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Yudoma-Maya Highlands
The Yudoma-Maya Highlands ( rus, Юдомо-Майское нагорье, r=Yudomo-Maiskoye Nagorye; sah, Юдома-Маайа хаптал хайалаах сиринэн ) are a mountainous area in the Sakha Republic and Khabarovsk Krai, Far Eastern Federal District, Russia. The settlement of Allakh-Yun is located in the area of the highlands on the right bank of the Allakh-Yun River. History The area of the Yudoma-Maya and the Aldan highlands, between the basins of the Aldan River and the Yudoma, was uncharted territory well until the 1930s. It was first surveyed in 1934 by geologist Yuri Bilibin (1901—1952) together with mining engineer Evgeny Bobin (1897—1941) in the course of an expedition sent by the government of the USSR. Bilibin and Bobin made a thorough topographic survey of the mountainous regions leading separate research parties. They described the highlands as "a disordered jumble of round hills with soft outlines". Geography The Yudoma-Maya Highlands are l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maya River
The Maya (russian: Мая) is a river in Khabarovsk Krai and Sakha, Russia. It is a right tributary of the Aldan of the Lena basin. The length of the river is . The area of its basin . The Maya freezes up in late October and stays under the ice until May. The Yudoma is one of the biggest tributaries of the Maya. The river is navigable up to upstream from its mouth. The Yudoma-Maya Highlands are located in the basin of the Maya.Юдомо-Майское нагорье / Great Soviet Encyclopedia; in 35 vol.] / Ch. ed. Yu.S. Osipov . - M .: , 2004—2017. The Maya was part of the river route from Yakutsk to the |
Yuri Alexandrovich Bilibin
Yuri Alexandrovich Bilibin (russian: Ю́рий Алекса́ндрович Били́бин; 19 May 1901 in Rostov – 4 May 1952 in Leningrad) was a Soviet geologist. Biography Between 1919-1921 he served in the Red Army. In 1926 he graduated from the Leningrad Mining Institute. He later became a member of the Soviet Academy of Sciences and in 1946 was awarded the Stalin Prize for his contribution in the discovery of gold deposits in northeast Siberia.Билибин Юрий Александрович / Great Soviet Encyclopedia; in 35 vols. / Ch. ed. Yu.S. Osipov . - M .: , 2004—2017. Together with mining engineer [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Russian Encyclopedia
The ''Great Russian Encyclopedia'' (GRE; russian: Большая российская энциклопедия, БРЭ, transliterated as ''Bolshaya rossiyskaya entsiklopediya'' or academically as ''Bolšaja rossijskaja enciklopedija'') is a universal Russian encyclopedia, completed in 36 volumes, published between 2004 and 2017 by Great Russian Encyclopedia, JSC (russian: Большая российская энциклопедия ПАО, transliterated as ''Bolshaya rossiyskaya entsiklopediya PAO''). It is released under the auspices of the Russian Academy of Sciences (RAS) after President Vladimir Putin signed a presidential decree №1156 in 2002. The complete edition was released by 2017. The chief editor of the encyclopedia is Yury Osipov, the president of the RAS. The editorial board has more than 80 RAS members, including the Nobel Prize laureates Zhores Alferov and Vitaly Ginzburg. The first, introductory volume, released in 2004, is dedicated to Russia. Thirty-fiv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dzhugdzhur Range
The Dzhugdzhur Mountains (russian: Джугджу́р) or Jugjur Mountains, meaning 'big bulge' in Evenki, are a mountain range along the western shores of the Sea of Okhotsk in the far east of Siberia. The mountains are quite deserted, the one exception being the gold mines that have operated in the range since the 1920s. Geography To the east the range is bound by the northwest coast of the Sea of Okhotsk. To the northwest the range limits with the Yudoma-Maya Highlands, to the southwest with the Stanovoy Range, to the south with the Dzhagdy Range and to the northeast with the Kolyma Mountains.Google Earth Geology The range was formed by an asymmetrical fold. The southwestern half of the mountains is composed of gneiss and granite from the Precambrian, while the northeast contains Mesozoic shale and limestone as well as Cretaceous and Paleocene igneous rock. Ecology and Climate The coastal stretch of the range is populated by Japanese stone pine and Dahurian larch. Part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Okhota River
The Okhota (russian: Охота, from an Even word ''окат'' (okat) meaning "river") is a river in Khabarovsk Krai which flows south to the Sea of Okhotsk near the port town of Okhotsk.Охота (река в Хабаровском крае) (''tr. "Okhota (river in the Khabarovsk Territory): Definition of "(literally) Hunting (river in the Khabarovsk Territory)" in the Great Soviet Encyclopedia"'') , accessed 4 November 2022 The Okhota is long, and its covers . (''tr. "River Okh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suntar-Khayata Range
Suntar-Khayata Range (russian: Сунтар-Хаята, sah, Сунтаар Хайата) is a granite mountain range rising along the border of the Sakha Republic in the north with Amur Oblast and Khabarovsk Krai in the south. The R504 Kolyma Highway passes through the northern part of the range by Kyubeme. Geography The Suntar-Khayata is approximately 450–550 km long and 60 km wide. high Mus-Khaya Mountain, located in the Sakha Republic, is the highest point of the range. Berill Mountain, at is the highest summit in Khabarovsk Krai. Mount Khakandya (Гора Хакандя) is an ultra-prominent peak that is high. The Suntar-Khayata Range is geographically a southeastern prolongation of the Verkhoyansk Range. Until mid 20th century it was treated as a separate range, together with the Skalisty Range, highest point , and the Sette Daban, highest point , to the southwest. The Yudoma-Maya Highlands are located to the south of the range [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Verkhoyansk Range
The Verkhoyansk Range (russian: Верхоянский хребет, ''Verkhojanskiy Khrebet''; sah, Үөһээ Дьааҥы сис хайата, ''Üöhee Chaangy sis khaĭata'') is a mountain range in the Sakha Republic, Russia near the settlement of Verkhoyansk, well-known for its frigid climate. It is part of the East Siberian Mountains. The range lies just west of the boundary of the Eurasian and the North American tectonic plates. The mountains were formed by folding, and represent an anticline. The Verkhoyansk Range was covered by glaciers during the Last Glacial Period and the mountains in the northern section, such as the Orulgan Range, display a typical Alpine relief. There are coal, silver, lead, tin and zinc deposits in the mountains. Geography Rising from the shores of the Buor-Khaya Gulf in the north, it runs southwards spanning roughly 1000 km (600 mi.) across Yakutia, east of the Central Yakutian Lowland, and west of the Chersky Range, reaching the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sette-Daban
The Sette-Daban (russian: Сетте-Дабан, sah, Сэттэ Дабаан) is a range of mountains in far North-eastern Russia. Administratively the range belongs partly to the Sakha Republic and partly to the Khabarovsk Krai of the Russian Federation. The area of the Sette-Daban is largely uninhabited. The R504 Kolyma Highway passes through the northern part of the range. The climate prevailing in the Sette-Daban is continental and severe. The average air temperature in January is a chilly . The average temperature in the river valleys may reach a maximum of in July. History In 1829, German physicist Georg Adolf Erman during a round-the-world (1828-1830) journey reported the existence of "Seven Ranges" (Sette Daban) between 135° and 140° E in the area of one of the upper tributaries of the Yudoma. The range was surveyed in 1934 by geologist Yuri Bilibin (1901—1952) together with mining engineer Evgeny Bobin (1897—1941) in the course of an expedition sent by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skalisty Range
The Skalisty Range (russian: Скалистый хребет; sah, Скалистай) is a range of mountains in far North-eastern Russia, part of the East Siberian System. Administratively the mountain chain belongs to the Sakha Republic. The area of the range is remote and desolate. The R504 Kolyma Highway passes through the northern part of the range. History The Skalisty Range, meaning "rocky" owing to numerous pointed crags of naked rock crowning the range, was relatively unknown until 1934. It was first surveyed by an expedition sent by the government of the Soviet Union led by geologist Yuri Bilibin (1901—1952) together with mining engineer Evgeny Bobin (1897—1941). Though located near the southern end of the Verkhoyansk Range, this remote mountain area had formerly not been considered part of it by geographers, along with the other ranges south and southeast of the course of the Aldan River and the Tompo. After conducting the first topographic survey of the area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
