Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 14 Glacial Landforms and the Ice Age Visualizing Physical Geography

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Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Chapter 14 Glacial Landforms and the Ice Age Visualizing Physical Geography by Alan Strahler and Zeeya Merali Slide 2 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Chapter Overview Glaciers Alpine Glaciers Ice Sheets and Sea Ice The Ice Age Slide 3 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Glaciers Glacier: large natural accumulation of land ice affected by present or past flowage Glacial ice has shaped many landforms in middle and high latitudes Glacial ice sheets affect global climate Glaciers reflect sunlight Glacial ice affects global heat transport Volume of glacial ice affects sea levels Large bodies of ice are plastic because of pressure on ice at bottom of mass Large body of ice can flow in response to gravity Ice on a slope can slide downwards Ice sheet: large thick plate of glacial ice moving outward in all directions Slide 4 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Glaciers Glacial ice builds up when snowfall in winter exceeds snow melted in summer Each annual layer of snow, melts, refreezes, forms ice Weight of ice compresses the lower layers into hard crystalline ice When the ice mass becomes thick enough, the lower layers flow plastically Glacial ice forms where temperatures are low and snowfall is high Alpine glacier: long, narrow mountain glacier occupying the floor of a trough-like valley Slide 5 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Glaciers Glaciers contain rock of all sizes Glaciers and ice sheets erode and deposit great quantities of sediment Glacial abrasion: rock fragments in a glacier scrape and grind the bedrock Plucking: moving ice plucks loosened rock material and carries it away Sediment is carried, then deposited when the ice melts Slide 6 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Upper part of the glacier is brittle Lower part is plastic Zone of accumulation: glacier is growing Zone of ablation: glacier is evaporating/melting Alpine glacier can slide downhill on meltwater and mud Rate of movement: few centimeters/day to several meters/day Surge: rapid movement of alpine glacier, up to 60 m/day for several months Slide 7 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Landforms Made by Alpine Glaciers Slide 8 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Landforms Made by Alpine Glaciers Slide 9 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Landforms Made by Alpine Glaciers Cirque: valley head enlarged and hollowed out by glaciers, producing bowl-shaped valley Arte: sharp ridge formed between two cirques Horn: steep-sided peak formed by glacial erosion from three sides Col: natural pass or low notch in an arte between opposed cirques Moraine: accumulation of rock debris carried by an alpine glacier and deposited by the ice to become a depositional landform Tarn: small lake occupying a rock basin in a cirque Hanging valley: stream valley that has been truncated by glacial erosion so as to appear in cross section in the upper wall of a glacial trough Slide 10 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Landforms Made by Alpine Glaciers Slide 11 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Alpine Glaciers Landforms Made by Alpine Glaciers Glacial trough: deep, steep- sided rock trench formed by alpine glacier erosion Fiord: narrow, deep ocean inlet partially filling a glacial trough Slide 12 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Ice Sheets and Sea Ice Ice Sheets of the Present Antarctic Ice Sheet 13 million sq km 4000 m thick Greenland Ice Sheet 1.7 million sq km 3000 m thick Slide 13 Visualizing Physical Geography Copyright 2008 John Wiley and Sons Publishers Inc. Ice Sheets and Sea Ice Sea Ice and Icebergs Sea Ice: floating ice of the oceans formed by direct freezing of ocean water Always