Evidence for a subsurface ocean on Europa (original) (raw)
- Letter
- Published: 22 January 1998
- Michael J. S. Belton2,
- Clark R. Chapman3,
- Merton E. Davies4,
- Paul Geissler5,
- Richard Greenberg5,
- Alfred S. McEwen5,
- Bruce R. Tufts5,
- Ronald Greeley6,
- Robert Sullivan7,
- James W. Head8,
- Robert T. Pappalardo8,
- Kenneth P. Klaasen9,
- Torrence V. Johnson9,
- James Kaufman9,
- David Senske9,
- Jeffrey Moore10,
- Gerhard Neukum11,
- Gerald Schubert12,
- Joseph A. Burns7,
- Peter Thomas7 &
- …
- Joseph Veverka7
Nature volume 391, pages 363–365 (1998)Cite this article
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Abstract
Ground-based spectroscopy of Jupiter's moon Europa, combined with gravity data, suggests that the satellite has an icy crust roughly 150 km thick and a rocky interior1,2,3,4. In addition, images obtained by the Voyager spacecraft revealed that Europa's surface is crossed by numerous intersecting ridges and dark bands (called lineae) and is sparsely cratered, indicating that the terrain is probably significantly younger than that of Ganymede and Callisto5. It has been suggested that Europa's thin outer ice shell might be separated from the moon's silicate interior by a liquid water layer, delayed or prevented from freezing by tidal heating6,7,8,9,10; in this model, the lineae could be explained by repetitive tidal deformation of the outer ice shell11,12,13. However, observational confirmation of a subsurface ocean was largely frustrated by the low resolution (>2 km per pixel) of the Voyager images14. Here we present high-resolution (54 m per pixel) Galileo spacecraft images of Europa, in which we find evidence for mobile ‘icebergs’. The detailed morphology of the terrain strongly supports the presence of liquid water at shallow depths below the surface, either today or at some time in the past. Moreover, lower-resolution observations of much larger regions suggest that the phenomena reported here are widespread.
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Authors and Affiliations
- US Geological Survey, 345 Middlefield Road, Menlo Park, 94025, California, USA
Michael H. Carr - National Optical Astronomy Observatory, 950 Cherry Street, Tucson, 85719, Arizona, USA
Michael J. S. Belton - Southwest Research Institute, 1050 Walnut Street, Boulder, 8030, Colorado, USA
Clark R. Chapman - Rand Corporation, 1700 Main Street, Santa Monica, 90406, California, USA
Merton E. Davies - Lunar and Planetary Laboratory, University of Arizona, Tucson, 85721, Arizona, USA
Paul Geissler, Richard Greenberg, Alfred S. McEwen & Bruce R. Tufts - Geology Department, Arizona State University, Tempe, 85287, Arizona, USA
Ronald Greeley - Cornell University, Ithaca, 14853, New York, USA
Robert Sullivan, Joseph A. Burns, Peter Thomas & Joseph Veverka - Geology Department, Brown University, Providence, 02912, Rhode Island, USA
James W. Head & Robert T. Pappalardo - Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, 911909, California, USA
Kenneth P. Klaasen, Torrence V. Johnson, James Kaufman & David Senske - NASA/Ames Research Center, Moffet Field, 94035, California, USA
Jeffrey Moore - DLR-Institut für Planetenerkundung, Rudower Chaussee 5, 12489, Berlin, Germany
Gerhard Neukum - Department of Earth and Space Sciences, University of California, Los Angeles, 90095, California, USA
Gerald Schubert
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Carr, M., Belton, M., Chapman, C. et al. Evidence for a subsurface ocean on Europa.Nature 391, 363–365 (1998). https://doi.org/10.1038/34857
- Received: 19 May 1997
- Accepted: 05 November 1997
- Issue Date: 22 January 1998
- DOI: https://doi.org/10.1038/34857
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