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
Convinced of the fruitlessness of all further efforts, Pachtussow bade
adieu with a sorrowful heart to the coast, which still stretched out
before him in undiscovered mystery, and sailed back again to Archangel
on September 20. Soon after his return he fell ill, and four weeks
later his mourning friends carried him to his grave.
The Arctic Ocean is so capricious that in the following year the
walrus-hunter Issakow, of Kem, who had no discoveries in view, was able
to round without difficulty the north-eastern extremity of Nova Zembla,
but, fearful of encountering the dangers of that dreadful coast, he
almost immediately returned.
During the two winters he spent in Nova Zembla, the steersman Ziwolka
had daily consulted the thermometer, and the result of his observations
gave to the western entrance of Mathew’s Straits a mean annual
temperature of +17°.
Thus Nova Zembla is colder than the west coast of Spitzbergen, which,
although still farther to the north, is more favorably situated with
regard to the winds and currents, and from five to ten degrees warmer
than the high northern parts of Siberia and continental America, which
sustain a comparatively numerous population, while Nova Zembla is
uninhabited. Hence this want, and the circumstance that the vegetation
of these islands scarcely rises a span above the ground, while the
forest region still penetrates far within the confines of the colder
continental regions above mentioned, are to be ascribed not to the
low mean annual temperature of Nova Zembla, but to the unfavorable
distribution of warmth over the various seasons of the year. For
although high Northern Siberia and America have a _far colder_ winter,
they enjoy a _considerably warmer_ summer, and this it is which in
the higher latitudes determines the existence or the development of
life on the dry land. During the winter the organic world is partly
sheltered under the snow, or else it migrates, or it produces within
itself sufficient warmth to defy the cold--and thus a few degrees more
or less at that time of the year are of no material consequence, while
the warmth of summer is absolutely indispensable to awaken life and
determine its development.
Public-domain text, read in full here on John Shaqi.
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