The Cornhill Magazine, Vol. I, January 1860Various
General
The Cornhill Magazine, Vol. I, January 1860
Various
England -- Periodicals; English literature -- Periodicals; Short stories, English -- Periodicals
We left Aberdeen on July 1, 1857; and after a favourable run across
the Atlantic, we made our first acquaintance with the Arctic Seas when
near the meridian of Cape Farewell, by falling in with the drift-wood
annually brought from Arctic Asia by the great current known as the
Spitzbergen current--the shattered and mangled state of these pine
logs bearing evidence of their long water-and-ice-borne drift. This
great Arctic current brings masses of ice from the Spitzbergen seas,
at seasons completely filling up the fiords, harbours, and indentations
on the south coast of Greenland, and often in a pack extending for 100
miles southward of Cape Farewell. A whole fleet of whale ships were,
in June, 1777, beset in lat. 76° north, and nearly in the meridian of
Spitzbergen, and were drifted southward by the current, until one by
one they were crushed. The last and only surviving ship arrived in
October, in latitude 61°, in Davis’ Straits, and the crew escaped to
the land near Cape Farewell, 116 in number, out of 450 men, who only a
few short months before were looking forward to a happy return to their
homes.
Late in the summer, the weather mild and the nights short, and with
steam-power at command, we had no occasion for much anxiety about this
ice, but determined to push direct for Frederickshaab, and with a fair
wind we steered to pass within sight of Cape Farewell. On the night of
the 13th July, we were becalmed, and on the following day we steamed
slowly to the north-westward, amidst countless numbers of sea-birds.
At daylight the coast of Greenland showed out in all its wild
magnificence. Cape Farewell bore north 45° east, distant twenty-five
miles; but from the peculiar formation of the adjacent land the
actual cape is difficult to distinguish. Hitherto we had not seen the
Spitzbergen ice; and we hoped that we might follow the coast round to
Frederickshaab without obstruction; but in the course of the forenoon
a sudden fall in the temperature of the sea, with a haziness in the
atmosphere to the northward, indicated our approach to ice. Straggling
and water-washed pieces were soon met with, and in the evening the
distant murmur of the sea, as it broke upon the edge of ice-floes,
warned us of our being near to a pack.
Public-domain text, read in full here on John Shaqi.
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