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(1) Pine snow falls: Pine snow with low adhesion is rolled off by a little looseness, which leads to the fall of other loose snow on the path. These rolling pine snows can cause avalanches over long distances under the acceleration of gravity. They can cause long-range avalanches. Although there are only snow layers on the surface, they may develop into deadly avalanches due to the large range of influence, distance, and speed. When climbing a steep slope, climbers must be aware of the dangers of falling pines.
(2) Snow slippage: The tight snow layer slides and alights due to external forces or gravity. Between different layers of snow, when its combination is not dense, a little external force can trigger its avalanche. It is possible for the thickness of snow slide to fall from 2 cm to more than 10 meters. However, due to snow slide caused by manpower, the thickness is usually less than 1.5M. In fact, most of them are less than 0.6M. The thickness and danger of snow layer Sex does not have a direct relationship. Some snow slides that are only a few centimeters thick still cause mountaineers to die. The focus is on the involvement of people in the avalanche process. The extent of this avalanche is determined by terrain and snow conditions, and can range from a few meters to more than two kilometers wide.
Snow slippage is another important indicator, including hard snow or soft snow, wet snow or dry snow, snow density and other factors, these factors will affect the speed, strength, avalanche of avalanche. The wet avalanche speed is about 10-35 M/Sec, while the faster dry avalanche can reach 20-70 M/Sec.
(3) Snowball collapse: The snowball is a piece of snow that blows snow and accumulates on the leeward side of a ridgeline cliff. When snow accumulates beyond the supporting force, snowball falls. In some places, the terrain and climate are very special. Snowballs will accumulate on both sides of the ridgeline. When the climbing route is under the snow ridge or on the ridgeline, avoid the dangerous area where the snowball falls.
(4) The collapse of the Hanging Glacier: When the end of the steeply collapsing river collapses, it collapses due to gravity or external forces. This ice crash usually entrains large amounts of rock, ice, snow, and runs for a long distance. The danger of overhanging glaciers is easier to observe, but it is impossible to predict the time and scale of its occurrence. Some glaciers only collapsed a little bit of ice, but the collapse of large glaciers was extraordinary and could destroy anything on the path. A while back (2002.09) The glacial collapse in the Caucasus Mountains in southern Russia may be an unprecedented disaster. The thickness of the glaciers that have collapsed exceeds 150M. The ice that travels more than 20 kilometers entrains hundreds of millions of tons of ice and stones and rushes downhill at high speed. Caused more than 100 deaths. When climbing a dangerous area where a glacier collapses, you will be exposed to extremely high risks. At this time, you must minimize the exposure to dangerous areas.
(2) Snow slippage: The tight snow layer slides and alights due to external forces or gravity. Between different layers of snow, when its combination is not dense, a little external force can trigger its avalanche. It is possible for the thickness of snow slide to fall from 2 cm to more than 10 meters. However, due to snow slide caused by manpower, the thickness is usually less than 1.5M. In fact, most of them are less than 0.6M. The thickness and danger of snow layer Sex does not have a direct relationship. Some snow slides that are only a few centimeters thick still cause mountaineers to die. The focus is on the involvement of people in the avalanche process. The extent of this avalanche is determined by terrain and snow conditions, and can range from a few meters to more than two kilometers wide.
Snow slippage is another important indicator, including hard snow or soft snow, wet snow or dry snow, snow density and other factors, these factors will affect the speed, strength, avalanche of avalanche. The wet avalanche speed is about 10-35 M/Sec, while the faster dry avalanche can reach 20-70 M/Sec.
(3) Snowball collapse: The snowball is a piece of snow that blows snow and accumulates on the leeward side of a ridgeline cliff. When snow accumulates beyond the supporting force, snowball falls. In some places, the terrain and climate are very special. Snowballs will accumulate on both sides of the ridgeline. When the climbing route is under the snow ridge or on the ridgeline, avoid the dangerous area where the snowball falls.
(4) The collapse of the Hanging Glacier: When the end of the steeply collapsing river collapses, it collapses due to gravity or external forces. This ice crash usually entrains large amounts of rock, ice, snow, and runs for a long distance. The danger of overhanging glaciers is easier to observe, but it is impossible to predict the time and scale of its occurrence. Some glaciers only collapsed a little bit of ice, but the collapse of large glaciers was extraordinary and could destroy anything on the path. A while back (2002.09) The glacial collapse in the Caucasus Mountains in southern Russia may be an unprecedented disaster. The thickness of the glaciers that have collapsed exceeds 150M. The ice that travels more than 20 kilometers entrains hundreds of millions of tons of ice and stones and rushes downhill at high speed. Caused more than 100 deaths. When climbing a dangerous area where a glacier collapses, you will be exposed to extremely high risks. At this time, you must minimize the exposure to dangerous areas.
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