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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.
While the term "mode" is still most commonly understood to refer to Ionian, Dorian, Phrygian, Lydian, Mixolydian, Aeolian, or Locrian modes in the diatonic scale; in modern music theory the word "mode" is also often used differently, to mean scales other than the diatonic.
Within the diatonic modes of the major scale, in addition to the Aeolian mode (which is the natural minor scale), the Dorian mode and the Phrygian mode also fall under this definition. Conversely, the Locrian mode has a minor third, but a diminished fifth (thus containing a diminished triad ), and is therefore not commonly referred to as a ...
Hypoaeolian mode on A Play ⓘ.. Hypoaeolian mode, literally meaning "below Aeolian", is the name assigned by Henricus Glareanus in his Dodecachordon (1547) to the musical plagal mode on A, which uses the diatonic octave species from E to the E an octave above, divided by the final into a second-species fourth (semitone–tone–tone) plus a first-species fifth (tone–semitone–tone–tone ...
The Aeolian dominant scale (Aeolian ♯ 3 scale), Mixolydian ♭ 6 scale, descending melodic major scale, or Hindu scale [1] [2] is the fifth mode of the ascending melodic minor scale. It is named Aeolian dominant because its sound derives from having a dominant seventh chord on the tonic in the context of what is otherwise the Aeolian mode .
[4] The actual meaning of the term "Aeolian cadence" is that a major key song resolves on the vi chord, which is the tonic chord of the relative minor key (the Mahler ends on the major tonic with an "added 6th," not on a VI chord.) The term derives from the fact that the Aeolian mode is rooted on the sixth step of the major scale.
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 ...
Eolianite or aeolianite is any rock formed by the lithification of sediment deposited by aeolian processes; that is, the wind. In common use, however, the term refers specifically to the most common form of eolianite: coastal limestone consisting of carbonate sediment of shallow marine biogenic origin, formed into coastal dunes by the wind, and ...
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