Physical properties of the planet MercuryThe global physical properties of Mercury are summarized with attention given to its figure and orbital parameters. The combination of properties suggests that Mercury has an extensive iron-rich core, possibly with a still-functioning dynamo, which is 42 percent of the interior by volume. Mercury's three major axes are comparable in size, indicating that the planet is a triaxial ellipsoid rather than an oblate spheroid. In terms of the domination of its surface by an intermediate plains terrane, it is more Venus- or Mars-like; however, due to the presence of a large metallic magnetic core, its interior may be more earth-like.
Document ID
19880064978
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Clark, Pamela E. (California Institute of Technology Jet Propulsion Laboratory, Pasadena, United States)