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
which might be easily broken down, still the new fall would be five feet
higher than the old one. But, so far as can now be discovered, there is
no geological necessity, so to speak, for making any such allowance. In
the new cataract the American Fall would still be the higher, and its
line across the channel nearly straight. The Canadian Fall would
undoubtedly present a curve, but more gradual and uniform than the
present horseshoe.
But there might possibly occur one new feature in the chasm-channel of
the river as the result of future recession. That would be the presence
in that channel of rocky islands, similar to that which has already
formed just below the American Fall. The points at which these islands
would be likely to form are those where the indurated rock of either the
Medina or the Niagara group lies near the surface of the water. This
probably was the case at the narrow bend below the Whirlpool, before
noticed, and from thence up to the outlet of the pool. After considering
what must have occurred in the last case, we may form some opinion
concerning the probabilities in reference to the first.
We can hardly resist the conclusion that masses of fallen rock must have
accumulated below the Whirlpool as we now see them under the American
Fall. But if so, where are they? The answer to this question brings us
to the consideration of the most remarkable phenomenon connected with
this wonderful river. To the beholder it is matter of astonishment what
can have become of the great mass of earth, rock, gravel, and bowlders,
large and small, which once filled the immense chasm that lies below
him. He learns that the water for a mile below the Falls is two hundred
feet deep, and flows over a mass of fallen rock and stone of great depth
lying below it; he sees a chasm of nearly double these dimensions, more
than half of which was once filled with solid rock; he beholds the large
quantities which have already fallen, which are still defiant, still
breasting the ceaseless hammering of the descending flood. For centuries
past this process has been going on, until a chasm seven miles long, a
thousand feet wide, and, including the secondary banks, more than four
hundred feet deep, has been excavated, and the material which filled it
entirely removed. How? By what? Frost was the agent, ice was his delver,
water his carrier, and the basin of Lake Ontario his dumping-ground.
Although there is little likelihood that islands similar to Goat Island
have existed in the channel from Lewiston upward, still it is probable
that, when the Fall receded from the rocky cape below the Whirlpool up
to the pool, it left masses of rock, large and small, lying on the rocky
floor and projecting above the surface of the water. As there were no
islands above, there were no broken, tumultuous rapids. As has been
before remarked, the water poured over in one broad, deep, resistless
flood. When frozen by the intense cold of winter, the great cakes of
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