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The universal geography : earth and its inhabitants

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Two hundred years ago the navigable channel flowed due east from Astrakhan;3G8RUSSIA IX EUROPE.since then it has shifted continually more to the right, <strong>and</strong> now runs south- southwest.<strong>The</strong> Balda also, which communicates by a side branch with the Akhtuba,has recently acquired considerable proportions at the expense of <strong>its</strong> neighbours,<strong>and</strong> has gradually swallowed up the last vestiges of the famous Baldinskiy convent.<strong>The</strong> bars <strong>and</strong> s<strong>and</strong>-banks, too, are constantly changing their position <strong>and</strong> depth.None of them have more than 7 feet 6 inches of water, <strong>and</strong> the second inimportance had only 18 inches in the summer of 1852. But for the prevailingsouth <strong>and</strong> south-west winds, which drivethe sedimentary matter of the main bedup stream, the Volga would be completely inaccessible. Hence the engineerDanilov now proposes to avoid the delta altogether by constructing a canal fromFig. 195.<strong>The</strong> Volga <strong>and</strong> Akht&ba.Scale 1 : 1,230,000.Tiirovll-.s of S.r.7|Astrakhan to the port of Serebrasovskaya, 114 miles to the south-west, whereoccurs the first deep bay south of the Volga.Without including the shorter windings, the Volga has a total length of2,230 miles, presenting, with <strong>its</strong> tributaries, about 7,200 miles of navigable waters.From the sources of the Kama to the delta, these waters cross sixteen parallelsof latitude, <strong>and</strong> nine isothermal degrees, so that while the mean annual temperatureof the upper region is at freezing point, it oscillates about 9° inthe delta. At Astrakhan the Volga is frozen for about 98 days, <strong>and</strong> atKazan for 152, while the Kama is ice-bound for six months at the junction ofthe Chusovaya above Perm. <strong>The</strong> rainfall of the basin is about 16 inches, whichwould give 700,000 cubic feet per second, were all the moisture to be carried offby the bed of the Volga. But much is absorbed by vegetation in the forests <strong>and</strong>steppes, <strong>and</strong> in the latter region direct evaporation may dissipate about 40 inchesduring the year in tracts fully exposed to the winds. Altogether about threefourthsof the rainfall are thus lost en route, <strong>and</strong> preliminary estimates havedetermined the mean discharge at about 203,000 cubic feet, which is less than two-

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