The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
From the Alps gigantic glaciers descended to the lowlands in all
directions. Then the Rhine glacier moved out far beyond the mountains
and joined with the glaciers of Savoy and Dauphiny on the plains of
France, while from the Southern Alps glaciers invaded the fertile
plains of Italy.
Glaciers of similar size and extent descended into the valleys of
the Rhine and Danube. The Pyrenees, some of the higher mountains of
the Spanish plateau, the higher mountains of France, the Apennines,
the Carpathians, the Balkans, the Urals, all had their ice-sheets.
Iceland and the Faroe Islands were buried under ice, and even Corsica
had snowfields and glaciers, some of which were not small.
Nearly one half of North America was buried in ice. Strangely enough,
it was not the whole northern half, but the north-eastern half that
was specially ice-invaded, and, more strangely still, not so much
the mountainous portions, though these were affected, as the plains.
Alaska was largely free from ice except on or about the mountains:
and there was less ice on the western plains than in the valley of
the Mississippi. Much the greater part of the four million square
miles of ice-field lay on the plains of Canada and in the upper
Mississippi valley. The Missouri and Ohio rivers like two great arms
embraced the borders of the ice-fields to which they owe their origin.
We do not propose to examine the several theories which have been
proposed to account for this extraordinary cold, for none is
completely acceptable or accepted, but we may just mention them. Dr.
Croll a century ago suggested that the cold may have been due to
the alterations in the shape of the earth's orbit, alterations which
astronomers tell us take place regularly, though very slowly and at
intervals of millions of years. If so, this glacial period was only
the last of many glacial periods; the traces of the earlier ones
having, however, been for the most part obliterated and destroyed.
Public-domain text, read in full here on John Shaqi.
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