The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
The speed of the earth as it moves round the sun is more than eighteen
miles a second—that is to say, it is three and a half times the critical
speed of five miles. In virtue of this speed the earth has a
corresponding quantity of energy. To find the equivalent of that energy
it must, as already explained, be remembered that the energy of a moving
body is proportional to the square of its velocity; it follows that the
energy of the earth, due to its motion round the sun, must be almost
twelve times as great as the energy of the earth would be if it moved at
the rate of only five miles a second. But, we have already seen that a
body with the velocity of five miles a second would, in virtue of that
motion, be endowed with a quantity of energy equal to that which would
be given out by the perfect combustion of an equal weight of coal. It
follows, therefore, that this earth of ours, solely in consequence of
the fact that it is moving in its orbit round the sun, is endowed with a
quantity of energy twelve times as great as all the energy that would be
given out in the combustion of a mass of coal equal to the earth in
weight. This may seem an astonishing statement; but its truth is
undoubted. If it should happen that the earth came into collision with
another body by which its velocity was stopped, the principle of the
conservation of energy tells us that this energy, which the earth has in
consequence of its motion, must forthwith be transformed, and the form
which it will assume is that of heat. Such a collision would generate as
much heat as could be produced by the combustion of twelve globes of
solid coal, each as heavy as the earth. We may indeed remark that the
coal-seams in our earth’s crust contain, in virtue of the fact that they
partake of the earth’s orbital motion, twelve times as much energy as
will ever be produced by their combustion.
It can hardly be doubted that such collisions as we have here imagined
do occasionally happen in some parts of space. Those remarkable new
stars which from time to time break out derive, in all probability,
their temporary lustre from collisions between bodies which were
previously non-luminous. But we need not go so far as inter-stellar
space for a striking illustration of the transformation of energy into
heat. In the pleasing phenomena of shooting stars our own atmosphere
provides us with beautiful illustrations of the same principle. The
shooting star so happily caught on Professor Barnard’s plate (Fig. 16)
may be cited as an example.
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CHAPTER VI.
HOW THE SUN’S HEAT IS MAINTAINED.
Public-domain text, read in full here on John Shaqi.
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