A secondary impact crater discovered in southeast Wyoming.

A secondary impact crater discovered in southeast Wyoming. (Image credit: Kent Sundell/Casper College)

Ricochet from a meteorite impact on Earth created a huge field of craters that have only been seen on other planets.

The site in southeast Wyoming has more than 30 craters that were formed about 280 million years ago, according to a new study. A meteorite impact hundreds of miles away blew boulders of bedrock into the air.

The study leader said that the craters were formed by blocks from a large primary crater.

The history of Earth was shaped by 5 mass extinction events.

There are secondary craters on other planets and moons, but they have never been found on Earth. The area was under scrutiny from the Chinese Chang'e 4 moon lander.

The scientists have identified 31 craters as secondary features.

The zone of craters was thought to have been caused by an asteroid breaking up in mid-air and sending rocks crashing into the ground. The researchers said individual craters ranged in diameter from 10 to 70 meters.

Secondary craters within Von Kármán Crater

Secondary craters within Von Kármán Crater, the Chang'e 4 landing region. (a) The great elliptic circle that linked the center of the Antoniadi Crater to the selected Chang'e 4 landing site. The base image is from the global mosaic obtained by China's Chang'e-2 mission. (b) Secondary craters within the Chang'e 4 landing region that are delivered by the Antoniadi Crater. White arrows mark the secondaries, and the yellow line is the possible trajectory of ejecta launched by the Antoniadi-forming impact. The location of this area is denoted as the white box in (a). The base image is from Japan's Kaguya lunar orbiter. (Image credit: Jun Huang, et al./AGU)

Several of the craters are clustered in small areas, which suggests a different origin story for the features.

The craters appear to be aligned along ray-like patterns, suggesting that they are secondary craters formed by debris flung out around a central, primary crater.

It will be difficult to find the source crater. The crater is thought to be deep buried in the Denver basin, near the Wyoming-Nebraska border.

Holbox Island and the Yalahau Lagoon on the northeast corner of Mexico’s Yucatan Peninsula

Holbox Island and the Yalahau Lagoon on the northeast corner of Mexico’s Yucatan Peninsula are featured in this image, acquired by the Korea Multi-purpose Satellite (Kompsat-2) of the Korea Aerospace Research Institute (KARI). (Image credit: KARI via ESA)

The source crater is expected to be roughly 50 to 65 km across. The crater in the Yucatán Peninsula is three times the diameter and is associated with the end of the dinosaurs.

All of the secondary craters were caused by bits of bedrock that were between 13 feet and 26 feet in diameter. They say the impactor could have been more than 2 km wide.

The study was published in the GSA Bulletin.

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