A snow wrist, a snowbank
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A windblown heap of snow is called a snowdrift. Snowdrifts can vary in size and shape depending on the strength of the wind and the amount of snowfall. They can accumulate in areas where the wind blows the snow from exposed surfaces and deposits it in piles.
A snowdrift, or
sastrugi (sā-str 'gə, sä'strə-) also zastrugi (sā-str 'gə, sä'strə-)
Long, wavelike ridges of snow, formed by the wind and found on the polar plains. Sastrugi are usually up to several meters high and are often parallel to the prevailing wind direction.
The American Heritage® Science Dictionary
Copyright © 2002. Published by Houghton Mifflin. All rights reserved.
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A snowdrift or bank. These are usually heavily packed, and dangerous, if one
should be caught in an avalanche.
A windblown pile of snow is called a snowdrift. This occurs when strong winds pick up loose snow and deposit it in a mound-like formation. Snowdrifts can vary in size and shape depending on the strength of the wind and the texture of the snow.
Avalanche is a sudden and fast flow of snow down a slope.
Sandy soil is easily blown by the wind due to its loose texture and lack of organic matter that help bind the soil particles together. Its lightweight composition makes it prone to erosion and displacement by wind action.
Snow falls upward in regions with strong winds, such as during winter storms or blizzards. When the wind is strong enough, it can lift snow off the ground and cause it to be blown upward, creating a phenomenon known as "snow ghosts."
Wind-blown dust is called "blown dust" or "windblown dust". This occurs when strong winds lift loose particles from the ground and transport them through the air.