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Kyuyol-Yuryakh
The Kyuyol-Yuryakh (russian: Кюёль-Юрях; sah, Күөл-үрэх, ''Küöl-ürex'') is a river in the Sakha Republic (Yakutia), Russia. It has a length of and a drainage basin area of . The river flows north of the Arctic Circle, across territories of the East Siberian Lowland in Allaikhovsky District. It flows across Soluntakh, the largest lake in the area. There are no settlements along its course. The name of the river comes from the Yakut ''"Kuöl/urekh"'' ''(Күөл-үрэх)'', meaning "lake/river". Course The Kyuyol-Yuryakh has its sources in a small lake of the northern end of the Yana-Indigirka Lowland, to the east of the Muksunuokha basin. The river heads first roughly southwards across a tundra area marked by permafrost and numerous small lakes. After a stretch it bends and flows in an ESE direction until it meets the western shore of lake Soluntakh, forming the primary inflow of the relatively large lake. The Kyuyol-Yuryakh then flows out of the lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Soluntakh
Soluntakh (russian: Солунтах; sah, Солунтах, ''Soluntax'') is a freshwater lake in the Sakha Republic (Yakutia), Russia. It is one of the largest lakes in the Allaikhovsky District. The region where Soluntakh lies is uninhabited. Like most bodies of water in the area in has not been studied enough. A sector of the lake is a protected area. Geography Soluntakh lake is located north of the Arctic circle, in the central part of the Yana-Indigirka Lowland. It is crossed from west to east by the long Kyuyol-Yuryakh river, which enters its western shore roughly in the middle. All other inflowing rivers are small. There are many smaller lakes in the vicinity. The lake begins to freeze in mid September and stays under ice until early June.Google Earth Fauna The greater white-fronted goose and bean goose are some of the bird species known to nest in the lake. Soluntakh has also been explored as one of the probable sites providing a habitat for the Siberian crane, a crit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 drained into the Arctic Ocean and the Pacific Ocean. Notable rivers of Russia in Europe are Volga (which is the longest river in Europe), Pechora, Don, Kama, Oka and the Northern Dvina, while several other rivers originate in Russia but flow into other countries, such as the Dnieper and the Western Dvina. In Asia, important rivers are the Ob, the Irtysh, the Yenisei, the Angara, the Lena, the Amur, the Yana, the Indigirka, and the Kolyma. In the list below, the rivers are grouped by the seas or oceans into which they flow. Rivers that flow into other rivers are ordered by the proximity of their point of confluence to the mouth of the main river, i.e., the lower in the list, the more upstream. There is an alphabetical list of rivers at the end of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uryung-Ulakh
The Uryung-Ulakh or Yuryung-Ulakh (russian: Урюнг-Улах or Юрюнг-Уулаах; sah, Үрүҥ Уулаах, ''Ürün Uulaax'') is a river in the Sakha Republic (Yakutia), Russia. It has a length of and a drainage basin area of . The river flows north of the Arctic Circle, across territories of the East Siberian Lowland in Allaikhovsky District marked by permafrost. There are no settlements along its course. Course The Uryung-Ulakh is the main tributary of the Khroma. It has its sources in the lake of the same name, a fairly large lake of the southeastern part of the Yana-Indigirka Lowland located to the south of the Muksunuokha basin. The river heads first roughly southeastwards across a tundra area of swamps and numerous small lakes. After a long stretch it bends and meanders in an northeastern direction until it meets the western shore of lake Usun-Ulakh-Tubata (Усун-Уулаах-Тубата), south of the mouth of the Kyuyol-Yuryakh in the same lake. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allaikhovsky District
Allaikhovsky District (russian: Алла́иховский улу́с; sah, Аллайыаха улууһа, ''Allayyakha uluuha'') is an administrativeConstitution of the Sakha Republic, Article 45 and municipalLaw #172-Z #351-III district (raion, or ''ulus''), one of the thirty-four in the Sakha Republic, Russia. It is located in the northeast of the republic towards the mouth of the Indigirka River and borders with the East Siberian Sea in the north, Nizhnekolymsky District in the east, Srednekolymsky District in the southeast, Abyysky District in the south, and with Ust-Yansky District in the west. The area of the district is .''Registry of the Administrative-Territorial Divisions of the Sakha Republic'' Its administrative center is the urban locality (an urban-type settlement) of Chokurdakh. As of the 2010 Census, the total population of the district was 3,050, with the population of Chokurdakh accounting for 77.6% of that number. Geography It is located north o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yana-Indigirka Lowland
The Yana-Indigirka Lowland (russian: Яно-Индигирская низменность; sah, Дьааҥы - Индигир намтала) is a large, low alluvial plain located in northern Siberia, Far Eastern Federal District, Russia. Administratively most of the territory of the lowland is part of the Sakha Republic (Yakutia). There are inhabited centers of population in the lowlands such as Chokurdakh, Olenegorsk and Nizhneyansk, but these are very few and scattered. Geography The lowland is named after the Yana River in the west and the Indigirka River in the east and is crossed by both rivers in their middle and lower courses. The area is mostly flat and very marshy, its northern limits extending for over from the Buor Khaya Gulf of the Laptev Sea in the west to the delta of river Indigirka in the East Siberian Sea in the east. It is limited by the Kyundyulyun, the northern end of the Selennyakh Range and the Polousny Range in the south. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permafrost
Permafrost is ground that continuously remains below 0 °C (32 °F) for two or more years, located on land or under the ocean. Most common in the Northern Hemisphere, around 15% of the Northern Hemisphere or 11% of the global surface is underlain by permafrost, with the total area of around 18 million km2. This includes substantial areas of Alaska, Greenland, Canada and Siberia. It can also be located on mountaintops in the Southern Hemisphere and beneath ice-free areas in the Antarctic. Permafrost does not have to be the first layer that is on the ground. It can be from an inch to several miles deep under the Earth's surface. It frequently occurs in ground ice, but it can also be present in non-porous bedrock. Permafrost is formed from ice holding various types of soil, sand, and rock in combination. Permafrost contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide, making tundra soil a carbon sink. As global war ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basins Of The East Siberian Sea
Drainage is the natural or artificial removal of a surface's water and sub-surface water from an area with excess of water. The internal drainage of most agricultural soils is good enough to prevent severe waterlogging (anaerobic conditions that harm root growth), but many soils need artificial drainage to improve production or to manage water supplies. History Early history The Indus Valley civilization had sewerage and drainage systems. All houses in the major cities of Harappa and Mohenjo-daro had access to water and drainage facilities. Waste water was directed to covered gravity sewers, which lined the major streets. 18th and 19th century The invention of hollow-pipe drainage is credited to Sir Hugh Dalrymple, who died in 1753. Current practices Geotextiles New storm water drainage systems incorporate geotextile filters that retain and prevent fine grains of soil from passing into and clogging the drain. Geotextiles are synthetic textile fabrics specially ... [...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] |
Khroma
The Khroma (russian: Хрома) is a river in the Sakha Republic (Yakutia) of the Russian Federation. It is long, and has a drainage basin of . Course The source of the Khroma is at the confluence of the Tamteken and the Nemalak-Arangas, flowing down from the Polousny Range.Хрома / ; in 35 vol.] / Ch. ed. Yu.S. Osipov . - M .: Great Russian Encyclopedia, 2004—2017. It crosses the , part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
