The geological time scale is divided into:
Eons (Such as the Proterozoic and the Phanerozoic)
THEN
Eras (Such as the Mesozoic and the Cenozoic)
THEN
Periods (Such as the Cretaceous and the Quaternary)
THEN
Series, alternatively Epoch (Such as the Pleistocene and the Holocene)
THEN
Stage (Such as the Campanian and the Tarantian)
fossil record geologic time scale
fossil record geologic time scale
Eon is the broadest division on the geologic time scale, representing the longest time span. Eons are further divided into eras, which are then subdivided into periods, epochs, and ages.
Yes, epochs are further divided into eras in the geologic time scale. The geologic time scale is divided into eons, which are then broken down into eras, which are further divided into periods, epochs, and ages. Each division represents a significant geological time period characterized by distinct events or changes in Earth's history.
The largest division of time on the geologic time scale is an eon. Eons are subdivided into eras, which are further divided into periods, epochs, and ages. The current eon, the Phanerozoic, began around 541 million years ago and is divided into the Paleozoic, Mesozoic, and Cenozoic eras.
geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
fossil record geologic time scale
Eon is the broadest division on the geologic time scale, representing the longest time span. Eons are further divided into eras, which are then subdivided into periods, epochs, and ages.
The largest expanse of time on the geologic time scale is the eon, which is further divided into eras. Eons are the longest subdivisions of time, representing billions of years of Earth's history.