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This University of Texas Arlington: Isostasy, Gravity, Magnetism, and Internal Heat ppt also includes:
An in-depth look at how isostasy works and the processes taking place during glaciation and the melting of glaciers. Looks at gravity and the effects of density differences within the crust and mantle, and at Earth's magnetic field and paleomagnetism. The geothermal gradient is also discussed.
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asthenosphere, continental crust, geothermal gradient, isostasy, lithosphere, magnetic reversal, mantle, mantle convection, oceanic crust, paleomagnetism, post-glacial rebound, earth's crust, earth's magnetic field, earth's magnetism, ohio pg.pt.2.e, pg.pt.2.f, pg.pt.3.a, university of texas arlington, university of texas arlington: isostasy, gravity, magnetism, and internal heat/ohio pg.pt.2.e, pg.pt.2.f, pg.pt.3.a, density differences in earth's interior, gravity, magnetism and isostasy, isostasy theory, magnetic field