Revista Comenius

Page 6

ROMANIA from the central crown of the Carpathians. They are fed by rainfall and melting snow, which causes considerable fluctuation in discharge and occasionally catastrophic flooding. In the east, river waters are collected by the Siret and the Prut. In the south, the rivers flow directly into the Danube, and in the west, waters are collected by the Tisza on Hungarian territory. The Danube is by far Romania’s most important river, not only for transportation, but also for the production of hydroelectric power. One of Europe’s largest hydroelectric stations is located at the Iron Gates, where the Danube surges through the Carpathian gorges. The Danube is an important water route for domestic shipping, as well as international trade. It is navigable for river vessels along its entire Romanian course and for seagoing ships as far as the port of Brăila. An obvious problem with the use of the Danube for inland transportation is its remoteness from most of the major industrial centers. Moreover, marshy banks and perennial flooding impede navigation in some areas. The Romanian Black Sea Coast stretches a little over 150 miles. The Black Sea is a continental sea, with a low tide and salinity and water temperatures of 77 - 79˚F in the summertime. Its wide, sandy beaches facing east and south-east become a major tourist attraction from May until September.

Lakes There are around 3,500 lakes in Romania, most of them small or medium. The largest are the lagoons and coastal lakes on the Black Sea shore, such as Razim (164 sq. miles) and Sinoe (66 sq. miles), or lakes along the Danube bank - Oltina (8.5 sq. miles); Brates (8.1 sq. miles). Formed at the end of the last Ice Age, the glacial lakes in the Carpathian Mountainsare small, but spectacular. Worth mentioning are the glacial lakes in the Retezat Mountains: Zanoaga,

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