A General History and Collection of Voyages and Travels — Volume 15 - Forming A Complete History Of The Origin And Progress Of Navigation, Discovery, And Commerce, By Sea And Land, From The Earliest Ages To The Present Time by Robert Kerr
page 42 of 713 (05%)
page 42 of 713 (05%)
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united the coast at the very point we had seen, and taken the bearing
of, the day we first came in with it, and proved to a demonstration that this land, which we had taken for part of a great continent, was no more than an island of seventy leagues in circuit. Who would have thought that an island of no greater extent than this, situated between the latitude of 54° and 55°, should, in the very height of summer, be in a manner wholly covered, many fathoms deep, with frozen snow, but more especially the S.W. coast? The very sides and craggy summits of the lofty mountains were cased with snow and ice; but the quantity which lay in the valleys is incredible; and at the bottom of the bays the coast was terminated by a wall of ice of considerable height. It can hardly be doubted that a great deal of ice is formed here in the water, which in the spring is broken off, and dispersed over the sea; but this island cannot produce the ten-thousandth part of what we saw; so that either there must be more land, or the ice is formed without it. These reflections led me to think that the land we had seen the preceding day might belong to an extensive track, and I still had hopes of discovering a continent. I must confess the disappointment I now met with did not affect me much; for, to judge of the bulk by the sample, it would not be worth the discovery. I called this island the isle of Georgia, in honour of his majesty. It is situated, between the latitudes of 53° 57' and 54° 57' S.; and between 38° 13' and 35° 34' west longitude. It extends S.E. by E. and N.W. by W., and is thirty-one leagues long in that direction; and its greatest breadth is about ten leagues. It seems to abound with bays and harbours, the N.E. coast especially; but the vast quantity of ice must render them inaccessible the greatest part of the year; or, at least, it must be dangerous lying in them, on account of the breaking up of the |
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