Niagara Falls is made up of two regions: the Horseshoe Falls and the American Falls. The Horseshoe Falls are located on the Canadian side, while the American Falls face the United States. These two are separated by Goat Island. Horseshoe Falls is 177 feet tall. The actual falls are actually only 70 feet tall, but the presence of rocks below adds to the effect.

The width of Horseshoe Falls is about 2,600 feet. Its counterpart, American Falls, is only 1,060 feet wide. A small section of these falls, known as Bridal Veil Falls, is located on the US side and is divided from the main falls by Luna Island Falls. The bridal veil name has been given due to its appearance. The actual amount of water varies due to the presence of two hydroelectric plants that draw water from the Niagara River into its reservoirs. His siphon greatly affects the flow of water over the cliff.

The Niagara River is a legacy of the Ice Age. The formation of the Falls began about 18,000 years ago, when the ice sheets of the Niagara River began to flow south into the Great Lake basins. Over the next 10,000 years, Niagara Falls took its present form. The falls are around 177 feet high and spread over a large area. The intensity of the water falling from here amounts to about six million cubic feet per minute over the crest line when the river flow is maximum; but on average 4 million cubic feet per minute of water falls. This intensity makes it the most powerful waterfall in all of North America.

Niagara Falls is not only impressive, but it serves a variety of purposes for the advancement of America. Did you know that these falls are a major source of electricity for Ontario? Yes, Niagara Falls has been a major source of hydroelectric power. Furthermore, they play an important role in America’s tourism and their industrial and commercial purposes cannot be underestimated.

You can easily travel to the falls from upstate New York and if you are staying overnight at one of the Buffalo hotels, you can arrange your transportation to the falls by hotel.