The topography of Mars is represented by a spherical harmonic model co
mplete to degree and order 50. The data source is a recently revised U
.S. Geological Survey compilation which encompasses a diverse array of
spacecraft measurements and Earth-based radar ranges. Because of the
disparate nature of the original data sources, it is difficult to obta
in reliable estimates of the likely errors in Martian topography. Howe
ver, the variance spectrum has a shape similar to that found for other
terrestrial planets, and the topography correlates well with recent e
stimates of the gravitational field of Mars. Both of these considerati
ons suggest that the existing data provide a reasonable approximation
to the true topography of Mars. Nevertheless, a detailed topographic m
apping of the planet, such as will be provided by the Mars Global Surv
eyor, will be required before significant advances are made in underst
anding the relationship between topography and gravity on Mars.