Difference between revisions of "Pytharniaca"

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Magdeologers believe the slow action of Pytharniaca is causing the uplift of the [[Jaggudorn Mountains]], transpiring over tens of thousands of years or even a million or more years.
 
Magdeologers believe the slow action of Pytharniaca is causing the uplift of the [[Jaggudorn Mountains]], transpiring over tens of thousands of years or even a million or more years.
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=Regions of Pytharniaca=
 
=Regions of Pytharniaca=
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[[File:MapGeoRegionsPytharnia.png|thumb|200px|The bio-regions of Pytharnia are based upon prevalent landforms and forestation as well as river basins.]]
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*Ambrulia
 
*Ambrulia
 
*The Amosgire
 
*The Amosgire

Revision as of 15:56, 28 October 2024

An asdarographic term that refers to the entire subcontinent of Pytharnia and used to disambiguate from the term Pytharnia that can also mean several political and cultural entities. Pytharniaca is the preferred term in the study of magdeology for the whole subcontinent.

Pytharniaca is a subcontinent of the northern hemisphere, colliding with the continent of Asdauria over a period of hundreds of thousands of years.

Magdeologers believe the slow action of Pytharniaca is causing the uplift of the Jaggudorn Mountains, transpiring over tens of thousands of years or even a million or more years.


Regions of Pytharniaca

The bio-regions of Pytharnia are based upon prevalent landforms and forestation as well as river basins.
  • Ambrulia
  • The Amosgire
  • Coniferous North
  • Dúrandworese Plains
  • ♦Durrhaunvish Drainage Basin
  • Gorrhevia
  • ♦High Lake
  • ♦Hyndernuse-Nystasy
  • Ithrad Mountains
  • Lake Lisgoria
  • Maritime Northwest
  • Marshes of Baihu
  • ♦Old Kemeria
  • Pytharnee Dromb Mountains
  • Shadevan Delta
  • Southern Disdrire Forest (includes Skelkast Forest)
  • Southwestern Pytharnia

See Also