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  • Cirques: Understanding Mountain Glacial Features
    The bowl-shaped depressions or hollows found near mountain peaks are called cirques.

    Here's some more information about them:

    * Formation: Cirques are formed by glacial erosion. As glaciers flow down mountains, they carve out these bowl-shaped depressions in the bedrock.

    * Location: They are typically found at the head of a valley, high up on a mountainside.

    * Features: Cirques often have steep, back walls and a lip on the downhill side. The bottom of a cirque may contain a small lake or tarn.

    * Importance: Cirques are important landforms in mountainous areas, and they provide evidence of past glaciation. They can also be important habitats for wildlife and sources of water.

    Let me know if you'd like to know more about glacial landforms!

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