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Like running water, gravity is the driving force
behind all glaciers. The ice moves material from high places and deposits it in low places There are 2 primary types of glaciers: Alpine (Valley) Glacier – These form in mountainous regions where the elevation is high enough to support ice all year round Continental Glacier (Ice Sheet) – These form over large land areas In very high latitudes. There are only 2 that exist in the world today, In Antarctica, and Greenland.
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Alpine Glaciers
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Alpine Glaciers Permanent snow accumulates when new snow falls on
old snow. Alpine Glaciers Like a slow moving river the ice starts sliding down the mountain in the valley between the peaks and ridges When the snow becomes thick enough the bottom layers get compressed into ice
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The ice whittles the peaks
into sharp points called horns
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World’s most famous horn,
The Matter Horn in Switzerland
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Merging glaciers Medial moraine
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After the snow melts, the glaciated mountains look like this
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U shaped valley
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Steep side of U shaped valley is called
a hanging wall
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Watch out for these crevasse
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Rock on the valley floor gets scratched
and polished Fresh surface not scratched
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Glacially polished bedrock
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More polishing with striations and glacial scratching
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The surface of glacier gets dirty in summer
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Glacial sediments are always unsorted At the front or leading edge
Of the glacier terminal moraine is pushed into a bank of unsorted sediments Glacial sediments are always unsorted
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Terminal moraine Outwash plain
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Calving occurs where a glacier meets the sea
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Icebergs form where chunks
of the glacier break off
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Some icebergs are as big as a city
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Continental Glaciers (Ice sheets)
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Great North American Ice sheet 10,000 years ago Today the ice sheet is
limited to only Greenland
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These are called transported soils
Throughout the mid-west and northeast there is much evidence that the region was covered by a mile thick layer of ice only 10,000 years ago Most of the soils here have been scraped from Canada and deposited by the glacier These are called transported soils
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As the glacier retreated northward,
It left behind much evidence of It’s presence
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Drumlin near the Finger Lakes
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Drumlin in Wisconsin Which direction is south?
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Erratic in Central Park
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Glacial Erratic in Yellowstone National park
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terminal moraine on north shore of Long Island
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Kettle lakes Esker in Wisconsin
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Kame
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Kame used for Sand and gravel
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