A voyage to Spitzbergen: containing an account of that country, of the zoology of the North; of the Shetland Islands; and of the whale fisheryLaing, John (Surgeon)
History
A voyage to Spitzbergen: containing an account of that country, of the zoology of the North; of the Shetland Islands; and of the whale fishery
Laing, John (Surgeon)
Animals -- Arctic regions; Shetland (Scotland) -- Description and travel; Svalbard (Norway) -- Description and travel; Whaling
“The weaker field is crushed with an awful noise: sometimes the
destruction is mutual. Pieces of huge dimensions and weight are not
unfrequently piled upon the top, to the height of twenty or thirty
feet, whilst doubtless a proportionate quantity is depressed beneath.
The view of those stupendous effects in _safety_, exhibits a picture
sublimely grand, but where there is danger of being overwhelmed, terror
and dismay must be the predominant feelings. The whale-fishers at
all times require unremitting vigilance to secure their safety, but
scarcely in any situation, so much as when navigating amidst those
fields. In foggy weather they are particularly dangerous, as their
motion cannot then be distinctly observed. It may easily be imagined,
that the strongest ship can no more withstand the shock of the contact
of two fields, than a sheet of paper can stop a musket ball. Numbers
of vessels, since the establishment of the fishery, have been thus
destroyed. Some have been thrown upon the ice; some have had their
hulls completely torn open; and others have been buried beneath the
heaped fragments of the ice.
“In the year 1804, I had a good opportunity of witnessing the effects
produced by the lesser masses in motion. Passing between two fields
of bay-ice, about a foot in thickness, they were observed rapidly to
approach each other, and before our ship could pass the strait, they
met, with a velocity of three or four miles per hour; the one overlaid
the other, and presently covered many acres of surface. The ship
proving an obstacle to the course of the ice, it squeezed up on both
sides, shaking her in a dreadful manner, and producing a loud grinding,
or lengthened and acute tremulous noise, accordingly as the degree of
pressure was diminished or increased, until it had risen as high as
the deck. After about two hours, the velocity was diminished to a state
of rest; and, soon afterwards, the two sheets of ice receded from each
other nearly as rapidly as they had before advanced. The ship, in this
case, did not receive any injury; but had the ice been only half a foot
thicker, she would probably have been wrecked.
Public-domain text, read in full here on John Shaqi.
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