The Rutherford model, also known as the Rutherford atomic model, the Nuclear atom or planetary atom was proposed by New Zealand physicist Ernest Rutherford in 1911.
In 1909, he used alpha particles to investigate the composition of gold foil.
The model described the atom as a small, dense, charitable compound called the nucleus, in which almost all of the residue is concentrated in the negative elements called electrons orbiting a certain distance like the planets orbiting the sun.
The conclusions were drawn from Rutherford scattering experiments. Most alpha particles flew straight without deviating. So there was nothing to stop them along the way. This means that most of the space in the foil is free and you can see the core.