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Geophysicists Show that Crust Temperature Variation Explains Half of Elevation Differences in North America

February 1, 2008

Geophysicists determined that tectonic mountain-building processes are not the only factor that determines elevation in North America. The temperature of the crust affects its density, and lower density crust will rise higher than colder, higher density crust. The heat in question comes from the Earthýs interior and also radioactive decay of various elements in the crust. Broadly, the Rocky Mountain region of the United States has the hottest crust, as well as the highest general elevation.

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Science Insider

WHY DOES THE EARTH NEED TO MOVE? The Earth's crust is quite thin compared to the diameter of our planet. The crust is made up of sections called plates, ranging from very small to the size of an entire continent. Both the Earth's surface and its interior are constantly moving.
Beneath the rigid plates of the earth's crust, lies the mantle -- mobile rock that slowly moves in circles, like a pot of thick soup that is heated to boiling. The heated soup rises to the surface, spreads and begins to cool, then sinks back to the bottom of the pot, where it reheats and rises again. This cycle is repeated over and over; this is called convective flow. This process occurs much more slowly inside the Earth.
Because of the heat and pressure that builds up beneath the surface, the crust is constantly being stressed, which breaks it up. This is known as plate tectonics. When two plates move away from each other, deep cracks are opened through the crust, allowing magma to rise to the surface and then cool, making new crust. Crust is destroyed when one plate dives under another. Plates can also slide horizontally past each other.

The American Geophysical Union contributed to the information contained in the TV portion of this report.

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More information on this story

Dr. David S. Chapman
Salt Lake City, UT
(801) 581-7642
david.chapman@gradschool.utah.edu

American Geophysical Union
Washington, DC 20009-1277
1-800-966-2481


© 2008 American Institute of Physics