Chapter Twelve

Editor's Note


One of the important aspects of geology is the ability to use the rock record to look back in time at earth history.  This not only gives scientists a window into the ancient earth but a method by which processes that occur beneath the earth’s surface and over long periods of geologic time can be studied.  The tools of this understanding involve measuring time itself against geologic events that have occurred in the past.  The measurement of time can either be relative, sequencing geologic events through the rock record, or absolute, measuring time by the breakdown of radioactive elements within the crust of the earth.  Both tools come into play in building our greater understanding of geologic time and earth history.


How Do Scientists Measure Earth Age?
Marsha Barber and Diana Schielde Bartos
Louisiana Energy & Environmental Resource & Information Center
Louisiana State University
http://www.leeric.lsu.edu/bgbb/1/measuring.html


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Additional Reading

Fossils, Rocks and Time
Lucy E. Edwards and John Pojeta, Jr.

http://pubs.usgs.gov/gip/fossils/
United States Geological Survey
online publication

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Geologic Time
William L. Newman
http://pubs.usgs.gov/gip/geotime/
United States Geological Survey
online publication

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