The physics of Earth
The chart below is a visual representation of a thousand years, from 2000 to 3000, of the stress building and stress releasing forces by the Jupiter system along the Jupiter-Sun axis, caused by the all planets.
The dots capture the date and force as the outer planets pass one another on each side of the Sun resolved along the Jupiter Sun axis. The chart is linear from high force to low force based on daily algebraic summations of forces of planets as they move through the solar system. The forces are resolved into two forces: stress building as planets move toward each other and stress releasing as they move away from each other.
In all planets, heat is generated by stress building and lost by stress releasing. During stress building the heat is used as specific heat to raise the temperate of the rock. Once the melting point of the rock is reached, the heat is used as latent heat to change the state of the rock to liquid. Some of the latent heat is taken from the specific heat of the surrounding rock cooling the rock. The opposite takes place during stress releasing. The latent heat to change the liquid to rock is transferred to the rock as specific heat raising the temperature of the rock.
One degree increase or decrease of Celsius heat causes one cubic feet of iron to expand or contract 1.198 ten millionth of a foot per foot or 253 feet across 4000 miles being the radius of Earth. The surface area of the liquid toward the surface of Earth is 7.5 times greater than the surface area toward the center of Earth. The discrepancy between the two surface areas is taken up more so in the mantle and crust of Earth than in the iron core center, giving the Earth the appearance of breathing. Stress building tightens the surface plates of Earth and loosens them during stress releasing.
