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  2. Crevasse - Wikipedia

    en.wikipedia.org/wiki/Crevasse

    Transverse crevasses, Chugach State Park, Alaska. A crevasse is a deep crack that forms in a glacier or ice sheet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear ...

  3. Glossary of climbing terms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_climbing_terms

    A A-grade Also aid climbing grade. The technical difficulty grading system for aid climbing (both for "original" and an adapted version for "new wave"), which goes: A0, A1, A2, A3, A4, A5 and up to A6 (for "new wave"). See C-grade. Abalakov thread Abalakov thread Also V-thread. A type of anchor used in abseiling especially in winter and in ice climbing. ABD Also assisted braking device. A term ...

  4. Bergschrund - Wikipedia

    en.wikipedia.org/wiki/Bergschrund

    A bergschrund (from the German for mountain cleft; sometimes abbreviated in English to "schrund") is a crevasse that forms where moving glacier ice separates from the stagnant ice or firn above. [1] It is often a serious obstacle for mountaineers. Bergschrunds extend to the bedrock, and can have a depth of well over 100 metres (330 ft).

  5. Crevass - Wikipedia

    en.wikipedia.org/?title=Crevass&redirect=no

    Pages for logged out editors learn more. Contributions; Talk; Crevass

  6. Crevasses - Wikipedia

    en.wikipedia.org/?title=Crevasses&redirect=no

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  7. Keanu Reeves is eager to once again suit up in John Constantine’s signature trench coat and tie. Nearly twenty years after he first brought the DC Comics/Vertigo character to life in Francis ...

  8. Fluvioglacial landform - Wikipedia

    en.wikipedia.org/wiki/Fluvioglacial_landform

    Low, straight ridges as much as 10 metres (33 ft) high may be formed where sediment fills in crevasses within the glacier or at its base. [8] A kame is a short mound or ridge with steep sides of sands and gravels deposited from melted ice. Kames may be isolated or formed in groups.

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