The Shigar River is a tributary to the Indus River, joining at the town of Skardu. The Basha and Braldu rivers are northern tributaries of the Shigar. Numerous complex granitic pegmatites and a few alpine-cleft metamorphic deposits are found in the Shigar Valley and its tributaries. Shigar Valley contains the Main Karokoram Thrust separating the metasediments (chlorite to amphibolite grade) on the Asian plate from the southern volcanoclastic rocks of the Kohistan-Ladakh island arc.
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References
- Blauwet, D., Smith, B., and Smith, C. (1997): A Guide to the Mineral Localities of the Northern Areas, Pakistan. Mineralogical Record 28(3), 183-200.
-Ikram Mineralogy information
-Hassam, Muhammad (2007) Mineralogy and Geochemistry of gemstones and the gemstone-bearing pegmatites in the Shigar Valley of Skardu, Northern Areas of Pakistan. PhD thesis, Peshawar University
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