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Tourism is a major economic factor, with millions of visitors coming to view the falls each year. Rainbow Bridge, which was completed in to replace the Falls View Bridge that collapsed inis one of several that cross the river downstream from the falls. Niagara County Community College, part of the State University of New York system, was founded in the city inand Niagara University is situated just outside the city limits. Tuscarora Indian Reservation is about 7 miles 11 km northeast. The falls lie on the border between Ontario, Can. For many decades the falls were an attraction for honeymooners and for such stunts as walking over the falls on a tightrope or going over them in a barrel.
Increasingly, however, the appeal of the site has become its beauty and uniqueness as a physical phenomenon. The falls are in two principal parts, separated by Goat Island. The larger division, adjoining the left, or Canadian, bank, is Horseshoe Falls; its height is feet 56 mand the length of its curving crest line is about 2, feet m. The American Falls, adjoining the right bank, are feet 58 m high and 1, feet m across. The shaping of the Niagara gorge downriver and the maintenance of the falls as a cataract depend upon peculiar geologic conditions.
The rock strata from the Silurian Period to million years ago in the Niagara gorge are nearly horizontal, dipping southward only about 20 feet per mile almost 4 m per km.
An upper layer of hard dolomite is underlain by softer layers of shale. Water exerts hydrostatic pressure and slowly dissolves the dolomite dqting infiltrating joints caused by glaciation and subsequent uplift. Dolomite blocks fall away as water from above also infiltrates and erodes the shale. The disposition of the rock strata provides the conditions for keeping the water constantly falling vertically from an overhanging ledge during a long period of recession movement upstream.