Which one of the following is the narrow belt parallel to the Shiwalik foothills where streams and rivers coming from the mountains deposit heavy materials of rocks and boulders?
Bhabar
The question asks us to identify a specific geographic division within the Northern Plains of India, located parallel to the Shiwalik foothills. This region is characterized by the deposition of heavy materials like rocks and boulders brought down by streams and rivers from the mountains. Let's examine the options provided to find the correct answer.
The vast Northern Plains of India can be broadly divided into different regions based on the depositional features brought down by rivers. Moving from the mountains towards the peninsular plateau, these belts are:
Let's look at the characteristics of each option:
Based on the analysis, the belt parallel to the Shiwalik foothills where streams deposit heavy materials of rocks and boulders is the Bhabar belt. This region is known for its coarse alluvial fans where the rivers lose energy quickly and drop larger sediments.
| Region | Location | Characteristics | Material |
|---|---|---|---|
| Bhabar | Parallel to Shiwaliks, 8-16 km wide | Streams disappear, porous | Pebbles, boulders, coarse sediments |
| Tarai | South of Bhabar | Wet, marshy, forested, streams re-emerge | Fine silt, clay (deposited as streams slow down) |
| Bhangar | Older alluvial plain, above flood level | Less fertile (compared to Khadar), Kankar nodules | Older alluvium |
| Khadar | Newer alluvial plain, floodplains | Very fertile, flooded annually | Newer alluvium, fine silt, clay |
Therefore, the Bhabar belt is the region that fits the description provided in the question.
| Belt | Width | Sediment Size | Stream Behavior |
|---|---|---|---|
| Bhabar | 8-16 km | Coarse (boulders, pebbles) | Streams disappear |
| Tarai | 15-30 km | Fine (silt, clay) | Streams re-emerge |
| Bhangar | Varies (older plain) | Older alluvium, Kankar | Above flood level |
| Khadar | Varies (floodplain) | Newer alluvium | Flooded annually |
The Bhabar belt, while not suitable for extensive agriculture due to the presence of large boulders and porous soil, is important for several reasons. The underground water table is quite high, and larger rivers often manage to flow on the surface. This region transitions into the Tarai belt, where the groundwater resurfaces, supporting dense vegetation and wildlife. The Bhabar region's primary characteristic is the significant deposition of coarse material as rivers exit the steeper slopes of the Shiwaliks and enter the flatter plains, leading to a rapid loss of carrying capacity.
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