About this waterfall.

About Beamer Falls

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Waterfalls get closed when people are injured or ruin lands.

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A very beautiful waterfall that is perhaps underappreciated. This waterfall is an interesting example of the washboard form. The river falls over a thick sequence of thin layers, probably shales and limestone interbedded with one another.

Some visitors have found a way to carefully but safely access the gorge below. There is a dirt path, and a spot where the vertical rock cliff is only about a meter high. This offers a short rock 'step ladder' to the trail below. Anyone choosing to use this route does so at their own risk. Anyone that cannot find this safe spot with certainty should not attempt to enter the gorge.

This waterfall is featured in the 'Waterfalls of Ontario' book. Please pick up a copy to learn more. This helps to support this project. NOTE: There are no safety railings at this waterfall. Anyone that chooses to visit does so at their own risk. The green stars are to indicate that you can see the falls easily. Getting to the base of the falls arguably requires yellow stars, although many people do it safely.

Some Key Facts
Region Greater Toronto
County Niagara
Near Grimsby
Watercourse Forty Mile Creek
Watershed / % Lakes 2 / 10%
Ownership Niagara Conservation
Landscape Rural uncovered
Size Medium
Type Washboard
Modification Natural
Access Easy
Top / Bottom Moderate to view / Moderate to reach
Trail conditions Uneven rock, steep slopes
Hiking Time 2 min
Coordinates 43.1833,-79.574
Parking
43.18277,-79.5731
Site ID WOO.NIA.003
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Finding Beamer Falls

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You could be injured, lost, or die visiting waterfalls. You are responsible for your safety. Learn your Risks and Responsibilities.

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Visiting Beamer Falls


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Waterfalls of Ontario Project

This project has been online since 1999, in print since 2003, and on social since 2011. (See archives: 2003, 2012, 2018). It was the first to inventory and map Ontario's waterfalls for recreational purposes. With your continued help, it grows. Learn more...
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This page last updated on April 20, 2024. Earlier versions can be examined on Archive.org, dating back to 2003.