Helmand River

Geography

The Helmand stretches for 1,150 km (710 mi). It rises in the northeastern part of Maidan Wardak Province in the Hindu Kush mountains, about 40 km west of Kabul (34°34′N 68°33′E / 34.567°N 68.550°E), flowing southwestward through Daykundi Province and Uruzgan Province. After passing through the city of Lashkargah in Helmand Province, it enters the desert of Dasht-e Margo, and then flows to the Sistan marshes and the Hamun-i-Helmand lake region around Zabol at the Afghan-Iranian border (31°9′N 61°33′E / 31.150°N 61.550°E). A few smaller rivers such as Tarnak and Arghandab flow into Helmand.

This river, managed by the Helmand and Arghandab Valley Authority, is used extensively for irrigation, although a buildup of mineral salts has decreased its usefulness in watering crops. For much of its length, the Helmand is free of salt. Its waters are essential for farmers in Afghanistan, but it feeds into the Hamun Lake and is also important to farmers in Iran's southeastern Sistan and Baluchistan province.

A number of hydroelectric dams have created artificial reservoirs on some of the Afghanistan's rivers including the Kajaki Dam on the Helmand River. The chief tributary of the Helmand river, the Arghandab River (confluence at 31°27′N 64°23′E / 31.450°N 64.383°E), also has a major dam, north of Kandahar.

History

The Helmand valley region is mentioned by name in the Avesta (Fargard 1:13) as the Aryan land of Haetumant, one of the early centres of the Zoroastrian faith in areas that are now Afghanistan. However, by the late first millennium BC and early first millennium AD, the preponderance of communities of Hindus and Buddhists in the Helmand and Kabul valleys led to Parthians referring to it as India. From 1758 to 1842, the Helmand formed the northern borders of the Brahui Khanate of Kalat.