Knowledge Hypermarket>>Geography>>Geography of 8th grade >> Geography: main river basins and their characteristics. Character of water mode of rivers (fall, slope; water mode, supply, water expenses in river, annual river run-off). Work of rivers, channel formation, including concepts of basis erosion, solid river run-off. The largest river systems of Ukraine.
MAIN RIVER BASINS The overwhelming majority of rivers in Ukraine (94 %) belong to the Black sea and the Azov sea basins. Only the rivers of the western part of the country are related to the Baltic sea basin. Some small rivers in the south of the country have no streamflow into the World Ocean. Such distribution of river run-off is caused by the general structure of the surface of Ukraine.
Thus it is impossible to imagine Ukraine without the Dnieper-Slavutych. For us it is not only the powerful waterway, picturesque beauty, but also the reflection of the soul of our nation, its history. On the banks of the Dnieper the kernel of the Ukrainian state – golden-domed Kyyiv was formed, the first Ukrainian democracy - the Zaporizhzhya Cossacks was born, from its steep slopes the national genius Taras Shevchenko admires the native spaces.
The Dnieperflows along the middle part of Ukraine from the north to the south. It collects waters almost from half of the country’s area, from its northern, western and eastern territories. The river begins with a small bog on the Valdai Hills, in Russia, at height of 220 m above sea level. Further it flows over the territory of Belarus and enters into Ukraine as the big flat river with a wide valley. It has a twisting channel with shallows, sleeves and islets. Depth of the Dnieper amounts to 3-12 m, width is 700-1 500 m. In its flood-lands there are many former river-bed lakes, boggy sites. The right bank of the river is high and mountainous, whereas the left one is low and flat. In areas where the Dnieper crosses the Ukrainian crystal board (between Dnipropetrovsk and Zaporizhzhya) once there were rapids that completely partitioned off the river. Now all of them are flooded by the waters of the Dniprovskyy reservoir. A number of reservoirs formed on the Dnieper did not only flood the rapids but also considerably changed the banks of the river and straightened its channel. On the Dnieper there are many islands (the Hortytsya within Zaporizhzhya, the Trukhanov within Kyyiv). With several creeks the Dnieper flows into the Dniprovsky estuary, and from it with one wide mouth - into the Black sea.
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The Dniester has length of 1 362 km with 705 km within Ukraine. Its source is on the slopes of the Carpathian mountains. In the upper courses it is the typical mountainous river, in the middle stream it turns into flat river with wide valley. Between the Podolska and the Prekarpatskaya heights the valley of Dniester is narrowed and obtains canyon-like forms. Its channel is extremely twisting. The Dniester runs into wide Dnistrovskyy estuary connected with its narrow mouth to the Black sea.
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The largest feeders of the Dniester are the Stryy, the Limnytsya, the Seret, the Zbruch, the Smotrych, the Murafa. The Dniester and its feeders have a mixed type of water supply. Flooding comes in spring whereas high waters occur in summer and in autumn. The waters of the Dniester are used for water supply of built-up areas and enterprises, irrigation of fields. On the river the Hydroelectric power station is built. In middle and bottom streams the Dniester is navigable, nevertheless, nowadays the river is almost not used as the transport channel. On the banks of the Dniester such well-known historical and cultural centers as Galych, Khotyn, Bilgorod-Dnistrovskyy are located. On the border of Ukraine with Romania the Danube flows with its bottom stream (with length of 175 km) — the second largest river of Europe according to its length (the general length is 2 960 km). It is one of the deepest rivers of Europe. It runs into the sea with several mouths. On the border of Ukraine the Kiliyskyy mouth is passing through the largest river run-off. The Kiliyskyy part of delta is actively put forward to the Black sea at the distance up to 180 m per year. The delta is rushy, cut with numerous channels, covered with lakes. These are the Danube River plavni - a unique place of wintering and rest during migration of many birds. The Danube has the mixed type of water supply with prevalence of rain waters. The river freezes only in times of very cold winters. The Tisa, the Prut, the Cheremosh and the Siret are the largest feeders of the Danube beginning in Ukraine. They begin in the Carpathian mountains where they have a steep stream, great number of cataracts and falls, their waters bear a lot of silt and stones which are deposited in due course on plains. The Danube is the important transport channel of Europe.
The middle-size rivers of the Sea of Azov basin according to their length are the Kalmius, the Berda, the Molochna, the Salgyr. They proceed in droughty areas and consequently are shallow, whereas the Salgyr in its bottom stream is dried up.
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I.L. Ditchuk, O.V.Zastavetska, I.V.Brushchenko Physical geography of Ukraine, 8th grade Sent by readers of the Internet siteГеографія 8 клас
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