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โ๏ธ Avalanches can reach speeds of up to 80 mph (129 km/h).
๐๏ธ Over 90% of avalanche victims are caught in the slide rather than triggered by it.
๐จ๏ธ The most common cause of avalanches is a heavy snowfall or rapid warming of the snowpack.
โ ๏ธ Avalanches can vary in size from small sluff slides to large, destructive flows that can bury whole valleys.
๐ An avalanche can travel as far as 1,500 feet (457 meters) downhill in just a matter of seconds.
๐ฌ๏ธ Wind-loading, where snow is deposited on windward slopes, is a major factor in avalanche formation.
๐งโโ๏ธ The steepness of the slope affects avalanche potential, with the most likely slopes being between 30 and 45 degrees.
๐จ In mountainous areas, avalanche forecasting and warning systems are crucial for public safety.
๐ The study of avalanches is known as 'avalanchology' and involves meteorology, snow physics, and terrain analysis.
๐ง Although most avalanches occur in winter, they can also happen in spring when temperatures rise and snow melts.
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