User:VectorGraphics/Latitude: Difference between revisions
No edit summary |
No edit summary |
||
| Line 11: | Line 11: | ||
Medial pairs with a higher latitude than ±45° tend to sound more dissonant against the axis or root than lower-latitude medials, and extremely low-latitude interval pairs may not sound distinct from each other. Higher latitude enables "cross-tonality", where both intervals in the pair can be played at once in the same chord, as in suspended or [[Arto and tendo theory|arto/tendo]] chords. | Medial pairs with a higher latitude than ±45° tend to sound more dissonant against the axis or root than lower-latitude medials, and extremely low-latitude interval pairs may not sound distinct from each other. Higher latitude enables "cross-tonality", where both intervals in the pair can be played at once in the same chord, as in suspended or [[Arto and tendo theory|arto/tendo]] chords. | ||
Here is a table of the latitude of medials up to | Here is a table of the latitude of medials up to ±30° in various EDOs, with respect to their fifth as the axis: | ||
{| class="wikitable" | |||
!Fifth size in edosteps | |||
!Edos | |||
!Latitude (±n°) | |||
|- | |||
|3 | |||
|5 | |||
|30 | |||
|- | |||
|4 | |||
|7 | |||
|0 | |||
|- | |||
|5 | |||
|9 | |||
|18 | |||
|- | |||
|6 | |||
|10 | |||
|0, 30 | |||
|- | |||
|7 | |||
|12 | |||
|12.8 | |||
|- | |||
|8 | |||
|13, 14 | |||
|0, 22.5 | |||
|- | |||
|9 | |||
|15, 16 | |||
|10, 30 | |||
|- | |||
|10 | |||
|17, 18 | |||
|0, 18 | |||
|- | |||
|11 | |||
|18, 19 | |||
|8.2, 24.5 | |||
|- | |||
|13 | |||
|22, 23 | |||
|6.9, 20.8 | |||
|- | |||
|14 | |||
|23, 24, 25 | |||
|0, 12.8, 25.7 | |||
|- | |||
|15 | |||
|25, 26, 27 | |||
|6, 18, 30 | |||
|- | |||
|16 | |||
|26, 27, 28 | |||
|0, 11.3, 22.5 | |||
|- | |||
|17 | |||
|28, 29, 30 | |||
|5.3, 15.9, 26.5 | |||
|- | |||
|18 | |||
|30, 31, 32 | |||
|0, 10, 20, 30 | |||
|- | |||
|20 | |||
|33, 34, 35, 36 | |||
|0, 9, 18, 27 | |||
|- | |||
|24 | |||
|39, 40, 41, 42, 43 | |||
|0, 7.5, 15, 22.5, 30 | |||
|- | |||
|31 | |||
|51, 52, 53, 54, 55, 56 | |||
|2.9, 8.7, 14.5, 20.3, 26.1 | |||
|} | |||
== Latitude-based interval regions == | == Latitude-based interval regions == | ||
Names can be given to intervals based on latitude. A table is provided here for fifths: | Names can be given to intervals based on latitude. A table is provided here for fifths: | ||
{| class="wikitable" | {| class="wikitable" | ||
|+ | |+ | ||
! | !Latitude | ||
!Major name | !Major name | ||
!Minor name | !Minor name | ||
| Line 25: | Line 100: | ||
!Type | !Type | ||
|- | |- | ||
| | |±0 to 3° | ||
|(Tendo)-neutral third | |(Tendo)-neutral third | ||
|(Arto)-neutral third | |(Arto)-neutral third | ||
| Line 31: | Line 106: | ||
| rowspan="7" |Third | | rowspan="7" |Third | ||
|- | |- | ||
| | |±3 to 7° | ||
|Submajor third | |Submajor third | ||
|Supraminor third | |Supraminor third | ||
|Intraclassical thirds | |Intraclassical thirds | ||
|- | |- | ||
| | |±7 to 12° | ||
|Classical major third | |Classical major third | ||
|Classical minor third | |Classical minor third | ||
|Classical thirds | |Classical thirds | ||
|- | |- | ||
| | |±12 to 16° | ||
|Pythagorean major third | |Pythagorean major third | ||
|Pythagorean minor third | |Pythagorean minor third | ||
|Pythagorean thirds | |Pythagorean thirds | ||
|- | |- | ||
| | |±16 to 20° | ||
|Neogothic major third | |Neogothic major third | ||
|Neogothic minor third | |Neogothic minor third | ||
|Neogothic thirds | |Neogothic thirds | ||
|- | |- | ||
| | |±20 to 24° | ||
|Septimal major third, supermajor third | |Septimal major third, supermajor third | ||
|Septimal minor third, subminor third | |Septimal minor third, subminor third | ||
|Septimal thirds | |Septimal thirds | ||
|- | |- | ||
| | |±24 to 28° | ||
|Tendo third, ultramajor third | |Tendo third, ultramajor third | ||
|Arto third, inframinor third | |Arto third, inframinor third | ||
|Tridecimal thirds/[[Interseptimal interval|interseptimals]] | |Tridecimal thirds/[[Interseptimal interval|interseptimals]] | ||
|- | |- | ||
| | |±28 to 32° | ||
|Major paraslendric | |Major paraslendric | ||
|Minor paraslendric | |Minor paraslendric | ||
| Line 67: | Line 142: | ||
| rowspan="6" |Second/fourth | | rowspan="6" |Second/fourth | ||
|- | |- | ||
| | |±32 to 36° | ||
|Supraslendric | |Supraslendric | ||
|Subslendric | |Subslendric | ||
|Extraslendrics | |Extraslendrics | ||
|- | |- | ||
| | |±36 to 40° | ||
|Major suspended | |Major suspended | ||
|Minor suspended | |Minor suspended | ||
|Suspendeds | |Suspendeds | ||
|- | |- | ||
| | |±40 to 44° | ||
|Suprasuspended | |Suprasuspended | ||
|Subsuspended | |Subsuspended | ||
|Extrasuspendeds | |Extrasuspendeds | ||
|- | |- | ||
| | |±44 to 48° | ||
|Major paratetracot | |Major paratetracot | ||
|Minor paratetracot | |Minor paratetracot | ||
|Paratetracots | |Paratetracots | ||
|- | |- | ||
| | |Beyond ±48° | ||
| colspan="3" | - | | colspan="3" | - | ||
|} | |} | ||
Diatonic and antidiatonic fifths can also be categorized by the | Diatonic and antidiatonic fifths can also be categorized by the latitude of the medials they generate: | ||
{| class="wikitable" | {| class="wikitable" | ||
|Third type | |Third type | ||
| Line 100: | Line 175: | ||
|Interseptimal | |Interseptimal | ||
|Inframedio | |Inframedio | ||
|654.6- | |654.6-660.5 | ||
|11edo | |11edo | ||
|- | |- | ||
|Septimal | |Septimal | ||
|Avila | |Avila | ||
| | |660.5-664.6 | ||
|29edo | |29edo | ||
|- | |- | ||
|Neogothic | |Neogothic | ||
|Pelogic | |Pelogic | ||
| | |664.6-668.7 | ||
|9edo | |9edo | ||
|- | |- | ||
|Pythagorean | |Pythagorean | ||
|Mediocratic | |Mediocratic | ||
| | |668.7-672.9 | ||
|25edo | |25edo | ||
|- | |- | ||
|Classical | |Classical | ||
|Mavila | |Mavila | ||
| | |672.9-678.2 | ||
|16edo | |16edo | ||
|- | |- | ||
|Intraclassical | |Intraclassical | ||
|Sharpmavila | |Sharpmavila | ||
|678. | |678.2-682.5 | ||
|30edo | |30edo | ||
|- | |- | ||
|Neutral | |Neutral | ||
|Neutral | |Neutral | ||
|682. | |682.5-689 | ||
|7edo | |7edo | ||
|- | |- | ||
|Intraclassical | |Intraclassical | ||
|Flattone | |Flattone | ||
| | |689-693.4 | ||
|26edo | |26edo | ||
|- | |- | ||
|Classical | |Classical | ||
|Meantone | |Meantone | ||
| | |693.4-699 | ||
|19edo | |19edo | ||
|- | |- | ||
|Pythagorean | |Pythagorean | ||
|Pythagorean | |Pythagorean | ||
| | |699-703.6 | ||
|12edo | |12edo | ||
|- | |- | ||
|Neogothic | |Neogothic | ||
|Neogothic | |Neogothic | ||
| | |703.6-708.2 | ||
|17edo | |17edo | ||
|- | |- | ||
|Septimal | |Septimal | ||
|Archy | |Archy | ||
| | |708.2-712.8 | ||
|22edo | |22edo | ||
|- | |- | ||
|Interseptimal | |Interseptimal | ||
|Ultrapyth | |Ultrapyth | ||
| | |712.8-720 | ||
|5edo | |5edo | ||
|} | |} | ||
| Line 167: | Line 242: | ||
[[Category:Terms]] | [[Category:Terms]] | ||
== | == Triads == | ||
Just triads containing arithmetic frequency divisions are always "major"; how major it is can be characterized by latitude. | |||
{| class="wikitable" | |||
|+ | |||
!Name | |||
!Triad | |||
!Latitude of medial | |||
|- | |||
| | |||
|1:3:5 | |||
|32.8° | |||
|- | |||
| | |||
|1:2:3 | |||
|23.5° | |||
|- | |||
| | |||
|3:5:7 | |||
|18.5° | |||
|- | |||
| | |||
|2:3:4 | |||
|15.3° | |||
|- | |||
| | |||
|5:7:9 | |||
|13° | |||
|- | |||
|Inverted major triad | |||
|3:4:5 | |||
|11.4° | |||
|- | |||
| | |||
|7:9:11 | |||
|10.1° | |||
|- | |||
|Major triad | |||
|4:5:6 | |||
|9.1° | |||
|- | |||
| | |||
|9:11:13 | |||
|8.2° | |||
|- | |||
| | |||
|5:6:7 | |||
|7.5° | |||
|- | |||
| | |||
|11:13:15 | |||
|7° | |||
|- | |||
|Quartal triad | |||
|6:7:8 | |||
|6.5° | |||
|- | |||
| | |||
|13:15:17 | |||
|6° | |||
|- | |||
| | |||
|7:8:9 | |||
|5.6° | |||
|- | |||
| | |||
|15:17:19 | |||
|5.3° | |||
|- | |||
| | |||
|8:9:10 | |||
|5° | |||
|} | |||