MadSci Network: Science History |
The different parts of the Earth's core were hypothesized to be made of different kinds (phases) of Fe when seismic waves were studied. Seismic waves travel through different materials at different speeds, and so you know or can figure out the material by knowing the starting velocity of the wave. Earthquakes have helped in determining the regions of Earth's core because we have gained such a good knowledge of where an earthquake wave (P or S) originates and where it ends. More about this can be found at the following 2 websites: http://www.anl.gov/OPA/factsheets/r3-02.htm http://www.anl.gov/OPA/factsheets/r3-02.htm
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