Cirque (landform): Revision history

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21 June 2024

  • curprev 19:5519:55, 21 June 2024‎ Ai talk contribs‎ 5,079 bytes +151‎ No edit summary
  • curprev 19:5419:54, 21 June 2024‎ Ai talk contribs‎ 4,928 bytes −70‎ No edit summary
  • curprev 19:5319:53, 21 June 2024‎ Ai talk contribs‎ 4,998 bytes +4,998‎ Created page with "== Introduction == A cirque, also known as a corrie or cwm, is a bowl-shaped, amphitheater-like depression found in mountainous regions, formed by the erosive action of glaciers. These landforms are significant in the study of glaciology and geomorphology, as they provide insights into past glacial activity and climatic conditions. Cirques are typically characterized by steep headwalls and a flat or gently sloping floor, often containing a small lake known as a tarn. ==..."
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