Stellar Evolution and Its Relations to Geological TimeCroll, James
Science
Stellar Evolution and Its Relations to Geological Time
Croll, James
Cosmogony; Geological time; Stars -- Evolution
“The major axes of these orbits may be assumed to be not very diverse,
and we may further assume that, to begin with, one set will preponderate
over the rest. Their elliptic paths may throw the periastron passage to
a considerable distance from the common centre of gravity; and if we
assume that the meteorites with this common mean distance are moving in
all planes, and that some are direct and some retrograde, there will be
a shell in which more collisions will take place than elsewhere. _Now,
this collision surface will be practically the only thing visible, and
will present to us the exact and hitherto unexplained appearance of a
planetary nebula—a body of the same intensity of luminosity at its edge
and centre—thus putting on an almost phosphorescent appearance._
“If the collision region has any great thickness, the centre should
appear dimmer than the portion nearer the edge.
“Such a collision surface, as I use the term, is presented to us during
a meteoric display by the upper part of our atmosphere.”[13]
[Footnote 13: _Proc. of Royal Society_, vol. xliv. p. 5.]
_Spheroidal nebulæ_, he considers, are produced by the rotation of what
was at first a globular rotating swarm of meteorites.
_Cometic nebulæ_ are explained, he considers, “on the supposition that
we have either a very condensed swarm moving at a very high velocity
through a sheet of meteorites at rest, or the swarm at rest surrounded
by a sheet, all moving in the same direction.”
In an able and interesting work, which seems almost utterly unknown in
England,[14] Professor Winchell has advanced views similar to those of
Tait and Lockyer regarding the nature and origin of nebulæ. But he, in
addition, discusses the further question of the origin of those swarms.
I shall have occasion to refer to Professor Winchell’s views more fully
when we come to the consideration of the pre-nebular condition of the
universe.
[Footnote 14: _World Life, or Comparative Geology_, by Alexander
Winchell, LL.D., Professor of Geology and Palæontology in the University
of Michigan. Chicago: S. C. Griggs & Co. 1883.]
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