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Physiography and Drainage Systems

Learn India's six physical divisions and its two great river families — one of the most repeated, high-scoring NDA Geography topics.

15 min read Class 11-12 level Exam-ready notes By The Cavalier
🎯 What you'll learn
  • Name and describe India's six major physiographic divisions and their key features
  • Distinguish the three parallel ranges and the regional names of the Himalayas
  • Compare Himalayan and Peninsular drainage systems with clear contrasts
  • Recall NDA facts on tributaries, passes, plateaus, coasts and islands

India is a land of stunning physical variety — snow-capped Himalayas, vast fertile plains, an ancient Peninsular plateau, long coastlines and scattered islands. Cutting across all of this flow the rivers, grouped into the young Himalayan and the old Peninsular systems. For the NDA written exam, this physiography-and-drainage combination is a reliable, almost-every-year source of marks. This Cavalier lesson makes it simple.

Why This Topic Matters for NDA

Indian physiography and drainage appear in the NDA General Ability Test almost every year. The questions are usually direct and factual: which river is a tributary of the Ganga, which pass connects to which region, where the Western and Eastern Ghats meet, or which division has the youngest mountains.

Because the answers are recall-based and rarely change, this is one of the most efficient areas to revise — no calculation, no diagrams to draw, just organised facts. If you can hold a clear mental map of India in your head, you can convert almost every such question into a sure mark.

Remember

Think of India in two layers: first the land (six physical divisions), then the water (two river families) flowing over it. Almost every NDA question fits into one of these two buckets.

The Six Physiographic Divisions

On the basis of relief and geological structure, India is divided into six major physiographic divisions. Knowing this list in order is the backbone of the whole topic.

  • The Northern and North-Eastern Mountains (the Himalayas)
  • The Northern Plain (Indo-Gangetic-Brahmaputra plain)
  • The Peninsular Plateau
  • The Indian Desert (the Thar)
  • The Coastal Plains (Western and Eastern)
  • The Islands (Andaman-Nicobar and Lakshadweep)

Each division has a distinct origin. The Himalayas and the Northern Plain are young features formed by the collision of the Indian and Eurasian plates and the deposition of river sediment. The Peninsular Plateau is one of the oldest and most stable landmasses on Earth, made of ancient hard rocks.

Key point

Memorise the six divisions in north-to-south order: Himalayas → Northern Plain → Peninsular Plateau → Thar Desert → Coastal Plains → Islands. This single list answers many "which division" questions instantly.

The Himalayas: Three Parallel Ranges

The Himalayas are the world's youngest fold mountains, formed where the Indian Plate collided with the Eurasian Plate. They stretch about 2,400 km in a great arc from the Indus gorge in the west to the Brahmaputra gorge in the east. Running lengthwise (longitudinally), they are made of three roughly parallel ranges.

The Great Himalayas (Himadri)

The northernmost and highest range, with an average height above 6,000 m. It holds the loftiest peaks including Mount Everest (Sagarmatha) and Kanchenjunga. Its core is composed of granite, and it is perennially snow-bound, feeding many glaciers.

The Middle Himalayas (Himachal or Lesser Himalaya)

Lying south of the Himadri, these ranges average 3,700–4,500 m. They contain famous hill stations and valleys — the Pir Panjal, Dhaula Dhar and Mahabharat ranges, and the well-known Kashmir, Kangra and Kullu valleys.

The Shiwaliks (Outer Himalayas)

The southernmost and lowest range (900–1,100 m), made of unconsolidated sediment brought down by rivers. The longitudinal valleys between the Shiwaliks and the Lesser Himalaya are called Duns — for example, Dehra Dun.

Exam tip

Order from north to south: Himadri (highest) → Himachal (middle) → Shiwalik (lowest). The flat-floored valleys in the Shiwalik zone are Duns — a frequent one-word answer.

Regional Divisions and Passes

From west to east, the Himalayas are also divided regionally by the rivers that cut across them: the Punjab Himalayas (Indus to Sutlej), Kumaon Himalayas (Sutlej to Kali), Nepal Himalayas (Kali to Tista) and Assam Himalayas (Tista to Dihang). Beyond the Dihang, the range bends sharply southward as the Purvanchal or Eastern Hills — the Patkai, Naga, Manipur and Mizo hills. Key passes include Zoji La (Kashmir to Ladakh), Nathu La and Jelep La (Sikkim to Tibet), Shipki La (Himachal) and Bomdi La (Arunachal Pradesh).

Remember

The Himalayas run roughly west to east, but the Purvanchal hills swing north to south along India's eastern border — a detail examiners like to test.

The Northern Plain

South of the Himalayas lies the Northern Plain, formed by the deposition of alluvium (fine river-borne sediment) by three river systems — the Indus, the Ganga and the Brahmaputra. It is one of the most fertile and densely populated regions on Earth.

Based on relief, the plain is divided into belts from north to south:

  • Bhabar — a narrow belt of pebbles along the Shiwalik foot where streams disappear underground.
  • Tarai — a wet, marshy zone south of the Bhabar where the streams re-emerge.
  • Bhangar — the older alluvium, slightly raised; it often contains lime nodules called kankar.
  • Khadar — the newer, fertile alluvium of the floodplains, renewed every flood.
Key point

Bhangar = old alluvium (higher, with kankar); Khadar = new alluvium (lower, more fertile). This pair is a classic NDA one-mark question.

The Peninsular Plateau

The Peninsular Plateau is a tableland of old crystalline, igneous and metamorphic rocks — part of the ancient landmass of Gondwana. It is the oldest and most stable physical unit of India. It has two broad parts.

The Central Highlands

North of the Narmada river, covering the Malwa plateau. They are bounded by the Aravallis on the north-west — one of the world's oldest fold mountain systems, now worn down to low hills.

The Deccan Plateau

A triangular landmass south of the Narmada. It is bordered by the Western Ghats (Sahyadris) on the west and the Eastern Ghats on the east. The north-western Deccan is covered by the famous black soil formed from lava — the Deccan Trap.

Exam tip

The Western Ghats are continuous and higher (crossed by passes like Thal Ghat, Bhor Ghat, Pal Ghat); the Eastern Ghats are broken and lower. The two ranges meet at the Nilgiri Hills in the south. Anai Mudi is the highest peak of Peninsular India.

Desert, Coastal Plains and Islands

The Indian Desert (Thar)

Lying to the west of the Aravallis, the Thar Desert is an undulating sandy plain with crescent-shaped dunes called barchans. Rainfall is below 150 mm a year. The Luni is the only large, mostly seasonal river of the region.

The Coastal Plains

The plateau is flanked by narrow coastal plains. The Western Coastal Plain is narrow and divided into the Konkan, Kannad and Malabar coasts. The broader Eastern Coastal Plain includes the Northern Circar and the Coromandel coast, and is rich in deltas built by the Mahanadi, Godavari, Krishna and Kaveri. Chilika Lake, India's largest coastal lagoon, lies on the eastern coast.

The Islands

India has two island groups. The Andaman and Nicobar Islands in the Bay of Bengal are larger and of volcanic and tectonic origin — Barren Island is India's only active volcano. The Lakshadweep Islands in the Arabian Sea are small coral islands.

Remember

Bay of Bengal islands = Andaman & Nicobar (volcanic/tectonic). Arabian Sea islands = Lakshadweep (coral). Don't swap them.

Drainage: The Two Great River Systems

Drainage means the river system of an area. Indian rivers fall into two broad families that differ in almost every way — this contrast is the single most tested idea in the drainage portion.

Himalayan Rivers

The Indus, Ganga and Brahmaputra and their tributaries. They are mostly perennial (flow all year) because they are fed by both monsoon rain and melting Himalayan snow. In their youthful stage they cut deep gorges, perform intense erosion, and in the plains form large meanders, ox-bow lakes and deltas.

Peninsular Rivers

The Mahanadi, Godavari, Krishna, Kaveri, Narmada and Tapi. They are largely seasonal, depending on monsoon rain alone, so they shrink in the dry season. They flow in shallow, fixed valleys with little erosive power, having reached a mature stage long ago.

Key point

Himalayan rivers = perennial, snow-fed, young, deep gorges and deltas. Peninsular rivers = seasonal, rain-fed, old, shallow fixed valleys. This contrast underlies most drainage MCQs.

Key Rivers and Their Tributaries

NDA loves questions on "which river is a tributary of which." Group them and they become easy.

The Ganga System

The Ganga rises from the Gangotri glacier (as the Bhagirathi). Its major left-bank tributaries are the Ghaghara, Gandak and Kosi (the Kosi is the "Sorrow of Bihar"); its main right-bank tributaries are the Yamuna, Son and the peninsular Chambal and Betwa (which join the Yamuna).

The Indus System

The Indus rises near Lake Mansarovar in Tibet. Its five Punjab tributaries are the Jhelum, Chenab, Ravi, Beas and Sutlej ("Punjab" means land of five waters).

West-Flowing Peninsular Rivers

The Narmada and Tapi are unusual: they flow west into the Arabian Sea through rift valleys and form estuaries, not deltas. Most other peninsular rivers flow east into the Bay of Bengal and build deltas.

Common mistake

Students assume all big rivers form deltas. The Narmada and Tapi form estuaries because they flow through narrow rift valleys with strong currents that flush sediment out to sea.

Worked Example: Reading a Drainage Question

NDA questions often describe a feature and ask you to name the river or division. Here is how to reason it out step by step.

Worked example

A river rises near Lake Mansarovar, is joined by five major tributaries, and flows into the Arabian Sea. Identify it and one of its tributaries.

Clue 1: source near Lake Mansarovar → either Indus or Brahmaputra Clue 2: "five major tributaries" → the land of five rivers (Punjab) Clue 3: flows into the Arabian Sea (west) → not the Brahmaputra (Bay of Bengal) Conclusion: the river is the INDUS A tributary: Sutlej (also Jhelum, Chenab, Ravi or Beas)

Notice the method: collect each clue, eliminate options, and the answer falls out. The same logic works for landform and division questions — match the description to the fact-pairs you memorised.

Common Mistakes to Avoid

A few confusions cost students easy marks every year. Fix them now.

  • Swapping Bhangar (old) and Khadar (new) alluvium — remember Khadar is fresher and more fertile.
  • Calling the Eastern Ghats continuous — only the Western Ghats are continuous and higher.
  • Thinking Lakshadweep is volcanic — it is coral; Andaman-Nicobar are volcanic/tectonic.
  • Assuming all peninsular rivers flow east — the Narmada and Tapi flow west.
  • Mixing up the Himalayan ranges — Himadri is highest, Shiwalik is lowest.
Common mistake

Many students confuse the Aravallis (one of the oldest fold mountains, in the north-west of the plateau) with young fold mountains. The Aravallis are ancient and heavily eroded — not young like the Himalayas.

Previous-Year Style Question

Try this in exam conditions, then check the reasoning below.

Previous-year style question

Q. Which one of the following correctly describes the Western and Eastern Ghats? (a) Both are continuous and of equal height (b) Western Ghats are continuous and higher; Eastern Ghats are broken and lower (c) Eastern Ghats are continuous and higher (d) Both are broken ranges

Answer: (b). The Western Ghats (Sahyadris) form a continuous, higher wall crossed only by a few passes, while the Eastern Ghats are discontinuous, eroded by rivers, and lower. The two ranges meet at the Nilgiri Hills in the south.

The trick is to recall the single contrast — continuous-and-high versus broken-and-low — and the answer is immediate.

Quick Recap and Revision

Run through this checklist the night before the exam — it covers the highest-yield facts of the whole topic.

60-second recap
  • Six divisions: Himalayas, Northern Plain, Peninsular Plateau, Thar Desert, Coastal Plains, Islands.
  • Three ranges: Himadri (highest) → Himachal (middle) → Shiwalik (lowest, with Duns).
  • Plain belts: Bhabar, Tarai, Bhangar (old), Khadar (new).
  • Ghats: Western continuous and higher; Eastern broken and lower; meet at the Nilgiris.
  • Islands: Andaman-Nicobar (volcanic, Barren active volcano); Lakshadweep (coral).
  • Rivers: Himalayan = perennial, snow-fed, deltas; Peninsular = seasonal, rain-fed; Narmada and Tapi flow west and form estuaries.
Exam tip

Sketch a rough outline map of India and label the six divisions and the main rivers. Drawing it twice fixes the layout far better than re-reading the text.

Frequently asked questions

How many physiographic divisions does India have?

India has six major physiographic divisions: the Northern and North-Eastern Mountains (Himalayas), the Northern Plain, the Peninsular Plateau, the Indian Desert (Thar), the Coastal Plains, and the Islands.

What is the difference between Himalayan and Peninsular rivers?

Himalayan rivers are perennial, fed by both rain and snowmelt, and form deep gorges and large deltas. Peninsular rivers are mostly seasonal, rain-fed, and flow in shallow, fixed valleys. The Narmada and Tapi are exceptions that flow west and form estuaries.

Why are the Western Ghats higher than the Eastern Ghats?

The Western Ghats form a continuous, higher edge of the Deccan Plateau, crossed by only a few passes, while the Eastern Ghats are lower and broken up by the many east-flowing rivers that cut through them. The two ranges meet at the Nilgiri Hills.

What is the difference between Bhangar and Khadar?

Bhangar is the older alluvium of the Northern Plain, lying slightly higher and often containing lime nodules called kankar. Khadar is the newer alluvium of the floodplains, renewed by floods each year and therefore more fertile.

Which are India's two island groups and how do they differ?

The Andaman and Nicobar Islands lie in the Bay of Bengal and are of volcanic and tectonic origin, with Barren Island being India's only active volcano. The Lakshadweep Islands lie in the Arabian Sea and are small coral islands.

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