The Younger Dryas Period, dating approximately 12,800 years ago, is characterized by an abrupt cooling event associated with widespread ecological disruption and mass extinction. Evidence suggests that this rapid climate shift may have been triggered by a cosmic event, forming the basis of the Younger Dryas impact hypothesis. This study compares sedimentary markers associated with the Younger Dryas with those found at known high-energy impact sites, including comets, airbursts, and lightning-related events. To establish a baseline for cosmic impact features, we analyzed soil and mineral sample
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