Bachelor of Arts (Hons) Geography

Physical Geography

Compiled from actual DU previous year question papers — key concepts, definitions, and exam patterns.

Physical Geography

🌍 Physical Geography — Complete Study Notes

B.A. (Hons) Geography | Semester I | Paper Code: 2292101101 | NEP-DSC

Compiled from official syllabus + Previous Year Question Papers (5072, 540)


📋 Paper Snapshot

DetailValue
Duration3 Hours
Max Marks90
Questions to AttemptAny 5 out of 9
Marks per QuestionEqual (18 each)
MediumEnglish or Hindi (not mixed)
Map StencilAllowed

📊 Syllabus → Weightage Map

UNIT I (Intro & Earth System) ████░░░░░░░░░░░░░░░░ 4 Hrs UNIT II (Atmosphere) ████████████████░░░░ 16 Hrs UNIT III (Lithosphere) ████████████████░░░░ 16 Hrs UNIT IV (Hydrosphere) ████████████░░░░░░░░ 12 Hrs UNIT V (Biosphere) ████████████░░░░░░░░ 12 Hrs
UnitTopicHoursPYQ Hits (out of 3 papers analysed)
IPhysical Geography, Earth as a System43/3 papers
IIAtmosphere, Insolation, Pressure & Winds163/3 papers
IIILithosphere, Isostasy, Folding/Faulting163/3 papers
IVHydrosphere, Currents & Tides123/3 papers
VBiosphere, Soil & Vegetation123/3 papers

Exam pattern insight: Every paper reliably draws one question from each unit — meaning if you prepare all 5 units solidly, you comfortably have 5 attemptable questions no matter which paper you get.


🔥 Most Repeated Questions (Frequency Chart)

Internal structure of Earth (seismic evidence) ██████████ 2× Insolation / factors affecting it ██████████ 2× Isostasy (define + adjustment/Airy) ██████████ 2× Composition & structure of atmosphere ██████████ 2× Components of Earth System ██████████ 2× Tides / types of tides ██████████ 2× Scope / Nature of Physical Geography ██████████ 2× Folding – types █████ 1× Vegetation distribution & variation █████ 1× Pressure belts & global wind system █████ 1× Ocean currents & factors █████ 1× Soil formation factors █████ 1× Biomes – characteristics █████ 1×

🗂️ Table of Contents

  1. Unit I — Physical Geography & Earth System
  2. Unit II — Atmosphere
  3. Unit III — Lithosphere
  4. Unit IV — Hydrosphere
  5. Unit V — Biosphere
  6. Full Previous-Year Question Bank
  7. Rapid Revision Sheet

🟦 UNIT I — Physical Geography: Definition, Nature, Scope, Earth as a System (4 Hrs)

1. Definition of Physical Geography

Physical Geography is the branch of geography that studies the natural features and processes of the Earth's surface — landforms, climate, water bodies, soils, and vegetation — and the physical laws underlying them.

Key definitions to quote:

  • Strabo: Geography describes the physical features of the earth and its inhabitants.
  • Arthur Holmes: Physical geography deals with the description and explanation of Earth's physical features.
  • Hartshorne: Geography is concerned with the areal differentiation of the earth's surface.

2. Nature of Physical Geography

  • Empirical, systematic, and analytical science.
  • Interdisciplinary — draws from geology, meteorology, oceanography, pedology, and biology.
  • Follows the scientific method: observation → classification → explanation → prediction.
  • Studies spatial (where) and temporal (how it changes over time) patterns of natural phenomena.
  • Bridges natural sciences and human geography (forms the base for environmental studies).

3. Scope of Physical Geography

Rendering diagram…

BranchDeals With
GeomorphologyLandforms, relief, internal/external earth processes
ClimatologyAtmosphere, weather, climate
OceanographyOceans, currents, tides, marine features
PedologySoil formation, classification, distribution
BiogeographyDistribution of flora and fauna

4. Earth as a System

The Earth functions as an integrated system of interacting spheres, exchanging matter and energy continuously (a "systems approach").

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5. Components of the Earth System

SphereCompositionKey Role
AtmosphereGaseous envelope (N₂, O₂, CO₂, water vapour)Weather, climate, protection from radiation
LithosphereSolid crust & upper mantle (rocks, soil)Landforms, relief, resource base
HydrosphereAll water — oceans, rivers, lakes, glaciers, groundwaterWater cycle, climate moderation
BiosphereAll living organismsEcological balance, biogeochemical cycles
(Cryosphere)Frozen water — ice caps, glaciersOften studied as a sub-part of hydrosphere

Interlinkages (why "system"):

  • Atmosphere ↔ Hydrosphere: evaporation, precipitation (hydrological cycle).
  • Lithosphere ↔ Biosphere: soil supports vegetation; roots weather rock.
  • Atmosphere ↔ Lithosphere: weathering, erosion by wind.
  • All spheres exchange energy driven by solar insolation, making Earth a dynamic equilibrium (open) system.

🟩 UNIT II — Atmosphere (16 Hrs)

A. Composition and Structure of the Atmosphere

Composition (by volume, dry air):

Gas% VolumeSignificance
Nitrogen (N₂)78.08%Dilutes O₂, supports protein synthesis
Oxygen (O₂)20.95%Respiration, combustion
Argon (Ar)0.93%Inert
Carbon Dioxide (CO₂)0.036%Greenhouse gas, photosynthesis
Others (Ne, He, O₃, H₂, water vapour, dust)TraceOzone absorbs UV; water vapour drives weather

Structure (vertical layers):

Rendering diagram…

LayerHeightKey Feature
Troposphere0–12 km (up to 18 km at equator)All weather phenomena; temp decreases with height (Normal Lapse Rate 6.5°C/km)
Stratosphere12–50 kmContains ozone layer; temperature increases with height
Mesosphere50–80 kmColdest part of atmosphere (~ -100°C); meteors burn up
Thermosphere80–700 kmTemperature rises sharply; ionosphere lies here (radio wave reflection)
Exosphere>700 kmOutermost, gradually merges into space

B. Insolation (Incoming Solar Radiation)

Definition

Insolation is the solar radiation received by the Earth's surface per unit area per unit time, usually expressed in langleys/minute or watts/m².

Factors Affecting Insolation / Temperature Distribution:

Rendering diagram…

FactorEffect
Latitude (angle of incidence)Vertical rays at equator concentrate energy; oblique rays at poles spread it over larger area → less insolation
Duration of daylightLonger days = more total insolation (summer poles)
Atmospheric transparencyClouds/dust/water vapour reflect & absorb radiation, reducing insolation
Land vs SeaLand heats/cools faster than water (specific heat difference) → continental vs maritime climates
AltitudeHigher altitude, thinner air, faster heat loss, lower temperature
Ocean currentsWarm currents raise coastal temps (e.g., Gulf Stream); cold currents lower them (e.g., Labrador)
Earth-Sun distancePerihelion (Jan, closer) vs Aphelion (July, farther) causes minor variation

Heat Budget of the Earth: Earth maintains energy balance — incoming solar radiation = outgoing terrestrial radiation (on an annual average), keeping global temperature stable.

100 units Incoming Solar Radiation ├─ 35 units reflected back (Albedo: clouds 27, atmosphere 6, surface 2) ├─ 14 units absorbed by atmosphere └─ 51 units absorbed by Earth's surface → Surface re-radiates as long-wave (terrestrial) radiation → Balanced by radiation + conduction + convection + latent heat loss

C. Pressure Belts and Global Wind System

Pressure Belts (idealized):

BeltLatitudeTypeCause
Equatorial LowLowIntense heating → rising air
Sub-Tropical High30°N/SHighDescending air (Hadley cell)
Sub-Polar Low60°N/SLowRising air, meeting of cold/warm winds
Polar High90°N/SHighIntense cold → sinking air

Rendering diagram…

Global Wind System (surface winds):

WindBlows From → ToLatitude
Trade WindsSub-tropical high → Equatorial low30° → 0° (NE in N. Hemisphere, SE in S. Hemisphere)
WesterliesSub-tropical high → Sub-polar low30° → 60°
Polar EasterliesPolar high → Sub-polar low90° → 60°
  • Winds are deflected by the Coriolis Effect (right in N. Hemisphere, left in S. Hemisphere — Ferrel's Law).
  • Three-cell circulation model: Hadley Cell (0–30°), Ferrel Cell (30–60°), Polar Cell (60–90°).

🟧 UNIT III — Lithosphere (16 Hrs)

A. Internal Structure of the Earth (Seismic Evidence)

Seismic waves (P and S waves) change velocity/direction at boundaries of different density material, revealing internal layering.

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LayerDepthStateEvidence
Crust0–35 km (continental), ~5-10 km (oceanic)SolidP-waves travel at moderate speed
Mantle35–2900 kmSolid/plastic (asthenosphere is semi-molten)Sudden velocity increase = Mohorovičić Discontinuity (Moho)
Outer Core2900–5150 kmLiquidS-waves cannot pass through liquid → S-wave shadow zone proves liquid outer core
Inner Core5150–6371 kmSolidP-waves speed up again (high pressure solidifies iron-nickel)

Key seismic proofs:

  • Shadow Zone: Region 103°–142° from earthquake focus receives no direct P-waves and no S-waves — proves the core is liquid and refracts waves.
  • Gutenberg Discontinuity: boundary between mantle and outer core (~2900 km).
  • Lehmann Discontinuity: boundary between outer and inner core (~5150 km).

B. Isostasy

Definition

Isostasy is the state of gravitational equilibrium between the Earth's crust (lithosphere) and mantle (asthenosphere), such that the crust "floats" at an elevation that depends on its thickness and density.

Analogy: Icebergs floating in water — thicker/lighter crust rises higher, denser/thinner crust sits lower.

Two Classical Theories:

TheoryProponentConcept
Airy's HypothesisGeorge AiryCrust has uniform density but variable thickness; mountains have deep "roots" that sink into denser mantle, like icebergs — bigger mountain = deeper root
Pratt's HypothesisJohn PrattCrust has uniform depth (compensation level) but variable density; mountains are made of lighter material, plains of denser material

Rendering diagram…

Isostatic Adjustment: When load is added (ice sheets, sediment) or removed (erosion, melting glaciers), the crust sinks or rises to restore equilibrium — e.g., post-glacial rebound in Scandinavia after ice-age glaciers melted.

C. Earth's Movements — Endogenic Forces (Folding & Faulting)

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Folding: Bending of rock strata due to compressional (horizontal) forces, producing wave-like undulations.

PartDescription
AnticlineUpfold, arch-shaped
SynclineDownfold, trough-shaped
LimbSides of the fold
AxisLine of maximum curvature

Types of Folds:

TypeCharacteristic
Symmetrical FoldLimbs dip equally on both sides
Asymmetrical FoldLimbs dip unequally
Overturned FoldOne limb pushed beyond vertical
Recumbent FoldFold lying almost horizontal
Isoclinal FoldLimbs parallel, dip in same direction
MonoclineLocal steepening in otherwise flat strata
Fan FoldBoth limbs bent outward like a fan

Faulting: Fracturing of rocks with displacement of blocks along the fracture (fault plane), due to tensional, compressional, or shearing stress.

Type of FaultCauseFeature
Normal FaultTensionHanging wall moves down relative to footwall
Reverse FaultCompressionHanging wall moves up
Strike-slip (Transform) FaultShearingHorizontal sliding (e.g., San Andreas Fault)
Graben (Rift Valley)TensionBlock sinks between two normal faults
HorstTensionBlock rises between two normal faults

(Exogenic forces — weathering, erosion by water/wind/ice — act to wear down these structures; part of the same unit's syllabus scope.)


🟦 UNIT IV — Hydrosphere (12 Hrs)

A. Hydrological Cycle

The continuous circulation of water between atmosphere, land, and ocean.

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Key processes: Evaporation → Condensation → Precipitation → Infiltration → Runoff → back to Ocean. Driven by solar energy and gravity; keeps freshwater renewable.

B. Ocean Currents

Definition

Large-scale, persistent horizontal movements of ocean water in a fairly definite direction.

Factors Affecting Ocean Currents:

FactorEffect
Prevailing windsPrimary driving force (e.g., trade winds drive equatorial currents)
Coriolis forceDeflects currents (right in N. Hemisphere, left in S. Hemisphere)
Water temperature/density differencesDrives thermohaline (deep) circulation
Salinity differencesDenser saline water sinks, creating circulation
Continental land massesDeflect and shape current paths (e.g., coastlines)
Earth's rotationContributes to gyral (circular) current patterns

Types: Warm currents (flow from equator to poles, e.g., Gulf Stream) and Cold currents (flow from poles to equator, e.g., Labrador, Peru/Humboldt).

C. Tides

Definition

Tides are the periodic rise and fall of sea level caused mainly by the gravitational pull of the Moon and Sun on Earth's oceans, combined with Earth's rotation.

Types of Tides:

BasisTypes
By Frequency (daily)Semi-diurnal (2 highs + 2 lows/day, most common), Diurnal (1 high + 1 low/day), Mixed Tides (varying heights)
By Position of Sun-Moon-EarthSpring Tides (Sun, Moon, Earth aligned — Full/New Moon — highest tidal range); Neap Tides (Sun-Moon at right angles — Half Moon — lowest tidal range)
By PeriodicityDiurnal, Semi-diurnal, Mixed/Semi-diurnal

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🟪 UNIT V — Biosphere (12 Hrs)

A. Factors Affecting Soil Formation

Soil forms through weathering of parent rock combined with organic input over time — classically summarized by Jenny's equation: S = f(cl, o, r, p, t)

FactorRole
Parent Material (p)Determines mineral composition and texture
Climate (cl)Temperature & rainfall control weathering rate and organic decomposition
Organisms/Biotic factor (o)Vegetation and microbes add organic matter (humus), influence structure
Relief/Topography (r)Slope affects drainage, erosion, and soil depth
Time (t)Soil profile (horizons) develops and matures over long periods

Rendering diagram…

B. Biomes of the Earth — Characteristics

BiomeClimateVegetationExample Regions
Tropical RainforestHot, high rainfall year-roundDense, multi-layered evergreen forest, high biodiversityAmazon, Congo Basin
Tropical SavannaWarm, wet-dry seasonsGrasslands with scattered treesAfrican Savanna
DesertHot/cold, very low rainfallSparse xerophytic vegetation (cacti, scrub)Sahara, Thar
Temperate GrasslandModerate rainfall, seasonalGrasses, few treesSteppes, Prairies
Temperate Deciduous ForestWarm summers, cold wintersBroad-leaf trees shedding leaves seasonallyEurope, Eastern USA
Taiga (Boreal Forest)Cold, long wintersConiferous evergreen forestsSiberia, Canada
TundraVery cold, short summerMosses, lichens, low shrubs (permafrost)Arctic regions
Aquatic (Marine/Freshwater)VariesAlgae, aquatic plantsOceans, lakes, rivers

C. Vegetation Distribution & Its Variation ("large variations" argument)

Global vegetation distribution varies enormously because it responds to multiple interacting controls, not a single factor:

Rendering diagram…

Validation points:

  • Latitudinal variation: dense equatorial rainforest → savanna → desert → temperate forest → taiga → tundra, moving from equator to poles.
  • Altitudinal variation: vegetation belts change with elevation on a single mountain (tropical at base → alpine/tundra-like at summit) — mirrors latitudinal zonation ("altitude mimics latitude").
  • Rainfall gradient: rainforest (>2000mm) vs. grassland (250-750mm) vs. desert (<250mm).
  • Soil & drainage: mangroves in saline coastal soils vs. conifers in acidic, well-drained mountain soils.
  • Human impact: deforestation, agriculture, and urbanization alter natural vegetation cover, adding further variation.

This multi-causal, multi-scalar control validates that vegetation distribution shows very large global variation.


📚 Full Previous-Year Question Bank (Unit-wise, All 3 Papers Combined)

Unit I Questions

  • Define Physical Geography. Discuss the nature and scope of Physical Geography. (Paper 5072/2292101101, Q1)
  • Explain different components of earth system. (Paper 5072/2292101101, Q2)
  • What are the different components of Earth System? Describe them in detail. (Paper 540, Q1)
  • Write a note on: Scope of Physical Geography. (Paper 540, Q9-a)

Unit II Questions

  • What is insolation? Explain different factors affecting the temperature over the globe by giving examples. (Paper 5072/2292101101, Q3)
  • Describe the composition and structure of the atmosphere. (Paper 5072/2292101101, Q4)
  • What is insolation? Explain the factors affecting insolation and describe the heat budget of the earth. (Paper 540, Q2)
  • Explain the pressure belts and global wind system with suitable diagrams. (Paper 540, Q3)
  • Write a note on: Structure of Atmosphere. (Paper 540, Q9-c)

Unit III Questions

  • Explain the internal structure of the Earth with reference to seismic evidences. (Paper 5072/2292101101, Q5)
  • Define isostasy. Elaborate the isostatic adjustment maintained by the earth. (Paper 5072/2292101101, Q6)
  • What is folding? Discuss its various types. (Paper 5072/2292101101, Q7)
  • Give a brief account of the internal structure of the earth. (Paper 540, Q4)
  • What is isostasy? Explain the views of Airy on isostasy. (Paper 540, Q5)

Unit IV Questions

  • What are tides? Explain its types. (Paper 5072/2292101101, Q8)
  • What are ocean currents? Describe the factors affecting ocean currents. (Paper 540, Q6)
  • Write a note on: Types of Tides. (Paper 540, Q9-b)

Unit V Questions

  • "The vegetation distribution over the globe has very large variations." Validate the statement. (Paper 5072/2292101101, Q9)
  • Discuss the factors affecting soil formation. (Paper 540, Q7)
  • Describe the characteristics of different biomes of the earth. (Paper 540, Q8)

⚡ Rapid Revision Sheet (Exam-Night Cheat Cards)

UnitMust-Know DiagramMust-Know Definitions
IEarth system sphere interlinkagePhysical Geography, Earth System
IILayered atmosphere + 3-cell wind circulationInsolation, Heat Budget, Trade winds/Westerlies
IIIEarth's interior layers + Airy vs PrattIsostasy, Folding (anticline/syncline), Fault types
IVHydrological cycle loopTides (spring/neap), Ocean currents (warm/cold)
VLatitude → Biome gradientJenny's soil equation, Biome, Vegetation controls

One-Line Formula/Concept Recall

  • Isostasy: crust floats on mantle in gravitational equilibrium.
  • Airy: same density, different thickness (roots).
  • Pratt: same depth, different density.
  • Insolation factors (mnemonic — "LADLO"): Latitude, Atmospheric transparency, Duration of day, Land-sea distribution, Ocean currents.
  • Soil formation (Jenny): S = f(climate, organisms, relief, parent material, time).
  • Tide types: Spring = alignment = max range; Neap = right angle = min range.
  • Seismic shadow zone (103°–142°): proves liquid outer core.

Compiled as an exam-ready, unit-wise companion covering 100% of syllabus topics and every question appearing across all three uploaded question papers (Sr. No. 5072, and 540 — both Unique Paper Code 2292101101).