Tzʌxîdȧr: Difference between revisions
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== Geology == | == Geology == | ||
Tzʌxîdȧr has been largely geologically inactive since the early AE. However, it is full of interesting geological features from the time of its creation. | |||
=== Formation === | === Formation === | ||
Tzʌxîdȧr was formed when the Xag̈iar plate ''Av̆òŋcuź'' collided with the plate ''Gôleɣ'', creating a large zone of exposed magma | Tzʌxîdȧr was formed when the Xag̈iar plate ''Av̆òŋcuź'' collided with the plate ''Gôleɣ'', creating a large zone of exposed magma. The magma was uplifted by the Tzʌxîdȧr Process, which is named after the mountain, and formed the volcano over millions of years. | ||
=== Volcanic Activity === | === Volcanic Activity === | ||
=== Mineral Deposits === | === Mineral Deposits === | ||
=== The Seam of Koigîxmór === | |||
== History and Culture == | == History and Culture == | ||
Revision as of 20:35, 26 February 2023
Tzʌxîdȧr ([ ̬ʦʌ.xi˨˥˨.d̪a͡ʭr̪]; mXOV(x) "Infinite Mountain") is an extinct sheild volcano and the largest mountain in the planes.
Tzʌxîdȧr stands 24,875 meters tall, nearly three times the height of Mount Everest. However, as it is a sheild-shaped mountain, its average slope is only six percent. Tzʌxîdȧr is 612 kilometers in diameter, on average.
Geology
Tzʌxîdȧr has been largely geologically inactive since the early AE. However, it is full of interesting geological features from the time of its creation.
Formation
Tzʌxîdȧr was formed when the Xag̈iar plate Av̆òŋcuź collided with the plate Gôleɣ, creating a large zone of exposed magma. The magma was uplifted by the Tzʌxîdȧr Process, which is named after the mountain, and formed the volcano over millions of years.
Volcanic Activity
Mineral Deposits
The Seam of Koigîxmór
History and Culture
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Religious Significance
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Measuring Tzʌxîdȧr's Height
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Other Names
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