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This page created 7-8-02 by Sara Donaldson |
The Geological thought of Professor Prestwich In designing his textbook, Professor Prestwich faced an interesting dichotomy.
Two basic philosophies competed in his geological world, at a time when
the relatively young science was still struggling to come to terms with
the liberating consequences of the concept of deep time. Thus,
in his Introduction he notes: On the Continent and in America the latter view prevails, but in
this country the theory of uniformity has been more generally held and
taught. His views are a moderate balance between an extreme view of uniformitarianism,
holding to incremental change of such slowness as to be essentially undetectable,
and a wholehearted reliance on special events or catastrophes.
In essence the argument is a geological equivalent to the steady
state versus big bang debate in the recent history of
Physics: The eloquence and ability with which Uniformitarianism has been
advocated, furthered by the palpable objections to the extreme views held
by some eminent geologists of the other school, led in England to its
very wide acceptance. But it must be borne in mind that uniformitarian
doctrines have probably been carried further by his followers than by
their distinguished advocate, Sir Charles Lyell, and also that the doctrine
on Non-uniformity must not be confounded with a blind reliance on catastrophes;
nor does it, as might be supposed from the tone of some of its opponents,
involve any questions respecting uniformity of law, but only those respecting
uniformity of action. I myself have long been led to conclude that the phenomena of Geology,
so far from showing uniformity of action in all time, present an unceasing
series of changes dependent upon the circumstances of the time; and that,
while the laws of Chemistry and Physics are unchangeable and as permanent
as the material universe itself, the exhibition of the consequences of
those laws in their operation on the earth has been, as new conditions
and new combinations successively arose in the course of its long geological
history, one of constant variation in degree and intensity of action. The conclusions that he reaches in the final paragraph are essentially those that underpin modern geological thought. My own thought is that we interpret through time by analogy drawn from the present. Some processes operate at lightning speed, others are incredibly slow: all interact in some way - there are no closed systems. Its a pity that uniformitarianism is such an ugly word!
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