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Wind erosion of soil at the foot of Chimborazo, Ecuador Rock carved by drifting sand below Fortification Rock in Arizona (Photo by Timothy H. O'Sullivan, USGS, 1871). Aeolian processes, also spelled eolian, [1] pertain to wind activity in the study of geology and weather and specifically to the wind's ability to shape the surface of the Earth (or other planets).
Atmospheric or wind-borne fugitive dust, also known as aeolian dust, comes from dry regions where high-speed winds can remove mostly silt-sized material, abrading susceptible surfaces. This includes areas where grazing , ploughing , vehicle use, and other human behaviors have further destabilized the land , though not all source areas have been ...
For more on USA TODAY’s Crossword Puzzles. USA TODAY’s Daily Crossword Puzzles. Sudoku & Crossword Puzzle Answers. This article originally appeared on USA TODAY: Crossword Blog & Answers for ...
Saltation is responsible for the majority (50–70%) of wind erosion, followed by suspension (30–40%), and then surface creep (5–25%). [24] [25] Silty soils tend to be the most affected by wind erosion; silt particles are relatively easily detached and carried away. [26] Wind erosion is much more severe in arid areas and during times of ...
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A loess (US: / ˈ l ɛ s, ˈ l ʌ s, ˈ l oʊ. ə s /, UK: / ˈ l oʊ. ə s, ˈ l ɜː s /; from German: Löss) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. [1] Ten percent of Earth's land area is covered by loesses or similar deposits. [2]
Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt can also be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles). Silt is a common material, making up 45% of average ...
Some 1.35 billion tons, or 8% of global river-borne sediment (16.5-17 billion tons globally), is transported by Ganges-Brahmaputra river system [5] annually according to decades old studies, it is unquantified how much variance year to year as well as the impact modern humans have on this amount by holding back sediment in dams, counteracted with increased development of erosion patterns.
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