Two large lobate thrust fault scarps, cliff-like landforms formed when crustal materials are pushed together, break, and are thrust upwards, that bound Mercury’s great valley (white arrows) are shown in this high incidence angle image mosaic.
Two large lobate thrust fault scarps, cliff-like landforms formed when crustal materials are pushed together, break, and are thrust upwards, that bound Mercury’s great valley (white arrows) are shown in this high incidence angle image mosaic.