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Io writes its history in hot metal

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  • Lionel Wilson

    (Lancaster University)

Abstract

The Galileo spacecraft has measured the temperature of lava flows on Jupiter's moon Io. At 1,700 to 2,000 K, they are far hotter than all previous estimates, implying that they are metal rich and therefore dense. It is difficult for dense lavas to erupt through a light crust, so perhaps Io has undergone relatively little heating and differentiation in the past, and still has a dense crust.

Suggested Citation

  • Lionel Wilson, 1998. "Io writes its history in hot metal," Nature, Nature, vol. 394(6693), pages 520-521, August.
    • Handle: RePEc:nat:nature:v:394:y:1998:i:6693:d:10.1038_28945
    DOI: 10.1038/28945
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