This article does not cite any sources. (November 2017) (Learn how and when to remove this template message)
The Rakshan River (Urdu: دریائے رخشن) rises at the Nidoki pass, south-west of Shireza, district Washuk, Balochistan, Pakistan. Under the name of Nag, and running south-westward, it unites with the lop stream at a point to west of Nag-e-Kalat. It then flows west-south-west through the centre of the long valley comprising the Panjgur District, Makran, and parallel with the Siahan Range on the north and Zangi Lak hills on the south. In Rakshan it possesses little or no water, in Panjgur, however, it expands into a series of bright clear pools (kor joh) connected with each other by small water channels running over a pebbly bed. The banks are here bordered with numerous date palms and most of the water is used for irrigation. To the west of Kallag, the last village in Panjgur is Dabbag, where there are more pools and much long grass, tamarisk and kahur trees in which wild pigs were to be found in the early 20th century.
The only considerable tributaries joining the river west of Panjgur are the Mazan Dashtuk from the west, the Askani from the east, and the Gwargo from the south. After traversing Panjgur, the main stream turns northward and joins the Mashkel River from Kuhak on the Iranian side just south of the point where it bursts through the Koh-e-Sabz range by the Tank-e-Grawag or Grawag defile.
The Mashkel River crosses the Siahan Range at Tank-e-Zurrati and runs along the western side of Kharan to the Hamun-i-Mashkel, the total length from the source of the Rakshan being 258 miles.
Through a considerable water course, the banks of the Rakshan are low, shelving and irregular, consisting of hard clay known as kork in the Balochi language. The river carries high floods, but owing to its breadth they never do much harm. The bed contains a little tamarisk or grass to relieve the monotony of the barren region which it traverses. Though the river is easy to cross, dangerous quicksands exist in some places.
In the times of the Malik rulers in the 16th century the river is said to have been dammed by the large band close to Bonistan village, the western part of Issai, the remains of which are still known as Band-e-Gillar.