Difference between revisions of "Phaswa Mountains"

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m (Arnoldii moved page The Ungagon Range to Darkine over redirect: no)
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{{Infobox mountain range
{{Infobox mountain range
|name                  = The Ungagon Range
|name                  = Darkine
|other_name            =  
|other_name            =  
|photo                  = Darkine-one.jpg
|photo                  = Darkine-one.jpg
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<!-- Geography -->
<!-- Geography -->
|country_type          = Countries
|country1              = {{flag|Hyuy En}}
|country                =
|country2              = {{flag|Liosol}}
{{Collapsible list
|country3              = {{flag|Karduv}}
  | title = 5 countries
|country4              = {{flag|Qonklaks}}
  | {{flag|Hyuy En}}
|country5               = {{flag|Suijo}}
  | {{flag|Liosol}}
|location               = [[Soltenna]]
  | {{flag|Karduv}}
  | {{flag|Qonklaks}}
}}
|country1               =  
|country2               =
|region_type            = Continent
|region                = [[Soltenna]]
|region1                =
|border                =  
|border                =  
|border1                =  
|border1                =  
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}}
}}


The '''Ungagon Range''' is a mountain range separating West and East [[Soltenna]]. It extends from northeastern [[Qonklaks]] to central western [[Liosol]], dividing [[Hyuy En]] into two geographically separate regions, and bordering the Rapheng and Laun ranges. The Ungagon hosts most of Soltenna's highest peaks and all of the region's 6000m peaks outside [[Mount Bevaseiyrna]], including Soltenna's second highest point in Mount Dyinsup whose height above sea level reached {{convert|6552|m|ft}}. Its English name is derived from the [[Broad Tolec language|Tolec]] and [[Qonklese language|Qonklese]] protonym "Ungu Agon", which means "gold mountain(s)".
The '''Darkine''' is a mountain range separating West and East [[Soltenna]]. It extends from northeastern [[Qonklaks]] to central western [[Liosol]], dividing [[Hyuy En]] into two geographically separate regions, and bordering the Rapheng and Lion ranges. The Darkine hosts most of Soltenna's highest peaks and all of the region's six-thousander peaks outside [[Mount Bevaseiyrna]], including Soltenna's second highest point in Mount Dyinsup whose height above sea level reached {{convert|6552|m|ft}}.


==Geology==
==Geology==
The Ungagon's geological history dates back to the (Paleozoic) era when the mountain was formed. It formed largely through collision of the (West Soltennan) and Rietic plates during the Darkine orogeny, which also formed the Rietic Mountains that is believed to have been the part of the Darkine before a rift valley comprising [[Lake Soltenna]] was formed around 50 million years ago, splitting the Rietic eastwards. This split increased volcanic activity of both mountain ranges. The Ungagon's highest point, Mount Dyinsup, is estimated to move at an annual rate of {{convert|1.4|mm|in|abbr=on}} upwards and {{convert|3.5|mm|in|abbr=on}} northwards.
The Darkine's geological history dates back to the (Paleozoic) era when the mountain was formed. It formed largely through collision of the (West Soltennan) and Rietic plates during the Darkine orogeny, which also formed the Rietic Mountains that is believed to have been the part of the Darkine before a rift valley comprising [[Lake Soltenna]] was formed around 50 million years ago, splitting the Rietic eastwards. This split increased volcanic activity of both mountain ranges. The Darkine's highest point, Mount Dyinsup, is estimated to move at an annual rate of {{convert|1.4|mm|in|abbr=on}} upwards and {{convert|3.5|mm|in|abbr=on}} northwards.


Most volcanoes in the region are now dormant, but is still subject to regular strong earthquakes from its tectonic activity. Darkine earthquakes are known to have caused damage indirectly through avalanches.
Most volcanoes in the region are now dormant, but is still subject to regular strong earthquakes from its tectonic activity. Darkine earthquakes are known to have caused damage indirectly through avalanches.
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Cold continental and semi-arid climates dominate the climate of the Darkine. Average annual temperature in the lakeside Hux Mlak, in comparison, is {{convert|14|C|F}}, while in Khin Mlak, average annual temperature falls to {{convert|6|C|F}}. Furthermore to the Mount Dyinsup slopes, average temperatures reached as low as {{convert|-5|C|F}}.
Cold continental and semi-arid climates dominate the climate of the Darkine. Average annual temperature in the lakeside Hux Mlak, in comparison, is {{convert|14|C|F}}, while in Khin Mlak, average annual temperature falls to {{convert|6|C|F}}. Furthermore to the Mount Dyinsup slopes, average temperatures reached as low as {{convert|-5|C|F}}.


Snow caps of the Ungagon Range feed three major rivers: the Zranx, Methinya, and Mang rivers. Due to the cold climate, the Ungagon highlands are overall scarce in vegetation, with most of the area being above the [[Wikipedia:Tree line|tree line]]. The Ungagon populace are thus reliant on these rivers to live and are scarce in numbers. Although minor, [[Wikipedia:Rain shadow|rain shadow effects]] caused by the Ungagon made some areas west of the range{{emdash}}northern [[Hyuy En]] and extreme eastern [[Karduv]]{{emdash}}drier than the eastern counterparts, which comprises the western half of the [[Lake Soltenna]] basin.
Snow caps of the Darkine Range feed three major rivers: the Zranx, Methinya, and Mang rivers. Due to the cold climate, the Darkine highlands are overall scarce in vegetation, with most of the area being above the [[Wikipedia:Tree line|tree line]]. The Darkine populace are thus reliant on these rivers to live and are scarce in numbers. Although minor, [[Wikipedia:Rain shadow|rain shadow effects]] caused by the Darkine made some areas west of the range{{emdash}}northern [[Hyuy En]] and extreme eastern [[Karduv]]{{emdash}}drier than the eastern counterparts, which comprises the western half of the [[Lake Soltenna]] basin.


==Significance==
==Significance==
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* [[Rietic Mountains]]
* [[Rietic Mountains]]


[[Category:Soltenna]]
[[Category:Geography of Soltenna]]
[[Category:Mountains]]
[[Category:Mountains]]

Revision as of 01:30, 22 July 2018

Darkine
Darkine-one.jpg
Highest point
PeakMount Dyinsup
46°40'43"N 12°2'29"W
Elevation6,552 m (21,496 ft)
Geography
LocationSoltenna
Countries

The Darkine is a mountain range separating West and East Soltenna. It extends from northeastern Qonklaks to central western Liosol, dividing Hyuy En into two geographically separate regions, and bordering the Rapheng and Lion ranges. The Darkine hosts most of Soltenna's highest peaks and all of the region's six-thousander peaks outside Mount Bevaseiyrna, including Soltenna's second highest point in Mount Dyinsup whose height above sea level reached 6,552 metres (21,496 ft).

Geology

The Darkine's geological history dates back to the (Paleozoic) era when the mountain was formed. It formed largely through collision of the (West Soltennan) and Rietic plates during the Darkine orogeny, which also formed the Rietic Mountains that is believed to have been the part of the Darkine before a rift valley comprising Lake Soltenna was formed around 50 million years ago, splitting the Rietic eastwards. This split increased volcanic activity of both mountain ranges. The Darkine's highest point, Mount Dyinsup, is estimated to move at an annual rate of 1.4 mm (0.055 in) upwards and 3.5 mm (0.14 in) northwards.

Most volcanoes in the region are now dormant, but is still subject to regular strong earthquakes from its tectonic activity. Darkine earthquakes are known to have caused damage indirectly through avalanches.

Climate

Cold continental and semi-arid climates dominate the climate of the Darkine. Average annual temperature in the lakeside Hux Mlak, in comparison, is 14 °C (57 °F), while in Khin Mlak, average annual temperature falls to 6 °C (43 °F). Furthermore to the Mount Dyinsup slopes, average temperatures reached as low as −5 °C (23 °F).

Snow caps of the Darkine Range feed three major rivers: the Zranx, Methinya, and Mang rivers. Due to the cold climate, the Darkine highlands are overall scarce in vegetation, with most of the area being above the tree line. The Darkine populace are thus reliant on these rivers to live and are scarce in numbers. Although minor, rain shadow effects caused by the Darkine made some areas west of the range—northern Hyuy En and extreme eastern Karduv—drier than the eastern counterparts, which comprises the western half of the Lake Soltenna basin.

Significance

See also