The Falls of Niagara and Other Famous CataractsHolley, George W. (George Washington)
History
The Falls of Niagara and Other Famous Cataracts
Holley, George W. (George Washington)
Niagara Falls (N.Y. and Ont.) -- Description and Travel; Niagara River (N.Y. and Ont.) -- History; Waterfalls
Thus it appears that the rate suggested was the result of a conjecture
founded on a guess. From certain oral and written statements which we
have been able to collect, we have made an estimate of the time which
was required to excavate the present chasm-channel from Lewiston upward.
During the last hundred and seventy-five years certain masses of rock
have been known to fall from the water-covered surface of the cataract,
and a statement as to the surface-measure of each mass was made. In
using these data it is supposed that each break extended to the bottom
of the precipice, although the whole mass did not fall at once. Of
course, the substructure must have worn out before the superstructure
could have gone down. Father Hennepin says that the projection of the
rock on the American side was so great that "four coaches" could "drive
abreast" beneath it. Seven years later, Baron La Hontan, referring to
the Canadian side, says "three men" could "cross in abreast." We cannot
assign less than twenty-four feet to the four coaches moving abreast.
The projection on the Canadian side has diminished but little, whereas
the overhang on the American side has almost entirely fallen, as is
abundantly shown by the huge pile of large bowlders now lying at the
foot of the precipice. Authentic accounts of similar abrasions are the
following: In 1818, a mass one hundred and sixty feet long by sixty feet
wide; and later in the same year a huge mass, the top surface of which
was estimated at half an acre. If this estimate was correct, it would
show an abrasion equivalent to nearly one foot of the whole surface of
the Canadian Fall. In 1829 two other masses, equal to the first that
fell in 1818, went down. In 1850 there fell a smaller mass, about fifty
feet long and ten feet wide. In 1852, a triangular mass fell, which was
about six hundred feet long, extending south from Goat Island beyond the
Terrapin Tower, and having an average width of twenty feet. Here we have
approximate data on which to base our calculations. In addition to
these, it is supposed that there have been unobserved abrasions by
piecemeal that equaled all the others. Combining these minor masses into
one grand mass and omitting fractions, the result is a bowlder
containing something more than twelve million cubic feet of rock. If
this were spread over a surface one thousand feet wide and one hundred
and sixty feet deep--about the average width and depth of the Falls
below the ferry--it would make a block about seventy-eight feet thick.
This, for one hundred and seventy-five years, is a little over five
inches a year. At this rate, to cut back six miles--the present length
of the chasm--would require nearly sixty thousand years, or ten thousand
years for a single mile, a mere shadow of time compared with the age of
the coralline limestone over which the water flows. So, if this estimate
is reasonably correct, two millenniums will be exhausted before
Professor Tyndall's prophecy can be fulfilled.
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