Article · Wikipedia archive · Last revised May 25, 2026

Gilgit River

The Gilgit River is a tributary of the Indus River, flowing through Gilgit Valley of Gilgit-Baltistan, Pakistan. The upper sections of the Gilgit River are also referred to as the Gupis River and Ghizer River.

Last revised
May 25, 2026
Read time
≈ 2 min
Length
467 w
Citations
5
Source
Gilgit River
Course of the Gilgit River
Native nameدریائے گلگت (Urdu)
Location
CountryPakistan
Autonomous territoryGilgit-Baltistan
DistrictsGupis-Yasin, Ghizer and Gilgit
Physical characteristics
Mouth 
 • coordinates
35°44′31″N 74°37′29″E / 35.74194°N 74.62472°E / 35.74194; 74.62472
Length240 km
Basin size
26,159 km2 (10,100 sq mi)
Discharge 
 • locationGilgit Gauging Station, Gilgit
 • average293 m3/s (10,300 cu ft/s)
 • minimum83 m3/s (2,900 cu ft/s)
 • maximum868 m3/s (30,700 cu ft/s)
Discharge 
 • locationAlam Bridge Station, Jaglot
 • average617 m3/s (21,800 cu ft/s)
 • minimum66 m3/s (2,300 cu ft/s)
 • maximum4,834 m3/s (170,700 cu ft/s)
Basin features
ProgressionIndusArabian Sea
Tributaries 
 • rightHunza River
WaterbodiesShandur Lake, Khukush Lake

The Gilgit River (Urdu: دریائے گلگت) is a tributary of the Indus River, flowing through Gilgit Valley of Gilgit-Baltistan, Pakistan.1 The upper sections of the Gilgit River are also referred to as the Gupis River and Ghizer River.

The Gilgit River is a tributary of the Indus River source ↗

Course

Gilgit River flows through various districts including Gupis-Yasin, Ghizer and Gilgit. It originates from Shandur Lake and proceeds to join the Indus River near the towns of Juglot and Bunji. During its course, Yasin River from Yasin Valley and Karambar/Ishkoman River from Karambar Lake in Ishkoman Valley join it. Hunza River is its largest tributary, contributing over half of its mean annual volume. The confluence of Gilgit River with Indus marks the meeting point of three prominent mountain ranges: the Hindu Kush, the Himalayas, and the Karakoram.2

Hydrology

The catchment area of Gilgit River is 26,159 km2 (10,100 sq mi).3 Before the confluence of Gilgit River with Hunza River, its mean annual discharge for the period 1981–2010 at Gilgit Gauging Station is 293 m3/s (10,300 cu ft/s), with a minimum and maximum discharge of 83 m3/s (2,900 cu ft/s) and 868 m3/s (30,700 cu ft/s), respectively.3 After receiving inflow from Hunza, its mean annual discharge for the period 1981–2015 at Alam Bridge Gauging Station was 617 m3/s (21,800 cu ft/s), with a minimum and maximum discharge of 66 m3/s (2,300 cu ft/s) and 4,834 m3/s (170,700 cu ft/s), respectively.1

See also

See also

References

References

  1. Adnan, Muhammad; Nabi, Ghulam; Saleem Poomee, Muhammad; Ashraf, Arshad (2017-09-01). "Snowmelt runoff prediction under changing climate in the Himalayan cryosphere: A case of Gilgit River Basin". Geoscience Frontiers. 8 (5): 941–949. Bibcode:2017GeoFr...8..941A. doi:10.1016/j.gsf.2016.08.008. ISSN 1674-9871.
  2. Adnan, Muhammad; Liu, Shiyin; Saifullah, Muhammad; Iqbal, Mudassar; Saddique, Qaisar; Ul Hussan, Waqas; Latif, Yasir (2024-12-31). "Estimation of changes in runoff and its sources in response to future climate change in a critical zone of the Karakoram mountainous region, Pakistan in the near and far future". Geomatics, Natural Hazards and Risk. 15 (1) 2291330. Bibcode:2024GNHR...1591330A. doi:10.1080/19475705.2023.2291330. ISSN 1947-5705.
  3. Ul Hussan, Waqas; Khurram Shahzad, Muhammad; Seidel, Frank; Costa, Anna; Nestmann, Franz (2020-03-06). "Comparative Assessment of Spatial Variability and Trends of Flows and Sediments under the Impact of Climate Change in the Upper Indus Basin". Water. 12 (3): 730. Bibcode:2020Water..12..730U. doi:10.3390/w12030730. ISSN 2073-4441.