NCERT Solutions for Class 8th Social Science Chapter 8 World Geography: Some Glimpses

Updated on 2026-09-19

About this chapter

The Earth is an oblate spheroid , so no flat map can be perfectly true. Every map projection is a compromise: the Mercator keeps shape and direction but swells sizes near the poles, the Robinson balances size against shape. To understand the world fairly, look at more than one projection. The oceans cover about 71 per cent of the Earth’s surface and hold 97 per cent of its water. They feed life, give us almost half our oxygen through plankton, and steady the climate by soaking up heat, releasing it slowly and adding moisture to the air. Currents, trenches and reefs make the ocean floor as varied as the land. Seas, gulfs, bays, straits and canals are named according to their shape and their link to the ocean, and each has shaped trade — the Persian Gulf, the Bay of Bengal, the Strait of Mal

  • Chapter opener
  • The Complexity of Mapping the Earth
  • The Blue of the Blue Planet, the Oceans
  • Asia
  • Roof of the world
  • The Urals
  • Europe
  • Africa
  • South America
  • The Australian Continent (Fig. 1.34)
Quick revision
TermWhat it meansWhere the chapter uses itFact to remember
Oblate spheroidA nearly spherical shape that bulges at the equator and is slightly flattened at the poles due to its rotationThe Complexity of Mapping the Earth, p. 2This curved shape is exactly why a flat map must distort something
Map projectionThe process of showing the Earth on a flat surfacepp. 2–3, Fig. 1.2Mercator preserves shape and direction; Robinson balances size and shape
PlanktonMicroscopic organisms that have chlorophyll and use sunlight and carbon-dioxide to make foodTHINK ABOUT IT, p. 4Oceans give us almost half the oxygen we breathe, and plankton make this possible
Ocean currentsGiant ‘rivers’ flowing through the ocean — warm ones from the equator to the poles, cold ones from the poles to the equatorOcean currents, pp. 5–6The Gulf Stream makes the United Kingdom warmer than other places at the same latitude
TrenchA very deep, V-shaped area of the seafloorOcean trenches, p. 6The Challenger Deep in the Mariana Trench reaches over 11,000 metres below sea level
ReefA ridge at or near the surface of the ocean, formed naturally or artificiallyThe Great Barrier Reef, pp. 7–8The Great Barrier Reef stretches over 2,000 km and covers about 350,000 square kilometres
TectonicGeological forces related to the movement of the Earth’s crustTibetan Plateau, p. 12The Indo-Australian–Eurasian collision raised both the Himalaya and the plateau behind it
SteppeA large area of flat unforested grassland with a temperate climate, hot summers, cold winters and moderate, often seasonal rainfallThe Eurasian Steppes, p. 14Spread over 8,000 km west to east; a global carbon sink
Water towersMountains that hold water at a height and release freshwater through melting snow and glaciersThe Urals, p. 15The Tibetan Plateau is called the ‘Third Pole’ for its freshwater reserves
Tundra / permafrostA treeless, cold plain whose soil stays frozen most of the time; that frozen soil is permafrostThe Urals, p. 16Melting permafrost releases carbon dioxide and methane, speeding up climate change
SavannahA tropical grassland with wide open spaces, scattered trees and seasonal rainfallAfrica, p. 20It lies mainly between tropical rainforests and deserts
Fast fashionReplication of trendy clothing fast and at low cost, discarded very quickly when trends changeAtacama Desert, p. 25The UN has called the Atacama clothing dump ‘an environmental and social emergency’
  1. Chapter opener — The Big Questions Page 1
  2. The Complexity of Mapping the Earth — LET’S EXPLORE Page 2
  3. The Blue of the Blue Planet, the Oceans — THINK ABOUT IT Page 4
  4. Asia — LET’S EXPLORE Page 11
  5. Roof of the world — In-text Questions Page 12
  6. The Urals — LET’S EXPLORE Page 15
  7. Europe — LET’S EXPLORE Page 18
  8. Africa — LET’S EXPLORE Page 22
  9. South America — LET’S EXPLORE Page 24
  10. The Australian Continent (Fig. 1.34) — In-text Questions Page 29
  11. End of chapter — Questions and activities Page 31–32
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