About this waterfall.

About Coniston Falls Lower

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Waterfalls get closed when people are injured or ruin lands.

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Conniston Falls are comprised of two major drops. The first set falls through a narrow notch in the bedrock, starting right under the bridge. About 30 m downstream is larger, wider falls, still not spectacular, but attractive nonetheless. The bedrock is believed to be quartzite belonging to the Mississagi formation.

NOTE: The lands (and roads) around this site are privately owned by industry, but the area immediately around the creek is crown land. I understand that road access is tolerated by industry, as a way of allowing for recreation at the river. A publicly accessible portage leads from a parking area towards the falls. It is common to see people fishing just downstream on the Wahnapitae River.

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. The uppermost part of the falls, near the bridge poses a particular risk, and visitors must stay back. Anyone that chooses to visit does so at their own risk.

Some Key Facts
Region Northeast
County Sudbury
Near Conniston
Watercourse Conniston Creek
Watershed / % Lakes 2 / 0%
Ownership Crown Land
Landscape Natural, open
Size Small
Type Cascade
Modification Bridge
Access Easy
Top / Bottom Danger / Moderate
Trail conditions
Hiking Time
Coordinates 46.4744,-80.8214
Parking
46.4752,-80.8201
Site ID WOO.SUD.019
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Finding Coniston Falls Lower

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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 Coniston Falls Lower


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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.