The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.Anonymous
Science
The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.
Anonymous
Arctic regions; Arctic regions -- Discovery and exploration -- British
It should be noted, however, that nowhere does the perpetual snow-line
descend to the water’s edge; nowhere has the spell of winter absolutely
crushed the life out of all vegetation. Lichens and grasses, on which
the reindeer gains its hardy subsistence, are found near lat. 80°; even
on the awful plains of Melville Island the snow melts at midsummer;
and the deserts of New Siberia afford food for considerable numbers of
lemmings. As far as man has reached to the north, says a popular and
accurate writer, vegetation, when fostered by a sheltered situation
and the refraction of solar heat from the rocks, has everywhere been
found to rise to a considerable altitude above the level of the sea;
and should there be land at the North Pole, we may reasonably suppose
that it is destitute neither of animal nor vegetable life. It would be
quite wrong to conclude that the cold of winter invariably increases
as we approach the Pole, the temperature of a land being controlled
by many other causes besides its latitude. Even in the most northern
regions visited by man, the influence of the sea, particularly where
favoured by warm currents, considerably mitigates the severity of the
winter, while at the same time it diminishes the heat of summer. On the
other hand, the large continental tracts of Asia or America that slope
towards the Pole, possess a more rigorous winter and a fiercer summer
than many coast lands or islands situated far nearer to the Pole. For
example: the western shores of Novaia Zemlaia, fronting a wide expanse
of sea, have an average winter temperature of only -4°, and a mean
summer temperature which rises very little above the freezing-point of
water (+ 36° 30’); while Yakutsk, situated in the centre of Siberia,
and 20° nearer to the Equator, has a winter temperature of -36° 6’, and
a summer of + 66° 6’.
But though such are the physical conditions of the Polar Regions, it
must not be supposed that Nature wears only a severe and repellent
aspect. There is something beautiful in the vast expanse of snowy plain
when seen by the light of a cloudless moon; something majestic in the
colossal glaciers which fill up the remote Arctic valleys; something
picturesque in the numerous icebergs which grandly sail down the dark
Polar waters; something mysterious and wonderful in the coruscations of
the Aurora, which illuminates the darkness of the winter nights with
the glory of the celestial fires. The law of compensation prevails in
the far North, as in the glowing and exuberant regions of the Tropics.
CHAPTER II.
THE ARCTIC HEAVENS: ATMOSPHERIC AND METEORIC PHENOMENA.
Public-domain text, read in full here on John Shaqi.
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