Credits: NASA Earth Observatory Image by Lauren Dauphin / University of Rochester Illustration by Julia Joshpe |
About two billion years ago, an impactor hurtled toward Earth, crashing into the planet in an area near present-day Johannesburg, South Africa. The impactor—most likely an asteroid—formed what is today the biggest crater on our planet. Scientists have widely accepted, based on previous research, that the impact structure, known as the Vredefort crater, was formed by an object about 15 kilometers (approximately 9.3 miles) in diameter that was travelling at a velocity of 15 kilometers per second.
But according to new research from the University of Rochester, the impactor may have been much bigger—and would have had devastating consequences across the planet. This research, published in the Journal of Geophysical Research, provides a more accurate understanding of the large impact and will allow researchers to better simulate impact events on Earth and other planets, both in the past and the future.
“Understanding the largest impact structure that we have on Earth is critical,” says Natalie Allen ’20, now a PhD student at John Hopkins University. Allen is the first author of the paper, based on research she conducted as an undergraduate at Rochester with Miki Nakajima, an assistant professor of Earth and environmental sciences. “Having access to the information provided by a structure like the Vredefort crater is a great opportunity to test our model and our understanding of the geologic evidence so we can better understand impacts on Earth and beyond.”