The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.Anonymous
Science
The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.
Anonymous
Arctic regions; Arctic regions -- Discovery and exploration -- British
He carefully examined iron which had passed under the steam-hammer, or
through the rolling-mill; clay and wax were subjected to the hydraulic
press. In all cases he detected signs of cleavage; and hence we are
justified in the inference that the phenomenon is invariably produced
by pressure in all bodies of irregular internal structure. Such is the
result with glacier-ice, from whose mass the air-bubbles introduced
by the snow are gradually expelled. At first of brilliant whiteness,
it assumes, in the parallel layers corresponding to the planes of
cleavage, those beautiful azure tints which characterize the veined
structure. So little has it to do with stratification, that in places
where this is apparent it has given rise to a series of horizontal
lines, while the parallel veinings, in the same masses of ice, are all
inclined at an angle of about 60°.
The tendency to cleavage in compact ice would seem to explain the
regular form of those fragments or detached pieces with which some
parts of the glaciers are covered. Usually they occur as cubes, or
as rectangular parallelopipeds. The Alpine mountaineers name them
_séracs_,--in allusion to their resemblance to certain cheeses
which bear this name, and which are manufactured in rectangular boxes.
They have been found in many parts of a really colossal size, measuring
fifty feet in length, breadth, and depth, and as regular in shape as if
they had been hewn with a chisel.
There are many interesting points connected with the formation and
constitution of glaciers which we should gladly discuss, but we are
confined by our limits to remarks of a general character, and we must
now pass on to speak of the phenomena attendant upon their motion.
No doubt, the traveller who for the first time comes in sight of one
of these huge ice-rivers, and sees the mighty mass apparently rooted
to its valley-bed, solid, unchangeable, adamantine, finds it hard to
believe that it moves onward with a certain and an unresting, though a
gradual progress. It looks like a noble river, suddenly petrified by
some overwhelming force: congealed, as it flowed, in a moment, by some
irresistible spell! Such, indeed, is the conception of the poet:--
“Ye ice-falls! ye that from the mountain’s brow
Adown enormous ravines slope amain....
Torrents, methinks, that heard a mighty voice,
And stopped at once amid their maddest plunge!
Motionless torrents! silent cataracts!”
Public-domain text, read in full here on John Shaqi.
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