The Polar World: A popular description of man and nature in the Arctic and Antarctic regions of the globeHartwig, G. (Georg)
History
The Polar World: A popular description of man and nature in the Arctic and Antarctic regions of the globe
Hartwig, G. (Georg)
Antarctica; Arctic peoples; Arctic regions; Natural history
Of all the lands situated either within or near the Arctic Circle none
enjoys a more temperate climate than the Norwegian coast. Here, and
nowhere else throughout the northern world, the birch and the fir-tree
climb the mountain-slopes to a height of 700 or 800 feet above the
level of the sea, as far as the 70th degree of latitude; here we still
find a flourishing agriculture in the interior of the Malanger Fjord in
69°. On the opposite side of the Polar Ocean extends the inaccessible
ice belt of East Greenland; Spitzbergen and Nova Zembla are not 400
miles distant from Talvig and Hammerfest, and yet these ports are never
blocked with ice, and even in the depth of winter remain constantly
open to navigation. What are the causes which in this favored region
banish the usual rigors of the Arctic zone? How comes it that the
winter even at the North Cape (mean temperature +22°) is much less
severe than at Quebec (mean temperature +14°), which is situated 25° of
latitude nearer to the equator?
The high mountain chains which separate Norway from Sweden and Finland,
and keep off the eastern gales issuing from the Siberian wastes, while
its coasts lie open to the mild south-westerly winds of the Atlantic,
no doubt account in some measure for the comparative mildness of
its climate; but the main cause of this phenomenon must no doubt be
sought for in the sea. Flowing into the Atlantic Ocean between Florida
and Cuba, the warm Gulf Stream traverses the sea from west to east,
and although about the middle of its course it partly turns to the
south, yet a considerable portion of its waters flows onward to the
north-east, and streaming through the wide portal between Iceland and
Great Britain, eventually reaches the coasts of Norway. Of course its
warmth diminishes as it advances to the north, but this is imparted to
the winds that sweep over it, and thus it not merely brings the seeds
of tropical plants from Equatorial America to the coasts of Norway, but
also the far more important advantages of a milder temperature.
The soil of Norway is generally rocky and sterile, but the sea amply
makes up for the deficiencies of the land, and with the produce of
their fisheries, of their forests, and their mines, the inhabitants are
able to purchase the few foreign articles which they require. Though
poor, and not seldom obliged to reap the gifts of nature amidst a
thousand hardships and dangers, they envy no other nation upon earth.
Public-domain text, read in full here on John Shaqi.
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