Classify Northern Plains.
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On the basis of its location, the Northern Indian plains can be classified into three categories: The river Indus along with its tributaries form the Punjab Plains. The river Ganga along with its tributaries form the Ganga Plains. The river Brahmaputra with its tributary form the Brahmaputra plains.
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Answer:
The Northern Plains are broadly divided into three sections:
The Northern Plains are broadly divided into three sections:Punjab Plains: The western part of the Northern Plain is called the Punjab Plains. It is formed by the river Indus and its tributaries.
The Northern Plains are broadly divided into three sections:Punjab Plains: The western part of the Northern Plain is called the Punjab Plains. It is formed by the river Indus and its tributaries.Ganga Plains: It extends between Ghaggar and Teesta rivers. It is spread over the states of North India, z’.e., Delhi, Haryana, UP, Bihar and parts of Jharkhand and West Bengal.
The Northern Plains are broadly divided into three sections:Punjab Plains: The western part of the Northern Plain is called the Punjab Plains. It is formed by the river Indus and its tributaries.Ganga Plains: It extends between Ghaggar and Teesta rivers. It is spread over the states of North India, z’.e., Delhi, Haryana, UP, Bihar and parts of Jharkhand and West Bengal.Brahmaputra Plains: To the east of the Ganga plain lies the Brahmaputra Plain. They cover the areas of Assam and Arunachal Pradesh.
The North Plains are broadly divided into four sections on the basis of relief features :
(i) Bhabar: The rivers after descending from the mountains deposit pebbles in a narrow belt lying parallel to the slopes of the Shiwaliks. This is known as Bhabar.
(i) Bhabar: The rivers after descending from the mountains deposit pebbles in a narrow belt lying parallel to the slopes of the Shiwaliks. This is known as Bhabar.(ii) Terai: To the south of Bhabar belt, the rivers and stream re-emerge and create a wet, swampy and marshy region known as the Terai. This was a thickly forested area but was later on cleared for cultivation.
(i) Bhabar: The rivers after descending from the mountains deposit pebbles in a narrow belt lying parallel to the slopes of the Shiwaliks. This is known as Bhabar.(ii) Terai: To the south of Bhabar belt, the rivers and stream re-emerge and create a wet, swampy and marshy region known as the Terai. This was a thickly forested area but was later on cleared for cultivation.(iii) Bhangar: The largest part of the northern plain is formed of older alluvium. They lie above the flood plains of the rivers and present a terrace-like feature. The soil in this region contains kankar modules in them. This part is known as bhangar.
(i) Bhabar: The rivers after descending from the mountains deposit pebbles in a narrow belt lying parallel to the slopes of the Shiwaliks. This is known as Bhabar.(ii) Terai: To the south of Bhabar belt, the rivers and stream re-emerge and create a wet, swampy and marshy region known as the Terai. This was a thickly forested area but was later on cleared for cultivation.(iii) Bhangar: The largest part of the northern plain is formed of older alluvium. They lie above the flood plains of the rivers and present a terrace-like feature. The soil in this region contains kankar modules in them. This part is known as bhangar.(iv) Khadar: The newer younger deposits of the floodplains are called khadar. They are renewed almost every year and are therefore fertile. They are ideal for cultivation.
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