Kuloy-Pinega Canal
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Kuloy-Pinega Canal
The Kuloy-Pinega Canal (russian: Кулой-Пинежский канал) is a canal connecting the rivers Kuloy and Pinega in Northern Russia at their closest points. The length of the canal is . The canal was constructed in 1928. The canal is located close to the settlement of Pinega in Pinezhsky District, Arkhangelsk Oblast, Russia. The Pinega flows in the north-western direction, and close to the settlement of Pinega sharply turns south-west. Formerly, the Kuloy and the Pinega were one waterway flowing to the Mezen Bay of the White Sea; then the Pinega turned to the Northern Dvina. During a certain period, there was a bifurcation between the Kuloy and the Pinega, when the discharge of the Pinega partially was flowing to the Northern Dvina and partially it was flowing to the Kuloy. Currently, the bifurcation does not exist, and the Pinega is fully discharged into the Northern Dvina. As a trace of the former bifurcation, there is a depression between the Pinega and the Kulo ...
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Pinega (river)
The Pinega (russian: Пинега) is a river in Verkhnetoyemsky, Pinezhsky, and Kholmogorsky Districts of Arkhangelsk Oblast in Russia. It is a right tributary of the Northern Dvina. It is long, and the area of its basin . Its main tributaries are the Ilesha, the Vyya, the Yula, the Pokshenga, and the Yozhuga. The Pinega is the main waterway of the Pinezhsky District, with many of the settlements in the district located on the river banks. The river basin includes the north-western part of the Krasnoborsky District, the eastern part of the Verkhnetoyemsky District, the eastern part of the Vinogradovsky District, the major part of the Pinezhsky District, the eastern part of the Kholmogorsky District, and minor areas in the Leshukonsky District and in the Udorsky District of the Komi Republic. The Pinega flows in the hilly landscape, on the western border of the Timan Ridge, in the coniferous forest (taiga). It freezes up in mid October or early November and stays under the ice ...
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River Bifurcation
River bifurcation (from la, furca, fork) occurs when a river flowing in a single stream separates into two or more separate streams (called distributaries) which then continue downstream. Some rivers form complex networks of distributaries, typically in their deltas. If the streams eventually merge again or empty into the same body of water, then the bifurcation forms a river island. River bifurcation may be temporary or semi-permanent, depending on the strength of the material that is dividing the two distributaries. For example, a mid-stream island of soil or silt in a delta is most likely temporary, due to low material strength. A location where a river divides around a rock fin, e.g. a volcanically formed dike, or a mountain, may be more lasting as a result of higher material strength and resistance to weathering and erosion. A bifurcation may also be man-made, for example when two streams are separated by a long bridge pier. Scientific study of bifurcation River bifurcati ...
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Buildings And Structures In Arkhangelsk Oblast
A building, or edifice, is an enclosed structure with a roof and walls standing more or less permanently in one place, such as a house or factory (although there's also portable buildings). Buildings come in a variety of sizes, shapes, and functions, and have been adapted throughout history for a wide number of factors, from building materials available, to weather conditions, land prices, ground conditions, specific uses, prestige, and aesthetic reasons. To better understand the term ''building'' compare the list of nonbuilding structures. Buildings serve several societal needs – primarily as shelter from weather, security, living space, privacy, to store belongings, and to comfortably live and work. A building as a shelter represents a physical division of the human habitat (a place of comfort and safety) and the ''outside'' (a place that at times may be harsh and harmful). Ever since the first cave paintings, buildings have also become objects or canvasses of much artis ...
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Kuloy River Basin
Kuloy (russian: Кулóй) is an urban locality (a work settlement) in Velsky District of Arkhangelsk Oblast, Russia, located on the Kuloy River, from Arkhangelsk and from Velsk, the administrative center of the district. History The history of the settlement goes back to August 25, 1942, when Kuloy railway station of the North Pechora Railway was opened. The station was necessary to access the work camp building the railway. The railway was built using forced labor by political prisoners, causing many deaths due to low safety and general health of workers. There were four men's and one women's work camp in Kuloy. Work conditions were extremely severe. The workers had to build their own ovens, get warm by standing near cast iron and write letters for their friends and family on pieces of newspapers. They made the ink to write by mixing coal residue with kerosene. In 1944, barracks were built to be used as dormitories for workers. Working on the railway was deemed volun ...
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Northern Dvina Basin
Northern may refer to the following: Geography * North, a point in direction * Northern Europe, the northern part or region of Europe * Northern Highland, a region of Wisconsin, United States * Northern Province, Sri Lanka * Northern Range, a range of hills in Trinidad Schools * Northern Collegiate Institute and Vocational School (NCIVS), a school in Sarnia, Canada * Northern Secondary School, Toronto, Canada * Northern Secondary School (Sturgeon Falls), Ontario, Canada * Northern University (other), various institutions * Northern Guilford High School, a public high school in Greensboro, North Carolina Companies * Arriva Rail North, a former train operating company in northern England * Northern Bank, commercial bank in Northern Ireland * Northern Foods, based in Leeds, England * Northern Pictures, an Australian-based television production company * Northern Rail, a former train operating company in northern England * Northern Railway of Canada, a defunct railway in On ...
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Canals In Russia
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ca ...
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Lock (water Transport)
A lock is a device used for raising and lowering boats, ships and other watercraft between stretches of water of different levels on river and canal waterways. The distinguishing feature of a lock is a fixed chamber in which the water level can be varied; whereas in a caisson lock, a boat lift, or on a canal inclined plane, it is the chamber itself (usually then called a caisson) that rises and falls. Locks are used to make a river more easily navigable, or to allow a canal to cross land that is not level. Later canals used more and larger locks to allow a more direct route to be taken. Pound lock A ''pound lock'' is most commonly used on canals and rivers today. A pound lock has a chamber with gates at both ends that control the level of water in the pound. In contrast, an earlier design with a single gate was known as a flash lock. Pound locks were first used in China during the Song Dynasty (960–1279 AD), having been pioneered by the Song politician and naval en ...
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Sotka River
Sotka ("a hundred" in Slavic languages) may refer to: * MR-UR-100 Sotka Soviet ballistic missile * T-34 medium tank, nicknamed ''sotka'' in Finnish * T-100 "Sotka", a Soviet heavy tank prototype considered while developing the Kliment Voroshilov tank * Sukhoi T-4 The Sukhoi T-4, or "Aircraft 100", or "Project 100", or "Sotka" was a Soviet high-speed reconnaissance, anti-ship and strategic bomber aircraft that did not proceed beyond the prototype stage. It is sometimes called the Su-100. Design and devel ..., a Soviet bomber aircraft * An area (a metric unit of area, one hundredth of a hectare) {{disambig ...
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Northern Dvina
, image = dvina.jpg , image_size = , image_caption = Northern Dvina starts as the confluence of Yug River (on left) and Sukhona River (on top) near Veliky Ustyug (photo 2001) , source1 = Confluence of Yug and Sukhona , source1_location = , mouth_location = Dvina Bay , subdivision_type1 = Country , subdivision_name1 = Russia , length = , source1_elevation = , mouth_elevation = , discharge1_avg = , basin_size = The Northern Dvina (russian: Се́верная Двина́, ; kv, Вы́нва / Výnva) is a river in northern Russia flowing through the Vologda Oblast and Arkhangelsk Oblast into the Dvina Bay of the White Sea. Along with the Pechora River to the east, it drains most of Northwest Russia into the Arctic Ocean. It should not be confused with Western Dvina. The principal tributaries of the Northern Dvina are the Vychegda (right), the Vaga (left), and the Pinega ( ...
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Kuloy (White Sea)
The Kuloy (russian: Кулой) is a river in Pinezhsky and Mezensky Districts of Arkhangelsk Oblast in Russia. Its mouth is located in the Mezen Bay of the White Sea. It is long, and the area of its basin . The principal tributaries of the Kuloy are the Kyolda (left), the Nemnyuga (right), and the Soyana (left). In the upper course, the Kuloy is known as the Sotka; the total length of the Sotka and the Kuloy is . In the low course, the Sotka approaches the middle course of the Pinega and passes within several kilometers from the Pinega. In this place, close to the settlement of Pinega, the Kuloy-Pinega Canal was constructed in 1926—1928, however, currently the canal is pretty much neglected. Below the mouth of the canal the river is known as the Kuloy; above the mouth, the river is known as the Sotka. The lower of the course of Kuloy, downstream from the selo of Kulogory, are navigable; the course adjacent to the canal is not navigable anymore. There is no passenger navi ...
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White Sea
The White Sea (russian: Белое море, ''Béloye móre''; Karelian and fi, Vienanmeri, lit. Dvina Sea; yrk, Сэрако ямʼ, ''Serako yam'') is a southern inlet of the Barents Sea located on the northwest coast of Russia. It is surrounded by Karelia to the west, the Kola Peninsula to the north, and the Kanin Peninsula to the northeast. The whole of the White Sea is under Russian sovereignty and considered to be part of the internal waters of Russia.A. D. Dobrovolskyi and B. S. Zalogi"Seas of USSR. White Sea" Moscow University (1982) (in Russian) Administratively, it is divided between Arkhangelsk and Murmansk oblasts and the Republic of Karelia. The major port of Arkhangelsk is located on the White Sea. For much of Russia's history this was Russia's main centre of international maritime trade, conducted by the Pomors ("seaside settlers") from Kholmogory. In the modern era it became an important Soviet naval and submarine base. The White Sea–Baltic Canal connec ...
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Mezen Bay
The Mezen Bay (russian: Мезенская губа) is located in Arkhangelsk Oblast and Nenets Autonomous Okrug in Northwestern Russia. It is one of four large bays and gulfs of the White Sea, the others being the Dvina Bay, the Onega Bay, and the Kandalaksha Gulf. The Mezen Bay is the easternmost of these, as it lies to the south of the Kanin Peninsula. Morzhovets Island lies at the entrance of the bay. The two main rivers emptying into the Mezen Bay are the Kuloy River, and the Mezen River. The area of the bay is . The Mezen Bay is long and wide. The tides in the Mezen Bay are up to high and are the biggest in the White Sea. The northern part of the bay, just south of Morzhovets Island, is crossed by the Arctic Circle. Historically, the Mezen Bay was the fishing area. The pomors who populated the coast fished along it. A sudden change of the weather could drive them off-shore. In this case, Morzhovets island was the last land before they got driven off to the Barents S ...
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