The Mystery of Devil’s Kettle Falls

If you’ve ever worried that we’ve solved all the mysteries of nature, fear not. Minnesota’s Devil’s Kettle Falls has been puzzling hikers and geologists for generations. At the falls, along Lake Superior’s north shore, a river forks at a rock outcropping. While one side tumbles down a two-step stone embankment and continues on like a normal waterfall, the other side vanishes into a deep hole and disappears—apparently forever.

Devilskettle

The Devil’s Kettle Waterfall. A scary-sounding name for the area’s most mysterious waterfall. Located on the Brule River flowing through Judge C.R. Magney State Park near Hovland, MN, 20 miles north of Grand Marais, MN, the Devil’s Kettle Waterfall has been baffling visitors for decades.  One side of the river rumbles onto a stone embankment and down the rocks. As waterfalls typically do.  The other side, however, flows into a geological wonder known as the Devil’s Kettle, and… disappears?

Well, perhaps not.  The mystery of the Devil’s Kettle Waterfall has been stumping visitors and geologists alike for a number of reasons.  For one, the rock that the Devil’s Kettle formed into is Rhyolite. Rhyolite is formed from a volcanic eruption.  It’s normal to find small kettles in this kind of rock near waterfalls because of the force of the water and the sand and rocks carried by the river flow.  However, the Devil’s Kettle is special in that this isn’t a small, shallow pothole. In fact, the bottom Devil’s Kettle cannot be seen. Its true exit point remains (mostly) unknown.

So how and why the Devil’s Kettle formed the way it did is one mystery. However, the mystery most often discussed when talking about the Devil’s Kettle is where exactly the water goes once it enters the Kettle.

Devils Kettle

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