NCERT Solutions for Class 11 Geography Chapter 2: Structure and Physiography
Master India's physical structure from Gondwanaland to the Himalayan fold mountains. This chapter covers all 6 physiographic divisions with complete NCERT solutions, important MCQs, comparison tables (Bhangar vs Khadar, Western vs Eastern Ghats), and expert exam tips for CBSE 2026-27.
Chapter at a Glance
Chapter 2: Structure and Physiography – Quick Reference
| Chapter Name | Structure and Physiography |
| Subject | Geography (Book 2: India: Physical Environment) |
| Board / Class | CBSE Class 11 |
| Target Year | 2026-27 |
| Key Topics | Geological Divisions, Himalayas, Northern Plains, Peninsular Plateau, Indian Desert, Coastal Plains, Islands |
| Difficulty Level | Moderate to High |
| Exam Weightage | 5–7 Marks (incl. map work) |
Key Facts – Quick Numbers to Memorise
Learning Objectives
Understand the geological history and structure of the Indian subcontinent including Gondwanaland and plate tectonics.
Identify and describe the six major physiographic divisions of India and their key features.
Differentiate between key features like Western Ghats and Eastern Ghats, or Khadar and Bhangar.
Explain the formation and significance of the Himalayas and the Northern Plains for India.
Appreciate the diverse landscape of our country and its impact on climate, agriculture, and human life.
Key Concepts & Definitions
NCERT Exercise MCQs – Practice & Self-Test
Extra Practice MCQs
Full NCERT Solutions – All Exercise Questions
The three major parallel ranges of the Himalayas from north to south are:
- The Great / Inner Himalayas (Himadri): Northernmost, most continuous range. Average height: 6,000 m. Contains prominent peaks — Mount Everest, Kanchenjunga.
- The Lesser / Middle Himalayas (Himachal): Altitude: 3,700–4,500 m. Known for famous hill stations — Shimla, Mussoorie, Nainital, and valleys — Kashmir, Kangra, Kullu.
- The Outer Himalayas (Shiwaliks): Outermost range, altitude 900–1,100 m. Composed of unconsolidated river sediments. Duns (longitudinal valleys) lie between Himachal and Shiwaliks — e.g., Dehra Dun.
The Malwa Plateau lies between the Aravali ranges (northwest) and the Vindhyan ranges (south). It is part of the Peninsular Plateau and is drained by rivers like the Chambal, Betwa, and Ken, which flow towards the northeast.
The Lakshadweep Islands are the island group of India that have a coral origin. They are a group of small coral islands and atolls located in the Arabian Sea, off the coast of Kerala. Corals are skeletons of tiny marine animals called polyps.
| Basis | Bhangar | Khadar |
|---|---|---|
| Composition | Older alluvium | Newer, younger alluvium |
| Location | Above the floodplains; largest part of northern plain | Floodplains along river banks |
| Fertility | Less fertile; not renewed regularly | Highly fertile; renewed every year by floods |
| Texture | Coarse; contains 'kankar' (calcareous concretions) | Fine, silty, clayey; no kankar nodules |
| Suitability | Requires more irrigation and fertilisers | Ideal for rice, wheat, sugarcane, jute |
| Basis | Western Ghats (Sahyadris) | Eastern Ghats |
|---|---|---|
| Continuity | Continuous; crossed only through passes | Discontinuous and irregular; dissected by rivers |
| Altitude | Higher; avg 900–1,600 m | Lower; avg ~600 m |
| Highest Peak | Anai Mudi (2,695 m) in Kerala | Jindhagada Peak (1,690 m) in Andhra Pradesh |
| Rainfall | Cause orographic rainfall; block monsoon winds | Lower rainfall; parallel to monsoon winds |
| Rivers | Source of Godavari, Krishna, Kaveri | No major river originates; dissected by west-originating rivers |
The six major physiographic divisions of India are:
- The Himalayan Mountains
- The Northern Plains
- The Peninsular Plateau
- The Indian Desert
- The Coastal Plains
- The Islands
Contrast: Himalayan Region vs. Peninsular Plateau
| Feature | Himalayan Region | Peninsular Plateau |
|---|---|---|
| Formation & Age | Geologically young fold mountains; formed by tectonic collision | Part of ancient Gondwana landmass; stable block |
| Rock Type | Sedimentary and metamorphic rocks | Old crystalline, igneous, metamorphic rocks |
| Topography | Loftiest peaks, deep valleys, rugged relief | Broad shallow valleys, rounded hills, gentle relief |
| Mountain Type | Young fold mountains | Tableland with relict mountains (Aravallis) |
| Height | Avg 6,000 m — world's highest | 600–900 m average |
| Rivers | Perennial — fed by glaciers + rain | Seasonal — dependent on monsoon only |
| Stability | Unstable; earthquake-prone | One of the most stable land blocks in the world |
The Northern Plains are formed by the depositional work of three major river systems — the Indus, Ganga, and Brahmaputra along with their tributaries.
- Formation: Alluvial deposits from the Himalayas — extremely fertile soil.
- Extent: 7 lakh sq.km., about 2,400 km long and 240–320 km broad.
- Sub-divisions: Punjab Plains (west, Indus system), Ganga Plains (largest — Haryana, Delhi, UP, Bihar, WB), Brahmaputra Plains (east, Assam).
- Relief (North to South): Bhabar → Terai → Bhangar → Khadar.
- Significance: Agriculturally very productive due to fertile soil, adequate water, flat terrain. Densely populated — rightly called the 'food bowl of India'.
Extra Board Exam Questions (2026-27)
- Fertile Soil: Rich alluvial soil brought by rivers — ideal for agriculture.
- Abundant Water: Perennial rivers like Ganga, Yamuna, Brahmaputra ensure year-round water supply.
- Favourable Climate: Suitable for growing a variety of crops.
- Flat Terrain: Easy to build infrastructure — roads, railways, industries — promoting economic growth and settlement.
- The Indian (Thar) Desert lies to the west of the Aravalli Hills.
- Undulating sandy plain covered with sand dunes.
- Rainfall <150 mm/year; arid climate with sparse vegetation.
- Luni is the only large ephemeral river in this region.
- Barchans (crescent-shaped dunes) are prominent; longitudinal dunes near the Indo-Pakistan border.
Formation: The Himalayas were formed by the collision of the Indo-Australian Plate with the Eurasian Plate. India was part of Gondwana supercontinent. After splitting from Gondwana, the Indian Plate drifted northwards and collided with Eurasia. The sedimentary rocks of the Tethys Sea (located between the two landmasses) were uplifted, folded, and compressed to form the Himalayan ranges. This process is still ongoing — the Himalayas are still rising and are prone to earthquakes.
Significance for India:
- Climatic Barrier: Blocks cold, dry Central Asian winds; traps monsoon winds forcing rain over the subcontinent.
- Source of Perennial Rivers: Himalayan glaciers feed Ganga, Indus, Brahmaputra — ensuring year-round water.
- Fertile Plains: Alluvial deposits from rivers form the Northern Plains.
- Rich Biodiversity: Unique flora and fauna found in the Himalayas.
- Defence: Natural defence barrier historically protecting India.
- Orographic Rainfall: Occurs when moist air is forced to rise over a mountain barrier. As air rises, it cools, condenses, and causes precipitation on the windward side.
- Highest peak of Western Ghats: Anai Mudi (2,695 m) in Kerala.
- Why Eastern Ghats are discontinuous: They have been eroded and cut through by large east-flowing rivers — Godavari, Krishna, Kaveri — originating in the Western Ghats.
- Major river dissecting Eastern Ghats: The Godavari river.
Common Mistakes to Avoid
Exam Preparation Tips for 2026-27
Frequently Asked Questions (FAQs)
Master Structure & Physiography 🚀
Understanding India's physical structure — from Gondwanaland to the Himalayan fold mountains — gives you a foundation for all subsequent geography chapters. Revise regularly, practice map-based questions, and master comparison tables to ace your 2026-27 board exam!
⚡ Practice Chapter 2 MCQs Free