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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.
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 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]
The other two river systems are dependent on the monsoons and shrink into rivulets during the dry season. The Himalayan rivers that flow westward into Punjab are the Indus, Jhelum, Chenab, Ravi, Beas, and Sutlej. [64] The Ganges-Brahmaputra-Meghana system has the largest catchment area of about 1,600,000 km 2 (620,000 sq mi). [65]
The Himalayan rivers, mainly fed by glaciers and snow melt, arise from the Himalayas. The Deccan rivers system consists of rivers in Peninsular India, that drain into the Bay of Bengal and the Arabian Sea. There are numerous short coastal rivers, predominantly on the West coast. There are few inland rivers, which do not drain into sea. [2] [3]
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 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).
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 ...