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Seismology. - GeoWeb

HookeHooke s Law (or )1760 MitchellRecognitionthatgroundmotiondueto earthquakesis relatedtowave propagation1821 NavierEquationofmotion1828 PoissonWave equation P&S-waves1885 RayleighTheoreticalaccountsurfacewaves Rayleigh&Love waves1892 MilneFirsthigh-qualityseismograph beginofobservationalperiod1897 WiechertPredictionofexistenceofdensecore (basedonmeteorites Fe-alloy)1900 OldhamCorrectidentificationofP,Sandsurfa cewaves1906 OldhamDemonstrationofexistenceofcorefrom seismicdata1906 GalitzinFirstfeed-backbroadbandseismogra ph1909 Mohorovi ci cCrust-mantleboundary1911 LoveLove waves(surfacewaves)1912 GutenbergDepthtocore-mantleboundary:2900 km1922 Turnerlocationofdeepearthquakesdownto600 km(butlocatedsomeat 2000km, )1928 WadatiAccuratelocationofdeepearthquakes Wadatai-Benioff zones1936 LehmanDiscoveryofinnercore1939 Jeffreys&BullenFirsttravel-timetables 1 DEarthmodel19

118 CHAPTER4. SEISMOLOGY. 4.2 Introduction With seismology1 we face the same problem as with gravity and geomagnetism; we can simply not offer a comprehensive treatment of the entire subject within the time frame of this course.

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The Magnetic Field of the Earth

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C for the most important minerals such as magnetite. This is the basis for paleomagnetism. (There is no such thing as paleogravity!) 3.1 The main field From the measurement of the magnetic field it became clear that the field has both internal and external sources, both of which exhibit a time dependence. Spherical harmonics is a very conve-

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