Ukvushvuynen Range
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The Ukvushvuynen Range (russian: горы Уквушвуйнен; zh, 乌克武什武伊年山), also known as Meingypilgyn Range (russian: Мэйнгыпильгынский хребет),
/ref> is a range of mountains in
Chukotka Autonomous Okrug Chukotka (russian: Чуко́тка), officially the Chukotka Autonomous Okrug,, ''Čukotkakèn avtonomnykèn okrug'', is the easternmost federal subjects of Russia, federal subject of Russia. It is an autonomous okrug situated in the Russian ...
,
Russian Far East The Russian Far East (russian: Дальний Восток России, r=Dal'niy Vostok Rossii, p=ˈdalʲnʲɪj vɐˈstok rɐˈsʲiɪ) is a region in Northeast Asia. It is the easternmost part of Russia and the Asian continent; and is admini ...
. Administratively the range is part of
Anadyr District Anadyrsky District (russian: Ана́дырский райо́н; Chukchi: , ''Kagyrgyn rajon'') is an administrativeLaw #33-OZ and municipalLaw #148-OZ district (raion), one of the six in Chukotka Autonomous Okrug, Russia. It is located in the c ...
.
Google Earth Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geog ...


Geography

The Ukvushvuynen Range is the easternmost subrange of the
Koryak Highlands The Koryak Mountains or Koryak Highlands () are an area of mountain ranges in Far-Eastern Siberia, Russia, located in Chukotka Autonomous Okrug and in Kamchatka Krai, with a small part in Magadan Oblast. The highest point in the system is the Mou ...
,
East Siberian Mountains The East Siberian Mountains or East Siberian Highlands ( rus, Восточно-Сибирское нагорье) are one of the largest mountain systems of the Russian Federation. They are located between the Central Yakutian Lowland and the Ber ...
. It stretches roughly from east to west in southern Chukotka, between the Koyverelan Range to the west and Cape Navarin in the
Bering Sea The Bering Sea (, ; rus, Бе́рингово мо́ре, r=Béringovo móre) is a marginal sea of the Northern Pacific Ocean. It forms, along with the Bering Strait, the divide between the two largest landmasses on Earth: Eurasia and The Ameri ...
to the east. To the northwest rises the
Rarytkin Range The Rarytkin Range (russian: хребет Рарыткин; ckt, Ръарыткын) is a range of mountains in Chukotka Autonomous Okrug, Russian Far East. Administratively the range is part of Anadyr District.Google Earth Geography The Raryt ...
and the
Velikaya River The Velikaya () is a river in Novosokolnichesky, Pustoshkinsky, Sebezhsky, Opochetsky, Pushkinogorsky, Ostrovsky, Palkinsky, and Pskovsky Districts of Pskov Oblast, as well as in the city of Pskov in Russia. It is a major tributary of La ...
flows into the
Anadyr Lowlands The Anadyr Lowlands (russian: Ана́дырская ни́зменность) are a low alluvial plain located in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia. Geography The lowlands are crossed by the Anadyr River in the m ...
. To the southwest stretches the Komeutyuyam Range. The highest mountains of the Ukvushvuynen Range are located in its western part. The highest summit is high Gora Krasnaya (гора красная), rising to the south of lake Yanragytgyn. Other high peaks of the range are high Gora Tsirk (гора цирк) and high mount Kenkeren (кэнкэрэн), the latter rising above the NW side of lake Maynits in the central part of the range. Vaamochka and Pekulney are
coastal lagoon A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') a ...
s that lie on the southern side of the range. The range has 28
mountain glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as ...
s. The Kakanaut River, a small river flowing southwards in the central part of the range into the NE bay of Lake Pekulney, gives its name to the Kakanaut
Maastrichtian The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from ...
geological formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...
.


Flora and climate

There are
shrub A shrub (often also called a bush) is a small-to-medium-sized perennial woody plant. Unlike herbaceous plants, shrubs have persistent woody stems above the ground. Shrubs can be either deciduous or evergreen. They are distinguished from trees ...
areas of
Siberian pine ''Pinus sibirica'', or Siberian pine, in the family Pinaceae is a species of pine tree that occurs in Siberia from 58°E in the Ural Mountains east to 126°E in the Stanovoy Range in southern Sakha Republic, and from Igarka at 68°N in the lower ...
in the lower mountain slopes, while the upper elevations are covered with
mountain tundra Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets ...
. The Ukvushvuynen Range has a
subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, ge ...
, somewhat moderated by the proximity of the ocean. The average temperature in January is and the temperature in July is . Very little precipitation falls in winter in the form of snow, most falls as rain in the summer. The average depth of the snow cover is .


Bibliography


Elizabeth L. Miller, Arthur Grantz, Simon Klemperer eds. - ''Tectonic Evolution of the Bering Shelf-Chukchi Sea-Arctic Margin and Adjacent Landmasses''


See also

*
Kakanaut Formation The Kakanaut Formation is a geological Formation (geology), formation in Siberia, whose strata date back to the Late Cretaceous (Maastrichtian). Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel et al., 2 ...


References


External links


Pekulney LakeHydrometeorology and hydrochemistry of the seas (p. 2)
Koryak Mountains Mountain ranges of Chukotka Autonomous Okrug Landforms of Siberia Anadyrsky District {{ChukotkaAutonomousOkrug-geo-stub