Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 2 of 2]Weld, Isaac
History
Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 2 of 2]
Weld, Isaac
Canada -- Description and travel -- Early works to 1800; United States -- Description and travel -- Early works to 1800
greater velocity at that side than it does at the other, as the rapids
above the precipice are strongest there. It is from the center of the
Horse-shoe Fall that arises that prodigious cloud of mist which may be
seen so far off. The extent of the Horse-shoe Fall can only be
ascertained by the eye; the general opinion of those who have most
frequently viewed it is, that it is not less than six hundred yards in
circumference. The island which separates it from the next fall is
supposed to be about three hundred and fifty yards wide; the second fall
is about five yards wide; the next island about thirty yards; and the
third, commonly called the Fort Schloper Fall, from being situated
towards the side of the river on which that fort stands, is judged to
admeasure at least as much as the large island. The whole extent of the
precipice, therefore, including the islands, is, according to this
computation, thirteen hundred and thirty-five yards. This is certainly
not an exaggerated statement. Some have supposed, that the line of the
falls altogether exceeds an English mile. The quantity of water carried
down the falls is prodigious. It will be found to amount to 670,255 tons
per minute, though calculated simply from the following data, which
ought to be correct, as coming from an experienced commander of one of
the King’s ships on Lake Erie, well acquainted in every respect with
that body of water, viz. that where Lake Erie, towards its eastern
extremity, is two miles and a half wide, the water is six feet deep, and
the current runs at the rate of two knots in an hour; but Niagara River,
between this part of Lake Erie and the falls, receives the waters of
several large creeks, the quantity carried down the falls must therefore
be greater than the foregoing computation makes it to be; if we say that
six hundred and seventy-two thousand tons of water are precipitated down
the falls every minute, the quantity will not probably be much
overrated.
[Sidenote: TABLE ROCK.]
Public-domain text, read in full here on John Shaqi.
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