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Yaroslavl State Pedogogical University
Yaroslavl ( rus, Ярослáвль, p=jɪrɐˈsɫavlʲ) is a city and the administrative center of Yaroslavl Oblast, Russia, located northeast of Moscow. The historic part of the city is a World Heritage Site, and is located at the confluence of the Volga and the Kotorosl rivers. It is part of the Golden Ring, a group of historic cities northeast of Moscow that have played an important role in Russian history. Population: Geography Location The city lies in the eastern portion of Yaroslavl Oblast. The nearest large towns are Tutayev ( to the northwest), Gavrilov-Yam ( to the south), and Nerekhta ( to the southeast). The historic center of Yaroslavl lies to the north of the mouth of the Kotorosl River on the right bank of the larger Volga River. The city's entire urban area covers around and includes a number of territories south of the Kotorosl and on the left bank of the Volga. With nearly 600,000 residents, Yaroslavl is, by population, the largest town on the Volga unt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yaroslav The Wise
Yaroslav the Wise or Yaroslav I Vladimirovich; russian: Ярослав Мудрый, ; uk, Ярослав Мудрий; non, Jarizleifr Valdamarsson; la, Iaroslaus Sapiens () was the Grand Prince of Kiev from 1019 until his death. He was also the Prince of Novgorod on three occasions, uniting the principalities for a time. Yaroslav's baptismal name was George ( orv, Гюрьгi, ) after Saint George. Rise to the throne The early years of Yaroslav's life are mostly unknown. He was one of the numerous sons of Vladimir the Great, presumably his second by Rogneda of Polotsk, although his actual age (as stated in the ''Primary Chronicle'' and corroborated by the examination of his skeleton in the 1930s) would place him among the youngest children of Vladimir. It has been suggested that Family life and children of Vladimir I#Yaroslav's parentage, he was a child begotten out of wedlock after Vladimir's divorce from Rogneda and marriage to Anna Porphyrogenita, or even that he was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tutayev
Tutayev (russian: Тута́ев) is a town in Yaroslavl Oblast, Russia. Population: It has previously been called Romanov-Borisoglebsk, and before that it was two towns separated by the Volga River: Romanov and Borisoglebsk. History Before 1918, it was called Romanov-Borisoglebsk (), and before 1822, when an order of the Tsar united them, there were two separate towns: Romanov (on the left bank of the Volga) and Borisoglebsk (on the right bank). Romanov has existed since the 14th century and Borisoglebsk—since the 15th century. Overview The majority of the population lives on the right bank of the river (the former Borisoglebsk). The areas of town nearest to the Volga's right bank have many old wooden houses and historical buildings (including the Resurrection Cathedral), but further away from the river, Soviet-era apartment buildings predominate. There is no bridge across the Volga in Tutayev, so people have to use a ferry or, alternatively, travel north to Rybinsk or s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Principality Of Yaroslavl
The Principality of Yaroslavl (russian: Ярославское княжество, Yaroslavskoye knyazhestvo) was a List of early East Slavic states, Rus' principality with its capital in the city of Yaroslavl. It existed from 1218 until 1463 (''de jure'' until 1471) when it became part of the Grand Duchy of Moscow. History Foundation The Principality of Yaroslavl separated from the Grand Duchy of Vladimir-Suzdal when the sons of Konstantin of Rostov, Konstantin Vsevolodovich divided his lands upon his death. Vsevolod Konstantinovich inherited the lands around Yaroslavl on both banks of the Volga River with its feeders — the Mologa River, Mologa, the Yukhot', the Ikhra, the Sit River, Sit', the Sheksna River, Sheksna and Lake Kubenskoye. In 1238 the city was sacked by the Mongol invasion of Kievan Rus'. In the Battle of the Sit River on March 4, 1238, Vsevolod Konstantinovich was killed and the Russians defeated. As the result, the Mongol-Tatar Yoke established upon the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thaw (weather)
Thaw is the period when the snow and ice melt, at the end of the winter, in cold climates. January thaw January thaw is a term applied to a thaw or rise in temperature in mid-winter found in mid-latitude North America. Sinusoidal estimates of expected temperatures, for northern locales, usually place the lowest temperatures around January 23 and the highest around July 24, and provide fairly accurate estimates of temperature expectations. Actual average temperatures in North America usually significantly differ twice over the course of the year * Mid-autumn temperatures tend to be warmer than predicted by the sinusoidal model, creating the impression of extended summer warmth known as Indian summer. * For five days around January 25, temperatures are usually significantly warmer than predicted by the sinusoidal estimate, and also warmer than neighboring temperatures on both sides. During this "thaw" period, usually lasting for about a week, temperatures are generally a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2006 European Cold Wave
The 2006 European cold wave was an unusual and deadly cold wave which resulted in abnormal winter conditions over much of Europe. Southern Europe saw cold and snow, while places in northern Norway saw abnormally mild conditions. The phenomenon started in early January 2006, in the region of the Polar Urals, with temperatures nosediving below -50°C, and extended to west Russia, then Central Europe where parts of Poland, Slovakia, and Austria saw temperatures drop below -30 °C. The cold wave resulted in the deaths of up to 50 people in Russia, and a significant death toll in Eastern Europe, including Ukraine, Moldova, and Romania. The abnormal conditions gradually abated towards the end of the month. According to Munich Re reinsurance company, it was the deadliest cold snap between 1980 and 2011, causing 790 fatalities throughout Europe. According to the International Federation of Red Cross and Red Crescent Societies, there were 884 deaths in Ukraine, 135 in Moscow, 13 in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperateness
In geography, the temperate climates of Earth occur in the middle latitudes (23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes. In temperate climates, not only do latitudinal positions influence temperature changes, but sea currents, prevailing wind direction, continentality (how large a landmass is) and altitude also shape temperate climates. The Köppen climate classification defines a climate as "temperate" C, when the mean temperature is above but below in the coldest month to account for the persistency of frost. However, other climate classifications set the minimum at . Zones and climates The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arctic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swampland
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inundat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Coniferous Forest
Temperate coniferous forest is a terrestrial biome defined by the World Wide Fund for Nature. Temperate coniferous forests are found predominantly in areas with warm summers and cool winters, and vary in their kinds of plant life. In some, needleleaf trees dominate, while others are home primarily to broadleaf evergreen trees or a mix of both tree types. A separate habitat type, the tropical coniferous forests, occurs in more tropical climates. Temperate coniferous forests are common in the coastal areas of regions that have mild winters and heavy rainfall, or inland in drier climates or montane areas. Many species of trees inhabit these forests including pine, cedar, fir, and redwood. The understory also contains a wide variety of herbaceous and shrub species. Temperate coniferous forests sustain the highest levels of biomass in any terrestrial ecosystem and are notable for trees of massive proportions in temperate rainforest regions. Structurally, these forests are rather si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Broadleaf And Mixed Forest
Temperate broadleaf and mixed forest is a temperate climate terrestrial habitat type defined by the World Wide Fund for Nature, with broadleaf tree ecoregions, and with conifer and broadleaf tree mixed coniferous forest ecoregions. These forests are richest and most distinctive in central China and eastern North America, with some other globally distinctive ecoregions in the Caucasus, the Himalayas, Southern Europe, Australasia, Southwestern South America and the Russian Far East. Ecology The typical structure of these forests includes four layers. * The uppermost layer is the canopy composed of tall mature trees ranging from high. Below the canopy is the three-layered, shade-tolerant understory that is roughly shorter than the canopy. * The top layer of the understory is the sub-canopy composed of smaller mature trees, saplings, and suppressed juvenile canopy layer trees awaiting an opening in the canopy. * Below the sub-canopy is the shrub layer, composed of low growi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East European Plain
The East European Plain (also called the Russian Plain, "Extending from eastern Poland through the entire European Russia to the Ural Mountaina, the ''East European Plain'' encompasses all of the Baltic states and Belarus, nearly all of Ukraine, and much of the European portion of Russia and reaches north into Finland." ''— Britannica''. or historically the Sarmatic Plain) is a vast interior plain extending east of the North European Plain, and comprising several plateaus stretching roughly from 25 degrees longitude eastward. It includes the westernmost Volhynian-Podolian Upland, the Central Russian Upland, and on the eastern border, encompasses the Volga Upland. The plain includes also a series of major river basins such as the Dnepr Basin, the Oka–Don Lowland, and the Volga Basin. Along the southernmost point of the East European Plain are the Caucasus and Crimean mountain ranges. Together with the North European Plain (covering much of north-western France, Netherlands, Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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