This observation shows lightly cratered plains in Elysium Planitia, a low-lying area located in the equatorial region of Mars. Part of the fault system known as the Cerberus Fossae runs through the center of this image. Elsewhere in Elysium Planitia, the Cerberus Fossae acted as a fissure-vent for erupting flood lavas, but here the geological activity appears to have been predominantly tectonic. Nonetheless, the raised, lobate (tongue-shaped) margin of an ancient lava flow is faintly discernible in the southern part of the image. Near the center of the image, a few relatively deep depressions, partly filled with dark sand, are visible in the Cerberus Fossae. These are pit craters formed by collapse as normal faulting progressed. The largest pit crater is about 110 meters (360 feet) wide and about 300 meters (980 feet) long.