The impact ejecta and chains of secondary craters extend as far as one radius from the rim.

Monoliths also occur naturally on Earth, but it has been suggested that the Phobos monolith may be a piece of impact ejecta.

The areas outside Raditladi are covered by the dark relatively blue impact ejecta.

The significant asymmetry in distribution of the impact ejecta indicates that Lofn was formed by an oblique impact.

The rock formed from impact ejecta which was later buried by newer impacts and lithified due to the pressure from overlying layers.

Other 'cracks' are probably grooves cut by impact ejecta, and some of the ridges may be ejecta deposits.

They may be composed of impact ejecta, some of which may have been molten.

Although its sediments have not been directly sampled, cores from the area contain high levels of nickel and magnetic components associated with impact ejecta.

Many large craters are surrounded by bright impact ejecta (rays) consisting of relatively fresh ice.

It is easy for the impact ejecta to be lost from these satellites into space.