Named for their shape, the 800-m (2,625-ft) wide and 50-m (164-ft) high Horseshoe Falls are formed by the turbulent waters of the Niagara River roaring over a semicircular cliff to plunge into the bubbling cauldron below. By these means the Niagara River adjusts to the differential between the water levels of lakes Erie and Ontario, which it connects. The falls remain an awe-inspiring sight, despite the fact that the flow of the river is regulated by hydroelectric companies, which siphon off a substantial part of the river to drive their turbines. One result has been a change in the rate of erosion. By the 1900s, the falls were eroding the cliff beneath them at a rate of 1 m (3 ft) a year. Today, the rate is down to 30 cm (1 ft) a year.
Horseshoe Falls
Shaped like a horseshoe, this is the larger set of falls at Niagara, being some 670 m (2,200 ft) wide and 57 m (188 ft) high.