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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).
In linguistics, Aeolic Greek (/ iː ˈ ɒ l ɪ k /), also known as Aeolian (/ iː ˈ oʊ l i ə n /), Lesbian or Lesbic dialect, is the set of dialects of Ancient Greek spoken mainly in Boeotia; in Thessaly; in the Aegean island of Lesbos; and in the Greek colonies of Aeolis in Anatolia and adjoining islands.
The Aeolian mode is the sixth mode of the major scale, that is, it is formed by starting on the sixth degree of the major scale. For example, if the Aeolian mode is used in its all-white-note pitch based on A, this would be an A-minor triad, which would be the submediant in the relative major key of C major.
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]
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 ...
Aeolian or eolian (depending on the parsing of æ) is the term for sediment transport by wind. This process results in the formation of ripples and sand dunes. Typically, the size of the transported sediment is fine sand (<1 mm) and smaller, because air is a fluid with low density and viscosity, and can therefore not exert very much shear on ...
Aeolian dialect, a dialect of Ancient Greek; Aeolian Islands, islands in the Tyrrhenian Sea, named after Aeolus the ruler of the winds; Aeolian or Aeolic order, an early order of Classical architecture; Aeolian landform, landforms, such as sand dunes, formed by wind; Aeolian processes, eolian sedimentation, wind-generated geologic processes
The Aeolian Islands (/ iː ˈ oʊ l i ən / ee-OH-lee-ən; Italian: Isole Eolie [ˈiːzole eˈɔːlje]; Sicilian: Ìsuli Eoli), sometimes referred to as the Lipari Islands or Lipari group (/ ˈ l ɪ p ə r i / LIP-ə-ree, Italian:) after their largest island, are a volcanic archipelago in the Tyrrhenian Sea north of Sicily, said to be named after Aeolus, the mythical ruler of the winds. [1]