Anaglyph images are produced using the data acquired by the nadir channel of the Mars Express High Resolution Stereo Camera (HRSC), the field of view of which is aligned perpendicular to the surface of Mars, and one of the four obliquely angled stereo channels. Anaglyphs create a realistic, three-dimensional impression of the landscape when viewed through red/blue or red/green glasses. This makes it easy to see that the numerous craters in the centre of the image, which originally would have had a bowl-shape, have been flooded by thin lava and sometimes filled almost to their edges with volcanic deposits. By contrast, the large crater at the right hand (northern) edge of the image, which is approximately 30 kilometres wide, has a formidable crater rim which would have prevented the lava from the flood to flow into the inside of the crater, which is approximately 2500 metres deep. Using the zoom function we can examine the Cerberus Fossae rift valley, whose width exceeds one kilometre in just a few places.