Shyok River | |
---|---|
![]() Shyok River | |
![]() Course of the Shyok | |
Etymology | "the river of death"[1] |
Location | |
Country | India, Pakistan |
Territory | Ladakh (India), Gilgit-Baltistan (Pakistan) |
District | Leh (India), Ghanche (Pakistan) |
Physical characteristics | |
Source | |
• coordinates | 35°21′N 77°37′E / 35.35°N 77.62°E |
Mouth | Indus River |
• coordinates | 35°14′N 75°55′E / 35.23°N 75.92°E |
Basin size | 33,347 km2 (12,875 sq mi)[2] |
Discharge | |
• location | Yugo gauging station, Pakistan.[3] |
• average | 1041 m3/sec |
• minimum | 859 m3/sec |
• maximum | 1199 m3/sec |
Basin features | |
River system | Indus River |
Tributaries | |
• left | Chip Chap River, Galwan River, Chang Chenmo River |
• right | Nubra River, Hushe River |
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The Shyok River is a tributary of the Indus River that flows through northern Ladakh in India and enters Gilgit-Baltistan in Pakistan, spanning approximately 550 km (340 mi).
It originates at the Rimo Glacier and follows an unusual course. Initially flowing southeast, it turns northwest upon meeting the Pangong Range, running nearly parallel to its earlier path. The Shyok Valley widens at the confluence with the Nubra River but then narrows abruptly into a gorge near Yagulung (34°46′N 77°08′E / 34.77°N 77.14°E), continuing through the villages of Bogdang, Turtuk[4], and Tyakshi before entering Baltistan. The valley widens again near the junction with the Saltoro River at Ghursay. The river ultimately joins the Indus at Keris, east of the town of Skardu.[5][6]
The Nubra River, originating from the Siachen Glacier, follows a similarly unusual path. Before reaching Diskit, it flows southeast but turns northwest after meeting the Shyok. The parallel behavior of these two rivers may reflect a series of Paleolithic fault lines trending northwest–southeast, which likely influenced the courses of their upper reaches.
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