geo.wikisort.org - Mountains

Search / Calendar

The Chukotka Mountains (Russian: Чукотское нагорье) or Chukotka Upland (Чукотская горная страна)[1] is a mountainous area in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia.[2]

Chukotka Mountains
Чукотское нагорье
Landscape of the Palyavaam Range
Highest point
PeakIskhodnaya
Elevation1,843 m (6,047 ft)
Dimensions
Length1,300 km (810 mi)
Geography
Location in the Chukotka Autonomous Okrug, Russia
CountryRussia
Federal subjectChukotka Autonomous Okrug
Range coordinates68°0′N 177°0′E
Parent rangeEast Siberian System
Geology
Age of rockJurassic, Triassic, Permian and Proterozoic
Type of rockSandstone, shale with granite intrusions and volcanic rocks

The ridges of this system are largely barren and desolate. About half of their area is above the Arctic Circle. The climate is one of the harshest in the Russian Federation, with minimum absolute temperatures reaching -73°С. Traditionally Chukchi people lived only in few intermontane areas, such as the Amguema valley that cuts across the vast mountain zone.


Geography


The Chukotka Mountains are one of the two main mountain regions of Chukotka. They rise west and east of the isthmus area of the Chukchi Peninsula, in the central Chukotka region, bounded by the Anadyr Highlands in the southwest. They are composed of mountains of middle height displaying alpine relief, as well as low mountains. They stretch in roughly WNW/ESE direction for 450 kilometers (280 mi), between the head of Chaun Bay and the Bering Sea shore. The ranges of the northern area consist of sandstone and shale with granite intrusions, while those of the southern part are made up of volcanic rocks. The highest peak is Mount Iskhodnaya (Исходная) in the Chantal Range.[2] which is 1,843 metres (6,047 ft) high[3][4] — or 1,887 metres (6,191 ft) according to other sources.[2]


Hydrography


Among the rivers that have their source in the mountains, the following deserve mention: the Amguema River with its tributaries Ekityki and Chantalveergyn, the Palyavaam, Pegtymel and Tanyurer of the Chukchi Sea side, as well as the Kanchalan and the Belaya River tributaries Bolshoi Pykarvaam and Bolshaya Osinovaya of the Pacific Ocean side. The largest lakes in the mountain area are Ekityki, Ioni and Koolen.[5]

There are 47 small glaciers in the ranges of the highlands, with a total area of 13.53 square kilometers (5.22 sq mi).[6]


Subranges


The system of the Chukotka Mountains comprises a number of subranges, including the following:[7][2][8]

Panorama of the Chukotka Mountains near Egvekinot.
Panorama of the Chukotka Mountains near Egvekinot.

Climate


The climate of the Chukotka Mountains area is severe, with short cool summers and very cold 8-month long winters where blizzards are common owing to the influence of both the Arctic Ocean and the Aleutian Low. The valley areas have a continental climate while the mountain ranges are under the influence of an oceanic climate, which is felt more in the lower altitude mountains and less in the medium-high ones.[9]


Flora and fauna


The lower slopes of the mountains have tundra vegetation, often marshy in the intermontane basins, while the higher altitudes are Arctic desert. Rivers are abundant in fish.[10]


References


  1. Геоморфология России (Geomorphology of Russia)
  2. Chukchi Highlands / Great Russian Encyclopedia; in 35 vol.] / Ch. ed. Yu.S. Osipov . - M .: Great Russian Encyclopedia, 2004—2017.
  3. Czukockie, Góry - Encyklopedia PWN - źródło wiarygodnej i rzetelnej wiedzy, encyklopedia.pwn.pl
  4. Wielka Encyklopedia Gór i Alpinizmu, tom 2 Góry Azji, Katowice: Wydawnictwo STAPIS, 2005, ISBN 83-88212-42-7.
  5. Chukotka Autonomous Okrug - Water of Russia
  6. John F. Shroder, Gregory B Greenwood, Mountain Ice and Water, Investigations of the Hydrologic Cycle in Alpine Environments; Volume 21. 1st Edition. p.98
  7. Oleg Leonidovič Kryžanovskij, A Checklist of the Ground-beetles of Russia and Adjacent Lands. p. 16
  8. Wetlands in Russia - Vol.4
  9. Soil zonality of the Chukotka Upland
  10. A.P. Gorkin. Encyclopedia "Geography". - ACT: Rosman, 2008 p. 1374 - ISBN 5353024435 (in Russian)



На других языках


[de] Hochland von Tschukotka

Das Hochland von Tschukotka (russisch Чуко́тское наго́рье/Tschukotskoje nagorje; auch Anadyrgebirge, russ. Ана́дырский хребе́т/Anadyrski chrebet[1], oder Tschukotkagebirge bzw. Tschuktschengebirge, russ. Чуко́тский хребе́т/Tschukotski chrebet[2]) ist ein bis 1843 m hohes Hochland bzw. -gebirge im äußersten Nordosten von Russland, im Föderationskreis Ferner Osten.[3]
- [en] Chukotka Mountains

[es] Cordillera de Chukotka

La cordillera de Chukotka, cordillera de Chukotska o cordillera de Ojotsko-Chukotsky, es una cadena montañosa en el extremo noreste de Siberia en Rusia, sobre el círculo polar ártico. Está compuesta por las Tierras altas de Anadyr y el sector sur de las tierras altas de Chukotka.[1] La zona de elevadas montañas se caracteriza también por sus pronunciados valles, y su origen es claramente glaciar. Los picos alcanzan elevaciones de 1 600 a 1 800 m snm.

[fr] Hauts-Plateaux tchouktches

Les Hauts-Plateaux tchouktches (russe : Чукотская горная страна) sont une zone montagneuse située dans l'Okroug Autonome de la Tchoukotka, dans l'Extrême-Orient russe. Ces plateaux, séparant l'Océan Arctique du Pacifique, sont principalement désolés et arides. Le tiers supérieur de la chaîne de montagnes se trouve au-delà du Cercle polaire. Le climat de la région est l'un des plus rudes de la Fédération de Russie, avec des températures minimales pouvant atteindre −73 °C[1]. Les rares habitants de la région, majoritairement des tchouktches, vivent dans les quelques vallées qui parsèment le relief, le principal village étant Amgouema.

[it] Altopiano dei Ciukci

L'altopiano dei Ciukci (in russo: Чуко́тское наго́рье?, Čukotskoe nagor'e) è un sistema montuoso situato nella parte nordorientale dell'estremo oriente russo; costituisce l'estrema parte settentrionale del vasto sistema di alteterre che costituisce la gran parte della Siberia orientale: gli Altopiani della Siberia Orientale.

[ru] Чукотское нагорье

Чуко́тское наго́рье[1] (Чукотский хребет[2], Анадырский хребет[3]) — система средневысотных хребтов и массивов в центральной части Чукотского автономного округа, в северо-восточной части Дальнего Востока России. Является частью Восточно-Сибирской возвышенности[de]. Длина около 450 км[4].



Текст в блоке "Читать" взят с сайта "Википедия" и доступен по лицензии Creative Commons Attribution-ShareAlike; в отдельных случаях могут действовать дополнительные условия.

Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.

2019-2025
WikiSort.org - проект по пересортировке и дополнению контента Википедии