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Cosmogenic isotopes are radioactive elements produced by cosmic-ray bombardment of Earth's atmosphere and surface. These isotopes, such as carbon-14, beryllium-10, and chlorine-36, are valuable tools in dating various materials.123

Carbon-14 dating, for instance, is used for organic materials up to about 60,000 years old. Other cosmogenic isotopes like beryllium-10 and chlorine-36 help date marine sediments, glacial ice, and even the exposure age of meteorites. The concentration of these isotopes can reveal information about past cosmic-ray intensity and geological processes.132

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