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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 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 supposed paleochannel of the Hakra is actually a paleochannel of the Sutlej, flowing into the Nara river bed, [13] presently a delta channel c.q. paleochannel of the Indus River. [75] [76] [77] At least 10,000 years ago, well before the rise of the Harappan civilization, the sutlej diverted its course, leaving the Ghaggar-Hakra as a monsoon ...
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 ...
Map of India showing the major rivers. With a land area of 3,287,263 km 2 (1,269,219 sq mi) consisting of diverse ecosystems, India has many rivers systems and perennial streams. [ 1 ] The rivers of India can be classified into four groups – Himalayan, Deccan, Coastal, and Inland drainage.
It is still connected to this paleochannel of the Sutlej, and possibly the Yamuna, which ended in the Nara River, presently a delta channel of the Indus River joining the sea via Sir Creek. [3] [5] [6] The Sutlej changed its course about 8,000-10,000 years ago, leaving the Ghaggar-Hakra as a system of monsoon-fed rivers terminating in the Thar ...
For instance, a high average erosion rate of 1.8 mm/yr has been reported in the frontal Sutlej's Himalayan catchment, contributing to large sedimentation load. [14] Below the Indo-Gangetic Plain lies the generally undeformed Indian Craton strata. All of them are bounded by the Main Frontal thrust (MFT) at the northeast side. [3]
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.