This computer-generated perspective view of Nereidum Montes was created using data obtained from the High-Resolution Stereo Camera (HRSC) on ESA’s Mars Express. Centred at around 40°S and 310°E, the image has a ground resolution of about 23 m per pixel. In the foreground near to the crater, a mud or ice-landslide is seen, possibly due to glacial processes. The striations along the slopes of both the right side of the inner crater wall and on the slopes of the range to the left of the crater indicate the presence of ice.