The Great Plain 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 approximately 2,400 km from east to west and 200 to 400 km from north to south. It covers an area of ​​approximately 580,000 km². Say no to plagiarism. Get Custom Essay on “Why Violent Video Games Should Not Be Banned”?Get Original EssayThe great plain of northern India was framed by the silt brought around the Indus-Ganga-Brahmaputra and its tributaries and it is known as the Indo-Ganga-Brahmaputra Plain. Geologists suggest that there was a shallow trough or geosyncline in the middle of the Himalayas and the Deccan level during the last geographical period of Himalayan development. After the uplift of the Himalayas, residues, flotsam and jetsam carried around the rivers began to collect there to shape the formidable alluvial plain of northern India. This vast plain is flat and dreary; it is described by some decent strains in the neighborhood. Thereafter, it could be classified into three divisions: The Punjab plain impoverished by the Indus. The plain is impoverished by the Indus and its tributaries, for example the Sutlej, the Beas and the Ravi. Only part of the Indus bowl is in India. The plain slopes delicately towards the southwest; thus the waterways follow the inclination of the land. The plain is largely made up of sediment. Dirt is permeable. The plain framed by the survey of new alluvium near the banks of the watercourses is called Bet. Extensive boulders, boulders, sand and soil cover the toe slope areas of the Punjab plain and are known as the 'Bhabar' plain or bhabar soil. This dirt cannot hold water. The new alluvium preserved near the banks of the watercourses of these streams shape a plain called Bet. The actual part of the Great Indian Plain is made up of Ganga bowl tiles. It extends from the eastern boundary of Punjab in the west to the fringe of Bangladesh in the east. It is a vast plain encompassing states such as Uttar Pradesh, Bihar and West Bengal. It is impoverished by waterways, for example Yamuna, Ganga, Ghaghara, Gandak, Kosi and Tista from the Himalayas in the north and Chambal, Betwa, Son and Damodar from the Himalayas in the south. The entire area is oriented to the south and southeast. It is a repetitive alluvial plain with few undulations. The lower compasses of the Ganges plain lie somewhat above ocean level; in any case, the upper part rises to 200 meters. The Ganges frames an extraordinary delta at its mouth. Its deltaic part presents the three particular highlights of the delta layout, for example, the mori-bund delta, the developed delta and the dynamic delta. The Ganges plain is the most populated part of India. The inhabitants of this plain are mainly occupied by the agri-food industry. Trade, industry and commerce are also prosperous. This plain can be separated into three areas: Keep in mind: this is just a sample. Get a personalized article from our expert writers now. Get Custom Essay Upper Ganga Plain: It extends from the Yamuna stream in the west to the city of Allahabad in the east. , Central Gangetic Plain: it extends from Allahabad (Uttar Pradesh) in the west to the Rajmahal slope in the east, Lower Gangetic Plain: it extends from the Rajmahal slope to the Bay of Bengal . The Brahmaputra Valley lies in the northeastern part of the nation and is cut between the Arunachal Himalayas in the north and the Meghalaya plateau in the south. The valley presents a flat plain. It is framed by wrecks and wrecks.