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| | PSR Discoveries:Hot Idea: Hot, Mushy Io |
 | | If correct, Io gives us an opportunity to study processes that operate in huge, global magma systems, which scientists believe were important during the early history of the Moon and Earth, and possibly other planetary bodies as well. |
 | | Current estimates of the density of Io's interior range from 3.148 to 3.878 grams per cubic centimeter, though the currently favored value is 3.280, closer to the mushy than to the solid interior. |
 | | For example, Io is being heated continuously, so it does not allow formation of a crust by the floatation of low-density mineral grains, as happened on the Moon. |
| www.psrd.hawaii.edu /Feb00/IoMagmaOcean.html (1910 words) |
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