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Badland topography is a characteristic feature of -
Question

Badland topography is a characteristic feature of -

A.

Nagauri Upland

B.

Ghaggar Basin

C.

Shekhawati Region

D.

Chambal Basin

Correct option is D

Ans. (d)
Badland topography refers to a landscape characterized by highly eroded landforms with deep gullies, ravines, and barren surfaces. It is formed due to intense water erosion, particularly in regions with weak and easily erodible rock structures. The Chambal Basin, located in central India, is widely known for its extensive badland topography.
The Chambal River and its tributaries have deeply eroded the soft alluvial deposits over time, creating numerous ravines. This makes the Chambal Valley a classic example of badland topography in India. Other rivers such as the Yamuna and Betwa also contribute to this type of erosion in adjoining regions.
Information Booster
· Badland topography is caused by gully erosion due to running water.
· The Chambal River is notorious for its deep ravines, making it difficult for agriculture and habitation.
· Such landscapes are also found in parts of Madhya Pradesh, Rajasthan, and Uttar Pradesh.
· The region is often associated with banditry in the past due to its inaccessible terrain.
· Similar badland formations are found in Dakshina Kannada (Karnataka) and parts of Maharashtra.
Additional Knowledge
1. Nagauri Upland – Incorrect
· Located in Rajasthan, this is a plateau-like region with semi-arid conditions.
· It lacks significant river erosion required for badland formation.
2. Ghaggar Basin – Incorrect
· The Ghaggar River is a seasonal river that does not create extensive erosion.
· The area is primarily a dry riverbed with little evidence of badland topography.
3. Shekhawati Region – Incorrect
· This region in Rajasthan is primarily semi-arid with sandy dunes.
· It does not have deep ravines or significant water erosion.
4. Chambal Basin – Correct
· Characterized by ravines, deep gullies, and dissected landforms.
· One of the most well-known badland regions in India.
· Formed due to the erosional activity of the Chambal River and its tributaries.

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