Chapter 1: Geographical Diversity of India Class 8th Social Science (Exploring Society:India and Beyond-I) NCERT Solution

Class 7 Social Science — Chapter 1: Geographical Diversity of India | Solutions
Exploring Society: India and Beyond · Grade 7 · Part 1

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.

12 In-text Questions9 Exercise QuestionsDiagrams & FiguresStep-wise Explanations

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).

Q1
Let’s Explore · Page 2
Look at the map of India at the end of your book. What are you able to observe? Which landforms can you identify on the map? What do the different colours on the map mean?

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.
What the colours mean

The colours are a height (altitude) code. The legend of a physical map tells us how high the land is:

ColourMeaningExample
Dark brown / whiteVery high land & snow-capped peaksGreater Himalayas
Light brown / yellowHills, plateaus, dry desert landDeccan Plateau, Thar
GreenLow, flat land (plains)Gangetic Plains
BlueWater — seas, oceans, big riversArabian Sea, Bay of Bengal
@edugrown The 5 Physical Regions of India 1. Himalayas 2. Northern (Gangetic) Plains 3. Thar Desert 4. Peninsular Plateau (Deccan Plateau) Western Ghats Eastern Ghats 5. Lakshadweep 5. Andaman & Nicobar Arabian Sea Bay of Bengal Indian Ocean
A quick visual tour of the five regions (photos from your textbook)
Himalayan range from space
1. The great mountain zone — the Himalayas (Fig. 1.2)
Multi-cropping in Uttar Pradesh
2. The plains of the Ganga and the Indus (Fig. 1.13)
Sand dunes of the Thar Desert
3. The desert region — the Thar (Fig. 1.21)
Dense forests of Chhattisgarh
4. The southern peninsula — the plateau (Fig. 1.27)
Coral reef in the Lakshadweep Islands
5. The islands — Lakshadweep (Fig. 1.36)
Coral reef in the Andaman Islands
5. The islands — Andaman (Fig. 1.37)

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.

Q2
Let’s Explore · Page 3
Do you recall your lesson on latitudes and longitudes? Can you read, approximately, the latitude and longitude where India lies? Identify the above features on India’s physical map.

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.

@edugrown Location of India (Latitude & Longitude) Tropic of Cancer (23.5°N) 37°N 8°N 68°E 97°E INDIA 8°N – 37°N, 68°E – 97°E
Features to identify on the physical map
  • 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!

Q3
Let’s Remember · Page 4
Many Himalayan peaks are over 8000 metres high and are called the ‘Eight Thousanders’. Can you name the highest mountain in the world?

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.
Satellite images of the Himalayan range
Fig. 1.2 — Satellite images of the Himalayan range; its length is about 2500 km.

Quick numerical: how tall is 8,849 m?

Step 1: Convert to kilometres: $$8849\ \text{m} = \frac{8849}{1000} = 8.849\ \text{km}$$
Step 2: Compare with a 3 m tall room: $$\frac{8849}{3} \approx 2950 \text{ rooms stacked up!}$$
Q4
Let’s Explore · Page 6
Can you locate the names of the states in the different parts of the Himalayas? Take the help of both the physical and political maps.

Using the political map together with the physical map, the Himalayan states/UTs of India (from west to east) are:

RegionStates / UTs
Western HimalayasLadakh (UT), Jammu & Kashmir (UT), Himachal Pradesh, Uttarakhand
Central / Eastern HimalayasSikkim, northern West Bengal (Darjeeling)
Eastern Himalayas & NE hillsArunachal Pradesh, Assam (hills), Nagaland, Manipur, Mizoram, Meghalaya, Tripura
The three parallel ranges
@edugrown Three Ranges of the Himalayas (Cross-section) Gangetic (Northern) Plains Himadri (Greater) Everest • Kanchenjunga — snow all year Himachal (Lesser) Shimla • Nainital • Darjeeling • Mussoorie Shivalik (Outer) Rolling hills, dense forests NORTH SOUTH
RangeAlso calledKey facts
HimadriGreater HimalayasHighest & most rugged; Mount Everest, Kanchenjunga; snow all year; very few settlements
HimachalLower / Lesser HimalayasModerate climate, rich biodiversity; hill stations — Nainital, Mussoorie (Uttarakhand), Darjeeling (West Bengal), Shimla (Himachal Pradesh)
ShivalikOuter HimalayasOutermost & lowest; rolling hills, dense forests, rich wildlife; transition zone to the Gangetic Plains
Great Himalayan National Park collage
Fig. 1.7 — Life in the Himalayan ranges: 1. Great Himalayan National Park 2. Himalayan monal 3. A monastery in Ladakh 4. The Beas river 5. Snow leopard 6. A local market 7. Rhododendron.
Kath-kuni house, Himachal Pradesh
Fig. 1.6 — Kath-kuni house, Himachal Pradesh. Stone + wood keeps the house warm and resists mild earthquakes.
Q5
Don’t Miss Out · Page 11
The Brahmaputra gets bigger during summer instead of drying up! Can you guess why?

Because the Brahmaputra is fed mainly by melting snow and glaciers of the Himalayas — not only by rain.

Gaumukh, the edge of the Gangotri Glacier
Fig. 1.3 — Gaumukh, the edge of the Gangotri Glacier. When such snow and ice melt in summer, the rivers swell.
Step-by-step reason
  1. In winter, the water in the high Himalayas is locked up as snow and ice, so less water reaches the river.
  2. In summer, the temperature rises, and the snow and glaciers melt rapidly.
  3. All this melt-water flows down into the river, so its volume increases.
  4. 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.

Q6
Let’s Explore · Page 11
Notice the concentration of lighting in the plains (in the night-time satellite image). What could be the reason for this concentration?
Satellite image of the Gangetic plains at night
Fig. 1.16 — Night satellite image of the Gangetic plains: a blaze of lights.

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.

Aerial view of Delhi with the river Yamuna
Fig. 1.12 — Aerial view of Delhi with the Yamuna: huge cities grow on the flat plains.
Modern agricultural practices in the plains
Fig. 1.11 — Modern agriculture feeds this huge population.
Modes of transport in the Gangetic plains
Fig. 1.15 — Rail and river transport in the Gangetic plains.
Q7
Let’s Explore · Page 12
What is the shape of a sand dune? While mountains are made of rock and their shape is fixed, why do you think sand dunes also have a similar shape, even though they are made of sand?
A traveller among the sand dunes of the Thar Desert
Fig. 1.21 — Sand dunes of the Thar Desert: hill-like, with one gentle side and one steep side.

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.

@edugrown Shape of a Sand Dune (Crescent / Barchan) WIND Gentle windward slope (sand is pushed up here) Crest Steep slip face (sand slides down ≈ 34°) Wind builds the same shape again and again → dunes look like hills, but they slowly MOVE.
Why sand takes a mountain-like shape
  1. The wind picks up loose grains of sand and pushes them along the ground.
  2. When the wind meets an obstacle (a rock, a bush), it slows down and drops the sand there. Sand piles up.
  3. Grains are carried up the gentle windward slope to the crest, then slide down the far side, which becomes steep.
  4. 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.
Camel vendor at the Pushkar Mela
Fig. 1.23 — Camel vendor at the Pushkar Mela, at the edge of the Thar.
Jaisalmer, the Golden City
Fig. 1.22 — Jaisalmer, the ‘Golden City’, rises in the middle of these dunes.

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”.

Q8
Let’s Explore · Page 14
Let’s go back to the map. Trace your path slowly from the Thar Desert towards the east. Do you see the Aravalli Hills?

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.

A part of the Aravallis, and the Aravallis seen from space
Fig. 1.25 — (Left) A part of the Aravallis; just beyond this range the Thar Desert begins. (Right) The Aravallis from space.
Key facts about the Aravallis
  • 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.
Kumbhalgarh Fort surrounded by the Aravallis
Fig. 1.26 — Kumbhalgarh Fort in the Aravallis; the hills made an excellent defence.

Interesting

A drive of only about 4½ hours takes you from Mount Abu (green hills) to Jodhpur (sandy desert) — a completely different geography!

Q9
Let’s Explore · Page 15
Look at the political map and identify the states that the Aravalli range spans. Did you see Delhi, Rajasthan, Haryana and Gujarat?

Yes. The Aravalli range stretches across four states/UTs of north-western India:

#State / UTWhat lies there
1GujaratThe southern end of the range begins here
2RajasthanThe main, longest part — Mount Abu, Chittorgarh, Kumbhalgarh, Ranthambore
3HaryanaThe low, broken northern hills
4DelhiThe 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.

Q10
Let’s Explore · Page 16
Look at the physical map of India given at the end of the book. Notice the direction of the flow of the rivers.

On the Peninsular Plateau, most big rivers flow from west to east, and only a few flow west.

@edugrown Why Peninsular Rivers Mostly Flow EAST Deccan Plateau — tilts gently to the EAST Western Ghats (higher) Eastern Ghats (lower) Godavari • Krishna • Kaveri • Mahanadi → Bay of Bengal Narmada, Tapti → Arabian Sea The land is high in the west and low in the east — water always runs downhill.
DirectionRiversDrain into
East-flowing (most)Godavari, Krishna, Kaveri, MahanadiBay of Bengal (they build large fertile deltas)
West-flowing (few)Narmada, TaptiArabian Sea (they form estuaries, not deltas)
Reason
  1. The Western Ghats are taller and stand close to the west coast like a wall.
  2. The Eastern Ghats are lower and broken.
  3. So the whole plateau tilts gently towards the east.
  4. 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.

Powerhouse Waterfalls at Periyakanal, near Munnar, Kerala
Fig. 1.28 — Waterfalls tumble down the steep Western Ghats.
Jog Falls in Karnataka
Fig. 1.1 — Jog Falls, Karnataka: the power of falling water is turned into hydroelectricity.
Q11
Let’s Explore · Page 17
Tribal communities are largely spread over the states of Jharkhand, West Bengal, Odisha, Assam, Madhya Pradesh, Chhattisgarh, Maharashtra, Telangana and Gujarat. Locate these states on the physical and political maps.
Dense forests of Chhattisgarh, home to many tribal communities
Fig. 1.27 — Dense forests of Chhattisgarh, home to many tribal communities.

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 mapStatesSome communities
Central plateau & forestsMadhya Pradesh, Chhattisgarh, Maharashtra, TelanganaGond, Baiga, Bhil, Korku
Eastern plateau & hillsJharkhand, Odisha, West BengalSanthal
Western plateau edgeGujaratBhil
North-eastern hills & valleyAssamMany north-eastern tribes
Coal mines in the plateau
Fig. 1.32 — The plateau is rich in minerals like coal — often right under these forests.
Shad Suk Mynsiem festival of the Khasi people
Fig. 1.41 — The Shad Suk Mynsiem festival: the Khasi people thank Nature.
What we learn
  • 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.
Q12
Let’s Explore · Page 19
Find five rivers that flow into the Bay of Bengal. Find out India’s coastal states and discuss the difference between the western and eastern coastal plains. What is it called when rivers split into multiple streams near the coast?
(a) Five rivers flowing into the Bay of Bengal
  1. Ganga
  2. Brahmaputra
  3. Mahanadi
  4. Godavari
  5. Krishna

(The Kaveri also flows into the Bay of Bengal.)

(b) India’s coastal states & UTs
CoastStates / UTs (in order)
West CoastGujarat, Maharashtra, Goa, Karnataka, Kerala (+ Daman & Diu, Dadra & Nagar Haveli, Lakshadweep)
East CoastTamil Nadu, Andhra Pradesh, Odisha, West Bengal (+ Puducherry, Andaman & Nicobar)
(c) Western vs Eastern coastal plains
FeatureWest CoastEast Coast
WidthNarrow — Western Ghats come very close to the seaWide plains
RiversShort, swift; rise in the Western GhatsLong, slow, big rivers from the plateau
River mouthsMostly estuaries (Narmada, Tapti are the largest)Large fertile deltas (Mahanadi, Godavari, Krishna, Kaveri)
CoastlineCoves, creeks, estuaries; alluvial depositsLagoons & lakes — Chilika Lake, Pulicat Lake
Stretches fromGujarat → KeralaGanga delta → Kanyakumari
Aerial view of the west coast
Fig. 1.34 — West coast: the Western Ghats stand very close to the Arabian Sea.
Satellite view of the East Coast of India
Fig. 1.35 — East coast: wide plains and big river deltas.
(d) When rivers split into many streams near the coast

These branches are called distributaries, and the triangular fan-shaped land they build is called a delta.

@edugrown How a Delta Forms (Distributaries) SEA River carrying silt DELTA Streams that split near the mouth = DISTRIBUTARIES Sediment settles → triangular / fan-shaped fertile land (Ganga–Brahmaputra delta = Sundarbans)
Mumbai on the west coast
Fig. 1.33 — Mumbai, on the west coast, is India’s financial centre; the coast has many ancient ports.
Floating dock of the Indian Navy near the Andaman Islands
Fig. 1.38 — A floating dock of the Indian Navy near the Andaman Islands.

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.

1
Exercise · Page 24
What, in your opinion, are two important geographical features of India? Why do you think they are important?

(This is an opinion question — here is a well-reasoned model answer.)

Feature 1 — The Himalayas
Satellite images of the Himalayan range
Fig. 1.2 — The Himalayan range, about 2500 km long.
  • 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.
Feature 2 — The Gangetic (Northern) Plains
Multi-cropping in Uttar Pradesh
Fig. 1.13 — Multi-cropping in the fertile Gangetic plains.
Rural women working in a paddy field in West Bengal
Fig. 1.14 — Paddy fields of West Bengal.
  • 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.
A third feature worth naming — our rivers and the life they support
Tiger in Bandhavgarh
Fig. 1.18 — The tiger, saved by Project Tiger.
The Indian gharial
Fig. 1.19 — The Indian gharial of our rivers, on the verge of extinction.

In one line

The Himalayas give us water and protection; the plains give us food and a home. Together they made Indian civilisation possible.

2
Exercise · Page 25
What do you think India might have looked like if the Himalayas did not exist? Write a short note or sketch a drawing to express your imagination.

If the Himalayas did not exist, India would be a very different — and much harsher — land.

Map showing India's journey to Eurasia
Fig. 1.4 — India's journey to Eurasia. The collision crumpled the land and raised the Himalayas.
Folded layers of Himalayan rock
Fig. 1.5 — Folded layers of Himalayan rock: proof of the collision that raised these mountains.
1. Climate would change completely
  • 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.
2. Rivers would dry up
  • 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.
3. People and history would change
  • 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.
@edugrown Collision that built the Himalayas INDIAN PLATE EURASIAN PLATE Himalayas (crumpled, folded rock) India still pushes north ≈ 5 cm / year Result: Himalayas rise ≈ 5 mm / year Like a carpet wrinkling when pushed

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.”

3
Exercise · Page 25
India has been called a ‘mini-continent’. Based on what you’ve read, why do you think this is so?

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 hasIndia’s own version
The highest mountainsThe Himalayas, with peaks over 8000 m
Great fertile plainsThe Gangetic Plains
Hot desertsThe Thar Desert
Cold desertsLadakh (winter below –30°C)
Ancient plateausThe Deccan (Peninsular) Plateau, the Aravallis
Long coastlinesOver 7500 km, on three seas
Islands & coral reefs & a volcanoLakshadweep, Andaman & Nicobar, Barren Island
Rain forests & heaviest rainfallThe Western Ghats, Meghalaya (Cherrapunji)
Many peoples, languages, religionsHundreds of languages, tribes and traditions
Moonland, Ladakh
Fig. 1.8 — Cold desert: Moonland, Ladakh.
Sand dunes of the Thar Desert
Fig. 1.21 — Hot desert: the Thar.
Pangong Tso, Ladakh
Fig. 1.10 — Pangong Tso, a salty high-altitude lake in Ladakh.
Yaks in the Himalayas
Fig. 1.9 — Yaks: milk, meat, wool, dung and transport for Himalayan people.
Active volcano on Barren Island
Fig. 1.39 — Barren Island: India’s only active volcano.
Seven Sisters Waterfalls, Meghalaya
Fig. 1.41 — Meghalaya: one of the wettest places on Earth.
Grey langur in Bandhavgarh National Park
Fig. 1.17 — Grey langur of the northern plains.
A peacock and peahen
Fig. 1.20 — The Indian peacock, our national bird.

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”.

4
Exercise · Page 25
Follow one of India’s big rivers from where it starts to where it meets the ocean. What are the different ways in which people might utilise this river along its journey?

Let us follow the Ganga — from a glacier in the Himalayas to the sea.

Gaumukh, the snout of the Gangotri Glacier
Fig. 1.3 — Gaumukh ('Cow's Mouth'), the edge of the Gangotri Glacier in Uttarakhand — where the Bhagirathi (Ganga) begins.
Stage of the journeyHow 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 valleysFast-flowing water turns turbines → hydroelectricity; river rafting and tourism.
3. Entering the plains — at HaridwarDrinking water; religious bathing and festivals; towns and temples grow on the banks.
4. Across the Gangetic PlainsIrrigation through canals; the silt makes soil fertile → farming and multi-cropping; industries use the water; fishing.
5. Lower courseTransport & trade — boats and ships have carried people and goods for millennia; ports and cities (e.g., Kolkata).
6. Mouth — the Ganga–Brahmaputra delta, the SundarbansFertile delta farming; fishing; mangrove forests protect the coast; home of the Royal Bengal Tiger; a UNESCO Heritage site.
Modes of transport in the Gangetic plains
Fig. 1.15 — Mid-course: boats and railways along the river.
Mangroves of the Sundarbans
Fig. 1.40 — The journey ends: mangroves of the Sundarbans delta.

Summary of uses

Drinking • Irrigation • Farming (fertile silt) • Hydroelectricity • Industry • Transport & trade • Fishing • Tourism • Religious and cultural life.

5
Exercise · Page 25
Why is the southern part of India referred to as a peninsular plateau?

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 peninsula

A 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
Part 2 — It is a plateau

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.
@edugrown The 5 Physical Regions of India 1. Himalayas 2. Northern (Gangetic) Plains 3. Thar Desert 4. Peninsular Plateau (Deccan Plateau) Western Ghats Eastern Ghats 5. Lakshadweep 5. Andaman & Nicobar Arabian Sea Bay of Bengal Indian Ocean
Life on the Peninsular Plateau
Lion-tailed macaque in the Western Ghats
Fig. 1.29 — Lion-tailed macaque of the Western Ghats.
King cobra of the Western Ghats
Fig. 1.30 — King cobra of the Western Ghats.
Insectivorous plant of the Western Ghats
Fig. 1.31 — An insectivorous plant that traps and digests insects.
Coal mines in the plateau
Fig. 1.32 — Coal mines: the plateau is rich in minerals.

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.

6
Exercise · Page 25
Which UNESCO Heritage Site mentioned in this chapter did you find more interesting? Write a short paragraph to describe what about it is interesting.
UNESCO sites mentioned in this chapter
  1. Great Himalayan National Park, Himachal Pradesh
  2. Jaisalmer Fort, Rajasthan (in the Thar Desert)
  3. The Western Ghats
  4. The Sundarbans (Ganga–Brahmaputra delta)
Model answer — the Sundarbans
Mangroves of the delta in the Sundarbans of West Bengal
Fig. 1.40 — Mangroves of the Sundarbans delta, West Bengal.

“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.”

Great Himalayan National Park collage
Fig. 1.7 — Great Himalayan National Park: snow leopard, Himalayan monal, the Beas river, rhododendron and a local market.
The other UNESCO sites in this chapter
Jaisalmer Fort
Fig. 1.22 — Jaisalmer Fort, a UNESCO World Heritage site in the Thar.
Waterfall in the Western Ghats
Fig. 1.28 — The Western Ghats, a UNESCO World Heritage Site.
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Exercise · Page 25
Look at the two maps of India, physical as well as political. Identify the place you are at now. Which physical feature of India would you use to describe its location?

(Answer according to where you live. Here is a worked example, and a method you can use for any place.)

Method — 3 easy steps
  1. Find your state on the political map.
  2. 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).
  3. Name the nearest big physical feature — a mountain range, river, plateau, desert or coast.
Worked example — Indore, Madhya Pradesh

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.”

A part of the Aravallis and the Aravallis from space
Fig. 1.25 — Match the political map with the physical map: here the Aravallis end and the Thar Desert begins.
If you live in…Describe your location as…
Delhi, Lucknow, Patna, KolkataOn the Gangetic (Northern) Plains
Jaipur, Jodhpur, JaisalmerIn / at the edge of the Thar Desert, near the Aravallis
Shimla, Dehradun, GangtokIn the Himalayas
Bhopal, Indore, Nagpur, HyderabadOn the Peninsular / Deccan Plateau
Mumbai, Goa, KochiOn the West Coast, near the Western Ghats
Chennai, Visakhapatnam, PuriOn the East Coast, near the Eastern Ghats
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Exercise · Page 25
Food preservation techniques differ from place to place across India. They are adapted to local conditions. Do a class project: gather different methods of preserving food.

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 & conditionsMethodExamples
Thar Desert / Rajasthan — hot, dry, very little waterSun-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 growsFreeze-drying & air-drying in the cold dry air; storing for winterDried vegetables and greens, dried apricots, dried meat, hard cheese (chhurpi)
Coastal regions (Kerala, Goa, Bengal) — plenty of fish, plenty of saltSalting & smokingSalted/dried fish (sukka fish), salted prawns
Gangetic Plains — plenty of grain and vegetables, humid summersPickling in oil, salt & spices; making jams & murabbas in sugarMango & lemon pickle, amla murabba
All over IndiaFermentation (good bacteria stop spoilage)Curd, idli/dosa batter, gundruk (north-east)
Modern methodsRefrigeration, canning, vacuum packingFrozen peas, canned juices
Why these methods work (the science)
  • 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.

Women fetching water and a rainwater harvesting structure
Fig. 1.24 — In the desert, water itself is precious: utensils are scoured with sand, and rainwater is stored in taanka or kunds.
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Exercise · Page 25
Despite having such different regions (mountains, deserts, plains, coasts), India remains one country. How do you think our geography has helped unite people?

India’s geography looks like it should divide people — but in fact it has bound them together.

1. A natural, well-defined home

The 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 region

Rivers 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.

Modes of transport in the Gangetic plains
Fig. 1.15 — Roads, railways and boats tie distant regions into one economy.
3. Shared sacred geography

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 other

Diversity 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 all

The 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.”

Living root bridges of Meghalaya
Fig. 1.42 — Living root bridges: people shaping their land with care.
Living roots bridge near Nongriat village
Fig. 1.41 — Nongriat, Cherrapunjee: tree roots woven over many years.
Jog Falls in Karnataka
Fig. 1.1 — Jog Falls, Karnataka: geography that gives beauty, power and life.

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