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
The declivity in the lower channel through the gorge is ninety feet; but
on the surface of the upper banks there is a rise of more than one
hundred feet in the same direction--that is, down the river. Hence, when
the Falls were at Lewiston they were more than two hundred and fifty
feet high. Now the greatest descent is one hundred and sixty-eight feet,
the diminution being the result of retrocession in the line of the
dip--from north-east to south-west--in the bed-rock. It is owing to
this dip that the surface of the water on the American side is ten feet
higher than it is on the Canadian. The continuous column of water,
however, is longest in the center of the Horseshoe, because of the
fallen rock and _débris_ lying at the foot of the other portions of the
Fall. At this time the upward slope of the bed-rock is such that--if it
shall prove to be sufficiently hard--the Falls, after receding four
miles farther, will be two hundred and twenty feet high.
It is evident from the descriptions of Father Hennepin and of Baron La
Hontan, that the upper stratum of rock over which the water falls must
have projected beyond the face of the rock below much farther than it
now does. The large masses of fallen rock lying at the foot of the
American and Horse-shoe Falls are evidence of this fact. Travelers still
go behind the sheet on the Canadian side, and into and through the Cave
of the Winds, on the American side. But they do not expect to keep dry
in so doing, nor to sun themselves on the rocks below, like the
"rattlesnakes" of former days. Nevertheless, there is no more exciting
nor exhilarating excursion to be made at the Falls than that through the
Cave of the Winds.
Nowhere else are the prismatic hues exhibited in such wonderful variety,
nor in such surpassing brilliancy and beauty. And although a rainbow is
not a spraybow, it may be admitted that a spraybow is a rainbow, formed
of drops of water, large or small. So here rainbow dust and shattered
rainbows are scattered around; rainbow bars and arches, horizontal and
perpendicular, are flashing and forming, breaking and reforming, around
and above the visitor in the most fantastic and delightful confusion of
form and effect. And if his fancy prompts him, he may arrange himself as
a portrait, at half or full length, in an annular bow. The enamored
Strephon may literally place his charming Delia in a living, sparkling
rainbow-frame, flecked all over with diamonds and pearls.
CHAPTER III.
The name Niagara--The musical dialect of the Hurons--Niagara one of
the oldest of Indian names--Description of the river, the Falls,
and the surrounding country.
Public-domain text, read in full here on John Shaqi.
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