BRIEF SURVEY OF MERCURY |
|
| Distance from sun: Perihelion | 46,000,000 km (28,600,000 mi) |
| Distance from sun: Mean | 58,000,000 km (36,000,000 mi) |
| Distance from sun: Aphelion | 70,000,000 km (43,500,000 mi) |
| Period of revolution | 88 earth days |
| Rotation period | 58.7 earth days |
| Eccentricity of orbit | 0.21 |
| Inclination of orbit | 7° |
| Mass (earth = 1) | 0.06 |
| Diameter | 4875 km (3030 mi) |
| Mean density (water = 1) | 5.4 |
| Natural satellites | 0 |
Spectroscopic studies indicate that only an extremely thin atmosphere, containing sodium and potassium, exists on Mercury, its atoms apparently diffusing from the crust of the planet. Collisions with other protoplanets early in the history of the solar system may have stripped away lighter materials, thereby accounting for Mercury’s great density. The force of gravity on the planet’s surface is about one-third of that on earth’s surface.
The Mariner 10 spacecraft passed Mercury twice in 1974 and once in 1975. It sent back pictures of a moonlike, crater-pocked surface and reported temperatures to be about 430° C (about 810° F) on the sunlit side and about –180° C (about –290° F) on the dark side. Mariner 10 also detected a magnetic field 1 percent that of the earth. Unlike that of the earth’s moon, the surface of Mercury is crisscrossed by long escarpments, dating perhaps from the period of contraction the planet experienced as it cooled some time early in its history.
In 1991 powerful radio telescopes on earth revealed unmistakable signals of vast sheets of ice in Mercury’s polar regions, areas that had not been covered by Mariner 10.
The perihelion (the point closest to the sun) in the orbit of Mercury advances at a slow rate. A full explanation of the motion of its orbit according to relativistic concepts was one of the first confirmations of the theory of relativity.
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