Tags: Crater.
Raditladi Basin is a large peak ring impact crater on Mercury with a diameter of 263 km. Inside its peak ring there is a system of concentric extensional troughs (graben) which are rare surface features on Mercury. The floor of Raditladi is partially covered by relatively light smooth plains which are thought to be a product of the effusive volcanism. The troughs may also have resulted from volcanic processes under the floor of Raditladi.
