Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Whence comes it, then, that there should be so much contrariety
in the solutions of the same problem, that are given by men who
proceed upon the same principles? May not this have been occasioned
by the conditions of the problem never having been all taken
into consideration at once; by which it has remained hitherto
indeterminate, and susceptible of many solutions,--all equally good,
when such or such conditions are abstracted; and all equally bad,
when a new condition comes to be known, or when the attention is
directed to some condition which had been formerly neglected?
_Nature and Conditions of the Problem._
To quit the language of mathematics, it may be asserted, that almost
all the authors of these systems, confining their attention to
certain difficulties which struck them more forcibly than others,
have endeavoured to solve these in a manner more or less plausible,
and have left unnoticed others, equally numerous, and equally
important. For example, the only difficulty with one consisted in
explaining the changes that had taken place in the level of the
sea; with another, it consisted in accounting for the solution of
all terrestrial substances in one and the same menstruum; and with
a third, in shewing how animals that were believed to be natives of
the torrid zone could live in the frigid zone. Exhausting all the
powers of the mind upon these questions, they conceived that they
had done every thing that was necessary when they had contrived some
method of answering them; and yet, while they neglected all the other
phenomena, they did not always think of determining with precision
the measure and limits of those which they had endeavoured to explain.
This is peculiarly the case with regard to the secondary formations,
which constitute, however, the most important and most difficult part
of the problem. During a long time, all that was done with respect
to these, consisted of feeble attempts to determine the order of
superposition of their strata, and the connections of these strata
with the species of animals and plants whose remains they contain.
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