Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
Baron Fourier, after making a curious series of experiments on the
cooling of incandescent bodies, considers it to be proved
mathematically, that the actual distribution of heat in the earth's
envelope is precisely that which would have taken place if the globe
had been formed in a medium of a very high temperature, and had
afterwards been constantly cooled.[210] He contends, that although no
contraction can be demonstrated to have taken place within the
historical period (the operation being slow and the time of observation
limited), yet it is no less certain that heat is annually passing out by
radiation from the interior of the globe into the planetary spaces. He
even undertook to demonstrate that the quantity of heat thus transmitted
into space in the course of every century, through every square metre of
the earth's surface, would suffice to melt a column of ice having a
square metre for its base, and being three metres (or 9 feet 10 inches)
high.
It is at the same time denied, that there is any assignable mode in
which the heat thus lost by radiation can be again restored to the
earth, and consequently the interior of our planet must, from the moment
of its creation, have been subject to refrigeration, and is destined
together with the sun and stars forever to grow colder. But I shall
point out in the sequel (chapter 31) many objections to these views, and
to the theory of the intense heat of the earth's central nucleus, and
shall then inquire how far the observed augmentation of temperature, as
we descend below the surface, may be referable to other causes
unconnected with the supposed pristine fluidity of the entire globe.
CHAPTER IX.
THEORY OF THE PROGRESSIVE DEVELOPMENT OF ORGANIC LIFE AT SUCCESSIVE
GEOLOGICAL PERIODS.
Theory of the progressive development of organic life--Evidence in
its support inconclusive--Vertebrated animals, and plants of the
most perfect organization, in strata of very high
antiquity--Differences between the organic remains of successive
formations--Comparative modern origin of the human race--The popular
doctrine of successive development not established by the admission
that man is of modern origin--Introduction of man, to what extent a
change in the system.
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