Difference between revisions of "13. Glacial periods"

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Return to [[History 8 Human Origins Concepts]]
 
Return to [[History 8 Human Origins Concepts]]
During interglacials, the Earth has normal climates-warm at the equator, cold at the poles.  Interglacial periods gradually grow colder, and the ice spreads south towards the Equator, covering large parts of Europe and North America.  Asia becomes bitterly cold and in some cases will not freeze if there is not a sufficient amount of rain.  After a certain number of years, it reverses back to an interglacial period and the cycle happens again.  This cycle is caused by variations in the Earth's orbit through time that change the amounts of solar radiation that hits the Earth in each season.
 
  
http://www.ncdc.noaa.gov/paleo/abrupt/images/data2-hemisphere.gif
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Glacial periods are periods in the Earth's history where the climate became ''cooler''. Interglacial periods are periods in Earths history where the climate became ''warmer''. The earth alternates between the two periods every 100,000 years. An example of a glacial period would be the last Ice Age. The last Ice age peaked around 16,000 BCE, and lowered temperatures around 65 degrees fahrenheit. Glacial and Interglacial periods change the organisms and ecosystems around them. For example, many large animals in North America became extinct due to the period changing to an interglacial period.  
  
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http://geology.utah.gov/wp-content/uploads/ice_ages2.gif
  
National Oceanic and Atmospheric Administration, "Glacial-Interglacial Periods" http://www.ncdc.noaa.gov/paleo/abrupt/data2.html
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          -Will Leger
Manual Chapter 3, page 23
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''Manual'' page 31
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'''Sources'''
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[http://arstechnica.com/science/2008/04/post-glacial-extinction/]
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'''Pictures'''
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[http://geology.utah.gov/wp-content/uploads/ice_ages2.gif]

Latest revision as of 12:01, 17 October 2015

Return to History 8 Human Origins Concepts

Glacial periods are periods in the Earth's history where the climate became cooler. Interglacial periods are periods in Earths history where the climate became warmer. The earth alternates between the two periods every 100,000 years. An example of a glacial period would be the last Ice Age. The last Ice age peaked around 16,000 BCE, and lowered temperatures around 65 degrees fahrenheit. Glacial and Interglacial periods change the organisms and ecosystems around them. For example, many large animals in North America became extinct due to the period changing to an interglacial period.

ice_ages2.gif

         -Will Leger


Manual page 31

Sources [1]


Pictures [2]