Андреевская энциклопедия Д.Л. Андреев: Энциклопедия с обширной библиографией Автор-составитель Михаил Белгородский Статьи по теме «Реки России»

Основная энциклопедия Расширение энциклопедии Словарь метонимий... Список заглавных статей Англоязычные статьи

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Дон

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Дон

Тематическая статья «Основной энциклопедии».
Относится к разделу Россия.

Содержание

Текст статьи

Использованные источники

Большой энциклопедический словарь.

Andreev encyclopædia An encyclopædia on Daniil Andreev with vast bibliography Mikhail Belgorodskiy, the author-compiler The articles on the topic “Rivers of Russia”

Basic encyclopædia Broadening of the encyclopædia A dictionary of metonymies... The list of title articles Russian articles

Contents of this page
(green font highlights the “Broadening of the encyclopædia” rubrics;
green font highlights the synonyms of “Basic encyclopædia” rubrics, which are absent in the reviewing texts)

Don River

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Don River

A thematic article of the “Basic encyclopædia.”
Falls into the category of Russia.

Contents

Text of the article     §1. Geography     §2. Physiography     §3. History and economy

Used sources A bibliography

(in Russian Дон), one of the great rivers of the European portion of Russia. It has been a vital artery in Russian history since the days of Peter I the Great, who initiated a hydrographic survey of its course. Throughout the world the river is associated with images of the turbulent and colourful Don Cossacks—romanticized in a famous series of novels by the 20th-century Russian writer Mikhail Sholokhov—and with a series of large-scale engineering projects that have enhanced the waterway's economic importance.
§1. Geography. The Don River rises in the small reservoir of Shat, located in the Central Russian Upland near the city of Novomoskovsk. It flows generally in a southerly direction for a total distance of 1,162 miles (1,870 kilometres), draining a basin of some 163,000 square miles (422,000 square kilometres), before it enters the Gulf of Taganrog in the Sea of Azov. It lies between the Volga River to the east and the Dnieper River to the west. In its middle and lower courses, from the confluence with the Chornaya Kalitva River to its mouth, the Don forms an enormous eastward-bulging arc as far as its junction with the Ilovlya River. Near the top of the arc, the vast Tsimlyansk Reservoir begins. The Volga–Don Ship Canal stretches from the upper part of the reservoir to the Volga, which at that point is a mere 50 miles distant. From its source in the Tula oblast, the Don crosses the Lipetsk, Voronezh, Volgograd, and Rostov oblasts, through the forest steppe and renowned steppe zones of southwestern Russia. Along the way it collects the waters of numerous tributaries, the most important of which are the Krasivaya Mecha, Sosna, Chornaya Kalitva, Chir, and Donets (right bank) and the Voronezh, Khopyor, Medveditsa, Ilovlya, Sal, and Manych (left bank). The river winds throughout its course, and the drop along its length is about 620 feet (190 metres).
§2. Physiography. In the upper portion of the Don—that is, as far downstream as the southeastward bend—the river flows along the eastern edge of the Central Russian Upland through a generally narrow valley. The right bank is pronounced, reaching heights of 160 feet above the river at the cities of Dankov and Lebedyan, and its limestone and chalk rocks are cut into by ravines and gullies. The left bank borders a flatter floodplain, and the river itself widens intermittently into small lakes; depths range from a few feet in the shoals to 33 feet, with a maximum width of 1,300 feet. In the middle course, to the beginning of the Tsimlyansk Reservoir, the valley widens to about four miles, and its path is marked by floodplains, more small lakes, and relict channels; the banks, especially the right bank, become steeper, with chalk, limestone, and sandstone predominating. The river narrows to 330–1,300 feet. The lower course is dominated by the nearly 190 miles of the Tsimlyansk Reservoir, completed in 1953. With an area of some 1,050 square miles and a maximum width of nearly 25 miles, the reservoir has an average depth of about 30 feet. Finally, the lower section of the Don has a valley width of 12–19 miles, with a huge floodplain and a braided river channel as much as 66 feet deep. The landscape of the upper and middle Don basin is characterized on the right bank by undulating plains cut into by jagged gorges and on the left bank by the smoother, pond-dotted topography of the Oka-Don Lowland. Farther downriver the vast open landscapes of the steppes predominate. Rich black chernozem soils fill almost the entire basin, though there are patches of gray forest soil in the north, where forests cover up to 12 percent of the area.
§3. History and economy. Archaeological evidence of early settlement of the Don River basin dates from the Upper Paleolithic (40,000–13,000 years ago). At the beginning of the 2nd century BC, tribes of herdsmen occupied the valley of the Don and developed livestock raising and crop agriculture there. The Tatars conquered the region during the first half of the 13th century AD. The Russian state, expanding southward from the Grand Principality of Moscow, incorporated the Don River basin between the middle of the 15th and 16th centuries. The famed Don Cossacks established themselves in independent military settlements along the middle and lower Don by the 16th century but subsequently came under tsarist control. Since the early 1950s the Don has undergone intensive economic development. The key to this was the creation of the huge Tsimlyansk Reservoir along its lower course. The project included a hydroelectric station, a fish elevator, two navigation locks, an irrigation canal, a 1,580-foot concrete dam, and an eight-mile earthen dam. By 1975 an additional 116 reservoirs, with volumes exceeding 35 million cubic feet each, existed in the basin. The Tsimlyansk Reservoir contributed to a rapid expansion of irrigation in the Don River basin, which grew from about 124,000 acres (50,000 hectares) in 1950 to nearly 2.5 million acres by 1980. In the upper basin an extensive network of ponds aids irrigation; these ponds are also used for raising fish. The significance of the Don as a navigable waterway greatly increased with the construction of the Volga–Don Ship Canal. The river itself is navigable from the mouth to the city of Liski (a distance of 842 miles) and in the spring for another 150 miles upstream. Navigation in the lower course has been facilitated greatly by the Tsimlyansk project. Navigation at the mouth of the Don is occasionally hindered by the declines in water level induced by strong, persistent offshore winds, while dredging operations are necessary to maintain and improve navigation in the upper reaches. The largest ports are Kalach-na-Donu, Tsimlyansk, and Rostov-na-Donu. The development of the Don has provided substantial economic benefits to the riverine populations as well as to the nation, but these alterations have reduced substantially the amount of water discharged at the river's mouth. This decrease –estimated in 1975 to be 20 percent of the 1950 level and still rising—has come chiefly from water diversion for irrigation and through evaporation from the artificial reservoirs; and, as a result of it, the salinity of the Sea of Azov has risen considerably, diminishing the sea's biological productivity and lowering fish catches.

Encyclopædia Britannica.

Klein, Richard G. Man and Culture in the Late Pleistocene. – 1969. # Deals with the Stone Age civilization of the Don River valley.

Raev, Boris A. Roman Imports in the Lower Don Basin / Trans. from Russian. – 1986. # Based on the result of the archaeological excavation in the Don River region.