Drainage system in india pdf

You May Also Like. Himalayan River. Peninsular River. Place of origin. Himalayan mountains covered with glaciers. Peninsular plateau and central highland. Perennial; receive water from glacier and rainfall.

Seasonal; dependent on monsoon rainfall. Antecedent and consequent leading to a dendritic pattern in plains. Superimposed, rejuvenated resulting in trellis, radial, and rectangular patterns. Long course, flowing through the rugged mountains experiencing headward erosion and river capturing; In plains, meandering and shifting off course.

Smaller, a fixed course with well-adjusted valleys. Catchment area. Very large basin. Young and youthful, active and deepening in the valleys. Old rivers with graded profile, and have almost reached their base levels. Dams In India. Himachal Pradesh and Punjab Border. Uttar Pradesh and Madhya Pradesh Border. Place of Origin. Brahmagiri Hills, Coorg Karnataka. Udaipur, Aravalli Hills Rajasthan. The Ganga originates from the Gangotri glacier near Gaumukh 3, m in the Uttarkashi district of Uttarakhand.

However, the river, when it originates from the Gangotri glacier is known as the Bhagirathi. At Devprayag , the Bhagirathi merges with another river, i. The total length of the Ganga in India is 2, km, which is shared by Uttarakhand km ; Uttar Pradesh 1, km ; Bihar km ; and West Bengal km. The Son is a major right bank tributary of the Ganga; however, major left bank tributaries are the Ramganga , the Gomati , the Ghaghara , the Gandak , the Kosi , and the Mahananda. Originating from the Yamunotri glacier on the western slopes of Banderpunch range 6, km , the Yamuna is the longest tributary of the Ganga.

The Chambal is famous for its badland topography, known as the Chambal ravines as shown in the image given below. The Damodar drains the eastern margins of the Chottanagpur plateau, where it flows through a rift valley and finally joins the Hugli.

Originating from the Darjeeling hills, the Mahananda joins the Ganga as its last left bank tributary in West Bengal. Originating from the Amarkantak plateau, the Son is a large south bank tributary of the Ganga; it joins the Ganga at Arrah, Bihar. The Brahmaputra originates from the Chemayungdung glacier of the Kailash range near the Mansarovar Lake. The Tista joins the Brahmaputra on its right bank in Bangladesh and from here, the river is known as the Yamuna.

The Mahanadi originates from Sihawa in Raipur district of Chhattisgarh and runs through Madhya Pradesh and Odisha and finally discharges its water into the Bay of Bengal. Popularly known as the Dakshin Ganga , the Godavari is the largest peninsular river system. The Godavari originates from Nasik district of Maharashtra and discharges its water into the Bay of Bengal. Originating from Mahabaleshwar in Sahyadri, the Krishna is the second largest east flowing Peninsular River.

The Koyna , the Tungabhadra , and the Bhima are the major tributaries of the Krishna. The Kaveri originates from the Brahmagiri hills 1,m located in Kogadu district of Karnataka. Major tributaries of the Kaveri are the Kabini , the Bhavani, and the Amravati. Flowing through a rift valley located between the Satpura in the south and the Vindhya range in the north, the Narmada forms Dhuandhar waterfall and a picturesque gorge of marble rocks nearby Jabalpur.

Flowing in the westward direction, Narmada finally empties into the Arabian Sea in the Bharuch district of Gujarat. Originating from Multai in the Betul district of Madhya Pradesh, Tapi is the other important westward flowing river emptying into the Arabian Sea.

Primarily, Luni originates in the Pushkar valley of the Aravalli range, Rajasthan in two branches, i. From here, the river is known as Luni.