After the impact, new rocks would continue to form in Southern Africa, and all the geological processes described above are still continuing today.
Nga murahu ha zwe zwa tshinyadziwa, hu mbo ḓi thoma manwe matombo kha ḽa Southern Africa, vhoṱhe vha vho ṱalutshedziwaho zwa geological nṱha zwi kha ḓi ya phanḓa na zwino.