Consequences of the tidal slowing of Mercury

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Gravitational Effects, Mercury (Planet), Planetary Evolution, Planetary Rotation, Tides, Craters, Energy Dissipation, Planetary Surfaces, Planetology

Scientific paper

Several ways are discussed in which Mercury's surface and interior could have been modified by the loss of any initial angular momentum as a result of rotational slowing by solar tides. The phenomena considered include the impact of hypothetical satellites on to the planet's surface following the tidal evolution of their orbits, the distribution of surface distortion and failure due to surface stresses and strains caused by the slowing of an initially unstressed oblate body, and the heating of the planet's interior by tidal slowing as well as present-day radial tides. It is shown that these processes are significant and should have produced observable effects, but that no such effects appear in Mariner 10 photographs. The absence of such effects is taken to indicate one of the following: (1) the resulting features have been obscured, (2) better resolution and greater coverage of the planet are necessary in order to detect such features, or (3) Mercury's primordial rotation was not similar to that of other solar-system bodies.

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