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A comparison of volcanic eruption processes on Earth, Moon, Mars, Io and Venus

Nature volume 302, pages 663–669 (1983)Cite this article

Abstract

The silicate planets and satellites display a wide range of physical, chemical and atmospheric characteristics which may influence the nature of volcanism, a major geological process common to the evolution of the surfaces of these bodies. Consideration of the process of magma ascent and eruption from first principles allows predictions to be made concerning volcanic eruption styles and expected landforms and deposits on each planetary body. Examination of actual land-forms and deposits in light of these predictions leads to a better understanding of the nature of volcanic eruption processes and outlines outstanding problems.

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  1. Department of Geological Sciences, Brown University, Providence, Rhode Island, 02912, USA

    Lionel Wilson & James W. Head III

  2. Lunar and Planetary Unit, Department of Environmental Sciences, University of Lancaster, Lancaster, LA1 4YQ, UK

    Lionel Wilson

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Wilson, L., Head, J. A comparison of volcanic eruption processes on Earth, Moon, Mars, Io and Venus. Nature 302, 663–669 (1983). https://doi.org/10.1038/302663a0

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