Notes
Glacial Processes

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Water gets into cracks in rocks
Freezes when temp. reaches below 0°C
Puts pressure on surrounding rock as it expands
When water melts, pressure = released
Repeated freezing & thawing widens cracks
Jagged pieces of rocks break off
http://www.youtube.com/watch?v=jFU6j8qD-84 (Embed)

Snow fills existing hollows on the hillside
Over many years, it turns to ice
When the hollow is full, the ice moves downhill as a corrie glacier
Freeze-thaw and plucking make backwall steep
Moraine dragged along the base of corrie glacier makes hollow deeper by abrasion
A lip gets left because erosion is less here. Also sometimes moraine is deposited
After the ice age, melt water was trapped by the lip making a small lake or tarn
Plucking
Rocks stick and freeze to the bottom or sides of a glacier
Plucked away from bedrock
Deposited
Leaves behind jagged rocks
Abrasion
Moraine embedded into glacier rubs against floors and sides of valley as it moves
Leaves behind smooth surface like sandpaper


Glacier wears away sides & floor of the valley
Causes valley to deepen, widen & straighten
When ice melts, a U-shaped valley with steep sides & flat floor is left
Narrow floors
Steep-sided
Straight wide flat floors with truncated spurs
Interlocking spurs are eroded away to leave cliff-like truncated spurs


Glaciers perched up on valley sides as hanging valleys
During the ice age many river valleys were filled with snow which turned to ice and moved down the slope as glaciers
Freeze-thaw weathering supplied the glacier with sharp rock fragments
Ice plucking & abrasion eroded the valley side & floor leaving a flat bottomed & steep sided valley known as glacial trough
Glacier scraped away interlocking spurs of the river valley leaving truncated spurs
Tributary valleys were left hanging above the main valley
After the ice melted, glacial troughs often filled with lakes called ribbon lakes because they are long & thin

Freeze-Thaw Weathering
Corrie
Erosion
U-Shaped Valley
Truncated Spurs & Hanging Valleys
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- Geography (Old) Note on Glacial Processes, created by vina_56 on 08/06/2013.
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