|
Polar Ural
The Polar Urals (russian: Полярный Урал) are a mountain range in the western part of the Yamalo-Nenets Autonomous Okrug and the northeastern part of Komi, Russian Federation. The border between Europe and Asia runs along the main ridge of the Polar Urals. Google Earth The Salekhard–Igarka Railway stretch of the Northern Railway runs along the valley of the Sob in the mountains. Geography The Polar Urals are a subrange of the Urals. They stretch roughly from SW to NE for forming the northern section of the long Ural chain. The range runs from the area of the sources of the Khulga river of the Ob basin in the south, to the Konstantinov Kamen mountain rising above Baydaratskaya Bay of the Kara Sea at the northern end. The predominant elevations of the ridges range between and , with individual peaks rising slightly higher. The highest peak is high Payer Mountain, located in the middle part. The mountains display traces of massive ancient glaciation in U-shaped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Russia
Russia (, , ), or the Russian Federation, is a transcontinental country spanning Eastern Europe and Northern Asia. It is the largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across eleven time zones and shares land boundaries with fourteen countries, more than any other country but China. It is the world's ninth-most populous country and Europe's most populous country, with a population of 146 million people. The country's capital and largest city is Moscow, the largest city entirely within Europe. Saint Petersburg is Russia's cultural centre and second-largest city. Other major urban areas include Novosibirsk, Yekaterinburg, Nizhny Novgorod, and Kazan. The East Slavs emerged as a recognisable group in Europe between the 3rd and 8th centuries CE. Kievan Rus' arose as a state in the 9th century, and in 988, it adopted Orthodox Christianity from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Railway (Russia)
The Severnaya Railway (Северная железная дорога; "Northern Railway") is a railway network linking Moscow with Arkhangelsk on the coast of the Arctic Ocean. It runs through Arkhangelsk, Komi, Vologda, Kostroma, Yaroslavl, Ivanovo, and Vladimir regions of the Russian Federation. Northern Railway counts its age from 15 September 1868 when its first part, Shuya-Ivanovo Railway connecting Ivanovo, Shuya and Novki, was opened. The Yaroslavl Railway, owned by Savva Mamontov, was one of the first railways in Russia. The Alexandrov–Yaroslavl–Vologda line was opened in 1872. There are several monuments to Savva Mamontov along the road. The original Moscow–Yaroslavl Mainline is no longer operated from Yaroslavl; it was transferred to the Moscow Railway in 1959. Yaroslavl-Vologda-Arkhangelsk line In 1894, the construction of the railway connecting Vologda with Arkhangelsk started. The decision was taken to construct the line along the shortest route, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pechora
Pechora (russian: Печо́ра; kv, Печӧра, ''Pećöra'') is a town in the Komi Republic, Russia, located on the Pechora River, west of and near the northern Ural Mountains. The area of the town is . Population: History Pechora was granted town status in 1949. Pechora was also the site of a Stalin-era gulag that operated from 1932 to 1953, although it was partially emptied in 1941 as many of the inmates were forced into service in the Red Army. There is a dedicated room at the Pechora museum where they display many of the records and artifacts that were recovered from the gulag. "Pechora" translates to "cave" in Ukrainian Administrative and municipal status Within the framework of administrative divisions, the town of Pechora is, together with two urban-type settlement administrative territories (comprising the urban-type settlements of Kozhva and Puteyets and eleven rural localities) and four rural-type settlement administrative territories (comprising seven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Usa (Pechora)
The Usa (russian: Уса́; kv, Усва, ''Usva'') is a river in the northeast corner of European Russia that drains the Polar Urals southwest into the Pechora. The Polar Urals tend to the northeast and the Usa runs parallel to them. It is in the Komi Republic of Russia and the largest tributary of the Pechora, which it joins from the right. It is long, with a drainage basin of . The Usa has an average discharge of , but this varies from a maximum of in June to a minimum of in April. History The Usa valley has been inhabited for 40,000 years, as evidenced by the archaeological site Mamontovaya Kurya (Russian: Мамонтовой Курьи, "the mammoth curve"). With the Russian conquest of Siberia it became one of the main routes into Siberia. The route ran from the Pechora, which connects to other rivers in northern Russia, up the Usa, across the low Kamen Portage and down the Sob River to Ob River where there were customhouses at the Sob barrier and Obdorsk. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris ( regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines ( till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
U-shaped Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Payer Mountain
Mount Payer (russian: Пайер) is a peak in the Yamalo-Nenets Autonomous Okrug, Russia. It is the highest point of the okrug and of the Polar Urals, as well as one of the highest of the wider Ural mountain system. The name of the mountain originated in the Nenets language ''"pai/er"'' (пай/ер), meaning "rock/master". Description Mount Payer is a high mountain located near the Arctic circle in the Polar Urals, a subrange of the Urals. It rises in the middle part of the range, in Shuryshkarsky District, near the border of the Komi Republic. Google Earth The mountain has three peaks, the highest of which is a high flat-topped rocky summit. The western peak is high, and the eastern . See also * Highest points of Russian Federal subjects * List of mountains and hills of Russia References External linksВосхождение на гору Пайер (1472 м), высшую точку Полярного Урала в рамках туристического прое ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kara Sea
The Kara Sea (russian: Ка́рское мо́ре, ''Karskoye more'') is a marginal sea, separated from the Barents Sea to the west by the Kara Strait and Novaya Zemlya, and from the Laptev Sea to the east by the Severnaya Zemlya archipelago. Ultimately the Kara, Barents and Laptev Seas are all extensions of the Arctic Ocean north of Siberia. The Kara Sea's northern limit is marked geographically by a line running from Cape Kohlsaat in Graham Bell Island, Franz Josef Land, to Cape Molotov (Arctic Cape), the northernmost point of Komsomolets Island in Severnaya Zemlya. The Kara Sea is roughly long and wide with an area of around and a mean depth of . Its main ports are Novy Port and Dikson and it is important as a fishing ground although the sea is ice-bound for all but two months of the year. The Kara Sea contains the East-Prinovozemelsky field (an extension of the West Siberian Oil Basin), containing significant undeveloped petroleum and natural gas. In 2014, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baydaratskaya Bay
Baydaratskaya Bay or Baydarata Bay (russian: Байдарацкая губа, Baydaratskaya guba, Tundra Nenets: Пэдарита, ''Pėdarita'') is a gulf in Russia, located in the southern part of the Kara Sea between the coastline of the Polar Urals, the northern end of the Ural Mountains, and Yamal Peninsula. The length of the gulf is approx. 180 km, mouth width - 78 km, depth - up to 20 m.Google Earth Surface water temperature is 5-6C during summertime. The gulf freezes up during winter. The rivers Baydarata, Yuribey, Kara, and some others flow into the Baydarata Bay. The gulf contains the following larger islands: Torasovey Island, Litke Island, and Levdiyev Island. The Yamal-Center gas pipeline is laid by Gazprom on the seabed The seabed (also known as the seafloor, sea floor, ocean floor, and ocean bottom) is the bottom of the ocean. All floors of the ocean are known as 'seabeds'. The structure of the seabed of the global ocean is governed by plate t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ob (river)
} The Ob ( rus, Обь, p=opʲ: Ob') is a major river in Russia. It is in western Siberia; and together with Irtysh forms the world's seventh-longest river system, at . It forms at the confluence of the Biya and Katun which have their origins in the Altai Mountains. It is the westernmost of the three great Siberian rivers that flow into the Arctic Ocean (the other two being the Yenisei and the Lena). Its flow is north-westward, then northward. The main city on its banks is Novosibirsk, the largest city in Siberia, and the third-largest city in Russia. It is where the Trans-Siberian Railway crosses the river. The Gulf of Ob is the world's longest estuary. Names The internationally known name of the river is based on the Russian name ''Обь'' (''Obʹ'' ). Possibly from Proto-Indo-Iranian '' *Hā́p-'', "river, water" (compare Vedic ''áp-'', Persian ''āb'', Tajik ''ob'', and Pashto ''obə'', "water"). Katz (1990) proposes Komi ''ob'' 'river' as the immediate source of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.JPG "Click for more on -> Moraine")
