Arete, cirques,and horns
Glacial erosion produces U - shaped valleys.
A cirque, also known as a Cwm or Corrie, is a feature of glacial erosion, formed in a mountainside.
U-shaped valleys, cirques, and fjords are landforms caused by glacial erosion. Glaciers carve these features into the landscape as they move and shape the land over time.
Caves are hollow places that often have an underground space. Caves are erosion landforms, fluvial landforms, karst landforms, and mountain and glacial landforms. Sea caves are oceanic or coastal landforms.
A drumlin is a long mound of glacial till that is formed by the movement of a glacier. As the glacier flows over the landscape, it reshapes the underlying material into these elongated, teardrop-shaped landforms.
The rocks may be formed via various means including: erosion, weathering, glacial action, or from a sudden disturbance.
Eskers
Glacial Erosion formed Yosemite Valley and the Sierra Nevada
Clifford Embleton has written: 'Geomorphology of Europe' 'Glaciers and glacial erosion' -- subject(s): Addresses, essays, lectures, Glacial erosion, Glaciers 'Glacial geomorphology' -- subject(s): Glacial landforms
Glacial erosion produces U - shaped valleys.
A cirque, also known as a Cwm or Corrie, is a feature of glacial erosion, formed in a mountainside.
U-shaped valleys, cirques, and fjords are landforms caused by glacial erosion. Glaciers carve these features into the landscape as they move and shape the land over time.
Caves are hollow places that often have an underground space. Caves are erosion landforms, fluvial landforms, karst landforms, and mountain and glacial landforms. Sea caves are oceanic or coastal landforms.
The sediments that formed the moraines were transported by glacial erosion. As glaciers advance and retreat, they pick up and carry various sediments, including rocks and soil, which are deposited as moraines when the glacier melts. These landforms indicate the former extent of glacial movement and the materials the glacier has moved during its flow.
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A drumlin is a long mound of glacial till that is formed by the movement of a glacier. As the glacier flows over the landscape, it reshapes the underlying material into these elongated, teardrop-shaped landforms.
erosion and glacial lakes