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The universal geography : earth and its inhabitants

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TIIK WHITE SEA. 349which it is distinguished by the parallelism of <strong>its</strong> bays <strong>and</strong> estuaries, a salientfeature of North Russian <strong>geography</strong>.<strong>The</strong> White Sea, with an area of from 47,000 to 48,000 square miles, must inrnany respects be considered as a lake, or rather a group of lakes, communicatingwith the Frozen Ocean. <strong>The</strong> narrow entrance rounding the Lapl<strong>and</strong> coast,while changing it to a saline gulf, has preserved <strong>its</strong> independent character in theaspect <strong>and</strong> outlines of <strong>its</strong> shores <strong>and</strong> the relief of <strong>its</strong> bed. Thus the "White Seais deeper than the ocean with which it is now connected, falling from about 170feet at <strong>its</strong> entrance to over 1,000 feet towards the extremity of the K<strong>and</strong>alakshaFig. 184. WbScale 1 : 5,200,000.E. of?.EafG55 to 110Fathoms.___ 50 Miles.Gulf. <strong>The</strong> Gulf of Onega, which, like <strong>its</strong> namesake of the Neva basin, mightalmost be called Lake Onega, is somewhat shallow, being no more than 260 feetdeep, <strong>and</strong> is separated by the Solovetzkiy Isles from the main basin. When theWhite Sea was a lake, like Ladoga <strong>and</strong> Onega, it was probably at a higher levelthan at present, <strong>and</strong> drained to the Polar Sea through a river forming a continuationof the Upper Dvina. But oscillations of level may have caused the sea toburst into the lacustrine basin, converting <strong>its</strong> fluvial outflow into a strait. <strong>The</strong>elevation of the entrance prevents the s<strong>and</strong> <strong>and</strong> mud from being carried seawards,<strong>and</strong> the basin is being slowly filled by the continuous depos<strong>its</strong> of the rivers, so

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