altho some of them attain considerable length. Only in the spring, when the snow-blanket melts, do their waters overflow the banks. In summer the water-level becomes very low, and the water of the early summer showers is stored up in the many ponds, which are found in large numbers, in the country about the sources of these rivers. All these plateau rivers are not even navigable for rafts; even the little fishers’ boat can hardly find its way along the muddy shoals. In its cañons the Dniester River assumes all the characteristics of a plateau river. Its waters generally take up the entire bottom of the cañon, leaving very little space for the abodes of men. The incline of the river [68]is not uniform, but constitutes a series of slight steps. Sections with rapid currents alternate with quiet depths. The small brooks which come down the short lateral gorges of the Dniester cañons bring great masses of loose stones and rubble into the river bed, as a result of the reckless destruction of forests, and build constantly growing cones of rubble, which the river must remove slowly and laboriously. They also form dangerous shoals and hinder the development of navigation on the Dniester. The river also forms regular rapids, near Yampil, where a layer of granite stretches clear across the river. For this reason the Dniester, tho navigable along a stretch of almost 800 km., has not become an important waterway. The navigation of the Dniester, which becomes more active from Khotin on, is now on the wane. Eight hundred years ago sea vessels were still able to reach the old Ukrainian royal city of Halich. The floods of the Dniester are famous. In the spring, when the snows melt in the Carpathians, the Dniester Plain is converted into a great river-lake. The Carpathian tributaries bring the main stream so much water, that it cannot easily flow off thru the narrow cañon, and so, floods the whole wide Dniester Valley for weeks. Then there is high water even in the cañon of the Dniester, but it has little scope. Near Tiraspol, the Dniester Valley widens out again. Swampy plavni wilds extend on both sides of the river. In a beautiful, rapidly growing delta, the Dniester empties into its liman, which it is slowly filling in with its precipitates. Two narrow outlets (hirló) break thru the bar of the liman and connect it with the sea. Between the Dniester and the Boh, not one river finally empties into the sea. Even the largest rivers of the region, the Little and Big Kuyalnik and the Tilihul end their courses in limans, which are entirely closed off by bars. [69]The valleys of these coastal rivers are narrow, becoming wider at last, when they are about to enter the limans. The current is always slow and the water often evaporates completely in the summer.