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China’s Jinlin Crater Confirmed as Earth’s Largest Known Holocene Impact Site

The identification relies on shock features in quartz, prompting follow-up work to refine the age as well as determine the meteorite’s composition.

Overview

  • Researchers report a bowl-shaped structure near Deqing in Guangdong measuring about 900 meters across and roughly 90 meters deep, preserved within a thick granite weathering crust.
  • The site surpasses Russia’s 300-meter Macha structure as the largest crater known to have formed during the Holocene epoch.
  • Planar deformation features in quartz record shock pressures of about 10–35 gigapascals, providing decisive evidence of an impact rather than a terrestrial process.
  • Formation age is estimated from local soil-erosion rates to the early-to-mid Holocene, a timeline experts note is inferred and will require more precise radiometric dating.
  • The impactor is concluded to have been a meteorite rather than a comet, the iron-versus-stony makeup remains unknown, and the find adds to roughly 200 confirmed impact craters worldwide.