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Progress in Earth and Planetary Science
Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

From: Iron snow, crystal floats, and inner-core growth: modes of core solidification and implications for dynamos in terrestrial planets and moons

Fig. 10

Global magnetic map of Mars. Map of the lithospheric part of the magnetic field model evaluated at the mean planetary radius of 3393.5 km. (top to bottom) The magnetic field intensity and the vertically down (Z), horizontally east (Y), and north (X) components are shown. (left to right) The north pole, mid-latitudes, and south pole are presented. Major impact basins are indicated by dashed lines, while the thick black line represents the zero level of the Mars Observer Laser Altimeter (MOLA) topography, indicating the topographic dichotomy boundary (after Morschhauser et al. 2014)

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