Ryazan Region
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Ryazan Region
Ryazan Oblast ( rus, Рязанская область, r=Ryazanskaya oblast, p=rʲɪˈzanskəjə ˈobləsʲtʲ) is a federal subject of Russia (an oblast). Its administrative center is the city of Ryazan, which is the oblast's largest city. Geography Ryazan Oblast borders Vladimir Oblast (N), Nizhny Novgorod Oblast (NE), the Republic of Mordovia (E), Penza Oblast (SE), Tambov Oblast (S), Lipetsk Oblast (SW), Tula Oblast (W), and Moscow Oblast (NW). In terms of physical geography, Ryazan Oblast lies in the central part of the Russian Plain between the Central Russian and Volga uplands. The terrain is flat, with the highest point of no more than 300 m above sea level. Soils are podzolic and boggy on the left bank of the Oka, changing southward to more fertile podzolic and leached black-earths ( chernozyom). Hydrography Most of the Ryazan Oblast lies within the Volga basin, with the Oka the principal river of the area. History Human occupation of the area of the Ryazan Oblast ...
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Coat Of Arms Of Ryazan Oblast
A coat typically is an outer clothing, garment for the upper body as worn by either gender for warmth or fashion. Coats typically have long sleeves and are open down the front and closing by means of Button (clothing), buttons, zippers, Velcro, hook-and-loop fasteners, toggles, a belt (clothing), belt, or a combination of some of these. Other possible features include Collar (clothing), collars, shoulder straps and hood (headgear), hoods. Etymology ''Coat'' is one of the earliest clothing category words in English language, English, attested as far back as the early Middle Ages. (''See also'' Clothing terminology.) The Oxford English Dictionary traces ''coat'' in its modern meaning to c. 1300, when it was written ''cote'' or ''cotte''. The word coat stems from Old French and then Latin ''cottus.'' It originates from the Proto-Indo-European language, Proto-Indo-European word for woolen clothes. An early use of ''coat'' in English is Mail (armour), coat of mail (chainmail), a tu ...
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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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Volga Finns
The Volga Finns (sometimes referred to as Eastern Finns) are a historical group of indigenous peoples of Russia living in the vicinity of the Volga, who speak Uralic languages. Their modern representatives are the Mari people, the Erzya and the Moksha Mordvins, as well as speakers of the extinct Merya, Muromian and Meshchera languages. The Permians are sometimes also grouped as Volga Finns. The modern representatives of Volga Finns live in the basins of the Sura and Moksha rivers, as well as (in smaller numbers) in the interfluve between the Volga and the Belaya rivers. The Mari language has two dialects, the Meadow Mari and the Hill Mari. Traditionally the Mari and the Mordvinic languages ( Erzya and Moksha) were considered to form a ''Volga-Finnic'' or ''Volgaic'' group within the Uralic language family, accepted by linguists like Robert Austerlitz (1968), Aurélien Sauvageot & Karl Heinrich Menges (1973) and Harald Haarmann (1974), but rejected by others like Björn Collin ...
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East Slavs
The East Slavs are the most populous subgroup of the Slavs. They speak the East Slavic languages, and formed the majority of the population of the medieval state Kievan Rus', which they claim as their cultural ancestor.John Channon & Robert Hudson, ''Penguin Historical Atlas of Russia'' (Penguin, 1995), p. 16. Today, the East Slavs consist of Belarusians, Russians, Rusyns, and Ukrainians. History Sources Researchers know relatively little about the Eastern Slavs prior to approximately 859 AD when the first events recorded in the '' Primary Chronicle'' occurred. The Eastern Slavs of these early times apparently lacked a written language. The few known facts come from archaeological digs, foreign travellers' accounts of the Rus' land, and linguistic comparative analyses of Slavic languages. Very few native Rus' documents dating before the 11th century (none before the 10th century) have survived. The earliest major manuscript with information on Rus' history, the '' Prim ...
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Upper Paleolithic
The Upper Paleolithic (or Upper Palaeolithic) is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago (the beginning of the Holocene), according to some theories coinciding with the appearance of behavioral modernity in early modern humans, until the advent of the Neolithic Revolution and agriculture. Anatomically modern humans (i.e. ''Homo sapiens'') are believed to have emerged in Africa around 300,000 years ago, it has been argued by some that their ways of life changed relatively little from that of archaic humans of the Middle Paleolithic, until about 50,000 years ago, when there was a marked increase in the diversity of Artefact (archaeology), artefacts found associated with modern human remains. This period coincides with the most common date assigned to early human migrations, expansion of modern humans from Africa throughout Asia and Eurasia, which contributed to the Neanderthal extinction, ex ...
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Volga Basin
The Volga (; russian: Во́лга, a=Ru-Волга.ogg, p=ˈvoɫɡə) is the longest river in Europe. Situated in Russia, it flows through Central Russia to Southern Russia and into the Caspian Sea. The Volga has a length of , and a catchment area of «Река Волга»
, Russian State Water Registry
which is more than twice the size of . It is also Europe's largest river in terms of average discharge at delta – between and – and of . It is widely regarded as the ...
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Chernozem
Chernozem (from rus, чернозём, p=tɕɪrnɐˈzʲɵm, r=chernozyom; "black ground"), also called black soil, is a black-colored soil containing a high percentage of humus (4% to 16%) and high percentages of phosphorus and ammonia compounds. Chernozem is very fertile soil and can produce high agricultural yields with its high moisture storage capacity. Chernozems are a Reference Soil Group of the World Reference Base for Soil Resources (WRB). Distribution The name comes from the Russian terms for black and soil, earth or land (''chorny'' + ''zemlya''). The soil, rich in organic matter presenting a black color, was first identified by Russian geologist Vasily Dokuchaev in 1883 in the tallgrass steppe or prairie of European Russia. Chernozem cover about 230 million hectares of land. There are two "chernozem belts" in the world. One is the Eurasian steppe which extends from eastern Croatia (Slavonia), along the Danube (northern Serbia, northern Bulgaria ( Danubian Pla ...
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Oka River
The Oka (russian: Ока́, ) is a river in central Russia, the largest right tributary of the Volga. It flows through the regions of Oryol, Tula, Kaluga, Moscow, Ryazan, Vladimir and Nizhny Novgorod and is navigable over a large part of its total length, as far upstream as the town of Kaluga. Its length is and its catchment area is .«Река Ока»
Russian State Water Registry
The Russian capital sits on one of the Oka's tributaries—the Moskva.


Name and history

The Oka river was the homeland of the Eastern Slavic

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 ...
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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 ...
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Russian 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 degree (angle), 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 drainage basin, river basins such as the Dnieper River, Dnepr Basin, the Oka–Don Lowland, and the Volga River, Volga Basin. Along the southernmost point of the East European Plain are the Caucasus Mountains, Caucasus and Crimean Mountains, Crimean mountain ranges. ...
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