GEOLOGICAL TIME.

Many ingenious calculations have been made to approximate the dates

of certain geological events; but these, it must be confessed, are

more amusing than instructive. For example, so many inches of silt are

yearly laid down in the delta of the Mississippi--how many centuries

will it have taken to accumulate a thickness of 30, 60, or 100 feet?

Again, the ledges of Niagara are wasting at the rate of so many feet

per century--how many years must the river have taken to cut its way

back from Queenstown to the present Falls? Again, lavas and melted

basalts cool, according to the size of the mass, at the rate of so many

degrees in a given time--how many millions of years must have elapsed,

supposing an original igneous condition of the earth, before its crust

had attained a state of solidity? or further, before its surface had

cooled down to the present mean temperature? For these and similar

computations, the student will at once perceive we want the necessary

uniformity of factor; and until we can bring elements of calculation as

exact as those of astronomy to bear on geological chronology, it will

be better to regard our “eras” and “epochs” and “systems” as so many

terms, indefinite in their duration, but sufficient for the magnitude

of the operations embraced within their limits.--_Advanced Textbook of

Geology, by David Page, F.G.S._

M. Rozet, in 1841, called attention to the fact, that the causes which

have produced irregularities in the structure of the globe have not yet

ceased to act, as is proved by earthquakes, volcanic eruptions, slow

and continuous movements of the crust of the earth in certain regions,

&c. We may, therefore, yet see repeated the great catastrophes which

the surface of the earth has undergone anteriorly to the historical

period.

At the meeting of the British Association in 1855, Mr. Hopkins excited

much controversy by his startling speculation--that 9000 years ago

the site on which London now stands was in the torrid zone; and that,

according to perpetual changes in progress, the whole of England would

in time arrive within the Arctic circle.

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