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Northern plains are generally described as flat land with no variations. It is not true. Justify
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Northern plains are generally described as flat land with no variation...
No, I do not agree that the Northern Indian Plains have no variation in relief features. The river flowing down from the Himalayas deposit sediments in a belt known as bhabar which runs parallel to the slopes of the Siwaliks. On the south of this belt exists the wet, swampy and marshy region known as the terai region. This region was densely covered with forests and was rich in flora and fauna. However, the forests were later brought down for the expansion of agriculture.

Most of the northern plains are formed of the older alluvium soil which is known as the bhangar plains. They lie above the flood plains of the river and present terrace-like features.
Therefore, we can say the Northern Indian Plains have variation in relief features.
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Northern plains are generally described as flat land with no variation...
Introduction:
The Northern plains are a vast region located in the northern part of the Indian subcontinent. While it is often believed that these plains are flat with no variations, this notion is not entirely accurate. In reality, the Northern plains exhibit a diverse landscape with a range of features and variations.

Diverse Topography:
Contrary to popular belief, the Northern plains are not uniformly flat. They encompass a wide range of topographical features, including valleys, hills, rivers, and floodplains. This diverse topography adds depth and variety to the region, making it far from monotonous.

Himalayan Foothills:
In the northernmost part of the Northern plains, the majestic Himalayan foothills form a prominent feature. These foothills are characterized by their undulating terrain and rising peaks, creating a beautiful and dramatic landscape. The foothills provide an important transition between the plains and the towering Himalayas.

Fluvial Systems:
One of the defining features of the Northern plains is its extensive fluvial system, comprising several major rivers such as the Ganges, Brahmaputra, and Yamuna. These rivers have carved their way through the plains over thousands of years, resulting in the formation of river valleys and floodplains. These valleys and floodplains exhibit significant variations in elevation, thus contradicting the notion of a flat landscape.

Alluvial Deposits:
The Northern plains are predominantly composed of fertile alluvial soil, which has been deposited by the rivers over time. These alluvial deposits are not evenly distributed, leading to variations in the landscape. Some areas may have thicker alluvial layers, resulting in slightly higher elevations, while others may have thinner layers, creating relatively lower-lying regions.

Terai Region:
The Terai region, located at the foothills of the Himalayas, is another significant feature of the Northern plains. It is characterized by its marshy and swampy terrain, which is interspersed with small hills and ridges. This region is far from being flat and adds further diversity to the overall topography of the Northern plains.

Conclusion:
In conclusion, the notion that the Northern plains are flat with no variations is not accurate. The region exhibits diverse topography, including the presence of Himalayan foothills, river valleys, floodplains, alluvial deposits, and the Terai region. These variations in the landscape make the Northern plains a visually appealing and geographically interesting area, contradicting the misconception of a monotonously flat land.
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Question No. 53 to 58 are based on the given text. Read the text carefully and answer the questions:The northern plain has been formed by the interplay of the three major river systems. This plain is formed of alluvial soil. The deposition of alluvium in a vast basin lying at the foothills of the Himalaya over millions of years formed this fertile plain. It spreads over an area of 7 lakh sq. km. The plain being about 2400 km long and 240 to 320 km broad, is a densely populated physiographic division. With a rich soil cover combined with an adequate water supply and favourable climate it is agriculturally a productive part of India The Northern Plain is broadly divided into three sections. The Western part of the Northern Plain is referred to as the Punjab Plains. Formed by the Indus and its tributaries, the larger part of this plain lies in Pakistan. The Indus and its tributaries - the Jhelum, the Chenab, the Ravi, the Beas and the Satluj originate in the Himalaya. This section of the plain is dominated by the doabs.The Ganga plain extends between Ghaggar and Teesta rivers. It is spread over the states of North India, Haryana, Delhi, U.P., Bihar, partly Jharkhand and West Bengal to its East, particularly in Assam lies the Brahmaputra plain. The northern plains are generally described as flat land with no variations in its relief. It is not true. These vast plains also have diverse relief features. According to the variations in relief features, the Northern plains can be divided into four regions. The rivers, after descending from the mountains deposit pebbles in a narrow belt of about 8 to 16 km in width lying parallel to the slopes of the Shiwaliks. It is known as bhabar. All the streams disappear in this bhabar belt. South of this belt, the streams and rivers re-emerge and create a wet, swampy and marshy region known as terai. This was a thickly forested region full of wildlife. The forests have been cleared to create agricultural land and to settle migrants from Pakistan after partition.Q. The northern plain has been formed by the interplay of the three major river systems. Name the rivers.

Question No. 53 to 58 are based on the given text. Read the text carefully and answer the questions:The northern plain has been formed by the interplay of the three major river systems. This plain is formed of alluvial soil. The deposition of alluvium in a vast basin lying at the foothills of the Himalaya over millions of years formed this fertile plain. It spreads over an area of 7 lakh sq. km. The plain being about 2400 km long and 240 to 320 km broad, is a densely populated physiographic division. With a rich soil cover combined with an adequate water supply and favourable climate it is agriculturally a productive part of India The Northern Plain is broadly divided into three sections. The Western part of the Northern Plain is referred to as the Punjab Plains. Formed by the Indus and its tributaries, the larger part of this plain lies in Pakistan. The Indus and its tributaries - the Jhelum, the Chenab, the Ravi, the Beas and the Satluj originate in the Himalaya. This section of the plain is dominated by the doabs.The Ganga plain extends between Ghaggar and Teesta rivers. It is spread over the states of North India, Haryana, Delhi, U.P., Bihar, partly Jharkhand and West Bengal to its East, particularly in Assam lies the Brahmaputra plain. The northern plains are generally described as flat land with no variations in its relief. It is not true. These vast plains also have diverse relief features. According to the variations in relief features, the Northern plains can be divided into four regions. The rivers, after descending from the mountains deposit pebbles in a narrow belt of about 8 to 16 km in width lying parallel to the slopes of the Shiwaliks. It is known as bhabar. All the streams disappear in this bhabar belt. South of this belt, the streams and rivers re-emerge and create a wet, swampy and marshy region known as terai. This was a thickly forested region full of wildlife. The forests have been cleared to create agricultural land and to settle migrants from Pakistan after partition.Q.The Northern plain is formed due to alluvial deposits brought by the Himalayan river(s) such as ________.

Question No. 53 to 58 are based on the given text. Read the text carefully and answer the questions:The northern plain has been formed by the interplay of the three major river systems. This plain is formed of alluvial soil. The deposition of alluvium in a vast basin lying at the foothills of the Himalaya over millions of years formed this fertile plain. It spreads over an area of 7 lakh sq. km. The plain being about 2400 km long and 240 to 320 km broad, is a densely populated physiographic division. With a rich soil cover combined with an adequate water supply and favourable climate it is agriculturally a productive part of India The Northern Plain is broadly divided into three sections. The Western part of the Northern Plain is referred to as the Punjab Plains. Formed by the Indus and its tributaries, the larger part of this plain lies in Pakistan. The Indus and its tributaries - the Jhelum, the Chenab, the Ravi, the Beas and the Satluj originate in the Himalaya. This section of the plain is dominated by the doabs.The Ganga plain extends between Ghaggar and Teesta rivers. It is spread over the states of North India, Haryana, Delhi, U.P., Bihar, partly Jharkhand and West Bengal to its East, particularly in Assam lies the Brahmaputra plain. The northern plains are generally described as flat land with no variations in its relief. It is not true. These vast plains also have diverse relief features. According to the variations in relief features, the Northern plains can be divided into four regions. The rivers, after descending from the mountains deposit pebbles in a narrow belt of about 8 to 16 km in width lying parallel to the slopes of the Shiwaliks. It is known as bhabar. All the streams disappear in this bhabar belt. South of this belt, the streams and rivers re-emerge and create a wet, swampy and marshy region known as terai. This was a thickly forested region full of wildlife. The forests have been cleared to create agricultural land and to settle migrants from Pakistan after partition.Q.Assertion (

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