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The universal geography : earth and its inhabitants

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THE SEA OF AZOV. 429the salt consumed in the empire. According to the dem<strong>and</strong> the Governmentextracts from 100,000 to 400,000 tons yearly from the district.*<strong>The</strong> Sivash, whose contours are in other respects so irregular, is separated fromthe Sea of Azov hy a remarkably regular strip of l<strong>and</strong>, named after the little portof Arabat, at <strong>its</strong> southern extremity. About 70 miles long, <strong>and</strong> varying in breadthfrom 1,800 to 5,800 yards, this singular formation is composed almost entirely ofs<strong>and</strong>, <strong>and</strong>, especially in the north, of argillaceous masses <strong>and</strong> calcareous rocks, whichFig. 22.3. Stkait of Yexi-Kaleh.Scale 1 : 500,000.E.ofRE.of CDepth to 13 Feet. 13 to 26 Feet. 26 Feet <strong>and</strong> upwards._____ 5 Miles.have served as supports for the s<strong>and</strong>y embankments disposed b) - the winds <strong>and</strong>currents along their line from shore to shore. <strong>The</strong> only break is at the northernextremity, where the " Putrid Sea " communicates at present through the Strait ofGenichesk with the Sea of Azov. Even this opening is widened or narrowed withthe direction of the winds <strong>and</strong> the quantity of s<strong>and</strong> brought with the current, either* Yield of the Crimean salines:— 1873, 386,741 tons; 1874, 242,228 tons; 1875, 94,878 tons ; 1876198,037 tons.)

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