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4 – Glacial Erosion
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glacier – a mass of ice and snow that moves downhill under the influence of gravity.
Salmon Glacier in British Columbia, Canada. Kenai Fjord National Park, Alaska, USA.
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glacier – a mass of ice and snow that moves downhill under the influence of gravity.
There are two types of Glaciers; 1 – Mountain (alpine or valley) glaciers.
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2 – Continental (ice sheets)
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Glacier movement glaciers always move downhill. advancing glaciers
more snow and ice accumulate than is lost by melting. the end of the glacier will move forward.
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retreating glaciers more ice and snow melt each year than accumulate. the furthest extent of the glacier (the end) does not extend as far downslope.
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Ice Movement the ice within a glacier moves more slowly along the sides of the glacier (friction). View of ice velocity from above glacier ( View of ice velocity from side of glacier (
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Glacial Erosional Features
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Till Unsorted (different sizes) & unstratified (not layered) rock material deposited directly by glacial ice.
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Moraine a deposit of till left behind when a glacier retreats.
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End moraine, Bylot Island, Canada
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Lateral moraine material that piles up along the sides of the glacier.
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Medial moraine a pile of material that runs down the middle of the glacier. produced when two glaciers come together and their lateral moraines join.
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Striations long parallel scratches left on rocks and bedrock by glacial movement. produced when the glacier drags rock material over the bedrock.
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Glacial grooves, Ontario, Canada
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U-shaped valley glacial valley - a u-shaped valley formed by glacial erosion.
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Hanging valley The U-shaped valley carved out by the main glacier is deeper than the valleys carved out by the tributary glaciers.
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Cirque a semicircular basin found at the head of a glacial valley.
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Cirque, Torngat Mountains, Newfoundland, Canada
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Arete a sharp divide that separates two adjoining cirques.
“A knife-like ridge.”
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Horn a pyramid-shaped peak formed where three or more cirques meet.
Matterhorn, in Switzerland.
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Torngat Mountains, Newfoundland, Canada
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GLACIAL DEPOSITIONAL FEATURES
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Till unsorted and unstratified rock material deposited directly by glacial ice.
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Outwash sediments deposited in front of a glacier by streams of meltwater.
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End Moraine a moraine that occurs at the ice front - rock pieces brought forward by the glacier’s motion build up as the ice melts.
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End moraine, Bylot Island, Canada
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Erratic a large boulder that has been transported into an area by a glacier.
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Perched erratic boulder, North West Territories, Canada
Perched erratic boulder, Newfoundland, Canada
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Drumlin a long, smooth, canoe-shaped hill. usually found in groups.
shaped by an advancing glacier.
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Drumlin field. Manitoba, Canada
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Outwash Plain a broad, stratified (layered), gently sloping deposit of sediment. formed beyond the terminal (end) moraine by streams from a melting glacier.
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Southwest Alaska 1996
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Esker a long, winding ridge.
formed when sand and gravel fill meltwater tunnels beneath a glacier.
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Kettle (kettle hole) a bowl-like hollow found in deposits of glacial outwash. formed when a large block of ice was left behind when a glacier melted.
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