About this waterfall.

About Maynard Falls

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This low waterfall is more of a rapids. It doesn't have a lot of height, but is close to 100 m in width. Bedrock does break through the water surface, but only as a scattering of miniature islands. The English River drains out of Maynard Lake through a narrows and then enters Tide Lake. The falls occur at the narrows.

While the drop here is maybe only a couple of metres, the flow through this channel can be quite powerful. This is no surprise, as the river drains over 50,000 square kilometres.

Barney shot this picture in 1963, as he watched his dad Fred Bruns and his friends Joe Loon and Andy Keewatin portage from Tide Lake to Maynard Lake at Maynard Falls.

This site is coded as red because I don't think it can be reached by land. To be clear, examination of Google Maps does show that a primitive road reaches the southwest corner of Maynard Lake. This is just a couple hundred metres from the falls. I have no idea if this road is passable. It leads 30 km north from Secondary Highway 671, and is initially known as Portal Rd. My guess is that this is not passable in anything but a jeep.

If you know anything about this site, and can offer some tips for this website, I'd be happy to hear from you.

Some Key Facts
Region Northwest
County Kenora
Near Maynard Lake
Watercourse English River
Watershed / % Lakes 5 / 1%
Ownership West English River Provincial Park
Landscape Wilderness
Size Medium
Type Rock Rapids
Modification Narural
Access No Land-based Access
Top / Bottom /
Trail conditions Overnight Water Route
Hiking Time
Coordinates 50.3441,-93.9442
Parking
50.3441,-93.9442
Site ID WOO.KEN.013
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Finding Maynard Falls

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Visiting Maynard 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.