Drainage System, Class 11 Geography (India: Physical Environment)
Updated 15 October 2026 · Fact-checked
Drainage System is Chapter 3 of NCERT India: Physical Environment for Class 11. It covers drainage patterns, catchment areas, river basins and watersheds, the classification of Indian drainage, the evolution and river systems of the Himalayan and Peninsular drainage, and the usability of river water, including inter-linking and pollution, with a full map list.
What Drainage System is about
Drainage is the flow of water through well-defined channels; a network of channels is a drainage system. The drainage pattern of an area results from the geological time period, the nature and structure of rocks, topography, slope, the amount of water and the periodicity of flow.
Key terms: a river drains its catchment area; the area drained by a river and its tributaries is a drainage basin; the boundary between basins is the watershed. Large catchments are river basins, small ones watersheds. Basins and watersheds are units where what happens in one part affects the whole, so they make good planning regions.
Patterns: dendritic (tree branches; northern plain rivers), radial (from a hill in all directions; Amarkantak), trellis (parallel primary tributaries joined at right angles), centripetal (into a lake or depression).
Classification: by sea: Bay of Bengal (about 77 per cent) and Arabian Sea (about 23 per cent), divided by the Delhi ridge, Aravalis and Sahyadris; by size: major (> 20,000 sq km, 14 basins), medium (2,000-20,000 sq km, 44), minor (< 2,000 sq km); by origin and nature: Himalayan and Peninsular (the scheme NCERT follows).
Himalayan drainage: perennial (snow and rain), deep gorges and V-shaped valleys in the mountains, meanders, oxbow lakes, floodplains, braided channels and deltas in the plains; frequent course shifts (the Kosi, 'sorrow of Bihar'). It evolved from a mighty Shiwalik or Indo-Brahma river that was dismembered into the Indus, Ganga and Brahmaputra systems.
Peninsular drainage: older; broad, graded shallow valleys; fixed courses, no meanders, non-perennial; mostly west to east, except the Narmada and Tapi in rift valleys. Shaped by three geological events. Major systems: Mahanadi, Godavari, Krishna, Kaveri, Narmada, Tapi, and the Luni in Rajasthan.
Usability: water is uneven in time and space; floods in one place, drought in another; inter-basin linkage, problems in using river water and pollution.
Out of syllabus: smaller west- and east-flowing rivers, river regimes and Table 3.1.
Weightage: This chapter is part of Unit II, Physiography, of India: Physical Environment, which carries 13 of the 70 theory marks in the school annual exam together with Structure and Physiography. Map work carries a further 5 marks for each book.Source: CBSE Geography (029) syllabus 2026-27, Class XI course structure
Key concepts
- Drainage, catchment, basin and watershed; drainage patterns
- NCERT section Drainage System (introduction)
Drainage: flow of water through well-defined channels; the network is a drainage system. Ill-defined or choked channels cause flooding.
Pattern depends on: geological time period, nature and structure of rocks, topography, slope, amount of water and periodicity of flow.
Terms:
- Catchment area: the specific area from which a river collects water.
- Drainage basin: area drained by a river and its tributaries.
- Watershed: the boundary line separating one basin from another; also the term for small catchments of rivulets and rills, while large ones are river basins.
- Basins and watersheds show unity: change in one part affects the whole, so they are ideal micro, meso or macro planning regions.
Patterns:
Pattern Description Example Dendritic Like the branches of a tree Rivers of the northern plain Radial Rivers rise on a hill and flow in all directions Rivers from the Amarkantak range Trellis Primary tributaries parallel; secondary ones join them at right angles - Centripetal Rivers flow from all directions into a lake or depression - Worked example
Rivers such as the Narmada and the Son start from the same highland and flow away in different directions, while streams in a basin drain inward into a lake. Name the two drainage patterns and give the NCERT example of the first. (2 marks)
Try it first, then show the solutionSolution
- Rivers rising on a hill and flowing out in all directions form a radial pattern; the rivers from the Amarkantak range are the NCERT example.
- Rivers draining from all sides into a lake or depression form a centripetal pattern.
Answer: Radial (Amarkantak range) and centripetal.
- Classification of Indian drainage
- NCERT section Drainage Systems of India
1. By discharge (orientation to the sea):
Group Share of drainage area Rivers Bay of Bengal About 77% Ganga, Brahmaputra, Mahanadi, Krishna, etc. Arabian Sea About 23% Indus, Narmada, Tapi, Mahi, Periyar Separated by the Delhi ridge, the Aravalis and the Sahyadris.
2. By size of watershed:
Category Catchment Number/examples Major > 20,000 sq km 14 basins: Ganga, Brahmaputra, Krishna, Tapi, Narmada, Mahi, Pennar, Sabarmati, Barak, etc. Medium 2,000-20,000 sq km 44 basins: Kalindi, Periyar, Meghna, etc. Minor < 2,000 sq km Many rivers in low-rainfall areas 3. By mode of origin, nature and characteristics: Himalayan and Peninsular drainage. Its problem: the Chambal, Betwa, Son, etc. (Peninsular in origin and older) belong to the Ganga system; still it is the most accepted basis, and NCERT follows it.
General: Indian drainage results from the evolution of the three physiographic units and the nature of precipitation. Most large Peninsular rivers rise in the Western Ghats and flow into the Bay of Bengal; the Narmada and Tapi are exceptions flowing to the Arabian Sea.
Worked example
Why is the Himalayan-Peninsular classification 'imperfect' even though it is the most accepted? (2 marks)
Try it first, then show the solutionSolution
- It groups rivers by origin and nature, but the Chambal, Betwa and Son, which rise on the Peninsula and are older, join the Ganga, a Himalayan system.
- So some rivers counted in the Himalayan (Ganga) system are Peninsular in origin and age.
Answer: Older Peninsular rivers like the Chambal, Betwa and Son belong to the Himalayan Ganga system.
- Himalayan drainage and its evolution
- NCERT section The Himalayan Drainage; Evolution of the Himalayan Drainage
Character:
- Mainly the Ganga, Indus and Brahmaputra basins.
- Perennial: fed by melting snow and rain.
- In the mountains: giant gorges carved as the Himalayas rose, V-shaped valleys, rapids and waterfalls; course highly tortuous.
- In the plains: flat valleys, oxbow lakes, floodplains, braided channels, deltas; strong meandering and frequent shifts of course.
- Kosi, 'sorrow of Bihar': brings huge sediment from its upper reaches, deposits it in the plains, blocks its course and shifts channels.
Evolution (one view among differing opinions):
- A mighty river, the Shiwalik or Indo-Brahma, flowed along the whole Himalaya from Assam to Punjab and Sind, discharging into the Gulf of Sind near lower Punjab in the Miocene (about 5-24 million years ago). Evidence: the remarkable continuity of the Shiwalik, its lacustrine origin and alluvial deposits (sand, silt, clay, boulders, conglomerates).
- It was dismembered into: (i) the Indus and its five tributaries (west); (ii) the Ganga and its Himalayan tributaries (centre); (iii) the Brahmaputra stretch in Assam with its tributaries (east).
- Causes: the Pleistocene upheaval in the western Himalaya, including uplift of the Potwar Plateau (Delhi Ridge), which became the Indus-Ganga divide; and the down-thrusting of the Malda gap (between the Rajmahal hills and Meghalaya plateau) in the mid-Pleistocene, which diverted the Ganga and Brahmaputra to the Bay of Bengal.
Worked example
What evidence supports the existence of the Indo-Brahma river? (2 marks)
Try it first, then show the solutionSolution
- The remarkable continuity of the Shiwalik hills along the Himalaya.
- Their lacustrine origin and alluvial deposits of sand, silt, clay, boulders and conglomerates, as left by a great river.
Answer: Continuous Shiwaliks with lake and river deposits along the whole range.
- The Indus system
- NCERT section The River Systems of the Himalayan Drainage
Indus (Sindhu):
- One of the world's largest basins: 11,65,000 sq km (India 321,289 sq km); length 2,880 km (India 1,114 km). Westernmost Himalayan river of India.
- Source: a glacier near Bokhar Chu (31°15'N, 81°40'E), 4,164 m, Kailash range, Tibet; called Singi Khamban (Lion's mouth).
- Flows north-west between the Ladakh and Zaskar ranges, through Ladakh and Baltistan; forms a spectacular gorge near Gilgit; enters Pakistan near Chilas (Dardistan).
- Himalayan tributaries: Shyok, Gilgit, Zaskar, Hunza, Nubra, Shigar, Gasting, Dras. At Attock it receives the Kabul (right bank); other right-bank tributaries (from the Sulaiman ranges): Khurram, Tochi, Gomal, Viboa, Sangar.
- Receives the Panjnad (Satluj, Beas, Ravi, Chenab, Jhelum) above Mithankot; enters the Arabian Sea east of Karachi. In India it flows through Ladakh and Jammu and Kashmir.
Tributaries:
River Source and key points Jhelum Spring at Verinag at the foot of the Pir Panjal; through Srinagar and Wular lake; deep gorge into Pakistan; joins the Chenab near Jhang Chenab Largest tributary; Chandra + Bhaga meet at Tandi near Keylong (hence Chandrabhaga); 1,180 km before Pakistan Ravi West of the Rohtang pass, Kullu hills; Chamba valley; between Pir Panjal and Dhauladhar; joins the Chenab near Sarai Sidhu Beas Beas Kund near Rohtang (4,000 m); Kullu valley; gorges at Kati and Largi; meets the Satluj near Harike Satluj Raksas tal near Mansarovar (4,555 m), called Langchen Khambab; parallel to the Indus for 400 km; through Shipki La; gorge at Rupar; antecedent river; feeds the Bhakra Nangal canal system Worked example
Which river is not part of the Panjnad: Ravi, Chenab, Indus or Jhelum? Name the five Panjnad rivers. (2 marks)
Try it first, then show the solutionSolution
- The Panjnad is the name for the five rivers of Punjab that join the Indus.
- They are the Satluj, Beas, Ravi, Chenab and Jhelum; the Indus itself is not one of them.
Answer: The Indus; Panjnad = Satluj, Beas, Ravi, Chenab, Jhelum.
- The Ganga system
- NCERT section The River Systems of the Himalayan Drainage
Ganga:
- Most important river in basin size and culture. Rises in the Gangotri glacier near Gaumukh (3,900 m), Uttarkashi, as the Bhagirathi; cuts the Central and Lesser Himalayas in gorges.
- Devprayag: Bhagirathi meets Alaknanda → Ganga. The Alaknanda rises in the Satopanth glacier above Badrinath; it is formed by the Dhauli and Vishnu Ganga at Joshimath (Vishnu Prayag); the Pindar joins at Karna Prayag, the Mandakini (Kali Ganga) at Rudra Prayag.
- Enters the plains at Haridwar; flows south, south-east and east; splits into the Bhagirathi and Padma.
- Length 2,525 km: Uttarakhand 110 km, Uttar Pradesh 1,450 km, Bihar 445 km, West Bengal 520 km. Basin about 8.6 lakh sq km in India; the largest river system in India.
- Right-bank: Son (major). Left-bank: Ramganga, Gomati, Ghaghara, Gandak, Kosi, Mahananda. Enters the Bay of Bengal near Sagar Island.
- Namami Gange Programme (flagship, June 2014): abatement of pollution and rejuvenation of the Ganga.
Tributaries:
River Key points Yamuna Westernmost and longest tributary; Yamunotri glacier, Banderpunch range (6,316 m); joins at Prayag (Allahabad); right bank: Chambal, Sind, Betwa, Ken (from the Peninsula); left bank: Hindan, Rind, Sengar, Varuna; feeds Western and Eastern Yamuna and Agra canals Chambal Near Mhow, Malwa plateau; gorge above Kota (Gandhisagar dam); Bundi, Sawai Madhopur, Dholpur; famous badland ravines Gandak Kaligandak + Trishulganga; Nepal Himalaya between Dhaulagiri and Everest; enters Bihar in Champaran; joins at Sonpur near Patna Ghaghara Glaciers of Mapchachungo; Tila, Seti, Beri; gorge at Shishapani; Sarda joins it; meets the Ganga at Chhapra Kosi Antecedent; source north of Everest (Arun); Son Kosi (west) + Tamur Kosi (east) → Sapt Kosi Ramganga Garhwal hills near Gairsain; enters UP plains near Najibabad; joins near Kannauj Damodar Eastern margins of the Chotanagpur plateau; rift valley; joins the Hugli; tributary Barakar; once 'sorrow of Bengal', tamed by the Damodar Valley Corporation Sarda (Saryu) Milam glacier (Goriganga); Kali or Chauk on the Indo-Nepal border; joins the Ghaghara Mahananda Darjiling hills; last left-bank tributary, in West Bengal Son Large south-bank tributary from Amarkantak; waterfalls at the plateau edge; joins near Arrah, west of Patna Worked example
Using NCERT's figures, what share of the Ganga's 2,525 km length lies in Uttar Pradesh? (1 mark)
Try it first, then show the solutionSolution
- Uttar Pradesh share = 1,450 km.
- 1,450 ÷ 2,525 × 100 ≈ 57.4 per cent.
Answer: About 57 per cent.
- The Brahmaputra system
- NCERT section The River Systems of the Himalayan Drainage
- One of the world's largest rivers; source: Chemayungdung glacier, Kailash range, near Mansarovar.
- Flows east for about 1,200 km through dry, flat southern Tibet as the Tsangpo ('the purifier'); main right-bank tributary in Tibet: Rango Tsangpo.
- Carves a deep gorge near Namcha Barwa (7,755 m); emerges from the foothills as the Siang or Dihang; enters India west of Sadiya (Arunachal Pradesh).
- Flowing south-west it receives the Dibang (Sikang) and Lohit (left bank); thereafter called the Brahmaputra.
- In its 750 km through the Assam valley: left-bank tributaries Burhi Dihing, Dhansari (South); right-bank Subansiri, Kameng, Manas, Sankosh. The Subansiri (from Tibet) is antecedent.
- Enters Bangladesh near Dhubri and flows south; the Tista joins on the right, after which it is the Jamuna; it merges with the Padma and enters the Bay of Bengal.
- Known for floods, channel shifting and bank erosion, because its tributaries are large and carry heavy sediment due to heavy rain in the catchment.
Worked example
Why is the Brahmaputra known for floods and bank erosion? (2 marks)
Try it first, then show the solutionSolution
- Most of its tributaries are large and bring large quantities of sediment.
- This is because of heavy rainfall in its catchment, causing floods, channel shifting and bank erosion.
Answer: Large, sediment-laden tributaries fed by heavy rainfall.
- Peninsular drainage: features and evolution
- NCERT section The Peninsular Drainage System
Older than the Himalayan system: shown by broad, largely graded, shallow valleys and mature rivers.
Water divide: the Western Ghats, close to the west coast, separate the major rivers flowing to the Bay of Bengal from small rivulets to the Arabian Sea.
Direction: most major rivers flow west to east, except the Narmada and Tapi. The Chambal, Sind, Betwa, Ken and Son (from the north of the Peninsula) belong to the Ganga system. Other major systems: Mahanadi, Godavari, Krishna, Kaveri.
Characteristics: fixed course, absence of meanders, non-perennial flow; the Narmada and Tapi in rift valleys are exceptions.
Three geological events shaped it:
1. Subsidence of the western flank of the Peninsula below the sea in the early Tertiary, disturbing the symmetry of rivers on either side of the original watershed.
2. Upheaval of the Himalayas, when the northern flank subsided with trough faulting; the Narmada and Tapi flow in trough faults and fill the original cracks with detritus, so they lack alluvial and deltaic deposits.
3. Slight tilting of the Peninsular block from north-west to south-east, orienting the drainage towards the Bay of Bengal.Worked example
Why do the Narmada and Tapi not form deltas? (2 marks)
Try it first, then show the solutionSolution
- They flow in trough faults (rift valleys) formed when the northern flank of the Peninsula subsided during the Himalayan upheaval.
- They fill these original cracks with their detritus, so they lack alluvial and deltaic deposits (and end in estuaries, e.g. the Narmada's 27 km estuary).
Answer: They flow in rift valleys and deposit their load in the faults, forming estuaries, not deltas.
- Peninsular river systems
- NCERT section The Peninsular Drainage System
River Source Length / basin Key points Mahanadi Near Sihawa, Raipur district, Chhattisgarh 851 km; 1.42 lakh sq km Through Odisha to the Bay of Bengal; some navigation in the lower course; basin 53% MP and Chhattisgarh, 47% Odisha Godavari (Dakshin Ganga) Nasik district, Maharashtra 1,465 km; 3.13 lakh sq km Largest Peninsular system; basin 49% Maharashtra, 20% MP and Chhattisgarh, rest Andhra Pradesh; tributaries Penganga, Indravati, Pranhita, Manjra; floods below Polavaram (gorge); navigable only in the delta; splits after Rajamundri into a large delta Krishna Near Mahabaleshwar, Sahyadri 1,401 km Second largest east-flowing river; tributaries Koyna, Tungabhadra, Bhima; basin 27% Maharashtra, 44% Karnataka, 29% Andhra Pradesh and Telangana Kaveri Brahmagiri hills (1,341 m), Kodagu, Karnataka 800 km; 81,155 sq km Upper basin gets south-west monsoon (summer) rain, lower basin north-east monsoon (winter) rain, so it flows all year with less fluctuation; basin 3% Kerala, 41% Karnataka, 56% Tamil Nadu; tributaries Kabini, Bhavani, Amravati Narmada Western flank of Amarkantak (about 1,057 m) 1,312 km; about 98,796 sq km Rift valley between Satpura (south) and Vindhyan (north); gorge in marble rocks and Dhuandhar falls near Jabalpur; 27 km estuary south of Bharuch; Sardar Sarovar Project Tapi Multai, Betul district, MP 724 km; 65,145 sq km West-flowing; basin 79% Maharashtra, 15% MP, 6% Gujarat Luni Near Pushkar in two branches (Saraswati, Sabarmati) joining at Govindgarh - Largest river system of Rajasthan, west of the Aravali; west to Telwara, then south-west to the Rann of Kachchh; ephemeral Worked example
Why does the Kaveri carry water throughout the year with less fluctuation than other Peninsular rivers? (2 marks)
Try it first, then show the solutionSolution
- Its upper catchment receives rain from the south-west monsoon in summer.
- Its lower catchment receives rain from the north-east monsoon in winter, so it gets water in both seasons.
Answer: Rain in both monsoons feeds different parts of its basin.
- Extent of usability of river water
- NCERT section Extent of Usability of River Water
Uneven water: rivers carry huge volumes but unevenly in time and space. Perennial rivers flow all year; non-perennial ones have little water in the dry season. In the rainy season much water is wasted in floods and flows to the sea; when one part floods, another may suffer drought: a question of management as much as availability.
Inter-basin linkage: transferring surplus water to deficit basins. Examples NCERT lists for teachers to explain include the Indira Gandhi Canal Project, the Periyar Diversion Scheme, the Beas-Satluj Link Canal, the Kurnool-Cuddapah Canal and the Ganga-Kaveri Link Canal. Questions raised: is a canal enough, how to lift water from plains to plateau (uneven terrain), and is there regular surplus in northern rivers.
Problems in using river water (for ranking):
1. Not available in sufficient quantity
2. River water pollution
3. Silt load
4. Uneven seasonal flow
5. Inter-state river water disputes
6. Shrinking channels as settlements extend towards the thalwegPollution sources: city sewage, industrial effluents and wastes, cremation and bodies thrown in rivers, immersion of flowers and idols during festivals, large-scale bathing and washing. Remedies: schemes such as the Ganga Action Plan, the campaign to clean the Yamuna at Delhi, and Namami Gange (and the Narmada conservation mission Namami Devi Narmade).
Worked example
In the same monsoon, Assam faces floods while parts of Rajasthan and Tamil Nadu face drought. How could linking rivers help, and what difficulty does the terrain pose? (2 marks)
Try it first, then show the solutionSolution
- Linking would carry surplus water from flood-prone basins to water-deficit basins, easing both floods and droughts and giving more assured water for irrigation and drinking in dry areas.
- Terrain is a problem: water would have to be lifted from the plains over the higher Peninsular uplands, so a simple canal is not enough.
Answer: Transfers surplus to deficit areas (flood and drought relief, irrigation, drinking water); uneven terrain makes transfer difficult.
Drainage System in real life
Each concept, met in an everyday situation. Read the situation, answer the question in your own words, then compare with the model answer. The one-line hook is what to remember.
Watershed as a planning unit
Suppose villages in the upper part of a small watershed cut down their forests, and a few years later villages downstream complain of muddy water and more floods.
Explain using the idea that a watershed is a unit. (2 marks)
Try it first, then show the solutionSolution
- River basins and watersheds are marked by unity: what happens in one part directly affects the others.
- Upstream deforestation increases runoff and silt, so downstream villages get muddy water and floods; so the watershed must be planned as one unit.
Answer: Upstream actions affect downstream areas, so the whole watershed must be planned together.
Memory hook: One watershed, one fate.
Drainage and flooding
Imagine a heavy shower in your neighbourhood where the street drains are choked with plastic.
Link what happens to the chapter's definition of drainage. (2 marks)
Try it first, then show the solutionSolution
- Drainage is the flow of water through well-defined channels.
- When channels are ill-defined or choked, water cannot flow away and flooding results, as NCERT notes.
Answer: Choked channels mean no drainage, so the street floods.
Memory hook: Clear channels, dry streets.
Seasonal flow and storage
Suppose a town on a Peninsular river has plenty of water in August but taps run dry in April.
Explain why, and suggest one solution from the chapter's discussion on usability. (2 marks)
Try it first, then show the solutionSolution
- Most Peninsular rivers are non-perennial: they depend on monsoon rain and carry little water in the dry season.
- Storing monsoon surplus (or transferring surplus water from other basins through inter-basin links) can supply the dry months.
Answer: Non-perennial flow; store or transfer surplus monsoon water.
Memory hook: Save the monsoon for the summer.
Topics in this chapter
Drainage System: key facts
- Drainage by sea
- Bay of Bengal about 77% | Arabian Sea about 23%
- Divided by the Delhi ridge, Aravalis and Sahyadris.
- Basins by size
- Major > 20,000 sq km (14)
- medium 2,000-20,000 (44)
- minor < 2,000
- Watersheds small, basins large.
- Patterns
Dendritic tree radial from hill trellis right angles centripetal into a lake - Amarkantak = radial.
- Indo-Brahma
- Miocene (5-24 Ma) → dismembered into Indus, Ganga, Brahmaputra (Pleistocene uplift of Potwar plateau; Malda gap down-throw)
- Evidence: Shiwalik continuity and deposits.
- Indus figures
- Basin 11,65,000 sq km (India 321,289); length 2,880 km (India 1,114)
- Source near Bokhar Chu, 4,164 m.
- Ganga figures
- Gaumukh 3,900 m; Devprayag confluence.
- Brahmaputra figures
- Tsangpo about 1,200 km in Tibet; 750 km in the Assam valley; gorge near Namcha Barwa (7,755 m)
- Becomes Jamuna after the Tista joins.
- Peninsular lengths
- Godavari largest Peninsular system.
- Basin share
- e.g. Tapi in Maharashtra: 65,145 × 79% ≈ 51,465 sq km.
Drainage System: diagrams to practise
Practise each one on paper: draw it from the checklist, then tick off every label.
Drainage patterns
Differences between patterns; 3 marks.
Draw
- Four small boxes.
- Dendritic: a tree-like branching network.
- Trellis: parallel main streams with short tributaries joining at right angles.
- Radial: streams flowing outward from a central hill.
- Centripetal: streams flowing inward into a central lake.
Label
- Dendritic (northern plain)
- Trellis
- Radial (Amarkantak)
- Centripetal (lake/depression)
Watch out: Add arrows to show flow direction; radial and centripetal look the same without arrows.
Ganga headwaters and prayags
Confluences of the Ganga; 2-3 marks.
Draw
- Two streams (Bhagirathi from Gaumukh, Alaknanda from Satopanth) joining at Devprayag.
- On the Alaknanda, mark the joining points of Dhauli/Vishnu Ganga, Pindar and Mandakini.
Label
- Gaumukh (Bhagirathi)
- Satopanth glacier (Alaknanda)
- Vishnu Prayag (Dhauli + Vishnu Ganga)
- Karna Prayag (Pindar)
- Rudra Prayag (Mandakini)
- Devprayag (Ganga begins)
- Haridwar (enters plains)
Watch out: Order downstream: Vishnu, Karna, Rudra, Dev.
Drainage System: map work
The places on the official CBSE map list for this chapter. Find each one on an outline map of India and practise marking it.
| Map item | Where it is | How to mark it |
|---|---|---|
| Indus | Enters India's Ladakh from Tibet, flows north-west between the Ladakh and Zaskar ranges into Pakistan, to the Arabian Sea east of Karachi. | Draw from south-west Tibet through Ladakh towards the north-west border with an arrow. |
| Satluj | From Raksas tal (Tibet) through Shipki La, Himachal Pradesh and Punjab, joining the Beas at Harike and then the Indus system in Pakistan. | Draw across Himachal into Punjab, south-west to the border. |
| Ganga | From Gaumukh (Uttarakhand), Haridwar, across Uttar Pradesh, Bihar and West Bengal to the Bay of Bengal near Sagar Island. | Draw the main course south-east across the northern plain to the delta. |
| Yamuna | From Yamunotri, past Delhi and Agra, joining the Ganga at Prayag (Allahabad). | Draw parallel to and west of the Ganga, joining it at Prayag. |
| Chambal | From near Mhow (Malwa plateau, MP) north through Kota (Rajasthan) to join the Yamuna. | Draw north-east from western MP through south-east Rajasthan to the Yamuna. |
| Damodar | Eastern Chotanagpur plateau (Jharkhand) east into West Bengal, joining the Hugli. | Draw east-south-east from Jharkhand to the Hugli. |
| Brahmaputra | Enters India as the Siang/Dihang west of Sadiya (Arunachal Pradesh), flows south-west through the Assam valley, enters Bangladesh near Dhubri. | Draw through Arunachal and Assam with an arrow to Bangladesh. |
| Mahanadi | From Sihawa (Chhattisgarh) east through Odisha to the Bay of Bengal. | Draw from Chhattisgarh to the Odisha coast. |
| Godavari | From Nasik (Maharashtra) south-east across Telangana and Andhra Pradesh to a large delta after Rajamundri. | Draw across the Deccan to the Andhra coast. |
| Krishna | From Mahabaleshwar (Maharashtra) east through Karnataka and Telangana-Andhra Pradesh to the Bay of Bengal. | Draw south of the Godavari to the Andhra coast. |
| Kaveri | From Brahmagiri hills (Kodagu, Karnataka) south-east through Tamil Nadu to the Bay of Bengal. | Draw from south Karnataka through Tamil Nadu to the coast. |
| Narmada | From Amarkantak west through a rift valley between the Vindhyan and Satpura to the Arabian Sea south of Bharuch. | Draw west across MP into Gujarat; show an estuary. |
| Tapti (Tapi) | From Multai (Betul, MP) west, south of and parallel to the Narmada, through Maharashtra to the Arabian Sea near Surat in Gujarat. | Draw west, south of the Narmada. |
| Luni | From near Pushkar (Ajmer, Rajasthan) south-west to the Rann of Kachchh. | Draw south-west across western Rajasthan, dashed to show it is ephemeral. |
| Lakes: Wular, Sambhar, Chilika, Kolleru, Pulicat, Vembanad | Wular: Kashmir valley on the Jhelum; Sambhar: Rajasthan near Jaipur (salt lake); Chilika: Odisha coast; Kolleru: Andhra Pradesh between the Godavari and Krishna deltas; Pulicat: Andhra Pradesh-Tamil Nadu coast north of Chennai; Vembanad: Kerala coast. | Shade each lake and label it. |
| Straits, bays, gulfs: Palk Strait, Rann of Kachchh, Gulf of Kachchh, Gulf of Mannar, Gulf of Khambhat | Palk Strait: between Tamil Nadu and Sri Lanka; Gulf of Mannar: south of it; Rann of Kachchh: salt marsh in north Gujarat; Gulf of Kachchh: north of the Kathiawar peninsula; Gulf of Khambhat: south-east of Kathiawar. | Label each in the sea or marsh area. |
How the school exam asks Drainage System
The question patterns to expect, and the method that works for each.
| Question type | How it is asked | Method |
|---|---|---|
| MCQ | 'Sorrow of Bengal', largest basin in India, river not in the Panjnad, river in a rift valley, confluence of Alaknanda and Bhagirathi. | Learn nickname-river pairs and the prayag confluences. |
| Differences (3 marks) | River basin vs watershed; dendritic vs trellis; radial vs centripetal; delta vs estuary. | Two-column comparison with an example each. |
| Long answer (5 marks) | Himalayan versus Peninsular rivers; a journey from Haridwar to Siliguri naming rivers; evolution of either system; usability of river water. | Use the comparison table; for journeys list rivers in order (Ganga, Ramganga, Sarda, Ghaghara, Gandak, Kosi, Mahananda). |
| Map work | Rivers, lakes, straits, bays and gulfs on an outline map of India. | Draw rivers from source to mouth with arrows; mark lakes with blue shading. |
Tricks to remember Drainage System
Short memory aids. Say each one aloud once, then use it on a question the same day.
Panjnad
'Sweet Bananas Ripen Can Juicy': Satluj, Beas, Ravi, Chenab, Jhelum.
Use it when: Five rivers of Punjab.
Ganga left-bank tributaries
'Ram Goes Ghar Gandak Kosi Mahan': Ramganga, Gomati, Ghaghara, Gandak, Kosi, Mahananda.
Use it when: Left-bank tributaries in order.
Prayags downstream
'Very Kind Rivers Dance': Vishnu, Karna, Rudra, Dev Prayag.
Use it when: Alaknanda-Bhagirathi confluences.
Peninsular lengths
'God Kept Nature Mighty, Kind, Tidy': Godavari 1,465, Krishna 1,401, Narmada 1,312, Mahanadi 851, Kaveri 800, Tapi 724.
Use it when: Order of lengths.
Peninsular events
'Sink, Split, Slope': western subsidence, trough faulting, tilt to the south-east.
Use it when: Evolution of Peninsular drainage.
Drainage System: exam-level solved questions
Ordered from exam level to HOTS. Cover the solution, write your own, then compare step by step.
Example 1: A river that wanders · 1 mark · MCQExam level
A village in north Bihar finds that the river which flowed past it twenty years ago now flows several kilometres away, after its old channel silted up. The river is most likely the:
(a) Son
(b) Kosi
(c) Yamuna
(d) Chambal
Try it first, then show the solutionSolution
- Himalayan rivers show a strong meandering tendency on the plains and shift their courses frequently.
- The Kosi, the "sorrow of Bihar", brings huge amounts of sediment from its upper reaches; its course gets blocked and the river changes its course.
Answer: (b) Kosi.
Example 2: A-R on Peninsular rivers · 1 mark · Assertion-reasonHarder exam level
Assertion (A): Most Peninsular rivers flow towards the Bay of Bengal.
Reason (R): The Peninsular block was slightly tilted from north-west to south-east.
(a) Both true, R explains A (b) Both true, R does not explain A (c) A true, R false (d) A false, R true
Try it first, then show the solutionSolution
- A is true: most major Peninsular rivers except the Narmada and Tapi flow east.
- R is true and explains A: the tilt oriented the drainage towards the Bay of Bengal.
Answer: (a).
Example 3: Two kinds of river mouth · 3 marks · Short answerHarder exam level
A ship can sail straight from the Arabian Sea up the Narmada to Bharuch, but near the mouth of the Godavari it must pick its way among many distributaries and sandbanks. Explain the difference in the two river mouths. (3 marks)
Try it first, then show the solutionSolution
- The Godavari, like most east-flowing Peninsular rivers, deposits its load where it meets the sea on the broad east coast, splitting into distributaries and building a large delta.
- The Narmada flows west through a rift valley and enters the sea through a broad, open tidal mouth, a 27 km long estuary south of Bharuch, without building a delta.
- So delta = river-built deposit with distributaries; estuary = open tidal mouth with little deposition.
Answer: The Godavari ends in a delta of deposits and distributaries; the Narmada ends in an open estuary.
Example 4: Two rivers, two histories · 5 marks · Long answerHarder exam level
Compare the Ganga at Patna in May with the Krishna at Vijayawada in May, and use the comparison to set out the main differences between Himalayan and Peninsular rivers in source, flow, valleys, course and age. (5 marks)
Try it first, then show the solutionSolution
- Source and flow: the Ganga is fed by snow and glaciers as well as rain, so it is perennial and flows even in May; the Krishna depends on monsoon rain only, so its flow is low in May (non-perennial or seasonal).
- Valleys: Himalayan rivers cut giant gorges and V-shaped valleys in the mountains; Peninsular rivers flow in broad, shallow, largely graded valleys with low gradients.
- Course: on the plains Himalayan rivers meander strongly and shift their courses (as the Kosi does); Peninsular rivers have fixed courses with no meanders.
- Age: Himalayan rivers are young and still eroding vigorously; Peninsular rivers are much older and have reached maturity.
- Mouths: both groups build deltas on the east (the Ganga's Sunderbans, the Krishna's delta), but the Narmada and Tapi in rift valleys form estuaries.
Answer: Himalayan rivers: snow-fed, perennial, gorge-cutting, meandering and young; Peninsular rivers: rain-fed, seasonal, shallow-valleyed, fixed-course and old.
Example 5: Haridwar to Siliguri · 5 marks · Long answerHOTS / competency
Suppose you travel from Haridwar to Siliguri along the Himalayan foothills. Name, in order, the important rivers you would cross, and describe one. (5 marks)
Try it first, then show the solutionSolution
- Start: the Ganga at Haridwar, where it enters the plains.
- Moving east: the Ramganga (from Gairsain), then the Sarda (Kali) on the Indo-Nepal border.
- Then the Ghaghara (from Mapchachungo, gorge at Shishapani), the Gandak (Kaligandak and Trishulganga, entering Bihar at Champaran).
- Then the Kosi (antecedent, Sapt Kosi), and finally the Mahananda near Siliguri (from the Darjiling hills).
- Description, e.g. the Kosi: rises north of Everest (Arun), joined by Son Kosi and Tamur Kosi; brings huge sediment, blocks its course and shifts it: 'sorrow of Bihar'.
Answer: Ganga → Ramganga → Sarda → Ghaghara → Gandak → Kosi → Mahananda; e.g. the Kosi shifts its course because of heavy sediment.
Example 6: Basin shares · 3 marks · Short answerHarder exam level
The Tapi basin is 65,145 sq km, with 79% in Maharashtra, 15% in Madhya Pradesh and 6% in Gujarat. Calculate the area in each state and say which state should lead basin planning. (3 marks)
Try it first, then show the solutionSolution
- Maharashtra: 65,145 × 0.79 ≈ 51,465 sq km; MP: 65,145 × 0.15 ≈ 9,772 sq km.
- Gujarat: 65,145 × 0.06 ≈ 3,909 sq km (total checks to 65,145).
- Since basins act as units where changes in one part affect the whole, all three must plan together; Maharashtra, with most of the area, has the largest stake.
Answer: About 51,465, 9,772 and 3,909 sq km; joint basin planning, led by Maharashtra.
Example 7: Evolution of Himalayan rivers · 3 marks · Short answerExam level
Explain how the Indo-Brahma river was dismembered into three systems. (3 marks)
Try it first, then show the solutionSolution
- The Indo-Brahma flowed along the Himalaya from Assam to Punjab and Sind into the Gulf of Sind in the Miocene.
- The Pleistocene upheaval in the western Himalaya, with uplift of the Potwar plateau (Delhi Ridge), created the Indus-Ganga divide.
- The mid-Pleistocene down-thrusting of the Malda gap diverted the Ganga and Brahmaputra towards the Bay of Bengal, giving the Indus, Ganga and Brahmaputra systems.
Answer: Uplift of the Potwar plateau and down-throw of the Malda gap split it into the Indus, Ganga and Brahmaputra.
Case-study practice (Section E style)
Read the situation, then answer every part. In a school exam set on the board pattern this is a 4-mark question split into 1 + 1 + 2 marks.
The Kosi
Read the passage. A river rising north of Mount Everest is joined in Nepal by two streams from the west and east and enters north Bihar. Each monsoon it carries enormous loads of sediment, which settle on the plains. Villagers report that the river 'moves' its channel by many kilometres over the years, flooding new areas.
(i) · 1 mark
Name the river and its popular title.
Answer
Answer: The Kosi, the 'sorrow of Bihar'.
(ii) · 1 mark
Name the two streams that join it in Nepal and the combined name.
Answer
Answer: Son Kosi (west) and Tamur Kosi (east); after uniting with the Arun it forms the Sapt Kosi.
(iii) · 2 marks
Explain why the river changes its course.
Answer
Answer: It brings huge quantities of sediment from its upper reaches and deposits them in the plains; the channel gets blocked and the river shifts to a new course, a common tendency of Himalayan rivers in the plains.
Two rivers of the Deccan
River A rises near Nasik, is 1,465 km long, floods below Polavaram and forms a large delta after Rajamundri. River B rises in the Brahmagiri hills, is 800 km long, and keeps flowing through the year with less fluctuation than other Peninsular rivers.
(i) · 1 mark
Identify rivers A and B.
Answer
Answer: A: Godavari; B: Kaveri.
(ii) · 1 mark
Why is A called the Dakshin Ganga?
Answer
Answer: It is the largest Peninsular river system (1,465 km, 3.13 lakh sq km basin).
(iii) · 2 marks
Why does B flow more steadily, and what are two of its tributaries?
Answer
Answer: Its upper basin receives south-west monsoon rain in summer and its lower basin north-east monsoon rain in winter. Tributaries: Kabini, Bhavani, Amravati (any two).
Where the marks are
How a typical answer is split into step marks. Show every step: a right final answer alone rarely earns full marks.
On a map, the streams of the northern plain branch like a tree, while in a folded upland the main streams run side by side and their tributaries meet them at right angles. Name and explain both patterns. (3 marks) (3 marks)
| Step | Marks |
|---|---|
| Dendritic: resembles the branches of a tree. | 1 |
| Example: rivers of the northern plain. | 1 |
| Trellis: primary tributaries flow parallel; secondary tributaries join them at right angles. | 1 |
Describe the Brahmaputra river system. (5 marks) (5 marks)
| Step | Marks |
|---|---|
| Source: Chemayungdung glacier near Mansarovar; flows east 1,200 km in Tibet as the Tsangpo; Rango Tsangpo tributary. | 1 |
| Gorge near Namcha Barwa; emerges as Siang/Dihang; enters India west of Sadiya. | 1 |
| Joined by Dibang and Lohit; 750 km through Assam; left: Burhi Dihing, Dhansari; right: Subansiri, Kameng, Manas, Sankosh. | 1 |
| Enters Bangladesh near Dhubri; Tista joins, called Jamuna; merges with the Padma. | 1 |
| Floods, channel shifting, bank erosion due to large sediment-laden tributaries and heavy rain. | 1 |
Where students lose marks in Drainage System
The slips examiners see most often, and what to write instead.
Mistake: Mixing up Kosi and Damodar nicknames
Both were 'sorrows'.
Wrong working
The Kosi is the sorrow of Bengal.
Right working
Kosi: sorrow of Bihar. Damodar: once sorrow of Bengal, tamed by the DVC.
Do this: Kosi-Bihar (both have an 'i'); Damodar-Bengal (D then B, as in DVC's home state).
Usually costs: 1 mark per MCQ.
Mistake: Wrong prayag order
Four similar names.
Wrong working
Bhagirathi and Alaknanda meet at Rudra Prayag.
Right working
They meet at Devprayag; Rudra Prayag is where the Mandakini joins the Alaknanda.
Do this: 'Very Kind Rivers Dance': Vishnu, Karna, Rudra, Dev downstream.
Usually costs: 1 mark.
Mistake: Saying the Narmada forms a delta
Assuming all big rivers form deltas.
Wrong working
The Narmada forms a large delta in Gujarat.
Right working
The Narmada flows in a rift valley and forms a 27 km estuary south of Bharuch.
Do this: Rift rivers end in estuaries.
Usually costs: 1-2 marks.
Mistake: Calling the Yamuna a left-bank tributary from the Peninsula
Confusing the Yamuna with its own tributaries.
Wrong working
The Yamuna rises in the Peninsular plateau.
Right working
The Yamuna rises in the Yamunotri glacier; its right-bank tributaries Chambal, Sind, Betwa, Ken come from the Peninsula.
Do this: Yamuna from ice; its right bank from rock.
Usually costs: 1 mark.
Mistake: Drawing the Tapi north of the Narmada
Map positions mixed.
Wrong working
Tapi drawn between the Vindhyan and Satpura.
Right working
The Narmada flows between the Vindhyan and Satpura; the Tapi is south of the Satpura, parallel to the Narmada.
Do this: N before T, north to south.
Usually costs: 1 map mark.
NCERT exercise guide: Drainage System
What each exercise in the NCERT chapter tests, how to approach it, and a question of the same kind solved step by step. Questions here are written in our own words.
Q1 Multiple choice (i-v)
What it tests: Sorrow of Bengal, largest basin, not in Panjnad, river in a rift valley, Alaknanda-Bhagirathi confluence.
How to approach it: Learn nicknames, Panjnad, rift rivers and prayags.
Like Q1(iv)
Which river flows in a rift valley? (a) Son (b) Tapi (c) Yamuna (d) Luni
Show the solutionSolution
- The Narmada and Tapi flow through rift valleys (trough faults).
- Of the options, the Tapi.
Answer: (b) Tapi.
Q2 Differences; Q3 (about 30 words); Q4 (not more than 125 words)
What it tests: Basin vs watershed, patterns, delta vs estuary; inter-linking, Peninsular characteristics; Himalayan vs Peninsular rivers, Haridwar-Siliguri journey.
How to approach it: Differences: two columns with examples. Long: comparison table or ordered list of rivers with one description.
Like Q2(iii)
Distinguish radial and centripetal drainage in two lines.
Show the solutionSolution
- Radial: outward from a hill (Amarkantak).
- Centripetal: inward into a lake or depression.
Answer: Radial drainage flows outward in all directions from a high point such as Amarkantak; centripetal drainage flows inward from all directions into a lake or depression.
Practice questions on Drainage System
Write each answer on paper first. Open the hint only if you are stuck, and the answer only when you have finished.
Q1 · 1 mark · MCQExam level
Which river system is the largest in India, draining about 8.6 lakh sq km within the country?
(a) Indus
(b) Brahmaputra
(c) Ganga
(d) GodavariHint
Perennial Himalayan and non-perennial Peninsular tributaries both join it.
Answer
(c) Ganga.
Q2 · 1 mark · MCQExam level
The Alaknanda and the Bhagirathi meet at:
(a) Vishnu Prayag
(b) Rudra Prayag
(c) Karna Prayag
(d) DevprayagHint
After this the river is called the Ganga.
Answer
(d) Devprayag.
Q3 · 1 mark · Assertion-reasonHarder exam level
Assertion (A): The Satluj is an antecedent river.
Reason (R): It passes through the Shipki La on the Himalayan ranges and comes out of a gorge at Rupar.
Choose (a)-(d).Hint
Both statements are in NCERT; does R define 'antecedent'?
Answer
(b). Both are true, but R describes its route; it does not by itself explain what makes a river antecedent (existing before the uplift and keeping its course).
Q4 · 2 marks · Short answerExam level
A district plans its water use separately for each small stream catchment, while the state plans for the whole Krishna catchment. Which unit is the river basin and which the watershed, and how do they differ? (2 marks)
Hint
Size of catchment.
Answer
The state's unit (the whole Krishna catchment) is the river basin, the large catchment of a major river; the district's small stream catchments are watersheds, the catchments of rivulets and rills. Basins are large; watersheds are small units used for local planning.
Q5 · 3 marks · Short answerExam level
A dam engineer says Peninsular rivers are easier to plan for than Himalayan ones because they "stay put". Using three characteristics of Peninsular rivers, explain what she means and give one drawback. (3 marks)
Hint
Fixed course, no meanders, seasonal flow.
Answer
Peninsular rivers have fixed courses, no meanders and broad, graded, shallow valleys, so their channels do not shift like the Kosi. The drawback is that they are non-perennial, fed only by rain, so their flow drops sharply in the dry season (the Kaveri is steadier). The Narmada and Tapi, in rift valleys, are exceptions in forming estuaries.
Q6 · 3 marks · Short answerHOTS / competency
Suppose a state plans to link a north Indian river to a Deccan river by a canal. Using the chapter, list three practical problems it must solve. (3 marks)
Hint
Terrain, surplus, disputes.
Answer
Uneven terrain: water must be lifted from the plains to the plateau. Surplus: it must check that northern rivers have regular surplus water (flow is seasonal). Disputes and silt: inter-state water disputes and heavy silt loads must be managed.
Q7 · 2 marks · Short answerHarder exam level
Why are the Himalayan rivers perennial while most Peninsular rivers are not? (2 marks)
Hint
Sources of water.
Answer
Himalayan rivers are fed by both melting snow and rainfall, so they flow all year; Peninsular rivers depend on rain alone, so they carry little water in the dry season.
Q8 · 5 marks · Long answerHarder exam level
Describe the three geological events that shaped Peninsular drainage. (5 marks)
Hint
Subsidence, trough faulting, tilting.
Answer
(i) Subsidence of the western flank below the sea in the early Tertiary, disturbing the symmetry of rivers on either side of the original watershed. (ii) Himalayan upheaval with subsidence of the northern flank and trough faulting; the Narmada and Tapi flow in these troughs and lack deltaic deposits. (iii) Slight tilting of the block from north-west to south-east, orienting the drainage towards the Bay of Bengal. Result: east-flowing rivers with deltas and two west-flowing rift-valley rivers with estuaries.
Q9 · 2 marks · Short answerHOTS / competency
Rank and justify two problems in using river water that you think most serious in a big city on a river. (2 marks)
Hint
Pollution, shrinking channels.
Answer
Pollution (sewage, industrial effluents, washing and immersion make water unusable) and shrinking channels as settlements extend towards the thalweg (raising flood risk). Both arise from urban pressure.
Test your recall
Answer in your head or on paper first, then open the card. Pulling an answer out of memory makes it stick far better than re-reading.
1.What is a watershed?Show answer
The boundary line separating one drainage basin from another (also the small catchment of rivulets).
2.What share of India's drainage area drains into the Bay of Bengal?Show answer
About 77 per cent.
3.In which period did the Indo-Brahma river flow?Show answer
The Miocene, some 5-24 million years ago.
4.Where does the Jhelum rise?Show answer
A spring at Verinag at the foot of the Pir Panjal.
5.Which is the largest tributary of the Indus?Show answer
The Chenab.
6.What is the Tsangpo?Show answer
The name of the Brahmaputra in Tibet, meaning 'the purifier'.
7.Why is the Godavari called Dakshin Ganga?Show answer
It is the largest Peninsular river system.
8.Name the largest river system of Rajasthan.Show answer
The Luni.
Best order to study it
- Learn drainage terms and the four patterns with diagrams.
- Learn the three bases of classification with the 77/23 and major/medium/minor figures.
- Learn Himalayan drainage features and evolution; then the Indus, Ganga and Brahmaputra systems.
- Learn Peninsular features, the three events and the river table.
- Learn usability of river water, then practise the full map list.
Quick revision checklist
The night before the exam: can you do each of these without looking?
- Drainage: flow through defined channels; pattern depends on rocks, slope, time, water.
- Patterns: dendritic (plains), radial (Amarkantak), trellis, centripetal.
- Basin, catchment, watershed; basins are planning units.
- Bay of Bengal 77%, Arabian Sea 23%; major 14, medium 44 basins.
- Himalayan: perennial, gorges, meanders, course shifts (Kosi); Indo-Brahma dismembered by Potwar uplift and Malda gap.
- Indus: 2,880 km; Panjnad above Mithankot; Chenab largest tributary; Satluj antecedent (Bhakra Nangal).
- Ganga: Gaumukh, Devprayag, Haridwar; 2,525 km; Yamuna longest tributary; Son right bank; Damodar sorrow of Bengal.
- Brahmaputra: Tsangpo, Namcha Barwa gorge, Siang, Sadiya, Dhubri, Jamuna; floods and bank erosion.
- Peninsular: older, fixed course, no meanders, non-perennial; three events; Narmada and Tapi in rift valleys.
- Godavari largest (1,465 km); Krishna 1,401; Kaveri steady (two monsoons); Narmada estuary 27 km; Luni ephemeral.
- Usability: uneven flow, floods and droughts, inter-basin links, pollution.
Drainage System: frequently asked questions
How many marks does Drainage System carry?
It is part of Unit II, Physiography, of India: Physical Environment, which carries 13 of the 70 theory marks in the 2026-27 syllabus together with Structure and Physiography. Its rivers, lakes, straits, bays and gulfs are on the map list.
Are river regimes and the smaller west- and east-flowing rivers in the syllabus?
No. Smaller rivers flowing west and east, river regimes and Table 3.1 were dropped in NCERT's rationalisation.
What is an antecedent river?
A river that existed before an uplift and kept its course by cutting down as the land rose. NCERT names the Satluj, Kosi and Subansiri as antecedent rivers.
Which lakes must I mark?
Wular, Sambhar, Chilika, Kolleru, Pulicat and Vembanad (identification on the map).
Based on: CBSE Geography (029) syllabus 2026-27 (Classes XI-XII); NCERT India: Physical Environment, Class XI, Chapter 3 (Reprint 2026-27)