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The Snowball Hypothesis for Earth


# 60630
The Snowball Hypothesis for Earth
This paper discusses the Snowball Hypothesis for Earth theory, which proposes that the Earth has a history of temperature cycles.
1,440 words (approx. 5.8 pages) | 5 sources | MLA | 2005 United States


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Paper Summary:

This paper explains that the Snowball Hypothesis for Earth, which is a theory speculating that the earth has experienced consistent cyclical hot and cold periods, can be considered a possible cause of the current trends toward warmer climates and rising seas. The author points out that the theory encompasses tropical sea-level glaciers, distributions of continents, carbon dioxide levels, solar input, banded iron formations and early bacterial life. The paper states that scientist speculate that approximately twenty thousand years ago, our deep ocean waters moved towards the freezing point, but those water temperatures were not near the equator as was the case during the Neoproterozoic period.

From the Paper:

"As we currently fear global warming, evidence may be pointing to eventual temperature shifts that follow the Yin and Yang of life. First, there are opposites hot and cold. The planet is merely going through its normal cyclical changes so we should not fear global warming any more than we should expect it as we should also expect another future snowball. "For the last million years, the Earth has been in its coldest state since the Neoproterozoic. We are now living in a relatively warm episode, some 80,000 years from the next glacial maximum, but some evidence suggests that each successive glaciation over the last several cycles has been getting stronger and stronger.""

Cite this paper

APA Citation:

The Snowball Hypothesis for Earth (2012, February 08). Retrieved February 13, 2012, from http://www.academon.com/Essay-The-Snowball-Hypothesis-for-Earth/60630

MLA Citation:

"The Snowball Hypothesis for Earth" 08 February 2012. Web. 13 Feb. 2012. <http://www.academon.com/Essay-The-Snowball-Hypothesis-for-Earth/60630>




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