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 the spring of 1852 a triangular mass, the vertex of which was just
beyond or south of the Terrapin Tower, while its altitude of more than
forty feet lay along the shore of the south corner of Goat Island, fell
in the night with the usual grinding crash. And with it fell some
isolated rocks which lay on the brink of the precipice in front of the
tower, and from which the tower derived its name. Before the tower was
built, some person looking at the rocks from the shore suggested that
they looked like huge terrapins sunning themselves on the edge of the
Fall. A few days after the fall of the triangular mass, a huge column of
rock a hundred feet high, about fourteen feet by twelve, and flat on the
top, became separated from the bank and settled down perpendicularly
until its top was about ten feet below the surface rock. It stood thus
about four years, when it began gradually to settle, as the shale and
stone were disintegrated beneath it, and finally it tumbled over upon
the rocks below, furnishing an illustration of the manner in which we
suppose the rocks which once accumulated below the Whirlpool must have
been broken down. In the spring of 1871 a portion of the west side of
the sharp angle of the Horseshoe, apparently about ten by thirty feet,
went down, producing a decided change in the curve.
On the 7th day of February, 1877, about eleven o'clock of a cold, cloudy
day, there occurred the most extensive abrasion of the Horseshoe Fall
ever noted. It extended from near the water's edge at Table Rock, more
than half the distance round the curve, some fifteen hundred feet, and
at the most salient angle the mass that fell was from fifty to one
hundred feet wide. By this downfall the contour of the Horseshoe was
decidedly changed, the reëntering angle being made acute and very
ragged. Less than three months afterward the abrasion was continued some
two hundred feet toward Goat Island.
The trembling earth and muffled thunder gave evidence of the immensity
of the mass of fallen rock, but no one saw it go down. For several
months after the fall, until the mass of rock got thoroughly settled in
the bed of the Falls, the exhibition of water-rockets, sent up a hundred
feet above the top of the precipice, was unique and beautiful. The
greatest angle of retrocession, which had previously been wearing toward
Goat Island, is again turning toward the center of the stream.
Public-domain text, read in full here on John Shaqi.
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