Objective: The purpose of this activity is to analyze the rate of erosion at Niagara Falls. Erosion rates in the past, present, and predicted future will be examined.
Materials Required: Everything that you need for this exercise is included in the on-screen components.
Time Required: approximately 45 minutes
Niagara Falls is the most famous waterfall in the world. It is not the highest waterfall in the world; that honor falls to Angel Falls in Venezuela with a height of 979 m (approximately 3,200 feet and 18 times as high as Niagara). It is, however, the world’s greatest waterfall by volume with approximately 2,800 m3 (6 million cubic feet) of water going over the falls every second during peak daytime tourist hours. It is the combination of flow volume, height, and characteristic shape that makes Niagara Falls such a beautiful waterfall.
Niagara Falls is formed by the Niagara River falling over a large ridge known as the Niagara Escarpment as it flows from Lake Erie to Lake Ontario. People who have not actually been to Niagara Falls are sometimes surprised to discover that Niagara Falls really consists of three separate waterfalls. The American Falls and the much smaller Bridal Veil Falls lie on the American side of the border, while the largest waterfall, the Horseshoe Falls, lies predominantly on the Canadian side of the border. The water flowing over the Horseshoe Falls has been the dominant agent of erosion in the formation of the Niagara River Gorge. For the purposes of this exercise, whenever the term “Niagara Falls” is used, it refers to the primary erosion caused by the current Horseshoe Falls.
Niagara Falls traces its origin to when the Niagara area first became free of ice after the last ice age.
Geologists have determined that Niagara Falls originated 12,500 years ago as meltwater from the retreating glacier began to carve what is today known as the Niagara Gorge. The falls began on the north side of the Niagara Escarpment near the present-day settlements of Queenston (Canadian side) and Lewiston (American side).
By 10,500 years ago, Niagara Falls had eroded to the location of the present-day Niagara Glen.
Use the distance tool to measure the distance that Niagara Falls traveled upstream from its origins 12,500 years ago until it reached Niagara Glen 10,500 years ago.
Changing drainage patterns resulted in Niagara Falls being stalled at Niagara Glen for approximately 5,000 years. About 5,500 years ago, Niagara Falls again began to advance as drainage flow returned to its previous pattern. Niagara Falls has continued to advance to this day. Accurate records about the location of Niagara Falls have been kept for the last several hundred years.
Time Interval | Distance Eroded (meters) | Erosion rate (meters / year) |
1678–1764 | 0.10 | 100 meters / 86 years ≈ 1.2 meters / year |
1764–1819 | 0.05 | 50 meters / 55 years ≈ 0.91 meters / year |
1819–1842 | 0.08 | 80 meters / 23 years ≈ 3.5 meters / year |
1842–1886 | 0.04 | 40 meters / 44 years ≈ 0.91 meters / year |
1886–2005 | 0.05 | 50 meters / 119 years ≈ 0.42 meters / year |
(Note: Actual answers may vary slightly because of accuracy in measurements, and location of the measurements. Answers should, however, be similar to those above and in the correct relative proportion to one another.)
Use the distance tool to measure the shortest distance along the Niagara River from the current location of the falls to the mouth of the river.