|
Cherny Iyus
Cherny Iyus is a mountain river in the northern part of Khakassia, Russia. It flows through the territories of the Shirinsky and Ordzhonikidze districts. Merging with the Bely Iyus it forms the Chulym River, the right tributary of the Ob. Etymology Also known as Hara-Üüs, Chërnyy Iyus, Chyorny Iyus, Chyorny Yus, Czernoi Ijus, Tchernoi Yious Russian name comes from local name . Occurs in the pre-reform spelling , and in the Khakass spelling . An analysis of the toponymy of the Khakass-Minusinsk basin and the areas adjacent to it indicates that, along with the stratified Turkic toponyms of a later origin, toponyms clarified from the Ugric and Samoyedic languages dominated here. The inhabitants of the Urals call the rivers flowing to the West White rivers; those that flow to the East or to Siberia, in Black rivers. Description Cherny Iyus belongs to the middle size rivers of Khakassia. The length of the river is long. Drainage basin of Cherny Iyus is . Sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordzhonikidzevsky District, Republic Of Khakassia
Ordzhonikidzevsky District (; Khakas: , ''Orconikidze aymağı'') is an administrativeLaw #20 and municipalLaw #61 district (raion), one of the eight in the Republic of Khakassia, Russia. It is located in the north of the republic. The area of the district is . Its administrative center An administrative centre is a seat of regional administration or local government, or a county town, or the place where the central administration of a commune, is located. In countries with French as the administrative language, such as Belgiu ... is the rural locality (a settlement) of Kopyovo. Population: The population of the administrative center accounts for 34.3% of the district's total population. References Notes Sources * * {{Use mdy dates, date=January 2013 Districts of Khakassia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mineral Water
Mineral water is water from a mineral spring that contains various minerals, such as salts and sulfur compounds. It is usually still, but may be sparkling ( carbonated/ effervescent). Traditionally, mineral waters were used or consumed at their spring sources, often referred to as "taking the waters" or "taking the cure," at places such as spas, baths and wells. Today, it is far more common for mineral water to be bottled at the source for distributed consumption. Travelling to the mineral water site for direct access to the water is now uncommon, and in many cases not possible because of exclusive commercial ownership rights. More than 4,000 brands of mineral water are commercially available worldwide. In many places the term "mineral water" is colloquially used to mean any bottled carbonated water or soda water, as opposed to tap water. Composition The more calcium and magnesium ions that are dissolved in water, the '' harder'' it is said to be; water with few diss ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siberia
Siberia ( ; , ) is an extensive geographical region comprising all of North Asia, from the Ural Mountains in the west to the Pacific Ocean in the east. It has formed a part of the sovereign territory of Russia and its predecessor states since the lengthy conquest of Siberia, which began with the fall of the Khanate of Sibir in 1582 and concluded with the annexation of Chukotka in 1778. Siberia is vast and sparsely populated, covering an area of over , but home to roughly a quarter of Russia's population. Novosibirsk, Krasnoyarsk, and Omsk are the largest cities in the area. Because Siberia is a geographic and historic concept and not a political entity, there is no single precise definition of its territorial borders. Traditionally, Siberia spans the entire expanse of land from the Ural Mountains to the Pacific Ocean, with the Ural River usually forming the southernmost portion of its western boundary, and includes most of the drainage basin of the Arctic Ocean. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daniel Gottlieb Messerschmidt
Daniel Gottlieb Messerschmidt (; September 16, 1685 – March 25, 1735) was an ethnic German physician, naturalist and geographer who lived in the Polish–Lithuanian Commonwealth and later in the Russian Empire. He was among the first to conduct a scientific exploration of Siberia, which led to the unearthing of the first fossil mammoth. Life and travels Messerschmidt was born in Danzig (then part of Royal Prussia in the Polish–Lithuanian Commonwealth) and studied medicine in Jena and Halle, where he obtained a doctorate degree on "... the brains as the predominant principle of all medical science" in 1713 and settled as a medical doctor in Danzig. He studied the natural history collections of Johann Philipp Breyne (1680–1764) and through Robert Erskine, superintendent of the Kunstkamera he was invited to St Petersburg. He arrived on April 9, 1718, and was introduced to the Russian emperor Peter the Great in 1716. By decree of November 5, 1718, Peter gave Messerschmidt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irtysh
The Irtysh is a river in Russia, China, and Kazakhstan. It is the chief tributary of the Ob (river), Ob and is also the longest tributary in the world. The river's source lies in the Altai Mountains, Mongolian Altai in Dzungaria (the northern part of Xinjiang, China) close to the border with Mongolia. The Irtysh's main tributaries include the Tobol, Demyanka and the Ishim (river), Ishim. The Ob-Irtysh system forms a major drainage basin in Asia, encompassing most of West Siberian Plain, Western Siberia and the Altai Mountains. Geography From its origins as the ''Kara-Irtysh'' (Black Irtysh) in the Mongolian Altay mountains in Xinjiang, China, the Irtysh flows northwest through Lake Zaysan in Kazakhstan, meeting the Ishim (river), Ishim and Tobol rivers before merging with the Ob near Khanty-Mansiysk in western Siberia, Russia after . The name Black Irtysh (''Kara-Irtysh'' in Kazakh, or ''Cherny Irtysh'' in Russian) is applied by some authors, especially in Russia and Kazakh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zyryanskoye, Tomsk Oblast
Zyryanskoye () is a rural locality (a '' selo'') and the administrative center of Zyryansky District, Tomsk Oblast, Russia Russia, or the Russian Federation, is a country spanning Eastern Europe and North Asia. It is the list of countries and dependencies by area, largest country in the world, and extends across Time in Russia, eleven time zones, sharing Borders .... Population: References Notes Sources * * Rural localities in Tomsk Oblast {{TomskOblast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Achinsk
Achinsk () is a city in Krasnoyarsk Krai, Russia, located on the right bank of the Chulym River near its intersection with the Trans-Siberian Railway, west of Krasnoyarsk. It has a population of 109,155 as of the 2010 Census. History Achinsk is one of the oldest known inhabited places in the area. Paleontological study has shown that people lived here as early as 28,000–20,000 BCE. Some of these ancient caves are located east of the city. The modern city, however, was founded on July 25, 1641 as an '' ostrog'' on the Bely Iyus River. After the fire of 1683, it was moved to the Chulym River (a tributary of the Ob); hence, the official foundation date of the city is considered to be July 25, 1683. The name of the location derives from the Turkic tribal group Achi or Achigi. The first fort in 1683 was built with high square stockade walls. In the corners were placed watch towers. Initially the garrison had fifteen Cossacks patrolling it. In 1710, a new woode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
State Water Register
State Water Register () is a systematized collection of documented information on water bodies owned by the Russian Federation, subjects of the Russian Federation, municipalities, individuals and legal entities and individual entrepreneurs, on their use, and on river basins and watershed districts.Постановление Правительства РФ № 253 от 28 апреля 2007 года «Положение о ведении Государственного водного реестра» The register was created by the Resolution (legal act) of the Government of the Russian Federation № 253 of 28 April 2007 signed by Prime Minister of Russia, Mikhail Fradkov. The information contained in the register is publicly available, except if classified Classified may refer to: General *Classified information, material that a government body deems to be sensitive *Classified advertising or "classifieds" Music *Classified (rapper) (born 1977), Canadian rapper * The Classifi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...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 mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, 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 (Lamination (geology), laminae) less than one centimeter in thickness. This property is called ''Fissility (geology), 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 narrower 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 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syenite
Syenite is a coarse-grained intrusive igneous rock with a general composition similar to that of granite, but deficient in quartz, which, if present at all, occurs in relatively small concentrations (< 5%). It is considered a granitoid. Some syenites contain larger proportions of components and smaller amounts of material than most granites; those are classed as being of . The |
