The Irish Penny Journal, Vol. 1 No. 38, March 20, 1841Various
History
The Irish Penny Journal, Vol. 1 No. 38, March 20, 1841
Various
Ireland -- Periodicals
Grand, however, as such floating fields of ice are, they are exceeded in
magnificence by bergs. One of these, Scoresby relates, was one mile in
circumference, fifteen hundred feet square, and a hundred feet above the
level of the sea; so that, allowing for the inequalities of its surface,
he considered its depth in the water seven hundred feet, its total
thickness eight hundred feet, and its weight about forty-five millions of
tons--an enormous mass, capable of transporting at least five millions
of tons of extraneous weight. In number, too, they are as remarkable
as in magnitude: above five hundred were counted by Scoresby from the
mast-head at one time, of which scarcely one was less than the hull of
a ship, about a hundred as high as the ship’s mast, and some twice that
height, or two hundred feet above the surface of the sea; hence in total
thickness about sixteen hundred feet. These, then, it must be admitted,
are mighty engines fitted for the transport of rocks of colossal
magnitude. But in the reasonings of sound philosophy, the apparent
fitness of an object to perform some particular function cannot be
deemed sufficient to establish the reality of its action: further proof
is necessary, either derived from analogy or from positive facts. In
respect to ice-fields, the easiest of observation, it is remarkable that
neither of the Captains Scoresby speaks of having noticed extraneous
matter upon them, unless the expression “heaps of rubbish,” in a passage
of the voyage of Scoresby senior, means rubbish of stones as well as
rubbish of ice. Examples will indeed be quoted from other writers, but
the comparative scarcity of transported matter on the upper surface of
the fields of ice, seems a natural consequence of their mode and place
of formation. Formed in bays or gulfs, some portions of them are broken
off by the violence of the waves at a distance from the shore, and never
therefore come in contact with rocks or stones; whilst others, grounding
in shallow water, encase many in the substance of their lower surface,
although none are seen on the upper.
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