Murzakar Mountains: Difference between revisions
Appearance
m Text replacement - "Terasil" to "Khamria" |
m Text replacement - "Citadel" to "Așdilu" |
||
| Line 7: | Line 7: | ||
}} | }} | ||
{{Mountain Ranges of Méniail Sections | {{Mountain Ranges of Méniail Sections | ||
|Introduction=The '''Murzkar Mountains''' are a mountain range located to the southwest of the | |Introduction=The '''Murzkar Mountains''' are a mountain range located to the southwest of the Așdilu Mountains. The mountains form the border of [[Khamria]] and [[Balúrail]] and Balúrail and the [[Gosterra]]. Known for their constant mist and fog the slopes are rich in biodiversity. | ||
|Etymology=The name "Murzkar Mountains" derives from the near perpetual mist that blankets the range. | |Etymology=The name "Murzkar Mountains" derives from the near perpetual mist that blankets the range. | ||
|Geography=Numerous rivers and streams flow down the mountainsides, fed by frequent rainfall and the condensation of mist.. | |Geography=Numerous rivers and streams flow down the mountainsides, fed by frequent rainfall and the condensation of mist.. | ||
Latest revision as of 03:15, 29 July 2026
| Murzakar Mountains | |
|---|---|
| Image | |
| Location | Murzkar Mountains in red |
| Realm(s) | Khamria • Balúrail • Gosterra |
Introduction
The Murzkar Mountains are a mountain range located to the southwest of the Așdilu Mountains. The mountains form the border of Khamria and Balúrail and Balúrail and the Gosterra. Known for their constant mist and fog the slopes are rich in biodiversity.
Etymology
The name "Murzkar Mountains" derives from the near perpetual mist that blankets the range.
Geography
Numerous rivers and streams flow down the mountainsides, fed by frequent rainfall and the condensation of mist..
Climate
The climate of the Murzkar Mountains is characterized by high humidity, frequent rain, and a constant presence of mist and fog. The mist, a constant presence due to the mountains’ elevation and proximity to moisture-laden winds coming off the ocean.

