Possible Ancient Oceans on Mars: Evidence from Mars Orbiter Laser Altimeter Data

Author:

Head James W.1,Hiesinger Harald1,Ivanov Mikhail A.12,Kreslavsky Mikhail A.13,Pratt Stephen1,Thomson Bradley J.1

Affiliation:

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

2. Vernadsky Institute, Russian Academy of Sciences, Kosygina 19, 117975, Moscow, Russia.

3. Kharkov Astronomical Observatory, Kharkov University, Sumska 35, 310022, Kharkov, Ukraine.

Abstract

High-resolution altimetric data define the detailed topography of the northern lowlands of Mars, and a range of data is consistent with the hypothesis that a lowland-encircling geologic contact represents the ancient shoreline of a large standing body of water present in middle Mars history. The contact altitude is close to an equipotential line, the topography is smoother at all scales below the contact than above it, the volume enclosed by this contact is within the range of estimates of available water on Mars, and a series of extensive terraces parallel the contact in many places.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference44 articles.

1. M. H. Carr Water on Mars (Oxford Univ. Press New York 1996).

2. V. R. Baker et al. in Mars H. H. Kieffer B. M. Jakosky C. W. Snyder M. S. Matthews Eds. (Univ. of Arizona Press Tucson AZ 1992) pp. 493–522.

3. S. W. Squyres et al. in Mars H. H. Kieffer B. M. Jakosky C. W. Snyder M. S. Matthews Eds. (Univ. of Arizona Press Tucson AZ 1992) pp. 523–554.

4. P. Thomas et al. in Mars H. H. Kieffer B. M. Jakosky C. W. Snyder M. S. Matthews Eds. (Univ. of Arizona Press Tucson AZ 1992) pp. 767–795.

5. K. L. Tanaka and D. H. Scott U.S. Geol. Surv. Misc. Invest. Ser. Map I-1802-C (1987).

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