Areas of incipient drain structure are sporadically developed, as are areas of scalding Confined stream terrace Sinuous channel within a confined meander belt, internally characterised by abundant scroll bars forming arcuate ridge and swale channel facies topography Ephemeral channel Unconfined stream terrace Lacustrine units Lunette Arcuate (convex-east)
crescentic dunes adjacent to and on the eastern side of dry lakes.