The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
On the village green stands an oak-tree, a veteran which some say dates
from the time of William the Conqueror, but which all agree must
certainly have been a magnificent piece of timber in the days of Queen
Elizabeth. The children play under that tree just as their parents and
their grandparents did before them. A year, a few years, even a
lifetime, may show no appreciable changes in a tree of such age and
stature. Its girth does not perceptibly increase in such a period. But
suppose that a butterfly whose life lasts but a day or two were to pass
his little span in and about this venerable oak. He would not be able to
perceive any changes in the tree during the insignificant period over
which his little life extended. Not alone the mighty trunk and the
branches, but even the very foliage itself would seem essentially the
same in the minutes of the butterfly’s extreme old age as they did in
the time of his life’s meridian or at the earliest moment of his youth.
To the observations of a spectator who viewed it under such ephemeral
conditions the oak-tree would appear steadfast, and might incautiously
be deemed eternal. If the butterfly could reflect on the subject, he
might perhaps argue that there could not be any change in progress in
the oak-tree, because although he had observed it carefully all his life
he could not detect any certain alteration. He might therefore not
improbably draw the preposterous conclusion that the oak-tree must
always have been just as large and just as green as he had invariably
known it; and he might also infer that just as the oak-tree is now, so
will it remain for all time.
[Illustration: Fig. 2.—A FAINT DIFFUSED NEBULOSITY (n.g.c. 1499; in
Perseus).
(_Photographed by Dr. Isaac Roberts, F.R.S._)]
Public-domain text, read in full here on John Shaqi.
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