Essays: Scientific, Political, & Speculative; Vol. 1 of 3: Library Edition (1891), Containing Seven Essays not before Republished, and Various other Additions.Spencer, Herbert
Philosophy
Essays: Scientific, Political, & Speculative; Vol. 1 of 3: Library Edition (1891), Containing Seven Essays not before Republished, and Various other Additions.
Spencer, Herbert
Philosophy; Political science; Science
Taking for data the appearances of the Earth's crust in a narrow
district of Germany; observing the constant order of superposition of
strata, and their respective physical characters; Werner drew the
inference that strata of like characters succeeded each other in like
order over the entire surface of the Earth. And seeing, from the
laminated structure of many formations and the organic remains contained
in others, that they were sedimentary; he further inferred that these
universal strata had been in succession precipitated from a chaotic
menstruum which once covered our planet. Thus, on a very incomplete
acquaintance with a thousandth part of the Earth's crust, he based a
sweeping generalization applying to the whole of it. This Neptunist
hypothesis, mark, borne out though it seemed to be by the most
conspicuous surrounding facts, was quite untenable if analyzed. That a
universal chaotic menstruum should deposit a series of numerous
sharply-defined strata, differing from one another in composition, is
incomprehensible. That the strata so deposited should contain the
remains of plants and animals, which could not have lived under the
supposed conditions, is still more incomprehensible. Physically absurd,
however, as was this hypothesis, it recognized, though under a distorted
form, one of the great agencies of geological change--the action of
water. It served also to express the fact, that the formations of the
Earth's crust stand in some kind of order. Further, it did a little
towards supplying a nomenclature, without which much progress was
impossible. Lastly, it furnished a standard with which successions of
strata in various regions could be compared, the differences noted, and
the actual sections tabulated. It was the first provisional
generalization; and was useful, if not indispensable, as a step to truer
ones.
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