Kalivian Mountains: Difference between revisions

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| photo = Ts'gaich'ra as seen from aircraft Tsgaichra.jpg

| photo_caption = Aerial view of Ts'gaich'ra and surrounding landscape

| country1 = [[Oscrelia]][[~~Baykalia~~]][[Great Morstaybishlia]][[North Ethalrian Confederacy]][[Thalria]][[Nolova]][[Tuvaltastan]]

| country1 = [[Oscrelia]][[Biramura]][[Great Morstaybishlia]][[North Ethalrian Confederacy]][[Thalria]][[Nolova]][[Tuvaltastan]]

| region_type = [[Wikipedia:Continent|Continent]]

| region = [[Aurora]]

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| highest = Ts'gaich’ra

| elevation_m = 6321

| highest_location = [[~~Baykalia~~]]

| highest_location = [[Biramura]]

| coordinates =

| range_coordinates =

Line 20:

| 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]], [[~~Baykalia~~]], [[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.

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]]

@@ Line 4: / Line 4: @@
 | photo             = Ts'gaich'ra as seen from aircraft Tsgaichra.jpg
 | photo_caption     = Aerial view of Ts'gaich'ra and surrounding landscape
-| country1          = [[Oscrelia]]</br >[[Baykalia]]</br >[[Great Morstaybishlia]]</br>[[North Ethalrian Confederacy]]</br >[[Thalria]]</br >[[Nolova]]</br >[[Tuvaltastan]]
+| country1          = [[Oscrelia]]</br >[[Biramura]]</br >[[Great Morstaybishlia]]</br>[[North Ethalrian Confederacy]]</br >[[Thalria]]</br >[[Nolova]]</br >[[Tuvaltastan]]
 | region_type       = [[Wikipedia:Continent|Continent]]
 | region            = [[Aurora]]
@@ Line 10: / Line 10: @@
 | highest           = Ts'gaich’ra
 | elevation_m       = 6321
-| highest_location  = [[Baykalia]]
+| highest_location  = [[Biramura]]
 | coordinates       =
 | range_coordinates =
@@ Line 20: / Line 20: @@
 | 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]], [[Baykalia]], [[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.
+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]]

Kalivian Mountains: Difference between revisions

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