Exam (elaborations)
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, cr...
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