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C o o r d i n a t e s : 6 7 ° 1 1 ′ 4 7 . 7 ″ N 1 6 5 ° 5 1 ′ 2 8 . 2 6 ″ E / 6 7 . 1 9 6 5 8 3 ° N 1 6 5 . 8 5 7 8 5 0 0 ° E / 67.196583; 165.8578500
F r o m W i k i p e d i a , t h e f r e e e n c y c l o p e d i a
( R e d i r e c t e d f r o m A n y u y R a n g e )
The Anyuy Mountains (Russian : Анюйский хребет ; Anyuyskiy Khrebet ), also known as South Anyuy Range are a range of mountains in far north-eastern Russia. Administratively the range is part of the Chukotka Autonomous Okrug , Russia . The area of the range is largely uninhabited.
Geography
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To the north rises the Chuvanay Range and to the northeast the Ilirney Range , on the other side of the Maly Anyuy River .[2] The Anyuy Range is part of the East Siberian System of mountains and is one of the subranges of the Anadyr Highlands .[3] To the east of the eastern end of the range rises the Shchuchy Range , stretching in a roughly southwestern direction, and to the south of the range rises the roughly parallel Oloy Range of the Kolyma Mountains .[2]
Although there are no glaciers in the range in present times, there is evidence of ancient glaciation. The Anyuy Range is drained by rivers Maly Anyuy , Bolshoy Anyuy , and Omolon .[4] The highest point is 1,779 metres (5,837 ft ) high Blokhin Peak (Пик Блохина) at 67°06′06 ″N 166°51′38 ″E / 67.10167°N 166.86056°E / 67.10167; 166.86056 ,[1] and the second highest 1,759 metres (5,771 ft ) high Pik Sovetskoy Gvardii (Soviet Guard Peak).[5]
In 1952 a volcano was discovered in the southern part of the range following examination of aerial images. The volcano was named Anyuyskiy .[6]
Flora
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There are sparse forests of larch in river valleys and the mountain slopes are covered with tundra vegetation, with rocky mountain tundra on the ridges and peaks.[5]
See also
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References
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^ Oleg Leonidovič Kryžanovskij, A Checklist of the Ground-beetles of Russia and Adjacent Lands. p. 16 ISBN 954-642-004-2
^ David M. Hopkins; John V. Matthews; Charles E. Schweger (1982). Paleoecology of Beringia . Elsevier. p. 45. ISBN 9780123558602 .
^ a b South Anyui Range // Great Soviet Encyclopedia : [in 30 vol.] / Ch. ed. A.M. Prokhorov . - 3rd ed. - M .: Soviet Encyclopedia, 1969-1978.
^ Pevzner, M. M.; Gertsev, D. O.; Fedorov, P. I.; Romanenko, F. A.; Kushcheva, Yu V. (1 January 2017). "Anyui Volcano in Chukotka: Age, structure, pecularities [sic] of rocks' composition and eruptions" . Lithology and Mineral Resources . 52 (1 ): 20–50. doi :10.1134/S0024490217010059 . ISSN 0024-4902 . S2CID 132021660 .
External links
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t
e
R e t r i e v e d f r o m " https://en.wikipedia.org/w/index.php?title=Anyuy_Mountains&oldid=1236027579 "
C a t e g o r i e s :
● M o u n t a i n r a n g e s o f C h u k o t k a A u t o n o m o u s O k r u g
● C h u k o t k a A u t o n o m o u s O k r u g g e o g r a p h y s t u b s
H i d d e n c a t e g o r i e s :
● P a g e s u s i n g g a d g e t W i k i M i n i A t l a s
● A r t i c l e s w i t h s h o r t d e s c r i p t i o n
● S h o r t d e s c r i p t i o n i s d i f f e r e n t f r o m W i k i d a t a
● C o o r d i n a t e s o n W i k i d a t a
● A r t i c l e s c o n t a i n i n g R u s s i a n - l a n g u a g e t e x t
● C o m m o n s c a t e g o r y l i n k i s l o c a l l y d e f i n e d
● A l l s t u b a r t i c l e s
● T h i s p a g e w a s l a s t e d i t e d o n 2 2 J u l y 2 0 2 4 , a t 1 3 : 5 1 ( U T C ) .
● T e x t i s a v a i l a b l e u n d e r t h e C r e a t i v e C o m m o n s A t t r i b u t i o n - S h a r e A l i k e L i c e n s e 4 . 0 ;
a d d i t i o n a l t e r m s m a y a p p l y . B y u s i n g t h i s s i t e , y o u a g r e e t o t h e T e r m s o f U s e a n d P r i v a c y P o l i c y . W i k i p e d i a ® i s a r e g i s t e r e d t r a d e m a r k o f t h e W i k i m e d i a F o u n d a t i o n , I n c . , a n o n - p r o f i t o r g a n i z a t i o n .
● P r i v a c y p o l i c y
● A b o u t W i k i p e d i a
● D i s c l a i m e r s
● C o n t a c t W i k i p e d i a
● C o d e o f C o n d u c t
● D e v e l o p e r s
● S t a t i s t i c s
● C o o k i e s t a t e m e n t
● M o b i l e v i e w