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Hadean

File:Artist's_concept_of_collision_at_HD_172555.jpg · Wikimedia Commons · See Wikimedia Commons

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Also known as Priscoan Period, Priscoan, Pre-Archean, Pre-Archean period, Pre-Archaean, Pre-Archaean period, Hadean Eon

The Hadean ( ) is the first and oldest of the four geologic eons of Earth's history, starting with the planet's formation about 4.6 Ga (estimated 4567.30 ± 0.16 Ma set by the age of the oldest solid material in the Solar System—protoplanetary disk dust particles—found as chondrules and calcium–aluminium-rich inclusions in some meteorites about 4.567 Ga), and ending 4.031 Ga, the age of the oldest known intact rock formations on Earth as recognized by the International Commission on Stratigraphy. The interplanetary collision that created the Moon occurred early in this eon. The H

AI overview

The Hadean is Earth's oldest geologic eon, beginning with the planet's formation approximately 4.6 billion years ago and ending about 4 billion years ago with the oldest known intact rock formations. This eon is significant because it encompasses Earth's earliest history, including the giant collision that created the Moon, though our direct knowledge of this period is limited by the scarcity of surviving rock records from that time.

AI-generated from the Wikipedia summary — may contain errors.

Key facts

Geologic timespan.color
Hadean
Geologic timespan.top_bar
all time
Geologic timespan.image_map
Artist's concept of collision at HD 172555.jpg
Geologic timespan.caption_map
Artist depiction of the hypothetical planet Theia colliding into Early Earth
Geologic timespan.image_art
Earearth.png
Geologic timespan.caption_art
Artist illustration of Earth and the Moon towards the middle/end of the Hadean eon
Geologic timespan.timeline
Eons
Geologic timespan.synonym1
Priscoan Period
Geologic timespan.synonym1_coined
Harland et al., 1989
Geologic timespan.celestial_body
earth
Geologic timespan.usage
Global (ICS)
Geologic timespan.chrono_unit
Eon
Geologic timespan.strat_unit
Eonothem
Geologic timespan.proposed_by
Preston Cloud, 1972
Geologic timespan.timespan_formality
Formal
Geologic timespan.lower_boundary_def
Age of the oldest solid material in the Solar System's protoplanetary disk (4567.30 ± 0.16) Ma
Geologic timespan.upper_boundary_def
Ten oldest U-Pb zircon ages
Geologic timespan.upper_gssa_location
Along the Acasta River, Northwest Territories, Canada

via Wikipedia infobox

Wikidata facts

Image
Hadean.png
Show 4 more facts
start time
4567300000
end time
4031000000
Commons category
Hadean
sRGB color hex triplet
AE027E
Sources (4)

via Wikidata · CC0

~10 min read

Article

11 sections
Contents
  • Etymology
  • Rock dating
  • Atmosphere
  • Oceans
  • Plate tectonics
  • Continents
  • Possible life
  • See also
  • References
  • Further reading
  • External links

The Hadean ( ) is the first and oldest of the four geologic eons of Earth's history, starting with the planet's formation about 4.6 Ga (estimated 4567.30 ± 0.16 Ma set by the age of the oldest solid material in the Solar System—protoplanetary disk dust particles—found as chondrules and calcium–aluminium-rich inclusions in some meteorites about 4.567 Ga), and ending 4.031 Ga, the age of the oldest known intact rock formations on Earth as recognized by the International Commission on Stratigraphy. The interplanetary collision that created the Moon occurred early in this eon. The Hadean eon was succeeded by the Archean eon, with the Late Heavy Bombardment hypothesized to have occurred at the Hadean-Archean boundary.

Hadean rocks are very rare, largely consisting of granular zircons from one locality (Jack Hills) in Western Australia. Hadean geophysical models remain controversial among geologists: plate tectonics and the growth of cratons into continents may have started in the Hadean, but there is still uncertainty.

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On the map

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