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
In all its features and characteristics the great water-course,
including the great lakes, which feeds the Niagara, is peculiar and
interesting. It is more than two thousand miles long; its utmost
surface-sources are scarcely six hundred feet above tide-water; its
bottom, at its greater depth, is more than four hundred feet below
tide-water. In all its course it receives less than two score of
affluents, and only two of these, the St. Maurice and the Saugeen, bring
to it any considerable quantity of water, and no flood in any of them
discolors its emerald surface from shore to shore. Only fierce gales of
wind bring up from its own depths the sediment that can discolor its
whole face. Far the greater portion of its water-supply is drawn from
countless hidden springs, lying deep in the bosom of the earth. In all
the elements of beautiful, picturesque, and enchanting scenery it is
unrivaled.
The rapids of the Niagara just above the Falls, from the Leaping Rock
down through the Witches' Caldron to the edge of the precipice, are
nearly a mile in width, and discharge ten million cubic feet of water
each minute. But for a combination of grandeur and beauty, and for
imparting a sense of almost infinite power, nothing can surpass the
Whirlpool Rapids below the Falls, where the ten million cubic feet of
water are compressed into a tortuous, tumultuous channel, less than four
hundred feet wide.
There are many lesser rapids in the St. Lawrence, from the Thousand
Islands to Montreal, the passage of which in the large lake steamers is
an exciting voyage. The constant changes of scenery at every turn and in
every rood of progress is almost bewildering. Then the alternation of
rapids and broad expanses of river, the bird-like motion as the steamer
sinks and sails down through the rapids, and the sense of relief when it
seems to rise and glide over the smooth river, vary and increase the
excitement. There is developed in one of those expanses a peculiar
geological feature called the Split Rock. The name is strictly accurate.
The descending steamer finds but one narrow channel, a little more than
its own width, through which it can pass in a stream more than half a
mile wide. It lies between the sharp corners of a broad, wedge-shaped
cleavage in an immense rock which, by some convulsion of nature--not by
any abrading process of the elements--has been literally split downward
more than eighty feet. The last crooked and turbulent rapid passed just
before reaching Montreal is the terror of the river pilots, and they
never attempt its passage except by daylight. From Montreal to the Gulf
of St. Lawrence the constantly deepening channel flows with an unbroken
current.
Public-domain text, read in full here on John Shaqi.
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