Radiocarbon dating can help study past earthquakes by providing precise age estimates for organic materials found in sediment layers affected by seismic activity. By dating materials such as charcoal or plant remains in sediments that have been displaced or disturbed by an earthquake, researchers can establish a timeline of seismic events. This information allows scientists to better understand the frequency, intensity, and impact of historical earthquakes on ecosystems and human societies. Additionally, it can aid in assessing earthquake recurrence intervals and informing future risk assessments.
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