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The key glacial processes shaping glaciated landscapes are erosion, transportation, and deposition.
Glacial erosion is a significant process that shapes glaciated landscapes. This occurs when a glacier moves over the land, picking up rocks and other debris in its path. There are two main types of glacial erosion: abrasion and plucking. Abrasion happens when the glacier grinds along the ground, smoothing and polishing the surface. This can create striations, which are long, straight lines etched into the rock. Plucking, on the other hand, occurs when the glacier freezes onto the rock and pulls pieces away as it moves. This can lead to the formation of jagged, irregular landscapes.
Transportation is another key process. As glaciers move, they transport the material they have eroded. This material, known as moraine, can be carried for many kilometres before being deposited. The transportation of moraine by glaciers can significantly alter the landscape, creating features such as drumlins (elongated hills) and eskers (long, winding ridges).
Deposition is the final key process. When a glacier melts, it deposits the material it has been carrying. This can occur in a variety of ways, depending on the nature of the glacier and the landscape. For example, if a glacier melts slowly, it may deposit its load gradually, creating a smooth, rolling landscape. If a glacier melts quickly, it may dump its load all at once, creating a more chaotic, jumbled landscape. The deposited material, known as till, can range in size from tiny particles of silt to huge boulders.
These processes of erosion, transportation, and deposition interact in complex ways to shape glaciated landscapes. The specific features of a given landscape will depend on a variety of factors, including the size and speed of the glacier, the nature of the underlying rock, and the climate. Despite this complexity, understanding these basic processes can provide a useful framework for interpreting the dramatic and beautiful landscapes that glaciers create.
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