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The '''cool early Earth''' (''CEE'') theory posits that the early planet [[Earth]] had a calm influx of [[bolide]]s and a cool climate allowing fluid water, after the [[Formation and evolution of the Solar System|planetary accretion]] but before the occurrence of the [[Late Heavy Bombardment]] in the [[Hadean]] geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 [[annum|billion years]] (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western [[Australia]]n [[Jack Hills#Oldest zircon on Earth|Jack Hills]] detrital [[zircon]]s dated to about 4.0–4.4 Ga ago,<ref>{{cite web
The '''cool osom early Earth''' (''CEE'') theory posits that the early planet [[Earth]] had a calm influx of [[bolide]]s and a cool climate allowing fluid water, after the [[Formation and evolution of the Solar System|planetary accretion]] but before the occurrence of the [[Late Heavy Bombardment]] in the [[Hadean]] geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 [[annum|billion years]] (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western [[Australia]]n [[Jack Hills#Oldest zircon on Earth|Jack Hills]] detrital [[zircon]]s dated to about 4.0–4.4 Ga ago,<ref>{{cite web
|url=http://rst.gsfc.nasa.gov/Sect19/Sect19_2a.html
|url=http://rst.gsfc.nasa.gov/Sect19/Sect19_2a.html
|title=Remote Sensing: The Earth as a Planet
|title=Remote Sensing: The Earth as a Planet

Revision as of 02:24, 20 July 2011

The cool osom early Earth (CEE) theory posits that the early planet Earth had a calm influx of bolides and a cool climate allowing fluid water, after the planetary accretion but before the occurrence of the Late Heavy Bombardment in the Hadean geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 billion years (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western Australian Jack Hills detrital zircons dated to about 4.0–4.4 Ga ago, [1] some time after the planetary accretion era of the early Hadean. The Cool Early Earth was immediately followed by the Late Heavy Bombardment.

See also

References

  1. ^ Nicholas M. Short, Sr., et al.ok. "Remote Sensing: The Earth as a Planet". Retrieved December 28, 2008. {{ cite web}}: Unknown parameter |update= ignored ( help)CS1 maint: multiple names: authors list ( link)

External links


Template:Geol-stub

From Wikipedia, the free encyclopedia
Content deleted Content added
No edit summary
No edit summary
Line 1: Line 1:
The '''cool early Earth''' (''CEE'') theory posits that the early planet [[Earth]] had a calm influx of [[bolide]]s and a cool climate allowing fluid water, after the [[Formation and evolution of the Solar System|planetary accretion]] but before the occurrence of the [[Late Heavy Bombardment]] in the [[Hadean]] geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 [[annum|billion years]] (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western [[Australia]]n [[Jack Hills#Oldest zircon on Earth|Jack Hills]] detrital [[zircon]]s dated to about 4.0–4.4 Ga ago,<ref>{{cite web
The '''cool osom early Earth''' (''CEE'') theory posits that the early planet [[Earth]] had a calm influx of [[bolide]]s and a cool climate allowing fluid water, after the [[Formation and evolution of the Solar System|planetary accretion]] but before the occurrence of the [[Late Heavy Bombardment]] in the [[Hadean]] geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 [[annum|billion years]] (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western [[Australia]]n [[Jack Hills#Oldest zircon on Earth|Jack Hills]] detrital [[zircon]]s dated to about 4.0–4.4 Ga ago,<ref>{{cite web
|url=http://rst.gsfc.nasa.gov/Sect19/Sect19_2a.html
|url=http://rst.gsfc.nasa.gov/Sect19/Sect19_2a.html
|title=Remote Sensing: The Earth as a Planet
|title=Remote Sensing: The Earth as a Planet

Revision as of 02:24, 20 July 2011

The cool osom early Earth (CEE) theory posits that the early planet Earth had a calm influx of bolides and a cool climate allowing fluid water, after the planetary accretion but before the occurrence of the Late Heavy Bombardment in the Hadean geological eon. The Cool Early Earth is believed to have been the state for some hundreds of million years around 4.2 billion years (Ga) ago. This Cool Early Earth theory is supported by supposed water conditions at the creation of western Australian Jack Hills detrital zircons dated to about 4.0–4.4 Ga ago, [1] some time after the planetary accretion era of the early Hadean. The Cool Early Earth was immediately followed by the Late Heavy Bombardment.

See also

References

  1. ^ Nicholas M. Short, Sr., et al.ok. "Remote Sensing: The Earth as a Planet". Retrieved December 28, 2008. {{ cite web}}: Unknown parameter |update= ignored ( help)CS1 maint: multiple names: authors list ( link)

External links


Template:Geol-stub


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