The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
The outer circle in Fig. 19 represents the track in which our earth now
revolves around the sun, and we are to understand that the radius of
this circle is about ninety-three million miles. We must imagine that
the innermost of the four circles represents the position of the sun.
Along its track the earth revolves year after year; so it has revolved
for centuries, so it has revolved since the days of the first monarch
that ever held sway in Britain, so it has revolved during all the time
over which history extends, so it has doubtless revolved for illimitable
periods anterior to history. For an interval of time that no one
presumes to define with any accuracy the earth has revolved in the same
track round that sun in heaven which, during all those ages, has
dispensed its benefits of light and heat for the sustenance of life on
our globe.
[Illustration: Fig. 19.—TO ILLUSTRATE THE HISTORY OF THE SUN.
Present orbit of Earth.
Sun in times very much earlier still.
Sun in very early times.
Present Sun.]
The sun appears constant during those few years in which man is allowed
to strut his little hour. The size of the sun and the lustre of the sun
has not appreciably altered. But the sun does not always remain the
same. It has not always shone with the brightness and vigour with which
it shines now; it will not continue for ever to dispense its benefits
with the same liberality that it does at present. The sun is always in a
state of change. It would not indeed be correct to refer to these
changes as growths, in the same sense in which we speak of the growth in
a tree. Decade after decade the tree waxes greater; but the sun, as we
have already explained, does not increase with the time, for the change
indeed lies the other way. It may well be that in this present era the
sun is near its prime, in so far as its capacity to radiate warmth and
brightness is concerned. It is, however, certain that the sun is not now
so large as it was in ancient days. The diminution of the orb is still
in progress. In these present days of its glorious splendour the orb of
day is much larger than it will be in that gloomy old age which destiny
assigns to it.
We have already shown how to give numerical precision to our facts. We
have stated that the sun’s diameter is diminishing at the rate of one
mile every eleven years. We have dwelt upon the remarkable significance
of that shrinkage in accounting for the sustentation of the sun’s heat.
We have now to call on this perennial diminution of the sun’s diameter
to provide some information as to the early history of our luminary.
Public-domain text, read in full here on John Shaqi.
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