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- Features of alpine glaciers include123:
- Cirques: Bowl-shaped mountain hollows where alpine glaciers begin to flow downhill.
- Arêtes: Narrow ridges formed by erosion between adjacent cirques.
- Lateral moraines: Accumulations of debris along the sides of the glacier.
- Hanging valleys: Smaller valleys that intersect with the main glacier valley.
- Terminal moraines: Piles of debris at the end of the glacier.
- Fjords: Deep, U-shaped coastal valleys formed by glacial erosion.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Alpine glaciers are slow-moving rivers of ice that flow from high mountains. Like the continental ones, they create lands by weathering and deposition. Examples of landforms by Alpine glaciers are arête, cirque, lateral moraines, hanging valley, terminal moraine, and fjords.eartheclipse.com/science/geography/alpine-glacier…Alpine glaciers form on mountainsides and move downward through valleys. Sometimes, alpine glaciers create or deepen valleys by pushing dirt, soil, and other materials out of their way. Alpine glaciers are found in high mountains of every continent except Australia (although there are many in New Zealand).education.nationalgeographic.org/resource/glacier …Alpine glaciers begin to flow downhill from bowl-shaped mountain hollows called cirques. As the glaciers overflow the cirque, they move downward. They dig deep into the terrain, forming rugged, dramatic landscapes. As they move, glaciers erode or wear away the land beneath and around them.media.nationalgeographic.org/assets/reference/ass… - People also ask
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