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Beryllium-10 is a synthetic isotope of beryllium, a light, alkaline-earth metal. Unlike the stable isotope beryllium-9, beryllium-10 is radioactive and undergoes beta decay with a half-life of 1.5 million years.12

Beryllium-10 is produced in the Earth's atmosphere by cosmic rays striking oxygen and nitrogen atoms. It is then deposited on Earth's surface through rain and snow, allowing scientists to track its migration. This isotope has been used in various scientific applications, including dating geological samples and studying the Earth's climate history by analyzing ice cores and ocean sediments. It has also provided insights into volcanic activity and the intensity of cosmic rays over long periods.3

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