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Glaciers and Long Island
How are Glaciers and Long Island related?
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Glaciers Snowfall exceeds melting. High altitudes and polar regions.
Gravity moves mass downhill. Firn = very dense snow layer.
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Continental Glaciers Ice sheets that cover continents.
Kilometers thick. Only 2 exist: - Greenland and Antarctica
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Valley Glaciers Begins in a cirque = bowl-shaped basin at mountaintop.
Crevasses = cracks in the glacier.
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Erosion U-shaped Valleys Cirques, Aretes and Horns.
Hanging Valleys - from tributary
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Erosion Striations = parallel scratches on bedrock... from rocks on bottom of glacier Polish = fine material rubs rock smooth.
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Striations
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Polish
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Deposition Moraines - Unsorted pile of debris = till
Erratics = large isolated boulders. Drumlins = long, low mounds of till with teardrop shape. Outwash Plain (sorted) = sediments that are “washed out” in front of glacier.
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Erratic
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Central Park, NYC
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Drumlin
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Lakes Kettle Formation:
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Kettle Lakes
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Glacial Lake Forms when ice dams a stream.
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Ice Age Glacier Limit
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