EVIDENCE FOR THERMAL FATIGUE ON MARS FROM ROCKFALL PATTERNS ON IMPACT CRATER SLOPES

International audience; Introduction: Individual block falls are one of the currently active surface processes on Mars. Similarly to Earth, clasts detach from upslope outcrops roll or bounce downslope, leaving a track on the substratum (Fig. 1). The trails show that the rockfalls are recent, as aeolian processes would infill topographic lows over time. Using rover-track erasure rates, these tracks are likely