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CHAP PACE I Sol1ds and L1qu1ds
Grav1ty and the Shape of the Earth
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actual amount anomalies atomic weight axis basalt centre clots compression continental drift continents contraction convection cooling core crust crystal density depth determine difference direction displacement distance distribution earth earthquakes eclogite effect elevation epicentre expected explain fact fluid force fracture friction G. I. Taylor geoid geological give granite gravity gravity anomalies heat height horizontal igneous rocks increase inequalities intermediate layer internal isostasy kilometres km./sec latitude lead less level surface liquid load lower layer magma mass material matter melting-point milligals moon moon's motion mountain formation mountain system movement needed observed ocean olivine original outflow period plane possible present pressure probably produce radioactivity regions result rigidity rise rocky shell rotation sea-level sediments seems seismology shortening sodium solid strength stress-differences suppose surface waves tachylyte theory thermal thickness thorium tidal tide tion unit area upper layers uranium variation velocity vertical viscosity volcanoes whole