For planets and moons, equilibrium is reached when the compression due to gravity is balanced by a pressure gradient in the opposite direction due to the strength of the material, at which point gravitational compression ceases.
This pressure gradient is in the opposite direction due to the strength of the material, at which point gravitational compression ceases. For planets and moons, equilibrium is reached when the compression is balanced by a pressure gradient.
For planets and moons, equilibrium is reached when the compression is balanced by a pressure gradient. This pressure gradient is in the opposite direction due to the strength of the material, at which point gravitational compression ceases.
For planets and moons, equilibrium is reached when the compression is balanced by a pressure gradient. This pressure gradient is in the opposite direction due to the strength of the material, at which point gravitational compression ceases.