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East European Forest Steppe
The East European forest steppe ecoregion (WWF ID: PA0419) is a patchwork of broadleaf forest stands and grasslands (steppe) that stretches 2,100 km across eastern Europe from the Ural Mountains in Ural, through Povolzhye, Central Russia to the middle of Ukraine.There are also isolated areas of similar character off the western end in eastern Romania, Moldova, and Bulgaria. The region forms a transition zone between the temperate forests to the north, and the steppe to the south. The forest-steppe is an area of Russia in which precipitation and evaporation are approximately equal. The ecoregion is in the Palearctic realm, with a Humid Continental climate. According to one definition of its boundaries, it covers . Location and description The ecoregion forms a long band, about 2,100 km long and 600 km wide, from western edge of Siberia at the Ural Mountains in Ural in the east, through Povolzhye, to Central Russia and Ukraine. Most of the terrain is rolling hills and some plai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kursk Oblast
Kursk Oblast ( rus, Курская область, r=Kurskaya oblast, p=ˈkurskəjə ˈobləsʲtʲ) is a federal subjects of Russia, federal subject of Russia (an oblast). Its administrative center is the types of inhabited localities in Russia, city of Kursk. As of the Russian Census (2010), 2010 Census, Kursk Oblast has a population of 1,127,081. Geography The oblast, with an average elevation of , occupies the southern slopes of the middle-Russian plateau. The surface is hilly and intersected by ravines. The central part of Kursk oblast is more elevated than the Seym Valley to the west. The Timsko-Shchigrinsky ridge contains the highest point in the oblast at above the sea level. The low relief, gentle slopes, and mild winters make the area suitable for farming, and much of the forest has been cleared. Chernozem soils cover around 70% of the oblast's territory; podsol soils cover 26%. ;Borders: ''Internal'': Bryansk Oblast (NW) (border length: ), Oryol Oblast (N, ), Lipetsk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volga Region
The Volga Region (russian: Поволжье, ''Povolzhye'', literally: "along the Volga") is a historical region in Russia that encompasses the drainage basin of the Volga River, the longest river in Europe, in central and southern European Russia. The Volga Region is culturally separated into three sections: * Upper Volga Region - from the Volga River's source (river), source in Tver Oblast to the Mouth (river), mouth of the Oka River in Nizhny Novgorod * Middle Volga Region - from the mouth of the Oka River to the mouth of the Kama River south of Kazan * Lower Volga Region - from the mouth of the Kama River to the Volga Delta in the Caspian Sea, in Astrakhan Oblast The geographic boundaries of the region are vague, and the term "Volga Region" is used to refer primarily to the Middle and Lower sections, which are included in the Volga Federal District and Volga economic region. Geography The Volga Region is almost entirely within the East European Plain, with a notable disti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prunus Stepposa
''Prunus spinosa'', called blackthorn or sloe, is a species of flowering plant in the rose family Rosaceae. The species is native to Europe, western Asia, and regionally in northwest Africa. It is locally naturalized in New Zealand, Tasmania, and the Pacific Northwest and New England regions of the United States. The fruits are used to make sloe gin in Britain and patxaran in Spain. The wood is used to make walking sticks, including the Irish shillelagh. Description ''Prunus spinosa'' is a large deciduous shrub or small tree growing to tall, with blackish bark and dense, stiff, spiny branches. The leaves are oval, long and broad, with a serrated margin. The flowers are about in diameter, with five creamy-white petals; they are produced shortly before the leaves in early spring, and are hermaphroditic, and insect-pollinated. The fruit, called a "sloe", is a drupe in diameter, black with a purple-blue waxy bloom, ripening in autumn and traditionally harvested – at leas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prunus Fruticosa
''Prunus fruticosa'', the European dwarf cherry, dwarf cherry, Mongolian cherry or steppe cherry is a deciduous, xerophytic, winter-hardy, cherry-bearing shrub. It is also called ground cherry and European ground cherry, but is not to be confused with plants in the distinct "Groundcherry" genus of ''Physalis''. ''Prunus fruticosa'' is native to Ciscaucasia, western Siberia, Kazakhstan, Xinjiang China, western Russia, Ukraine, Poland, Czech Republic, Germany, Belarus, Moldova, Bulgaria, Romania, Hungary, Serbia, Austria, and Italy. Description As a shrub ''Prunus fruticosa'' grows high and as wide, in almost any soil, but best in loamy soil, spreading via suckers. Roots are abundant. The plant requires full sun, it is a steppe rather than a forest plant, although it does form thickets at the edges of open forest. The bark is dark brown with yellow lenticels. The leaves are oblanceolate to obovate, about 12 mm by 6 mm, with acuminate apex, glabrous above, thick, ser ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caragana Frutex .
Its native range is Bulgaria to China.
''Caragana frutex'' is a species of flowering plant belonging to the family Fabaceae The Fabaceae or Leguminosae,International Code of Nomenc ... References {{Taxonbar, from=Q1017262 Hedysareae ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Humid continental climates are generally found between latitudes 30° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are rare and isolat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Humid continental climates are generally found between latitudes 30° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are rare and isolat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volga Upland
The Volga Upland, also known as the Volga Uplands, Volga Hills, or Volga Plateau, (Russian: Приволжская возвышенность - Privolzhskaya vozvyshennost) is a vast region of the East European Plain in the European part of Russia that lies west of the Volga River and east of the Central Russian Upland. The uplands lie in the cool continental climate zone, characterised by large fluctuations in seasonal temperatures and generally little rainfall. Outside of the cities in the region, population density is generally between 28 and 129 inhabitants per square mile. Geography The uplands run for approximately in a southwest-northeasterly direction from Volgograd to Kazan. The Tsimlyansk Reservoir lies at the southwestern end of the Volga Upland, with the Kuybyshev Reservoir at the northeastern end. The landscape on the Volga Uplands is hilly, and several rivers have cut into it, such as the Khopyor, Medveditsa and the Sura. The Volga-Don Canal cuts through the l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oka–Don Lowland
The Oka–Don Lowlands (russian: Окско-Донская равнина) (also: Oka–Don Plain), is a flat plain in European Russia, bounded on the north by the Oka River (and the Meshchera Lowlands), on the south by the Don River, on the west by the Central Russian Upland, and on the east by the Volga Upland. The area is part of the larger East European Plain. The terrain is flat, with altitude averaging 160 meters above sea level, and the rivers meander on broad floodplains. Agricultural use of the plain is high, mostly for grain growing – wheat, barley and rye. The plain provides a flat south–north route for transportation, situated between uplands. Until a line of forts was built across the territory by the Russian government in the 1640s (the Belgorod Line), the plain was a route for Tatar invasion from the south. Topography The plain is about 250 km west–east, and 500 km north–south. The central and southern parts are sometimes called the "Tambov plain", ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Russian Upland
The Central Russian Upland (also Central Upland and East European Upland) is an upland area of the East European Plain and is an undulating plateau with an average elevation of . Its highest peak is measured at . The southeastern portion of the upland known as the Kalach Upland. The Central Upland is built of Precambrian deposits of the crystalline Voronezh Massif. Location It spans approximately 180,000 miles² (480,000 km2) in central and southern European Russia northeast of Ukraine, extending from the Oka river to the Donets river. The upland stretches across number of regions in Ukraine and the European portion of Russian Federation. Its north and northwest borders are considered to be Oka River and an imaginary line Kaluga-Ryazan. To the southeast towards the Donets River, the upland changes into the Donets Lowland. To the east its natural border is defined by the Oka–Don Lowland and to the west there is the Dnieper Lowland. Most of the upland lies within the bor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dnieper Lowland
Dnieper Lowland () is a major geographic feature of the Central Ukraine region and the East European Plain. Location It lies along the midstream of Dnieper river mostly on its left bank from Belarus all the way to Dnipropetrovsk Oblast. The lowland is an extended valley of Dnieper with a system of floodplains. To its northwest is located the swampy Polesian Lowland, to the northeast and east is Central Russian Upland, on the right bank of Dnieper rises Dnieper Upland, which with Zaporizhia Ridge is connected with Donets-Azov Plateau. Tectonics Geologically, it is part of the Dnieper-Donets Depression which is rich on deposits of oil, gas, rock salt, and construction materials. Description The Dnieper Lowland is divided into bigger Dnieper Plain and smaller Poltava Plain. Dnieper Plain is located around Kyiv near confluence of Desna and Dnieper, while Poltava Plain is closer to the city of Poltava. External links Dnieper Lowlandat Ukrainian Soviet Encyclopedia The ''Ukraini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
