Fig. 6From: Sensitivity of elastic thickness to water in the Martian lithosphereRheological structures of the Martian lithosphere at Pavonis Mons, Alba Patera, and NE Arabia Terra calculated under dry (a) and wet (b) conditions. The plastic strength changes across the crust-mantle boundary (Moho) due to a change in flow laws. Elastic thickness was calculated from the integrated bending moment within the lithosphere (see text for details)Back to article page