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  2. Cirque - Wikipedia

    en.wikipedia.org/wiki/Cirque

    Cirque. A cirque (French: [siʁk]; from the Latin word circus) is an amphitheatre -like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic: coire, meaning a pot or cauldron) [1] and cwm (Welsh for 'valley'; pronounced [kʊm]). A cirque may also be a similarly shaped landform arising from ...

  3. Pyramidal peak - Wikipedia

    en.wikipedia.org/wiki/Pyramidal_peak

    Pyramidal peak. The Matterhorn, a classic example of a pyramidal peak. A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks.

  4. Cirque de Gavarnie - Wikipedia

    en.wikipedia.org/wiki/Cirque_de_Gavarnie

    The Cirque de Gavarnie (French pronunciation: [siʁk də ɡavaʁni]) is a cirque in the central Pyrenees, in Southwestern France, close to the border of Spain. It is within the commune of Gavarnie, the department of Hautes-Pyrénées, and the Pyrénées National Park. Major features of the cirque are La Brèche de Roland (English: Roland's Pass ...

  5. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Cirques are where ice begins to accumulate in a glacier. Two glacial cirques may form back to back and erode their backwalls until only a narrow ridge, called an arête is left. This structure may result in a mountain pass. If multiple cirques encircle a single mountain, they create pointed pyramidal peaks; particularly steep examples are ...

  6. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Erosional landforms. As the glaciers expand, due to their accumulating weight of snow and ice they crush, abrade, and scour surfaces such as rocks and bedrock.The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys.

  7. Cirque glacier - Wikipedia

    en.wikipedia.org/wiki/Cirque_glacier

    Cirque glacier. A cirque glacier is formed in a cirque, a bowl-shaped depression on the side of or near mountains. Snow and ice accumulation in corries often occurs as the result of avalanching from higher surrounding slopes. If a cirque glacier advances far enough, it may become a valley glacier. Additionally, if a valley glacier retreats ...

  8. Cirque stairway - Wikipedia

    en.wikipedia.org/wiki/Cirque_stairway

    Cirque stairway. A cirque stairway or sequence of cirque steps is a stepped succession of glacially eroded rock basins. [1] Their individual formation is that of a cirque . These steps are arranged one above and behind the other at different heights in the terrain and caused by the same morphodynamic processes, albeit resulting in different ...

  9. Cirque du Soleil - Wikipedia

    en.wikipedia.org/wiki/Cirque_du_Soleil

    Cirque du Soleil (French: [siʁk dy sɔlɛj], Canadian French: [sɪʁk d͡zy sɔlɛj]; "Circus of the Sun" or "Sun Circus") is a Canadian entertainment company and the largest contemporary circus producer in the world. [7] Located in the inner-city area of Saint-Michel, Montreal, it was founded in Baie-Saint-Paul on 16 June 1984 by former ...