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The Peninsular River System is an Indian River System. It is one of two types of Indian River System, along with the Himalayan River System. The Peninsular River System's major rivers are the following: [1] The rivers mainly drain in the rural area of India. The rivers have both religious and cultural significance to Indian people.
The Lesser Himalaya (LH) tectonic plate is mainly formed by Upper Proterozoic to lower Cambrian detrital sediments from the passive Indian margin intercalated with some granites and acid volcanics (1840 ±70 Ma [17]). These sediments are thrust over the Sub-himalayan range along the Main Boundary Thrust (MBT).
Antecedent drainage stream. An antecedent stream is a stream that maintains its original course and pattern despite the changes in underlying rock topography. A stream with a dendritic drainage pattern, for example, can be subject to slow tectonic uplift. However, as the uplift occurs, the stream erodes through the rising ridge to form a steep ...
The paleogeography of the India–Asia collision system is the reconstructed geological and geomorphological evolution within the collision zone of the Himalayan orogenic belt. The continental collision between the Indian Plate and Eurasian Plate is one of the world's most renowned and most studied convergent systems.
sedimentary. The Himalayas, or Himalaya (/ ˌhɪməˈleɪ.ə, hɪˈmɑːləjə / HIM-ə-LAY-ə, hih-MAH-lə-yə) [b] is a mountain range in Asia, separating the plains of the Indian subcontinent from the Tibetan Plateau. The range has some of the Earth 's highest peaks, including the highest, Mount Everest.
The Indo-Gangetic Plain, also known as the North Indian River Plain, is a 700-thousand km 2 (172-million-acre) fertile plain encompassing northern regions of the Indian subcontinent, including most of modern-day northern and eastern India, most of eastern-Pakistan, virtually all of Bangladesh and southern plains of Nepal. [1]
The river is prone to catastrophic flooding in the spring when the Himalayan snow melts. The average discharge of the Brahmaputra is about ~22,000 m 3 /s (780,000 cu ft/s), [2] [7] and floods reach about 103,000 m 3 /s (3,600,000 cu ft/s). [2] [10] It is a classic example of a braided river and is highly susceptible to channel migration and ...
The Hooghly River is formed by the confluence of the Bhagirathi River and Ajay River at Katwa, and Hooghly has a number of tributaries of its own. The largest is the Damodar River, which is 625 km (388 mi) long, with a drainage basin of 25,820 km 2 (9,970 sq mi). [26] The Hooghly River empties into the Bay of Bengal near Sagar Island. [27]