Earth age × 365.25 ÷ planet year
First convert your Earth age to Earth days, then divide by that planet's orbital period in days. A shorter orbit produces more planet-years in the same elapsed time.
A "year" just means one full orbit around the Sun — and that takes wildly different amounts of time depending which planet you're standing on. Enter your age below to find out.
Explore Kepler's third law: for planets around the Sun, orbital period squared is proportional to the semi-major axis cubed. Choose a planet to compare an idealized prediction with NASA's rounded orbital period.
On small screens, scroll the plot sideways to inspect its logarithmic labels. The numbers below remain fully visible.
These axes are logarithmic, not equally spaced in AU or years. The plot shows the ideal two-body Sun–planet approximation, not orbital position, speed or inclination. Distances are approximate semi-major axes; periods use NASA rounded values, so prediction and published period can differ slightly.
Evidence: NASA — Orbits and Kepler's Laws and NASA Planetary Fact Sheet. The original eight-planet period list above remains readable without JavaScript.
The calculator changes the unit used to count your age; it does not change how much time has actually passed.
First convert your Earth age to Earth days, then divide by that planet's orbital period in days. A shorter orbit produces more planet-years in the same elapsed time.
Mars takes about 687 Earth days to orbit the Sun, so a 12-year-old on Earth has lived through only about 6.4 Martian years.
This is a calendar comparison, not a claim that people age faster or slower on different planets. The same elapsed time is being counted with different orbital clocks.
The IAU three-criteria rule explained.
What actually keeps a planet orbiting for that long.
Watch every planet's real relative orbital speed in the 3D model.