Ukraine, the land and its people

by Stepan Rudnytskyi

The important Dniester River attains a length of over 1300 km., and possesses the greatest variety of distinct sections of river of all the Ukrainian streams. It originates in the High Beskid, near the village of Vovche, as a very energetic, wild creek. In a defile it advances into the sub-Carpathian hill-country, where it has deposited great masses of rubble. The mountain stream changes rapidly into a lowland stream and forms great swamps in the Dniester Plain, which, in high-water time, are converted [[67]]into large river lakes. From the left bank, the Dniester here receives the muddy Vereshitza (from the Rostoche), which forms many ponds, from Western Podolia, the Hnila Lipa. All the remaining tributaries of this section of the Dnieper come from the Carpathians, on the left the Strviazh (Strivihor), on the right the Bistritza, the mighty meandering river Striy with the Opir, and the Svicha (with the Misunka). All these rivers are mountain streams, flow in beautiful defiles, and deposit great masses of rubble on the verge of the Carpathians. Beginning at the delta of the Svicha, the Dniester Plain becomes a wide, flat-bottomed valley, in which the river flows along in great bends and receives the Limnitzia and both the Bistritzas from the Carpathians. Near Nizniv the banks approach each other very closely and the Dniester enters a yar (cañon), not leaving its steep sides until near Tiraspol. The Podolian tributaries of the Dniester on the left side, the Zolota Lipa, Stripa, Sereth, Zbruch, Smotrich, Ushitza, Murakhva, Yahorlik, roll their turbid waters in similar cañons toward the Dniester. The Bessarabian tributaries, on the contrary, have wide, swampy valleys. All these plateau rivers are slight in volume of water, 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.

The Boh, falsely named the Southern Bug, is a real plateau river. It rises in the village of Kupil, near the source of the Sbruch, on the Austrian border, and flows as a typical Podolian mud-streamlet, in a flat valley, covered with ponds and swamps. But, beginning at Mezibiz, its bed becomes rocky, the valley slopes become high and keep approaching each other. The Boh Valley gradually becomes a cañon-like “yar,” altho it is at no point so deep as the Dniester Valley. The granite-gneiss formations of the Ukrainian horst appear here as picturesque shore rocks and slopes along the river and form innumerable rapids (as, for example, Constantinivka) in the river bed. Stony beds and narrow, rocky valleys are also found in the most important tributaries of the Boh—the Sob, Siniukha, Inhul on the left; the Kodima and Chichiclea on the right. All of them have little water, and in dry summers only a chain of ponds marks the valley road of the river. The main stream, too, has not much water, being unfit for navigation even in the time of the spring floods. Only the last 130 kilometers of its course, from Vosnesensk down, are navigable. At the entrance of the Inhul the Boh begins to widen considerably, the current becomes slow, and the depth at Mikolaiv sufficiently great to enable smaller sea vessels to reach its harbor. Slowly widening, the river gradually turns into the Buh liman, which has the winding outline of a river and unites with the great liman of the Dnieper. The entire length of the Boh is over 750 kilometers.

We now come to the main river of the Ukraine, the majestic Dnieper. To the Ukrainian people the Dnieper bears the same significance as the “Matushka Volga” to [[70]]the Russians, the Vistula to the Poles, and the Rhine to the Germans. The Dnieper is the sacred river of the Ukraine. Like a divinity it was honored by the old Polans, the founders of the ancient Ukrainian state of Kiev; Slavutitza was the name given it by the Ukrainians of the monarchy. It was esteemed as a father and provider by the brave Zaporog Cossacks, the champions of Ukrainian liberty. For many centuries the Dnieper has played an important part in the folk-lore and literature of the Ukraine, in traditions and fairy-stories and folk-tales and in thousands of folk-songs; since ancient times it has been sung by all Ukrainian poets, from the unknown bard of the epic of Ihor, to the greatest of all Ukrainian poets, Taras Shevchenko, and so on, down to the youngest generation of the poets of the Ukraine. To them all, the Dnieper is the symbol of the Ukraine, of its life, and of its past. Not without cause did Shevchenko ask to be buried on the mountain shore of the Dnieper, “that I may see the endless plains and the Dnieper and the crags of its banks and hear the rushing of the Rushing One.” For no one is able to repeat the impressions which fill the soul of every Ukrainian when he looks down from this beautiful observation point of Shevchenko’s grave upon the majestic river below. How many thoughts, then, arise about the glorious, and yet so unspeakably sad, past of the Ukraine, about its miserable present and the great future toward which the nation tends, amid great difficulties, as does the Dnieper toward the Black Sea over the porohs. And we do not wonder that the Dnieper has become the national sanctuary of the Ukraine. With this river are connected all the important events of the historical life of the Ukraine. The Dnieper was the father of the ancient Ukrainian empire of Kiev; by way of the Dnieper a higher culture made its way into the Ukraine; on the Dnieper the Ukrainian Cossack element developed, which, after centuries of [[71]]subjugation, gave the Ukrainians a new government. The Dnieper River has, since hoary antiquity, been the most important channel of intercourse between the North and the South of Eastern Europe; it has been the means of connecting the Ukraine with the sea and the cultural realm of Southern Europe. Its present importance, despite the low grade of culture in Eastern Europe, and despite Russian mismanagement, is great, and is growing rapidly. And if in the future the river is made accessible to sea-going vessels and becomes a road for large-scale navigation, its significance may become almost incalculable.

The Dnieper is the third largest river in Europe, after the Volga and the Danube. The length of its course is more than 2100 km. The region it drains includes 527,000 sq. km., not much less than the whole of France. Among the streams of the globe the Dnieper ranks thirty-second.

If the Dniester possesses some of the properties of a Central European river, namely, mountainous country at its source and many mountain tributaries; if the Boh is a genuine plateau river; the Dnieper, on the other hand, is the real type of a river in Eastern Europe. It rises in White Russia near the village of Clozove. A little swamp, which was formerly a small lake, situated at a height of 256 m., forms the source of the river. Because of this small height of the source, the Dnieper has, as, in fact, all the Eastern European rivers have, a very insignificant incline and an average speed of current of 0.4 m. per second. The source of the Dnieper lies near the sources of the Dvina and the Volga, as well as the source streams of the Neva.

Near its source the Dnieper is a small, muddy streamlet, which seeks its way southward in a flat valley, three miles wide, between swamps and moors. But quickly its volume increases, and, as near the source as Dorogobuz, the river becomes navigable for smaller vessels. Here it suddenly [[72]]turns to the west, both valley slopes, but especially the left one, become higher and steeper, the valley narrows down to ½ km. But after a short stretch it becomes wide and swampy again at Smolensk. The depth of the river is very irregular, the pools (plessa) attaining a depth of 5 meters, the rapids often less than ½ meter. From Smolensk to Orsha the Dnieper Valley again becomes hardly 1 kilometer wide, between high banks. On the left bank picturesque, rocky precipices appear. At Orsha the Dnieper turns to the south, retaining this direction as far as Kiev. Down to Shclov the Dnieper Valley remains narrow, with steep slopes, then it widens slowly but steadily. The depth of the river reaches 10 meters, but many shoals, great morain boulders and broken sandstone make navigation difficult. Below Mogilev the spurs of the White Russian and Central Russian plateaus withdraw from the Dnieper and show only on the left side. The river reaches the low plain of the Polissye and flows in majestic turns thru swamps and meadows which are dotted with old river beds. In this section of its course the Dnieper receives the Druch and the voluminous, navigable Beresina on the right, and the navigable Soz on the left. The Dnieper receives an especially great amount of water from the Beresina. River navigation is doubled below its entrance, mainly because of innumerable rafts which are traveling to the treeless South Ukraine and the Black Sea from the forests of White Russia.