GGR100H1 Lecture : Glaciers, The Ice Age & Paleovegetation pkg. Lectures from March 17th and 22nd, Including the three broad topics in the title and all their subdivisions.

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Agents of erosion: wind/water/ice act to transport materials that"ve been loosened by physical/chemical weathering and mass wasting. Ice: pwrful aoerosion b/c can move massive amnts. of sediment. > glacial: significant area of earth covered in ice; much glacial erosion potential. Greenland/mountains/arctic , but ice is still available in high latitudes/elevations. Large mass of flowing land ice; plastic body that flows. Ice on land under pressure begins to flow, becoming a glacier. Mass balance: glacier fed (accumulates) from precipitation in form of snow at the top, and ablates (melts) at the bottom. > can"t form in dry, high temperature areas. >glaciers form in conditions of low temperature and adequate snowfall/ppt. > in certain areas, snowfall from winter doesn"t melt in summer and continues to accumulate. Persisting snow is compacted over time into glacial ice (firn), due to intense pressure from the heaviness of piling precipitation.

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