The Falls of Niagara and Other Famous Cataracts — John Shaqi
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
ice would descend with crushing force on these rocks. The smaller ones
would be broken, pulverized, and swept down-stream, the channel for the
water would be enlarged gradually, and the larger masses thus partially
undermined. Then the spray and dashing water would freeze and the ice
accumulate upon them until they were toppled over. Then the falling ice
would recommence its chipping labors, and with every piece of ice
knocked off, a portion of the rock would go with it. Finally, as the
cold continued, the master force, the mightiest of mechanical powers,
would be brought into action. The vast quantities of ice pouring over
the precipice would freeze together, agglomerate, and form an
ice-bridge. The roof being formed, the succeeding cakes of ice would be
drawn under, and, raising it, be frozen to it. This process goes on.
Every piece of rock above and below the surface is embraced in a
relentless icy grip. Millions of tons are frozen fast together. The
water and ice continue to plunge over the precipice. The principle of
the hydrostatic press is made effective. Then commences a crushing and
grinding process which is perfectly terrific. Under the resistless
pressure brought to bear upon it, the huge mass moves half an inch in
one direction, and an hundred cubic feet of rock are crushed to powder.
There is a pause. Then again the immense structure moves half an inch
another way, and once more the crumbling atoms attest its awful power.
This goes on for weeks continuously. Finally the temperature changes.
The sunlight becomes potent; the ice ceases to form; the warm rays
loosen the grip of the ice-bridge along the borders of the chasm below.
The water becomes more abundant; the bridge rises, bringing in its icy
grasp whatever it had attached itself to beneath; it breaks up into
masses of different dimensions: each mass starts downward with the
growing current, breaking down or filing off everything with which it
comes in contact. Fearful sounds come up from the hidden depths, from
the mills which are slowly pulverizing the massive rock. The smaller
bits and finer particles, after filling the interstices between the
larger rocks in the bottom of the chasm, are borne lakeward. The heavier
portions make a part of the journey this year; they will make another
part next year, and another the next, being constantly disintegrated and
pulverized.
This work has been going on for many centuries. The result is seen in
the vast bar of unknown depth which is spread over the bottom of Lake
Ontario around the mouth of the river. On the inner side of the bar the
water is from sixty to eighty feet deep, on the bar it is twenty-five
feet deep, and outside of it in the lake it reaches a depth of six
hundred feet.
[Illustration: GREAT ICICLES UNDER THE AMERICAN FALL]
Public-domain text, read in full here on John Shaqi.
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