One alluvial soil in the Gangetic plains gets a fresh layer almost every single year. Rivers renew it faster than farmers can wear it out. This article covers Khadar soil: how it forms, and why it stays so fertile.


Must Know
- Khadar is the newer alluvium of the Indo-Gangetic Plain, deposited in low-lying floodplains close to river level.
- It is renewed almost every year, as monsoon floods deposit fresh silt, clay, and nutrients.
- This is distinct from Bhangar, the older, higher-terrace alluvium. Floods no longer reach it, and it is covered in IndGeo0080.
- In Punjab, Khadar-rich floodplains are known locally as “Bet,” or “Betlands,” a local farming term.
- Khadar supports crops including rice, wheat, sugarcane, and oilseeds, and ranks among the most productive farmland in the Ganges basin.
Good to Know
- Khadar is found widely across Punjab, Haryana, Uttar Pradesh, Bihar, and West Bengal, concentrated along the major river floodplains.
- Unlike Bhangar, Khadar generally lacks the alkaline kankar nodules that can reduce fertility in older alluvium.
- Khadar’s texture ranges from sandy loam to fine clay, varying with how far a plot sits from the active river channel.
Test Yourself
Great to Know
- Khadar and Bhangar sit only a short distance apart geographically, yet differ sharply in fertility and stability. Elevation, not distance, decides which soil a plot of land actually has.
- Relying on annual floods for fertility is a double-edged trait. The same floods that renew Khadar’s nutrients can also destroy crops and property in a bad monsoon year.
- Farmers have long favoured Khadar for its yield, despite the flood risk. That choice shows how short-term productivity often outweighs long-term risk in real farming decisions.
Leave a Reply