Canada -- Description and travel; United States -- Description and travel
The torrent flows briskly out of the long and narrow vault, while some
distance above is the lowest of the series of cataracts--the Sherman
Fall--where the water plunges over a parapet of rock forty feet high
into a huge basin it has worked out. The amber-colored waters boil
furiously in this cauldron. Above the Sherman Fall the stream flows
through rapids, the chasm broadening and the lofty walls rising higher
as the hill-tops are more elevated, mounting to two hundred feet above
the torrent at a lofty point called the Pinnacle. The floor of the
ravine is level, and becomes quite wide, with massive slabs, weighing
tons, resting upon it, showing the power of freshets which bring them
down from above, and will ultimately carry them completely through the
gorge to its outlet, so resistless is the sweep of the raging flood at
such times, when every bound these huge stones make over the rocky
floor causes the neighboring hills to vibrate, the stifled thunder of
their progress being heard above the roar of waters. At the head of
this widened gorge is the High Falls, in a grand amphitheatre, the
cataract broken into parts and combining all the varieties of cascade
and waterfall, being one hundred feet high, and the walls of the chasm
rising eighty feet higher to the surface of the land above, which
keeps on rising as the ends of the limestone strata are surmounted.
The top of this High Fall is another perpendicular wall stretching
diagonally across the chasm, and below it the protruding layers of
rock form a sort of huge stairway. Down this the waters fall in
varying fashion, finally condensing as a mass of whirling, shifting
foam into a dark pool beneath. This splendid cataract is fringed about
with evergreens and shrubbery, for between the dark thin slabs of
limestone are inserted thinner strata of crumbling shale, and these
give root-hold to the cedars and other nodding branches clinging to
the walls of the ravine. The waterfall begins at the top with the
color of melted topaz, and is unlike anything elsewhere seen, for the
hemlocks and spruces of the mountain regions impart the amber hue to
the torrent. Descending, the changing tints become steadily lighter,
until the brown turns to a creamy white, which is finally lost under
the cloud of spray at the foot of the lower stairway slide, while
beyond, the water rushes away black in hue and driving forward almost
as if shot from a cannon.
Public-domain text, read in full here on John Shaqi.
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