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
This is a period double what the gravitation theory of the source of the
sun’s energy can afford. And if the rate of denudation be taken at one
foot in 6,000 years, which is, as we have seen, probably nearer the
truth, then this would make the age of the stratified rocks 56,000,000
years.
There seems to be a little ambiguity about Mr. Wallace’s result. Do the
177,200 feet represent the quantity of rock which presently exists, or
do they represent the total quantity which has been formed during all
past ages? If the former, then the 28,000,000 years are but a fraction
of the time which must have been required; for, as we have been shown,
the materials composing the stratified rocks have, on an average, been
deposited at least three or four times over. If, on the other hand, the
thickness is meant to represent the total quantity of rock which has
been formed during the whole of past geological time, then the question
arises, by what means could this quantity possibly be ascertained? In
other words, how was the relation between the present quantity and the
total quantity ascertained? But in either case the result is wholly
irreconcilable with the gravitation theory of the source of the sun’s
heat.
_Method as applied directly._—We have seen that it is impossible to
determine the actual age of the earth from the stratified rocks, even if
we knew with perfect accuracy their present total amount. We have also
seen that from the rate of deposition we cannot fix with any degree of
certainty a minimum value for the age of these rocks. We can, however,
by means of the first or direct application of the method, assign with
tolerable accuracy, as was shown on a former occasion,[33] a minimum age
to the earth. We can be far more certain of the time which must have
been required to remove by denudation, say, a thousand feet of rock than
we can possibly be of the time required to have deposited a thousand
feet of sediment. The thousand feet of sediment may, under certain
conditions, have been deposited in a hundred years, while under other
conditions they may have required a million of years. In fact, nothing
can be more uncertain than the rate of deposition: it depends upon such
a multitude of circumstances. At the mouth of a great river, for
example, a foot of sediment may be deposited in a single day, whereas in
some places, as in mid-ocean, it may require a million of years to
deposit the same amount. But in reference to subaërial denudation no
such uncertainty exists.
[Footnote 33: _Quart. Journ. of Science_, July 1877; _Climate and
Cosmology_, chap. xvii.]
The utter inadequacy of a period of 20,000,000 years for the age of our
earth is demonstrable from the enormous thickness of rock which is known
to have been removed off certain areas by denudation. I shall now
briefly refer to a few of the many facts which might be adduced on this
point.
Public-domain text, read in full here on John Shaqi.
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