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Physical Process

Glacial Erosion

Glacial and Periglacial Processes

The wearing away of bedrock and sediment by moving glacial ice, working through plucking, in which ice freezes onto joint-bounded blocks of rock and tears them free, and abrasion, in which rock fragments embedded in the ice's base grind and scratch the surface beneath. It is the dominant force carving U-shaped valleys, cirques and fjords in glaciated mountain landscapes.

Facts
Process Type
Glacial 1
Timescale
approximately 100,000 years to form a U-shaped valley, mountain ranges erode over millions of years 1
Connections

Caused By

Causes

Source Arete Formation (Wikipedia)
Source Cirque Formation (Wikipedia)
Source Roche Moutonnee Formation (Wikipedia)
Sources
1. Glacial erosion - Wikipedia
  • Glaciers section, processes sentence
    Glaciers erode predominantly by three different processes: abrasion/scouring, plucking, and ice thrusting.
  • Glaciers section, timescale paragraph
    Scientists also provide a numerical estimate of the time required for the ultimate formation of a steady-shaped U-shaped valley, approximately 100,000 years. Mountain ranges take millions of years to erode to the degree they effectively cease to exist.
View the Source
Cirque Formation (Wikipedia)
Wikimedia FoundationCauses: Cirque FormationView the Source
Arete Formation (Wikipedia)
Wikimedia FoundationCauses: Arete FormationView the Source
Roche Moutonnee Formation (Wikipedia)
Wikimedia FoundationCauses: Roche Moutonnee FormationView the Source
Glacial Plucking (Wikipedia)
Wikimedia FoundationEncompasses: Glacial PluckingView the Source
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