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ally clotted with ice before he had time to dry it. The hunters described the sensation of handling their guns as similar to that of touching red-hot iron; and so excessive was the pain, that they were obliged to wrap thongs of leather round the triggers to prevent their fingers coming in contact with the steel. Numbers of the Indian inhabitants of the country perish from cold and hunger every year--indeed, it seems wonderful that human beings should attempt to live in such a country; yet much further north, the hardy Esquimaux, subsisting on whale's blubber and seal's flesh, contrives to support life in tolerable comfort. To the south of the Arctic Circle stunted fir-trees begin to appear, and at length grow so thickly, that it is with difficulty a passage can be made amid them. Frequently the explorer has to clamber over fallen trees, through rivulets, bogs, and swamps, till often the difficulties in the way appear insurmountable to all but the boldest and the most persevering. MOUNTAINS. On the western side of the continent rises gradually from the Polar regions the mighty chain which runs throughout its whole length--a distance of altogether 10,000 miles. The northern portion, known as the Rocky Mountains, runs for 3000 miles, in two parallel chains, to the plains of Mexico, flanked by two other parallel ranges on the west,--the most northern of which are the Sea Alps of the north-west coast, and on the southern, the mountains of California. At the north-western end of the Sea Alps rises the lofty mountain of Mount Elias, 17,000 feet in height--the highest mountain in North America--not far from Behring Bay; while another range, the Chippewayan, stretches eastward, culminating in Mount Brown, 10,000 feet in height, and gradually diminishing, till it sinks into insignificance towards the Arctic Circle. Point Barrow is the most northern point of America on the western side. It consists of a long narrow spit, composed of gravel and loose sand, which the pressure of the ice has forced up into numerous masses, having the appearance of rocks. From this point eastward to the mouth of the Mackenzie River the coast declines a little south of east. The various mountain ranges existing on the eastern side of the continent, including the chain of the Alleghanies, form what is called the Appalachian system. It consists of numerous parallel chains, some of which form detached ridges, the whole running from the nor
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