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Winds may erode, transport, and deposit materials and are effective agents in regions with sparse vegetation, a lack of soil moisture and a large supply of unconsolidated sediments. Although water is a much more powerful eroding force than wind, aeolian processes are important in arid environments such as deserts. [2]
Aeolian landforms, or Eolian landforms, are produced by either the erosive or depositive action of wind. These features may be built up from sand or snow , [ 1 ] or eroded into rock, snow, or ice. Aeolian landforms are commonly observed in sandy deserts and on frozen lakes or sea ice and have been observed and studied around Earth and on other ...
The name Aeolian (lit. ' of the wind ') derives from the Greek name Aeolus, aiolos (αίολος) literally meaning "changeable", "quickly moving". [7] They spoke an Ancient Greek dialect that is referred to as Aeolic. [2] According to Herodotus, it was said that the Aeolians were previously called Pelasgians. [8]
Aeolis (/ ˈ iː ə l ɪ s /; Ancient Greek: Αἰολίς, romanized: Aiolís), or Aeolia (/ iː ˈ oʊ l i ə /; Ancient Greek: Αἰολία, romanized: Aiolía), was an area that comprised the west and northwestern region of Asia Minor (modern-day Turkey), mostly along the coast, and also several offshore islands (particularly Lesbos), where the Aeolian Greek city-states were located.
The name is from the Spanish word placer, meaning "alluvial sand". Placer mining is an important source of gold, and was the main technique used in the early years of many gold rushes, including the California Gold Rush. Types of placer deposits include alluvium, eluvium, beach placers, aeolian placers and paleo-placers. [2]
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