Exploring North Dakota’s Mysterious Red Wing Crater: A Geological Wonder
In a state known for its vast plains and thriving oil industry, North Dakota has yet another claim to fame buried beneath its surface—an ancient impact crater, a relic from a time long before the oil rigs dotted the landscape.
Named the Red Wing Crater, this geological marvel has intrigued scientists and sparked wild theories for decades, and it seems that even locals are still uncovering its secrets.
Dating back approximately 200 million years to the Triassic era, the Red Wing Crater was formed when a meteorite collided with what is now McKenzie County, North Dakota, just a stone's throw away from the North Unit of Theodore Roosevelt National Park.
However, unlike some famous craters visible to the naked eye, such as Arizona's Meteor Crater, Red Wing remains hidden beneath layers of Jurassic-era rock, lying approximately 6,000 feet below the surface.
For years, geologists have utilized seismic techniques to detect the presence of this crater, which spans roughly 5 1/2 miles in diameter. What's truly fascinating is that its location coincides with ground zero for North Dakota's oil boom.
As it turns out, there's a curious correlation between impact craters and oil exploration—find a crater of a certain age, and chances are you'll strike oil.
The discovery of the Red Wing Crater has also sparked broader speculation. In 1998, geophysicist David Rowley of the University of Chicago, along with John Spray of the University of New Brunswick and Simon Kelley of Open University, proposed an intriguing hypothesis.
They suggested that Red Wing may be just one of five craters formed in a multiple-impact event.
This hypothesis posits that several celestial objects, possibly fragments of a comet or loosely clustered asteroids, collided with Earth in rapid succession, akin to the famous Shoemaker-Levy impacts on Jupiter in 1994.
Alongside Red Wing, other potential impact sites include Saint Martin crater in Manitoba, Manicouagan crater in northern Quebec, Rochechouart crater in France, and Obolon crater in Ukraine.
Of these, Manicouagan stands out, having formed a distinctive ring-shaped lake. This multiple impact event theory proposes a scenario where these objects, after being captured by Earth's gravitational pull, orbited the planet before crashing down in a series of strikes.
Further evidence for this theory comes from proposed impact sites like Wells Creek, Tennessee, and speculations about additional impacts in prehistoric oceans. However, the validity of Rowley's multiple impact event hypothesis remains a subject of debate among scientists.
While the mystery of the Red Wing Crater and its potential cosmic connections continues to intrigue researchers, it also serves as a reminder of the hidden wonders lurking beneath our feet.
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