THE GIST OF NCERT
GEOGRAPHY class 7
                 Chapter 1: Environment
1.1 Definition of Environment
      Environment refers to the place, people, things, and nature surrounding any
       living organism.
      It is a combination of natural and human-made phenomena.
      Natural Environment includes biotic (living) and abiotic (non-living)
       conditions.
      Human Environment includes human activities, creations, and interactions.
      Word Origin: Environment comes from French ‘environner’, meaning
       neighbourhood.
1.2 Components of Natural Environment
      Includes land, water, air, plants, animals.
      Domains of the environment:
           o Lithosphere (land)
           o Hydrosphere (water)
           o Atmosphere (air)
           o Biosphere (living world)
1.3 Lithosphere
      Solid crust or hard top layer of Earth, made of rocks and minerals, with a
       thin soil layer.
      Includes mountains, plateaus, plains, valleys – found on both continents and
       ocean floors.
      Provides land for agriculture, forests, human settlements, and is a source of
       minerals.
1.4 Hydrosphere
      Refers to all forms of water bodies – rivers, lakes, seas, oceans.
      Water is essential for life.
1.5 Atmosphere
      Thin layer of air surrounding the Earth, held by gravitational force.
      Protects from harmful solar rays and heat.
      Composed of gases, dust, and water vapour.
      Weather and climate result from atmospheric changes.
1.6 Biosphere
      Includes all plants and animals; the living world.
      A narrow zone where land, water, and air interact to support life.
1.7 Ecosystem
      Defined as interaction among living organisms and their physical &
       chemical surroundings.
      Examples: Rainforests, grasslands, deserts, mountains, rivers, ponds,
       oceans.
      All elements are linked by energy and material transfer.
1.8 Human Environment
      Humans interact and modify the environment to fulfill needs.
      Early humans lived simply, adapted to nature, and used natural resources
       directly.
      Over time, needs increased, leading to development of tools, farming, animal
       domestication, and settled life.
      Key human advances:
           o Invention of wheel
           o Agricultural surplus
           o Barter system: Trade without money
           o Trade and commerce growth
           o Industrial Revolution: Enabled mass production
           o Transport became faster
           o Information Revolution led to instant global communication
1.9 Important Fact
      World Environment Day is celebrated on 5th June every year to raise
       awareness about environmental protection.
              Chapter 2: Inside Our Earth
2.1 Earth – A Dynamic Planet
      Earth is constantly undergoing internal and external changes.
      Like an onion, Earth has concentric layers.
2.2 Interior of the Earth
      Crust:
          o   Outermost, thinnest layer.
          o   Thickness: 35 km (continental), 5 km (oceanic).
          o   Composition:
                   Continental Crust: Silica + Alumina = SIAL.
                   Oceanic Crust: Silica + Magnesium = SIMAL.
      Mantle:
          o Below crust, extends to 2900 km depth.
          o 84% of Earth’s volume.
      Core:
          o Innermost layer, radius ~3500 km.
          o Composition: Nickel + Iron = NIFE.
          o Very high temperature and pressure.
          o Makes up 15% of Earth’s volume.
      Total Earth radius = 6371 km.
2.3 Rocks and Minerals
       Earth’s crust is made of rocks – natural mass of mineral matter.
       Rocks vary in colour, size, texture.
2.4 Types of Rocks
       Igneous Rocks (Primary Rocks):
           o Formed from cooling of molten magma.
           o Types:
                  Extrusive Igneous Rocks: Magma cools on surface, fine-
                     grained (e.g., Basalt – Deccan Plateau).
                  Intrusive Igneous Rocks: Magma cools inside crust, coarse-
                     grained (e.g., Granite – used in grinders).
       Sedimentary Rocks:
           o Formed from compressed and hardened sediments.
           o Example: Sandstone (from sand grains).
           o May contain fossils (remains of ancient life).
       Metamorphic Rocks:
           o Formed when igneous/sedimentary rocks change under heat &
              pressure.
           o Example: Granite → Gneiss, Coal → Diamond.
2.5 Rock Cycle
       Rock cycle = continuous transformation of rocks.
           o Magma → Igneous Rock → Sediments → Sedimentary Rock → Heat &
              Pressure → Metamorphic Rock → Melts → Magma again.
2.6 Minerals
       Naturally occurring substances with fixed physical properties and chemical
        composition.
       Importance:
           o As fuels: coal, natural gas, petroleum.
           o In industries: iron, aluminium, gold, uranium.
           o In medicine, fertilisers, etc.
2.7 Important Terms
       Crust: Earth’s outermost hard layer.
       Mantle: Layer beneath crust.
       Core: Earth’s inner part (nickel + iron).
       Rock: Solid part of Earth’s crust, made of minerals.
       Mineral: Naturally occurring, non-living solid.
       Rock Cycle: Transformation process of one rock type into another.
       Fossils: Remains of dead plants/animals in rocks.
.
         Chapter 3: Our Changing Earth
3.1 Lithospheric Plates
      Earth’s crust consists of large and small rigid plates carrying continents and
       ocean floors.
      These are called lithospheric plates.
      Plates move a few millimetres per year due to circular movement of molten
       magma inside the Earth.
3.2 Forces Causing Earth Movements
      Endogenic Forces: Originate inside the Earth (e.g., earthquakes, volcanoes).
      Exogenic Forces: Originate on Earth’s surface (e.g., weathering, erosion).
3.3 Endogenic Forces – Sudden Movements
      Volcano: An opening (vent) in Earth's crust where molten material erupts.
      Earthquake:
          o Vibration of Earth’s surface due to plate movement.
          o Focus: Place inside crust where movement starts.
          o Epicentre: Point directly above focus on Earth’s surface.
          o Waves: Vibrations radiate outward from epicentre.
3.4 Types of Earthquake Waves
   1. P waves (Primary) – Longitudinal
   2. S waves (Secondary) – Transverse
   3. Surface waves – Most destructive
3.5 Measuring Earthquakes
      Measured by Seismograph.
      Magnitude: Richter Scale.
         o <2.0 – Minor; 5.0 – Damage likely; ≥7.0 – Major quake.
3.6 Earthquake Preparedness
      Safe Spots: Under table, desk, or against interior wall corner.
      Avoid: Fireplaces, chimneys, windows, mirrors.
      Be Prepared: Spread awareness to reduce impact.
      Local signs: Unusual animal behaviour may indicate upcoming quakes.
3.7 Major Landform Evolution
      Caused by weathering (breaking of rocks) and erosion (wearing away by water,
       wind, ice).
      Deposition of eroded material forms new landforms.
3.8 Work of a River
      Waterfall: Formed when river tumbles over steep slopes or hard rock (e.g.,
       Angel Falls – Venezuela; Niagara Falls – USA/Canada; Victoria Falls –
       Zambia/Zimbabwe).
      Meander: Large bend in river.
          o Ox-bow Lake: Formed when meander loop is cut off from main river.
      Floodplain: Formed by deposited sediments during floods.
          o Raised river banks = Levees.
      Delta:
          o Formed as river slows down near sea, breaks into distributaries, and
              deposits sediments at river mouth.
3.9 Work of Sea Waves (Coastal Landforms)
      Sea waves erode and deposit material along the coast, forming coastal
       landforms.
      Sea Caves: Cracks in coastal rocks enlarge to form hollow caves.
      Sea Arches: Roof of large sea cave remains, forming an arch.
      Stacks: Roof eroded further; only vertical walls remain.
      Sea Cliff: Steep rocky coast rising vertically above sea water.
      Beaches: Formed by deposition of sediments along the shore.
3.10 Work of Ice (Glacial Landforms)
      Glaciers: Rivers of ice that erode landscape by bulldozing soil and rocks.
      Create deep hollows, later filled with water to form glacial lakes.
      Glacial Moraine: Deposits of rocks, sand, silt left behind by glaciers.
3.11 Work of Wind (Desert Landforms)
      Wind is a major agent of erosion and deposition in deserts.
      Mushroom Rocks: Wind erodes lower section of rocks more, forming narrow
       base and wide top.
      Sand Dunes: Formed when wind-blown sand is deposited in small hill-like
       structures.
      Loess: Fine sand carried over long distances by wind, deposited in large areas
       (e.g., China).
3.12 Important Terms Summary
      Earthquake: Sudden shaking due to movement in Earth’s crust.
      Volcano: Opening in Earth’s crust where molten material erupts.
      Focus: Origin point of an earthquake inside Earth.
      Epicentre: Surface point directly above the focus.
      Weathering: Breaking of rocks on Earth’s surface.
      Erosion: Wearing away of landscape by water, wind, or ice.
      Sea Caves → Sea Arches → Stacks → Sea Cliffs: Sequence of landform
       evolution by sea wave erosion.
                             Chapter 4: Air
4.1 Atmosphere – Definition and Importance
       The atmosphere is a blanket of air surrounding Earth.
       It sustains life, provides oxygen for breathing, and protects from harmful solar
        radiation.
       Acts as a temperature regulator, preventing extreme heating (day) or freezing
        (night).
4.2 Greenhouse Effect and Global Warming
       Carbon dioxide (CO₂) traps heat radiated by Earth, creating a greenhouse
        effect—essential for maintaining Earth's temperature.
       Global warming: Excess CO₂ from burning fuels (coal, oil) increases Earth’s
        temperature, causing:
            o Melting snow, rising sea levels, floods, and climate changes.
            o Possible extinction of plant and animal species.
4.3 Composition of Atmosphere
       Major Gases:
           o Nitrogen (78%) – Plants need it; soil bacteria convert it into usable
               form.
           o Oxygen (21%) – Vital for breathing; replenished by photosynthesis.
           o Carbon dioxide (0.03%) – Used by plants; balanced through respiration
               and photosynthesis.
       Minor Gases: Argon, Helium, Ozone, Hydrogen.
       Dust particles and water vapour are also present.
       Air circulation: Warm air rises, cold air sinks, causing movement of air.
4.4 Structure of the Atmosphere
Divided into 5 layers based on temperature and height:
       Layer        Height                            Key Features
                               Most important; weather phenomena (rain, fog, hail)
Troposphere      0–13 km
                               occur here.
                               Clear sky; ideal for flying; contains ozone layer (UV
Stratosphere     13–50 km
                               shield).
Mesosphere       50–80 km      Meteorites burn up in this layer.
                               Temperature rises; Ionosphere helps in radio
Thermosphere 80–400 km
                               transmission.
                 Above 400     Uppermost layer; gases like helium, hydrogen escape
Exosphere
                 km            to space.
4.5 Weather and Climate
       Weather: Hour-to-hour, day-to-day condition of atmosphere (e.g., rain,
        sunshine, wind).
       Climate: Average weather condition over a long period.
       Daily weather forecasts help predict short-term atmospheric changes.
4.6 Temperature
      Degree of hotness or coldness of the air.
      Influenced by insolation – solar energy received by Earth.
      Insolation decreases from equator to poles, hence poles are colder.
      Urban Heat Island Effect: Cities are warmer than villages due to heat-retaining
       materials (e.g., concrete, asphalt).
      Standard Unit: Degree Celsius (°C); water freezes at 0°C and boils at 100°C.
4.7 Air Pressure
      Defined as pressure exerted by air's weight on Earth’s surface.
      Highest at sea level, decreases with height.
      Warm air → rises → low pressure → cloudy skies & rain.
      Cold air → sinks → high pressure → clear skies & sun.
      Wind blows from high pressure to low pressure areas.
      Astronaut suits are pressurized to prevent internal bleeding due to lack of
       external pressure.
4.8 Wind
      Wind: Movement of air from high to low pressure.
      Types of Winds:
          1. Permanent Winds: Trade winds, Westerlies, Easterlies – blow year-
             round in fixed direction.
          2. Seasonal Winds: Change direction by season – e.g., Monsoon in India.
          3. Local Winds: Blow in small areas for short periods – e.g., land and sea
             breeze, Loo (hot, dry wind in northern India).
      Winds are named after the direction they blow from – e.g., Westerly.
4.9 Cyclone – Nature’s Fury
      Example: Odisha cyclone (Bay of Bengal) – caused wind damage, heavy rain,
       tidal surges.
      Impact: Flooding, coastal destruction, severe weather due to depression
       formation.
4.10 Moisture and Humidity
      Moisture: Water vapour in air.
      Humidity: Amount of moisture in air at any time.
          o Hot air holds more moisture → more humid.
      Clouds: Form when water vapour condenses into droplets.
      When droplets become heavy → precipitation (rain, snow, sleet, hail).
      Types of Rainfall:
          1. Convectional Rainfall
          2. Orographic Rainfall
          3. Cyclonic Rainfall
      Rainwater replenishes groundwater; trees help prevent floods.
                             Chapter 5: Water
1. The Water Cycle
        Definition: The continuous process of evaporation, condensation, and
         precipitation by which water circulates between oceans, land, and atmosphere.
        Process:
            o Evaporation: Water turns into vapour due to sun’s heat.
            o Condensation: Vapour cools to form clouds.
            o Precipitation: Water falls as rain, snow, or sleet.
Do You Know? 3/4th of the Earth’s surface is covered with water.
2. Sources of Freshwater
       Source       Nature                      Notes
Rivers              Fresh     Surface runoff from land
Ponds               Fresh     Small inland water bodies
Springs             Fresh     Natural groundwater outlets
Glaciers            Fresh     Frozen freshwater reserves
Oceans & Seas       Saline    Contain dissolved salts, mainly NaCl
Salinity: Amount of salt (grams) in 1000 grams of water.
Average ocean salinity: 35 ppt (parts per thousand).
Dead Sea Salinity: ~340 grams/litre → high density, swimmers float.
3. Distribution of Water Bodies on Earth
     Water Body        % of Total Water Nature
Oceans                 97.3%            Saline
Ice-caps (glaciers)    2.0%             Fresh
Groundwater            0.68%            Fresh
Freshwater Lakes       0.009%           Fresh
Inland Seas/Salt Lakes 0.009%           Saline
Atmosphere             0.0019%          Fresh
Rivers                 0.00001%         Fresh
4. Ocean Circulation – An Overview
        Definition: Continuous movement of ocean water due to external forces like
         wind, gravity, and Earth’s rotation.
        Types of Movements:
            o Waves – surface water rise and fall.
            o Tides – periodic rise/fall due to gravity.
            o Currents – stream-like movement of water.
Do You Know? March 22 is observed as World Water Day to promote water
conservation.
5. Waves
      Definition: Alternate rising and falling of ocean surface water.
      Cause: Winds scraping across ocean surface.
      Effect: Bigger waves with stronger winds.
      Storm Waves: During storms, high-speed winds generate large waves →
       potential destruction.
Tsunami – A Special Type of Wave
      Definition: Huge tidal wave caused by underwater earthquake, volcanic
       eruption, or landslide.
      Height: Can reach up to 15 m or more.
      Speed: Travels up to 700–900 km/hr.
Do You Know? Tsunami means Harbour Wave in Japanese – often destroys harbours.
2004 Indian Ocean Tsunami Case Study
      Date: 26 December 2004
      Epicentre: Near western boundary of Sumatra (Magnitude: 9.0 Richter scale)
      Cause:
          o Indian Plate subducted under Burma Plate → sudden sea floor
              movement.
          o Water displacement → tsunami waves.
         Impact                                      Details
Speed                    Initially 800 km/hr → slowed to 70 km/hr near coast
Reach                    Up to 3 km inland
Casualties               Over 10,000 deaths in India
Most Affected Regions    Tamil Nadu, Andhra Pradesh, Kerala, Puducherry, Andaman
(India)                  & Nicobar Islands
                         Property destruction, loss of life, land submergence (e.g.,
Damage
                         Indira Point)
Observation: People gathered at shore to watch water withdrawal → heavy casualties
due to lack of awareness and early warning systems.
6. Significance of Tsunami Preparedness
      Problem: No tsunami warning systems in Indian Ocean at that time.
      Contrast: Pacific Ocean has early warning systems due to high seismic activity.
      Lesson: Need for early monitoring, public awareness, and infrastructure to
       minimize future damage.
Important Terms
      Salinity: Salt content in water.
      Water Cycle: Circulation of water through evaporation, condensation,
       precipitation.
      Tsunami: Large wave caused by underwater disturbances.
      Precipitation: Rain, snow, sleet falling from clouds.
      Condensation: Vapour cooling into water droplets..
7 Tides
       Definition: Rhythmic rise and fall of ocean water twice a day.
           o High Tide: Water rises to highest level, covering much of shore.
           o Low Tide: Water falls to lowest level and recedes from shore.
Causes of Tides:
       Gravitational pull of the moon and sun on Earth’s water.
       Stronger moon’s pull (due to proximity) causes greater tide effects.
Spring Tide:
       Occurs on Full Moon & New Moon days.
       Earth, Moon, and Sun are in a straight line.
       Causes highest tides.
Neap Tide:
       Occurs on First Quarter & Last Quarter moon phases.
       Gravitational pull of Sun and Moon acts in opposite directions.
       Causes low tides.
Importance of Tides:
       Navigation: High tides raise water levels near shores, aiding ship movement
        into harbours.
       Fishing: More fish come near shore during high tide → better catch.
       Tidal Energy: Rise/fall of tides used in some places for electricity generation.
8 Ocean Currents
       Definition: Streams of ocean water flowing constantly in definite directions
        on ocean surface.
       Can be Warm or Cold.
Types:
    1. Warm Ocean Currents:
          o Originate near equator, flow towards poles.
          o E.g. Gulf Stream (Atlantic Ocean)
    2. Cold Ocean Currents:
          o Originate near poles, flow towards tropics.
          o E.g. Labrador Current (North Atlantic)
Impact of Ocean Currents:
       Temperature Regulation:
           o Warm currents → increase coastal temperatures.
           o Cold currents → cool down nearby land areas.
       Fishing Grounds:
           o Where warm and cold currents meet → nutrient-rich waters → best
               fishing zones.
           o Examples:
                    Coasts of Japan (Kuroshio + Oyashio)
                    Eastern North America
        Navigation Hazard: Meeting of currents causes foggy weather, affects
         visibility and shipping safety.
Important Definitions (For Prelims):
       Term                        Meaning
Tide           Rhythmic rise/fall of sea water twice daily.
Spring Tide    Highest tide (Moon, Earth, Sun aligned).
Neap Tide      Lowest tide (Moon at quarter phases).
Ocean Current Constant flow of water in definite direction.
Terrarium      Enclosure for growing small house plants.
Saline         Water with salt content (e.g., oceans, salt lakes).
Do You Know?
        Salinity: Salt in 1000g of water.
             o Average ocean salinity = 35 ppt.
        Tsunami: In Japanese – “Harbour Wave”.
        World Water Day: 22 March (theme: water conservation).
 CHAPTER 6: NATURAL VEGETATION AND
              WILDLIFE
1. Natural Vegetation – Definition
        Natural Vegetation: Plants that grow naturally without human interference.
        Classification of Natural Vegetation:
          Category           Region Type                       Description
         Forests    High temperature & rainfall areas Dense/open tree cover
         Grasslands Moderate rainfall areas           Grass dominant
         Shrubs     Dry regions                       Thorny bushes, scrub vegetation
2. Types of Forests and Their Features
A. Tropical Evergreen Forests (Tropical Rainforests)
        Location: Near the equator and tropics.
        Climate: Hot & heavy rainfall throughout the year.
        Features:
            o No dry season → trees do not shed leaves together → evergreen.
            o Dense canopy prevents sunlight from reaching ground.
          o Hardwood trees: Rosewood, Ebony, Mahogany.
      Wildlife: Anaconda (can kill/eat large animals like crocodiles), monkeys, birds.
B. Tropical Deciduous Forests (Monsoon Forests)
      Location: India, Northern Australia, Central America.
      Climate: Seasonal changes → dry and wet seasons.
      Features:
          o Trees shed leaves in dry season to conserve water.
          o Hardwood trees: Sal, Teak, Neem, Shisham → used for furniture,
              transport, construction.
      Wildlife: Tigers, Lions, Elephants, Langurs, Monkeys.
C. Temperate Evergreen Forests
      Location: Mid-latitude coastal regions – e.g., SE USA, South China, SE
       Brazil.
      Features:
          o Mix of hardwood and softwood trees: Oak, Pine, Eucalyptus.
          o Moderate rainfall, no distinct dry season.
D. Temperate Deciduous Forests
      Location: NE USA, China, New Zealand, Chile, Western Europe.
      Features:
          o Trees shed leaves in dry season.
          o Common trees: Oak, Ash, Beech.
      Wildlife: Deer, Foxes, Wolves, Birds (Pheasants, Monals).
E. Mediterranean Vegetation
      Location:
          o Around Mediterranean Sea in Europe, Africa, Asia.
          o Also in California (USA), SW Africa, SW South America, SW
              Australia.
      Climate: Hot dry summers, mild rainy winters.
      Features:
          o Trees have thick bark, waxy leaves to reduce water loss.
          o Vegetation cleared for fruit cultivation: Oranges, Figs, Olives, Grapes.
      Wildlife: Sparse wildlife due to human modification.
Do You Know? Mediterranean regions are known as “Orchards of the World” due to
rich fruit cultivation.
F. Coniferous Forests (Taiga)
      Location: Higher latitudes (50°–70° N Hemisphere) and higher altitudes (e.g.,
       Himalayas).
      Features:
          o Evergreen softwood trees: Chir, Pine, Cedar.
          o Used for pulp (paper, newsprint), match/packing boxes.
          o Wildlife: Silver Fox, Mink, Polar Bear.
Summary Table: Forest Types & Key Details
   Forest Type           Key Trees                Wildlife                Uses
Tropical           Rosewood, Ebony,        Anaconda, Birds,       Timber, Oxygen
Evergreen          Mahogany                Monkeys                source
Tropical           Sal, Teak, Neem,        Tiger, Elephant,
                                                                  Furniture, Transport
Deciduous          Shisham                 Langur
Temperate                                                         Timber,
                   Oak, Pine, Eucalyptus Moderate wildlife
Evergreen                                                         Construction
Temperate
                   Oak, Ash, Beech         Deer, Fox, Pheasant    Timber, Hunting
Deciduous
                   Olive, Fig, Citrus
Mediterranean                              Sparse wildlife        Fruit cultivation
                   fruits
                                           Silver Fox, Mink,      Paper, Newsprint,
Coniferous (Taiga) Chir, Pine, Cedar
                                           Polar Bear             Packing
3. Grasslands – Types and Features
A. Tropical Grasslands
      Location: On either side of the equator extending to the tropics.
      Rainfall: Moderate to low rainfall.
      Vegetation:
          o Tall grasses – up to 3–4 metres in height.
      Example: Savannah Grasslands of Africa.
      Wildlife: Elephants, Zebras, Giraffes, Deer, Leopards.
Do You Know?
Grasslands have different names across regions:
 Region Grassland Name
East Africa Savanna
Brazil      Campos
Venezuela Llanos
B. Temperate Grasslands
      Location: Mid-latitudinal zones, interior of continents.
      Vegetation:
          o Short and nutritious grass.
      Wildlife: Wild Buffaloes, Bisons, Antelopes.
Do You Know?
Names of Temperate Grasslands:
   Region     Grassland Name
Argentina     Pampas
North America Prairie
South Africa Veld
Central Asia Steppe
Australia     Downs
4. Desert Vegetation – Thorny Bushes
      Location: Tropical deserts, mostly on western margins of continents.
      Climate: Scanty rainfall, scorching heat.
      Vegetation:
          o Sparse cover – thorny bushes, shrubs.
      Indian Example: Thar Desert (Great Indian Desert).
      Wildlife: Camel, Desert Fox, Snakes, Lizards.
Do You Know?
Desert regions can be identified on the world map – e.g., Sahara (Africa), Gobi (Asia),
Atacama (South America).
5. Tundra Vegetation (Polar Region)
      Location: Polar regions – Europe, Asia, North America.
      Climate: Extremely cold, short summer.
      Vegetation:
          o Only mosses, lichens, and small shrubs grow.
      Wildlife:
          o Animals with thick fur/skin to survive cold:
              Seals, Walruses, Musk-oxen, Arctic Owl, Polar Bear, Snow Fox.
6. Important Terms – Glossary
    Term                                      Definition
Vegetation    Plants in general, or plants in a specific area.
Wildlife      Wild animals collectively.
Tropical      Area between the two Tropics; hot and humid.
Deciduous     Trees that shed leaves annually.
Temperate     Moderate climate – neither too hot nor too cold.
              Region around Mediterranean Sea; mild, dry summers and wet
Mediterranean
              winters.
Coniferous    Trees with cones and evergreen leaves (e.g., Pine, Cedar).
Tundra        Flat, treeless Arctic region – cold with short vegetation season.
        CHAPTER 7: HUMAN ENVIRONMENT –
          SETTLEMENT, TRANSPORT AND
               COMMUNICATION
1. Human Settlements
A. Definition
      Settlement: A place where people build homes and live.
      Early Humans: Lived in trees and caves; later began growing food and
       needed permanent homes.
B. Development of Settlements
        Earliest settlements grew near river valleys (due to water availability and
         fertile soil).
        Growth of trade, commerce, and manufacturing led to larger settlements and
         civilizations.
Do You Know?
Famous ancient river valley civilizations:
        Indus (India)
        Tigris-Euphrates (Mesopotamia)
        Nile (Egypt)
        Hwang-He (China)
2. Types of Settlements
A. By Duration
   Type                                 Characteristics
Temporary Occupied for short time, e.g., by hunters, gatherers, shifting cultivators.
Permanent People build permanent homes, engage in agriculture, trade, etc.
        Transhumance: Seasonal movement of people who rear animals, moving in
         search of pastures.
3. Transport – Evolution and Importance
A. Definition
        Transport: The means by which people and goods move from one place to
         another.
B. Historical Development
        Early humans walked, used animals for carrying goods.
        Invention of wheel made transport easier.
        Today, transport includes modern vehicles, but animals are still used in many
         regions.
Examples of Animal Transport:
        Region              Animals Used
India             Donkeys, Mules, Bullocks, Camels
Andes Mountains Llamas
Tibet             Yaks
4. Roadways
A. Types of Roads
       Type                              Description
Metalled Roads    Pucca roads, made of concrete/tar; found mostly in plains.
Unmetalled Roads Kutcha roads; used in rural/remote areas.
B. Special Road Constructions
      Subways/Underpasses: Roads built underground.
      Flyovers: Roads built above ground on raised structures.
Important Fact:
      Manali-Leh Highway (Himalayas) – one of the highest roads in the world.
      Xining-Lhasa Train (China) runs at 4,000 m altitude, highest point at 5,072 m.
Do You Know?
      India has National and State highways.
      The Golden Quadrilateral Expressway connects Delhi, Mumbai, Chennai,
       Kolkata.
5. Railways
      Railways carry heavy goods and passengers over long distances, quickly and
       cheaply.
      Development began after invention of the steam engine during the Industrial
       Revolution.
      Today, diesel and electric engines are common; some areas have superfast
       trains.
      Railway networks are dense in plains; in mountains, fewer due to construction
       difficulty.
      Indian Railways: One of the largest networks in the world and largest in
       Asia.
Do You Know?
The Trans-Siberian Railway is the longest railway line, connecting St. Petersburg to
Vladivostok (Russia).
6. Waterways
      One of the oldest and cheapest transport modes, ideal for heavy and bulky
       goods.
      Two types:
          o Inland Waterways: Rivers, lakes (e.g., Ganga–Brahmaputra, Great
              Lakes, Nile).
          o Sea Routes: Used for international trade, connected to ports.
      Major Ports:
          o Asia – Mumbai, Singapore
          o North America – New York, Los Angeles
          o South America – Rio de Janeiro
          o Africa – Durban, Cape Town
          o Australia – Sydney
          o   Europe – London, Rotterdam
7. Airways
      Fastest transport mode, developed in early 20th century.
      Most expensive due to high fuel cost; weather (fog, storms) affects travel.
      Reaches remote areas where roads/railways are absent.
      Helicopters used in disaster relief, rescue, and supply operations.
      Major Airports: Delhi, Mumbai, New York, London, Paris, Cairo.
8. Communication
      Communication: Process of conveying messages and information.
      Modern technology has enabled fast and global communication.
      Mass media: Newspapers, radio, TV – reach large audiences.
      Satellites: Enhance communication, help in weather forecasts, disaster
       warning, resource mapping.
      Internet: Enables emails, online bookings, access to global information.
      Mobile phones: Popular wireless communication tool.
      Global Society: Interconnected world through information and
       communication technologies (ICTs).
Important Terms
      Transport – Movement of people and goods.
      Communication – Process of message exchange.
      Mass Media – Media used to reach large public (e.g., TV, Internet).
      Transhumance – Seasonal movement for grazing pastures.
      Settlement – Place to live, may be temporary or permanent.
        Chapter 8: Human Environment
        Interactions – The Tropical and
              Subtropical Region
8.1 The Amazon Basin – Location and Geography
      The Amazon Basin lies in the equatorial region (between 10°N and 10°S).
      The Amazon River flows from west to east, originating in the Andes
       Mountains and draining into the Atlantic Ocean.
      The mouth of a river is the place where it flows into another water body.
      The basin covers Brazil, parts of Peru, Bolivia, Ecuador, Colombia, and
       Venezuela.
Do You Know?
Spanish explorers named the river Amazon after encountering tribes resembling
Amazons, the fierce female warriors of Roman lore.
8.2 Climate of the Amazon Basin
    The region has a hot and wet equatorial
         climate throughout the year.
         Day and night temperatures are high; humidity remains consistently high.
         Daily rainfall is common, often sudden. The air feels sticky.
8.3 Rainforests – Vegetation and Wildlife
         Heavy rainfall supports dense rainforests.
         The forest canopy forms a dense roof, preventing sunlight from reaching the
          forest floor.
         Only shade-tolerant plants grow on the dark, damp ground.
         Orchids and bromeliads grow as epiphytes (plant parasites).
Fauna of the Amazon Rainforest
         Birds: Toucans, hummingbirds, bird of paradise – bright plumage, large beaks,
          loud calls.
         Animals: Monkeys, sloths, anteaters (tapirs).
         Reptiles: Snakes (python, boa constrictor), crocodiles, anaconda.
         Insects: Thousands of species.
         Fishes: Includes piranha – a flesh-eating species.
Do You Know?
Bromeliads store water in their leaves; frogs lay eggs in these water pockets.
8.4 People of the Rainforests – Lifestyle and Agriculture
         People clear small forest patches to grow food – practice slash and burn
          agriculture.
         Men hunt and fish; women grow tapioca, pineapple, sweet potato.
         Staple food: Manioc (cassava) – grows underground like potatoes.
         Diet also includes queen ants and egg sacs.
         Cash crops: Coffee, maize, cocoa.
Housing
         Houses built from wood; types:
             o Thatched beehive-shaped huts.
             o Maloca: Large, apartment-like houses with steep slanting roofs.
Do You Know?
Slash and burn farming: Trees are cut and burnt to release nutrients into the soil. After
a few years, soil becomes infertile, and a new patch is cleared.
8.5 Environmental Impact of Development
         Earlier, river navigation was the only way to access forest interiors.
         In 1970, the Trans-Amazon Highway made rainforests more accessible.
         Aircraft and helicopters now reach remote areas.
         Indigenous people were displaced and resettled but continued traditional
          farming.
Consequences of Forest Destruction
         Rainforests are rapidly disappearing, mainly due to developmental
          activities.
         Loss of forests leads to soil erosion; rain washes away topsoil.
         Lush forests are replaced by barren land, affecting biodiversity and climate.
8.6 Ganga-Brahmaputra Basin – Location and Geography
      Formed by tributaries of Ganga and Brahmaputra rivers (e.g., Ghaghra, Son,
       Chambal, Gandak, Kosi).
      Located in the subtropical region (between 10°N and 30°N latitudes).
      Main landforms: Ganga-Brahmaputra plains, Himalayan foothills, and the
       Sundarbans delta.
      Ox-bow lakes are common in the plains.
      Climate: Monsoon type – hot summers, cool winters; rainfall from June to
       September.
8.7 Population and Settlement Patterns
      Population density varies due to topography.
          o Mountains: Sparse population due to steep slopes and difficult terrain.
          o Plains: Densely populated due to fertile soil and flat land.
      Population density examples:
          o Uttarakhand: 189 persons/km²
          o West Bengal: 1029 persons/km²
          o Bihar: 1102 persons/km²
8.8 Agriculture – Crops and Techniques
      Main occupation: Agriculture.
      Staple crop: Paddy (rice) – grown in areas with high rainfall.
      Other food crops: Wheat, maize, sorghum, gram, millets.
      Cash crops: Sugarcane, jute, banana (plantations in plains).
      Tea plantations: Found in West Bengal and Assam.
      Sericulture (silk farming): Practiced in Bihar and Assam.
      In hilly regions, crops are grown using terrace farming.
Do You Know?
Terrace farming creates flat areas on steep slopes to reduce water runoff and grow
crops efficiently.
8.9 Natural Vegetation
      Plains: Tropical deciduous trees like teak, sal, peepal.
      Brahmaputra plain: Rich in bamboo groves.
      Sundarbans delta: Covered with mangrove forests.
      Mountains (Uttarakhand, Sikkim, Arunachal Pradesh): Coniferous trees –
       pine, deodar, fir.
8.10 Wildlife
      Common animals: Elephants, tigers, deer, monkeys.
      One-horned rhinoceros: Found in Brahmaputra plains.
      Sundarbans delta: Home to Bengal tiger, crocodiles, alligators.
      Aquatic life: Rivers, lakes, and the Bay of Bengal have rohu, catla, hilsa fish.
      Susu (blind dolphin) found in Ganga and Brahmaputra rivers – indicator of
       river health.
Do You Know?
Susu dolphins are endangered due to pollution from untreated urban and industrial
waste.
8.11 Transport and Cities
      All four modes of transport (road, rail, air, water) are well-developed in the
       basin.
           o Plains: Extensive roadways and railways.
           o Waterways: Important for river transport; Kolkata is a major port on
              Hooghly River.
           o Airports: Present in several cities.
8.12 Major Cities and Pollution
      Major cities: Allahabad, Kanpur, Varanasi, Lucknow, Patna, Kolkata.
      These cities discharge waste into rivers, causing river pollution.
8.13 Tourism and Cultural Importance
      Major tourist places:
          o Taj Mahal (Agra), Allahabad (confluence of Ganga and Yamuna),
          o Buddhist stupas (Uttar Pradesh, Bihar),
          o Lucknow’s Imambara,
          o Kaziranga and Manas Wildlife Sanctuaries (Assam),
          o Tribal culture (Arunachal Pradesh).
Important Terms
      Basin: Area drained by a river and its tributaries.
      Delta: Low flat land where a river divides before flowing into the sea.
      Rainforest: Dense tropical forest with heavy rainfall.
      Slash and burn: Farming method involving cutting and burning trees.
      Mouth: Where a river flows into another water body.
        Chapter 9: Life in the Temperate
                  Grasslands
9.1 Grasslands – Definition and Types
      Grasslands: Regions where grasses dominate plant life.
      Cover about 25% of Earth’s land surface.
      Vegetation depends on climate and soil conditions.
      Classified into:
          o Temperate grasslands – e.g., Prairies.
          o Tropical grasslands – e.g., Savannas (covered in Part 2).
9.2 The Prairies – Location and Origin
      Prairies: Temperate grasslands of North America.
          o Origin: Latin word priata meaning meadow.
      Landscape: Flat, gently sloping or hilly, mostly treeless.
          o Tall grasses (up to 2 m) form a "sea of grass".
          o Some woodlands in river valleys.
      Bounded by Rocky Mountains (West) and Great Lakes (East).
      Located in parts of USA and Canada.
          o USA: Drained by tributaries of Mississippi River.
          o   Canada: Drained by Saskatchewan River tributaries.
Do You Know?
Native tribes such as the Apache, Crow, Cree, Pawnee lived here. Known as “Red
Indians” by European settlers.
9.3 Climate of the Prairies
      Continental climate – large temperature variations.
          o Summer: Warm (~20°C).
          o Winter: Cold (down to –20°C in Winnipeg, Canada); snow cover
              common.
      Moderate rainfall – ideal for grass growth.
      Chinook: Hot local wind in winter; melts snow quickly, making pasture
       available.
Do You Know?
Chinook winds cause sudden warming, aiding winter grazing.
9.4 Flora and Fauna
      Mostly tree-less, except near water sources (willow, alder, poplar).
      Fertile soil – suitable for agriculture where rainfall >50 cm.
          o Main crop: Maize.
          o Others: Potato, soybean, cotton, alfalfa.
      Low-rainfall areas: Sparse grass, ideal for cattle rearing.
          o Large cattle farms = Ranches; managed by cowboys.
      Key animals:
          o Bison (American buffalo) – once near extinction; now protected.
          o Others: Rabbits, coyotes, gophers, prairie dogs.
9.5 People and Economy
      People are hardworking, utilizing natural resources efficiently.
      Located in USA and Canada – among world’s most developed nations.
          o Use of scientific farming, tractors, harvesters, combines.
      Agricultural surplus – especially wheat; called “Granaries of the World”.
      Dairy farming: Major industry; dairy belt from Great Lakes to Atlantic
       Coast.
      Development of food processing industries due to:
          o Surplus agriculture
          o Dairy farming
      Rich in coal, iron; excellent transport network (roads, rail, canals).
          o Result: One of the most industrialised regions globally.
Do You Know?
Major cities –
USA: Chicago, Minneapolis, Indianapolis, Kansas, Denver
Canada: Edmonton, Saskatoon, Calgary, Winnipeg
The Velds (South Africa)
9.6 The Velds – Location and Physical Features
      Velds: Temperate grasslands of South Africa.
      Terrain: Rolling plateaus, elevation 600–1100 m.                            o
                                                                                   o
      Bounded by:
          o Drakensberg Mountains (East)
          o Kalahari Desert (West)
      High Velds (NE): Some parts rise >1600 m.
      Drained by rivers: Orange and Limpopo tributaries.
Do You Know?
The name “Veld” was given by Dutch settlers before British colonization.
9.7 Climate of the Velds
      Mild climate due to Indian Ocean influence.
      Winter (June–Aug): Cold and dry; temp. 5°C to 10°C; July is coldest.
      Summer (Nov–Feb): Short and warm; e.g., Johannesburg ~20°C.
      Rainfall: Mainly in summer; due to warm ocean currents.
          o If winter rainfall is low → risk of drought.
9.8 Flora and Fauna
      Vegetation: Sparse; dominated by grass cover.
          o Red grass common in bush velds.
          o High Velds: Trees like acacia and maroola.
      Wildlife:
          o Predators: Lion, leopard, cheetah.
          o Herbivore: Kudu.
9.9 People and Economic Activities
Agriculture and Animal Rearing
      Soil fertility: Generally low, due to discontinuous grasses and exposed surface.
           o In fertile areas, crops grown:
                     Food crops: Maize, wheat, barley, oats, potato.
                     Cash crops: Tobacco, sugarcane, cotton.
      Sheep rearing:
           o Most important occupation.
           o Breed: Merino sheep – known for warm wool.
           o Basis of wool industry.
      Dairy farming:
           o Cattle reared in warmer, wetter areas.
           o Produce butter, cheese for domestic use and export.
Mining and Industry
      Rich mineral reserves:
          o Coal, iron → iron and steel industry.
          o Gold (Johannesburg – "Gold Capital")
          o Diamonds (Kimberley – famous diamond mines)
Do You Know?
Mining of gold and diamonds established trade with Britain; led to South Africa’s
colonization.
      Well-developed transport network supports mining and trade.
Important Cities and Historical Significance
       City              Known For
Johannesburg Gold mining capital of the world
Kimberley      Diamond mining hub
Key Terms to Remember
        Veld: Open, uncultivated grassland in Southern Africa.
        Prairie: Grassland in North America.
        Combine: Machine for cutting, threshing, cleaning crops.
        Ranch: Large farm for rearing animals (mainly in North America).
        Flora and Fauna: Plant and animal life of a region.
        Bison: American buffalo.
              Chapter 10: Life in the Deserts
The Hot Desert – The Sahara Desert
10.1 Deserts – An Overview
        Deserts are regions with low rainfall, sparse vegetation, and extreme
         temperatures.
        Two types based on temperature:
            o Hot deserts – e.g., Sahara
            o Cold deserts – e.g., Ladakh (India), Gobi (Mongolia)
        People adapt and live where water is available (e.g., oases).
10.2 The Sahara Desert – Location and Extent
        World’s largest hot desert, located in North Africa.
        Area: ~8.54 million sq. km (India ~3.2 million sq. km for comparison).
        Covers 11 countries:
            o Algeria, Chad, Egypt, Libya, Mali, Mauritania, Morocco, Niger, Sudan,
                Tunisia, Western Sahara.
        Terrain includes:
            o Sand dunes, gravel plains, rocky plateaus (elevation up to 2500 m).
Do You Know?
Ancient cave paintings show Sahara was once lush and green with rivers and wildlife
(e.g., crocodiles, elephants).
10.3 Climate of the Sahara Desert
        Scorching hot days (up to 50°C) and freezing nights (~0°C).
        Rainfall: Very low; short rainy season.
        Sky: Clear and cloudless – high evaporation rate.
        Al Azizia, Libya – recorded highest temperature (57.7°C) in 1922.
10.4 Flora and Fauna
       Vegetation adapted to dryness:
           o Cactus, date palms, acacia.
           o Oasis – fertile areas with water and greenery (e.g., date palms).
       Wildlife:
           o Camels, hyenas, jackals, foxes, scorpions, snakes, lizards.
Do You Know?
Fossil remains of fish found in Sahara – indicates it was once water-rich.
10.5 Life of People in the Sahara
Nomadic Tribes
       Bedouins, Tuaregs – traditional nomadic herders.
           o Livestock: Goats, sheep, camels, horses.
           o Products: Milk, hides (leather items), hair (mats, carpets, clothes,
              blankets).
       Wear heavy robes for protection against dust storms and heat.
Settled Population
       Live around oases and Nile Valley (Egypt).
           o Grow date palms, rice, wheat, barley, beans.
           o Egyptian cotton – globally famous crop.
10.6 Modern Transformations
       Oil discovery in Algeria, Libya, Egypt:
            o Transformed the economy; rise of oil & gas industries.
       Other minerals: Iron, phosphorus, manganese, uranium.
       Cultural landscape changing:
            o Modern buildings, roads, superhighways replacing camel paths.
            o Trucks replace camels in salt trade.
            o Tuaregs now act as tourist guides; many shift to urban jobs.
Do You Know?
Oases form in depressions where underground water reaches surface.
Example: Tafilalet Oasis in Morocco (~13,000 sq.km) – among largest oases in the
world.
Key Terms to Remember
        Term                                     Meaning
Oasis                Fertile area in a desert where water is available
Nomad                Person who moves from place to place for food, water, pasture
Depression           Low landform created by wind erosion, exposing groundwater
Bedouins/Tuaregs Nomadic tribes in the Sahara
10.7 Ladakh – Location and Physical Features
      Ladakh is a cold desert located in the Great Himalayas, eastern Jammu &
       Kashmir (UT).
      Enclosed by:
          o Karakoram Range (North)
          o Zanskar Mountains (South)
      Major river: Indus River – forms deep valleys and gorges.
      Famous glacier: Gangri Glacier.
Word Origin:
“La” = mountain pass; “Dak” = country → Ladakh = Land of Mountain Passes.
      Altitude: Varies from 3000 m (Kargil) to 8000 m (Karakoram).
10.8 Climate of Ladakh
      High altitude results in extremely cold and dry climate.
      Air is thin → intense sun exposure during the day.
      Summer temperatures: slightly above 0°C (day), <30°C (night).
      Winter temperatures: fall below –40°C.
      Lies in rain shadow of Himalayas → scanty rainfall (~10 cm/year).
      Experience of freezing winds and burning sun simultaneously.
Do You Know?
Drass (Ladakh) is one of the coldest inhabited places on Earth.
Ladakh is also called Khapachang = Land of Snow.
10.9 Flora and Fauna
      Due to high aridity, vegetation is sparse:
          o Scanty grasses, shrubs, willows, poplars in valleys.
          o Summer bloom: apples, apricots, walnuts.
Birds and Animals:
      Birds: Robins, Redstarts, Tibetan Snowcock, Ravens, Hoopoe (many
       migratory).
      Animals: Wild goats, wild sheep, yak, Ladakhi dogs.
          o Provide milk, meat, hides.
          o Yak’s milk → cheese and butter.
          o Sheep/goat hair → woollens.
Do You Know?
Chiru (Tibetan antelope) – endangered species, hunted for shahtoosh wool.
10.10 Life of People in Ladakh
      Resemblance with people of Tibet and Central Asia.
      Religion: Muslims and Buddhists.
      Famous Buddhist monasteries (Gompas): Hemis, Thiksey, Shey, Lamayuru.
Occupation and Agriculture:
      Summer crops: Barley, potatoes, peas, beans, turnips.
      Winter: People engage in festivities, ceremonies due to harsh climate.
      Women: Work in household, fields, manage shops/businesses.
10.11 Connectivity and Tourism
         Capital: Leh – well connected via road and air.
             o NH-1A connects Leh to Kashmir Valley via Zoji La Pass.
             o Other Himalayan passes: Rohtang La, Baralacha La, Lungalacha La,
                  Tanglang La.
Do You Know?
Willow trees of Ladakh used for making finest cricket bats.
         Tourism – Major activity:
              o Visit Gompas, trekking, view glaciers, festivals.
         Life is changing due to modernisation but people maintain harmony with
          nature.
              o Resources like water and fuel are used with great care, nothing is
                  wasted.
Key Terms to Remember
   Term                                 Meaning
Cold Desert Arid region with extremely cold climate and low rainfall
Glacier       Large, slow-moving mass of ice
Grove         Cluster of trees (e.g., willows, poplars)
Monastery Place where monks live and worship
Gompa         Buddhist monastery in Ladakh, Tibet, Nepal, Bhutan
Shahtoosh Fine wool from Chiru antelope (highly valued, endangered)