Beginning at the liman of the Dnieper, the coast is strongly indented as far as the bay of Karkinit, but these indentations (Yahorlik, Tendra, Kharilgach) are closed off by long tongues of land and the undersea extension of the bar of Bakalsk. The west coast of Crimea is also a uniform liman coast, increasing constantly in height, however, toward the south. At the Alma delta the coast becomes steep and has two excellent harbors, Sevastopol and Balaklava, which are submerged deep valleys. The southeast coast of the Crimean peninsula is a strongly marked acclivitous shore. The steep descent of the Yaila Mountains has been transformed here, thru the abrasive action of the sea, into a beautiful coastline. Eruptive rock, capable of offering great resistance, is found here in places,
forming picturesque capes, jetties and crags, between which lie pretty little bays and coves. The agreeable climate, the clear sky, the good sea-baths and the beautiful country annually lure to this Ukrainian Riviera thousands of consumptives and health-seekers. There are rows and rows of cottage-colonies and mansions.
Beginning at the crescent-shaped bay of Feodosia, the coast again becomes lower and also has a number of salty lagoons and bars. Of the same description are the coasts of the Strait of Kerch, leading into the Sea of Azof, which is 35,000 sq. km. in area. This extremely flat sea is often compared to a liman. Numerous tongues of land (Biriucha, Obitochna, Berdianska, Kossa, etc.) jut out here into the sea, showing very clearly in their direction the effect of the cyclonal motion of the air. The low coast has an enormous number of limans and lagoons, e. g., Utluk, Mius, Molochni, Yeski, Akhtirski, Tamanski, Kisiltash, etc. The most remarkable part of the Sea of Azof, however, is the Sivash. A bar 111 km. in length shuts the Sivash off from the Sea of Azof, leaving only a connecting passage of 150 m.,near Henichesk. The curiously ragged banks of red-clay, the salt swamps, lagoons and islands, the bracken, ill-smelling water, which is salty in summer, and in a few spots at other times as well, have given the Sivash the name of Foul Sea (Hnile More).
The eastern part of the Ukraine's Black Sea coast is a mountainous cliff-coast again. The plications of the western Caucasus, which approach the sea obliquely, are here so quickly destroyed by the powerful abrasive action of the surf, that the erosive action of the rivers and mountain streams cannot keep pace. Therefore, the crest is difficult of access and only the two harbors of Novorossiysk and Gelendshik offer shelter for ships along this part of the coast. But even this shelter is doubtful, because of the bora-like winds.
As we perceive from this description of the Ukrainian coast, it is not one which would promote navigation among the inhabitants. Lack of harbors, isolation, remoteness from the main lines of the world's traffic, never could have an encouraging effect upon the development of navigation among the Ukrainians. Despite all this, however, they developed very high seafaring qualities in the time of the old Kingdom- of Kiev and later on in the Cossack period, and the present age, too, has brought a revival of the nautical skill of the Ukrainian coast population.
General Survey of the Physical Geography of Ukraine
The Ukrainian Mountain Country
Glancing at the map of the Ukraine, we perceive at once that in this country we should seek in vain for such a variety of surface configuration as is peculiar to Central or Western Europe. In Germany or France there appear in a comparatively small space the most varied landscape — chains of high mountains, central chains of mountains, terrace and hill country, plateaus and plains.
It is different here in our wide Ukraine. One can travel hundreds of miles in any direction without seeing a change in the character of the scenery. The uniformity which is typical for Eastern Europe is peculiar also to the Ukraine. But not to the extent that it is to Great Russia, where the endlessness of the flat country wearies the eye of the traveler. For there are in the Ukraine landscapes of high and central chains of mountains, picturesque hill districts and richly cut plateaus, marshy plains and steppes strewn with barrows. There is, then, in the Ukraine, a variety of surface configuration, but on a large scale, not as in Western or Central Europe, confined in a small space.