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
It will be observed that the theory here begins in the middle of a
process. It begins with the assumption of a mass in the act of
condensing under the influence of gravity. It offers no explanation of
the origin of the mass, or how it came to be in this attenuated state,
or in what condition it existed before the materials began to draw
together. These are, however, inquiries which naturally force themselves
on our attention. If the nebular theory be a true theory of the origin
of the solar system, then this nebulous mass must have had an antecedent
history, and we cannot help feeling the instinctive desire of tracing
the chain of causation farther back. The mind presses towards an
absolute beginning. It is the goal to which it aspires, and no amount of
failure will ever deter it from renewing its efforts. Of recent years a
considerable amount of attention has been devoted to inquiries in this
direction; nearly all of which, it is true, has necessarily been of a
speculative and hypothetical character. But hypothesis, as Mr. Locyker
remarks, is the life-blood of investigation.
The nebular hypothesis is so highly probable as to have gained almost
universal acceptance. In fact, it contains very little of a hypothetical
nature. It is, as Mr. Mill says, “an example of legitimate reasoning
from a present effect to its past cause, according to the known laws of
that cause.” Like the hypothesis of a luminiferous ether, if it is not a
true theory, one would almost think that it deserves to be so.
There seems no reason why inquiries should stop at the point where
Laplace began. The same line of reasoning may yet carry us back into the
pre-nebular region, and perhaps with as great a degree of certainty as
it has done in the nebular; though, no doubt, the farther back we
proceed, the more difficult probably will the inquiry become. But, be
all this as it may, there can be little doubt that the path of
investigation is a legitimate one, and also one which is worthy of being
traced out.
I shall now briefly refer to some of the leading views which have been
expressed in regard to the pre-nebular history of the universe, and
shall afterwards consider the additional light which the theory
discussed in this volume seems to cast on the subject.
The commonly received opinion is that the nebulæ were formed from
ordinary matter existing in a high state of division, and widely
diffused through space. The “cosmical dust,” as it is called, was the
universal “world-stuff,” out of which all things were supposed to be
formed. It is held that in receding backwards in pre-nebular times, the
smaller, more simple, and elementary the materials were. Out of this
primitive cosmical dust, or world-stuff, by aggregation, the materials
became successively larger and more complex. The theory of the origin of
nebulæ, on this principle, has been clearly stated by Professor
Winchell, and I here give a brief outline of his views on the subject.
Public-domain text, read in full here on John Shaqi.
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