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Lateral Range
The Lateral Range (russian: Боковой хребет; ka, გვერდითი ქედი; az, Yan silsiləsi) is a mountain range in the Russian Federation and Georgia, with a very small part in Azerbaijan. The range is part of the Greater Caucasus. Some swathes of the range are protected areas, under the Kabardino-Balkaria Nature Reserve and the North Ossetia Nature Reserve. Geology In its western part the range is composed of Paleozoic and Triassic sedimentary rocks, in its central part of Upper Proterozoic and Paleozoic crystalline schist and granite, and in its eastern part of Jurassic shale. Geography The Lateral Range is characterized by alpine landforms. It runs parallel to the northern side of the Main Caucasian Range, to the south of the Skalisty Range, along the Krasnodar Territory, Karachay-Cherkessia, Kabardino-Balkaria, North Ossetia, Ingushetia, Chechnya and Dagestan federal subjects of Russia, as well as the countries of Georgia and Azerbaijan.Google ... [...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] |
North Ossetia Nature Reserve
North Ossetia Nature Reserve (russian: Северо-Осетинский заповедник) (also Severo-Osetinsky) is a Russian 'zapovednik' (strict nature reserve) in the high mountains on the northern slope of the Caucasus Mountains with the heights ranging from 650 meters - 4,249 meters. There are 76 glaciers in the reserve with a total area of . The site is centered on the Ardon River valley, in the Alagirsky District of North Ossetia-Alania. It was formally created in 1967, and covers a total area of . Topography The North Ossetia Reserve has a terrain that steep mountain slopes and deep river valleys. The Ardon River (in English, "Mad River") basin in the reserve has five parallel ridges running north–south. The reserve is bounded on the north by foothills and steppes running down to the town of Alagir, on the east by further north-slope river valleys, on the south by the main ridge of the Caucasus Mountains, and on the west by Alaniya National Park. There are mor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caucasus
The Caucasus () or Caucasia (), is a region between the Black Sea and the Caspian Sea, mainly comprising Armenia, Azerbaijan, Georgia, and parts of Southern Russia. The Caucasus Mountains, including the Greater Caucasus range, have historically been considered as a natural barrier between Eastern Europe and Western Asia. Mount Elbrus in Russia, Europe's highest mountain, is situated in the Western Caucasus. On the southern side, the Lesser Caucasus includes the Javakheti Plateau and the Armenian highlands, part of which is in Turkey. The Caucasus is divided into the North Caucasus and South Caucasus, although the Western Caucasus also exists as a distinct geographic space within the North Caucasus. The Greater Caucasus mountain range in the north is mostly shared by Russia and Georgia as well as the northernmost parts of Azerbaijan. The Lesser Caucasus mountain range in the south is occupied by several independent states, mostly by Armenia, Azerbaijan, and Georgia, but also ... [...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] |
Krasnodar Territory
Krasnodar Krai (russian: Краснода́рский край, r=Krasnodarsky kray, p=krəsnɐˈdarskʲɪj kraj) is a federal subject of Russia (a krai), located in the North Caucasus region in Southern Russia and administratively a part of the Southern Federal District. Its administrative center is the city of Krasnodar. The third most populous federal subject, the krai had a population of 5,226,647 as of the 2010 Census. Krasnodar Krai is formally and informally referred to as Kuban (russian: Кубань), a term denoting the historical region of Kuban situated between the Sea of Azov and the Kuban River which is mostly composed of the krai's territory. It is bordered by Rostov Oblast to the north, Stavropol Krai to the east, Karachay-Cherkessia to the south-east, and Adygea is an enclave entirely within the krai. Krasnodar Krai shares an international border with the disputed region of Georgia, Abkhazia, to the south, and borders annexed Crimea to the west, across t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skalisty Range, Caucasus
Skalisty Range (russian: Скалистый хребет) is a mountain range in the Greater Caucasus, Russian Federation. Geography The Skalisty Range is a chain of ten separate mountain massifs stretching parallel to the northern side of the Lateral Range along the Krasnodar Territory, Karachay-Cherkessia, Kabardino-Balkaria and North Ossetia federal subjects. Its high mountain massifs are separated by the upper reaches of the rivers flowing on the northern slope of the Greater Caucasus. It extends from northwest to southeast for 931 km from the upper course of the Belaya River, a left tributary of the Kuban, to the west, reaching almost the Terek River in the east, in the area of Vladikavkaz town.Google Earth The average height of the Skalisty Range is between and in the west, reaching in the east. The highest point is high Karakaya, located between rivers Chegem and Cherek in the Republic of Kabardino-Balkaria. The ridge has steep, in places vertical, southern sl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Caucasian Range
The Main Caucasian Range (russian: Главный Кавказский хребет; ka, კავკასიონის მთავარი წყალგამყოფი ქედი; az, Baş Qafqaz silsiləsi) is a mountain range in the Russian Federation, Georgia and Azerbaijan. It is the dividing range of the Greater Caucasus. The protected areas of the range are the Teberda Nature Reserve, Kabardino-Balkaria Nature Reserve and the North Ossetia Nature Reserve. Geography The Main Caucasian Range marks the divide between the North Caucasus to the north and the South Caucasus to the south. It stretches from Mount Chugush near the Black Sea, to the Khizi District of Azerbaijan near the Caspian Sea. The main range runs parallel to the southern side of the Lateral Range, along Abkhazia, Adygea, the Krasnodar Territory, Karachay-Cherkessia, Kabardino-Balkaria, North Ossetia, Ingushetia, Chechnya and Dagestan federal subjects of Russia, as well as the countries of Georg ... [...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] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crystalline Rock
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification. The word ''crystal'' derives from the Ancient Greek word (), meaning both "ice" and "rock crystal", from (), "icy cold, frost". Examples of large crystals include snowflakes, diamonds, and table salt. Most inorganic solids are not crystals but polycrystals, i.e. many microscopic crystals fused together into a single solid. Polycrystals include most metals, rocks, ceramics, and ice. A third category of sol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
