Niagara Falls and Niagara-on-the-Lake geography and history

The Niagara region is defined by its unique geography, where the Niagara River connects Lake Erie to Lake Ontario, creating a landscape shaped by water, rock, and international borders.

Niagara Falls consists of three distinct waterfalls: the American Falls and Bridal Veil Falls on the United States side, and the Horseshoe Falls, which is situated primarily on the Canadian side. The Horseshoe Falls features a drop of 57 meters and a curved crest approximately 670 meters long. The river cuts through the Niagara Escarpment, a geological formation composed of dolomite, limestone, and other sedimentary rocks. While the rocks themselves are hundreds of millions of years old, the falls were formed approximately 12,000 years ago by glacial meltwater.

Nearby, the town of Niagara-on-the-Lake sits at the mouth of the river where it enters Lake Ontario. The town's layout and historical character, featuring Georgian and British classical architecture from the post-1812 era, are closely tied to its riverside location. The surrounding area is characterized by orchards, vineyards, and agricultural land.