Two famous Arizona landmarks, the Grand Canyon and Meteor Crater, may have a surprising link. New research from the University of Arizona and the University of New Mexico suggests a meteorite impact could have caused significant geological changes in the region.
According to a study published in the journal Geology, the meteor that formed Meteor Crater over 56,000 years ago might have triggered a massive landslide. This landslide may have blocked the Colorado River, creating an ancient lake that stretched 50 miles and reached depths of around 300 feet.
Chris Baisan, a senior research specialist at the University of Arizona, explains, “It’s crucial to examine how meteor impacts influence our planet. This particular strike might have created a connection to a paleolake in the Grand Canyon that formed around the same time.”
For decades, scientists have puzzled over driftwood and lake sediments found in Stanton’s Cave, located 150 feet above the Colorado River. The central mystery has been: how did that driftwood end up there? Karl Karlstrom, a distinguished professor at the University of New Mexico, pointed out that creating such a lake would have required flood levels ten times greater than any seen in recent history.
Research in the 1980s by Richard Hereford from the U.S. Geological Survey offered early evidence of a rockslide in Nankoweap Canyon, downstream from the cave. This rockslide could have formed the dam that led the driftwood into the cave’s depths. Originally radiocarbon-dated to over 35,000 years, advancements in dating techniques subsequently revealed the driftwood to be about 55,000 years old.
Interestingly, Baisan and co-author Jonathan Palmer, who specializes in ancient dating, stumbled upon a potential link during a visit to Meteor Crater. Palmer noted the age of the impact and wondered if it could relate to the ecological changes observed in the Grand Canyon.
The study posits a strong connection between the meteor’s impact and the formation of the paleolake, providing compelling evidence from multiple locations along the river. Both wood and sediment samples dated to about 55,600 years, reinforcing the researchers’ theory.
The implications of this research are exciting. David Kring, a Meteor Crater Science Coordinator, calculated that the impact would have caused significant ground shaking, possibly reaching magnitudes of 5.4 to 6.0 on the Richter scale. This shaking would have arrived in a matter of seconds, likely triggering the landslide.
While the researchers admit they don’t have conclusive proof, the combination of the meteorite impact, landslide, lake deposits, and driftwood is remarkable. Some experts argue that such catastrophic events are rare but critically important to our understanding of Earth’s geology and history.
In summary, the story of how a meteorite impact shaped landscapes and ecosystems continues to intrigue scientists. Research like this not only deepens our understanding of geological processes but also enhances our appreciation of the dramatic events that have shaped our planet over millennia.
For more detailed insights, check the original research published in Geology here.