The Knickerbocker, Vol. 22, No. 3, September 1843

Transcriber's note: The following Table of Contents has been added for the convenience of the reader.
Vol. XXII. SEPTEMBER, 1843. No. 3.
'There's nothing great or bright, thou glorious Fall! Thou may st not to the fancy's sense recall.' Morpeth.
Numbers have labored to describe this imposing spectacle, but no pen can exhaust the subject, or do full justice to its grandeur. It is great, indescribable, mighty; and the sensations it produces are indefinite, confused, and wholly unlike and above the emotions raised by other scenes and other causes. It would be presumption to offer a description; although the image of the passing moment is so deeply fixed in the mind, that all else can be dismissed at pleasure, and the imagination conduct us, as often as we will, to a seat on Table-Rock where we can again see the dashing waters roll up in billows above the verge, then gliding over, literally tumble into myriads of particles before they are lost in the rising spray.
One idea impressed me strongly, while enjoying this triumph of Nature's eccentricities; that the Canada Fall was to the American as Great Britain to the United States. Both of the same majestic pattern, equally lofty, created by the same stream, and side by side; but the former more powerful, more irresistible, more overwhelming; while the latter possesses another kind of beauty, less angry, less furious, less threatening, but yet grand and magnificent, and, take away the other fall, incomparable.
Undoubtedly in ages past this mighty tide rolled over in an unbroken sheet; but having worn away in a slow retreat to its present position, a rock unyielding and immovable separated the stream into two unequal divisions; and, judging from the past, the future would seem to forewarn changes equally great. The Canada Fall, however, can gain nothing by the wearings of time. It can have no larger proportion, no higher ledge; but on the other hand, some shifting rock, some rupture in the bed of the river above, may direct the larger share into the American channel, and the relative character of the two be reversed.