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Minusinsk Hollow
Minusinsk Basin or Khakass-Minusinsk Basin (russian: Минусинская (Хакасско-Минусинская) котловина, ''Minusinskaya (Chakassko-Minusinskaya) kotlovina'') is in Khakassia and Krasnoyarsk Krai, Russia located among mountains of South Siberia. Geography It is bounded on the west by Kuznetsk Alatau, and east by the Sayan Mountains. See Geography of South-Central Siberia. Elevation varies between 200–700 m, constituting a plain with sparse hillocks and cut by valleys."Minusinsk Basin" an article from the '''' [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yenisey River
The Yenisey (russian: Енисе́й, ''Yeniséy''; mn, Горлог мөрөн, ''Gorlog mörön''; Buryat: Горлог мүрэн, ''Gorlog müren''; Tuvan: Улуг-Хем, ''Uluğ-Hem''; Khakas: Ким суғ, ''Kim suğ''; Ket: Ӄук, ''Quk''; Nenets: Ензя-ям’, ''Enzja-jam''), also romanised as Yenisei, Enisei, or Jenisej, is the fifth-longest river system in the world, and the largest to drain into the Arctic Ocean. Rising in Mungaragiyn-gol in Mongolia, it follows a northerly course before draining into the Yenisey Gulf in the Kara Sea. The Yenisey divides the Western Siberian Plain in the west from the Central Siberian Plateau to the east; it drains a large part of central Siberia. It is the central one of three large Siberian rivers that flow into the Arctic Ocean (the other two being the Ob and the Lena). The maximum depth of the Yenisey is and the average depth is . The depth of river outflow is and inflow is . Geography The Yenisey proper, from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abakan River
The Abakan (russian: Абака́н), (from the Khakas word for "bear's blood") is a river in the Republic of Khakassia, Russia. It is a left tributary of the Yenisey. The river is used for log driving and irrigation. The city of Abakan is located at the confluence of the Abakan and the Yenisey. Course It is formed by the confluence of the rivers Bolshoy Abakan and Maly Abakan. It rises in the western Sayan Mountains and flows northeast through the Minusinsk Depression to the Yenisey. It is about long from the Bolshoy Abakan's source, and for the Abakan proper. Its drainage basin covers . See also *List of rivers of Russia Russia can be divided into a European and an Asian part. The dividing line is generally considered to be the Ural Mountains. The European part is drained into the Arctic Ocean, Baltic Sea, Black Sea, and Caspian Sea. The Asian part is drain ... References Further reading * Rivers of Khakassia {{Russia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of 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-c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Khakassia
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, Stratum, 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 Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Depressions Of Russia
Depression may refer to: Mental health * Depression (mood), a state of low mood and aversion to activity * Mood disorders characterized by depression are commonly referred to as simply ''depression'', including: ** Dysthymia, also known as persistent depressive disorder ** Major depressive disorder, also known as clinical depression Economics * Economic depression, a sustained, long-term downturn in economic activity in one or more economies ** Great Depression, a severe economic depression during the 1930s, commonly referred to as simply ''the Depression'' ** Long Depression, an economic depression during 1873–96, known at the time as the ''Great Depression'' Biology * Depression (kinesiology), an anatomical term of motion, refers to downward movement, the opposite of elevation * Depression (physiology), a reduction in a biological variable or the function of an organ * Central nervous system depression, physiological depression of the central nervous system that can result ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Minusinsk Coal Basin
Minusinsk (russian: Минуси́нск; kjh, Минсуғ) is a historical town in Krasnoyarsk Krai, Russia. Population: 44,500 (1973). Geography Minusinsk marks the center of the Minusinsk Hollow, one of the most important archaeological areas north of Pazyryk. It is associated with the Afanasevo, Tashtyk, and Tagar cultures—all of them named after settlements in the vicinity of Minusinsk. History "About 330-200 B.C. the iron age triumphed at Minusinsk, producing spiked axes, partly bronze and partly iron, and a group of large collective burial places." Greco-Roman funerary masks, like those found at Pazyryk, make up the "Minusinsk group: at Trifonova, Bateni, Beya, Kali, Znamenka, etc." "The Indo-European aristocracy with its Sarmatian connections was succeeded at Minusinsk by the Kirghiz after the third century A.D." The Russian settlement of Minyusinskoye () was founded in 1739-1740Н. И. Дроздов, В. С. Боровец "Енисейский энцик ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saline Water
Saline water (more commonly known as salt water) is water that contains a high concentration of dissolved salts (mainly sodium chloride). On the United States Geological Survey (USGS) salinity scale, saline water is saltier than brackish water, but less salty than brine. The salt concentration is usually expressed in parts per thousand (permille, ‰) and parts per million (ppm). The USGS salinity scale defines three levels of saline water. The salt concentration in slightly saline water is 1,000 to 3,000 ppm (0.1–0.3%); in moderately saline water is 3,000 to 10,000 ppm (0.3–1%); and in highly saline water is 10,000 to 35,000 ppm (1–3.5%). Seawater has a salinity of roughly 35,000 ppm, equivalent to 35 grams of salt per one liter (or kilogram) of water. The saturation level is only nominally dependent on the temperature of the water. At one liter of water can dissolve about 357 grams of salt, a concentration of 26.3% w/w. At boiling () the amount that can be dissolved in o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abakan
Abakan (russian: Абака́н, p=ɐbɐˈkan; Khakas: , ''Ağban''/, ''Abaxan'') is the capital city of the Republic of Khakassia, Russia, located in the central part of Minusinsk Depression, at the confluence of the Yenisei and Abakan Rivers. As of the 2010 Census, it had a population of 165,214—a slight increase over 165,197 recorded during the 2002 Census and a further increase from 154,092 recorded during the 1989 Census. History Abakansky '' ostrog'' (), also known as Abakansk (), was built at the mouth of the Abakan River in 1675. In the 1780s, the '' selo'' of Ust-Abakanskoye () was established in this area. It was granted town status and given its current name on 30 April 1931.Resolution of April 30, 1931 Chinese exiles In 1940, Russian construction workers found ancient ruins during the construction of a highway between Abakan and Askiz. When the site was excavated by Soviet archaeologists in 1941–1945, they realized that they had discovered a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuba River
The Tuba (russian: Туба́) is a river in Krasnoyarsk Krai in Siberia in Russia. It is formed by the confluence of the rivers Kazyr (Казыр) and Amyl (Амы́л) and is a right tributary of the Yenisey. The length of the river proper is or from the headwaters of the Kazyr in the Eastern Sayan Mountains in the Minusinsk Hollow. The area of its basin, which includes more than a thousand lakes, is . The Tuba flows into the Krasnoyarsk Reservoir Krasnoyarsk Reservoir, known also as the Krasnoyarsk Sea, is an artificial lake which was created by the construction of the Krasnoyarsk Dam. It is one of the largest artificial reservoirs in the world. In Russia, it now ranks second (after the Br ... so that the mouth of the Tuba is actually part of the reservoir. The river is navigable at high water to from its mouth, but it freezes sometime around late October to early December, and thaws from April to early May. There are two (sometimes considered three) road bridges and a r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Soviet Encyclopedia
The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya entsiklopediya'' (or '' Great Russian Encyclopedia'') in an updated and revised form. The GSE claimed to be "the first Marxist–Leninist general-purpose encyclopedia". Origins The idea of the ''Great Soviet Encyclopedia'' emerged in 1923 on the initiative of Otto Schmidt, a member of the Russian Academy of Sciences. In early 1924 Schmidt worked with a group which included Mikhail Pokrovsky, (rector of the Institute of Red Professors), Nikolai Meshcheryakov (Former head of the Glavit, the State Administration of Publishing Affairs), Valery Bryusov (poet), Veniamin Kagan (mathematician) and Konstantin Kuzminsky to draw up a proposal which was agreed to in April 1924. Also involved was Anatoly Lunacharsky, People's Commissar of Education ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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