northern plains have diverse relief feature justify
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The most characteristic feature of the great plains of Northern India is their extreme horizontality. From the geomorphological aspect there is no difference between the Indus basin and the Ganga-Brahmaputra basin.
They are classified into four distinct divisions:
1. Bhabar belt: made up of pebbles and boulders, the streams flow underground, adjacent to foothills
2. Terai belt: composed of new alluvium, region is damped and thickly forested and receives heavy rainfall throughout the year and has a variety of wildlife.
3. Bangar Belt: composed of old alluvium, forms Gangetic delta, covered by laterite deposits
4. Khadar Belt: made up of new alluvium of the flood zones.
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They are classified into four distinct divisions:
1. Bhabar belt: made up of pebbles and boulders, the streams flow underground, adjacent to foothills
2. Terai belt: composed of new alluvium, region is damped and thickly forested and receives heavy rainfall throughout the year and has a variety of wildlife.
3. Bangar Belt: composed of old alluvium, forms Gangetic delta, covered by laterite deposits
4. Khadar Belt: made up of new alluvium of the flood zones.
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