|Native name||Обь (Russian)|
|Region||Altai Krai, Novosibirsk Oblast, Tomsk Oblast, Khanty-Mansi Autonomous Okrug, Yamalia|
|Cities||Biysk, Barnaul, Novosibirsk, Nizhnevartovsk, Surgut|
|• location||Belukha Mountain, Altai Republic|
|• elevation||2,300 m (7,500 ft)|
|• location||Lake Teletskoye, Altai Republic|
|• elevation||434 m (1,424 ft)|
|3rd source||Most distant source: Ob-Irtysh system|
|• location||near Mang-tai-ch’ia-ta-fan pass, Altai Mountains, Xinjiang, China|
|• elevation||2,960 m (9,710 ft)|
|Source confluence||Near Biysk|
|• location||Altai Krai|
|• elevation||195 m (640 ft)|
|Mouth||Gulf of Ob|
|Ob Delta, Yamalia|
|0 m (0 ft)|
|Length||3,700 km (2,300 mi)|
|Basin size||2,972,497 km2 (1,147,688 sq mi) to 2,994,238 km2 (1,156,082 sq mi)|
|• minimum||140 m (460 ft)|
|• average||3,000 m (9,800 ft)|
|• maximum||19,000 m (62,000 ft)|
|• average||9 m (30 ft)|
|• maximum||40 m (130 ft)|
|• location||Salekhard (Basin size: 2,917,508 km2 (1,126,456 sq mi))|
|• average||(Period of data: 1971–2015)12,889 m3/s (455,200 cu ft/s)
(Period of data: 1930–1984)12,475.1 m3/s (440,550 cu ft/s)(Period of data: 1999–2008)13,500 m3/s (480,000 cu ft/s)
|• minimum||2,360 m3/s (83,000 cu ft/s)|
|• maximum||40,200 m3/s (1,420,000 cu ft/s)|
|• location||Ob Estuary, Gulf of Ob (Kara Sea), Russia|
|• average||(Period of data: 1940–2017)402 km3/a (12,700 m3/s) (Period of data: 1984–2018)414 km3/a (13,100 m3/s)|
|• left||Katun, Anuy, Charysh, Aley, Parabel, Vasyugan, Irtysh, Severnaya Sosva|
|• right||Biya, Berd, Inya, Tom, Chulym, Ket, Tym, Vakh, Pim, Kazym|
The Ob (Обь, IPA: [opʲ]) is a major river in Russia. It is in western Siberia; and together with Irtysh forms the world's seventh-longest river system, at 5,410 kilometres (3,360 mi). It forms at the confluence of the Biya and Katun which have their origins in the Altai Mountains. It is the westernmost of the three great Siberian rivers that flow into the Arctic Ocean (the other two being the Yenisei and the Lena). Its flow is north-westward, then northward.
The internationally known name of the river is based on the Russian name Обь (Obʹ ). Possibly from Proto-Indo-Iranian *Hā́p-, "river, water" (compare Vedic Sanskrit áp-, Persian āb, Tajik ob, and Pashto obə, "water"). Katz (1990) proposes Komi ob 'river' as the immediate source of derivation for the Russian name. Katz's proposal of a common Finno-Ugric root, borrowed early on from a pre-Indo-Iranian source related to Sanskrit ambhas- 'water' is deemed improbable by Rédei (1992), who prefers to analyse this as a later loan from a descendant of the non-nasal root form *Hā́p-.
The Ob forms 25 km (16 mi) southwest of Biysk in Altai Krai at the confluence of the Biya and Katun rivers. Both these streams have their origin in the Altai Mountains, which gradually give way to the Ob Plateau. The Biya has its sources in Lake Teletskoye and the 700 kilometres (430 mi) long Katun in a glacier on Mount Byelukha.
The Ob itself is in Russia. Its tributaries extend into northern Kazakhstan, a western corner of China and a tiny upland parcel of the western tip of Mongolia, where the wider borders match the drainage basin almost precisely. The river splits into more than one arm after the large Irtysh flows into it at about 69° E. Originating in China, the Irtysh is the furthest source of the Ob. From their respective sources to the confluence, the Irtysh measures 4,248 kilometers (2,640 mi) and the Ob 2,538 km (1,577 mi). Other noteworthy tributaries are: from the east, the Tom, Chulym, Ket, Tym and Vakh rivers; and, from the west and south, the Vasyugan, Irtysh (with the Ishim and Tobol rivers), and Severnaya Sosva.
The Ob zigzags west and north until it reaches 55° N, where it curves to the northwest, south of the Siberian Uvaly, at the western end of which it bends northwards, wheeling finally eastwards into the Gulf of Ob, a 1,000-kilometre-long (620-mile) bay of the Kara Sea, separating the Yamal Peninsula from the Gyda Peninsula.
The combined Ob-Irtysh system, the fourth-longest river system of Asia (after Yenisei, and China's Yangzi and Yellow rivers), is 5,410 kilometres (3,360 mi) long, and the area of its basin 2,990,000 square kilometres (1,150,000 sq mi). The river basin of the Ob consists mostly of steppe, taiga, swamps, tundra, and semi-desert topography. The floodplains of the Ob are characterised by many tributaries and lakes. The Ob is icebound at southern Barnaul from early in November to near the end of April, and at northern Salekhard, 150 km (93 mi) above its mouth, from the end of October to the beginning of June.[needs update] The Ob River crosses several climatic zones. The upper Ob valley, in the south, supports grapes, melons and watermelons, whereas the lower reaches of the Ob are Arctic tundra. The most temperate climates on the Ob are at Biysk, Barnaul, and Novosibirsk.
The Ob provides irrigation, drinking water, hydroelectric energy, and fishing (the river hosts more than 50 species of fish). There are several hydroelectric power plants along the Ob river, the largest being Novosibirskaya GES.
The navigable waters within the Ob basin reach a total length of 15,000 km (9,300 mi). The importance of navigation in the Ob basin for transport was particularly great before the completion of the Trans-Siberian Railway, since, despite the general south-to-north direction of the flow of Ob and most of its tributaries, the width of the Ob basin provided for (somewhat indirect) transport in the east–west direction as well.
Until the early 20th century, a particularly important western river-port was Tyumen, located on the Tura, a tributary of the Tobol. Reached by an extension of the Yekaterinburg–Perm railway in 1885, and thus obtaining a rail link to the Kama and Volga rivers in the heart of Russia, Tyumen became an important railhead for some years until the railway extended further east. In the eastern reaches of the Ob basin, Tomsk on the Tom functioned as an important terminus.
Tyumen had its first steamboat in 1836, and steamboats have navigated the middle reaches of the Ob since 1845. In 1916, there were 49 steamers on the Ob; 10 on the Yenisei.
In an attempt to extend the Ob navigable system even further, a system of canals, utilising the Ket, 900 km (560 mi) long in all, was built in the late 19th-century to connect the Ob with the Yenisei, but soon abandoned as being uncompetitive with the railway.
The Trans-Siberian Railway, once completed, provided for more direct, year-round transport in the east–west direction. But the Ob river-system still remained important for connecting the huge expanses of Tyumen Oblast and Tomsk Oblast with the major cities along the Trans-Siberian route, such as Novosibirsk or Omsk. In the second half of the 20th century, construction of rail links to Labytnangi, Tobolsk, and the oil and gas cities of Surgut, and Nizhnevartovsk provided more railheads, but did not diminish the importance of the waterways for reaching places still not served by the rail.
A dam built near Novosibirsk in 1956 created the then-largest artificial lake in Siberia, called Novosibirsk Reservoir. From the 1960s through 1980s, Soviet engineers and administrators contemplated a gigantic project to divert some of the waters of Ob and Irtysh to Kazakhstan and the Soviet Central Asian republics, replenishing the Aral Sea as well. The project never left the drawing board, abandoned in 1986 for economic and environmental considerations.
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|from the left||from the right|
Cities along the river include:
From a confluence to a source:
- Surgut Bridge
- Railway bridge in Surgut
- Shegarsky bridge
- The bridge of "northern bypass" of Novosibirsk
- Dimitrov bridge in Novosibirsk
- First railway bridge across the Ob (Trans-Siberian Railway)
- Communal (October) bridge in Novosibirsk
- Metro bridge in Novosibirsk – longest Metro Bridge in the world
- Bugrinsky Bridge
- Komsomol railway bridge in Novosibirsk
- The bridge above the lock of Novosibirskaya HPP
- Railway bridge in Kamen-na-Obi
- Communal bridge (railway, automobile) in Barnaul
- New bridge in Barnaul
- "Ob River". Archived from the original on 2022-10-22. Retrieved 2022-10-22.
- "Ob River at Salekhard". River Discharge Database. Center for Sustainability and the Global Environment. 2010-02-13. Archived from the original on 2010-06-12. Retrieved 2010-11-06.
- "Changing freshwater contributions to the Arctic | Elementa: Science of the Anthropocene | University of California Press". Archived from the original on 2021-11-26. Retrieved 2021-11-26.
- "River Discharge". Archived from the original on 2007-02-10. Retrieved 2021-10-11.
- Katz, Hartmut. Zum Flußnamen Ob. — Specimena Sibirica III, pp. 93–95. Wien.
- Rédei, Károly. Szófejtések. — Nyelvtudományi Közlemenyek 93, pp. 125–135.
- public domain: Chisholm, Hugh, ed. (1911). "Ob". Encyclopædia Britannica. Vol. 19 (11th ed.). Cambridge University Press. p. 944. One or more of the preceding sentences incorporates text from a publication now in the
- Приобское плато Archived 2022-07-02 at the Wayback Machine; Great Soviet Encyclopedia in 30 vols. — Ch. ed. A.M. Prokhorov. – 3rd ed. – M. Soviet Encyclopedia, 1969–1978. (in Russian)
- "Location of Novosibirskaya GES". Google Maps. Archived from the original on 9 September 2022. Retrieved 1 July 2017.
- Douglas R. Weiner, "A Little Corner of Freedom: Russian Nature Protection from Stalin to Gorbachev" Archived 2017-01-09 at the Wayback Machine. University of California Press, 1999. ISBN 0-520-23213-5. p. 415
- Michael H. Glantz, "Creeping Environmental Problems and Sustainable Development in the Aral Sea..." Archived 2017-01-09 at the Wayback Machine. ISBN 0-521-62086-4. p. 174