Russia

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Russia, country that stretches over a vast expanse of eastern Europe and northern Asia. Once the preeminent republic of the Union of Soviet Socialist Republics (U.S.S.R.; commonly known as the Soviet Union), Russia became an independent country after the dissolution of the Soviet Union in December 1991. Russia is a land of superlatives. By far the world’s largest country, it covers nearly twice the territory of Canada, the second largest. It extends across the whole of northern Asia and the eastern third of Europe, spanning 11 time zones and incorporating a great range of environments and landforms, from deserts to semiarid steppes to deep forests and Arctic tundra. Russia contains Europe’s longest river, the Volga, and its largest lake, Ladoga. Russia also is home to the world’s deepest lake, Baikal, and the country recorded the world’s lowest temperature outside the North and South poles. Quick Facts Russia See article: flag of Russia Audio File: National anthem of Russia Head Of Government: Prime Minister: Mikhail Mishustin Capital: Moscow Population: (2026 est.) 142,557,000 Currency Exchange Rate: 1 USD equals 80.205 Russian ruble Head Of State: President: Vladimir Putin St. Petersburg 1 of 2 St. PetersburgSt. Petersburg, Russia. Cathedral of the Resurrection of Christ, St. Petersburg, Russia 2 of 2 Cathedral of the Resurrection of Christ, St. Petersburg, RussiaThe Cathedral of the Resurrection of Christ (commonly known as the Church of the Savior on Spilled Blood) is illuminated at night in St. Petersburg, Russia. The inhabitants of Russia are quite diverse. Most are ethnic Russians, but there also are more than 120 other ethnic groups present, speaking many languages and following disparate religious and cultural traditions. Most of the Russian population is concentrated in the European portion of the country, especially in the fertile region surrounding Moscow, the capital. Moscow and St. Petersburg (formerly Leningrad) are the two most important cultural and financial centres in Russia and are among the most picturesque cities in the world. Russians are also populous in Asia, however; beginning in the 17th century, and particularly pronounced throughout much of the 20th century, a steady flow of ethnic Russians and Russian-speaking people moved eastward into Siberia, where cities such as Vladivostok and Irkutsk now flourish. Russia’s climate is extreme, with forbidding winters that have several times famously saved the country from foreign invaders. Although the climate adds a layer of difficulty to daily life, the land is a generous source of crops and materials, including vast reserves of oil, gas, and precious metals. That richness of resources has not translated into an easy life for most of the country’s people, however; indeed, much of Russia’s history has been a grim tale of the very wealthy and powerful few ruling over a great mass of their poor and powerless compatriots. Serfdom endured well into the modern era; the years of Soviet communist rule (1917–91), especially the long dictatorship of Joseph Stalin, saw subjugation of a different and more exacting sort. The Russian republic was established immediately after the Russian Revolution of 1917 and became a union republic in 1922. During the post-World War II era, Russia was a central player in international affairs, locked in a Cold War struggle with the United States. In 1991, following the dissolution of the Soviet Union, Russia joined with several other former Soviet republics to form a loose coalition, the Commonwealth of Independent States (CIS). Although the demise of Soviet-style communism and the subsequent collapse of the Soviet Union brought profound political and economic changes, including the beginnings of the formation of a large middle class, for much of the postcommunist era Russians had to endure a generally weak economy, high inflation, and a complex of social ills that served to lower life expectancy significantly. Despite such profound problems, Russia showed promise of achieving its potential as a world power once again, as if to exemplify a favourite proverb, stated in the 19th century by Austrian statesman Klemens, Fürst (prince) von Metternich: “Russia is never as strong as she appears, and never as weak as she appears.” Russia can boast a long tradition of excellence in every aspect of the arts and sciences. Prerevolutionary Russian society produced the writings and music of such giants of world culture as Anton Chekhov, Aleksandr Pushkin, Leo Tolstoy, Nikolay Gogol, Fyodor Dostoyevsky, and Pyotr Ilyich Tchaikovsky. The 1917 revolution and the changes it brought were reflected in the works of such noted figures as the novelists Maxim Gorky, Boris Pasternak, and Aleksandr Solzhenitsyn and the composers Dmitry Shostakovich and Sergey Prokofiev. And the late Soviet and postcommunist eras witnessed a revival of interest in once-forbidden artists such as the poets Vladimir Mayakovsky and Anna Akhmatova while ushering in new talents such as the novelist Victor Pelevin and the writer and journalist Tatyana Tolstaya, whose celebration of the arrival of winter in St. Petersburg, a beloved event, suggests the resilience and stoutheartedness of her people: Russia is bounded to the north and east by the Arctic and Pacific oceans, and it has small frontages in the northwest on the Baltic Sea at St. Petersburg and at the detached Russian oblast (region) of Kaliningrad (a part of what was once East Prussia annexed in 1945), which also abuts Poland and Lithuania. To the south Russia borders North Korea, China, Mongolia, and Kazakhstan, Azerbaijan, and Georgia. To the southwest and west it borders Ukraine, Belarus, Latvia, and Estonia, as well as Finland and Norway. Extending nearly halfway around the Northern Hemisphere and covering much of eastern and northeastern Europe and all of northern Asia, Russia has a maximum east-west extent of some 5,600 miles (9,000 km) and a north-south width of 1,500 to 2,500 miles (2,500 to 4,000 km). There is an enormous variety of landforms and landscapes, which occur mainly in a series of broad latitudinal belts. Arctic deserts lie in the extreme north, giving way southward to the tundra and then to the forest zones, which cover about half of the country and give it much of its character. South of the forest zone lie the wooded steppe and the steppe, beyond which are small sections of semidesert along the northern shore of the Caspian Sea. Much of Russia lies at latitudes where the winter cold is intense and where evaporation can barely keep pace with the accumulation of moisture, engendering abundant rivers, lakes, and swamps. Permafrost covers some 4 million square miles (10 million square km)—an area seven times larger than the drainage basin of the Volga River, Europe’s longest river—making settlement and road building difficult in vast areas. In the European areas of Russia, the permafrost occurs in the tundra and the forest-tundra zone. In western Siberia permafrost occurs along the Yenisey River, and it covers almost all areas east of the river, except for south Kamchatka province, Sakhalin Island, and Primorsky Kray (the Maritime Region). On the basis of geologic structure and relief, Russia can be divided into two main parts—western and eastern—roughly along the line of the Yenisey River. In the western section, which occupies some two-fifths of Russia’s total area, lowland plains predominate over vast areas broken only by low hills and plateaus. In the eastern section the bulk of the terrain is mountainous, although there are some extensive lowlands. Given these topological factors, Russia may be subdivided into six main relief regions: the Kola-Karelian region, the Russian Plain, the Ural Mountains, the West Siberian Plain, the Central Siberian Plateau, and the mountains of the south and east. Kola-Karelia, the smallest of Russia’s relief regions, lies in the northwestern part of European Russia between the Finnish border and the White Sea. Karelia is a low, ice-scraped plateau with a maximum elevation of 1,896 feet (578 metres), but for the most part it is below 650 feet (200 metres); low ridges and knolls alternate with lake- and marsh-filled hollows. The Kola Peninsula is similar, but the small Khibiny mountain range rises to nearly 4,000 feet (1,200 metres). Mineral-rich ancient rocks lie at or near the surface in many places. Western Russia makes up the largest part of one of the great lowland areas of the world, the Russian Plain (also called the East European Plain), which extends into Russia from the western border eastward for 1,000 miles (1,600 km) to the Ural Mountains and from the Arctic Ocean more than 1,500 miles (2,400 km) to the Caucasus Mountains and the Caspian Sea. About half of this vast area lies at elevations of less than 650 feet (200 metres) above sea level, and the highest point (in the Valdai Hills, northwest of Moscow) reaches only 1,125 feet (343 metres). Nevertheless, the detailed topography is quite varied. North of the latitude on which Moscow lies, features characteristic of lowland glacial deposition predominate, and morainic ridges, of which the most pronounced are the Valdai Hills and the Smolensk Upland, which rises to 1,050 feet (320 metres), stand out above low, poorly drained hollows interspersed with lakes and marshes. South of Moscow there is a west-east alternation of rolling plateaus and extensive plains. In the west the Central Russian Upland, with a maximum elevation of 950 feet (290 metres), separates the lowlands of the upper Dnieper River valley from those of the Oka and Don rivers, beyond which the Volga Hills rise gently to 1,230 feet (375 metres) before descending abruptly to the Volga River. Small river valleys are sharply incised into these uplands, whereas the major rivers cross the lowlands in broad, shallow floodplains. East of the Volga is the large Caspian Depression, parts of which lie more than 90 feet (25 metres) below sea level. The Russian Plain also extends southward through the Azov-Caspian isthmus (in the North Caucasus region) to the foot of the Caucasus Mountains, the crest line of which forms the boundary between Russia and the Transcaucasian states of Georgia and Azerbaijan; just inside this border is Mount Elbrus, which at 18,510 feet (5,642 metres) is the highest point in Russia. The large Kuban and Kuma plains of the North Caucasus are separated by the Stavropol Upland at elevations of 1,000 to 2,000 feet (300 to 600 metres). A belt of low mountains and plateaus 1,150 to 1,500 feet (350 to 460 metres) high flanks the Ural Mountains proper along the eastern edge of the Russian Plain. The north-south spine of the Urals extends about 1,300 miles (2,100 km) from the Arctic coast to the border with Kazakhstan and is extended an additional 600 miles (1,000 km) into the Arctic Ocean by Novaya Zemlya, an archipelago that consists of two large islands and several smaller ones. Although the Urals form the traditional boundary between Europe and Asia, they do not significantly impede movement. The highest peak, Mount Narodnaya, reaches 6,217 feet (1,895 metres), but the system is largely composed of a series of broken, parallel ridges with summits generally between 3,000 and 5,000 feet (900 and 1,500 metres); several low passes cut through the system, particularly in the central section between Perm and Yekaterinburg, which carry the main routes from Europe into Siberia. Many districts contain mineral-rich rocks. Russia’s most extensive region, the West Siberian Plain, is the most striking single relief feature of the country and quite possibly of the world. Covering an area well in excess of 1 million square miles (2.6 million square km)—one-seventh of Russia’s total area—it stretches about 1,200 miles (1,900 km) from the Urals to the Yenisey and 1,500 miles (2,400 km) from the Arctic Ocean to the foothills of the Altai Mountains. Only in the extreme south do elevations exceed 650 feet (200 metres), and more than half the plain lies below 330 feet (100 metres). Vast floodplains and some of the world’s largest swamps are characteristic features, particularly of the plain’s northern half. Slightly higher and drier territory is located south of latitude 55° N, where the bulk of the region’s population is concentrated. Occupying most of the area between the Yenisey and Lena rivers, the Central Siberian Plateau comprises a series of sharply dissected plateau surfaces ranging in elevation from 1,000 to 2,300 feet (300 to 700 metres). Toward its northern edge the Putoran Mountains rise to 5,581 feet (1,701 metres). The plateau’s southern side is bounded by the Eastern Sayan and Baikal (Baikalia) mountains; to the north it descends to the North Siberian Lowland, an eastward extension of the West Siberian Plain. Farther north the Byrranga Mountains reach 3,760 feet (1,146 metres) on the Taymyr (Taimyr) Peninsula, which extends into the Arctic Ocean. On its eastern side the Central Siberian Plateau gives way to the low-lying Central Yakut Lowland. A narrow lowland corridor from the Sea of Okhotsk to the Bering Sea separates these complex fold-mountain systems from the Kamchatka-Kuril region, where the Koryak and Sredinny mountains rise to 8,405 and 11,880 feet (2,562 and 3,621 metres), respectively, forming a northeast-southwest chain that extends along the Pacific-rimmed Kamchatka Peninsula. The peninsula contains numerous volcanic peaks (many of which are still active), including Klyuchevskaya Volcano, which at 15,584 feet (4,750 metres) is the highest point in far-eastern Russia; several other volcanoes rise well above 10,000 feet (3,050 metres). This volcanic zone, part of the great circum-Pacific ring of seismic activity, continues southeastward through the Kuril Islands chain and into Japan. Southeastern Siberia contains many high mountain ranges and extensive lowland plains. The most prominent mountains are the Badzhalsky Mountains, which rise to 8,661 feet (2,640 metres), to the west of the lower Amur, and the Sikhote-Alin, which reach 6,814 feet (2,077 metres), between the Amur-Ussuri lowlands and the Pacific. Sakhalin Island is separated from the Siberian mainland by the Tatar Strait, which is only about 4 miles (6 km) wide at its narrowest point. Some 600 miles (970 km) from north to south but only 25 to 95 miles (40 to 150 km) across, Sakhalin comprises a lowland plain in the north and, in the south, the parallel Eastern and Western Sakhalin mountain ranges, which reach 5,279 and 4,347 feet (1,609 and 1,325 metres), respectively. Drainage Rivers Angara River Angara RiverThe Angara River at Irkutsk, Russia. The vast lowland plains that dominate the Russian landscape carry some of the world’s longest rivers. Five main drainage basins may be distinguished: the Arctic, Pacific, Baltic, Black Sea, and Caspian. Of these basins the most extensive by far is the Arctic, which lies mostly in Siberia but also includes the northern part of the Russian Plain. The greater part of this basin is drained by three gigantic rivers: the Ob (2,268 miles [3,650 km], which with its main tributary, the Irtysh, extends for a continuous 3,362 miles [5,410 km]), the Yenisey (2,540 miles [4,090 km]), and the Lena (2,734 miles [4,400 km]). Their catchments cover a total area in excess of 3 million square miles (8 million square km) in Siberia north of the Stanovoy Range, and their combined discharge into the Arctic averages 1,750,000 cubic feet (50,000 cubic metres) per second. Smaller, but still impressive, rivers make up the remainder of the Arctic drainage: in the European section these include the Northern Dvina (with its tributaries the Vychegda and Sukhona) and the Pechora, and in Siberia the Indigirka and Kolyma. The Siberian rivers provide transport arteries from the interior to the Arctic sea route, although these are blocked by ice for long periods every year. They have extremely gentle gradients—the Ob, for example, falls only 650 feet (200 metres) in more than 1,250 miles (2,010 km)—causing them to meander slowly across immense floodplains. Owing to their northward flow, the upper reaches thaw before the lower parts, and floods occur over vast areas, which lead to the development of huge swamps. The Vasyuganye Swamp at the Ob-Irtysh confluence covers some 19,000 square miles (49,000 square km). The rest of Siberia, some 1.8 million square miles (4.7 million square km), is drained into the Pacific. In the north, where the watershed is close to the coast, numerous small rivers descend abruptly from the mountains, but the bulk of southeastern Siberia is drained by the large Amur system. Over much of its 1,755-mile (2,824-km) length, the Amur forms the boundary that divides Russia and China. The Ussuri, one of the Amur’s tributaries, forms another considerable length of the border. Three drainage basins cover European Russia south of the Arctic basin. The Dnieper, of which only the upper reaches are in Russia, and the 1,162-mile- (1,870-km-) long Don flow south to the Black Sea, and a small northwestern section drains to the Baltic. The longest European river is the Volga. Rising in the Valdai Hills northwest of Moscow, it follows a course of 2,193 miles (3,530 km) to the Caspian Sea. Outranked only by the Siberian rivers, the Volga drains an area of 533,000 square miles (1,380,000 square km). Separated only by short overland portages and supplemented by several canals, the rivers of the Russian Plain have long been important transport arteries; indeed, the Volga system carries two-thirds of all Russian waterway traffic. Lakes Bolshiye Koty on Lake Baikal 1 of 2 Bolshiye Koty on Lake BaikalHarbor of Bolshiye Koty on Lake Baikal, southeastern Siberia. Lake Baikal: The world's deepest and oldest lake2 of 2 Lake Baikal: The world's deepest and oldest lakeOverview of Lake Baikal in Siberia, Russia, the deepest and oldest lake in the world. See all videos for this article Russia contains some two million fresh- and saltwater lakes. In the European section the largest lakes are Ladoga and Onega in the northwest, with surface areas of 6,830 (inclusive of islands) and 3,753 square miles (17,690 and 9,720 square km), respectively; Peipus, with an area of 1,370 square miles (3,550 square km), on the Estonian border; and the Rybinsk Reservoir on the Volga north of Moscow. Narrow lakes 100 to 200 miles (160 to 320 km) long are located behind barrages (dams) on the Don, Volga, and Kama. In Siberia similar artificial lakes are located on the upper Yenisey and its tributary the Angara, where the 340-mile- (550-km-) long Bratsk Reservoir is among the world’s largest. All these are dwarfed by Lake Baikal, the largest body of fresh water in the world. Some 395 miles (636 km) long and with an average width of 30 miles (50 km), Baikal has a surface area of 12,200 square miles (31,500 square km) and a maximum depth of 5,315 feet (1,620 metres). (See Researcher’s Note: Maximum depth of Lake Baikal.) There are innumerable smaller lakes found mainly in the ill-drained low-lying parts of the Russian and West Siberian plains, especially in their more northerly parts. Some of these reach considerable size, notably Beloye (White) Lake and Lakes Top, Vyg, and Ilmen, each occupying more than 400 square miles (1,000 square km) in the European northwest, and Lake Chany (770 square miles [1,990 square km]) in southwestern Siberia. Climate of Russia Several basic factors determine Russia’s variable climates. The country’s vast size and compact shape—the great bulk of the land is more than 250 miles (400 km) from the sea, while certain parts lie as much as 1,500 miles (2,400 km) away—produce a dominance of continental regimes. The country’s northerly latitude ensures that these are cold continental regimes—only southwestern Russia (the North Caucasus region and the lower Don and Volga basins), small sections of southern Siberia, and the maritime region of southeastern Siberia are below latitude 50° N, and more than half the federation is north of latitude 60° N. The great mountain barriers to the south and east prevent the ingress of ameliorating influences from the Indian and Pacific oceans, but the absence of relief barriers on the western and northern sides leaves the country open to Atlantic and Arctic influences. In effect there are only two seasons, winter and summer; spring and autumn are brief periods of rapid change from one extreme to the other. Atmospheric pressure and winds The cooling of the Eurasian landmass in winter leads to the development of an intense high-pressure cell over the country’s interior; mean January pressures range above 1,040 millibars along the southern boundary of Siberia, from which a ridge of high pressure runs westward along Russia’s borders with Kazakhstan and Ukraine. Movement of air outward from these high-pressure zones ensures that winds are mainly from the southwest in European Russia, from the south over much of Siberia, and from the northwest along the Pacific coast. This situation reverses itself in summer, when the landmass heats up; low pressure develops over the Asian interior, and air moves inward—from the northwest in the European section, from the north in Siberia, and from the southeast along the Pacific. Temperature The air movements even out the north-south contrasts in winter temperatures, which might be expected to occur as a result of latitude. Thus, on the Russian Plain isotherms have a north-south trend, and temperatures at each latitude decline from the west toward a cold pole in northeastern Siberia. From west to east within a narrow latitudinal range, the January mean is 18 °F (−8 °C) at St. Petersburg, −17 °F (−27 °C) at Turukhansk in the West Siberian Plain, −46 °F (−43 °C) at Yakutsk, and −58 °F (−50 °C) at Verkhoyansk. Along the Mongolian border the average temperature is only a degree or two above that along the Arctic coast 1,500 miles (2,400 km) farther north. Outblowing winds also depress temperatures along the Pacific coast; Vladivostok, at the same latitude as the French Riviera, has a January mean of 7 °F (−14 °C). In summer, temperatures are more closely connected with latitude; July mean temperatures range from 39 °F (4 °C) in the Arctic islands to 68 °F (20 °C) along the country’s southern border. Extreme temperatures diverge greatly from these means. The world’s lowest minimum January temperature (outside Antarctica) occurred at Oymyakon, southeast of Verkhoyansk, where a temperature of −96 °F (−71 °C) was recorded, while July maxima above 100 °F (38 °C) have occurred at several stations. The net result is a vast seasonal range that increases toward the country’s interior; for example, January and July means differ by 52 °F (29 °C) at Moscow, 76 °F (42 °C) at Turukhansk, and 115 °F (64 °C) at Yakutsk. Extreme winter cold is characteristic of most of Russia; the frost-free period exceeds six months only in the North Caucasus and varies with latitude from five to three months in the European section to three months to less than two in Siberia. Precipitation The main characteristics of precipitation throughout Russia are the modest to low total amounts and the pronounced summer maximum. Across the European plains and western Siberia, total precipitation declines from northwest to southeast. In these regions, except in a few places close to the Baltic, precipitation generally remains below 24 inches (600 mm), falling from 21 inches (533 mm) at Moscow to about 8 inches (203 mm) along the border with Kazakhstan. In eastern Siberia, totals are generally less than 16 inches (406 mm) and as little as 5 inches (127 mm) along the Arctic coast. Precipitation increases again along the Pacific (24 inches [600 mm] in Vladivostok), where the moisture-laden onshore summer monsoon brings significant precipitation. Amounts vary with elevation; the higher parts of the Urals receive more than 28 inches (711 mm), and the mountains of Kamchatka province and the Sikhote-Alin receive well over 40 inches (1,015 mm) annually. Snow is a pronounced feature for the entire country, and its depth and duration have important effects on agriculture. The duration of snow cover varies with both latitude and altitude, ranging from 40 to 200 days across the Russian Plain and from 120 to 250 days in Siberia. Soils and plant and animal life Why is the village of Shoyna sinking in sand? Why is the village of Shoyna sinking in sand?Learn about Shoyna, a former port on the White Sea that is sinking into the sand in Nenets autonomous okrug, Russia. See all videos for this article Climate, soils, vegetation, and animal life are closely interrelated, and variations among these within Russia form a series of broad latitudinal environmental belts that sweep across the country’s plains and plateaus from the western border to the Lena River. In the mountain zones of the south and east, the pattern is more complex because elevation rather than latitude is the dominant factor, and there are striking changes over relatively short distances. Within Russia there are six main environmental belts (some with subdivisions): Arctic desert, tundra, taiga, mixed and deciduous forest, wooded steppe, and steppe. Forests of various kinds account for more than two-fifths of Russia’s total land area. The endangered Siberian tiger inhabiting pockets of forest in the Primorye and Khabarovsk territories of far-eastern Russia has been the focus of intense conservation efforts, both in and outside of the country. Opened passport with visas, stamps, seals, world map. (travel, tourism) Britannica Quiz Guess the Country by Its Neighbors Quiz Arctic desert Arctic desert—confined to the islands of Franz Josef Land, much of the Novaya Zemlya and Severnaya Zemlya archipelagoes, and the New Siberian Islands—is completely barren land with little or no vegetation. Considerable areas are ice-covered. Tundra Nearly one-tenth of Russian territory is tundra, a treeless, marshy plain. Occupying a narrow coastal belt in the extreme north of the European Plain, the tundra widens to a maximum of about 300 miles (500 km) in Siberia. Tundra soils are extremely poor. The moisture surplus caused by low temperatures results in the area’s being poorly drained, and the limited and discontinuous vegetation cover provides little organic matter; moreover, this matter decays slowly, and the soils are highly acidic. Tundra soils are frozen for much of the year, and during the summer thaw drainage is inhibited by the presence of permafrost beneath the thawed surface layer. A typical tundra soil has a shallow surface layer of raw humus, beneath which there is a horizon (soil layer) of gley (sticky, clayey soil) resting on the permafrost. Vegetation changes from north to south, and three subdivisions are recognized: Arctic tundra, with much bare ground and extensive areas of mosses and lichens; shrubby tundra, with mosses, lichens, herbaceous plants, dwarf Arctic birch, and shrub willow; and wooded tundra, with more extensive areas of stunted birch, larch, and spruce. There are considerable stretches of sphagnum bog. Apart from reindeer, which are herded by the indigenous population, the main animal species are the Arctic foxes, musk oxen, beavers, lemmings, snowy owls, and ptarmigan. Taiga birch trees and conifers, West Siberian Plain birch trees and conifers, West Siberian PlainA stand of birch trees and conifers in the taiga of the West Siberian Plain, near Nizhnevartovsk, Russia. South of the tundra lies the vast taiga (boreal forest) zone, the largest of the environmental regions. It occupies the Russian and West Siberian plains north of latitude 56°–58° N together with most of the territory east of the Yenisey River. The western taiga, where the climate is less extreme, is often distinguished from the eastern taiga beyond the Yenisey. In the western section forests of spruce and fir in moister areas alternate with shrubs and grasses interspersed with pine on lighter soils. These species also are present in the east, but the larch becomes dominant there. Only small areas have been cleared for agriculture, mainly in the European part, and the taiga remains the world’s largest timber reserve. However, coniferous forest is not continuous; there are large stands of birch, alder, and willow and, in poorly drained areas, huge stretches of swamp and peat bog. The taiga is rich in fur-bearing animals, such as sables, squirrels, marten, foxes, and ermines, and it is also home to many elks, bears, muskrat, and wolves. Throughout the taiga zone the dominant soil type is the podzol, a product of the intense leaching characteristic of this area of moisture surplus. The forest vegetation provides a surface layer of highly acidic raw humus that decomposes slowly, producing humic acids. Percolating downward, acidic groundwater removes iron and calcium compounds from the upper layers, which, as a result, are pale in colour. Soluble materials are redeposited at lower levels, often resulting in an iron-rich hardpan that impedes the drainage of the upper horizons, which leads to the formation of gley podzols. Applications of lime and fertilizer are required for successful agriculture. Mixed and deciduous forest As conditions become warmer with decreasing latitude, deciduous species appear in greater numbers and eventually become dominant. The triangular mixed and deciduous forest belt is widest along Russia’s western border and narrows toward the Urals. Oak and spruce are the main trees, but there also are growths of ash, aspen, birch, elm, hornbeam, maple, and pine. East of the Urals as far as the Altai Mountains, a narrow belt of birch and aspen woodland separates the taiga from the wooded steppe. Much of the mixed and deciduous forest zone has been cleared for agriculture, particularly in the European section. As a result, the wildlife is less plentiful, but roe deer, wolves, foxes, and squirrels are common. Soils also show a north-south gradation. As the moisture surplus diminishes, leaching becomes less intense, and true podzols give way to gray and brown forest soils, which are less acidic and have a much greater organic content and a higher natural fertility. A second zone of mixed forest occurs in the Amur-Ussuri-Zeya lowlands of southeastern Siberia and includes Asiatic species of oak, hornbeam, elm, and hazel. Wooded steppe and steppe The southward succession is continued by the wooded steppe, which, as its name suggests, is transitional between the forest zone and the steppe proper. Forests of oak and other species (now largely cleared for agriculture) in the European section and birch and aspen across the West Siberian Plain alternate with areas of open grassland that become increasingly extensive toward the south. The wooded steppe eventually gives way to the true steppe, which occupies a belt some 200 miles (320 km) across and extends from southern Ukraine through northern Kazakhstan to the Altai. Russia has a relatively small share of the Eurasian Steppe, mainly in the North Caucasus and lower Volga regions, though pockets of wooded steppe and steppe also occur in basins among the mountains of southern Siberia. The natural steppe vegetation is composed mainly of turf grasses such as bunchgrass, fescue, bluegrass, and agropyron. Perennial grasses, mosses, and lichens also grow on the steppe, and drought-resistant species are common in the south, where the sequence continues in Kazakhstan through dry steppe and semidesert to the great deserts of Central Asia. Woodland is by no means wholly absent, occurring in damper areas in river valleys and depressions. Much of the steppe vegetation, particularly in the west, has been replaced by grain cultivation. The absence of natural shelter on the open steppe has conditioned the kind of animals that inhabit it. Typical rodents of the zone include the marmot and other such burrowing animals and various mouse species. Skunks, foxes, and wolves are common, and antelope inhabit the south. The most common birds are bustards, eagles, kestrels, larks, and gray partridge. Chernozem (black earth) is the distinctive soil of the steppe, taking its name from the very dark upper horizon—often more than three feet (one metre) thick—which is rich in humus derived from the thick grass cover. Winter frost and summer drought inhibit the decomposition of organic matter, and high evaporation rates prevent leaching; as a result, humus accumulates. Calcium compounds are leached downward by the spring snowmelt but are drawn upward in summer and become concentrated in a lime-rich horizon beneath the humus layer. Low acidity and a high humus content combine to give the chernozems a high natural fertility, which has helped make the steppe the country’s main source of grain. People Ethnic groups and languages Although ethnic Russians comprise more than four-fifths of the country’s total population, Russia is a diverse, multiethnic society. More than 120 ethnic groups, many with their own national territories, speaking some 100 languages live within Russia’s borders. Many of these groups are small—in some cases consisting of fewer than a thousand individuals—and, in addition to Russians, only a handful of groups have more than a million members each: the Tatars, Ukrainians, Chuvash, Bashkir, Chechens, and Armenians. The diversity of peoples is reflected in the 21 minority republics, 10 autonomous districts, and autonomous region contained within the Russian Federation. In most of these divisions, the eponymous nationality (which gives its name to the division) is outnumbered by Russians. Since the early 1990s, ethnicity has underlain numerous conflicts (e.g., in Chechnya and Dagestan) within and between these units; many national minorities have demanded more autonomy and, in a few cases, even complete independence. Those parts of Russia that do not form autonomous ethnic units are divided into various territories (kraya) and regions (oblasti), and there are two federal cities (St. Petersburg and Moscow). For more detail on Russian regions, see below Regional and local government. Linguistically, the population of Russia can be divided into the Indo-European group, comprising East Slavic speakers and smaller numbers speaking several other languages; the Altaic group, including Turkic, Manchu-Tungus, and Mongolian; the Uralic group, including Finno-Ugric and Samoyedic; and the Caucasian group, comprising Abkhazo-Adyghian and Nakho-Dagestanian. Because few of the languages of the smaller indigenous minorities are taught in the schools, it is likely that some will disappear. The Indo-European group East Slavs—mainly Russians but including some Ukrainians and Belarusians—constitute more than four-fifths of the total population and are prevalent throughout the country. The Slavs emerged as a recognizable group in eastern Europe between the 3rd and 8th centuries ad, and the first Slav state, Kievan Rus, arose in the 9th century. After the Mongol invasions the centre of gravity shifted to Moscow, and the Russian Empire expanded to the Baltic, Arctic, and Pacific, numerically overwhelming the indigenous peoples. Despite its wide dispersal, the Russian language is homogeneous throughout Russia. Indo-Iranian speakers include the Ossetes of the Caucasus. In addition, there are sizable contingents of German speakers, who mainly populate southwestern Siberia, and Jews (recognized as an ethnolinguistic group rather than a religious one), who live mainly in European Russia; the numbers of both groups have declined through emigration. The Altaic group Turkic speakers dominate the Altaic group. They live mainly in the Central Asian republics, but there is an important cluster of Turkic speakers between the middle Volga and southern Urals, comprising the Bashkir, Chuvash, and Tatars. A second cluster, in the North Caucasus region, includes the Balkar, Karachay, Kumyk, and Nogay. There also are numerous Turkic-speaking groups in southern Siberia between the Urals and Lake Baikal: the Altai, Khakass, Shor, Tofalar, and Tyvans (Tuvans; they inhabit the area once known as Tannu Tuva, which was annexed by the Soviet Union in 1944). The Sakha (Yakut) live mainly in the middle Lena basin, and the Dolgan are concentrated in the Arctic. Manchu-Tungus languages are spoken by the Evenk, Even, and other small groups that are widely dispersed throughout eastern Siberia. The Buryat, who live in the Lake Baikal region, and the Kalmyk, who live primarily to the west of the lower Volga, speak Mongolian tongues. The Uralic group The Uralic group, which is widely disseminated in the Eurasian forest and tundra zones, has complex origins. Finnic peoples inhabit the European section: the Mordvin, Mari (formerly Cheremis), Udmurt (Votyak) and Komi (Zyryan), and the closely related Komi-Permyaks live around the upper Volga and in the Urals, while Karelians, Finns, and Veps inhabit the northwest. The Mansi (Vogul) and Khanty (Ostyak) are spread thinly over the lower Ob basin (see Khanty and Mansi). The Samoyedic group also has few members dispersed over a vast area: the Nenets in the tundra and forest tundra from the Kola Peninsula to the Yenisey, the Selkup around the middle Ob, and the Nganasan mainly in the Taymyr Peninsula. The Caucasian group There are numerous small groups of Caucasian speakers in the North Caucasus region of Russia. Abaza, Adyghian, and Kabardian (Circassian) are similar languages but differ sharply from the languages of the Nakh group (Chechen and Ingush) and of the Dagestanian group (Avar, Lezgian, Dargin, Lak, Tabasaran, and a dozen more). Other groups Several Paleo-Siberian groups that share a common mode of life but differ linguistically are located in far eastern Siberia. The Chukchi, Koryak, and Itelmen (Kamchadal) belong to a group known as Luorawetlan, which is distinct from the Eskimo-Aleut group. The languages of the Nivkh (Gilyak) along the lower Amur and on Sakhalin Island, of the Yukaghir of the Kolyma Lowland, and of the Ket of the middle Yenisey are completely isolated, though it is likely that Yukaghir is a relative of the Uralic languages. Religion of Russia Cathedral of St. Basil the Blessed Cathedral of St. Basil the BlessedCathedral of St. Basil the Blessed, Moscow, Russia. Although ethnic differences in Russia have long contained a religious element, the position of religious organizations and of their individual adherents has varied with political circumstances. In the 10th century Prince Vladimir I, who was converted by missionaries from Byzantium, adopted Christianity as the official religion for Russia, and for nearly 1,000 years thereafter the Russian Orthodox church was the country’s dominant religious institution. After the communists took power in 1917, religious institutions suffered. The church was forced to forfeit most of its property, and many monks were evicted from their monasteries. The constitution of the former Soviet Union nominally guaranteed religious freedom, but religious activities were greatly constrained, and membership in religious organizations was considered incompatible with membership in the Communist Party. Thus, open profession of religious belief was a hindrance to individual advancement. More-open expression of Christian beliefs was permitted during World War II, when the government sought the support of Christians and Jews in the fight against fascism, but restrictions were reimposed when the war ended. In the 1980s, under the reformist regime of Mikhail Gorbachev, a policy of glasnost (“openness”) was declared, allowing greater toleration for the open practice of religion. The subsequent dissolution of the Soviet Union made religious freedom a reality and revealed that large sections of the population had continued to practice a variety of faiths. Indeed, Russian nationalists who emerged beginning in the 1990s identified the Russian Orthodox church as a major element of Russian culture. Trinity–St. Sergius monastery Trinity–St. Sergius monasteryChurch officials being greeted outside the Trinity–St. Sergius monastery, the centre of Russian Orthodoxy, in Sergiyev Posad, Russia, north of Moscow. Today Russian Orthodoxy is the country’s largest religious denomination, representing more than half of all adherents. Organized religion was repressed by Soviet authorities for most of the 20th century, and the nonreligious still constitute more than one-fourth of the population. Other Christian denominations are much smaller and include the Old Believers, who separated from the Russian Orthodox church in the 17th century, and Baptist and Evangelical groups, which grew somewhat in membership during the 20th century. Catholics, both Western rite (Roman) and Eastern rite (Uniate), and Lutherans were numerous in the former Soviet Union but lived mainly outside present-day Russia, where there are few adherents. Muslims constitute Russia’s second largest religious group. In 1997 legislation was enacted that constrained denominations outside five “traditional” religions—Russian Orthodoxy, several other Christian denominations, Islam, Judaism, and Buddhism—restricting the activities of groups not registered in the country for at least 15 years. For example, groups not meeting this requirement at the time the law was implemented (such as Roman Catholics and Mormons) were unable to operate educational institutions or disseminate religious literature. monks praying at the Ivolginsky Datsan temple monks praying at the Ivolginsky Datsan templeA Buddhist monk beating a drum as other monks pray in the Ivolginsky Datsan temple, Buryatia republic, eastern Siberia, Russia. Although there is some degree of correlation between language and religion, the two do not correspond entirely. Slavs are overwhelmingly Orthodox Christian. Turkic speakers are predominantly Muslim, although several Turkic groups in Russia are not. For example, Christianity predominates among the Chuvash, Buddhism prevails among large numbers of Altai, Khakass, and Tyvans, and many Turkic speakers east of the Yenisey have retained their shamanistic beliefs (though some have converted to Christianity). Buddhism is common among the Mongolian-speaking Buryat and Kalmyk. Jews long suffered discrimination in Russia, including purges in the 19th century, repression under the regime of Joseph Stalin, and Nazi atrocities on Russian soil during World War II. Beginning with Gorbachev’s reformist policies in the 1980s, Jewish emigration to Israel and elsewhere was permitted on an increasing scale, and the number of Jews living in Russia (and all parts of the former Soviet Union) has decreased. Prior to the breakup of the Soviet Union, about one-third of its Jewish population lived in Russia (though many did not practice Judaism), and now about one-tenth of all Jews in Russia reside in Moscow. In the 1930s Stalin established the Jewish Autonomous Region in the Soviet Far East as a Jewish province, though by the early 21st century only about 5 percent of the province’s population was Jewish. Settlement patterns Beginning in the 1890s and continuing throughout the next century, many people in Russia migrated from the European portion of the country to Siberia, which constitutes three-fourths of the country’s territory but contains only about one-fifth of its population. Some four-fifths of the country’s population live in the main settled belt of European Russia, extending between St. Petersburg (northwestern Russia), Kemerovo (Siberia), Orsk (southern Urals), and Krasnodar (northern Caucasus). Population densities in the rural areas in this section range from 25 to 250 persons per square mile, with the higher concentrations occurring in the wooded steppe. In the cities, particularly Moscow, population densities are comparable to other European cities. East of the Urals, across the southern part of the West Siberian Plain, rural densities are considerably lower, rarely exceeding 65 persons per square mile. Beyond the Yenisey the settled zone breaks up into a series of pockets in the extreme south, along the line of the Trans-Siberian Railroad, of which the largest is that in the Amur-Ussuri-Zeya lowlands of southeastern Siberia. In the second half of the 20th century, rural depopulation was a pronounced characteristic, occurring faster in the European section. In the last decades of the 20th century, the rural population fell by some one-fourth in the European section, though it grew in what is now the Southern federal district. Because migration out of rural areas was particularly prevalent among the young, many rural areas are now inhabited primarily by the elderly. The bulk of the rural population lives in large villages associated with the collective and state farms (kolkhozy and sovkhozy, respectively) established by the former Soviet regime. These farms have carried on the long-established Russian tradition of communal farming from nucleated settlements. Individual farms started to reappear in the post-Soviet years. By 1995 there were nearly 300,000 private farms, though in the next decade the numbers stagnated or declined. Private farms, however, still produce a tiny fraction of agricultural output. Vast stretches of thinly settled and empty territories lie north of the main settled belt. Sakha (Yakutia)—a minority republic that, with an area of about 1.2 million square miles (3.1 million square km) and about one million inhabitants, has a density of less than one person per square mile—is typical of this zone. Since the mid-19th century, industrialization and economic development have led to a substantial increase in urbanization. Nearly three-fourths of Russia’s population live in what are classified as urban areas. Moscow, the largest metropolis, has twice the population of its nearest rival, St. Petersburg, which in turn dwarfs the size of Russia’s other major cities, such as Chelyabinsk, Kazan, Nizhny Novgorod (formerly Gorky), Novosibirsk, Omsk, Perm, Rostov-na-Donu, Samara (formerly Kuybyshev), Ufa, and Yekaterinburg (formerly Sverdlovsk). Several major urban concentrations have developed in the main industrial regions. St. Petersburg (the tsarist capital) stands alone as the northernmost metropolis, whereas Moscow and Nizhny Novgorod are part of the large urbanized central industrial region, which has a score of large cities, numerous smaller towns, and an urban population that constitutes about one-fifth of Russia’s total. In the Ural Mountains region, the towns are more widely spaced and include numerous small mining and industrial centres as well as a number of towns with more than 250,000 inhabitants, which altogether amount to an urban population about half that of the Moscow region. The only slightly less-populous Volga region has towns strung out along the riverbanks, with a particularly dense concentration in the vicinity of Samara. European Russia also includes a portion of the Donets Basin (Donbass) industrial zone, arbitrarily split by the Russia-Ukraine boundary; this area’s largest city is Rostov-na-Donu, but there are numerous smaller centres. Khabarovsk KhabarovskStreet scene in Khabarovsk, a major transportation hub in the Russian Far East. The main urban concentration east of the Urals is in the Kuznetsk Basin (Kuzbass), which is a centre for mining and industry. Major cities also occur at widely separated points along the length of the Trans-Siberian Railroad, including, from west to east, Omsk, Novosibirsk, Krasnoyarsk, Irkutsk, Ulan-Ude, Chita, Khabarovsk, and Vladivostok. A few very isolated cities are located in the far north, notably the ports of Murmansk and Arkhangelsk and mining centres such as Vorkuta and Norilsk. Resort towns are a feature of the North Caucasus region, including Sochi (on the Black Sea), Pyatigorsk, and Mineralnye Vody. Elsewhere, the capitals of provinces and other administrative divisions are the main towns, having grown to considerable size as the organizing centres for their territories. Demographic trends During the 1990s Russia began experiencing a negative population growth rate. Primary reasons for this was a decline in the fertility rate (particularly of ethnic Russians) similar to that in Japan and in many western European countries. There was also a steep drop in life expectancy beginning in the early 1990s, a result of inadequacies in the health-care system and poor nutrition; high smoking and alcoholism rates and environmental pollution were also considered contributing factors. Declines in life expectancy were more pronounced among men and resulted in a growing gap between the number of men and women in the country. Higher rates of natural increase (population growth resulting from more births than deaths) continue among some minority groups, particularly those of Islamic background. Until the 1990s migration from the European sector to Siberia was the primary cause of regional variations in population growth rates. For example, in the 1980s, when Russia’s population increased by about 7 percent, growth exceeded 15 percent in much of Siberia but was less than 2 percent in parts of western Russia. During the 1990s, however, eastern Siberia (at least according to official statistics) suffered a dramatic population decline, a result of substantial outmigrations caused by the phaseout of heavy government subsidies, upon which it was heavily dependent. The long-declining Russian birth rate has led to a progressive aging of the population. In the early 21st century, for example, roughly one-sixth of the population of Russia was below age 15, while the proportion of those age 60 and above topped one-fifth. The proportion of children was generally higher, and that of the elderly lower, among the non-Russian ethnic groups, which have maintained a somewhat higher birth rate. An aging population and the drop in fertility rates led many demographers to foresee a long-term labour shortage. Economy of Russia The Russian republic, by virtue of its great size and abundant natural resources, played a leading role in the economy of the Soviet Union. In the first decades of the Soviet regime, these resources made possible great economic advances, including the rapid development of mining, metallurgy, and heavy engineering, the expansion of the railway network, and a massive increase in the energy supply. In the 1960s a second phase of Soviet industrial development began to exert a particularly strong effect on the Russian republic. In addition to further growth in established industries—especially in the production of oil, gas, and electricity and in the chemical industries—there was a marked diversification in industrial output, including a limited expansion in consumer goods. In the years before the dissolution of the Soviet Union, however, the economy of Russia and of the entire country was in a state of decline, and official statistics masked industrial inefficiencies. After the collapse of the Soviet Union in 1991, the Russian government implemented a series of radical reforms designed to transform the economy from one that was centrally planned and controlled to one based on capitalist principles. Major components of the reforms included establishing privately owned industrial and commercial ventures (using both foreign and Russian investment) and privatizing state-owned enterprises. To encourage privatization, the government issued vouchers to Russian citizens that enabled them to purchase of shares in privatized firms, though in practice these vouchers frequently were sold for cash and were accumulated by entrepreneurs. A commodity- and stock-exchange system also was established. The privatization process was slow, however, and many firms—particularly in the heavy industries—remained under state ownership. In addition, there was significant debate regarding the buying and selling of land. In 2001 the government legalized the sale of land, though it did so only for urban housing and industrial real estate—which together accounted for only a small fraction of Russia’s total area. At the beginning of the 21st century, similar legislation was also under discussion for rural and agricultural areas. Though full private ownership of land is provided for in the 1993 constitution, the practice has not yet been implemented. As a result of delays in implementing structural reforms, the conversion to market-based agriculture was slow, as many clung to the old, familiar collective system. The reforms beginning in the 1990s caused considerable hardships for the average Russian citizen; in the decade after the dissolution of the Soviet Union, the Russian economy contracted by more than two-fifths. The monetary system was in disarray: the removal of price controls caused a huge escalation in inflation and prices; the value of the ruble, the country’s currency, plummeted; and real incomes fell dramatically. Conditions began to improve by the mid-1990s, but the recovery was interrupted in 1998 by a severe financial crisis, which caused the government to sharply devalue the ruble. Numerous banks became insolvent, and millions of citizens lost their life savings. Gradually, corrective measures were implemented. For example, the licensing of private banks became more rigorous, and the government cracked down on tax evasion, which had been rampant since the implementation of economic reforms. To accommodate business growth, taxes on medium and small enterprises were moderated, and the government began to offer incentives for reinvesting profits into the domestic economy. By the early 21st century, the measures had begun to have a positive effect on the Russian economy, which showed signs of recovery and stable growth. Steady earnings from oil exports permitted investments in factories, and the devalued currency made Russian goods more competitive on the international market. In the post-Soviet years, foreign direct investment was encouraged, but it was constrained by unfavourable conditions, including state intervention in industry, corruption, and weakness in the rule of law. An upsurge in violence by organized crime syndicates contributed to hampering Western investment, and though the activity of such groups was curtailed in the early 21st century, it still presented severe obstacles to both Western and Russian businesses. Investment by non-Russian companies was also discouraged by moves taken by the Russian government to increase state ownership in various industries, including oil and gas, aviation, and automobile manufacturing. In addition to the difficulties the country encountered in its effort to restructure the economy, Russia had been subjected to serious long-term environmental degradation during the Soviet period, the full extent of which became apparent only in the 1990s. The most visible aspects of this situation—such as the Chernobyl accident at a nuclear power plant in Ukraine in 1986, widespread industrial pollution, and the drastic reduction in the volume of the Aral Sea as a result of inflow diversions—were only symptomatic of decades of wasteful resource exploitation. These environmental concerns placed another burden on Russia’s already overwhelmed economic structure. The economic foundation of the country itself remained similar to that which had been developed during the Soviet period. For purposes of description it is convenient to refer to the official set of 11 traditional economic regions into which Russia is divided (though the federal districts created in 2000 have begun to replace the traditional economic regions for statistical purposes). In Europe the regions are the North, Northwest, Central, Volga-Vyatka, Central Black Earth, North Caucasus, Volga, and Ural, and in Asia they are West Siberia, East Siberia, and the Far East. Agriculture, forestry, and fishing Agriculture The harshness of the Russian environment is reflected in the small proportion of land that is used for farming. Agricultural land constitutes less than one-sixth of the country’s territory, and less than one-tenth of the total land area is arable. About three-fifths of Russian farmland is used to grow crops; the remainder is devoted to pasture and meadow. Overall, agriculture contributes little more than 5 percent to Russia’s gross domestic product (GDP), though the sector employs about one-eighth of the total labour force. The main product of Russian farming has always been grain, which occupies considerably more than half of the cropland. Wheat is the chief cereal, followed by barley, rye, and oats. More than one-third of the sown area is devoted to fodder crops—sown grasses, clovers, root crops, and, in the southern districts, corn (maize). The remaining farmland is devoted to industrial crops, such as sunflowers, sugar beets, and flax, and to potatoes and other vegetables. Variations in relief, soil, and climate produce pronounced regional variations in agriculture. In European Russia the proportion of land devoted to crops increases southward, from virtually none in the North region to about two-thirds in the Central Black Earth region. In West and East Siberia and the Far East, crops are largely confined to the southern fringe. Even in West Siberia, where the cultivated zone is at its widest, crops occupy less than one-tenth of the region’s territory, and the proportion falls to negligible levels in East Siberia and the Far East. Cereals occupy more than two-thirds of the cropland in most regions but less than half in the damper Northwest and Central regions, where fodder crops and livestock are more important. The intensity of farming and the yields achieved are generally much higher in the European section than in Siberia. The same is also the case for livestock farming. In general, the old collective farms and state farms have continued to function in post-Soviet Russia, though they have often been renamed as cooperatives or labour-management firms. Privatized farms have experienced significant obstacles, because many in the agricultural sector treated them as pariahs, and the land that many were allocated was unproductive or inaccessible. Thus, the bulk of the grain continues to be produced by very large agricultural enterprises, particularly those in the Northern Caucasus and in the Volga economic regions. Forestry Russia contains the world’s largest forest reserves, and its lumbering, pulp, paper, and woodworking industries are particularly important. More than two-fifths of Russia is forested, and the country has more than one-fifth of the world’s total forests—an area nearly as large as the continental United States. However, Russian forests have very slow rates of growth because of the cold, continental climate, and the country has lost about one-third of its estimated original forest area. Legislation was implemented in the late 1990s to moderate further deforestation. Nevertheless, logging continued to endanger the last intact forest landscapes of northern European Russia. Similar risks have also spread to areas east of the Urals. The forestry industry employs some one million people. Coniferous species are predominant; Russia produces about one-fifth of the world’s softwood. The country is among the world leaders in the production of many other wood-related products, and timber, saw lumber, pulp, paper, cardboard, and roundwood contribute to Russia’s export income. Fishing sturgeon fishing sturgeon fishingFishing for beluga sturgeon in the Volga River, Volgograd, Russia. The fishing industry plays a significant role in the Russian economy. With access to the substantial resources of both the Atlantic and Pacific oceans, marine fishing is particularly well developed, and Russia’s fleet of factory ships can process huge catches at remote locations. The chief European ocean-fishing ports are Kaliningrad and St. Petersburg on the Baltic Sea and Murmansk and Arkhangelsk in the far north. Russia’s chief Pacific port is Vladivostok, but there are several others, particularly in Sakhalin and Kamchatka provinces. Smaller-scale fishing takes place in the Sea of Azov and the Black and Caspian seas (the Caspian sturgeon is the source of the world’s finest caviar), but reduced river flows and pollution from agricultural runoff, industrial waste, and sewage dumping have thinned fish populations. There are important inland fisheries on lakes and rivers, including a good deal of fish farming. The Russian fishing industry rivals the size of the world’s other leading producers (Japan, the United States, and China). Russia produces about one-third of all canned fish and some one-fourth of the world’s total fresh and frozen fish. The privatization of fishing in the 1990s shifted the industry’s focus from production for domestic consumption to exports. Especially important catches are pollack, herring, cod, and salmon. Russia’s earnings from the export of fish are steadily larger than from grain export. Salmon, crabmeat, caviar, beluga, sterlet, and herring were among the important seafoods generating export income. Resources and power natural gas facility natural gas facilityNatural gas facility near Kursk, Russia. Russia has enormous energy resources and significant deposits of many different minerals. Most, if not all, of the raw materials required by modern industry are found within its borders. Its coal reserves are particularly extensive. The biggest fields lie in the remote Tunguska and Lena basins of East Siberia and the Far East, but these are largely untapped, and the bulk of output comes from more southerly fields along the Trans-Siberian Railroad. About three-fourths of Russia’s coal is produced in Siberia—some two-fifths from the Kuznetsk Basin alone and the remainder from the Kansk-Achinsk, Cheremkhovo, and South Yakut basins and numerous smaller sources. The production of hard (anthracite) coal in European Russia takes place mainly in the eastern Donets Basin and, in the Arctic, in the Pechora Basin around Vorkuta. Privatization of the coal industry began in the 1990s, and by the early 21st century some three-fifths of overall coal production was coming from privatized mines. However, the removal of state subsidies also forced the closure of many unprofitable mines. The most severe cuts in coal output occurred in the Central and Ural economic regions and in Rostov province of the North Caucasus region. Coal mines in regions with access to large reserves of oil and natural gas fared better. Siberia, Russia: oil well 1 of 2 Siberia, Russia: oil wellCrude oil is pumped from a well in western Siberia, Russia. gas pipelines from Russia to Europe 2 of 2 gas pipelines from Russia to EuropeMajor gas pipelines from Russia to Europe. Russia is among the world’s leading producers of oil, extracting about one-fifth of the global total. It also is responsible for more than one-fourth of the world’s total natural gas output. The great bulk of oil and natural gas comes from the huge fields that underlie the northern part of the West Siberia region. Another significant source of reserves is the Volga-Ural zone, and the remainder is derived mainly from the Komi-Ukhta field (North region); the North Caucasus region, once the Soviet Union’s leading producer, is now of little importance. Extensive pipeline systems link production sites to all regions of the country, the neighbouring former Soviet republics, and, across the western frontier, numerous European countries. There are some 600 large thermal power plants, more than 100 hydroelectric stations, and several nuclear power plants that generate electricity. About three-fourths of electricity is generated in thermal stations; some two-thirds of thermal generation is from oil and gas. The remaining power output is produced by hydroelectric and nuclear plants. Most of the hydroelectricity comes from huge stations on the Volga, Kama, Ob, Yenisey, Angara, and Zeya rivers. Nuclear power production expanded rapidly before development was checked by the Chernobyl accident in Ukraine in 1986. Much of Siberia’s electricity output is transmitted to the European region along high-voltage lines. Russia also produces large quantities of iron ore, mainly from the Kursk Magnetic Anomaly (Central Black Earth region), Kola Peninsula, Urals, and Siberia. Although there is steel production in every economic region, the largest steel-producing plants are located mainly in the Urals, Central Black Earth region, and Kuznetsk Basin. Russia produces about one-sixth of the world’s iron ore and between one-tenth and one-fifth of all nonferrous, rare, and precious metals. Nonferrous metals are available in great variety from many districts, but by far the most important are those of the Ural region, which is Russia’s main centre of nonferrous metallurgy. Russia is a major producer of cobalt, chrome, copper, gold, lead, manganese, nickel, platinum, tungsten, vanadium, and zinc. The country produces much of its aluminum from plants powered by the Siberian hydroelectric stations, but bauxite deposits are relatively meagre. Manufacturing of Russia Machine building Russia’s machine-building industry provides most of the country’s needs, including steam boilers and turbines, electric generators, grain combines, automobiles, and electric locomotives, and it fills much of its demand for shipbuilding, electric-power-generating and transmitting equipment, consumer durables, machine tools, instruments, and automation components. Russia’s factories also produce armaments, including tanks, jet fighters, and rockets, which are sold to many countries and contribute significantly to Russia’s export income. Older automobile factories are located in Moscow and Nizhny Novgorod; the largest plants are those at Tolyatti (near Samara) and at Naberezhnye Chelny (in Tatarstan; a heavy truck factory). Smaller producers of road vehicles are in Miass, Ulyanovsk, and Izhevsk. Chemicals Because of the complex history of the development of the chemical industries and the great variety of raw materials involved, chemical manufacture is widely dispersed. The industry initially utilized mineral salts, coke-oven and smelter gases, timber, and foodstuffs (mainly potatoes) as their raw materials. On this basis synthetic-rubber factories were built in the Central Black Earth and Central regions, areas of large-scale potato production; sulfuric acid plants were developed in the Urals and North Caucasus, where there was nonferrous metallurgy; and potassium and phosphatic fertilizer plants were constructed at sites in several regions, near deposits of potassium salts and phosphorites. As oil and gas input increased in the second half of the 20th century, new chemical plants were built, particularly in the Volga, Ural, and North Caucasus zones and in other regions served by pipelines, which helped to reduce the dependence on traditional resources. Chemical industries requiring large quantities of electric power, such as those based on cellulose, are particularly important in Siberia, where both timber and electricity are plentiful. Overall, Russia’s chemical industry lags in scale and diversity compared with those of the United States, Canada, China, and the countries of the European Union. Light industry Textile industries are heavily concentrated in European Russia, especially in the Central region, which produces a large share of the country’s clothing and footwear. Cotton textiles are dominant, with the raw cotton supplied mainly by Central Asian countries. In the zone between the Volga and Oka rivers, east of Moscow, there are numerous cotton-textile towns, the largest of which are Ivanovo, Kostroma, and Yaroslavl. Durable consumer goods (e.g., refrigerators, washing machines, radios, and television sets) are produced primarily in areas with a tradition of skilled industry, notably in and around Moscow and St. Petersburg. Finance Russia’s monetary unit is the ruble, which is now freely convertible, a radical departure from the practice of artificial exchange rates and rigid restrictions that existed during the Soviet era. The Russian Central Bank (RCB), which took over the functions of the Soviet-era Gosbank, is exclusively responsible for regulating the country’s monetary system. The bank’s primary function is to protect and stabilize the ruble, which it attempts to do through its control of foreign exchange. Under the constitution adopted in 1993, the RCB was given greater autonomy from the central government than the Gosbank had enjoyed, but its head is appointed by the president and subject to approval by the State Duma, the lower house of the Russian legislature. In 1995 the RCB was granted the authority to oversee all banking transactions, set exchange-rate policies, license banks, and service the country’s debt. To maintain its hard currency reserves, the RCB relies on the obligation of all exporters to convert half their hard-currency earnings into rubles. In the mid-1990s the RCB established a system of supervision and inspection of the country’s commercial banks. During much of the 1990s Russia’s financial system was in a state of chaos, largely because many of the thousands of banks that formed after the fall of communism became insolvent, particularly during the economic crisis of the late 1990s. Even with consolidation of the banking industry, at the beginning of the early 21st century there were more than 1,000 Russian commercial banks, many of which were state-owned or were institutions that offered few financing opportunities for small- and medium-size businesses. Dozens of foreign banks also operate in the country. The state-owned Russian commercial banks, such as Vneshtorgbank and Sberbank, shadow the RCB both in the pursuit of stability and in operations philosophy. The banking sector is frequently accused of cronyism, benefiting only a select few, particularly former communist apparatchiks. Before the banking crisis in the late 1990s, private commercial banks mushroomed, but most of them acted as outsourcing financial agents for enterprises inherited from the Soviet era. By the beginning of the 21st century, two major clusters of banks had survived. One cluster, which included the National Reserve Bank, Gazprombank, Promstroybank, and International Moscow Bank, served the oil and gas industry. The second cluster, consisting of banks servicing the government of Moscow, included the Bank of Moscow, Mosbusinessbank, Guta Bank, Most Bank, Unikombank, International Financial Corporation, Sobinbank, MDM Bank, Toribank, Promradtekhbank, and dozens of smaller banks. Trade During the communist period the Russian republic traded extensively with the other Soviet republics, from which it “imported” a variety of commodities that it was unable to produce in sufficient quantities itself. These included cotton (from Central Asia) and other high-value agricultural products, grain (mainly from Kazakhstan), and various minerals. In return, Russia “exported” oil and gas to republics with a weak energy base, such as Belorussia (now Belarus) and the Baltic states, and sent its skilled-engineering products and consumer goods to most of its partners. By the late 1990s trade between the former union republics no longer continued in any systematic manner, particularly because agreement could not be reached on the prices to be charged for goods previously exchanged at artificially low rates during the Soviet period. Still, Russia generally has a positive trade balance with the former republics of the Soviet Union. International trade during the Soviet era was rather limited until the 1960s, and most of it was governed by bilateral and multilateral arrangements with the other members of Comecon (Council for Mutual Economic Assistance), the Soviet-led trade organization of communist eastern European countries. As Soviet economic expansion slowed during the 1970s and ’80s, it became apparent that further growth required large quantities of high-tech equipment from the West. To finance these imports, increasing amounts of hard currency were needed, and this could be obtained only by increasing exports to the West. As a result, Russia came to rely heavily on oil and gas exports as a source for its hard currency needs. With Comecon’s collapse and the dissolution of the Soviet Union itself, individual republics began to develop their own trading relations with the outside world. Russia, with its large resources of oil, gas, and minerals, seemed well placed to continue the type of trading relations with the West already developed by the former Soviet Union. Group of Eight Group of EightThe Group of Eight leaders at Konstantinovsky Palace in Strelna, Russia, for the 2006 summit. In 1994 Russia signed an agreement that strengthened economic ties with the European Union, and Russia soon joined economic discussions with the Group of Seven (G-7), which represented the most advanced economies of the world; in 1997 it was admitted as member of the Group of Eight (G-8). However, that membership was suspended indefinitely after Russia annexed the Ukrainian autonomous republic of Crimea in 2014. Russia’s long-delayed application to join the World Trade Organization was finally granted in 2012. In January 2015 Russia became a founding member of the Eurasian Economic Union. The trade bloc, which included Armenia, Belarus, Kazakhstan, and Kyrgyzstan, was intended as a counterweight to expanding EU political and economic influence in the former Soviet sphere. Foreign trade is tremendously important to the Russian economy. The country has generally enjoyed a healthy trade surplus since the dissolution of the Soviet Union. Primary exports include oil, metals, machinery, chemicals, and forestry products. Principal imports include machinery and foods. Among Russia’s leading trade partners are Germany, the United States, Belarus, Ukraine, and China. Services During the Soviet era the service sector suffered from drastic inadequacies. The state-owned services, which made no effort to respond to consumer demand, were hampered by inefficient bureaucratization. In the post-Soviet era private-sector services grew dramatically, and many of the shortages that characterized the previous era were eliminated. By the beginning of the 21st century, services accounted for more than half of GDP. Still, complaints remained regarding the provision of services by the public sector, particularly the police, schools, and hospitals. Owing to budget shortfalls, many of the public-sector services are poorly financed and have been unable to retain skilled employees. Travel and tourism account for several million jobs in Russia. Some 20 million foreign visitors travel to Russia each year, though many of these visitors are seasonal workers from former Soviet republics. Free from the restrictions of Soviet times, Russians have increasingly traveled abroad. Labour and taxation Before the dissolution of the Soviet Union, an overarching All-Union Central Council of Trade Unions nominally represented the interests of workers, though it was controlled by the governing Communist Party. In the mid-1980s there was increasing labour unrest, particularly from miners, and greater rights were granted to workers. Since the collapse of communism, labour relations have been in constant flux, and several labour codes have been adopted. Trade union reform in 2001 effectively provided the Federation of Independent Trade Unions of the Russian Federation, which represents some 50 million workers organized into various branches, a monopoly on most union activity. Alternative trade unions were unable to operate unless they represented at least half of the employees at a company. The primary sector continues to provide employment for a large proportion of the workforce, with one-eighth of workers employed in agriculture and one-fifth in mining and manufacturing. Still, the service sector (including banking, insurance, and other financial services) has grown appreciably and now employs about three-fifths of all Russian workers. Tax laws have undergone dramatic reform since the dissolution of the Soviet Union. As a result of high tax rates, the large number of unreported incomes (particularly related to organized-crime syndicates), and general fraud, the government failed to collect a significant proportion of the revenue to which it was legally entitled. In the early 21st century, to combat fraud and encourage investment, the government simplified the tax system and reduced the overall tax burden, particularly on businesses. For example, corporate taxes were reduced by about one-third, a flat tax was imposed on incomes, and the value-added tax on the sale of goods was reduced. A single natural resource extraction tax also replaced three existing resource taxes. The value-added tax is a large source of government revenue. Transportation and telecommunications Rails and snow Rails and snowThe Baikal-Amur railway running through Siberia, Russia. Russia’s vast size and the great distances that often separate sources of raw materials and foodstuffs from consumers place a heavy burden on the transport system. One result has been the continuing dominance of the railways, which account for about nine-tenths of the country’s freight turnover (three-fifths if pipelines are included) and half of all passenger movement. Nevertheless, the rail network is a very open one, and its density varies regionally: it is highest in the Northwest, Central, and Central Black Earth regions and lowest in East and West Siberia and the Far East. Some two-thirds of the railway network lies along the main belt of settlements. The railway network of European Russia is nearly seven times as dense as that found in the Asian portion of the country. Indeed, east of the Urals the term network is a misnomer, since the system consists of only a few major trunk routes (e.g., the Trans-Siberian Railroad and Baikal-Amur Mainline) with feeder branches to sites of economic importance. Russian railways are among the world’s leading freight carriers, the line from the Kuznetsk Basin to the Urals being especially prominent. The railways are owned and run by a joint-stock company controlled by the state. Much of the country’s rolling stock is obsolete. Apart from highways linking the major cities of European Russia, the road system is underdeveloped and carries only a tiny fraction of all freight. The private automobile became a symbol of middle-class status in the post-Soviet years, but the percentage of people owning vehicles is still quite small. Inland waterways carry a much larger volume. Although the greatest volume is carried on the Volga system, river transport is most vital in areas devoid of railways. In addition to its vital role in foreign trade, maritime transport also has some importance in linking the various regions of Russia, particularly those that face the Arctic seaboard. Traffic on the Arctic Ocean route is seasonal. Air transport plays an increasingly important role. Russian airlines carry only a minute fraction of all freight, chiefly high-value items to and from the remote parts of Siberia, where aircraft are sometimes the only means of transport. Airlines are responsible for nearly one-fifth of all passenger movement. Aeroflot (renamed Aeroflot-Russian Airlines in June 2000), formerly the state airline of the Soviet Union, is the country’s largest air carrier; the Russian government maintains majority ownership of Aeroflot. Sheremetyevo and Domodedovo in Moscow and Pulkovo in St. Petersburg are the country’s major airports, with the older Sheremetyevo airport losing tenants to the more modern Domodedovo. Most major cities have service to international or domestic locations. The Russian telecommunications sector is inferior to those of other industrialized countries. For example, in the early 1990s only about one-third of the country’s households had a telephone. Largely through foreign investment, however, the country’s telecommunications infrastructure has been greatly improved. In 1997 the State Committee on Communications and Informatics was formed from the Ministry of Communications and the State Committee on Information Technology to regulate telecommunications policies, oversee the liberalization of the sector, and encourage competition; by the beginning of the 21st century, there were more than 1,000 telecommunications companies. Nevertheless, several large companies, such as Svyazinvest and Rostelkom, control much of Russia’s telecommunications industry. In addition, Internet use in Russia grew very slowly in the 1990s, particularly outside the major urban areas, but it has since grown fairly steadily.