Location and History On April 24, 1996 Canadas seventh largest case approximate range was established. It is called Wapusk matter commons (pronounced waa-pusk). Wapusk National Park protects 11,475 km2 of land. It is located at the northern edge of where Manitoba meets Hudson Bay. The primitive inhabitants of the region today are Inuit, Dene and Cree, the three nations who were trading in concert at this throng place long before the ovalbumin man discovered the riches of the new world. Ecozone Components The Wapusk National Park is located in the Hudson Plains ecozone. This field of study park is marked by short composed summers and very long cold winters. The sozzled annual temperature is nigh -4°C but usually ranging from -19°C to 10.5°C. The park is considered a cold desert, receiving only 12 inches of foolhardiness annually. The area of the national park is cover with tundra and boreal forests. along the coast and in the northern part of the national park , a treeless tundra of little arctic vegation such as willows, midget birch trees and cotton plant grass dominates, gradually giving way of life inland to an open woodland of vegetation characterized by legion(predicate) black merry and tamarack trees, moss and along the rivers a hook of white snappish woodland.
Wetlands occupy a lot of the national park with peeing system lying everywhere covering one-half of the lands get hold with lakes, bogs, fens, streams and rivers. The land is a young landscape where the body of water has been slow rising since the retreat of the last continental glaciers more or less 900 0 years ago continues to experience rising w! ater levels of intimately 1 metre per century. The soil consists of permafrost. The permafrost, or wintry arrogate of the tundra, begins about two feet down. It is ground that has been frozen for at least(prenominal) two years, supporting an upper layer... If you want to get a full essay, order it on our website:
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