A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
This highly satisfactory conclusion was an orthodox belief of celestial
mechanics until 1853, when Professor Adams of Neptunian fame, with whom
complex analyses were a pastime, reviewed Laplace's calculation, and
discovered an error which, when corrected, left about half the moon's
acceleration unaccounted for. This was a momentous discrepancy, which at
first no one could explain. But presently Professor Helmholtz, the great
German physicist, suggested that a key might be found in tidal friction,
which, acting as a perpetual brake on the earth's rotation, and
affecting not merely the waters but the entire substance of our planet,
must in the long sweep of time have changed its rate of rotation. Thus
the seeming acceleration of the moon might be accounted for as actual
retardation of the earth's rotation--a lengthening of the day instead of
a shortening of the month.
Again the earth was shown to be at fault, but this time the moon could
not be exonerated, while the estimated stability of our system, instead
of being re-established, was quite upset. For the tidal retardation is
not an oscillatory change which will presently correct itself, like the
orbital wobble, but a perpetual change, acting always in one direction.
Unless fully counteracted by some opposing reaction, therefore (as
it seems not to be), the effect must be cumulative, the ultimate
consequences disastrous. The exact character of these consequences was
first estimated by Professor G. H. Darwin in 1879. He showed that tidal
friction, in retarding the earth, must also push the moon out from the
parent planet on a spiral orbit. Plainly, then, the moon must formerly
have been nearer the earth than at present. At some very remote period
it must have actually touched the earth; must, in other words, have been
thrown off from the then plastic mass of the earth, as a polyp buds out
from its parent polyp. At that time the earth was spinning about in a
day of from two to four hours.
Now the day has been lengthened to twenty-four hours, and the moon has
been thrust out to a distance of a quarter-million miles; but the end is
not yet. The same progress of events must continue, till, at some remote
period in the future, the day has come to equal the month, lunar tidal
action has ceased, and one face of the earth looks out always at the
moon with that same fixed stare which even now the moon has been brought
to assume towards her parent orb. Should we choose to take even greater
liberties with the future, it may be made to appear (though some
astronomers dissent from this prediction) that, as solar tidal action
still continues, the day must finally exceed the month, and lengthen out
little by little towards coincidence with the year; and that the moon
meantime must pause in its outward flight, and come swinging back on a
descending spiral, until finally, after the lapse of untold aeons, it
ploughs and ricochets along the surface of the earth, and plunges to
catastrophic destruction.
Public-domain text, read in full here on John Shaqi.
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