An avalanche is a swift descent of snow down a sloped surface. They occur spontaneously due to causes like heavy snowfall or snowpack instability, or by external triggers like human activity or seismic events. Consisting primarily of snow and air, large avalanches can incorporate and transport ice, rocks, and trees due to their powerful force.
In March 1910, two major avalanches occurred: the Wellington avalanche on March 1 killed 96 people in Washington state, and three days later, the Rogers Pass avalanche killed 62 railroad workers in British Columbia, Canada.
In December 1916, approximately 10,000 soldiers from both sides of the Austrian-Italian front died in avalanches during World War I.
In 1924, Professor Lagotala worked on modeling avalanche behavior in preparation for the Winter Olympics in Chamonix.
From 1950 to 2021, 1,169 people died in avalanches in the United States.
From 1950 to 2021, 1,169 people died in avalanches in the United States.
In the Northern Hemisphere winter of 1950 to 1951, approximately 649 avalanches were recorded in a three-month period throughout the Alps in Austria, France, Switzerland, Italy and Germany. This series of avalanches killed around 265 people and was termed the Winter of Terror.
In 1955, A. Voellmy's "Ueber die Zerstörungskraft von Lawinen" (On the Destructive Force of Avalanches) was published and popularized Lagotala's avalanche modeling method.
On March 20, 1968, the Biały Jar avalanche in Poland swept away 24 people, resulting in 19 fatalities, including Russian, East German, and Polish citizens.
In 1990, an earthquake triggered a large avalanche on Lenin Peak in Kyrgyzstan, wiping out a mountain climbing camp and killing 43 climbers.
In April 1993, Europe adopted a standardized avalanche risk scale to replace earlier non-standard national schemes.
In 1993, the Bayburt Üzengili avalanche in Turkey killed 60 individuals.
In a 1996 study, Jamieson et al. found that 83% of avalanches in recreational settings were caused by those involved, while all accidents in residential, industrial, and transportation settings were due to spontaneous natural avalanches.
Following the 1999 Galtür avalanche disaster, scientific studies using radar confirmed the hypothesis that a saltation layer forms between the surface and airborne components of an avalanche.
In 1999, a large avalanche in Montroc, France, killed 12 people in their chalets, leading to the mayor's conviction for not evacuating the area.
In 1999, it was described that wet snow avalanches are low-velocity suspensions of snow and water confined to the track surface, capable of generating powerful destructive forces due to their mass and density, often associated with climatic cycles at the end of winter.
In 1999, the Galtür avalanche hit the Austrian village of Galtür, which was thought to be in a safe zone, resulting in 31 deaths.
In 2001, it was reported that globally an average of 150 people die each year from avalanches.
On January 28, 2003, the Tatra Mountains avalanche swept away nine out of thirteen students heading to the summit of Rysy in the Tatra Mountains.
In May 2003, descriptions for the European avalanche risk scale were updated to enhance uniformity.
In April 2006, it was reported that 445 people died in avalanches throughout North America during the 11-year period ending April 2006.
As of 2007, the D2FRAM (Dynamical Two-Flow-Regime Avalanche Model) was still undergoing validation.
From 1950 to 2021, 1,169 people died in avalanches in the United States.
From 1950 to 2021, 1,169 people died in avalanches in the United States.
On July 3, 2022, a serac collapse on the Marmolada Glacier in Italy caused an avalanche that killed 11 alpinists and injured eight.
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