Explain the classification of northern plains on the basis of the variation in relief features
Answers
Explanation:
Physical Features of India : Classify the northern plains on the basis of variation in the relief features. Ans : - Northern plains are alluvial plains formed by deposition of sediments brought down by the rivers. ... The stream disappear in this belt as the bhabar plain.
Answer:
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Based on the relief features; the northern plain can be divided into four regions, viz. Bhabar, Terai, Bhangar and Khadar.
1. Bhabar:
After descending from the mountains, the rivers deposit pebbles in a narrow belt.The width of this belt is about 8 to 16 kms.It lies parallel to the Shiwaliks.Bhabhar is the gently-sloping coarse alluvial zone below the Siwalik Hills (outermost foothills of Himalayas) where streams disappear into permeable sediments. The underground water level is deep in this region.
2. Terai:
The Terai region lies towards the south of the bhabar belt. In this region, the streams reappear and make a wet, swampy and marshy region. This region was full of forest and wildlife but after partition, all this area was cleared and was converted into agricultural land for the settlement of the migrants.
3. Bhangar:
Bhangar is the largest part of the northern plain and is composed of the oldest alluvial soil. They lie above the flood plains. They resemble terraces. The soil of this region is locally known as kankar and is composed of calcareous deposits.
4. Khadar:
The floodplains formed by younger alluvium are called Khadar.The soil in this region is renewed every year and is highly fertile.This region is very suitable for intensive agricultural activities.
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