MOS scale: Difference between revisions

Wikispaces>Andrew_Heathwaite
**Imported revision 246086881 - Original comment: **
Wikispaces>genewardsmith
**Imported revision 275397570 - Original comment: **
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<h2>IMPORTED REVISION FROM WIKISPACES</h2>
<h2>IMPORTED REVISION FROM WIKISPACES</h2>
This is an imported revision from Wikispaces. The revision metadata is included below for reference:<br>
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: This revision was by author [[User:Andrew_Heathwaite|Andrew_Heathwaite]] and made on <tt>2011-08-15 16:12:43 UTC</tt>.<br>
: This revision was by author [[User:genewardsmith|genewardsmith]] and made on <tt>2011-11-14 18:48:59 UTC</tt>.<br>
: The original revision id was <tt>246086881</tt>.<br>
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Note that an octave scale with a period a 1/N fraction of an octave will be a MOS if it is a MOS, identically, within each period.
Note that an octave scale with a period a 1/N fraction of an octave will be a MOS if it is a MOS, identically, within each period.


The term MOS and the scale construction method were invented by Erv Wilson in 1975. His original paper can be found here [[http://anaphoria.com/mos.PDF]]. There is also an introduction [[http://anaphoria.com/wilsonintroMOS.html]]. In academic music theory, MOS are known as //well-formed scales// and the introduction of the concept is attributed to a 1989 paper by Norman Carey and David Clampitt. A great deal of interesting work has been done on scales in academic circles extending these ideas.
The term MOS and the scale construction method were invented by Erv Wilson in 1975. His original paper can be found here [[http://anaphoria.com/mos.PDF]]. There is also an introduction [[http://anaphoria.com/wilsonintroMOS.html]]. Wilson considered only MOS with period an octave, and hence some people prefer to use the term [[distributional evenness|distributionally even scale]], with acronym DE, for the more general concept. MOS/DE scales are also sometimes known as //well-formed scales//, the term used in the 1989 paper by Norman Carey and David Clampitt. A great deal of interesting work has been done on scales in academic circles extending these ideas.
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=Mathematical Properties of MOS=  
=Mathematical Properties of MOS=  
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Note that an octave scale with a period a 1/N fraction of an octave will be a MOS if it is a MOS, identically, within each period.&lt;br /&gt;
Note that an octave scale with a period a 1/N fraction of an octave will be a MOS if it is a MOS, identically, within each period.&lt;br /&gt;
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The term MOS and the scale construction method were invented by Erv Wilson in 1975. His original paper can be found here &lt;a class="wiki_link_ext" href="http://anaphoria.com/mos.PDF" rel="nofollow"&gt;http://anaphoria.com/mos.PDF&lt;/a&gt;. There is also an introduction &lt;a class="wiki_link_ext" href="http://anaphoria.com/wilsonintroMOS.html" rel="nofollow"&gt;http://anaphoria.com/wilsonintroMOS.html&lt;/a&gt;. In academic music theory, MOS are known as &lt;em&gt;well-formed scales&lt;/em&gt; and the introduction of the concept is attributed to a 1989 paper by Norman Carey and David Clampitt. A great deal of interesting work has been done on scales in academic circles extending these ideas.&lt;br /&gt;
The term MOS and the scale construction method were invented by Erv Wilson in 1975. His original paper can be found here &lt;a class="wiki_link_ext" href="http://anaphoria.com/mos.PDF" rel="nofollow"&gt;http://anaphoria.com/mos.PDF&lt;/a&gt;. There is also an introduction &lt;a class="wiki_link_ext" href="http://anaphoria.com/wilsonintroMOS.html" rel="nofollow"&gt;http://anaphoria.com/wilsonintroMOS.html&lt;/a&gt;. Wilson considered only MOS with period an octave, and hence some people prefer to use the term &lt;a class="wiki_link" href="/distributional%20evenness"&gt;distributionally even scale&lt;/a&gt;, with acronym DE, for the more general concept. MOS/DE scales are also sometimes known as &lt;em&gt;well-formed scales&lt;/em&gt;, the term used in the 1989 paper by Norman Carey and David Clampitt. A great deal of interesting work has been done on scales in academic circles extending these ideas.&lt;br /&gt;
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