What Scientists Found Beneath the Great Lakes Midcontinent Rift Changes Its Entire History

Discover Tube
Discover Tube

Beneath Lake Superior and the Great Lakes lies the remains of a geological event that almost tore North America apart.

New research is challenging the long-standing idea that the Midcontinent Rift formed mainly through massive crustal faulting. Reanalysis of seismic data suggests that enormous magma intrusions, volcanic loading and basin subsidence may have played a much bigger role than scientists once thought.

In this DiscoverTube investigation, we explore how a 1.1-billion-year-old failed rift evolved, why it stopped before creating a new ocean, and how its buried structure helped shape the landscape beneath Lake Superior.

The rift failed to split the continent.

But it preserved one of North America’s most extraordinary geological records.

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