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=
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;Coniferous North
 +
;Maritime Northwest
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;Southern Disdrire Forest (includes Skelkast Forest)
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;Marshes of Baihu
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;The Amosgire
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;Ithrad Mountains
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;Dúrandworese Plains
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;Lake Lisgoria
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;Gorrhevia
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;Southeastern Pytharnia
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;Ambrulia
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;Shadevan Delta
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;Pytharnee Dromb Mountains
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=See Also=
 
=See Also=

Revision as of 15:16, 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

Coniferous North
Maritime Northwest
Southern Disdrire Forest (includes Skelkast Forest)
Marshes of Baihu
The Amosgire
Ithrad Mountains
Dúrandworese Plains
Lake Lisgoria
Gorrhevia
Southeastern Pytharnia
Ambrulia
Shadevan Delta
Pytharnee Dromb Mountains


See Also