Analysis of images from the HiRISE (High Resolution Imaging Science Experiment) camera, on the Mars Reconnaissance Orbiter seems to indicate that warming weather on Mars may have melted ice-rich soils as recently as 2 million years ago. The geographical features that point to this event were originally thought to have been volcanic in origin, but Matthew Balme, a research scientist with the Tucson-based Planetary Science Institute has looked afresh at the images and now believes they were formed by the expansion and contraction of ice due to freeze/thaw cycles. If true, then the equator region would be an ideal place to look for signs of past life.