Cited by 941Planetary Science and ExplorationAstro and Planetary ScienceGeological Modeling and Analysis

The Global Topography of Mars and Implications for Surface Evolution

Smith, David E., Zuber, Maria T., Solomon, Sean C., Phillips, Roger J., Head, James W., Garvin, James B., Banerdt, W. Bruce, Muhleman, Duane O. +12 more·1999·Science

Abstract

Elevations measured by the Mars Orbiter Laser Altimeter have yielded a high-accuracy global map of the topography of Mars. Dominant features include the low northern hemisphere, the Tharsis province, and the Hellas impact basin. The northern hemisphere depression is primarily a long-wavelength effect that has been shaped by an internal mechanism. The topography of Tharsis consists of two broad rises. Material excavated from Hellas contributes to the high elevation of the southern hemisphere and to the scarp along the hemispheric boundary. The present topography has three major drainage centers, with the northern lowlands being the largest. The two polar cap volumes yield an upper limit of the present surface water inventory of 3.2 to 4.7 million cubic kilometers.

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Crossref · 10.1126/science.284.5419.1495

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  • Carbonate-bearing rocks in Lucaya's central pit today lie at a MOLA elevation of ~1.4-1.5 km relative datum.

    “The carbonate-bearing rocks in Lucaya's central pit today lie at a MOLA elevation of ~1.4-1.5 km relative datum [Smith et al., 1999].”

    From Orbital evidence for more widespread carbonate-bearing rocks on Mars (2016) · cites this paper as Smith et al., 1999

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Authors
Smith, D. E., Zuber, M. T., Solomon, S. C., Phillips, R. J., Head, J. W., Garvin, J. B., Banerdt, W. B., Muhleman, D. O., Pettengill, G. H., Neumann, G. A., Lemoine, F. G., Abshire, J. B., Aharonson, O., David, C., Brown, Hauck, S. A., Ivanov, A. B., McGovern, P. J., Zwally, H. J., & Duxbury, T. C.
Affiliations
  • Goddard Space Flight Center (US)
  • Carnegie Institution for Science (US)
  • Washington University in St. Louis (US)
  • Department of Geological Sciences, Brown University, Providence, RI 02912, USA.
  • Jet Propulsion Laboratory (US)
  • California Institute of Technology (US)
  • Massachusetts Institute of Technology (US)
Corresponding author
Smith, David E.
Venue
Science
Published
1999-05-28
Volume
284
Issue
5419
Pages
1495-1503
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2147284262
Cited by
941
References
3
Citations by year
2026: 16 · 2025: 17 · 2024: 28 · 2023: 30 · 2022: 34 · 2021: 32 · 2020: 16 · 2019: 72 · 2018: 33 · 2017: 37 · 2016: 22 · 2015: 35 · 2014: 25 · 2013: 28 · 2012: 26
FWCI
47.49
Type
journal article
Language
en
Open access
closed
Locations
  • Science (publishedVersion)
  • PubMed (publishedVersion)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Planetary Science and Exploration
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological Modeling and Analysis
Keywords
Mars topography, Mars Orbiter Laser Altimeter, Mars surface evolution, hemispheric dichotomy, watershed, polar cap
MeSH terms
Extraterrestrial Environment, Ice, Water, Mars, Evolution, Planetary

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