absolute dating
Quick Summary
Absolute dating, also known as geochronology, is the scientific field dedicated to determining the precise age of Earth's rocks and geological formations. Unlike relative dating, which establishes the sequence of events, absolute dating provides a numerical age, often measured in years.12
This is primarily achieved through radiometric dating, which relies on the predictable decay rates of radioactive isotopes within minerals. By measuring the ratio of parent radioactive atoms to their stable daughter atoms, scientists can calculate the time elapsed since the mineral formed. Common methods include uranium-lead dating, which is highly precise, and carbon-14 dating, used for dating organic materials up to about 60,000 years old. These techniques are crucial for understanding Earth's history, correlating geological events globally, and calibrating the fossil record.1234
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