CGC 1D1 Mr. Zapfe.  Final changes occurred which gave Canada’s landforms their present shape  Continuing collision of North American and Pacific Plates.

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Presentation transcript:

CGC 1D1 Mr. Zapfe

 Final changes occurred which gave Canada’s landforms their present shape  Continuing collision of North American and Pacific Plates completed the formation of the Rocky Mountains  During the last 2 million years, Canada and much of the world experienced an Ice Age

 Ice sheets cover much of North America  Human beings develop  Age of mammals  Modern forms of life evolve

 Period of time when freezing temperatures created ice sheets across the continents

 The ice age created huge masses of ice called glaciers  As glaciers moved, their actions were like giant earth-moving machines, scraping and gouging the land they covered

 Like the forces of erosion, the movement of glaciers carves and gouges the landscape, but also deposits sediments of clay, silt, sand and gravel to form a variety of depositional features  Because this happened recently (in geologic time) glaciation has had an enormous effect on Canada’s geography setting the current pattern of rivers, hills and plains

Alpine Glaciers Glaciers found in mountainous regions Move from areas of high elevation to low elevation under the force of gravity Movement usually only a few cm a year Continental Glaciers Glaciers that spread out to cover a large portion of the continent Move under their own weight

 Advance or retreat of a glacier is determined by the balance between ice build-up and ice melt

 U-Shaped Valleys

 Striations

 Glacial Spillways

 Misfit Streams

 Cirques and Alpine Glacial Features

 Glacial Erratics

 Glacial Till and Till plains

 Moraines

 Drumlins

 Eskers

 Kettle Lakes