Chapter 1 — Geographical Diversity of India
Complete, detailed solutions to every In-text question (Let’s Explore / Let’s Remember / Don’t Miss Out) and every Exercise question, with original textbook figures and custom diagrams.
In-text Questions — Solutions
Questions from the “Let’s Explore”, “Let’s Remember” and “Don’t Miss Out” boxes inside the chapter (pages 2–19).
What we observe: India is a very large country whose land is not the same everywhere. Snowy mountains stand in the north, flat plains lie just below them, a sandy desert is in the west, a large triangular plateau covers the middle and south, long coastlines run along both sides, and small islands lie out in the sea.
Landforms we can identify- Mountains – the Himalayas in the north; the Aravallis in the west; the Western and Eastern Ghats along the coasts; the Garo–Khasi–Jaintia hills in the north-east.
- Plains – the flat, fertile Gangetic (Northern) Plains, and the narrow coastal plains.
- Plateau – the Peninsular (Deccan) Plateau in the middle and south.
- Desert – the Thar Desert in the west.
- Islands – Lakshadweep in the Arabian Sea; Andaman & Nicobar in the Bay of Bengal.
The colours are a height (altitude) code. The legend of a physical map tells us how high the land is:
| Colour | Meaning | Example |
|---|---|---|
| Dark brown / white | Very high land & snow-capped peaks | Greater Himalayas |
| Light brown / yellow | Hills, plateaus, dry desert land | Deccan Plateau, Thar |
| Green | Low, flat land (plains) | Gangetic Plains |
| Blue | Water — seas, oceans, big rivers | Arabian Sea, Bay of Bengal |
Remember the five regions
(1) The great mountain zone (2) The plains of the Ganga and the Indus (3) The desert region (4) The southern peninsula (5) The islands.
Yes. Reading the grid lines on the map, India lies roughly:
India’s approximate location
Latitude: about 8°N to 37°N • Longitude: about 68°E to 97°E
The Tropic of Cancer (23½°N) passes almost through the middle of the country. So India lies entirely in the Northern Hemisphere and in the Eastern Hemisphere.
- Himalayas — the long wall of mountains in the north (natural barrier).
- Thar Desert — yellow patch in the west.
- Arabian Sea — blue, to the west.
- Indian Ocean — blue, to the south.
- Bay of Bengal — blue, to the east.
Why this matters
Because the Tropic of Cancer cuts through India, the northern half is in the sub-tropical zone and the southern half in the tropical zone. This is one big reason India has such varied climate — snow in Ladakh and hot beaches in Kanyakumari at the same time!
The highest mountain in the world is Mount Everest, standing at about 8,849 metres above sea level. It lies in the Himadri (Greater Himalayas), on the border of Nepal and China (Tibet).
- In Nepali it is called Sagarmatha; in Tibetan, Chomolungma.
- India’s own highest peak is Kanchenjunga (about 8,586 m) in Sikkim — the third highest in the world.
- The Himalayas stretch across six countries: India, Nepal, Bhutan, China, Pakistan and Afghanistan.
Quick numerical: how tall is 8,849 m?
Using the political map together with the physical map, the Himalayan states/UTs of India (from west to east) are:
| Region | States / UTs |
|---|---|
| Western Himalayas | Ladakh (UT), Jammu & Kashmir (UT), Himachal Pradesh, Uttarakhand |
| Central / Eastern Himalayas | Sikkim, northern West Bengal (Darjeeling) |
| Eastern Himalayas & NE hills | Arunachal Pradesh, Assam (hills), Nagaland, Manipur, Mizoram, Meghalaya, Tripura |
| Range | Also called | Key facts |
|---|---|---|
| Himadri | Greater Himalayas | Highest & most rugged; Mount Everest, Kanchenjunga; snow all year; very few settlements |
| Himachal | Lower / Lesser Himalayas | Moderate climate, rich biodiversity; hill stations — Nainital, Mussoorie (Uttarakhand), Darjeeling (West Bengal), Shimla (Himachal Pradesh) |
| Shivalik | Outer Himalayas | Outermost & lowest; rolling hills, dense forests, rich wildlife; transition zone to the Gangetic Plains |
Because the Brahmaputra is fed mainly by melting snow and glaciers of the Himalayas — not only by rain.
- In winter, the water in the high Himalayas is locked up as snow and ice, so less water reaches the river.
- In summer, the temperature rises, and the snow and glaciers melt rapidly.
- All this melt-water flows down into the river, so its volume increases.
- Summer is also when the monsoon rains arrive in the Brahmaputra basin (Assam and the north-east get very heavy rainfall) — adding even more water.
That is why…
Rivers fed by Himalayan snow (Ganga, Indus, Brahmaputra) are perennial — they flow all year and actually swell in summer, while rivers fed only by rain (like many peninsular rivers) shrink in summer. This is also why the Himalayas are called the ‘Water Tower of Asia’.
Also note
Most Indian rivers are named after goddesses (Ganga, Yamuna, Kaveri). Brahmaputra is an exception — the name means ‘the son of Brahma’, a male name.
The bright lights show where large numbers of people live. The Gangetic Plains are among the most densely populated regions on Earth. Reasons:
- Flat land — easy to build houses, roads, railways, factories and cities.
- Very fertile soil — rivers bring minerals/alluvium, so farming is abundant and can support a huge population.
- Plenty of water — the Ganga, Indus, Brahmaputra and their tributaries never dry up.
- Easy transport & trade — an elaborate road and railway network, plus river transport used for millennia.
- Hence many big cities and industries (Delhi, Kanpur, Lucknow, Patna, Kolkata) → more electricity → more light at night.
Compare
The Himalayas, the Thar Desert and the thick forests of the plateau look dark in the same image — harsh conditions there mean fewer people, fewer towns, and fewer lights.
Shape: A sand dune is hill-like — it has a gentle slope on the side facing the wind, a sharp crest, and a steep slope on the sheltered side. Many dunes are crescent-shaped (called barchans). Dunes can rise as high as 150 metres.
Why sand takes a mountain-like shape- The wind picks up loose grains of sand and pushes them along the ground.
- When the wind meets an obstacle (a rock, a bush), it slows down and drops the sand there. Sand piles up.
- Grains are carried up the gentle windward slope to the crest, then slide down the far side, which becomes steep.
- Sand cannot pile steeper than about 34° (its “angle of rest”) — beyond that it collapses. So the wind keeps rebuilding the same shape again and again.
The big difference
A mountain’s shape is fixed (solid rock). A dune’s shape is fixed only in form, not in place — the grains keep moving, so the whole dune slowly travels across the desert. It is a “moving hill”.
Yes. Moving east from the golden-yellow Thar Desert, we meet a long, narrow, brownish ridge running south-west to north-east — these are the Aravalli Hills.
- Among the oldest mountains in the world — about 2.5 billion years old.
- Highest peak: Mount Abu (over 1700 m); most hills are only 300–900 m high (worn down by erosion over ages).
- They act as a natural barrier that stops the Thar Desert from spreading further east.
- Rich in marble, granite, zinc and copper. At the ancient Zawar mines, Indians were the first in the world to master zinc extraction, over eight centuries ago.
- Historic forts here: Chittorgarh, Kumbhalgarh, Ranthambore.
Interesting
A drive of only about 4½ hours takes you from Mount Abu (green hills) to Jodhpur (sandy desert) — a completely different geography!
Yes. The Aravalli range stretches across four states/UTs of north-western India:
| # | State / UT | What lies there |
|---|---|---|
| 1 | Gujarat | The southern end of the range begins here |
| 2 | Rajasthan | The main, longest part — Mount Abu, Chittorgarh, Kumbhalgarh, Ranthambore |
| 3 | Haryana | The low, broken northern hills |
| 4 | Delhi | The northern tip of the range ends here (the Delhi Ridge) |
So the range runs roughly south-west (Gujarat) → north-east (Delhi), cutting diagonally across north-western India.
Why is this so important?
Standing like a green wall, the Aravallis block the eastward march of the Thar Desert and influence the climate and rainfall of north-western India. If the Aravallis were destroyed, the desert would creep towards Delhi.
On the Peninsular Plateau, most big rivers flow from west to east, and only a few flow west.
| Direction | Rivers | Drain into |
|---|---|---|
| East-flowing (most) | Godavari, Krishna, Kaveri, Mahanadi | Bay of Bengal (they build large fertile deltas) |
| West-flowing (few) | Narmada, Tapti | Arabian Sea (they form estuaries, not deltas) |
- The Western Ghats are taller and stand close to the west coast like a wall.
- The Eastern Ghats are lower and broken.
- So the whole plateau tilts gently towards the east.
- Water always flows downhill → most rivers run east into the Bay of Bengal.
Northern rivers
In the north, the Ganga and Brahmaputra also flow eastwards into the Bay of Bengal, while the Indus flows west/south-west into the Arabian Sea.
When we place these states on the physical map, we notice something striking: almost all of them lie on or around the forested Peninsular (Deccan) Plateau and the eastern hilly belt.
| Where on the physical map | States | Some communities |
|---|---|---|
| Central plateau & forests | Madhya Pradesh, Chhattisgarh, Maharashtra, Telangana | Gond, Baiga, Bhil, Korku |
| Eastern plateau & hills | Jharkhand, Odisha, West Bengal | Santhal |
| Western plateau edge | Gujarat | Bhil |
| North-eastern hills & valley | Assam | Many north-eastern tribes |
- Tribal communities live mostly in hilly, forested plateau regions, not in the crowded plains.
- They have distinct languages, traditions and ways of life, closely connected to Nature.
- The forests give them food, medicine, wood and livelihood — so geography shapes culture.
- Ganga
- Brahmaputra
- Mahanadi
- Godavari
- Krishna
(The Kaveri also flows into the Bay of Bengal.)
(b) India’s coastal states & UTs| Coast | States / UTs (in order) |
|---|---|
| West Coast | Gujarat, Maharashtra, Goa, Karnataka, Kerala (+ Daman & Diu, Dadra & Nagar Haveli, Lakshadweep) |
| East Coast | Tamil Nadu, Andhra Pradesh, Odisha, West Bengal (+ Puducherry, Andaman & Nicobar) |
| Feature | West Coast | East Coast |
|---|---|---|
| Width | Narrow — Western Ghats come very close to the sea | Wide plains |
| Rivers | Short, swift; rise in the Western Ghats | Long, slow, big rivers from the plateau |
| River mouths | Mostly estuaries (Narmada, Tapti are the largest) | Large fertile deltas (Mahanadi, Godavari, Krishna, Kaveri) |
| Coastline | Coves, creeks, estuaries; alluvial deposits | Lagoons & lakes — Chilika Lake, Pulicat Lake |
| Stretches from | Gujarat → Kerala | Ganga delta → Kanyakumari |
These branches are called distributaries, and the triangular fan-shaped land they build is called a delta.
Note
India’s coastline is over 7500 km long — with golden beaches, black rocks, coral reefs and thick jungles.
Questions and Activities — Solutions
The end-of-chapter exercise, pages 24–25.
(This is an opinion question — here is a well-reasoned model answer.)
Feature 1 — The Himalayas- They act as a natural barrier in the north, protecting India from icy cold winds from Central Asia — this keeps our winters milder.
- They block the monsoon winds and force them to give rain to the plains.
- Their snow and glaciers feed the Ganga, Indus and Brahmaputra all year round — that is why they are called the ‘Water Tower of Asia’. Hundreds of millions of people get water for drinking, farming and industry.
- They are sacred to many cultures — temples and monasteries attract monks and pilgrims.
- Rivers deposit mineral-rich soil, making the land extremely fertile → abundant agriculture and food for the nation.
- The flat land allowed roads, railways and cities to develop; rivers have been used for travel and trade for millennia.
- A large proportion of India’s population lives here, and our civilisation grew along these rivers.
In one line
The Himalayas give us water and protection; the plains give us food and a home. Together they made Indian civilisation possible.
If the Himalayas did not exist, India would be a very different — and much harsher — land.
- The freezing winds from Central Asia would rush straight into the plains → winters would be bitterly cold, perhaps freezing.
- The monsoon clouds would not be stopped, so they would drift away → far less rainfall. Much of India could turn dry, arid, even desert-like.
- No snow, no glaciers → no melt-water. The Ganga, Indus and Brahmaputra would be small seasonal streams or would not exist.
- Without river silt, the fertile Gangetic Plains would never have formed.
- Less water and poor soil → little agriculture → far fewer people.
- Without a natural wall in the north, India would have been open to invasions from every direction, and would not have developed its own distinct culture in the way it did.
Short note (model)
“An India without the Himalayas would be a cold, dry, dusty land. There would be no perennial rivers, no green plains, no monsoon showers — and the rich civilisation that grew on the banks of the Ganga might never have been born.”
A continent contains almost every kind of landform, climate and culture. India, though only one country, contains all of these inside its own borders — that is why it is called a mini-continent.
| What a continent has | India’s own version |
|---|---|
| The highest mountains | The Himalayas, with peaks over 8000 m |
| Great fertile plains | The Gangetic Plains |
| Hot deserts | The Thar Desert |
| Cold deserts | Ladakh (winter below –30°C) |
| Ancient plateaus | The Deccan (Peninsular) Plateau, the Aravallis |
| Long coastlines | Over 7500 km, on three seas |
| Islands & coral reefs & a volcano | Lakshadweep, Andaman & Nicobar, Barren Island |
| Rain forests & heaviest rainfall | The Western Ghats, Meghalaya (Cherrapunji) |
| Many peoples, languages, religions | Hundreds of languages, tribes and traditions |
Also
India is the seventh-largest country in the world, and it even gives its name to the Indian Subcontinent — a whole region of Asia. A single country holding a continent’s worth of variety truly deserves the name “mini-continent”.
Let us follow the Ganga — from a glacier in the Himalayas to the sea.
| Stage of the journey | How people use the river |
|---|---|
| 1. Source — Gaumukh, the snout of the Gangotri Glacier (Uttarakhand). Here it is called the Bhagirathi. | Sacred site; pilgrimage and trekking destination. |
| 2. Mountain course — rushing down steep Himalayan valleys | Fast-flowing water turns turbines → hydroelectricity; river rafting and tourism. |
| 3. Entering the plains — at Haridwar | Drinking water; religious bathing and festivals; towns and temples grow on the banks. |
| 4. Across the Gangetic Plains | Irrigation through canals; the silt makes soil fertile → farming and multi-cropping; industries use the water; fishing. |
| 5. Lower course | Transport & trade — boats and ships have carried people and goods for millennia; ports and cities (e.g., Kolkata). |
| 6. Mouth — the Ganga–Brahmaputra delta, the Sundarbans | Fertile delta farming; fishing; mangrove forests protect the coast; home of the Royal Bengal Tiger; a UNESCO Heritage site. |
Summary of uses
Drinking • Irrigation • Farming (fertile silt) • Hydroelectricity • Industry • Transport & trade • Fishing • Tourism • Religious and cultural life.
Because it is both a peninsula and a plateau at the same time. The name simply joins the two facts.
Part 1 — It is a peninsulaA peninsula is a piece of land surrounded by water on three sides. Southern India is surrounded by water on three sides:
- West → the Arabian Sea
- East → the Bay of Bengal
- South → the Indian Ocean
A plateau is a landform that rises above the surrounding land and has a more or less flat top, often with steep sides. Southern India is a raised, triangular, flat-topped highland (the Deccan Plateau), bordered by two mountain ranges:
- Western Ghats — taller, run like a wall along the west coast, with beautiful monsoon waterfalls. (Northern part = Sahyadri Hills; a UNESCO World Heritage Site.)
- Eastern Ghats — lower and broken into smaller hills.
Conclusion
Peninsula (water on three sides) + Plateau (raised flat highland) = Peninsular Plateau. It is also one of the oldest land formations in the world, rich in minerals, forests and fertile land, which makes it vital for India’s economy.
- Great Himalayan National Park, Himachal Pradesh
- Jaisalmer Fort, Rajasthan (in the Thar Desert)
- The Western Ghats
- The Sundarbans (Ganga–Brahmaputra delta)
“The UNESCO site I found most interesting is the Sundarbans. It is the world’s largest mangrove forest, lying in the delta of the Ganga and the Brahmaputra. What fascinates me is that it is a unique combination of river, sea and land — the water is neither fully fresh nor fully salty, and the mangrove trees grow with their roots half in the water. About half of the delta lies in India and the rest in Bangladesh. It is the home of the magnificent Royal Bengal Tiger, which has learned to swim between the islands — something tigers elsewhere rarely do. The mangroves also act as a natural shield, protecting the coast from cyclones and storms. A forest that protects people and shelters tigers is truly worth preserving.”
Alternative (Great Himalayan National Park)
“It has a wide diversity of flora and fauna — including the rare snow leopard and the colourful Himalayan monal. What I like most is that its biodiversity is protected both by the government and by the village communities who live inside the park — people and nature working together.”
(Answer according to where you live. Here is a worked example, and a method you can use for any place.)
Method — 3 easy steps- Find your state on the political map.
- Look at the same spot on the physical map and note the colour (green = plain, brown/yellow = plateau or desert, dark brown/white = mountains, blue = water).
- Name the nearest big physical feature — a mountain range, river, plateau, desert or coast.
On the political map, Indore is in Madhya Pradesh, in central India. On the physical map, the same area is coloured light brown — meaning raised land. So Indore lies on the Malwa Plateau, the northern part of the great Peninsular (Deccan) Plateau. The Vindhya range lies to its south and the Narmada river (a west-flowing river) flows in the valley beyond it.
Describing its location: “Indore is located on the Peninsular Plateau of India, north of the Narmada valley and the Vindhyas.”
| If you live in… | Describe your location as… |
|---|---|
| Delhi, Lucknow, Patna, Kolkata | On the Gangetic (Northern) Plains |
| Jaipur, Jodhpur, Jaisalmer | In / at the edge of the Thar Desert, near the Aravallis |
| Shimla, Dehradun, Gangtok | In the Himalayas |
| Bhopal, Indore, Nagpur, Hyderabad | On the Peninsular / Deccan Plateau |
| Mumbai, Goa, Kochi | On the West Coast, near the Western Ghats |
| Chennai, Visakhapatnam, Puri | On the East Coast, near the Eastern Ghats |
The way people preserve food depends on the climate and geography of their region. Here is a ready project table you can build on.
| Region & conditions | Method | Examples |
|---|---|---|
| Thar Desert / Rajasthan — hot, dry, very little water | Sun-drying (the dry heat removes moisture so food doesn’t rot) | Dried ker-sangri, papad, mangodi, dried red chillies |
| Ladakh / Himalayas — freezing cold, long winter, nothing grows | Freeze-drying & air-drying in the cold dry air; storing for winter | Dried vegetables and greens, dried apricots, dried meat, hard cheese (chhurpi) |
| Coastal regions (Kerala, Goa, Bengal) — plenty of fish, plenty of salt | Salting & smoking | Salted/dried fish (sukka fish), salted prawns |
| Gangetic Plains — plenty of grain and vegetables, humid summers | Pickling in oil, salt & spices; making jams & murabbas in sugar | Mango & lemon pickle, amla murabba |
| All over India | Fermentation (good bacteria stop spoilage) | Curd, idli/dosa batter, gundruk (north-east) |
| Modern methods | Refrigeration, canning, vacuum packing | Frozen peas, canned juices |
- Food spoils because of bacteria, fungi and moisture.
- Drying removes the water they need. Salt and sugar pull water out of microbes. Oil keeps air out. Cold slows microbes down.
Project idea
Ask your grandparents what they dried or pickled at home. Note the season when it was made and the season it was eaten in. You will see how families store the surplus of one season to survive the shortage of another — exactly the hint in the textbook: drying vegetables when they are in season for use during the off-season.
India’s geography looks like it should divide people — but in fact it has bound them together.
1. A natural, well-defined homeThe Himalayas in the north, the Thar Desert and Arabian Sea in the west, the Indian Ocean in the south and the Bay of Bengal in the east form a clear natural boundary. Sri Aurobindo said that by its very geography India “appears to be quite distinct from other countries, and that itself gives it a certain national character.” People inside this frame have always felt they belong to one land.
2. Rivers connect region to regionRivers do not stop at borders. The Ganga and Brahmaputra have carried people, goods and ideas for millennia; the Godavari, Krishna and Kaveri water the south. Rivers became highways of trade and sacred places of pilgrimage for everyone.
Mountains, rivers and holy places are revered across regions — a pilgrim from Tamil Nadu travels to the Himalayas, and someone from Uttarakhand travels to Kanyakumari. Temples and monasteries in the Himalayas attract seekers “from around the world”.
4. Different regions need each otherDiversity creates exchange: the plains grow grain, the plateau supplies minerals and coal, the coasts give fish and ports for trade, the hills give timber, tea and fruit, the desert gives wool and crafts. No region can live alone — trade knits them together.
5. The monsoon — one rhythm for allThe same monsoon brings rain from Kerala to Kashmir. Sowing, harvests and festivals follow it, so people across India live by a shared seasonal calendar.
In short
The land gave India a common frame, common rivers, common seasons and a shared sacred geography. Our diversity is not a wall — it is the reason we depend on and enrich one another. As the astronaut Rakesh Sharma said of India from space: “Sāre jahān se achchha.”
