Sidereal Rotation Period of Mercury
| Value | 5,067,360 s |
| Status | Conventional / typical value |
| Source | NASA NSSDC Planetary Fact Sheet, Mercury (sidereal rotation period, 1407.6 h) |
| Categories | Astronomicalsolar-systemplanets |
| Planck time | 9.3992355e+49 tP |
| attosecond | 5.0673600e+24 as |
| femtosecond | 5.0673600e+21 fs |
| picosecond | 5.0673600e+18 ps |
| nanosecond | 5.0673600e+15 ns |
| shake | 506,736,000,000,000 shake |
| microsecond | 5,067,360,000,000 μs |
| millisecond | 5,067,360,000 ms |
| second | 5,067,360 s |
| minute | 84,456 min |
| hour | 1,407.6 h |
| sidereal day | 58.810578 sd |
| day | 58.65 d |
| week | 8.3785714 wk |
| fortnight | 4.1892857 fn |
| month | 1.926939 mo |
| year | 0.16057495 yr |
| decade | 0.016057495 dec |
| century | 0.0016057495 cent |
| millennium | 0.00016057495 mil |
| megayear | 1.6057495e-07 Myr |
| eon | 1.6057495e-10 eon |
Learning zone
For eighty years the textbooks were wrong about this number. Schiaparelli concluded in 1889 that Mercury keeps one face to the Sun, rotating once per 88-day orbit the way the Moon does to Earth, and the tidal-locking argument was so plausible that nobody checked until Pettengill and Dyce bounced radar off the planet from Arecibo in 1965. The Doppler spread of the echoes gave 59 days, not 88.
The true state is subtler than a simple lock: Mercury rotates exactly three times for every two orbits, the only 3:2 spin-orbit resonance known in the solar system. The high eccentricity makes it stable — tidal torques are strongest at perihelion, and at perihelion the 3:2 spin briefly matches the orbital angular rate, so the Sun's grip finds nothing to correct. Italian dynamicist Giuseppe Colombo worked out the mechanism within a year of the radar result.