The
experiment was performed in 1797–98 by the English scientist Henry Cavendish. He
followed a method prescribed and used apparatus built by his countryman, the
geologist John Michell, who had died in 1793. The apparatus employed was a
torsion balance, essentially a stretched wire supporting spherical weights.
Attraction between pairs of weights caused the wire to twist slightly, which
thus allowed the first calculation of the value of the gravitational constant G.
The experiment was popularly known as weighing the Earth because determination
of G permitted calculation of the Earth's mass.