Q5. How many of the following statements are correct regarding geomorphological features of the Indo-Ganga-Brahmaputra Plain?
- Bhabar region has high porosity, causing streams to disappear underground.
- Terai is marshy and swampy because rivers re-emerge from Bhabar.
- Khadar plains lie above flood levels and are composed of older alluvium.
- Bangar is less fertile than Khadar but can be cultivated with irrigation.
Select the correct option:
Answer: C [Only three ]
Explanation: Explanation:
Statement 1 is correct: Bhabar is the northernmost zone of the Indo-Gangetic plains, located along the foothills of the Shivaliks. It is composed of coarse sediments such as boulders, pebbles, and gravel, deposited by fast-flowing Himalayan streams.
Because these materials have very high porosity and permeability, the streams disappear underground as soon as they enter the Bhabar belt.
Statement 2 is correct: Just south of the Bhabar lies the Terai region, where the gradient decreases and the underground water from Bhabar resurfaces. This results in marshy, swampy land, with lush vegetation and high groundwater levels. The Terai is therefore characterized by wetlands and thick forests, formed due to the re-emergence of rivers lost in the Bhabar zone.
Statement 3 is incorrect: Khadar refers to the younger alluvium, deposited annually by river floods. It forms the active floodplains, which are lower in elevation and highly fertile.
The statement wrongly describes Khadar as being “above flood levels” and made of “older alluvium”—these are characteristics of Bhangar, not Khadar.
Statement 4 is correct: Bangar consists of older alluvium and lies on the higher terraces, away from the active floodplains. It is less fertile than Khadar because it contains kankar (calcareous concretions) that reduce soil fertility.
However, Bangar soils can still be cultivated effectively when supported by adequate irrigation, making them productive despite being comparatively less fertile.