IX. THE BLACK SEA.

Route Page

82. From Constantinople to Constantza 561

83. From Constantinople to Odessa 563

84. From Odessa to Batum 568

Yalta, 569.

85. From Batum to Constantinople 571

The =Black Sea= (Turk. _Kara Denis_; Russ. _Chornoye More_; p. xxxiv),

the _Pontus Euxinus_ of the ancients, sometimes deserves its name for

the dark-blue hue of its waters, which is markedly different from the

blue of the Mediterranean. Its area, nearly equal to that of the Baltic,

amounts to 163,689 sq. M., without including the 14,519 sq. M. of the

_Sea of Azov_ (p. xxxiv) which is united with the Black Sea by the

narrow Straits of Kertch (p. 570) and separated from the shallow Gulf of

Odessa (p. 564) by the Crimean Peninsula. The basin proper of the Black

Sea is a huge depression, falling away rapidly from its margin to its

centre, where it reaches a depth of ca. 7365 ft. Its flow and ebb are

not perceptible. Owing to the great rivers it receives its surface-water

is but slightly salt (1.8 per cent), but the deep water is more saline

(2.2 to 2.3 per cent). The bottom is coated with black mud impregnated

with sulphuretted hydrogen and is therefore entirely destitute of animal

life. On warm summer nights the phosphorescence of the water is very

observable. As in the Mediterranean, the vessels are often followed by

dolphins.

During almost the whole of summer gentle N. and N.E. winds, with a clear

sky, prevail in the S.W. part of the Black Sea. At other seasons the

wind is very variable. The N.W. and W. winds often bring fog, which

makes the entrance of the Bosporus difficult. In winter and about the

time of the equinox dangerous storms from the S. and S.E. are by no

means rare.

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