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
Suppose that this catastrophe were to take place. Would that be the
end of all things? No. Out of the fiery mist many millions of miles
across--like one of those great nebulæ which the telescopes reveal
to us--order would be evolved. Two things would at once begin to
happen, since in the Universe nothing stands still. The fiery mist
would be giving out heat all about it, sending out heat-waves as a
fire or a red-hot poker will do. The red-hot poker cools; so, too,
would the fiery nebula. Then the nebula would begin to condense; not
quite in the same way that a cloud of steam does, for it would be
whirling all the time, and its fiery particles would be all trying
to fall inwards, just as anything dropped from our hands tends to
fall towards the centre of the earth. As this whirling mass of gas
condensed some great masses of it would become detached, and would
begin to enjoy separate existences of their own.
Let us imagine, for the sake of argument, that a mass of gas vast
enough, when it condensed, to form the earth itself became detached
from the parent nebula. Suppose we follow its history. At first it
may have been a globe hardly distinguishable from a whirling flame.
In brightness it was like the Sun, and like the Sun, it was covered
with elemental gases. It was, in fact, in its earliest days a sphere
of gas continually giving out heat, and continually cooling, till
from a sphere like the Sun it became a ball like Jupiter. It had
an intermediate stage when its gases were condensing into liquids,
as steam condenses into water; for though the nebula as a whole
was hot it was always travelling through cold space. Gradually the
earth became partly liquid and partly gas. For millions of years it
continued to revolve as a ball of liquid--still cooling--still being
pressed very hard at its central parts by the weight of all the gases
and liquids round it, till at last the first crust of solid matter
began to form on the liquid surface. This crust continued to thicken,
but it was subject to many appalling catastrophes and breakages.
We have already used the occurrence of the tides of the earth as an
instance of the Sun's attraction. The Sun (and the Moon) attract the
waters of the earth, pulling them up towards themselves. So would
they also attract the molten materials of which the early earth was
composed. The liquid mass would be continually surging like a tide
against its wall of solid crust, and the liquid would now and again
burst through. There must have been a time when the thin solid crust
covering the molten interior became, owing to the solidification
and contraction of the crust, much too small to contain the liquid
material. The lava would then break through, and would form huge
craters, not unlike some of those which we see on the Moon. We can
faintly imagine these terrible outbreaks in which the molten tide
rose not thirty or forty feet but many miles high!
Public-domain text, read in full here on John Shaqi.
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