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A glissade is a climbing technique mostly used in mountaineering and alpine climbing where a climber starts a controlled slide down a snow and/or ice slope to speed up their descent. Glissading is ideally done later in the day when the snow is softer. [1] [2]
Trees showing the presence of creep. Downhill creep, also known as soil creep or commonly just creep, is a type of creep characterized by the slow, downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress.
A discipline of skiing that involves sliding down snow-covered slopes on skis with fixed-heel bindings, as opposed to other types of skiing (such as cross-country) which use skis with free-heel bindings. Alpine skiing is popular as a recreational activity and competitive sport, both at ski resorts and off-piste. alpine touring (AT)
Alpine skiers. Alpine skiing, or downhill skiing, is the pastime of sliding down snow-covered slopes on skis with fixed-heel bindings, unlike other types of skiing (cross-country, Telemark, or ski jumping), which use skis with free-heel bindings.
The sliding criterion has been developed for stresses that would occur in slopes between 2 and 25 metres (6.6 and 82.0 ft), hence, in the order of maximum 0.6 megapascals (87 psi). The sliding criterion is based on back analyses of slope instability and earlier work of ISRM [ 5 ] and Laubscher. [ 6 ]
Slope stability refers to the condition of inclined soil or rock slopes to withstand or undergo movement; the opposite condition is called slope instability or slope failure. The stability condition of slopes is a subject of study and research in soil mechanics , geotechnical engineering , and engineering geology .
Rockslide at Oddicombe Beach in Devon, UK Rockslides in Nigeria Landslips. A rockslide is a type of landslide caused by rock failure in which part of the bedding plane of failure passes through compacted rock and material collapses en masse and not in individual blocks.
The slide areas are devoid of trees and vegetation and are covered in granite rock and decomposed granite sand. This gives the barren slopes a whitish color, and the distinctive slide zones are plainly visible from points to the southeast of the mountain in Washoe Valley. The most recent large slide occurred on May 30, 1983.