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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