late Cretaceous, 76.5–75 Ma …   Wikipedia

  • Oldman Formation — Stratigraphic range: Upper Cretaceous, 77.5–76.5 Ma …   Wikipedia

  • Horseshoe-Canyon-Formation — Die Horseshoe Canyon Formation an ihrer Typlokalität im Horseshoe Canyon, nahe Drumheller, Alberta. Die dunklen Bänder sind Kohleschichten. Die Horseshoe Canyon Formation ist eine Abfolge von Sedimentgesteinen der späten Kreidezeit, die in der… …   Deutsch Wikipedia

  • Two Medicine Formation — The Two Medicine Formation is a geologic formation, or rock body, that was deposited between 83.5 ± 0.7 Ma to 70.6 ± 0.6 Ma (million years ago), during Campanian (Late Cretaceous) time, and is located in northwestern Montana. It crops out to the… …   Wikipedia

  • Clearwater Formation — Stratigraphic range: Albian …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”