Experimental evidence supporting Newton's law of universal gravitation, specifically the inverse-square law (1/R^2), is primarily derived from observations of planetary orbits and laboratory tests like the torsion balance. While these methods establish upper limits on potential deviations (denoted as x in 1/R^(2+x)), they do not provide definitive proof that x equals zero. The stability of non-circular orbits further constrains the possible values of x, suggesting it must be very close to zero. General Relativity introduces minor corrections to Newton's law, observable in specific cases like Mercury's orbit, but does not fundamentally alter its application for most practical purposes. Overall, while the inverse-square law is widely accepted, ongoing experiments continue to test its limits and potential deviations.