NCERT Solutions for Class 11 Geography Chapter 3: Drainage System
Trace the journey of India's mighty rivers from glaciers to the sea. This chapter covers drainage patterns, the Himalayan vs Peninsular river systems, the complete Ganga river system, Panch Prayag, and the Panchnad — with all NCERT solutions updated for CBSE Board Exams 2026-27.
Chapter at a Glance
Chapter 3: Drainage System – Quick Reference
| Chapter Name | Drainage System |
| Subject | Geography (Book 2: India: Physical Environment) |
| Board / Class | CBSE Class 11 |
| Target Year | 2026-27 |
| Key Topics | Himalayan & Peninsular Rivers, River Basins, Drainage Patterns, Ganga System, Indus, Brahmaputra, Panchnad |
| Difficulty Level | Moderate |
| Exam Weightage | 5–7 Marks (incl. map work) |
Key Facts – Quick Numbers to Memorise
Learning Objectives
Understand the meaning of drainage, drainage basin, and watershed and how they differ.
Identify and describe different drainage patterns: dendritic, trellis, radial, and centripetal.
Differentiate between the Himalayan and Peninsular river systems in terms of origin, nature, and course.
Trace the complete course and major tributaries of the Ganga, Indus, and Brahmaputra rivers.
Describe the characteristics of major Peninsular rivers like Godavari, Krishna, Narmada, and Tapi.
Analyse the concept of river regimes and factors affecting them across different seasons.
Key Concepts & Definitions
2. Trellis — Rectangular; folded mountains with alternating hard/soft rock; Singhbhum
3. Radial — Spokes of wheel; dome/peak; Amarkantak (Narmada, Son)
4. Centripetal — Converge inward to lake/depression; Loktak Lake, Manipur
NCERT Exercise MCQs – Practice & Self-Test
Extra Practice MCQs
Full NCERT Solutions – All Exercise Questions
| Basis | River Basin | Watershed |
|---|---|---|
| Size | Large area drained by a major river and its tributaries | Smaller area drained by a smaller stream or river |
| Unit | Macro-level planning unit | Micro or meso-level planning unit |
| Example | The Ganga Basin, The Amazon Basin | Watershed of a small local stream or 'nala' |
| Relationship | Composed of many smaller watersheds | Part of a larger river basin |
| Basis | Dendritic Pattern | Trellis Pattern |
|---|---|---|
| Appearance | Resembles the branches of a tree | Rectangular pattern, like a garden trellis |
| Formation | Uniform, non-resistant rock terrain | Folded mountains with alternating hard and soft rocks |
| Tributaries | Join main river at acute angles | Parallel; join main river at right angles |
| Example | Ganga river system in northern plains | Rivers in Singhbhum region, Chotanagpur |
| Basis | Radial Pattern | Centripetal Pattern |
|---|---|---|
| Flow Direction | From central high point outward in all directions | From all directions inward to a central depression |
| Appearance | Like spokes of a wheel | Rivers converging to a single point |
| Topography | Dome-shaped hill or volcanic cone | Basin or depression with no outlet to the sea |
| Example | Rivers from Amarkantak Plateau (Narmada, Son) | Streams into Loktak Lake, Manipur |
- Water Scarcity Management: Transfers water from surplus basins (Ganga) to deficit basins (Peninsular India).
- Irrigation: Expands net irrigated area, boosts agricultural production and food security.
- Flood & Drought Control: Mitigates simultaneous floods in one region and drought in another.
- Navigation & Hydropower: Creates navigable waterway network and generates hydroelectric power.
- Origin: Peninsular Plateau and central highlands.
- Water Source: Seasonal / non-perennial — depend on monsoon rainfall only.
- Course: Shorter, shallower, with well-developed graded valleys compared to Himalayan rivers.
Useful Effects:
- Fertile Silt: Floods deposit fine, fertile khadar soil over plains — excellent for agriculture.
- Recharge Groundwater: Floodwaters seep into the ground, raising the water table.
- Clean Riverbeds: High-velocity floodwater flushes pollutants and sediments from the riverbed.
Harmful Effects:
- Loss of Life & Property: Houses, roads, bridges, crops destroyed — huge economic losses.
- Diseases: Stagnant water breeds mosquitoes and bacteria — cholera, malaria, dengue outbreaks.
- Disruption: Transport, communication, and power supply disrupted; communities isolated.
Flood Control Methods:
Structural: Dams & Reservoirs (store excess water); Embankments & Levees (contain rivers within banks); Channel Improvement (deepening/widening).
Non-Structural: Afforestation (reduces runoff); Floodplain Zoning (no construction in flood-prone areas); Flood Forecasting (timely warnings and evacuation).
| Feature | Himalayan Rivers | Peninsular Rivers |
|---|---|---|
| Origin | Himalayan mountains covered with glaciers | Peninsular Plateau and central highlands |
| Nature of Flow | Perennial — fed by glaciers + rainfall | Seasonal — dependent on monsoon only |
| Drainage Type | Antecedent and consequent; dendritic in plains | Superimposed and rejuvenated; trellis, radial, rectangular |
| Course Length | Long; rugged mountains, intense erosion | Shorter; well-defined graded profile; shallower valleys |
| Catchment Area | Very large basins | Relatively smaller basins |
| Age | Young, active; often shift course | Old rivers with a stable course |
| Deltas/Estuaries | Form large deltas (e.g., Sundarban Delta) | West-flowing → estuaries (Narmada, Tapi); East-flowing → deltas (Godavari, Krishna) |
| Examples | Ganga, Indus, Brahmaputra | Godavari, Krishna, Kaveri, Narmada, Tapi |
Extra Board Exam Questions (2026-27)
- Source: Originates as the Bhagirathi from Gangotri glacier. Joins Alaknanda at Devprayag → becomes the Ganga.
- Upper Course: Flows through narrow Himalayan valleys. Emerges onto the plains at Haridwar.
- Middle Course: Flows across the vast North Indian Plains.
- Right-bank tributaries: Yamuna (joins at Prayagraj/Allahabad), Son, Damodar.
- Left-bank tributaries: Ramganga, Ghaghara, Gandak, Kosi.
- Lower Course: In West Bengal, it bifurcates — Hooghly (distributary) flows south through Kolkata to Bay of Bengal. Main branch (Padma) flows into Bangladesh, joins Jamuna (Brahmaputra) and Meghna → forms the world's largest delta, the Sundarban Delta.
- Vishnuprayag — Alaknanda meets DhauliGanga
- Nandaprayag — Alaknanda meets Nandakini
- Karnaprayag — Alaknanda meets Pindar
- Rudraprayag — Alaknanda meets Mandakini
- Devprayag — Alaknanda meets Bhagirathi → becomes the Ganga
- Dendritic Pattern: Resembles tree branches. Develops where the river follows slope with uniform, non-resistant rock. Example: Rivers of the Northern Plains (Ganga system).
- Trellis Pattern: Develops in folded topography with alternating hard and soft rocks. Primary tributaries are parallel, shorter secondary tributaries join at right angles. Example: Rivers in Singhbhum region of Chotanagpur.
- Radial Pattern: Streams flow from a central peak outward like spokes of a wheel. Example: Narmada, Son, and Mahanadi originating from Amarkantak Plateau.
- Centripetal Pattern: Rivers flow from all directions into a central lake or depression. Example: Streams flowing into Loktak Lake in Manipur.
- Why Peninsular rivers are 'mature': They flow through stable, graded, broad valleys. They have completed most of their erosional work and have a fixed course.
- Water divide in Peninsular India: The Western Ghats.
- Why most Peninsular rivers flow west to east: The general slope of the Peninsular Plateau is from the west (higher elevation) to the east (lower elevation).
Common Mistakes to Avoid
Exam Preparation Tips for 2026-27
Frequently Asked Questions (FAQs)
Master the Drainage System 🌊
Mastering the Drainage System chapter is all about understanding the story of India's rivers. It's a fascinating and high-scoring topic with rich map work. Keep revising comparison tables and practicing river maps. For best results, solve Previous Year Questions (PYQs) to understand the exam pattern.
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