Ural Region

Ural (russian: Урал) is a geographical region located around the Ural Mountains, between the East European and West Siberian plains. It is considered a part of Eurasian Steppe, extending approximately from the North to the South; from the Arctic Ocean to the end of the Ural River near Orsk city. The border between Europe and Asia runs along the Eastern side of the Ural Mountains. Ural mostly lies within Russia but also includes a small part of Northwestern Kazakhstan. This is a historical, not an official entity, with borders overlapping its Western Volga and Eastern Siberia neighboring regions. At some point in the past, parts of the currently existing Ural region were considered a gateway to Siberia, or even Siberia itself, and were combined with the Volga administrative the divisions. Today, there are two official namesake entities: the Ural Federal District and the Ural economic region. While the latter follows the historical borders, the former is a political product; the District omits Western Ural and includes Western Siberia instead.

The historical center of the Ural is Cherdyn, which is now a small town in Perm Krai.
Perm was an administrative center of the gubernia with the same name by 1797. Most of the territory of historical and modern Ural was included in Perm Gubernia. The administrative center of Urals was moved to Sverdlovsk (nowadays Yekaterinburg) after the Russian Revolution and Civil War. In the present, the Ural economic region does not have an administrative and informal capital, whereas Yekaterinburg is the administrative center of the Ural Federal District.

Etymology

From the 11th century, the region of the Ural Mountains was called ''Kamyen (Камень, "the Stone") by Russians. In the mid-16th – early 17th century, the southern parts became known as Ural, which later spread to the entire area. The name probably originated from Turkic "aral". This word literally means "island" and was used for any territory different from the surrounding terrain. In Bashkortostan there is a 13th-century legend about a hero named Ural. He sacrificed his life for the sake of his people, and they poured a stone pile over his grave, which later turned into the Ural Mountains.

Topography

By topography and other natural features, Ural is divided, from north to south, into the Polar (or Arctic), Near-Polar (or Sub-Arctic), Northern, Central and Southern parts. The Polar Ural has an area of about 25,000 km² and a strongly dissected relief. The Near-Polar Ural is wider (up to 150 km) and higher than the Polar Ural. The Northern Ural consists of a series of parallel ridges with the height up to 1,000–1,300 m and longitudinal depressions, which are elongated from north to south. The Central Ural is the lowest part of Urals, with the highest mountain of 994 m (Basegi) and a smooth relief. The relief of Southern Ural is more complex, with numerous valleys and ridges directed south-west and meridionally.

Geology

Urals contains 48 species of economically valuable ores and minerals. Eastern regions are rich in chalcopyrite, nickel oxide, chromite and magnetite ores, as well as in coal (Chelyabinsk Oblast), bauxite, gold and platinum. Western Ural contains deposits of coal, oil, gas and potassium salts. The speciality of Urals is precious and semi-precious stones, such as emerald, amethyst, aquamarine, jasper, rhodonite, malachite and diamond.

Climate

The climate of Ural is continental. The ridges of the Ural Mountains are elongated from north to south, they effectively absorb sunlight thereby increasing the temperature. The areas west to the Ural Mountains are 1–2 °C warmer in winter than the eastern regions because the former are warmed by the Atlantic winds whereas the eastern slopes are chilled by the Siberian air masses. The average January temperatures increase in the western areas from –20 °C in the Polar to –15 °C in the Southern Urals and the corresponding temperatures in July are 10 °C and 20 °C. The western areas also received more rainfall than the eastern ones by 150–300 mm per year. The highest precipitation (1000 mm) is in the Northern Ural that causes the average height of snow up to 90 cm. The eastern parts receive from 500 to 600 mm on the north to 300–400 mm on the south.

Rivers and lakes

Most Ural rivers belong to the basin of the Arctic Ocean. They include Tobol, Iset, Tura, Pechora, Lozva and Severnaya Sosva Rivers. The southern rivers – Ural, Kama, Belaya and Chusovaya Rivers – belong to the Caspian Sea basin. Western rivers, especially north-western ones, are more affluent. They have high and long (2–3 months) floods in May–June (June–July in the Polar Ural). The south-eastern rivers are much narrower and may dry up in summer. Rivers are fed by melting snow and precipitations. The largest lakes are on the east of the Central and Southern Urals. They include Tawatui, Argazi, Uvildy and Turgoyak. The deepest lake (136 m) is Bolshoe Schuchye. Rivers and lakes are used as a water supply, transport routes and for waterlogging. Some rivers have dams forming the Kama and Votkinsk Reservoirs.

Flora

The landscapes of Ural change both in the latitudinal and vertical directions and are dominated by steppes and forests. Steppes lie mostly in the southern and especially south-eastern Urals. Meadow steppes have developed in the lower parts of mountain slopes and are covered with various clovers, daisies, filipendula, meadow-grass and foxtail millet, reaching the height of 60–80 cm. Many lands are cultivated. Moving to the south, the meadow steppes become more sparse, dry and low. The steep gravelly slopes of mountains and hills of eastern slopes of the Southern Ural are mostly covered with rocky steppes. Valleys of the rivers contain willow, poplar and caragana shrubs.

Forest landscapes of Urals are diverse, especially the southern part. The western areas are dominated by dark coniferous taiga forests which change to mixed and deciduous forests on the south. The eastern mountain slopes have light coniferous taiga forests. Southern Ural is most diverse in the forest composition; here together with coniferous forests also abundant are other tree species such as larch, oak, birch, maple and elm. The Northern Ural is dominated by Siberian species of fir, cedar, spruce and pine. Forests are much more sparse in Polar Ural. Whereas in other Ural Mountains areas they grow up to the heights of 1 km, the forests cease at 250–400 m in the Polar Urals. The polar forests are low and are mixed with swamps, lichen

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