Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
We learn from Von Buch that the most southern point on the continent of
Europe at which a glacier comes down to the sea is in Norway, in lat.
67° N.[296] But Mr. Darwin has shown, that they extend to the sea, in
South America, in latitudes more than 20° nearer the equator than in
Europe; as, for example, in Chili, where, in the Gulf of Penas, lat. 46°
40' S., or the latitude of central France; and in Sir George Eyre's
Sound, in the latitude of Paris, they give origin to icebergs, which
were seen in 1834 carrying angular pieces of granite, and stranding them
in fiords, where the shores were composed of clay-slate.[297] A large
proportion, however, of the ice-islands seen floating both in the
northern and southern hemispheres, are probably not generated by
glaciers, but rather by the accumulation of coast ice. When the sea
freezes at the base of a lofty precipice, the sheet of ice is prevented
from adhering to the land by the rise and fall of the tide.
Nevertheless, it often continues on the shore at the foot of the cliff,
and receives accessions of drift snow blown from the land. Under the
weight of this snow the ice sinks slowly if the water be deep, and the
snow is gradually converted into ice by partial liquefaction and
re-congelation. In this manner, islands of ice of great thickness and
many leagues in length, originate, and are eventually blown out to sea
by off-shore winds. In their interior are inclosed many fragments of
stone which had fallen upon them from overhanging cliffs during their
formation. Such floating icebergs are commonly flat-topped, but their
lower portions are liable to melt in latitudes where the ocean at a
moderate depth is usually warmer than the surface water and the air.
Hence their centre of gravity changes continually, and they turn over
and assume very irregular shapes.
In a voyage of discovery made in the antarctic regions in 1839, a
dark-colored angular mass of rock was seen imbedded in an iceberg,
drifting along in mid-ocean in lat. 61° S. That part of the rock which
was visible was about 12 feet in height, and from 5 to 6 in width, but
the dark color of the surrounding ice indicated that much more of the
stone was concealed. A sketch made by Mr. Macnab, when the vessel was
within a quarter of a mile of it, is now published.[298] This iceberg,
one of many observed at sea on the same day, was between 250 and 300
feet high, and was no less than 1400 miles from any certainly known
land. It is exceedingly improbable, says Mr. Darwin, in his notice of
this phenomenon, that any land will hereafter be discovered within 100
miles of the spot, and it must be remembered that the erratic was still
firmly fixed in the ice, and may have sailed for many a league farther
before it dropped to the bottom.[299]
Public-domain text, read in full here on John Shaqi.
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