Serac
A serac (originally from Swiss French sérac) is a block or column of glacial ice, often formed by intersecting crevasses on a glacier. Commonly house-sized or larger, they are dangerous to mountaineers since they may topple with little warning. Even when stabilized by persistent cold weather, they can be an impediment to glacier travel.
Seracs are found within an icefall, often in large numbers, or on ice faces on the lower edge of a hanging glacier.[1] Examples of the latter in the Alps are found on the northeast face of Piz Roseg, the north face of the Dent d'Hérens, and the north face of Lyskamm. They are well-known obstacles on many of the world's highest mountains, Kanchenjunga (located on the border of India and Nepal) in particular.
Incidents
The collapse of large seracs was responsible for at least 8 of the 11 deaths of the August 2008 climbing accident on K2.[2] In April 2014, a large serac broke off and caused an avalanche on Mount Everest, which was responsible for the death of 16 climbers.
On a 1970 Japanese expedition to Mount Everest Kyak Tsering was killed by a falling serac.[3]
Gallery
Serac at Russell Glacier in Greenland
Seracs in firn at 10,000 feet (3,050 meters) on the Winthrop Glacier of Mount Rainier in Washington, USA
Seracs of Bossons Glacier, south-eastern France, seen from the trail junction
More seracs at Bossons Glacier
Seracs in Piloto Glacier in Cordillera Darwin, Tierra del Fuego
See also
References
- ↑ Post, Austin; Lachapelle, Edward R. (2000). Glacier Ice (Revised ed.). Seattle: University of Washington Press. ISBN 0-295-97910-0.
- ↑ Perlez, Jane (August 5, 2008). "More Are Feared Dead Near K2's Harsh Summit". The New York Times. Retrieved November 20, 2010.
- ↑ "THE JAPANESE MOUNT EVEREST EXPEDITION, 1969-1970".
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