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The 13307/13308 Ganga Sutlej Express runs from Dhanbad Junction via Netaji Subhas Chandra Bose Gomoh, Gaya Junction, Mughalsarai Junction, Varanasi Junction, Jaunpur Junction, Akbarpur Junction, Ayodhya Junction, Lucknow Charbagh, Laksar Junction,Ambala Cantonment Junction, Ludhiana Junction, Phillaur Junction, Nakodar Junction, Lohian Khas Junction to Firozpur Cantonment.
The Middle Ganga Plain stretches to the east of the Upper Ganga plain and forms part of eastern Uttar Pradesh and Bihar. It covers an area of 1.44 km 2 (0.56 sq mi), stretching 330 km (210 mi) in north–south direction and 600 km (370 mi) in the east–west direction. The elevation varies from 100 m (330 ft) in the western boundary to 30 m (98 ...
The Upper Ganges canal is the important and the original Ganges Canal, which starts at the Bhimgoda Barrage near Har ki Pauri at Haridwar, traverses Roorkee, Purquazi, Sardhana (Meerut district), Muradnagar, Dasna, Bulandshahr, Khurja, Harduaganj and continues to Nanau (near Akrabad) in Aligarh district, where it bifurcates into the Kanpur branch and Etawah branch.
The Sutlej River [a] is a major river in Asia, flowing through China, India and Pakistan, and is the longest of the five major rivers of the Punjab region. It is also known as Satadru ; [ 3 ] and is the easternmost tributary of the Indus River .
The Triveni Sangam, the intersection of the Yamuna River and the Ganges River. In Hindu tradition, Triveni Sangam is the confluence (Sanskrit: sangama) of three rivers that is a sacred place, with a bath here said to flush away all of one's sins and free one from the cycle of rebirth.
Śutudrī́ – Identified with Sutlej. Marúdvr̥dhā – Identified with Mahuvardhavan. [5] Haryana: Sarasvati [7] Āpayā́ and Āpayā́ – Streams/rivers of Sarasvati basin. [5] Drishadvati [5] [6] [8] Eastern Rivers: Áśmanvatī – Identified with Assan. Yamúnā – Identified with Yamuna. Aṃśumátī – Probably an epithet for ...
The river Sutlej separates Doaba from the Malwa region of India to its south and the river Beas separates Doaba from the Majha region, split between Pakistan and India, to its north. Scheduled castes form more than 40% of the population in Doaba. This area is also called the NRI Hub of Punjab as a consequence of the migration of a significant ...
The Singtali and Subathu Formation made up the older sub-group while the Dharamsala and Siwalik Formation made up the younger one. Separating the two is an Oligocene unconformity . [ 13 ] It has been suggested that there was a period of non-deposition during the Oligocene due to temporary uplifting of the Indian continent.