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Kolka Glacier : ウィキペディア英語版
Kolka Glacier

Kolka Glacier ((オセット語:Хъолхъа)) is a glacier in North Ossetia, Russia, near Mount Kazbek, known for its surging properties. The most recent and the most powerful surge took place on September 20, 2002, resulting in deaths of at least 125 people〔(【引用サイトリンク】 publisher = NASA Earth Observatory )〕
==Morphology==

There are only a small number of glaciers in the Genaldon River's basin, the largest being Maili at approximately in area. The Kolka Glacier, located next to Maili, is a cirque / valley glacier, with some hanging parts. Kolka is fed by avalanches and collapses of firn and ice all year-round. Its lowest and highest points are located at and above mean sea level respectively. More than two thirds of the ablation zone's surface is covered by a morainal layer up to thick. This and other features, such as relatively gentle slopes, a deep cirque and the presence of a lateral moraine restricting the ice flow and forcing it to make a sharp turn, makes the glacier very prone to accumulation of subglacial meltwater.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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