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Stanovik Range
The Stanovik ( rus, Становик) is a mountain range in the Transbaikal Region (Zabaykalsky Krai) of Siberia, Russia. The southern end of the range is very close to the border with Mongolia. The nearest village is Mordoy (Мордой), Kyrinsky District. The range is part of the Trans-Baikal conifer forests ecoregion. Geography The Stanovik Range is part of the Khentei-Daur Highlands, South Siberian System. It rises on the left bank of the upper course of the Onon River and stretches roughly northeastwards for over between two of its left tributaries, the Kyra and the Aksha. It is bound by the Bylir River valley to the west and near its source it connects with the Khentei Range. The width of the Stanovik ranges between a maximum of and a minimum of .Google Earth The average summits of the Stanovik reach between and . The highest point is a high unnamed peak. Much like in neighboring ranges, the relief is dominated by moderate height mountains with an abundance of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Russia
Russia (, , ), or the Russian Federation, is a List of transcontinental countries, transcontinental country spanning Eastern Europe and North Asia, Northern Asia. It is the List of countries and dependencies by area, largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across Time in Russia, eleven time zones and shares Borders of Russia, land boundaries with fourteen countries, more than List of countries and territories by land borders, any other country but China. It is the List of countries and dependencies by population, world's ninth-most populous country and List of European countries by population, Europe's most populous country, with a population of 146 million people. The country's capital and List of cities and towns in Russia by population, largest city is Moscow, the List of European cities by population within city limits, largest city entirely within E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Siberian System
The South Siberian Mountains ( rus, Южно-Сибирские горы) are one of the largest mountain systems of the Russian Federation. The total area of the system of mountain ranges is more than 1.5 million km². The South Siberian Mountains are located in the Siberian and Far Eastern Federal Districts of Russia, as well as partly in Mongolia. The territory of the mountain system is one of the Great Russian Regions. Geography The system is composed of a number of ranges aligned in an east–west direction stretching for almost . Part of them are near the border with Mongolia and China, while others rise further north. To the south the South Siberian ranges merge with the Mongolian and Chinese mountain chains and plateaus. In the west lies the Dzungarian Basin and to the east the Mongolian Plateau. To the north the South Siberian Mountains merge with the West Siberian Lowland and the Central Siberian Plateau, both on the Russian side. To the southeast the Baikal Range is sep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sokhondo Nature Reserve
Sokhondo Nature Reserve (russian: Сохондинский заповедник) (also Sokhondinskiy) is a Russian 'zapovednik' (strict nature reserve) in the south of Eastern Siberia, 25 km north of the border with Mongolia. It is the farthest source of the Amur River, and is centered on the Sokhondo Mountain massif (), in the highest sector of the Khentei-Chikoy Highlands in the Khentei Range mountain range. The Sokhondo massif has two peaks (Big Sokhondo and Little Sokhondo), and is an ancient volcano. Also within the borders are many lakes of glacial origin. In 1985, Sokhondo was named a UNESCO MAB (Man and Biosphere) Biosphere Reserve. The reserve is situated in the Chita district of Chita Oblast. Topography The Sokhondo Reserve is in a mountainous area of the trans-Baikal region (east of Lake Baikal). The two main peaks (Big Sokhondo and Little Sokhondo) are within 100 meters of each other in height, but are separated by rivers and valleys. To the southeast of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains And Hills Of Russia ...
This is a list of mountains and hills of Russia. List by elevation Over 5000 meters 4000 to 4999 meters 3000 to 3999 meters 2000 to 2999 meters 1000 to 1999 meters Under 1000 metres See also *Highest points of Russian Federal subjects *List of Altai mountains *List of mountains in Mongolia *List of mountains in China *List of ultras of Northeast Asia *List of volcanoes in Russia *List of lakes of Russia Notes References External links Russia - Highest Mountainsfrom GeoNamesfrom World AtlasRussia mountainsfrom Peakery {{Russia topics Russia Russia Russia Mountains and hills Russia Russia Russia (, , ), or the Russian Federation, is a List of transcontinental countries, transcontinental country spanning Eastern Europe and North Asia, Northern Asia. It is the List of countries and dependencies by area, largest country in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Golets (geography)
Golets ( rus, голец), plural Goltsy ( rus, Гольцы), is a type of bald mountain summit of certain areas of Siberia. The term is part of the geographical name of several peaks in the region. Description ''Golets'' protrude above the treeline and are usually round or blunt. They are barren, rocky or stony, and only rarely lichens or stunted small scrubs such as Siberian pine, may grow on them. Bare rock slopes, kurums and cliffs are common. The term is usually found in the names of mountaintops in the South Siberian System, especially in Transbaikalia and the Sayan Mountains. The zone below the golets is normally the highest of the altitudinal vegetation zones, above the mountain tundra of the alpine belt.Sizykh, A. (2016) ''Formation of an Ecotone at the Boundary of Forest and Mountain Tundra—Morskoy Ridge as an Example, Middle Part of Eastern Coast of Lake Baikal.'' Open Access Library Journal, 3, 1-4. This kind of mountains may consist in single high peaks connect ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dwarf Cedar
''Pinus sibirica'', or Siberian pine, in the family Pinaceae is a species of pine tree that occurs in Siberia from 58°E in the Ural Mountains east to 126°E in the Stanovoy Range in southern Sakha Republic, and from Igarka at 68°N in the lower Yenisei River, Yenisei valley, south to 45°N in central Mongolia. Description ''Pinus sibirica'' is a member of the Pinus classification, white pine group, ''Pinus'' subgenus ''Strobus'', and like all members of that group, the leaves ('needles') are in fascicles (bundles) of five, with a deciduous sheath. They are 5–10 cm long. Siberian pine conifer cone, cones are 5–9 cm long. The 9–12 mm long seeds have only a vestigial wing and are dispersed by spotted nutcrackers. Siberian pine is treated as a variety or subspecies of the very similar Swiss pine (''Pinus cembra'') by some botanists. It differs in having slightly larger cones, and needles with three resin canals instead of two in Swiss pine. Like other European ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga
Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces, and larches. The taiga or boreal forest has been called the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean (including much of Siberia), much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan (on the island of Hokkaidō). The main tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly spruce, Scandinavian and Finnish taiga consists of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earthquake
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for Episodic tremor and slip, non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Google Earth
Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geographic information system, GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a Computer keyboard, keyboard or computer mouse, mouse. The program can also be downloaded on a smartphone or Tablet computer, tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Khentei Range
The Khentei Range ( rus, Хэнтэй) is a mountain range in the Transbaikal Region (Zabaykalsky Krai) of Siberia, Russia. The range is part of the Trans-Baikal conifer forests ecoregion. The Sokhondo Nature Reserve is located in the area of the range. Geography The Khentei Range is part of the Khentei-Daur Highlands, South Siberian System. It rises on the right bank of the upper course of the Ingoda River and stretches roughly northeastwards for over until the source of the Bylir River, where it joins with the Stanovik Range. The maximum width of the range is . Its southern spurs connect with the Onon-Baldzhin Range and in the west with the Pereval Range.Google Earth The predominant summits of the Khentei Range reach between and . The highest point is high Mount Golets Sokhondo, a ‘’golets’’-type of mountain with a bald peak. Other important peaks are Buryktyn-Yang () and Uluri Golets (). The relief is marked by a strong degree of horizontal and vertical di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
