Kalivian Mountains: Difference between revisions

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{{Infobox mountain
| name = Kalivian Mountains
| native_name = Ts'k’edeli
| photo = Ts'gaich'ra as seen from aircraft Tsgaichra.jpg
| photo_caption = Aerial view of [[Ts'gaich'ra]] and surrounding landscape
| country1 = [[Oscrelia]]</br >[[Biramura]]</br >[[Great Morstaybishlia]]</br>[[North Ethalrian Confederacy]]</br >[[Thalria]]</br >[[Nolova]]</br >[[Tuvaltastan]]
| country1 = [[Oscrelia]]
| country2 region_type = [[BaykaliaWikipedia:Continent|Continent]]
| country3 = [[Morstaybishlia]]
| country4 = [[North Ethalrian Confederacy]]
| country5 = [[Thalria]]
| country6 = [[Nolova]]
| country7 = [[Tuvaltastan]]
| region_type = [[Continent]]
| region = [[Aurora]]
| border =
| highest = [[Ts'gaich’ra]]
| elevation_m = 6321
| highest_location = [[BaykaliaBiramura]]
| coordinates = {{coord|27|59|N|86|55|E|region:IN|format=dms|display=inline,title}}
| range_coordinates =
| length_km = 2470
| geology = [[Wikipedia:Metamorphic rock|Metamorphic]], [[Wikipedia:Sedimentary rock|sedimentary]]
| period =
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| map_caption = The general location of the Kalivian mountain range
}}
The '''Kalivian Mountains''' are a [[wikipedia:Mountain range|mountain range]] system that lies entirely within eastern [[Aurora]], across eight different countries: [[Oscrelia]], [[Biramura]], [[Great Morstaybishlia]], [[North Ethalrian Confederacy|The North Ethalrian Confederacy]], [[Thalria]], [[Nolova]], and [[Tuvaltastan]]. The mountains were formed approximately 250-180 million years ago as the Auroran and Salovic tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Ts'gaich'ra and lower elevations becoming isolated, like the Posolic Valley.
 
[[Category:Salovian Places]] [[Category:Aurora]]
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