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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

  • 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

  • Exam (elaborations) • 12 pages • 2024
  • 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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