Continental Ice Sheets Study guides, Class notes & Summaries
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Continental Ice Sheets - Glaciers formed in non-mountainous areas of continents Only 2 exist today: Greenland and Antarctica Ice Shelfs: Where they meet the sea Vary in thickness from hundreds of feet to two miles deep Crustal Depression - Enormous weight
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Continental Ice Sheets - Glaciers formed in non-mountainous areas of continents 
Only 2 exist today: Greenland and Antarctica 
Ice Shelfs: Where they meet the sea 
Vary in thickness from hundreds of feet to two miles deep 
Crustal Depression - Enormous weight of ice sheets 
Isostatic adjustment, crust is rebounding where glacial ice existed 
Response to weight loss 
Depositional Glacial Landforms - All debris in the ice is eventually brought to the 
ablation zone and deposited 
Modes: 
Directed...
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