ranging from 46 to 70 million kilometers. It takes 87.969 earth days to complete an orbit. The diagram on the right illustrates the effects of the eccentricity, showing Mercury's orbit overlaid with a circular orbit having the same
semi-major axis. The higher velocity of the planet when it is near perihelion is clear from the greater distance it covers in each 5-day interval. The size of the spheres, inversely proportional to their distance from the Sun, is used to illustrate the varying heliocentric distance. This varying distance to the Sun, combined with a 3:2
spin-orbit resonance of the planet's rotation around its axis, result in complex variations of the surface temperature.
[13] This resonance makes a single day on Mercury last exactly two Mercury years, or about 176 Earth days.
[69]
Mercury's orbit is inclined by 7 degrees to the plane of Earth's orbit (the
ecliptic), as shown in the diagram on the right. As a result,
transits of Mercury across the face of the Sun can only occur when the planet is crossing the plane of the ecliptic at the time it lies between the Earth and the Sun. This occurs about every seven years on average.
[70]
Mercury's
axial tilt is almost zero,
[71] with the best measured value as low as 0.027 degrees.
[7] This is significantly smaller than that of
Jupiter, which has the second smallest axial tilt of all planets at 3.1 degrees. This means that to an observer at Mercury's poles, the center of the Sun never rises more than 2.1
arcminutes above the horizon.
[7]
At certain points on Mercury's surface, an observer would be able to see the Sun rise about halfway, then reverse and set before rising again, all within the same
Mercurian day. This is because approximately four Earth days before
perihelion, Mercury's angular
orbital velocity exactly equals its angular
rotational velocity so that the Sun's
apparent motion ceases; at perihelion, Mercury's angular orbital velocity then exceeds the angular rotational velocity. Thus, to a hypothetical observer on Mercury, the Sun appears to move in a
retrograde direction. Four days after perihelion, the Sun’s normal apparent motion resumes at these points.
[13]
Mercury attains inferior conjunction (near approach to the Earth) every 116 Earth days on average,
[3] but this interval can range from 105 days to 129 days due to the planet’s eccentric orbit. Mercury can come as close as 77.3 million km to the Earth,
[3] but it will not be closer to Earth than 80 Gm until AD 28,622. The next approach to within 82.1 Gm is in 2679, and to within 82 Gm in 4487.
[72] Its period of
retrograde motion as seen from Earth can vary from 8 to 15 days on either side of inferior conjunction. This large range arises from the planet's high orbital eccentricity.
[13]
Spin–orbit resonance

After one orbit, Mercury has rotated 1.5 times, so after two complete orbits the same hemisphere is again illuminated.
For many years it was thought that Mercury was synchronously
tidally locked with the Sun,
rotating once for each orbit and always keeping the same face directed towards the Sun, in the same way that the same side of the Moon always faces the Earth.
Radar observations in 1965 proved that the planet has a 3:2 spin–orbit resonance, rotating three times for every two revolutions around the Sun; the eccentricity of Mercury’s orbit makes this resonance stable—at perihelion, when the solar tide is strongest, the Sun is nearly still in Mercury’s sky.
[73]
The original reason astronomers thought it was synchronously locked was that, whenever Mercury was best placed for observation, it was always nearly at the same point in its 3:2 resonance, hence showing the same face. This is because, coincidentally, Mercury's rotation period is almost exactly half of its synodic period with respect to Earth. Due to Mercury's 3:2 spin–orbit resonance, a
solar day (the length between two
meridian transits of the Sun) lasts about 176 Earth days.
[13] A
sidereal day (the period of rotation) lasts about 58.7 Earth days.
[13]
Simulations indicate that the
orbital eccentricity of Mercury varies
chaotically from nearly zero (circular) to more than 0.45 over millions of years due to
perturbations from the other planets.
[13][74] This is thought to explain Mercury's 3:2 spin-orbit resonance (rather than the more usual 1:1), since this state is more likely to arise during a period of high eccentricity.
[75] Numerical simulations show that a future
secular orbital resonant perihelion interaction with Jupiter may cause the eccentricity of Mercury's orbit to increase to the point where there is a 1% chance that the planet may collide with Venus within the next five billion years.