The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
As those two bodies met they would possess a certain moment of momentum,
and this moment of momentum would remain for ever unaltered, no matter
what may be the future vicissitudes of the system.
For the sake of simplicity in describing what has occurred, we have
spoken as if the two bodies were of equal mass, and, moving with equal
velocities from opposite points of the heavens, dashed into collision.
But what actually happens cannot have been quite so symmetrical. There
is one feature in the solar system which absolutely proves that the
collision cannot have taken place precisely in the way we have laid
down. If it had happened that two equal masses had been hurled into
collision with equal velocities from precisely opposite directions, then
there could have been no resultant moment of momentum. From the
principle of the conservation of moment of momentum, we can see that, if
absent in the beginning, it could never originate later. As, however, we
have a large moment of momentum in the movements of the planets and the
sun, it is certain that the collision cannot have taken place in a
manner quite so simple.
[Illustration: Fig. 53.—CLUSTER WITH STARS OF 17TH MAGNITUDE
(n.g.c. 6705; in Antinous).
(_Photographed by Dr. Isaac Roberts, F.R.S._)]
The probabilities of the case show that it is almost infinitely unlikely
that two bodies of equal dimensions, and moving with equal velocities in
opposite directions, should come squarely into collision. It would be
much more likely that the bodies should be not of the same size, not
moving with the same velocity, and should collide partially rather than
squarely. The collision may have been, in fact, little more than a
graze. The probabilities of the case are such as to show that what
actually occurred was a collision between two unequal masses, which were
moving in directions inclined to each other and with different
velocities. It is easy to show that, granted sufficiently great
velocities, an impact which fell far short of direct collision might
still produce enough heat to transform the whole solar system into
vapour.
The circumstances which would naturally accompany so transcendent an
incident will also go far to account for a difficulty which has been
often felt with regard to the evolution of the system from a nebula.
Were such a collision to take place we should certainly not expect that
the resulting nebulous mass, the product of a shock of such stupendous
violence, would be a homogeneous or symmetrical object. Portions of the
colliding body would become more highly heated than others; portions of
the bodies would not be so completely transformed into vapour as would
other parts. There would thus be differences in the nebula at the
different parts of its mass. This non-homogeneity would be connected
with the formation and growth of planets in the different parts of the
nebula.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account