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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.
The Dorian mode is very similar to the modern natural minor scale (see Aeolian mode below). The only difference with respect to the natural minor scale is in the sixth scale degree, which is a major sixth (M6) above the tonic, rather than a minor sixth (m6). Tonic triad: Dm; Tonic seventh chord: Dm 7; Dominant triad: Am
[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 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). Winds may erode , transport, and deposit materials and are effective agents in regions with sparse vegetation , a lack of soil moisture and a large ...
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 .
The half diminished scale is a seven-note musical scale.It is more commonly known as the Locrian ♯ 2 scale [1] or the Aeolian ♭ 5 scale, names that avoid confusion with the diminished scale and the half-diminished seventh chord (minor seventh, diminished fifth).
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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 ...