The Bhangar is composed of old alluvium of the Middle Pleistocene age and forms the alluvial terrace above the level of floodplains.
Remnants of the Bhangar are eroded by every change in the direction of river channels and are being leveled down by their meandering tendencies.
On the other hand, the Khadar is composed of newer alluvium and forms the floodplains along the river banks. A new layer of alluvium is deposited by river flood almost every year. These deposits are normally confined to the vicinity of the present river channels.
The khadar imperceptibly mergers into the deltic and other accumulation of prehistoric times.