Glacial Landforms YouTube Lecture Handouts
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A glacier is a moving mass of ice at speeds averaging few meters a day.
Types of Glaciers: continental glaciers, ice caps, piedmont glaciers and valley glaciers.
Glacial Deposition
- Outwash Plain: When the glacier reaches its lowest point and melts, it leaves behind a stratified deposition material called till plain or an outwash plain.
- Esker: Winding ridge of un-assorted depositions of rock, gravel, clay etc. running along a glacier in a till plain.
- Kame Terraces: Broken ridges or un-assorted depositions looking like hump in a till plain.
- Drumlin: Inverted boat-shaped deposition in a till plain caused by deposition.
- Kettle Holes: Formed when the deposited material in a till plain gets depressed locally and forms a basin.
Glacial Erosion
- Plucking: Water freezes into joints in the rock. Glacier moves and rock is pulled away or ‘plucked’ from the base of the valley.
- Abrasion: Rock plucked away by the glacier (moraine) scrapes the valley bottom and sides.
- Freeze – thaw or frost shattering
Corrie
- Armchair shaped depression with a steep back wall and a shallow rock lip
- Formed in high mountain areas where glaciers start
- Snow collects in a small hollow
- Compacts and turns to ice
- Ice plucks rocks from the back wall
- Ice scours the rock away through abrasion
U Shaped Valleys & Truncated Spurs
- Formed as a glacier moves through a river valley removing the interlocking spurs
- Steep sides and wide flat floor
- Truncated spurs
Arêtes and Pyramidal Peaks
- Two corries erode back to back
- Narrow ‘knife edge’ like ridge
- Three or more corries result in a ‘Pyramidal Peak’
Hanging Valleys
- Former river tributary originally joined the river at the same height as the main valley
- Glacier fills a former river valley- tributary glaciers join the main glacier at a higher level
- Glacier erodes the tributary valley hanging at the side of the main valley
- Stream plunges over the edge as a waterfall
✍ Manishika