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
| Detail | Value |
|---|---|
| Duration | 3 Hours |
| Max Marks | 90 |
| Questions to Attempt | Any 5 out of 9 |
| Marks per Question | Equal (18 each) |
| Medium | English or Hindi (not mixed) |
| Map Stencil | Allowed |
📊 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
| Unit | Topic | Hours | PYQ Hits (out of 3 papers analysed) |
|---|---|---|---|
| I | Physical Geography, Earth as a System | 4 | 3/3 papers |
| II | Atmosphere, Insolation, Pressure & Winds | 16 | 3/3 papers |
| III | Lithosphere, Isostasy, Folding/Faulting | 16 | 3/3 papers |
| IV | Hydrosphere, Currents & Tides | 12 | 3/3 papers |
| V | Biosphere, Soil & Vegetation | 12 | 3/3 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
- Unit I — Physical Geography & Earth System
- Unit II — Atmosphere
- Unit III — Lithosphere
- Unit IV — Hydrosphere
- Unit V — Biosphere
- Full Previous-Year Question Bank
- 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…
| Branch | Deals With |
|---|---|
| Geomorphology | Landforms, relief, internal/external earth processes |
| Climatology | Atmosphere, weather, climate |
| Oceanography | Oceans, currents, tides, marine features |
| Pedology | Soil formation, classification, distribution |
| Biogeography | Distribution 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").
Rendering diagram…
5. Components of the Earth System
| Sphere | Composition | Key Role |
|---|---|---|
| Atmosphere | Gaseous envelope (N₂, O₂, CO₂, water vapour) | Weather, climate, protection from radiation |
| Lithosphere | Solid crust & upper mantle (rocks, soil) | Landforms, relief, resource base |
| Hydrosphere | All water — oceans, rivers, lakes, glaciers, groundwater | Water cycle, climate moderation |
| Biosphere | All living organisms | Ecological balance, biogeochemical cycles |
| (Cryosphere) | Frozen water — ice caps, glaciers | Often 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 | % Volume | Significance |
|---|---|---|
| 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) | Trace | Ozone absorbs UV; water vapour drives weather |
Structure (vertical layers):
Rendering diagram…
| Layer | Height | Key Feature |
|---|---|---|
| Troposphere | 0–12 km (up to 18 km at equator) | All weather phenomena; temp decreases with height (Normal Lapse Rate 6.5°C/km) |
| Stratosphere | 12–50 km | Contains ozone layer; temperature increases with height |
| Mesosphere | 50–80 km | Coldest part of atmosphere (~ -100°C); meteors burn up |
| Thermosphere | 80–700 km | Temperature rises sharply; ionosphere lies here (radio wave reflection) |
| Exosphere | >700 km | Outermost, gradually merges into space |
B. Insolation (Incoming Solar Radiation)
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…
| Factor | Effect |
|---|---|
| Latitude (angle of incidence) | Vertical rays at equator concentrate energy; oblique rays at poles spread it over larger area → less insolation |
| Duration of daylight | Longer days = more total insolation (summer poles) |
| Atmospheric transparency | Clouds/dust/water vapour reflect & absorb radiation, reducing insolation |
| Land vs Sea | Land heats/cools faster than water (specific heat difference) → continental vs maritime climates |
| Altitude | Higher altitude, thinner air, faster heat loss, lower temperature |
| Ocean currents | Warm currents raise coastal temps (e.g., Gulf Stream); cold currents lower them (e.g., Labrador) |
| Earth-Sun distance | Perihelion (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):
| Belt | Latitude | Type | Cause |
|---|---|---|---|
| Equatorial Low | 0° | Low | Intense heating → rising air |
| Sub-Tropical High | 30°N/S | High | Descending air (Hadley cell) |
| Sub-Polar Low | 60°N/S | Low | Rising air, meeting of cold/warm winds |
| Polar High | 90°N/S | High | Intense cold → sinking air |
Rendering diagram…
Global Wind System (surface winds):
| Wind | Blows From → To | Latitude |
|---|---|---|
| Trade Winds | Sub-tropical high → Equatorial low | 30° → 0° (NE in N. Hemisphere, SE in S. Hemisphere) |
| Westerlies | Sub-tropical high → Sub-polar low | 30° → 60° |
| Polar Easterlies | Polar high → Sub-polar low | 90° → 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.
Rendering diagram…
| Layer | Depth | State | Evidence |
|---|---|---|---|
| Crust | 0–35 km (continental), ~5-10 km (oceanic) | Solid | P-waves travel at moderate speed |
| Mantle | 35–2900 km | Solid/plastic (asthenosphere is semi-molten) | Sudden velocity increase = Mohorovičić Discontinuity (Moho) |
| Outer Core | 2900–5150 km | Liquid | S-waves cannot pass through liquid → S-wave shadow zone proves liquid outer core |
| Inner Core | 5150–6371 km | Solid | P-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
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:
| Theory | Proponent | Concept |
|---|---|---|
| Airy's Hypothesis | George Airy | Crust has uniform density but variable thickness; mountains have deep "roots" that sink into denser mantle, like icebergs — bigger mountain = deeper root |
| Pratt's Hypothesis | John Pratt | Crust 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)
Rendering diagram…
Folding: Bending of rock strata due to compressional (horizontal) forces, producing wave-like undulations.
| Part | Description |
|---|---|
| Anticline | Upfold, arch-shaped |
| Syncline | Downfold, trough-shaped |
| Limb | Sides of the fold |
| Axis | Line of maximum curvature |
Types of Folds:
| Type | Characteristic |
|---|---|
| Symmetrical Fold | Limbs dip equally on both sides |
| Asymmetrical Fold | Limbs dip unequally |
| Overturned Fold | One limb pushed beyond vertical |
| Recumbent Fold | Fold lying almost horizontal |
| Isoclinal Fold | Limbs parallel, dip in same direction |
| Monocline | Local steepening in otherwise flat strata |
| Fan Fold | Both 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 Fault | Cause | Feature |
|---|---|---|
| Normal Fault | Tension | Hanging wall moves down relative to footwall |
| Reverse Fault | Compression | Hanging wall moves up |
| Strike-slip (Transform) Fault | Shearing | Horizontal sliding (e.g., San Andreas Fault) |
| Graben (Rift Valley) | Tension | Block sinks between two normal faults |
| Horst | Tension | Block 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.
Rendering diagram…
Key processes: Evaporation → Condensation → Precipitation → Infiltration → Runoff → back to Ocean. Driven by solar energy and gravity; keeps freshwater renewable.
B. Ocean Currents
Large-scale, persistent horizontal movements of ocean water in a fairly definite direction.
Factors Affecting Ocean Currents:
| Factor | Effect |
|---|---|
| Prevailing winds | Primary driving force (e.g., trade winds drive equatorial currents) |
| Coriolis force | Deflects currents (right in N. Hemisphere, left in S. Hemisphere) |
| Water temperature/density differences | Drives thermohaline (deep) circulation |
| Salinity differences | Denser saline water sinks, creating circulation |
| Continental land masses | Deflect and shape current paths (e.g., coastlines) |
| Earth's rotation | Contributes 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
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:
| Basis | Types |
|---|---|
| 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-Earth | Spring Tides (Sun, Moon, Earth aligned — Full/New Moon — highest tidal range); Neap Tides (Sun-Moon at right angles — Half Moon — lowest tidal range) |
| By Periodicity | Diurnal, Semi-diurnal, Mixed/Semi-diurnal |
Rendering diagram…
🟪 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)
| Factor | Role |
|---|---|
| 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
| Biome | Climate | Vegetation | Example Regions |
|---|---|---|---|
| Tropical Rainforest | Hot, high rainfall year-round | Dense, multi-layered evergreen forest, high biodiversity | Amazon, Congo Basin |
| Tropical Savanna | Warm, wet-dry seasons | Grasslands with scattered trees | African Savanna |
| Desert | Hot/cold, very low rainfall | Sparse xerophytic vegetation (cacti, scrub) | Sahara, Thar |
| Temperate Grassland | Moderate rainfall, seasonal | Grasses, few trees | Steppes, Prairies |
| Temperate Deciduous Forest | Warm summers, cold winters | Broad-leaf trees shedding leaves seasonally | Europe, Eastern USA |
| Taiga (Boreal Forest) | Cold, long winters | Coniferous evergreen forests | Siberia, Canada |
| Tundra | Very cold, short summer | Mosses, lichens, low shrubs (permafrost) | Arctic regions |
| Aquatic (Marine/Freshwater) | Varies | Algae, aquatic plants | Oceans, 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)
| Unit | Must-Know Diagram | Must-Know Definitions |
|---|---|---|
| I | Earth system sphere interlinkage | Physical Geography, Earth System |
| II | Layered atmosphere + 3-cell wind circulation | Insolation, Heat Budget, Trade winds/Westerlies |
| III | Earth's interior layers + Airy vs Pratt | Isostasy, Folding (anticline/syncline), Fault types |
| IV | Hydrological cycle loop | Tides (spring/neap), Ocean currents (warm/cold) |
| V | Latitude → Biome gradient | Jenny'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).
