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
All ice becomes exceedingly fragile towards the close of the
whale-fishing season, when the temperate air thaws its surface,
and changes its solid structure into a brittle mass of imperfectly
attached columns. Bergs in this state being struck by an axe, for
the purpose of placing a mooring anchor, have been known to rend
asunder, and precipitate the careless seaman into the yawning
chasm; whilst, occasionally, the masses are hurled apart, and fall
in contrary directions with a prodigious crash, burying boats and
men in one common ruin. The awful effect produced by a solid mass,
many thousands, or even millions, of tons in weight, changing its
situation with the velocity of a falling body, whereby its aspiring
summit is in a moment buried in the ocean, can be more easily
imagined than described. Though a blow with an edge-tool on brittle
ice does not sever the mass, still it is often succeeded by a
crackling noise, proving the mass to be ready to burst from the force
of internal expansion, or from the destruction of its texture by a
warm temperature. It is common, when ships moor to icebergs, to lie
as remote from them as their ropes will allow, and yet accidents
sometimes happen, though the ship ride at the distance of a hundred
yards from the ice. In the year 1812, while the Thomas, of Hull,
captain Taylor, lay moored to an iceberg in Davis’s Strait, a _calf_
was detached from beneath, and rose with such tremendous force, that
the keel of the ship was lifted on a level with water at the bow,
and the stern was nearly immersed beneath the surface. Fortunately,
the blow was received on the keel, and the ship was not materially
damaged.
From the deep pools of water found in the summer season on the
depressed surface of some bergs, or from streams running down their
sides, the ships navigating where they abound are presented with
opportunities for watering with the greatest ease and dispatch. For
this purpose, casks are landed upon the lower bergs, filled, and
rolled into the sea; but, from the higher, the water is conveyed by
means of a long tube of canvas, or leather, called a _hose_, into
casks placed in the boats, at the side of the ice, or even upon the
deck of the ship.
Public-domain text, read in full here on John Shaqi.
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