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
Then, life still being absent from the earth, the _Oceanic Era_
began. The waters condensed into an ocean over the earth, or else
collected in some great oceanic depression. Lands presently emerged
from it. It was a hot ocean, steaming no doubt, for its temperature
was perhaps about 500° F. Some one may ask--Why, then, did it not
steam away into clouds? The answer is that the atmosphere was still
very heavy in that past era, probably still exerting a pressure
as much as fifty times as great as to-day. The pressure of the
atmosphere at the earth's surface to-day is usually about fifteen
pounds to the square inch. In such circumstances water boils rapidly
away at the temperature of 212° F. But if the water be taken up to
the top of Mont Blanc, where the air pressure is less than that at
the sea-level (or if, which amounts to the same thing, we reduce the
pressure on the water's surface by placing it under the receiver
of an air-pump and partially exhaust the air), it will boil at a
lower temperature than this. If, on the other hand, we increase
the pressure on the surface of the water by any means, such, for
example, as by placing it in a chamber of compressed air, the water
can be heated to a higher temperature without boiling away. In the
bygone era of which we are speaking the pressure of the atmosphere
on the water's surface was 700 lb. or 800 lb. to the square inch;
and therefore it could be heated up to a high temperature without
evaporating rapidly.
Another thing began to happen in those days. All bodies in space
attract one another; the Sun attracts its planets; the planets
attract the Sun and their satellites; and the satellites in their
turn attract the planets. Ages before the earth had a moon these
forces were at work. But the attractions of solid bodies for one
another do not bring about any very perceptible alterations in their
shapes; though if the bodies are spinning they effect slow changes in
their speed of rotation. It is different when the bodies are liquid,
or if they have liquid surfaces. Then the attractions of a sun or
a moon on a planet begin to draw up the waters of the planet and
produce tides. The attraction of the earth would produce tides on
the Moon if an ocean existed there; and, it is suspected, do produce
something resembling tides on the present surface of the Sun.[8] As
soon, therefore, as oceans appeared on the earth the waters began
to ebb and flow in tides. (Another consequence of this constant ebb
and flow was that the friction of these movements began to diminish
the speed of the earth's rotation--just as a string that was placed
round the circumference of a spinning-top would, if constantly
pulled backwards and forwards, gradually help to slow down the top.)
Then oceanic waves and currents would begin to eat a way into the
land that was on their borders, or which was emerging from their
depths. Rivers would begin to arise, and they would carry on the
work of erosion.
Public-domain text, read in full here on John Shaqi.
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