Geological facts; or, the crust of the earth, what it is, and what are its usesBarrett, W. G. (William Garland)
Religion
Geological facts; or, the crust of the earth, what it is, and what are its uses
Barrett, W. G. (William Garland)
Geology
Here, again, we may anticipate future remarks. It may be thought—by some
it has been roundly asserted—that these _fossils were placed in their
present situations by the deluge_. Without entering into the theological
question, as to the universality or partiality of the Noachian flood,
although, as we shall hereafter see, there is but one opinion on that
subject held by our best geologists, namely, that the deluge recorded in
the Bible was simply the subsidence or submerging of so much of the
earth, _and no more_, as was then inhabited by man, and that so partial
and so limited was its character, and so brief its duration, compared
with those vast geological epochs we have been considering, that there
are no traces in nature of that event at all, _i.e._ that we have no one
single fossil that can be referred to that event,—without, we repeat,
entering upon the investigation of this subject, which will be done in a
subsequent part of this volume, we would merely remark, in reply to this
absurd notion, that the Wealden is evidently an _alluvial_, and not a
_diluvial_ formation; and as these terms are so frequently used as if
they were synonymous, we shall venture upon our old habit of
explanation. An _alluvial_ deposit is formed by the _ordinary_, but a
_diluvial_ deposit by the _extraordinary_ action of water. Thus all the
straths and carses of Scotland, and our English dales or dells, (may not
the remote etymology be _delta_?) are all of alluvial formation; while,
as owing their origin to diluvial, or the violent action of water, we
are to ascribe the heaps of rubbish, gravel, sand and boulders, that are
found in firm compact together.
Thus, if we take a basin of water holding a quantity of earthy matter in
solution, and place it on a quiet table, and allow the earthy matter
gradually to subside, that which is found at the bottom of the basin is
an _alluvial_ formation, deposited by the quiet and ordinary action of
water.
But when, as sometimes here in Royston, a sudden and heavy rain occurs,
when for a while “the windows of heaven” seem opened, and the
surrounding hills pour down their rushing streams through the town,
filling, as unfortunately they do on such occasions, the cellars of our
neighbours in the bottom of the town, with sticks, stones, flint,
gravel, bits of chalk, paper, bones, cloth, and a variety of
intermingled sundries too numerous to mention, and all huddled together
in wild confusion, then is formed in such ill-fated cellars a _diluvial_
deposit, occasioned by the extraordinary action of water.
Public-domain text, read in full here on John Shaqi.
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