Celestial mechanics

Why planets don’t fall into the Sun

Gravity pulls every world inward. Sideways speed keeps them missing the center — forever falling, never landing. That balance is an orbit.

Kepler’s first law

Planets travel in ellipses with the Sun at one focus — not perfect circles. Earth’s path is nearly round (eccentricity 0.017); Pluto’s is much more oval (0.25).

Kepler’s second law

A line from the Sun to a planet sweeps equal areas in equal times. Near perihelion a planet speeds up; near aphelion it slows. Comets show this dramatically.

Kepler’s third law

The square of the orbital period scales with the cube of the semi-major axis: P² ∝ a³. Double the distance and the year grows by about 2.8×.

Period vs distance

Drag the distance slider. Watch how long a full orbit takes when the semi-major axis changes. The demo uses Kepler’s third law with Earth’s year as the unit.

Orbital period: 1.00 Earth years

Inner track ≈ Mercury; mid track ≈ Earth; outer tracks approach Jupiter’s distance in this simplified scale.

Eccentricity playground

Raise eccentricity and the ellipse stretches. The Sun stays at a focus, so the planet skims close then coasts far away.

*Halley’s comet is more eccentric than this slider allows; the button sets a strong ellipse for comparison.

Orbital periods at a glance

Body Mean distance (AU) Period Eccentricity Inclination
Mercury0.3988 days0.2067.0°
Venus0.72225 days0.0073.4°
Earth1.00365.25 days0.0170.0°
Mars1.52687 days0.0931.9°
Jupiter5.2011.9 years0.0491.3°
Saturn9.5829.5 years0.0572.5°
Uranus19.284 years0.0460.8°
Neptune30.1165 years0.0101.8°
Pluto39.5248 years0.24917.2°

Watch periods live

In the simulator, crank the speed and count how many Earth years pass while Neptune barely moves.

Open simulator