The gravity constant, known as G, was famously measured by Henry Cavendish using a torsion balance in a laboratory experiment. Newton's theory of gravitation allows scientists to calculate the mass of planets by analyzing the relationship between their orbital radius and period, particularly when the orbiting object is much lighter than the central mass. The mass of Earth is easily determined through direct measurements of gravitational force at its surface. Historical experiments, such as the 18th Century pendulum test on Schiehallion Mountain, provided early estimates of Earth's density and helped confirm G. Notably, the value of GM for Earth is known with greater precision than the individual values of G or M.