Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic MarvelsBuel, James W. (James William)
History
Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic Marvels
Buel, James W. (James William)
United States -- Pictorial works
For some reason or other the temperature gradually fell, and great
glaciers forming in the northern regions, the highlands of Canada and
the Arctic Circles, submerged Northern Europe and reduced Canada and
half of the United States to the present condition of Greenland. Those
who see glaciers to-day can form little idea of the enormous
possibilities of semi-fluid ice. Only in Alaska, where the Muir Glacier
empties itself into the Muir inlet at the rate of seventy feet a day,
can we form any idea of the glacier as a destructive agency. This
glacier empties two hundred million cubic feet of ice into the sea every
day; that is to say, 45,000 tons of ice fall into the water every minute
in avalanches with detonations which sound like the booming of a
cannonnade. The very earth seems to tremble, and the sea boils and foams
with the continual discharge of fresh icebergs. “From observations upon
living glaciers,” says Dr. Wright, “and from the known nature of ice, we
may learn to recognize the track of a glacier as readily and
unmistakably as we would the familiar foot-prints of an animal.” By the
effects of ice-grinding, rocks are smoothed and polished, rounded and
mammillated. They are, moreover, striated. “These may be called glacial
hieroglyphics; glacial deposits are equally distinctive. They are of
three different kinds—ground moraine, terminal moraine, and erratic
bowlders. The heights to which the ice-flood rose are frequently self-
registered on the mountains which once breasted its flow. They serve, in
Dr. Wright’s phrase, as ‘glaciometers.’ Thus it has been learned that
the ice was a mile thick in New England and a couple of thousand feet
thick in Pennsylvania. The date of the close of the Glacial Epoch in the
United States can scarcely, then, be placed earlier than 6,000 B. C. For
it was, we repeat, the withdrawal of the ice that set the chronometer of
the Falls going. The Falls of Niagara, indeed, constitute in themselves,
in Dr. Wright’s apt phrase, ‘a glacial chronometer.’”
[Illustration: TAKU GLACIER, ALASKA.]
It was this tremendous agency of glacial action that gave us Northwest
America as we have it at present. “The inexhaustible fertility of the
Far West is an endowment from vanished glaciers.”
Public-domain text, read in full here on John Shaqi.
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