The Chukotka Mountains () or Chukotka Upland ()Геоморфология России (Geomorphology of Russia) is a mountainous area in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia.Chukchi Highlands / Great Russian Encyclopedia; in 35 vol.] / Ch. ed. Yu.S. Osipov . - M .: Great Russian Encyclopedia, 2004—2017.

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 . 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 roughly WNW/ESE for , 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, which is highCzukockie, Góry - Encyklopedia PWN - źródło wiarygodnej i rzetelnej wiedzy, encyklopedia.pwn.plWielka Encyklopedia Gór i Alpinizmu, tom 2 Góry Azji, Katowice: Wydawnictwo STAPIS, 2005, . — or according to other sources. 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, Ervynaygytgyn, Yanranaygytgyn, Ioni, Pychgynmygytgyn, Medvezhye, Achchyon, and Koolen.Chukotka Autonomous Okrug - Water of Russia

There are 47 small glaciers in the ranges of the highlands, with a total area of .John F. Shroder, Gregory B Greenwood, Mountain Ice and Water, Investigations of the Hydrologic Cycle in Alpine Environments; Volume 21. 1st Edition. p.98

Subranges The system of the Chukotka Mountains comprises a number of subranges, including the following:Oleg Leonidovič Kryžanovskij, A Checklist of the Ground-beetles of Russia and Adjacent Lands. p. 16Wetlands in Russia - Vol.4

Shelag Range, highest point — the northwesternmost, reaching up to Cape Shelagsky. Ichuveem Range, highest point . Ekvyvatap Range, highest point . Pegtymel Range, highest point . Palyavaam Range, highest point . Chantal Range, highest point . Ekityk Range, highest point . Pekulney Range, highest point . Iskaten Range, highest point . Ghenkanyi Range, highest point — the easternmost, near the Bering Sea.

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.

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.A.P. Gorkin. Encyclopedia "Geography". - ACT: Rosman, 2008 p. 1374 - (in Russian)

References

External links

Geography of Chukotka Autonomous Okrug Geology of Chukotka