The Arctic regions and the northern whale-fisheryScoresby, William
History
The Arctic regions and the northern whale-fishery
Scoresby, William
Arctic regions; Whaling -- Arctic regions
A most extraordinary appearance of the Foreland, or Charles’s Island,
Spitzbergen, occurred on the 16th of July, 1814. While sailing to the
southward, along the coast, with an easterly wind, I observed what
appeared to be a mountain, in the form of a slender, but elevated,
monument. I was surprised that I had never seen it before, and
was more astonished when I saw, not far distant, a prodigious and
perfect arch thrown across a valley, of above a league in breadth.
The neighbouring mountains disclosed the cause, by exhibiting an
unnatural elevation with the columnar structure of looming objects.
Presently, the scene was changed, the mountains along the whole coast
assumed the most fantastical forms; the appearance of castles, with
lofty spires, towers, and battlements, would, in a few minutes, be
converted into a vast arch or romantic bridge. These varied, and
sometimes beautiful, metamorphoses naturally suggested the reality
of fairy descriptions; for the air was perfectly transparent; the
contrast of snow and rocks was quite distinct; even in the substance
of the most uncommon phantasms, though examined with a powerful
telescope, and every object deemed to possess every possible
stability. I never before observed a phenomenon so varied or so
amusing. The land was not alone affected by this peculiar refraction,
since every object between the north-east and south-east points of
the compass was, more or less, deformed by it. A mass of ice on
the horizon appeared of the height of a cliff, and the prismatic
structure of its front suggested the idea of basaltic columns. It
may be remarked, that these phenomena took place on a clear evening,
after an uncommonly warm afternoon.
I observed many other peculiar effects of refraction. Such phenomena
are frequent on the commencement or approach of easterly winds,
and are probably occasioned by the commixture, near the surface of
the land or sea, of two streams of air of different temperatures,
so as to occasion an irregular deposition of imperfectly condensed
vapour, which, when passing the verge of the horizon, produced these
appearances.
_Parhelia_, mock suns, and _corona_, haloes, are perhaps not so
frequent in Greenland as in some parts of America. I do not recollect
to have observed them more than thrice. In the first instance, I did
not minutely notice the particulars. I recollect, however, there were
two or three parhelia, and four or five coloured circles, some of
which almost equalled in their colours the brilliancy of the rainbow.
On the second occasion, several parhelia were succeeded by a lunar
halo, together with the aurora borealis, and proved the harbingers
of a tremendous tempest. The last phenomenon of the kind which I
saw, consisted of a large circle of luminous whiteness, passing
through the centre of the sun, in a direction nearly parallel with
the horizon, intersected in various places with coloured circles of
smaller dimensions.
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