Name the tributaries of Indus.

The tributaries of Indus are Chenab, Ravi, Beas, and Sutlej

Rivers and their Tributaries

Table of Contents

The Indian drainage system is an amalgamation of a large number of small and big rivers which stands out as the outcome of the evolutionary process of the three major physiographic units and the nature and characteristics of precipitation. India is the land of a large number of rivers—both major and minor. This article will specifically deal with the major rivers and their tributaries. The Indian river system is one of the most important scoring sections for UPSC CSE. In this article, we will discuss the major rivers and their tributaries, and compare between Himalayan and Peninsular rivers.

Rivers and their Tributaries

Rivers	Tributaries
Indus	Jhelum, Chenab, Ravi, Beas, and Sutlej
Ganga	Yamuna, Chambal, Son, Damodar, Mahakali, Ghagra, Ramganga, Kosi, Gandak.
Yamuna	Tons, Hindon, Chambal, Sindh, Betwa, Ken.
Chambal	Banas, Sind, Betwa, Ken.
Son	Johilla, Gopad, Rihand, Kanhar, North Koel.
Narmada	Amaravati, Bhukhi, Tawa, Banger
Brahmaputra	Subansiri, Kameng, Belsire, Dhansiri, Manas, Sankosh, Tista, Dibru, Dihing, Kalang, Burhi, Dikhu.
Mahanadi	Ib, Hasdo, Sheonath, Sondur, Pairi, Ong, Tel.
Godavari	Penganga, Wardha, Weinganga, Indravati, Sabari, Manjira.
Krishna	Koyna, Tungabhadra, Ghatprabha, Malprabha, Bhima, Musi, Munneru.
Kaveri	Harangi, Hemavati, Kabini, Bhavani, Arkavathy, Lakshmana Tirtha, Noyyal, and Arkavati.

Rivers of India

Comparison between the Himalayan and the Peninsular River

Sl. No.	Aspects	Himalayan River	Peninsular River
1.	Place of origin	Himalayan mountains covered with Glaciers	Peninsular plateau and central highland
2.	Nature of flow	Perennial; receive water from the glacier and rainfall	Seasonal; dependent on monsoon Rainfall
3.	Type of drainage	Antecedent and consequent leading to the dendritic pattern in plains	Superimposed, rejuvenated resulting in trellis, radial and rectangular patterns
4.	Nature of river	Long course, flowing through the rugged mountains experiencing headward erosion and river capturing; In plains meandering and shifting of Course	Smaller, fixed course with well-adjusted valleys
5.	Catchment area	Very large basins	Relatively smaller basin
6.	Age of the river	Young and youthful, active and deepening in the valleys	Old rivers with graded profiles, and have almost reached their base levels

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