TABLE ROCK.

Table Rock itself is an object of much curiosity. It is an overhanging cliff, extending along the bank to the very junction with the Horseshoe Fall. Its shape and dimensions have been several times changed within the memory and observation of the present generation, and “the oldest inhabitants” remember it as projecting far beyond its present limits. In July, 1818, a mass some thirty or forty feet wide, and about one hundred and sixty feet in length, fell into the bed of the river. In December, 1828, three sections, comprising a very large portion of the overhanging cliff, and extending to the verge of the Horseshoe Fall, broke off and fell with a terrible crash. In the summer of 1829, another large mass separated and fell, and in June, 1850, still another, the latter about 60 feet wide by 200 long. The precipice still hangs far out over the perpendicular, and with these losses in view, the reader can readily imagine its appearance before the action of the elements had robbed it of so much that made it celebrated.

Several other objects of interest are to be seen on the Canada side, which will be mentioned further on in these pages, and we will now proceed to a description of the principal objects of interest immediately connected with the Falls. In crossing the river to the American shore, the visitor has a choice of two methods. He may descend the bank and cross by the ferry, or may go over the New Suspension Bridge. If intending to return, he will do well to go over by the bridge and re-cross by the ferry.