Tunka Goltsy
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Tunka Goltsy
The Tunka Goltsy (russian: Тункинские гольцы) is a mountain range in Buryatia, Far Eastern Federal District, Russia. Geography Its length is 160 km, it is the easternmost part of the Eastern Sayan. Highest summit Strelnikov Peak (Algan Mundarga), 3157 m. Rivers: Irkut and other tributaries of Angara River See also *List of mountains and hills of Russia *Golets (geography) *Tunkin Depression Tunkin Depression is a volcanic field in Russia. The Tunkin Depression itself is a tectonic depression, part of the Baikal Rift Zone, between Lake Baikal and Khövsgöl Nuur. The depression consists of a number of basins and is covered by allu ... References Russian * Sayan Mountains {{Siberia-geo-stub ...
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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 ...
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Far Eastern Federal District
The Far Eastern Federal District (russian: Дальневосто́чный федера́льный о́круг, ''Dalnevostochny federalny okrug'') is the largest of the federal districts of Russia, eight federal districts of Russia but the least populated, with a population of 8,371,257 (75.5% urban) according to the Russian Census (2010), 2010 Census. The federal district lies entirely within the easternmost part of Asia and is coextensive with the Russian Far East. History The Far Eastern Federal District was established on May 18, 2000, by President of Russia, President Vladimir Putin and is currently being governed by presidential envoy Yury Trutnev. In November 2018, Buryatia and Zabaykalsky Krai were added to the federal district. The seat of the Far Eastern Federal District was moved from Khabarovsk to Vladivostok in December 2018. Demographics Federal subjects Largest cities (with population over 75,000) There are 82 cities in the Far Eastern Federal Di ...
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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 ...
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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 ...
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Angara River
The Angara ( Buryat and mn, Ангар, ''Angar'',  "Cleft"; russian: Ангара́, ''Angará'') is a major river in Siberia, which traces a course through Russia's Irkutsk Oblast and Krasnoyarsk Krai. It drains out of Lake Baikal and is the headwater tributary of the Yenisey. It is long, and has a drainage basin of . It was formerly known as the Lower or Nizhnyaya Angara (distinguishing it from the Upper Angara). Below its junction with the Ilim, it was formerly known as the Upper Tunguska (russian: Верхняя Тунгуска, ''Verkhnyaya Tunguska'', distinguishing it from the Lower Tunguska) and, with the names reversed, as the Lower Tunguska. Course Leaving Lake Baikal near the settlement of Listvyanka, the Angara flows north past the Irkutsk Oblast cities of Irkutsk, Angarsk, Bratsk, and Ust-Ilimsk. It then crosses the Angara Range and turns west, entering Krasnoyarsk Krai, and joining the Yenisey near Strelka, south-east of Lesosibirsk. Dams and reservoirs ...
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Tributaries
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & Scott ...
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Irkut River
The Irkut (russian: Ирку́т; Buryat and mn, Эрхүү гол, ''Erhüü go''l) is a river in the Buryat Republic and Irkutsk Oblast of Russia. It is a left tributary of the Angara. It flows out of lake Ilchir which is situated 50 km away from the highest peak of the Eastern Sayan Mountains, Munku-Sardyk. The length of the river is . The area of its basin is . The Irkut freezes up in late October or mid-November and stays icebound until late April or early May. The city of Irkutsk is located at the mouth of the Irkut on the Angara. Image:Irkut1.jpg, Irkut near the village of Zaktuy in the Tunkinsky National Park The Tunka or Tunkinsky National Park (Russian: Тункинский) is a national park located in south central Siberia. It covers a mountainous region centered on the Irkut River valley (also referred to as the Tunka Valley) that continues from ... Image:Irkut river from train.jpg, The Irkut as seen from a train window (near its confluence with the Angara ...
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Eastern Sayan
The Sayan Mountains (russian: Саяны ''Sajany''; mn, Соёны нуруу, ''Soyonï nurû''; otk, 𐰚𐰇𐰏𐰢𐰤, Kögmen) are a mountain range in southern Siberia, Russia (Buryatia, Irkutsk Oblast, Krasnoyarsk Krai, Tuva Republic and Khakassia) and northern Mongolia. In the past, it served as the border between Mongolia and Russia. The Sayan Mountains' towering peaks and cool lakes southwest of Tuva give rise to the tributaries that merge to become one of Siberia's major rivers, the Yenisei River, which flows north over 3,400 kilometres (2000 mi) to the Arctic Ocean. This is a protected and isolated area, having been kept closed by the Soviet Union since 1944. Geography Western Sayan At 92°E the Western Sayan system is pierced by the Ulug-Khem (russian: Улуг-Хем) or Upper Yenisei River, and at 106°, at its eastern extremity, it terminates above the depression of the Selenga-Orkhon Valley. It stretches almost at a right angle to the Western Sayan fo ...
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Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean ...
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Federal Subject
The federal subjects of Russia, also referred to as the subjects of the Russian Federation (russian: субъекты Российской Федерации, subyekty Rossiyskoy Federatsii) or simply as the subjects of the federation (russian: субъекты федерации, subyekty federatsii), are the constituent entities of Russia, its top-level political divisions according to the Constitution of Russia. Kaliningrad Oblast is the only federal subject geographically separated from the rest of the Russian Federation by other countries. According to the Russian Constitution, the Russian Federation consists of republics, krais, oblasts, cities of federal importance, an autonomous oblast and autonomous okrugs, all of which are equal subjects of the Russian Federation. Three Russian cities of federal importance (Moscow, Saint Petersburg, and Sevastopol) have a status of both city and separate federal subject which comprises other cities and towns (Zelenograd, Troitsk, ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ...
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