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Inya (Sea Of Okhotsk)
The Inya ( rus, Иня) is a river in Okhotsky District, Khabarovsk Krai, Russian Far East. It has a drainage basin of and a length of . The river is a tourist destination for rafting and kayaking. The basin of the Inya is a spawning ground for salmon. Other fish species are also abundant in its waters, as well as crab fisheries near the mouth. Course The Inya river has its source at an elevation of in the Khel-Degi (Хэл-Дэги) lake, part of a lake system of the eastern end of the Suntar-Khayata range. The Inya flows roughly southwards across mountainous terrain with waterfalls and rapids in an area of mountain tundra. The Kheidzhan Range on the left side of its valley separates it from the Taui (Kava) basin in the east. In its last stretch the river expands and fans out in many arms through a widening floodplain parallel to the Ulbeya to the west. Finally it flows into the Sea of Okhotsk by the Novaya Inya settlement. There are no other inhabited places near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Far Eastern Federal District
The Far Eastern Federal District (russian: Дальневосто́чный федера́льный о́круг, ''Dalnevostochny federalny okrug'') is the largest of the federal districts of Russia, eight federal districts of Russia but the least populated, with a population of 8,371,257 (75.5% urban) according to the Russian Census (2010), 2010 Census. The federal district lies entirely within the easternmost part of Asia and is coextensive with the Russian Far East. History The Far Eastern Federal District was established on May 18, 2000, by President of Russia, President Vladimir Putin and is currently being governed by presidential envoy Yury Trutnev. In November 2018, Buryatia and Zabaykalsky Krai were added to the federal district. The seat of the Far Eastern Federal District was moved from Khabarovsk to Vladivostok in December 2018. Demographics Federal subjects Largest cities (with population over 75,000) There are 82 cities in the Far Eastern Federal Di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suntar-Khayata
Suntar-Khayata Range (russian: Сунтар-Хаята, sah, Сунтаар Хайата) is a granite mountain range rising along the border of the Sakha Republic in the north with Amur Oblast and Khabarovsk Krai in the south. The R504 Kolyma Highway passes through the northern part of the range by Kyubeme. Geography The Suntar-Khayata is approximately 450–550 km long and 60 km wide. high Mus-Khaya Mountain, located in the Sakha Republic, is the highest point of the range. Berill Mountain, at is the highest summit in Khabarovsk Krai. Mount Khakandya (Гора Хакандя) is an ultra-prominent peak that is high. The Suntar-Khayata Range is geographically a southeastern prolongation of the Verkhoyansk Range. Until mid 20th century it was treated as a separate range, together with the Skalisty Range, highest point , and the Sette Daban, highest point , to the southwest. The Yudoma-Maya Highlands are located to the south of the range [...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] |
Sette-Daban & Suntar-Khayata ONC D-8
The Sette-Daban (russian: Сетте-Дабан, sah, Сэттэ Дабаан) is a range of mountains in far North-eastern Russia. Administratively the range belongs partly to the Sakha Republic and partly to the Khabarovsk Krai of the Russian Federation. The area of the Sette-Daban is largely uninhabited. The R504 Kolyma Highway passes through the northern part of the range. The climate prevailing in the Sette-Daban is continental and severe. The average air temperature in January is a chilly . The average temperature in the river valleys may reach a maximum of in July. History In 1829, German physicist Georg Adolf Erman during a round-the-world (1828-1830) journey reported the existence of "Seven Ranges" (Sette Daban) between 135° and 140° E in the area of one of the upper tributaries of the Yudoma. The range was surveyed in 1934 by geologist Yuri Bilibin (1901—1952) together with mining engineer Evgeny Bobin (1897—1941) in the course of an expedition sent by the ... [...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] |
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] |
Taui
The Taui ( rus, Тауй), also known as Kava ( rus, Кава) part of its course, is a river in Khabarovsk Krai and Magadan Oblast, Russian Far East. It has a drainage basin of . The river is a spawning ground for salmon and is part of the Magadan Nature Reserve. Its last stretch is navigable. Course The Taui river, as the Kava, is formed at an elevation of at the confluence of rivers Rasava and Lozovaya flowing from the Kheidzhan Range, Upper Kolyma Highlands. The Taui flows first southeastwards and then roughly eastwards along the Kava-Taui Plain (Кава-Тауйская равнина), a wide floodplain. In its last stretch it enters an area of wetlands. Finally it flows into the Amakhton Bay, part of the Taui Bay of the Sea of Okhotsk. Its mouth lies west of the Arman lagoon and just southwest of the mouth of the Yana. Google Earth The river freezes before mid October and stays frozen until mid May. The Kheidzhan Range separates the Taui basin from the Inya ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Tundra
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as ''Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Portions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rapids
Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality. Rapids are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are eas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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