• The number of asteroid impacts on the Earth and the Moon increased by two to three times starting around 290 million years ago, according to a study.
  • The research provides evidence for a dramatic change in the rate of asteroid impacts on both Earth and the Moon that occurred around the end of the Paleozoic era.
  • The implication is that since that time we have been in a period of relatively high rate of asteroid impacts that is 2.6 times higher than it was prior to 290 million years ago.
  • It had been previously assumed that most of the Earth’s older craters produced by asteroid impacts have been erased by erosion and other geologic processes
  • The relative rarity of large craters on Earth older than 290 million years and younger than 650 million years is not because we lost the craters, but because the impact rate during that time was lower than it is now
  • Scientists have for decades tried to understand the rate that asteroids hit Earth by using radiometric dating of the rocks around them to determine their ages.
  • Since it was believed erosion caused some craters to disappear, it was difficult to find an accurate impact rate and determine whether it had changed over time.
  • However, there was no way to determine the ages of lunar craters until NASA’s Lunar Reconnaissance Orbiter (LRO) started circling the Moon a decade ago and studying its surface.
  • Using LRO data, the team was able to assemble a list of ages of all lunar craters younger than about a billion years.
  • During the lunar night, rocks radiate much more heat than fine-grained soil called regolith.
  • This allows scientists to distinguish rocks from fine particles in thermal images.
  • It became clear that the reason why Earth has fewer older craters on its most stable regions is because the impact rate was lower up until about 290 million years ago.
  • The reason for the jump in the impact rate is unknown, though the researchers speculate it might be related to large collisions taking place more than 300 million years ago in the main asteroid belt between the orbits of Mars and Jupiter.