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Kelimyar
The Kelimyar (russian: Келимяр sah, Кэлимээр, ''Kelimeer'') is a river in Yakutia (Sakha Republic), Russia. It is a tributary of the Olenyok (river), Olenyok with a length of and a drainage basin area of . The river flows north of the Arctic Circle across a desolate area of Bulunsky District devoid of settlements. The nearest inhabited places are Taymylyr, located downstream from its confluence with the Olenyok, and Sklad (Tyumyati), located a little upstream. History In 1875, during his third Siberian expedition, Alexander Chekanovsky intended to "go along the banks of the Lena to the mouth and, if possible, then go to the mouth of the Olenyok (river), Olenyok from the Laptev Sea." From a barge Chekanovsky navigated the Lena River for a distance of about from Yakutsk to the mouth to the Eyekit river, its last major left tributary. He explored inland from the deep and wide lower course of the Eyekit, and then along the rocky and mountainous watershed area ly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chekanovsky Ridge
The Chekanovsky Ridge (russian: Кряж Чекановского; sah, Чекановскай томтороот) is a range of mountains in the Bulunsky District, Yakutia, Russian Federation. The area of the range is uninhabited. The range was named after explorer of Siberia Alexander Chekanovsky (1833–1876). History Rising in a remote and unexplored area, the range was formerly unknown. In 1875, during his third Siberian expedition, Alexander Chekanovsky intended to "go along the banks of the Lena to the mouth and, if possible, then go to the mouth of the Olenyok (river), Olenyok from the Laptev Sea." He hoped to have time to conduct geological exploration of the banks of the Lena River before the onset of winter, but a short summer frustrated his plans. From a barge Chekanovsky navigated the Lena River for a distance of about from Yakutsk to the mouth to the Eyekit river, its last major left tributary. He explored inland from the deep and wide lower course of the Eyekit, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alexander Chekanovsky
Aleksander Piotr Czekanowski, or Aleksandr Lavrentyevich Chekanovsky (russian: Александр Лаврентьевич Чекановский, 24 February 1833 – 30 October 1876) was a Polish geologist and explorer of Siberia during his exile after participating in the January Uprising. He took part in and later led several expeditions, surveying and mapping the geology of Eastern Siberia. He was released from exile in 1875, and in 1876 took up the post of custodian in the Mineralogical Museum of the Academy of Sciences. Biography Aleksander Czekanowski was born on 12 February 1833 in Krzemieniec, Volhynia. His father Wawrzyniec ran a boarding house and was an honorary assistant in a zoological office at a high school. Shortly after the birth of Alexander, his family moved to Kiev. In 1850 Alexander began studying medicine at the Faculty of Medicine in Kiev. While there he also attended lectures on natural science and participated in local field trips during which he develop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taymylyr
Taymylyr (russian: Таймылыр; sah, Таймылыыр, translit=Taymılıır) is a rural locality (a '' selo'') and the administrative center of Tyumetinsky Rural Okrug of Bulunsky District in the Sakha Republic, Russia, located from Tiksi, the administrative center of the district.''Registry of the Administrative-Territorial Divisions of the Sakha Republic'' Its population as of the 2010 Census was 757,Sakha Republic Territorial Branch of the Federal State Statistics Service. Results of the 2010 All-Russian CensusЧисленность населения по районам, городским и сельским населённым пунктам(''Population Counts by Districts, Urban and Rural Inhabited Localities'') down from 900 recorded during the 2002 Census. Geography Taymylyr lies north of the Arctic Circle, on the left bank of the Olenyok River, downstream of its confluence with the Kelimyar. The nearest settlement is Ust-Olenyok located further downriver. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sklad
Sklad or Tyumyati (russian: Тюмяти; sah, Тумат, ''Tumat'') is a rural locality (a '' selo''), the only inhabited locality, and the administrative center of Tumatsky Rural Okrug of Bulunsky District in the Sakha Republic, Russia, located from Tiksi, the administrative center of the district.''Registry of the Administrative-Territorial Divisions of the Sakha Republic'' Its population as of the 2010 Census was 10,Sakha Republic Territorial Branch of the Federal State Statistics Service. Results of the 2010 All-Russian CensusЧисленность населения по районам, городским и сельским населённым пунктам(''Population Counts by Districts, Urban and Rural Inhabited Localities'') up from 9 recorded during the 2002 Census. Geography Sklad lies north of the Arctic Circle, on the left bank of the Olenyok River, upstream of its confluence with the Kelimyar. The nearest settlement is Taymylyr located further down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olenyok (river)
The Olenyok (russian: Оленёк, sometimes spelled ''Оленек'', ''Olenek''; sah, Өлөөн, Ölöön) is a major river in northern Siberian Russia, west of the lower Lena and east of the Anabar. It is long, of which around is navigable. Average water discharge is . The Olenyok is known for its abundance in fish. It is frozen for over eight months every year and the climate in its area is harsh because of the direct influence of the Arctic. History In 1633 Ivan Rebrov reached the Olenyok from the Lena delta and built a fort. In 1642–44 Rebrov and Fedot Alekseyev Popov reached the river but were driven out by the natives. Pioneering Russian Arctic explorer Vasili Pronchishchev and his wife Tatiana (Maria) died of scurvy in the area of the river in September 1736, while mapping the coasts of the Laptev Sea. After their deaths, husband and wife were interred at Ust-Olenyok, near the mouth of the Olenyok. Their tomb was moved after the bodies were exhumed in 1999. In 195 ... [...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] |
Rivers Of The Sakha Republic
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...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] |
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] |
Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Whereve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eyekit
The Eyekit (russian: Эекит, sah, Эйэкит) is a river in the Sakha Republic (Yakutia), Russia. It is a left tributary of the Lena. Its length is from the sources of the Buor Eyekit. The area of its basin including the latter is . The Eyekit flows across the Bulunsky district. The banks of the river are uninhabited. Geography The Eyekit is the last major tributary of the Lena before it ends in the Arctic Ocean. It originates in the southeastern slopes of the Kystyk Plateau, at the northeastern limit of the Central Siberian Plateau as the Buor-Eyekit. In its upper course it flows southeast, then it reaches a floodplain with small lakes and swamps and turns northeast. After being joined by the Tas-Eyekit from the left, it flows roughly eastwards cutting across the southern end of the Chekanovsky Ridge, north of a large bend of the Lena. Finally it meets the left bank of the great river a little north of Kyusyur, upstream of its mouth in the Laptev Sea.Google Earth The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
