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Bhabar is a narrow belt ranging between 8-10 km parallel to the Shiwalik foothills at the break-up of the slope.
South of the Bhabar is the Tarai belt, with an approximate width of 10-20 km. Here, most of the streams and rivers re-emerge without having any properly demarcated channel, thereby, creating marshy and swampy conditions known as the Tarai.
Khadar is composed of newer alluvium and forms the flood plains along the river banks.
Bhangar is the older alluvium that are formed along the river beds, thus forming terraces higher than the flood plain.
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