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The article focuses on the characteristics of the rivers flowing through the territory of the Dzhankoy region and Dzhankoy town okrug in the Republic of the Crimea (Istochnaya, Tselinnaya, Vygonnaya, Sivash, Zavet-Leninskaya, Mirnovka with Stepnaya, Pobednaya, Stal’naya, Zelyonaya, Gvardeiskaya, Blagodatnaya, Velikosel’skaya). In the main these rivers are temporary watercourses, filled up with water during thaw in winter and after rains. They are slightly inclined from the south to the north. Their headwaters are on the height of little more than 20-30 m, but their estuaries may have negative values of absolute heights. The most characteristic feature of the rivers studied is the fact that their watercourses were straightened and deepened in the 60s-70s of the last century and they began to be used as collectors. It was caused by putting into operation the first stage of the Severo-Krymsky canal. After that the level of ground waters rose and this resulted in water logging of the territory and flooding the settlements. Water discharge depended, in the main, upon dumping of drain water, the volume of which had sharply reduced after cutting off the Dneeper water to the Severo-Krymsky canal.

The characteristics of the Dzhankoy Region Rivers and Dzhankoy Town Okrug of the Republic of the Crimea