This colored view of Mercury was produced using images from the first Messenger mission. These colors are not Mercury's true colors; they have been enhanced to differentiate the chemical and mineralogical aspects of the rocks that make up Mercury's surface.
Image source: NASA / Johns Hopkins University Applied Physics Laboratory / Carnegie Institution of Washington.
This article presents the characteristics of Mercury, the smallest planet in the Solar System and the closest to the Sun. Its major peculiarities are: extreme temperature variations (430°C during the day, -180°C at night) due to the lack of atmosphere; the presence of water ice in polar craters, protected from solar radiation; and an eccentric orbit (0.205) combined with a 3:2 spin-orbit resonance (3 rotations for 2 revolutions), making a solar day (176 Earth days) twice as long as its year (88 days). The Messenger mission confirmed the polar ice and the composition of its surface.
Mercury, the smallest planet in the Solar System and the closest to the Sun (at an average distance of about 58 million km), has exceptional characteristics. Extreme temperatures: the side exposed to the Sun reaches 430°C, while the night side drops to -180°C, a thermal contrast unmatched in the Solar System, due to the almost total absence of an atmosphere to regulate heat. Presence of water ice and organic materials in the craters of the North and South poles. The bottom is permanently in shadow, acting as cold traps that preserve these volatiles. Its eccentric orbit (eccentricity of 0.205), the most elongated of the planets, varies in distance from the Sun from 46 to 70 million km. This eccentricity, combined with its slow rotation, creates a 3:2 spin-orbit resonance: Mercury rotates three times on itself for two orbits around the Sun, meaning a solar day lasts 176 Earth days (twice its year of 88 days). The Messenger mission (2004–2015) confirmed these discoveries, making Mercury a world that is both extremely hot and paradoxically icy at the poles.
N.B.: The official definition of a planet (since 2006) requires that it orbits the Sun, has a spherical shape due to its own gravity, and has "cleared" its orbit.
Mercury experiences the greatest temperature variations in the Solar System. This peculiarity is due to two factors: its proximity to the Sun and the almost total absence of an atmosphere to regulate heat. The side exposed to the Sun, where it is eternal day, can reach scorching temperatures of about 430°C, enough to melt lead. Simultaneously, the side plunged into darkness sees the temperature drop to -180°C. No other planet has such a violent thermal contrast between its day and night sides.
Despite its equatorial furnace, a surprising discovery was made by the Messenger mission: the existence of water ice and other frozen organic materials in the craters of Mercury's poles. The bottom of these craters, located at the North and South poles, is permanently in shadow from the Sun's rays. These cold traps act as cosmic freezers, preserving volatiles that would instantly vaporize elsewhere on the planet. This discovery makes Mercury a surprising member of the family of icy worlds.
Mercury's orbit is the most eccentric (most elongated) of all the planets in the Solar System. Its distance from the Sun thus varies enormously, from 46 million kilometers at its closest (perihelion) to 70 million kilometers at its farthest (aphelion). This high eccentricity, combined with its slow rotation, creates a fascinating phenomenon: a 3:2 spin-orbit resonance. This means that the planet rotates three times on itself for two orbits around the Sun. As a result, a solar day on Mercury (from one sunrise to the next) lasts the equivalent of 176 Earth days, or twice as long as its year of 88 days.
Mercury never strays more than 27 degrees from the Sun (this is the angle of the clock hands when it is one o'clock). Learn more.
Beneath a thin layer of rock, Mercury hides a iron core that is proportionally gigantic: it represents about 85% of the planet's radius, compared to only 55% for Earth. This oversized core explains Mercury's exceptionally high density, the second highest in the Solar System, just behind Earth. Its origin remains debated: a giant impact could have torn away a large part of the planet's primitive mantle, leaving only a disproportionate core.
Despite its very slow rotation, Mercury generates a global magnetic field, about 100 times weaker than Earth's but very real. Its very existence intrigues scientists: for a planet so small and with such slow rotation, one would expect the metallic core to have long since solidified, which would make an internal dynamo impossible. Understanding how this magnetic field persists is one of the main objectives of the European and Japanese BepiColombo mission, whose two probes are scheduled to enter orbit around Mercury in late November 2026.
Lacking a significant atmosphere to protect it, Mercury's surface bears the traces of billions of years of bombardment: it is as heavily cratered as the Moon. The most impressive of these impacts, the Caloris Basin, measures about 1,550 km in diameter. The planet also has lobate scarps, long cliffs formed by the cooling and contraction of the core over billions of years, which have shrunk the planet's diameter by several kilometers.
Sources:
• NASA Science – Mercury, https://science.nasa.gov/mercury/
• NASA Solar System Exploration – Mercury Facts, https://solarsystem.nasa.gov/planets/mercury/overview/
• ESA – BepiColombo Mission, https://www.esa.int/Science_Exploration/Space_Science/BepiColombo
• CNES – BepiColombo, https://cnes.fr/projets/bepicolombo
• NASA – MESSENGER Mission, https://science.nasa.gov/mission/messenger/
Mercury experiences the greatest temperature variations in the Solar System (430°C during the day, -180°C at night) for two reasons:
• Its proximity to the Sun: the exposed side receives intense radiation.
• Its almost total lack of atmosphere: without air to retain heat, the night side cools immediately. No other planet has such a violent thermal contrast between its day and night sides.
Although the equatorial surface is scorching, craters located at the poles (North and South) have their bottoms permanently in shadow from the Sun's rays, as Mercury has almost no axial tilt (0.034°). These cold traps act as cosmic freezers, preserving water ice and other organic volatiles that would instantly vaporize elsewhere. This discovery was confirmed by the Messenger mission.
The 3:2 spin-orbit resonance means that Mercury rotates three times on itself for two orbits around the Sun. This is due to the planet's eccentric orbit and the Sun's tidal forces. As a result, a solar day (from one sunrise to the next) lasts 176 Earth days, or twice as long as its year (88 days).
Mercury has the most eccentric orbit (0.205) of all the planets in the Solar System. Its distance from the Sun varies enormously: 46 million km at perihelion (closest) and 70 million km at aphelion (farthest). This high eccentricity is likely the result of ancient gravitational perturbations, particularly from interactions with Jupiter and Venus.
The Messenger mission (NASA, 2004–2015) made several major discoveries:
• Confirmation of the presence of water ice and frozen organic materials in polar craters.
• Detailed mapping of the surface, revealing well-preserved volcanoes and craters.
• The discovery that Mercury has an extremely large metallic core (about 85% of its radius), giving it a magnetic field.
• Detection of sulfur and other volatile elements on its surface, indicating a composition different from other terrestrial planets.
Mercury has an extremely tenuous exosphere, not a true atmosphere. It is composed of atoms released from the surface by the solar wind and meteoroid impacts, including hydrogen, helium, sodium, potassium, and calcium. Its pressure is less than 10⁻¹⁴ bar (about one trillionth of a billionth of Earth's atmospheric pressure), making it negligible for thermal regulation.