Ukraine, the land and its people : $b an introduction to its geographyRudnytskyi, Stepan
Science
Ukraine, the land and its people : $b an introduction to its geography
Rudnytskyi, Stepan
Ukraine; Ukrainians
Toward the southwest, too, Podolia declines with a similar steep border, but this
one is neither so uniform nor so high and picturesque. These steep borders owe their
origin to a recent uprising, which has affected the Podolian Plateau, especially in
the west, since the glacial period. To the same cause the picturesque, beautifully
wooded, eroded hill-country of the Opilye owes its origin, a section which extends
southeast from Lemberg in the regions of Rohatin and Berezani to the Dniester, and
which, with its peaks, reaches a height of 440 m. Most remarkable, however, is the
long chain of rocky hills which extends from Brody to the southeast toward Kamenetz
Podilski. This chain of hills, which bears the name of Toutri, is marked on all maps
by the wilfully chosen name of Medobori. The limestone rock, which contains a great
amount of fossils, forms fantastic crags on the more than 400 m. peaks of the hill-chain,
which look down upon the land like old fortresses. The entire chain of hills is a
new-tertiary coral and briozone reef which, after the withdrawal of the sea, remained behind as a long rock dyke.
Beyond this hilly region the entire Podolian Plateau has a flat, undulating surface.
Beginning as far back as the upper Sereth and Sbruch we find typical steppe-plains.
The farther southwest, the more flat, undulating and steppe-like sections do we meet,
until finally the Podolian elevation gradually merges in the Pontian steppe-plain.
Much variety and beauty is given to the appearance of the Podolian landscape by the
valleys of the Dniester tributaries on the left. In their upper parts they are wide
and have flat, swampy ground, many ponds and bogs [41]and gentle valley declines. In its further course the river begins to cut in more
and more deeply, the valley becomes constantly narrower and deeper and winds on in
regular bends, the valley-sides become higher and steeper, bare walls of rock take
the place of the soft green slopes. We are in a Podolian “yar,” in a miniature cañon.
In the sides of the yars the geologic history of the Podolia is engraved in imperishable letters. The river has sawed the plateau thru as tho
with a gigantic saw, and has exposed the various layers of stone. As a rule they lie
nearly horizontally above one another.
Public-domain text, read in full here on John Shaqi.
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