Man and the Glacial PeriodWright, G. Frederick (George Frederick)
History
Man and the Glacial Period
Wright, G. Frederick (George Frederick)
Glacial epoch; Prehistoric peoples
In Tierra del Fuego, where the mountains are only from three thousand
to four thousand feet in height and in latitude less than 55°, Darwin
reports that "every valley is filled with streams of ice descending to
the sea-coast," and that the inlets penetrated by his party presented
miniature likenesses of the polar sea.
[Illustration: Fig. 9.--Floating berg, showing the proportions above and
under the water. About seven feet under water to one above.]
_Antarctic Continent._--Of the so-called Antarctic Continent little is
known; but icebergs of great size are frequently encountered up to 58°
south latitude, in the direction of Cape Horn, and as far as latitude
33° in the direction of Cape of Good Hope. Nearly all that is known
about this continent was discovered by Sir J. C. Ross during the period
extending from 1839 to 1843, when, between the parallels of 70° and 78°
south latitude, he encountered in his explorations a precipitous mountain
coast, rising from seven thousand to ten thousand feet above tide.
Through the valleys intervening between the mountain-ranges huge glaciers
descended, and "projected in many places several miles into the sea and
terminated in lofty, perpendicular cliffs. In a few places the rocks
broke through their icy covering, by which alone we could be assured that
land formed the nucleus of this, to appearance, enormous iceberg."[AG]
[Footnote AG: Quoted by Whitney in Climatic Changes, p. 314.]
Again, speaking of the region in the vicinity of the lofty volcanoes
Terror and Erebus, between ten thousand and twelve thousand feet high,
the same navigator says:
"We perceived a low, white line extending from its extreme eastern
point, as far as the eye could discern, to the eastward. It presented
an extraordinary appearance, gradually increasing in height as we got
nearer to it, and proving at length to be a perpendicular cliff of ice,
between one hundred and fifty and two hundred feet above the level of
the sea, perfectly flat and level at the top, and without any fissures
or promontories on its even, seaward face. What was beyond it we could
not imagine; for, being much higher than our mast-head, we could not
see anything except the summit of a lofty range of mountains extending
to the southward as far as the seventy-ninth degree of latitude. These
mountains, being the southernmost land hitherto discovered, I felt
great satisfaction in naming after Sir Edward Parry.... Whether Parry
Mountains again take an easterly trending and form the base to which this
extraordinary mass of ice is attached, must be left for future navigators
to determine. If there be land to the southward it must be very remote,
or of much less elevation than any other part of the coast we have seen,
or it would have appeared above the barrier."
Public-domain text, read in full here on John Shaqi.
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