Tzʌxîdȧr: Difference between revisions
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'''Tzʌxîdȧr''' | {{Infobox Mountain|Name=Tzʌxîdȧr|highest=25,415m|highest location=Tzʌxîdȧr Summit|coords=42°56′12″S 0°0′0″E|coord_system=<br>Xerôj Coordinates (Tzʌxîdȧr defines the prime meridian)|elevation=12,889m|elevation_ref=above|elevation_system=Average Xerôj Elevation|etymology=''tzʌ'' "infinite" + ''xîdȧr'' "mountain" (from mXOV(x))|name1=Kādūghe|source1=Khơlīvh|name2=Dagbyř|source2=Gylhev|name3=Tsokätírh|source3=Old Ẋov̆íì|image=Tzuxidar_map_v1.png|caption=A map of Tzʌxîdȧr}}'''Tzʌxîdȧr''' {{LangSnippet|IPA= ̬ʦʌ.xi˨˥˨.d̪a͡ʭr̪|meaning=Infinite Mountain|langcode=mXOV(x)|langlink=Ẋov̆íì}} 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 == | == 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 === | === Volcanic Activity === | ||
=== Mineral Deposits === | === Mineral Deposits === | ||
=== The Seam of Koigîxmór === | |||
== History and Culture == | == History and Culture == |
Latest revision as of 19:36, 27 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[edit | edit source]
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[edit | edit source]
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[edit | edit source]
Mineral Deposits[edit | edit source]
The Seam of Koigîxmór[edit | edit source]
History and Culture[edit | edit source]
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Religious Significance[edit | edit source]
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Measuring Tzʌxîdȧr's Height[edit | edit source]
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Other Names[edit | edit source]
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