The mass of the Earth has been determined through:

  • A
    Use of Kepler's $T^2/R^3$ constancy law
  • B
    Sampling the density of the Earth's crust and using $R$
  • C
    Cavendish's determination of $G$ and using $R$ and $g$ at the surface
  • D
    Use of periods of satellites at different heights above the Earth's surface

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