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Dzhugdzhur
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] |
Stanovoy Range
The Stanovoy Range (russian: Станово́й хребе́т, ''Stanovoy khrebet''; sah, Сир кура; ), is a mountain range located in the Sakha Republic and Amur Oblast, Far Eastern Federal District. It is also known as Sükebayatur and Sükhbaatar in Mongolian, or the Stanovoy Mountains, or Outer Khingan Range in English. The range was first studied and scientifically described by Russian researcher Alexander von Middendorff. History The range formed the border between Russia and China from 1689 (Treaty of Nerchinsk) to 1858 (Treaty of Aigun). Etymology The Evenks grouped the Dzhugdzhur, Stanovoy, and Yablonoi ranges under the name "Dzhugdzhur". In Evenk folklore this mountain system is known as the "backbone of the Earth". Geography The range runs roughly from west to east at the southern end of the Sakha Republic and the northern limit of Amur Oblast for roughly . It is bound by the Olyokma River in the west and the Uchur River in the east, which separates it ... [...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] |
Team Fortress 2
''Team Fortress 2'' is a 2007 multiplayer first-person shooter, first-person shooter game developed and published by Valve Corporation. It is the sequel to the 1996 ''Team Fortress'' Mod (video gaming), mod for ''Quake (video game), Quake'' and its 1999 remake, ''Team Fortress Classic''. The game was released in October 2007 as part of ''The Orange Box'' for Windows and the Xbox 360, and ported to the PlayStation 3 in December 2007. It was released as a standalone game for Windows in April 2008, and updated to support Mac OS X in June 2010 and Linux in February 2013. It is distributed online through Valve's digital retailer Steam (service), Steam, with Electronic Arts managing retail and console editions. Players join one of two teams—RED and BLU—and choose one of nine character classes to play as in game modes such as capture the flag and King of the Hill (game), king of the hill. Development was led by John Cook and Robin Walker (game designer), Robin Walker, the developer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siberia
Siberia ( ; rus, Сибирь, r=Sibir', p=sʲɪˈbʲirʲ, a=Ru-Сибирь.ogg) is an extensive geographical region, constituting all of North Asia, from the Ural Mountains in the west to the Pacific Ocean in the east. It has been a part of Russia since the latter half of the 16th century, after the Russians conquered lands east of the Ural Mountains. Siberia is vast and sparsely populated, covering an area of over , but home to merely one-fifth of Russia's population. Novosibirsk, Krasnoyarsk and Omsk are the largest cities in the region. Because Siberia is a geographic and historic region and not a political entity, there is no single precise definition of its territorial borders. Traditionally, Siberia extends eastwards from the Ural Mountains to the Pacific Ocean, and includes most of the drainage basin of the Arctic Ocean. The river Yenisey divides Siberia into two parts, Western and Eastern. Siberia stretches southwards from the Arctic Ocean to the hills of north-ce ... [...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] |
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 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] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Russian Far East
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jezo Spruce
''Picea jezoensis'' (sometimes misspelled ''Picea yezoensis''), the dark-bark spruce, Ezo spruce, Yezo spruce, or Jezo spruce, is a large evergreen tree growing to 30–50 m tall and with a trunk diameter of up to 2 m. It is native to northeast Asia, from the mountains of central Japan and the Changbai Mountains on the China-North Korea border, north to eastern Siberia, including the Sikhote-Alin, Kuril Islands, Sakhalin and Kamchatka. It is found in cold but humid temperate rain forests, and nowhere does its range extend more than 400 km from the Pacific Ocean. The specific epithet ''jezoensis'' derives from Ezo, an old name for Hokkaido and other islands north of the Japanese island of Honshu, where the species is found. The bark is thin and scaly, becoming fissured in old trees. The crown is broad conic. The shoots are pale buff-brown, glabrous (hairless) but with prominent pulvini. The leaves are needle-like, 15–20 mm long, 2 mm broad, flattened in cross-section, dar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dahurian Larch
''Larix gmelinii'', the Dahurian larch or Gmelin larch, is a species of larch native to eastern Siberia and adjacent northeastern Mongolia, northeastern China (Heilongjiang), South Korea and North Korea. Description ''Larix gmelinii'' is a medium-sized deciduous coniferous tree reaching 10–30 m tall, rarely 40 m, with a trunk up to 1 m diameter. The crown is broad conic; both the main branches and the side branches are level, the side branches only rarely drooping. The shoots are dimorphic, with growth divided into long shoots (typically 5–30 cm long) and bearing several buds, and short shoots only 1–2 mm long with only a single bud. The leaves are needle-like, light green, 2–3 cm long; they turn bright yellow to orange before they fall in the autumn, leaving the variably downy reddish-brown shoots bare until the next spring. The cones are erect, ovoid, 1–2 cm (rarely 2.5 cm) long, with 15–25 moderately reflexed seed scales; they are gre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Japanese Stone Pine
''Pinus pumila'', commonly known as the Siberian dwarf pine, dwarf Siberian pine, dwarf stone pine, Japanese stone pine, or creeping pine, is a tree in the family Pinaceae native to northeastern Asia and the Japanese isles. It shares the common name ''creeping pine'' with several other plants. Description The Siberian dwarf pine is a coniferous evergreen shrub ranging from in height, exceptionally up to , but may have individual branches that extend farther along the ground in length. In the mountains of northern Japan, it sometimes hybridises with the related Japanese white pine ('' Pinus parviflora''); these hybrids (''Pinus'' × ''hakkodensis'') are larger than ''P. pumila'', reaching tall on occasion. The leaves are needle-like, formed in bundles of five and are 4–6 centimetres long. The cones are 2.5–4.5 cm long, with large nut-like seeds (pine nuts). Distribution The range covers the Far East, Eastern Siberia, north-east of Mongolia, north-east of China ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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