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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).
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]
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 Himalayan watershed is the source of majority of the major river systems in India including the three longest rivers–the Ganges, the Brahmaputra and the Indus. [3][4] These three river systems are fed by more than 5000 glaciers. [5] The Aravalli range in the north-west serves the origin of few of the rivers such as the Chambal, the Banas ...
Indus River. The Indus Gorge is formed as the Indus River bends around the Nanga Parbat massif, shown towering behind, defining the western anchor of the Himalayan mountain range. The Indus (/ ˈɪndəs / IN-dəs) is a transboundary river of Asia and a trans- Himalayan river of South and Central Asia. [7]
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]
Due to continental drift, the India Plate split from Madagascar and collided with the Eurasian Plate resulting in the formation of the Himalayas.. The earliest phase of tectonic evolution was marked by the cooling and solidification of the upper crust of the earth's surface in the Archaean Era (prior to 2.5 billion years) which is represented by the exposure of gneisses and granites especially ...