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ReportsAmalthea's Density Is Less Than That of Water![]() ![]()
Radio Doppler data from the Galileo spacecraft's encounter with Amalthea, one of Jupiter's small inner moons, on 5 November 2002 yield a mass of (2.08 ± 0.15) x 1018 kilograms. Images of Amalthea from two Voyager spacecraft in 1979 and Galileo imaging between November 1996 and June 1997 yield a volume of (2.43 ± 0.22) x 106 cubic kilometers. The satellite thus has a density of 857 ± 99 kilograms per cubic meter. We suggest that Amalthea is porous and composed of water ice, as well as rocky material, and thus formed in a cold region of the solar system, possibly not at its present location near Jupiter.
1 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA.
2 Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA. 3 Institute of Geophysics and Planetary Physics, Los Angeles, CA 90095-1567, USA. 4 Center for Radio Physics and Space Research, Cornell University, Ithaca, NY 14853-4901, USA. 5 Institute of Geodesy and Geophysics, Vienna University of Technology, A-1040 Vienna, Austria.
* To whom correspondence should be addressed. E-mail: john.d.anderson{at}jpl.nasa.gov
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Science. ISSN 0036-8075 (print), 1095-9203 (online)