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  2. 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:
    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.
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  5. WEBLearn about the formation, features, and landforms of alpine glaciers, which are found in high mountain regions. See how glaciers erode, sculpt, and create valleys, lakes, and fiords.

  6. WEBValley glaciers (also known as alpine glaciers or mountain glaciers) excel at sculpting mountains into jagged ridges, peaks, and deep U-shaped valleys as these highly erosive rivers of ice progress down mountainous …

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    WEBOct 19, 2023 · Glaciers fall into two groups: alpine glaciers and ice sheets. Alpine glaciers form on mountainsides and move downward through valleys. Sometimes, alpine glaciers create or deepen valleys by pushing …

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  9. WEBSome of the other features associated with glacier erosion in alpine regions are cirques, horns, and arêtes (Figure 10af-3). Cirques are the bowl shaped depressions found at the head of glacial valleys.

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    WEBThere are three general types of glaciers: alpine or valley glaciers, ice sheets, and ice caps. Most alpine glaciers are located in the world’s major mountain ranges such as the Andes, Rockies, Alps, and Himalayas, …

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