The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
We must now imagine a globe, not merely two inches in diameter like one
of these little lamps, but a globe 186,000,000 miles in diameter, a
globe so large that the earth’s orbit would just form a girdle round it.
Even if this globe had been exhausted, so that its density was only the
twelve-thousandth part of the ordinary atmospheric density, it would
still contain more material than is found in the sun in heaven. Thus our
reasoning has conducted us to the notion of an epoch when the sun—or
rather I should say the matter composing the sun—formed something
totally different from the orb which we know so well. The matter in that
very diffuse state would not dispense light and heat as a sun in the
sense in which we understand the word. However vast might be the store
of energy which it contained—a store indeed thousands of times greater
than our present sun possesses—yet it would hardly be possessed of the
power of effective radiation. It would assuredly not be able to warm and
light a world associated with it, in the same way as the sun now
provides so gloriously for our wants and comfort.
[Illustration: Fig. 21.—THE GREAT COMET OF 1882.
(_Photographed on November 7th, 1882, by Sir David Gill, K.C.B._)]
But it is certain that in those early days there was no earth to be
warmed and lighted. Our globe, even if it can be said to have existed at
all, was truly “without form and void.” At the time when the sun was
swollen into a great globe of gas or rarefied matter, the elementary
substances which were to form the future earth were in a condition
utterly different from that of our present globe. The history of this
earth itself involves another chapter of the argument. Let it suffice to
notice, for the present, that our reasoning has led us to a time when
the sun consisted only of a rarefied gaseous material, and let us give
to the matter in this condition the name which astronomers apply to any
object of a similar character wherever they may meet with it in the
universe. Suppose that we could observe through our telescopes at the
present moment an object in remote space which was like what the sun
must have been at that early stage of its existence which we have been
considering, I do not think that the object would be unfamiliar to
astronomers. There is, indeed, no doubt that there are many objects
visible at this moment, and nightly studied in our observatories, which
are formed of matter just in the same state as the sun was in those
early times. Examined with a good telescope, the object would seem like
a small stain of light on the black background of the sky. The observer
would at once call it a nebula. In these modern days he would probably
apply the spectroscope to it, and this instrument would assure him that
the object he was looking at was a mass of incandescent gas. Such an
object would in all probability not greatly differ from many nebulæ now
known to us.
Public-domain text, read in full here on John Shaqi.
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