The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
We can now understand the transformation of these buoyant carbon vapours
which soar upwards in the sun. They attain an elevation at which the
fearful intensity of the solar heat has been so far abated by the cold
of outer space that the carbon gas is not permitted to remain any longer
in the form of gas; it must return to the liquid or to the solid state.
In the first stage on this return the carbon gas becomes transformed,
just in the same way as watery vapour ascending from the earth becomes
transformed into the fleecy cloud. Under the influence of its fall in
temperature the carbon vapour collects into a clustering host of little
beads of carbon. This is the origin of the glorious solar clouds. Each
particle of carbon in that magnificent radiant surface has a
temperature, and consequently a power of radiation, probably exceeding
that with which the filament of carbon glows in the incandescent
electric arc. When we consider that millions of millions of square miles
on our luminary are covered with clouds, of which every particle is so
intensely bright, we shall perhaps be able to form some idea of that
inimitable splendour which even across the awful gulf of ninety-three
million miles transmits the indescribable glory of daylight.
We are perhaps at present living rather too close to the period itself
to be able to appreciate to its full extent the greatness of that
characteristic discovery made in astronomy during the century just
closed, to which the present chapter relates. In the early part of the
last century it might have been said—indeed, by a certain very
distinguished philosopher it actually was said—that a limit could be
laid down bounding the possibilities of our knowledge of the heavenly
bodies. It was admitted that we might study the movements of the
different orbs in vastly greater detail than had been hitherto
attempted, and that we might calculate the forces to which those orbs
were submitted. With the help of mathematical analysis we might pursue
the consequences of these forces to their remote ramifications; we might
determine where the various orbs were situated at inimitably remote
periods in the past. We might calculate the positions which they shall
attain at epochs to be reached in the illimitably remote future; we
might discover innumerable new stars and worlds; and we might map down
and survey the distant parts of the universe. We might even sound the
depths of space and determine the distances of the more remote celestial
bodies, much more distant than any of those which have already yielded
their secrets; we might measure the dimensions of those bodies and
determine their weights; we might add scores or hundreds to the list of
the known planets; we might multiply many times the number of known
nebulæ and star-clusters; we might make measurements of many thousands
of double stars; we might essay the sublime task of forming an inventory
of the stars of the universe and compiling a catalogue in which the
Public-domain text, read in full here on John Shaqi.
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