• Home
  • Chemistry
  • Astronomy
  • Energy
  • Nature
  • Biology
  • Physics
  • Electronics
  • Understanding the Geologic Time Scale: Eons and Eras
    The geologic time scale is divided into four major subdivisions:

    1. Eons: The largest and broadest divisions of geologic time.

    * Precambrian Eon: The earliest and longest eon, encompassing the vast majority of Earth's history, from about 4.5 billion years ago to 541 million years ago.

    * Phanerozoic Eon: The current eon, starting at the end of the Precambrian and continuing to the present.

    2. Eras: Within each eon, there are multiple eras.

    * Precambrian Eon: This eon doesn't have formal eras, but it is sometimes informally divided into three parts: Hadean, Archean, and Proterozoic.

    * Phanerozoic Eon:

    * Paleozoic Era: (541-252 million years ago) "Old Life" - rise of complex life forms.

    * Mesozoic Era: (252-66 million years ago) "Middle Life" - age of dinosaurs.

    * Cenozoic Era: (66 million years ago to present) "Recent Life" - age of mammals.

    3. Periods: Eras are further subdivided into periods.

    * Paleozoic Era: Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian

    * Mesozoic Era: Triassic, Jurassic, Cretaceous

    * Cenozoic Era: Paleogene (Paleocene, Eocene, Oligocene), Neogene (Miocene, Pliocene), Quaternary (Pleistocene, Holocene)

    4. Epochs: Periods are further subdivided into epochs (except for the Quaternary period, which is often divided into two epochs).

    * Paleogene: Paleocene, Eocene, Oligocene

    * Neogene: Miocene, Pliocene

    * Quaternary: Pleistocene, Holocene

    Note: The geologic time scale is a constantly evolving system, and the specific boundaries between units may be adjusted as new information becomes available.

    Science Discoveries © www.scienceaq.com