Shahrud (river) explained

The Shahrood or Shah-Rud (Persian: شاهرود, Shāhrūd, literally meaning The great river or the river of the king), also translated as Shah River, is a river of northern Iran.

Course

The Shahrood originates on the slopes of the Takht-e Suleyman Massif at 4,850 m. (36.3667°N 108°W).[1] The Taleqan and Alamut rivers conjoin in the village of Shirkou to form the Shahrud river.[2] The Alamut river, the northern tributary, starts near the summit of Alam-Kuh, the second highest peak in Iran, and flows through a steep gorges.[3] The Shahrood then flows westward through the southern Alborz mountain range to its confluence with the Sefid River. It is a right-hand tributary of the Sefid, which then flows north through the Alborz into the Caspian Sea.

The Shahrood is about 175km (109miles) long.[1]

Central Alborz mountain range map

The Shahrood is #12 on the map's left.

External links

Notes and References

  1. http://www.briancoad.com/introduction/caspianseabasin.htm "Introduction - Drainage Basins - Caspian Sea"
  2. Campbell, Anthony (2004) "A Visit to Alamut (1966)" The Assassins of Alamut p. 6.
  3. Book: Fisher, W. B.. 1. Cambridge University Press. 978-1-139-05492-8. 1–110. Fisher. W. B. . The Cambridge History of Iran. Physical geography. Cambridge. 2022-05-29. 1968-10-01. https://www.cambridge.org/core/product/identifier/CBO9781139054928A005/type/book_part.