The Great Plains of Northern India lies south of the Himalayas. It is, in fact, limited by the Himalayas to the north and the Deccan level to the south. This plain extends for approximately 2,400 km from east to west and 200 to 400 km from north to south. It extends over an area of ​​approximately 580,000 square kilometres. Say no to plagiarism. Get a tailor-made essay on "Why Violent Video Games Shouldn't Be Banned"? Get an original essay The great plain of northern India was framed by silt brought around the Indo-Ganga-Brahmaputra and their tributaries and is famously known as the Indo-Ganga-Brahmaputra Plain. Geologists suggest that there was a shallow depression or geosyncline in the center of the Himalayas and at the Deccan level during the last geographical period of the development of the Himalayas. After the uplift of the Himalayas, debris, debris and waste carried by waterways began to gather there to shape the unique alluvial plain of northern India. This vast plain is flat and dreary; it is described by some decent neighborhood varieties. Subsequently, it could be classified into three divisions: The Indus-depleted Punjab plain. The Gangetic plain depleted by the Ganges. The Brahmaputra valley depleted by the Brahmaputra. The western part of the Northern Plain is known as Punjab Plain. The plain is depleted by the Indus and its tributaries, for example, Sutlej, Beas and Ravi. Only a piece of the Indus basin is found in India. The plain slopes gently towards the south-west; thus the waterways follow the inclination of the land. The plain is mostly made up of sediments. Dirt is permeable. The plain that is framed by the new alluvial prospect close to the banks of the stream is called Bet. Vast rocks, rocks, sand and earth cover the slope areas of the Punjab plain and are known as 'Bhabar' plain or bhabar soil. This dirt cannot hold water. The new alluvium maintained near the banks of the streams of these waterways forms a plain called Bet. The real part of the Great Indian Plain consists of the tiled basin of the Ganges. It extends from the eastern border of Punjab in the west to the border of Bangladesh in the east. It is a large plain spanning states, for example, Uttar Pradesh, Bihar and West Bengal. It is depleted from the streams, for example, Yamuna, Ganga, Ghaghara, Gandak, Kosi and Tista from the Himalayas in the north and Chambal, Betwa, Son and Damodar from the south. The whole area is inclined towards the south and south-east. It is a repetitive floodplain with few undulations. The lower circumference of the Gangetic plain is slightly above the ocean level; in any case the upper part rises up to 200 metres. The Ganges frames an extraordinary delta at its mouth. Its delta part shows the three highlights of the delta arrangement, i.e. the mori-bund delta, the developed delta and the dynamic delta. The Gangetic plain is the most crowded part of India. The inhabitants of this plain are essentially involved in agri-food. Trade, industry and commerce are also prosperous. This plain could be divided into three areas: Please note: this is just an example. Get a custom paper from our expert writers now. Get a Custom Essay Upper Gangetic Plain: Extends from Yamuna stream in the west to Allahabad city in the east, Central Gangetic Plain: Extends from Allahabad (Uttar Pradesh) in the west to Rajmahal slope in the east, Gangetic Plain Lower Ganga: Extends from the Rajmahal side to the Bay of Bengal. The Brahmaputra valley is located in the north-eastern part of the country and is bounded between the Arunachal Himalayas in the north and the Meghalaya plateau in the south. There.