The Global Topography of Mars and Implications for Surface Evolution

David E. Smith(Goddard Space Flight Center), M. T. Zuber(Goddard Space Flight Center), Sean C. Solomon(Carnegie Institution for Science), R. J. Phillips(Washington University in St. Louis), J. W. Head(Brown University), J. B. Garvin(Goddard Space Flight Center), W. B. Banerdt(Jet Propulsion Laboratory), D. O. Muhleman(California Institute of Technology), G. H. Pettengill(Massachusetts Institute of Technology), G. A. Neumann(Goddard Space Flight Center), F. G. Lemoine(Goddard Space Flight Center), James B. Abshire(Goddard Space Flight Center), O. Aharonson(Massachusetts Institute of Technology), Cristiam David, Brown(Washington University in St. Louis), S. A. Hauck(Washington University in St. Louis), A. B. Ivanov(California Institute of Technology), P. J. McGovern(Carnegie Institution for Science), H. Jay Zwally(Goddard Space Flight Center), T. Duxbury(Jet Propulsion Laboratory)
Cited by 929

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.


Related Papers

No related papers found

Powered by citation graph analysis