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14.3: Reading Earth's History

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    55240
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    Rocks preserve a record of events that have occurred throughout Earth’s long history. This section introduces the geological time scale and examines how geologists determine the sequence and ages of past events. Relative dating methods establish whether rocks and events are older or younger than one another, while isotopic dating provides numerical ages. Together, these methods allow geologists to reconstruct Earth’s history across billions of years.


    14.3: Reading Earth's History is shared under a CC BY-NC-SA license and was authored, remixed, and/or curated by LibreTexts.

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