The Outline of Science, Vol. 1 (of 4): A Plain Story Simply ToldThomson, J. Arthur (John Arthur)
Science
The Outline of Science, Vol. 1 (of 4): A Plain Story Simply Told
Thomson, J. Arthur (John Arthur)
Science
Since the earth is slowing down, it follows that it was once rotating
faster. There was a period, a long time ago, when the day comprised only
twenty hours. Going farther back still we come to a day of ten hours,
until, inconceivable ages ago, the earth must have been rotating on its
axis in a period of from three to four hours.
At this point let us stop and inquire what was happening to the moon. We
have seen that at present the moon is getting farther and farther away.
It follows, therefore, that when the day was shorter the moon was
nearer. As we go farther back in time we find the moon nearer and nearer
to an earth rotating faster and faster. When we reach the period we have
already mentioned, the period when the earth completed a revolution in
three or four hours, we find that the moon was so near as to be almost
grazing the earth. This fact is very remarkable. Everybody knows that
there is a _critical velocity_ for a rotating flywheel, a velocity
beyond which the flywheel would fly into pieces because the centrifugal
force developed is so great as to overcome the cohesion of the molecules
of the flywheel. We have already likened our earth to a flywheel, and we
have traced its history back to the point where it was rotating with
immense velocity. We have also seen that, at that moment, the moon was
barely separated from the earth. The conclusion is irresistible. In an
age more remote the earth _did_ fly in pieces, and one of those pieces
is the moon. Such, in brief outline, is the tidal theory of the origin
of the earth-moon system.
The Day Becoming Longer
Public-domain text, read in full here on John Shaqi.
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