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The universal geography : earth and its inhabitants

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NOVAYA ZEMLYA. 359frequented by the Russian fishers <strong>its</strong> existence was first revealed to the Westafter "Willoughby's voyage in 1553. It was again visited in 1556 by StephenBurrough, who also circumnavigated Waigatch by the two Stra<strong>its</strong> of Yugor <strong>and</strong>Kara, separating it from Russia <strong>and</strong> the southern extremity of Novaya Zemlya.Barents followed, <strong>and</strong> perished here during the hard winter of 1597, <strong>and</strong> in 1871the Norwegian Carlsen discovered in lat. 7G U 7', near the north-east end of thenorthern isl<strong>and</strong>, the house where Barents <strong>and</strong> Heemskerk had wintered two hundred<strong>and</strong> seventy-four years previously.All the objects found in it were collected <strong>and</strong>brought to Holl<strong>and</strong>, <strong>and</strong> the Amsterdam Geographical Society now proposes to raisea monument on a neighbouring headl<strong>and</strong> in honour of the famous navigator.Novaya Zemlya may, on the whole, be considered as a continuation of the Uralrange, with which it is connected by Waigatch <strong>and</strong> the Pae Kkoi chain of likeFig. 1S9.'Waigatch Isl<strong>and</strong> <strong>and</strong> Kara <strong>and</strong> Ycgor Stra<strong>its</strong>.Scale 1 = 2.6K>.0(in.Depth in Fathoms.i to 125. 125 to 230.60 Males.geological formation.<strong>The</strong> connection is interrupted, without being destroyed, bythe two intervening stra<strong>its</strong>, beyond which the system traversesthe entire lengthof Novaya Zemlya, describing an arc 540 miles long, with <strong>its</strong> convex side turnedtowards Spitzbergen. <strong>The</strong> isl<strong>and</strong> is divided into two unequal parts by theMatochkin Shar, a channel some 30 feet deep, skirted by the highest elevationsin the range. Like the Urals themselves, these heights slope gently westwards,<strong>and</strong> abruptly towards the east, a disposition maintained also by the bed of the sea,which shoals gradually on the west <strong>and</strong> dips rapidly on the east side, where theline of 110 fathoms runs close to the shore.B B 2

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