The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
The nebular theory at once supplies the explanation of the unanimity in
the rotation of the planets, just as it supplied the explanation of the
unanimity in the directions of their revolutions. To explain the
rotation of a planet on its axis, let us imagine that one portion of the
contracting nebula has acquired exceptional density. In virtue of its
superior attraction it absorbs more and more material from the adjacent
parts of the nebula, and this will ultimately be consolidated into the
planet, though in its initial stages this contracting matter will remain
part of the nebula. We have shown that the law which decrees that the
moment of momentum must remain constant will require that, after a
certain advance in the contraction, all the parts of the nebula shall
rotate in the same direction. Thus we find that the sun, or rather the
parts of the nebula that are to form the sun, and the parts that are to
form the planets are all turning round together.
[Illustration: Fig. 51.—AN ELONGATED IRREGULAR NEBULA
(n.g.c. 6992; in Cygnus). (_Dr. W. E. Wilson, F.R.S._)
(_From the Astronomical and Physical Researches at Daramona
Observatory._)]
At this point we may consider a geometrical principle which, though
really quite simple, is not always easily understood. It has indeed
presented considerable difficulty to many people. Suppose that an
ordinary card is laid on a flat board, and that, with a bradawl, a hole
is made through the card into the board. The hole may be at the centre,
or at one of the corners, or a little way in from one of the edges, or
in any other position whatever on the card. Now suppose that a postage
stamp is stuck upon the card anywhere, and that the card is then moved
around the bradawl. How are we to describe the motion of that postage
stamp? It would certainly be revolving around the bradawl; but this
motion we may consider as composed of two others. At any instant we may
accurately represent the movement of the postage stamp by considering
that its centre was moving in a direction perpendicular to the line
joining that centre to the hole made by the bradawl, and that it also
had a rotation around its centre, the period of that rotation being just
the same as the time the card would take to go round the bradawl. Thus
we see that the movement of the postage stamp contains at any moment a
movement of translation and a movement of rotation.
Public-domain text, read in full here on John Shaqi.
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