Earth's equilibrium surface temperature is primarily influenced by solar radiation and atmospheric effects, with internal fission and gravitational tidal forces contributing minimally. The core of the Earth has not solidified due to its large volume and the insulating properties of the crust, which hinder efficient heat transfer. The core was likely remelted after Earth's formation due to internal radioactive decay, rather than solidifying completely. The formation of the Moon from a Mars-sized impactor also contributed significant heat, preventing solidification. Overall, the interplay of these factors maintains the current surface temperature around 300K.