Straddling the border between Ontario, Canada, and New York, USA, Niagara Falls is not a single cascade but a trio of waterfalls that together form one of the world's most famous natural spectacles.
The falls exist because the Niagara River flows over the Niagara Escarpment, a 100 km (62 mi) cuesta of resistant Silurian limestone and dolomite overlying softer shale. The caprock resists erosion; the shale undercuts, causing the cap to collapse and the falls to retreat upstream—currently ~30 cm/year (slowed by water diversion for hydroelectricity).
~12,000 years ago, the retreating Wisconsin Glacier carved the Niagara Gorge and established the drainage route from Lake Erie to Lake Ontario. The falls were born at the escarpment's edge and have marched south ever since.
Millions visit annually. Experiences include:
Niagara is a green energy giant. The first hydro plant opened in 1895. Today, multiple plants (Sir Adam Beck, Robert Moses) divert ~50-75% of flow (treaty-regulated), generating ~4.9 GW—powering millions of homes in Ontario and New York.
Niagara Falls is both a sublime geological spectacle and an engineered energy asset. Its beauty draws lovers and tourists; its power lights cities. Few places so perfectly unite nature's grandeur with human ingenuity.