The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
So far we have spoken of only a single planet; let us now suppose that a
second planet, B, is also to move in revolution about the same sun. This
planet may be as great as A, or bigger, or smaller, but we shall still
assume that both planets are inconsiderable in comparison with S. We may
assume that B revolves at the same distance as A, or it may be nearer,
or further. The orbit of B might also have been in the same plane as A,
or—and here is the important point—it might have been in a plane
inclined at any angle whatever to the orbit of A. The two planes might,
indeed, have been perpendicular. No matter how varied may be the
circumstances of the two planets, the sun would accept the control of
each of them; each would be guided in its own orbit, whether that orbit
be a circle, or whether it be an ellipse of any eccentricity whatever.
So far as the attraction of the sun is concerned, each of these planets
would remain for ever in the same plane as that in which it originally
started. Let us now suppose a third planet to be added. Here again we
may assume every variety in the conditions of mass and distance. We may
also assume that the plane which contains the orbit of this third planet
is inclined at any angle whatever to the planes of the preceding
planets. In the same way we may add a fourth planet, and a fifth; and in
order to parallel the actual circumstance of our solar system, so far as
its more important members are concerned, we may add a sixth, and a
seventh, and an eighth. The planes of these orbits are subjected to a
single condition only. Each one of them passes through the centre of the
sun. If this requirement is fulfilled, the planes may be in other
respects as different as possible.
In the actual solar system the circumstances are, however, very
different from what we have represented in this imaginary solar system.
It is the most obvious characteristic of the tracks of Jupiter and
Venus, and the other planets belonging to the sun, that the planes in
which they respectively move coincide very nearly with the plane in
which the earth revolves. We must suppose all the orbits of our
imaginary system to be flattened down, nearly into a plane, before we
can transform the imaginary system of planets I have described into the
semblance of an actual solar system.
If the orbits of the planets had been arranged in planes which were
placed at random, we may presume they would have been inclined at very
varied angles. As they are not so disposed, we may conclude that the
planes have not been put down at random; we must conclude that there has
been some cause in action which, if we may so describe it, has
superintended the planes of these orbits and ordained that they should
be placed in a very particular manner.
Public-domain text, read in full here on John Shaqi.
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