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
frequented than the other; the ladders, properly so called, are strong,
and firmly placed, and none of them, owing to the frequent breaks in the
cliff, are required to be of such a great length but what even a lady
might pass up or down them without fear of danger. To descend over the
rugged rocks, however, the whole way down to the bottom of the cliff, is
certainly no trifling undertaking, and few ladies, I believe, could be
found of sufficient strength of body to encounter the fatigue of such an
expedition.
On arriving at the bottom of the cliff, you find yourself in the midst
of huge piles of mishapen rocks, with great masses of earth and rocks
projecting from the side of the cliff, and overgrown with pines and
cedars hanging over your head, apparently ready to crumble down and
crush you to atoms. Many of the large trees grow with their heads
downwards, being suspended by their roots, which had taken such a firm
hold in the ground at the top of the cliff, that when part of it gave
way the trees did not fall altogether. The river before you here is
somewhat more than a quarter of a mile wide; and on the opposite side of
it, a little to the right, the Fort Schloper Fall is seen to great
advantage; what you see of the Horse-shoe Fall also appears in a very
favourable point of view; the projecting cliff conceals nearly one half
of it. The Fort Schloper Fall is skirted at bottom by milk white foam,
which ascends in thick volumes from the rocks; but it is not seen to
rise above the fall like a cloud of smoke, as is the case at the
Horse-shoe Fall; never the less the spray is so considerable, that it
descends on the opposite side of the river, at the foot of Simcoe’s
Ladder, like rain.
Having reached the margin of the river, we proceeded towards the Great
Fall, along the strand, which for a considerable part of the way thither
consists of horizontal beds of limestone rock, covered with gravel,
except, indeed, where great piles of stones have fallen from the sides
of the cliff. These horizontal beds of rock, in some places, extend very
far into the river, forming points which break the force of the current,
and occasion strong eddies along particular parts of the shore. Here
great numbers of the bodies of fishes, squirrels, foxes, and various
other animals, that, unable to stem the current of the river above the
falls, have been carried down them, and consequently killed, are washed
up. The shore is likewise found strewed with trees, and large pieces of
timber, that have been swept away from the saw mills above the falls,
and carried down the precipice. The timber is generally terribly
shattered, and the carcases of all the large animals, particularly of
the large fishes, are found very much bruised. A dreadful stench arises
from the quantity of putrid matter lying on the shore, and numberless
birds of prey, attracted by it, are always seen hovering about the
place.
[Sidenote: FATE OF AN INDIAN.]
Public-domain text, read in full here on John Shaqi.
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