Siligir
The river flows just north of the Arctic Circle across a lonely, desolate area of Olenyoksky District devoid of settlements. There are very large bitumen deposits along the Siligir basin.
Course
The Siligir is formed in the Central Siberian Plateau at the confluence of the 124 km (77 mi) long Orto-Siligir (Орто-Силигир) and the 100 km (62 mi) long Usuk-Siligir (Усук-Силигир). The river flows initially northwards, bending to the NNE after a stretch, and then to the northeast. Finally it bends again to the north and meets the right bank of the Olenyok 1,351 km (839 mi) from its mouth. The confluence is downstream of Olenyok village, one of the few inhabited localities of the area. The river is frozen between early October and the second half of May.
Tributaries
The Siligir has some very large tributaries, such as the 169 km (105 mi) long Onnyoo-Siligir (Russian: Онньоо-Силигир; Yakut: Өнньүө Силигир) and the 128 km (80 mi) long Siligirkeen (Силигиркээн), both from the left.
Fauna
The main fish species found in the waters of the Siligir are lenok, taimen, grayling, pike and perch. In some stretches there are whitefish and nelma.
See also
References
- ^ "Река Силигир in the State Water Register of Russia". textual.ru (in Russian).
- ^ Силигир / Great Soviet Encyclopedia: in 30 vols. / Ch. ed. A.M. Prokhorov. - 3rd ed. - M. Soviet Encyclopedia, 1969-1978
- ^ East Siberian Bitumen Deposits
- ^ R A French, Alan Wood, Christian R. Thauer, Helen Routledge. The Development of Siberia: People and Resources, p. 243
- ^ "Топографска карта Q-49 50; M 1:1 000 000 - Topographic USSR Chart (in Russian)". Retrieved 29 April 2022.
- ^ "Топографска карта R-49 50; M 1:1 000 000 - Topographic USSR Chart (in Russian)". Retrieved 29 April 2022.
- ^ nature.ykt.ru (Силигир)
- ^ Fishing trip on Siligir and Olenyok