Chersky Range
Template:Short description Script error: No such module "For". Template:Expand Russian Template:Infobox mountain The Chersky Range (Template:Langx, Template:Langx) is a chain of mountains in northeastern Siberia between the Yana and Indigirka Rivers. Administratively, the area of the range belongs to the Sakha Republic, although a small section in the east is within Magadan Oblast. The highest peak in the range is the Script error: No such module "convert".-tall Peak Pobeda, part of the Ulakhan-Chistay Range. The range also includes important places of traditional Yakut culture, such as Ynnakh Mountain (Mat'-Gora) and kigilyakh rock formations.[1]
The Moma Natural Park is a protected area located in the southern zone of the range.[2]
History
At some time between 1633 and 1642, Poznik Ivanov ascended a tributary of the lower Lena, crossed the Verkhoyansk Range to the upper Yana, and then crossed the Chersky Range to the Indigirka.[3] The range was sighted in 1926 by Sergei Obruchev (Vladimir Obruchev's son) and named by the Russian Geographical Society after the Polish explorer and geographer Ivan Chersky (or Jan Czerski).[4]
Geography
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The geographic boundaries of the mountain system are the Yana–Oymyakon Highlands in the southwest, the Upper Kolyma Highlands in the southeast, and the Momo-Selennyakh Depression in the northeast.[5]
Subranges
The system of the Chersky Range comprises a number of subranges running generally from northwest to southeast, including the following:
Between the Yana and Indigirka rivers:
- Burkat Range, highest point Script error: No such module "convert".
- Khadaranya Range, highest point Script error: No such module "convert".
- Ymiysky Range, highest point Script error: No such module "convert".
- Kisilyakh Range, highest point Script error: No such module "convert"., by the confluence of the Adycha and the Yana
- Tas-Khayakhtakh, highest point Script error: No such module "convert".
- Kurundya Range, highest point Script error: No such module "convert".
- Dogdo Range, highest point Script error: No such module "convert".
- Chemalgin Range, highest point Script error: No such module "convert".
- Yana-Oymyakon Highlands
- Elgi Plateau (Эльгинское плоскогорье), highest point Script error: No such module "convert".
- Oymyakon Plateau, highest point Script error: No such module "convert".
- Yana Plateau, highest point Script error: No such module "convert".
- Tirekhtyakh Range and Nelgesin Range, between the Adycha and Sartang rivers
In the upper Kolyma river basin:
- Ulakhan-Chistay, highest point Script error: No such module "convert"., near the southern end
- Okhandya Range, highest point Script error: No such module "convert"., the highest point of Magadan Oblast.[6]
- Cherge Range, highest point Script error: No such module "convert".
- Angachak Range, highest point Script error: No such module "convert".
- Arga-Tas, highest point Script error: No such module "convert".
Between the Chibagalakh and Adycha rivers
- Chibagalakh Range, highest point Script error: No such module "convert".
- Onyol Range (Онёлский хребет), highest point Script error: No such module "convert".
- Borong Range, highest point Script error: No such module "convert". (west of the Charky)
- Nendelgin Range, highest point Script error: No such module "convert". (east of the Adycha)[7]
- Porozhny Range, highest point Script error: No such module "convert".
- Silyap Range, highest point Mount Chyon (Гора Чён) Script error: No such module "convert".[8]
Between the Indigirka and the Nera rivers:
- Tas-Kystabyt, highest point Script error: No such module "convert".
- Khalkan Range, highest point Script error: No such module "convert"., a southern prolongation of Tas-Kystabyt
Northeastern outliers
In some works, a few roughly-parallel ranges located off the main system to the northeast, such as the Kyun-Tas Range (highest point Script error: No such module "convert".), the Selennyakh Range (highest point highest point Saltag-Tas (Script error: No such module "convert".), and the adjacent Moma Range (highest point Script error: No such module "convert".), with the Moma-Selennyakh Depression running along their western side, are included in the Chersky mountain system.[9]
Other ranges of the system include the Irgichin Range, Inyalin Range, Volchan Range, Silen Range, and Polyarny Range, among others.[10]
Hydrography
The Chersky System includes three main river basins:
- Yana River, covering the western and northwestern parts of the mountain system. It includes rivers Oldzho and Adycha with its tributaries Tuostakh and Charky.
- Indigirka River, covering the northeastern, central, and southwestern parts of the system, with rivers Selennyakh, Moma, and Nera, among others.
- Kolyma River, covering the eastern, southeastern, and southern parts of the system, with rivers Zyryanka, Rassokha, Omulyovka, Yasachnaya, Taskan, Debin, and Byoryolyokh, among others.
Some of the higher ranges with alpine relief have glaciers. There are roughly 350 glaciers in the system, with a total area of Script error: No such module "convert"..[11] There are also small lakes in the swampy valleys of some rivers, as well as lakes of glacial origin, such as Emanda and Tabanda.
Tectonics
The range lies on the boundary between the Eurasian and North American tectonic plates.[12]
The precise nature of the boundary between the North American and Eurasian tectonic plates in the area of the Chersky Range is still not fully understood and is the subject of ongoing research. By the 1980s, the Chersky Range was considered mostly a zone of continental rifting where the crust was spreading apart.[13] However, the currentScript error: No such module "Unsubst". view is that the Chersky Range is mostly an active suture zone, a continental convergent plate boundary, where compression is occurring as the two plates press against each other.[14] There is thought to be a point in the Chersky Range where the extensional forces coming from the north change to the compressional forces noted throughout most of the range. The Chersky Range is also thought to include a geologic triple junction where the Ulakhan Fault intersects the suture zone. Whatever the exact nature of the regional tectonics, the Chersky Range is seismically active. It connects in the north with the landward extension of the Laptev Sea Rift, itself a continental extension of the Mid-Arctic Gakkel Ridge.
Climate
The Chersky mountains, along with the neighboring Verkhoyansk Range, have a moderating effect on the climate of Siberia. The ridges obstruct west-moving air flows, decreasing the amount of snowfall in the plains to the west.
See also
References
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- ↑ Кисиляхи
- ↑ Script error: No such module "citation/CS1".
- ↑ G. Patrick March,'Eastern Destiny:Russia in Asia and the North Pacific, 1996, chapter 3
- ↑ Script error: No such module "Citation/CS1".
- ↑ Хребет Черского (in Russian)
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Массив Чен
- ↑ Chersky Range // Great Russian Encyclopedia : [in 35 vols.] / Ch. ed. Yu.S. Osipov . - M , 2004—2017.
- ↑ Oleg Leonidovič Kryžanovskij, A Checklist of the Ground-beetles of Russia and Adjacent Lands. p. 15
- ↑ Черского хребет (в Якутской АССР и Магаданской обл.), Great Soviet Encyclopedia
- ↑ News Archive – The Earth Institute at Columbia University
- ↑ "Geodynamics and Late Cenozoic Evolution of the Asia/Pacific Transitional Zone", in Tectonics, International Geological Congress Staff, 27th International Geological Congress, Published 1984 by VSP
- ↑ The Physical Geography of Northern Eurasia, ed. Maria Shahgedanova, published by Oxford University Press 2003
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