In what region of Mercury would you find the intercrater plains?

The intercrater plains of Mercury are primarily found in heavily cratered areas. This region is characterized by a relatively smooth and flat landscape that exists between the larger craters. These plains are thought to be the result of volcanic activity and the subsequent infilling of impact craters over geological time.

Heavily cratered areas indicate regions that have been impacted by numerous meteorites, contributing to the complex geology of Mercury. The smoothness of the intercrater plains contrasts with the ruggedness of the craters and suggests that volcanic material has been deposited in these locations, thereby modifying the landscape. Therefore, identifying intercrater plains in heavily cratered areas emphasizes their formation history and geological significance on Mercury.