Cirque erosion results in the formation of bowl-shaped depressions at the head of a valley glacier. Deposition can occur when the glacier melts, depositing sediment and creating a small lake called a tarn in the cirque basin.
A cirque, also known as a Cwm or Corrie, is a feature of glacial erosion, formed in a mountainside.
Cirques are typically formed as a result of erosion. They are amphitheater-like hollows on a mountain's side, created by glacial erosion processes such as plucking and abrasion.
Cirque formation is predominantly the result of glacial erosion. Glaciers carve out deep bowl-shaped depressions in the mountains due to their erosive power. Over time, the movement of ice sculpts the landscape into these distinctive features.
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.
A cirque, also known as a Cwm or Corrie, is a feature of glacial erosion, formed in a mountainside.
Cirques are typically formed as a result of erosion. They are amphitheater-like hollows on a mountain's side, created by glacial erosion processes such as plucking and abrasion.
kettle is a result of erosion though the material is an ancient deposition
deposition
deposition
deposition
A horn is erosion
erosion
Cirque formation is predominantly the result of glacial erosion. Glaciers carve out deep bowl-shaped depressions in the mountains due to their erosive power. Over time, the movement of ice sculpts the landscape into these distinctive features.
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