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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] |
Ulakhan-Bom
The Ulakhan-Bom (russian: Улахан-Бом; sah, Улахан Бом, meaning "Big Obstacle") is a range of mountains in far Russian Far East, North-eastern Russia, a southern prolongation of the Verkhoyansk Range, part of the East Siberian System. Administratively the mountain chain belongs to the Sakha Republic. The urban locality of Solnechny, Sakha Republic, Solnechny is located near the slopes of the range, by the Allakh-Yun River. Geography The Ulakhan-Bom stretches roughly from north to south for about to the west of the Sette-Daban, forming a group of three parallel ranges, together with the Skalisty Range further to the east. It is bound in the north by the Tompo, Tompo River, which separates it from the Verkhoyansk Range proper. To the west it is bound by the wide Aldan River valley and to the south by the Yudoma River. The Tyry river cuts across the northern section of the Ulakhan-Bom. The Khanda (river), Khanda river cuts across the range further south. The small ... [...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] |
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] |
Khabarovsk Krai
Khabarovsk Krai ( rus, Хабаровский край, r=Khabarovsky kray, p=xɐˈbarəfskʲɪj kraj) is a federal subject (a krai) of Russia. It is geographically located in the Russian Far East and is a part of the Far Eastern Federal District. The administrative centre of the krai is the city of Khabarovsk, which is home to roughly half of the krai's population and the largest city in the Russian Far East (just ahead of Vladivostok). Khabarovsk Krai is the fourth-largest federal subject by area, and has a population of 1,343,869 as of 2010. The southern region lies mostly in the basin of the lower Amur River, with the mouth of the river located at Nikolaevsk-on-Amur draining into the Strait of Tartary, which separates Khabarovsk Krai from the island of Sakhalin. The north occupies a vast mountainous area along the coastline of the Sea of Okhotsk, a marginal sea of the Pacific Ocean. Khabarovsk Krai is bordered by Magadan Oblast to the north, Amur Oblast, Jewish Au ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allakh-Yun River
The Allakh-Yun (russian: Аллах-Юнь, sah, Ааллаах Үүн, ''Aallaax Üün'') is a river in Sakha Republic and Khabarovsk Krai, Russia. It is a right tributary of the Aldan. It is long, and has a drainage basin of . Geography The Allakh-Yun arises at an elevation of around as the outflow from the mountain lake Amparyndzha, in the south-eastern Verkhoyansk Range. It flows generally in a south-westerly direction through a narrow valley along the Yudoma-Maya Highlands, to the east of the Sette-Daban range. The river cuts through the Ulakhan-Bom Ridge, before flowing into the Aldan by the southern end of the Kyllakh Range, at an elevation of , approximately from the settlement of Eldikan. Google Earth At its mouth, the Allakh-Yun is about wide and deep. The Allakh-Yun freezes over from mid-October until late May. Local economy and infrastructure The river is navigable on its lower and middle sections. The surrounding area is very sparsely settled, with the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tompo River
The Tompo (russian: Томпо) is a river in the Sakha Republic (Yakutia), Russia, a right tributary of the Aldan, part of the Lena basin. River Tompo gives its name to the Tompo District. It flows across desolate regions, Topolinoye being the only inhabited place in the long course of the river.Google Earth The Tompo is not navigable. The area of the river's drainage basin is . Course The Tompo originates in the southern slopes of the Elgi Plateau. For about , the river displays the characteristics of a typical mountain river, flowing within a deep and narrow valley bound by steep slopes. In its uppermost course the Tompo runs roughly northward along the northern side of the Suntar-Khayata mountains; after roughly it turns and follows a generally westward direction for about through the southern part of the Elgi Plateau. Downstream from the mouth of the Delinya, its 2nd largest tributary, which flows from the central part of the Yana-Oymyakon Highlands, the Tompo bends SSE i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Siberian System
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 Bering Strait in the Far Eastern Federal District and Northeast Siberia. The whole area of the East Siberian System has a very low population density. The territory of the mountain system is one of the Great Russian Regions. In some areas of the East Siberian Mountains, such as the Kisilyakh Range and the Oymyakon Plateau there are kigilyakhs, the rock formations that are highly valued in the culture of the Yakuts. Geography The East Siberian System consists of several separate sections of mountain ranges rising to the north and south of the Arctic Circle. The main group of ranges stretches for a distance of nearly from the Lena River valley to Cape Dezhnev, at the eastern end of the Chukotka Peninsula. Although it reaches a width of roughly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Khandyga
Khandyga (russian: Хандыга; sah, Хаандыга) is an urban locality (an urban-type settlement) and the administrative center of Tomponsky District in the Sakha Republic, Russia, northeast of Yakutsk, the capital of the republic. As of the 2010 Census, its population was 6,638. Geography Khandyga is located on the northeast corner of the Aldan River, by a bend where the river turns from north to west. The R504 Kolyma Highway passes through the town and the Ulakhan-Bom and Sette-Daban mountain ranges rise to the east. History It was founded in 1938 as a base for the construction of the Kolyma Highway towards Magadan. During World War II, an airfield was built here for the Alaska-Siberian air route used to ferry American Lend-Lease aircraft to the Eastern Front.Lebedev, pp. 44–49 From 1951 until 1954, it served as a base for Yanstroy forced-labor camp of the gulag network. In 1954, Khandyga became the administrative center of Tomponsky District. It was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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] |
Eduard Suess
Eduard Suess (; 20 August 1831 - 26 April 1914) was an Austrian geologist and an expert on the geography of the Alps. He is responsible for hypothesising two major former geographical features, the supercontinent Gondwana (proposed in 1861) and the Tethys Ocean. Biography Eduard Suess was born on 20 August 1831 in London, England, the oldest son of Adolph Heinrich Suess, a Lutheran Saxon merchant, and mother Eleonore Friederike Zdekauer. Adolph Heinrich Suess was born on 11 March 1797 in Saxony, Holy Roman Empire and died on 24 May 1862 in Vienna, Austrian Empire, German confederation; Eleonore Friederike Zdekauer was born in Prague, nowadays part of the Czech Republic, which once belonged to the Holy Roman Empire and the Austrian Empire. When Eduard Suess was born, his family relocated to Prague, and then to Vienna when he was 14. He became interested in geology at a young age. While working as an assistant at the Hofmuseum in Vienna, he published his first paper—on the g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lena Plateau
The Lena Plateau, also known as Prilensky Plateau ( rus, Приленское плато, ''Prilenskoye Plato''; sah, Өлүөнэтээҕи хаптал хайалаах сир), is one of the great plateaus of Siberia. Administratively it is mostly within the Sakha Republic (Yakutia), with a small sector in the Irkutsk Oblast, Far Eastern Federal District, Russia. The plateau is named after the Lena River, which flows across it.Google Earth Protected areas There are spectacularly eroded rock formations composed of gypsum-bearing and saline limestone, dolomite and, in some places sandstone, in different spots of the plateau. The Lena Pillars, lining the banks of river Lena in the region, are the most well-known of these features. They were declared a UNESCO World Heritage Site in 2012. Other protected areas in the plateau are the Sinyyaya Pillars by river Sinyaya, and the Turuuk Khaya Rocks by the Lyutenge River. The Olyokma Nature Reserve is located on the eastern side, partl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
