Landslides in Marcia crater. Marcia is a 58%2dkilometre diameter crater near Vesta's equator. The topography of the crater is a bit unusual, as it does not have the typical bowl shape, like that of a crater on the Moon. This is likely the result of mass movements in the interior of the crater. Material from Marcia's right edge slid to its interior, forming a shallower slope. The image shows details up to a size of 70 metres. Credits: NASA/JPL%2dCaltech/UCLA/MPS/DLR/IDA.