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Age of Earth
Approximately 4.54 billion years old.
Radiometric dating
A method used to determine Earth's age by measuring radioactive decay.
Geologic time
Divided into Eon, Era, Period, and Epoch based on major Earth events.
Eon
The broadest division of geologic time, spanning billions of years.
Eras
Subdivisions of eons marked by major changes in life forms.
Paleozoic Era
Spanning 541 to 252 million years ago, known as the 'Age of Invertebrates & Amphibians'.
Mass Extinctions
Catastrophic events that erase a large percentage of species and mark boundaries between eras.
Law of Superposition
In undisturbed sedimentary rock layers, older layers are at the bottom.
Index Fossils
Fossils used to date rock layers, derived from organisms that were widespread and lived for a short time.
Cenozoic Era
Last era, started 66 million years ago, characterized as the 'Age of Mammals'.