Faults in Olivine-Rich Terrain
This observation is in the Northern Hemisphere of Mars, in a region northeast of Alba Patera, between Tantalus Fossae and Mareotis Fossae. Both are a group of troughs that likely formed due to the stretching and faulting of the planet’s crust.
Image is less than 5 km (3 mi) across and is 296 km (184 mi) above the surface. For full images including scale bars, please visit the below link.