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 New Zealand the marks of the Glacial period are unequivocal The
glaciers which now come down from the lofty mountains upon the South
Island of New Zealand to within a few hundred feet of the sea then
descended to the sea-level. The longest existing glacier in New Zealand
is sixteen miles, but formerly one of them had a length of seventy-eight
miles. One of the ancient moraines contains a boulder from thirty to
forty feet in diameter, and the amount of glacial _débris_ covering the
mountain-sides is said to be enormous. Reports have also been recently
brought of signs of ancient glaciers in Australia.
[Illustration: Fig. 38.--Generalised view of the whole glaciated region
of North America. The area of motionless ground-ice is shown by the white
lines in northern part of Alaska.]
According to Darwin, there are distinct signs of glaciation upon the
plains of Patagonia sixty or seventy miles east of the foot of the
mountains, and in the Straits of Magellan he found great masses of
unstratified glacial material containing boulders which were at least
one hundred and thirty miles away from their parent rock; while upon
the island of Chiloe he found embedded in "hardened mud" boulders which
must have come from the mountain-chains of the continent. Agassiz also
observed unquestionable glacial phenomena on various parts of the Fuegian
coast, and indeed everywhere on the continent south of latitude 37°.
Between Concepcion and Arauco, in latitude 37°, Agassiz observed, near
the sea-level, a glacial surface well marked with furrows and scratches,
and as well preserved, he says, "as any he had seen under the glaciers of
the present day."
[Illustration: Fig. 39.--Quartzite boulder of 45 cubic metres, on Mont
Lachat, 800 metres above the valley of the Belley, in Ain, France
(Falsan).]
CHAPTER VI.
ANCIENT GLACIERS IN THE EASTERN HEMISPHERE.
About two million square miles of northern Europe were covered with
perennial ice during the Glacial period. From the scratches upon the
rocks, and from the direction in which material has been transported,
it is evident that the main centre of radiation is to be found in the
mountains of Scandinavia, and that the glaciers still existing in Norway
are the lineal descendants of those of the great Ice age.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account