An arête is a thin, almost knife-like, ridge of rock which is typically formed when two glaciers erode parallel U-shaped valleys, or else when two corrie glaciers erode back-to-back. An arête is a formed as a result of erosion, though the material it is made of may be an ancient deposition (this, however, is irrelevant).
An arete is typically a result of erosion, specifically glaciation. It forms when two adjacent glaciers erode parallel valleys, leaving a sharp ridge or peak in between. Deposition, on the other hand, tends to create landforms like moraines or deltas.
kettle is a result of erosion though the material is an ancient deposition
A crevasse forms as a result of erosion. It is a deep crack or fissure in a glacier caused by movement and stress, rather than a location of deposition of sediment.
Loess is a result of deposition. It is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust.
A glacial lake is typically a result of both erosion and deposition. Glacial erosion carves out depressions in the landscape, creating basins where water accumulates. Meanwhile, glacial deposition can form moraines or other features that dam up water and contribute to the formation of a glacial lake.
An arete is typically a result of erosion, specifically glaciation. It forms when two adjacent glaciers erode parallel valleys, leaving a sharp ridge or peak in between. Deposition, on the other hand, tends to create landforms like moraines or deltas.
kettle is a result of erosion though the material is an ancient deposition
deposition
deposition
deposition
A horn is erosion
erosion
Yes. Since dunes are the result of erosion, they are categorized as deposition.
it will turn to snow
kettle is a result of erosion though the material is an ancient deposition
A crevasse forms as a result of erosion. It is a deep crack or fissure in a glacier caused by movement and stress, rather than a location of deposition of sediment.
Loess is a result of deposition. It is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust.