The nature of the landscape of the Dnieper Plateau is, consequently, different from that of the Volhynian or Podolian. The lightly undulating plateau, gradually becoming flatter toward the east and south and broken up only near the river valleys into flat dome-shaped hills; the valleys of the rivers, wide, not deep, and yet with rocky river beds and rocky slopes, with loess gorges and walls; the mighty Dnieper with its picturesque mountain shores; the never-ending grain steppes crossed by little woods, mohilas and long, extended old walls of rock—this is the landscape view of the old Kiev country, the heart of the Ukraine. The Dnieper Plateau becomes constantly lower toward the southeast, without, however, losing its original landscape nature in the least. Near the Dnieper rapids we see, quite distinctly, that the miocene-covered sub-layer of granite of the Ukrainian plateau group stretches straight across the river and is the cause of its rapids. But the differences in level at that point are no longer different from the variations in a plain. In the region of the source of the Samara and along the Donetz the land finally rises above the 200 m. level again. We are now in the Donetz Plateau. As near as Isium we confront the first boundary post [52]of the plateau in the steep chalk rocks of Mt. Kremianetz on the Donetz River. Further down we see the picturesque rocks of the famous monastery of “the Holy Hills.” All these are parts of the northern verge of the plateau, which is its limit on the north. Near Slavianoserbsk and Luhansk this picturesque border reaches a height of 70 m. The course of the Donetz also forms the eastern boundary; the southern boundary is formed by the small strip of the Pontian Plain on the shore of the Sea of Azof; the western border is denoted by the plain on the left bank of the Dnieper. The Donetz Plateau stretches in a long flat ridge from N. W. W. to S. E. E., and extends a flat side-ridge to either side. The longer one goes southward, almost as far as Mariupol, the other northward to Bakhmut. The surface of the plateau is very level and declines very flatly toward all sides. Only light billows of land traverse the steppe surface, which is strewn with countless tumuli. In the south these hills often have a core of granite. The river valleys have steep, altho not high slopes. They divide the uniform surface of the heights but slightly. From the surface configuration one could never guess that at this point there was once a mountain range which fell victim to the exogenous forces of the earth’s water and air blanket. Only an insignificant part of the surface of the Donetz Plateau lies more than 300 m. high; the highest point, Tovsta Mohila, barely reaching 370 m.