Geochronology is the science of determining the absolute age of rocks, fossils, and sediments, as well as the timing of geological events. This field is essential for understanding the timeline of Earth's history and the processes that have shaped the planet over billions of years.
There are several methods used in geochronology to determine the age of geological materials:
Geochronology has numerous applications in the field of Earth science:
To excel in geochronology, consider the following study tips:
By mastering geochronology, you'll gain a deeper appreciation for Earth's history and the processes that have shaped the planet over time.
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