Gavrilovsky District
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Gavrilovsky District
Gavrilovsky District (russian: Гаври́ловский райо́н) is an administrativeLaw #72-Z and municipalLaw #232-Z district (raion), one of the administrative divisions of Tambov Oblast, twenty-three in Tambov Oblast, Russia. It is located in the east of the oblast. The district borders with Pichayevsky District in the north, Belinsky District of Penza Oblast in the east, Kirsanovsky District in the south, and with Bondarsky District in the west. The area of the district is . Its administrative center is the types of inhabited localities in Russia, rural locality (a ''village#Russia, selo'') of Gavrilovka 2-ya. Population: 12,032 (Russian Census (2010), 2010 Census); The population of Gavrilovka 2-ya accounts for 22.2% of the district's total population. Geography Gavrilovsky District is on the east-central side of Tambov Oblast, bordering on Penza Oblast. The district is about 70 km east of the city of Tambov, 50 km southeast of Morshansk, and 15 km nor ...
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Tambov Oblast
Tambov Oblast (russian: Тамбо́вская о́бласть, ''Tambovskaya oblast'') is a federal subject of Russia (an oblast). Its administrative center is the city of Tambov. As of the 2010 Census, its population was 1,091,994. Geography Tambov Oblast is situated in forest steppe. It borders on the Ryazan, Penza, Saratov, Voronezh and Lipetsk Oblasts. History The oldest known population of the Tambov region, the Mordovians-Moksha, formed as a nation of local ethnic groups from the 6th century BC. The first Russian settlers arrived in the pre-Mongol period, but the final settlement occurred in the 17th century. To protect the southern borders of Russia from the raids of the Tatars, and to further develop the Black Soil region, the Russian government built the walled cities of Kozlov (1635) and Tambov (1636). The cities protected the main path of nomad raids on Russian land and paved the way for a quick settlement of the region. Kozlovsky Uyezd originally existed ...
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Tambov
Tambov (, ; rus, Тамбов, p=tɐmˈbof) is a types of inhabited localities in Russia, city and the administrative center of Tambov Oblast, Central Federal District, central Russia, at the confluence of the Tsna River (Moksha basin), Tsna and Studenets Rivers, about south-southeast of Moscow. Population: 280,161 (Russian Census (2010), 2010 Census); 293,658 (Russian Census (2002), 2002 Census); Etymology The name "Tambov" originates from the Moksha language, Mokshan word( mdf, томбале, tombale, the other side, the remote one) Geography Urban layout In terms of its layout, Tambov was no different from other fortified cities - the Kremlin, the prison and a small settlement. The chosen place was in full compliance with the requirements of the fortification. From the north and east, the new fortress was washed by rivers, and from the west and south it was protected by artificial ditches filled with water by the Studenets River. The Kremlin was surrounded by a six-meter w ...
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Zoya Kosmodemyanskaya
Zoya Anatolyevna Kosmodemyanskaya ( rus, Зо́я Анато́льевна Космодемья́нская, p=ˈzojə kəsmədʲɪˈmʲjanskəjə; September 13, 1923 – November 29, 1941) was a Soviet partisan. She was executed after acts of sabotage against the invading armies of Nazi Germany; after stories emerged of her defiance towards her captors, she was posthumously declared a Hero of the Soviet Union.Kazimiera J. Cottam: ''Women in War and Resistance: Selected Biographies of Soviet Women Soldiers'', , page 297 She became one of the most revered heroines of the Soviet Union. Family The Kosmodemyansky family name was constructed by joining the names of Saints Cosmas and Damian ( () and () in Russian). From the 17th century, the Kosmodemyansky were priests in the Russian Orthodox Church. Zoya's grandfather Pyotr Kosmodemyansky was murdered in 1918 by militant atheists for his opposition to blasphemy. Zoya (her name is a Russian form of the Greek name Zoe, which means "l ...
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Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ...
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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 ...
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ...
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Gavrilovka 2-ya, Tambov Oblast
Gavrilovka (russian: Гаври́ловка) is the name of several inhabited localities in Russia. ;Urban localities *Gavrilovka, Dzerzhinsk, Nizhny Novgorod Oblast, a work settlement under the administrative jurisdiction of the city of oblast significance of Dzerzhinsk in Nizhny Novgorod Oblast ;Rural localities * Gavrilovka, Bala-Chetyrmansky Selsoviet, Fyodorovsky District, Republic of Bashkortostan, a '' selo'' in Bala-Chetyrmansky Selsoviet of Fyodorovsky District in the Republic of Bashkortostan * Gavrilovka, Fedorovsky Selsoviet, Fyodorovsky District, Republic of Bashkortostan, a village in Fedorovsky Selsoviet of Fyodorovsky District in the Republic of Bashkortostan * Gavrilovka, Kugarchinsky District, Republic of Bashkortostan, a village in Irtyubyaksky Selsoviet of Kugarchinsky District in the Republic of Bashkortostan * Gavrilovka, Kirovsky District, Kaluga Oblast, a village in Kirovsky District of Kaluga Oblast * Gavrilovka, Tarussky District, Kaluga Oblast, a vill ...
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Volga Uplands
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 th ...
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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", ...
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Don River (Russia)
The Don ( rus, Дон, p=don) is the fifth-longest river in Europe. Flowing from Central Russia to the Sea of Azov in Southern Russia, it is one of Russia's largest rivers and played an important role for traders from the Byzantine Empire. Its basin is between the Dnieper basin to the west, the lower Volga basin immediately to the east, and the Oka basin (tributary of the Volga) to the north. Native to much of the basin were Slavic nomads. The Don rises in the town of Novomoskovsk southeast of Tula (in turn south of Moscow), and flows 1,870 kilometres to the Sea of Azov. The river's upper half ribbles (meanders subtly) south; however, its lower half consists of a great eastern curve, including Voronezh, making its final stretch, an estuary, run west south-west. The main city on the river is Rostov-on-Don. Its main tributary is the Seversky Donets, centred on the mid-eastern end of Ukraine, thus the other country in the overall basin. To the east of a series of thr ...
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Khopyor River
The Khopyor (, also transliterated as Khoper) is a river in European Russia, the biggest left tributary of the river Don.Хопёр
It is long, with a watershed of .«Река Хопер»
Russian State Water Registry
The width is . The Khopyor is navigable up to from the mouth. The maximum discharge is ; the aver ...
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