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Pennsylvania Geology Final Report Volume 1 1981

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6 GEOLOGICAL SIJRVEY OF PENNSYLVANIA.<br />

explaining the comparative quietness, or the comparative<br />

commotion of tlie age of each. Going backward in time<br />

and downward through the rocks, he is compelled to give<br />

time-names as well as mineral-names to the formations or<br />

of beds which he describes. But his time-names<br />

groups<br />

can only be comparative, such as new and old, newer and<br />

older, recent, ancient and archaic. Andihis mineral-names<br />

also can only be : comparative uj)per, middle and lower.<br />

These terms, however, can present no well-defined idea to<br />

an}^ mind but that of a geologist, for they are the terms in<br />

daily use among men for events which run their course in<br />

a few days, or years, or centuries of human time, or for<br />

things which are measurable by inches, yards or miles in the<br />

country where those who use them live. A single one of<br />

the principal rock formations of <strong>Pennsylvania</strong> required<br />

more time for its deposit than the duration of the human<br />

race from its first appearance on the planet until now. The<br />

age of our primeval forest can hardly compare with the age<br />

which one large coal bed reached before its life was destroj^ed<br />

by the invasion of the overl jdng sands. If the limestone<br />

dej^osits of the Cumberland valley could be measured not<br />

by feet and yards but by years and centuries, and compared<br />

with events of human history, we should merely get<br />

a vague notion of enormous time, expressed by the old<br />

phrase "a thousand years is as a single day."<br />

Nevertheless, however ineffectual will prove the effort to<br />

frame a clear idea of the whole course of geological time, or<br />

even to define with any distinctness its major sub-divisions,<br />

it is absolutely indispensable for the understanding of the<br />

geology of any region to suspend our habitual estimates of<br />

human events, and substitute for them the largest possible<br />

conceptions of geological time, upon the grandest scale<br />

which we are capable of imagining.<br />

To the human individual who seldom lives beyond threescore<br />

years and ten, and whose short life is crowded with<br />

business affairs, time is considered a precious commodity to<br />

be spent with economy, its loss and its waste lamented, and<br />

its use converted into a religious duty.<br />

But these ideas are products of the latest age of human<br />

1<br />

I

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