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Pages in category "Landforms of Saskatchewan" The following 16 pages are in this category, out of 16 total. This list may not reflect recent changes. A.
Landforms of Illinois by county (103 C) Bodies of water of Illinois (5 C) Wetlands of Illinois (2 C, 14 P) A. Algific talus slopes (3 P) Natural arches of Illinois (2 ...
The wealth of the state mainly arises from this abundance of soil and the favorable agrarian conditions it provides. Illinois is a major coal-producing state. Much of the bedrock surface is of Pennsylvanian age, including "cyclothemes", regular sequences of limestone, shale and coal layers. Newer rocks may have once existed in the State, but ...
The geography of Saskatchewan is unique among the provinces and territories of Canada in some respects. It is one of only two landlocked regions (Alberta is the other) and it is the only region whose borders are not based on natural features like coasts, lakes, rivers, or drainage divides.
The region covers an area of about 800,000 sq. km and expands across three Canadian provinces (Saskatchewan, Manitoba, and Alberta) and five U.S. states (Minnesota, Iowa, North and South Dakota, and Montana). The hydrology of the wetlands is variable, which results in long term productivity and biodiversity.
Landforms of Pope County, Illinois (1 C, 3 P) Landforms of Pulaski County, Illinois (1 C, 1 P) Landforms of Putnam County, Illinois (1 C, 1 P) R.
The location of the Province of Saskatchewan in Canada. The following outline is provided as an overview of and topical guide to Saskatchewan: . Saskatchewan – central prairie province in Canada, with an area of 588,276 square kilometres (227,100 sq mi), bounded on the west by Alberta, on the north by the Northwest Territories, on the east by Manitoba, and on the south by the U.S. states of ...
The Athabasca basin, a historical fluvial siliciclastic basin with sediments from the Hudsonian mountains with the occasional rare marine sequence. [16] [dead link ] The Athabasca basin was formed during the Statherian or Paleohelikian 1.7 to 1.6 billion years ago when coarse fluvial and marine clastic sediments were laid down containing gold, copper, lead, zinc, and uranium oxides.