This oblique view of the sloping edge of the stack of icy layers over the South Pole has some interesting morphologies.
The slope appears to be eroding from a combination of landslides, block falls, and sublimation. The bright icy exposure in the larger landslide scar (upper right) suggests that this was a relatively recent event.
Small-scale textures over the scene are due to both blowing wind and the thermal expansion and contraction of shallow ice.