In the Geography chapter 'Physical Features of India' (Class 9), the massive Northern Plains are formed by the alluvial soil brought down by the Himalayan rivers. This alluvial soil is divided into two distinct categories based on its age and location: Bhangar and Khadar.
Together, Bhangar and Khadar make the Northern Plains the most agriculturally productive and densely populated region in India.
A third, related term is 'Bhabar', which is a narrow belt of porous pebbles at the very foot of the Himalayas where river streams completely disappear underground.
| Feature | Bhangar | Khadar |
|---|---|---|
| Age | Old Alluvium | New Alluvium |
| Location | Away from the river (higher ground) | Near the river banks (floodplains) |
| Renewal | Not renewed frequently | Renewed almost every year by floods |
| Texture | Coarse, contains 'Kankar' nodules | Very fine, smooth, and sandy |
| Fertility | Less fertile | Highly fertile |
States located in the Indo-Gangetic plain, such as Punjab, Haryana, Uttar Pradesh, Bihar, and West Bengal, are primarily covered by Bhangar and Khadar soils.
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