Halil River
Halīl River or HalīlRood (also Haliri River, known as the Kharaw or ZarDasht River in its upper reaches) is a river stretching for some 390 kilometres (240 mi) running in the Baft, Jiroft and Kahnuj districts of Kerman Province, Iran.
| Halil River Haliri River, Kharaw or ZarDasht River (upper reaches) | |
|---|---|
Zardasht river, the longest tributary of Halil river | |
| Location | |
| Country | Iran |
| Province | Kerman |
| Physical characteristics | |
| Source | Kuh-e Shah mountain |
| • location | 20 km (12 mi) north-east of Baft |
| • elevation | 4,400 m (14,400 ft) above sea level |
| Mouth | Hamun-e Jaz Murian |
• location | Baluchistan |
| Length | 390 km (240 mi) |
| Basin features | |
| Tributaries | |
| • left | Zardasht River, Rabor River |
| • right | Narab River |
| Longest tributary | Zardasht River |
The Halil rises at 4,400 metres (14,400 ft) above sea level in the Kuh-e shah mountain about 20 kilometres (12 mi) to the north-east of Baft, flowing to the south-west until it is joined by the Zardasht and Rabor rivers. Turning towards the south, it flows along the foothills of the Bahr aseman mountains, then to the south-east until Jiroft Dam, which is 130 metres (430 ft) high, about 40 kilometres (25 mi) upstream of Jiroft (28°51′30″N 57°28′0″E) at the confluence with the Narab. It passes some 15 kilometres (9 mi) east of Kahnuj and terminates in the Hamun-e Jaz Murian of Baluchistan.
The climate of the Halil Rud or Halilrood (Rud or Rood means "river" in Persian) basin is extremely hot in summer and of moderate temperature in winter. 57 °C (135 °F) in August 1933.
The Halil riverbanks are subject to periodical flooding, including the historical flood which destroyed Jiroft in ca. AD 1000, and one in 1993.