Vestiges of the Natural History of CreationChambers, Robert
Science
Vestiges of the Natural History of Creation
Chambers, Robert
Creation; Evolution (Biology)
The earliest stratified rocks contain no matters which are not to be
found in the primitive granite. They are the same in material, but only
changed into new forms and combinations; hence they have been called by
Mr. Lyell, metamorphic rocks. But how comes it that some of them are
composed almost exclusively of one of the materials of granite; the mica
schists, for example, of mica—the quartz rocks, of quartz, &c.? For this
there are both chemical and mechanical causes. Suppose that a river has
a certain quantity of material to carry down, it is evident that it will
soonest drop the larger particles, and carry the lightest farthest on.
To such a cause is it owing that some of the materials of the worn-down
granite have settled in one place and some in another. {52} Again, some
of these materials must be presumed to have been in a state of chemical
solution in the primeval seas. It would be, of course, in conformity
with chemical laws, that certain of these materials would be precipitated
singly, or in modified combinations, to the bottom, so as to form rocks
by themselves.
The rocks hitherto spoken of contain none of those petrified remains of
vegetables and animals which abound so much in subsequently formed rocks,
and tell so wondrous a tale of the past history of our globe. They
simply contain, as has been said, mineral materials derived from the
primitive mass, and which appear to have been formed into strata in seas
of vast depth. The absence from these rocks of all traces of vegetable
and animal life, joined to a consideration of the excessive temperature
which seems to have prevailed in their epoch, has led to the inference
that no plants or animals of any kind then existed. A few geologists
have indeed endeavoured to shew that the absence of organic remains is no
proof of the globe having been then unfruitful or uninhabited, as the
heat to which these rocks have been subjected at the time of their
solidification, might have obliterated any remains of either plants or
animals which were included in them. But this is only an hypothesis of
negation; and it certainly seems very unlikely that a degree of heat
sufficient to obliterate the remains of plants or animals when dead,
would ever allow of their coming into or continuing in existence.
COMMENCEMENT OF ORGANIC LIFE—
SEA PLANTS, CORALS, ETC.
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