Mansuriyyah: Difference between revisions
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===Formation of Modern Mansuri State=== | ===Formation of Modern Mansuri State=== | ||
==Geography== | |||
Located in Western Siduri, Mansuriyyah host a wide range of different climates and topography. The West has a humid Mediterranean climate, becoming increasingly arid towards the interior. The North is mostly mountainous with temperate climate, transitioning into a continental climate towards the Northeast. | |||
===Climate=== | |||
===Topography=== | |||
===Water=== | |||
With large swathes of Mansuri territory being semi-arid steppes or desert, water sources are of vital importance. The main rivers are the Shabb, running on the South and marking most of the border with Mubata, while the Azraq river, born from the Jibal al-Barad, and crisscrossing Mansuriyyah from the Southeast until the Northwest, where it flows into the Juwayqi Gulf. A number of smaller watercourses flow down from the Matras mountains into the Azraq basin. A number of lakes exist in the Qafqaz highlands in the Northeast. The arid deserts of central Mansuriyyah contain a number of oases but lack permanent water courses, as the few rivers that flow eastward from the Qartaba mounts disappear into the semi-arid plateaus of Badiyat al-Hawram. | |||
===Fauna and Flora=== |
Revision as of 14:36, 24 February 2020
Mansuriyyah is a nation located in the continent of Siduri in Tyran. It borders Ruvelka on the North, Allamunika on the East, and Mubata on the South
History
Prehistory and early history
Al-Bashiri Caliphate
Rawwadid Dynasty
Arkoennite Conquest
Formation of Modern Mansuri State
Geography
Located in Western Siduri, Mansuriyyah host a wide range of different climates and topography. The West has a humid Mediterranean climate, becoming increasingly arid towards the interior. The North is mostly mountainous with temperate climate, transitioning into a continental climate towards the Northeast.
Climate
Topography
Water
With large swathes of Mansuri territory being semi-arid steppes or desert, water sources are of vital importance. The main rivers are the Shabb, running on the South and marking most of the border with Mubata, while the Azraq river, born from the Jibal al-Barad, and crisscrossing Mansuriyyah from the Southeast until the Northwest, where it flows into the Juwayqi Gulf. A number of smaller watercourses flow down from the Matras mountains into the Azraq basin. A number of lakes exist in the Qafqaz highlands in the Northeast. The arid deserts of central Mansuriyyah contain a number of oases but lack permanent water courses, as the few rivers that flow eastward from the Qartaba mounts disappear into the semi-arid plateaus of Badiyat al-Hawram.