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Examples of Erosional Landforms; Landform Description Image Deflation basin: A depression in the land that can be found in deserts due to the removal of particles by wind; it can also be referred to as a "blowout". Blowout outside of Earth, Texas: Ventifacts: Rock samples that demonstrate the erosion caused by aeolian processes over time.
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).
Aeolian landform – Landforms produced by action of the winds include: Dry lake – Area that contained a standing surface water body; Sandhill – Type of ecological community or xeric wildfire-maintained ecosystem; Ventifact – Rock that has been eroded by wind-driven sand or ice crystals; Yardang – Streamlined aeolian landform
The Bibliography of Aeolian Research (BAR) is a comprehensive 2015 bibliography focused on the study of the detachment, transport, and deposition of sediments by wind. [ 1 ] Aeolian research is a sub-discipline of the physical sciences that focuses on the activity of the winds, with an emphasis on the winds' ability to interact with and shape ...
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It is unclear to which extent different rauks in Gotland started to form from a cliffed coast, a dissected coast or from glacial landforms. [5] A comparison of photographs from 1900 and from 1966 has shown that some rauks had been destroyed during that period. [5] Carl Linnaeus, who visited Gotland in 1741, was the first scientist to describe ...
Bank erosion is the wearing away of the banks of a stream or river. This is distinguished from changes on the bed of the watercourse, which is referred to as scour. Erosion and changes in the form of river banks may be measured by inserting metal rods into the bank and marking the position of the bank surface along the rods at different times. [17]
Transverse aeolian ridges There is some thought that transverse aeolian ridges are a form of fossilized ripple, but there is no conclusive evidence so far. Fluid drag ripples Also known as aerodynamic ripples, these are formed with fine, well-sorted grain particles accompanied by high velocity winds which result in long, flat ripples. The flat ...
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