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Anabar Shield
Anabar Shield (russian: Анабарский щит) is a shield in Siberia. It is an exposed basement of the Siberian Craton. Together with the Aldan Shield to the southeast, the Anabar Shield is one of the main features of the craton. On the surface it appears as an upland of moderate height, built of gneisses and crystalline shales folded in the Archean. There are numerous dislocations and intrusions. The outer zone has slightly undulated layers of Proterozoic deposits.Анабарский массив The Anabar Shield coincides geographically with the |
Sibiria Craton NO
Sibiria is a Swedish indie pop band from Östersund Östersund (; sma, Staare) is an urban area (city) in Jämtland in the middle of Sweden. It is the seat of Östersund Municipality and the capital of Jämtland County. Östersund is located at the shores of Sweden's fifth-largest lake, Storsjön, ..., signed by the record label Hybris. It was founded in 2003 by the guitarist Martin Abrahamsson (also in the band Vapnet), the singer Martin Hanberg (Vapnet) and the guitarist Erik Laquist. In 2006, the drummer Eric Ramsey joined the band. Discography Albums *''Norrlands Inland'' (September 28, 2005) *''Inom Familjen'' (November 15, 2006) Singles *"Sibiria" (CDR) (April 2, 2003) *"Ljusdal" (CDR) (February 11, 2004) *"#3" (CDR) (August 8, 2004) *"Christian Olsson" (CDR) (August 8, 2005) *"(Jag kunde ha varit) Vem som helst" (MP3) (September 17, 2005) *"Omtagning" (CDR) (June 25, 2006) *"Det har varit svårare" (MP3) (October 25, 2006) External links Official website {{ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Siberian Plateau
The Central Siberian Plateau (russian: Среднесибирское плоскогорье, Srednesibirskoye ploskogorye; sah, Орто Сибиир хаптал хайалаах сирэ) is a vast mountainous area in Siberia, one of the Great Russian Regions. Geography The plateau occupies a great part of central Siberia between the Yenisei and Lena rivers. It is located in the Siberian Platform and extends over an area of , between the Yenisei in the west and the Central Yakutian Lowland in the east. To the south it is bound by the Altai Mountains, Salair Ridge, Kuznetsk Alatau, the Eastern and Western Sayan Mountains and other mountains of Tuva, as well as the North Baikal Highlands and Baikal Mountains. To the north of the plateau lie the North Siberian Lowland and to the east the plateau gives way to the Central Yakutian Lowland and the Lena Plateau. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Krasnoyarsk Krai
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of Eart ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunguska Basin
The Tunguska Basin is a sedimentary basin, in Siberia. Geography Much of the Siberian Traps Large Igneous Province is inside. The area is of about in Krasnoyarsk Territory and Sakha Republic, between the Yenisei and Lena rivers. It contains a huge untapped coal reserve. Its main settlements there are Norilsk, Igarka, and Yeniseisk. The Tunguska rivers cross the basin. On June 30, 1908, near the Stony Tunguska River the Tunguska Event took place. Geology Boreholes in the Tunguska Basin indicate ubiquitous and abundant sills, which have great lateral extension. The Tunguska Basin makes up much of the Siberian Craton and has several subbasins. See also * Tunguska Plateau The Tunguska Plateau ( rus, Тунгусское плато) is a mountain plateau in Krasnoyarsk Krai, Siberia, Russia. It is a part of the Central Siberian Plateau. The plateau is located in largely uninhabited area, the village of Noginsk was ... References External links Encyclopedia.com ref ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Shields And Cratons
A craton is an ancient part of the Earth's continental crust which has been more or less stable since Precambrian times. Cratons whose ancient rocks are widely exposed at the surface, often with relatively subdued relief, are known as shields. If the ancient rocks are largely overlain by a cover of younger rocks then the 'hidden' craton may be referred to as a platform. List of shields * Western Ethiopian Shield * Amazonian Shield of central South America **Guiana Shield **Guaporé or Central Brazilian Shield * The Angaran Shield of West Siberia *Arabian-Nubian Shield * (Western) Australian Shield *Baltic Shield of Scandinavia and Eastern Europe *Canadian Shield a.k.a. Laurentian Shield *The China-Korean Shield containing the North China Craton *The East Antarctic Shield containing the East Antarctic Craton * Indian Shield *Man Shield List of named cratons Listed by modern continent and Gondwana, include: West Gondwana South America *Amazonian Craton **Guiana Shield ** ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Birekte Terrane
The Birekte (russian: Биректе; sah, Билэктэ) is a river in Yakutia (Sakha Republic), Russia. It is a tributary of the Olenyok with a length of . Its drainage basin area is . The river flows north of the Arctic Circle, across a lonely, desolate area devoid of settlements. Course The Birekte is a left tributary of the Olenyok. Its sources are in the northern fringes of the Central Siberian Plateau. It heads first southwards and, after the confluence of the Omonos, it flows roughly northeastwards. Finally it joins the left bank of the Olenyok river downstream from the confluence of the Ukukit, upstream of its mouth.Google Earth The river is fed by rain and snow. It is frozen between early October and late May. The longest tributary is the long Omonos (Омоноос) from the right. Birekte Terrane The Birekte terrane is located by the Anabar Shield, in the north-eastern part of the Siberian Craton, in the basins of the Popigay, Anabar, Birekte and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctica
Arctica or Arctida was an ancient continent which formed approximately 2.565 billion years ago in the Neoarchean era. It was made of Archaean cratons, including the Siberian Craton, with its Anabar/Aldan shields in Siberia, and the Slave, Wyoming, Superior, and North Atlantic cratons in North America. Arctica was named by because the Arctic Ocean formed by the separation of the North American and Siberian cratons. Russian geologists writing in English call the continent "Arctida" since it was given that name in 1987, alternatively the Hyperborean craton, in reference to the hyperboreans in Greek mythology. Nikolay Shatsky () was the first to assume that the crust in the Arctic region was of continental origin. Shatsky, however, was a "fixist" and, erroneously, explained the presence of Precambrian and Paleozoic metamorphic rocks on the New Siberian, Wrangel, and De long Islands with subduction. "Mobilists", on the other hand, also erroneously, proposed that N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akitkan
The Akitkan Range (russian: хребет Акиткан; zh, 阿基特坎山) is a mountain range in Irkutsk Oblast and Buryatia, Russian Federation.Google Earth The Paleoproterozoic Akitkan Orogen is named after the range. History Between 1855 and 1858 Ivan Kryzhin (d. 1884) took part in the Eastern Siberian expedition led by Russian astronomer and traveler Ludwig Schwarz. In 1857 he mapped the Kirenga River and, while exploring its right tributary, the Cherepanikha, Kryzhin discovered the formerly unknown Akitkan Range rising above the area of its source. The North Baikal Highlands, where the range rises, were explored between 1909 and 1911 by Russian geologist Pavel Preobrazhensky (1874 - 1944). He surveyed the river valley of the Chechuy, a right tributary of the Lena with its sources in the Akitkan. Overcoming numerous difficulties, Preobrazhensky managed to map for the first time a stretch of the Akitkan Range. Geography The Akitkan stretches roughly northwards for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kotuy
The Kotuy () is a river in Krasnoyarsk Krai, Russia. It is one of the two rivers that form the Khatanga; the other one being the Kheta. The Kotuy is long, and the area of its basin is . It freezes up in late September or early October and breaks up in late May or early June. Course The Kotuy has its source in the Putorana Mountains and flows north, cutting from the south across the western side of the Anabar Plateau. After leaving the plateau area it flows northwestwards until the confluence with the Kheta to form the Khatanga, a little distance upstream from Khatanga town.Google Earth Its main tributaries are the Moyero, the Tukalan, the Eriyechka, the Changada, and the Kotuykan, which has its source in the highest part of the Anabar Plateau. Lake Yessey is part of the river basin. See also *List of rivers of Russia Russia can be divided into a European and an Asian part. The dividing line is generally considered to be the Ural Mountains. The European part is dra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olenyok River
The Olenyok (russian: Оленёк, sometimes spelled ''Оленек'', ''Olenek''; sah, Өлөөн, Ölöön) is a major river in northern Siberian Russia, west of the lower Lena and east of the Anabar. It is long, of which around is navigable. Average water discharge is . The Olenyok is known for its abundance in fish. It is frozen for over eight months every year and the climate in its area is harsh because of the direct influence of the Arctic. History In 1633 Ivan Rebrov reached the Olenyok from the Lena delta and built a fort. In 1642–44 Rebrov and Fedot Alekseyev Popov reached the river but were driven out by the natives. Pioneering Russian Arctic explorer Vasili Pronchishchev and his wife Tatiana (Maria) died of scurvy in the area of the river in September 1736, while mapping the coasts of the Laptev Sea. After their deaths, husband and wife were interred at Ust-Olenyok, near the mouth of the Olenyok. Their tomb was moved after the bodies were exhumed in 1999. In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anabar River
The Anabar ( rus, Анабар, r=Anabar, in its upper course: Большая Куонамка ''Bolshaya Kuonamka''; sah, Анаабыр, translit=Anaabyr) is a river in Sakha, Russia. It is long ( counting the long Bolshaya Kuonamka ("Big Kuonamka") stretch of its upper course) and has a drainage basin of . Course The Anabar is formed at the confluence of the Malaya Kuonamka and Bolshaya Kuonamka at the edge of the North Siberian Lowland. The length of the Anabar proper is . The two rivers forming it have their sources in the northeastern part of the Anabar Plateau, part of the Central Siberian Plateau. There are many lakes in its basin. The Anabar basin is located between rivers Khatanga and Olenyok. The mouth of the river is in the Anabar Bay. Its mean annual discharge is , concentrated heavily in early summer when the ice that covers the river for most of the year thaws. The Uele river flows into the Laptev Sea close to the mouth of the Anabar, but it is not its tri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anabar Plateau
The Anabar Plateau ( rus, Анабарское плато) is a mountain plateau in Krasnoyarsk Krai and the Sakha Republic (Yakutia), Siberia, Russia. The plateau is in a latitude dominated by permafrost. The permafrost thickness under the Anabar Plateau reaches . Geography The Anabar Plateau is located north of the Arctic Circle in northeastern Krasnoyarsk Krai and northwestern Sakha Republic, SSE of the Taymyr Depression, the central part of the North Siberian Lowland. It is located north of the Vilyuy Plateau and is the northernmost feature of the Central Siberian Plateau, to which it is connected in the southeast. To the southwest it runs into the higher Putorana Mountains, the border between both not being well-defined. The average height of the plateau surface is around . There are slightly higher tableland type elevations running across the plateau area, mostly in a roughly east to west direction. The highest point is a high unnamed summit. The Big Kuonamka, which f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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