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General Studies 3% exam weight

Topic 1

Part of the BPSC study roadmap. General Studies topic geogra-001 of General Studies.

Physical Geography: Geomorphology

🟢 Lite — Quick Review (1h–1d)

Rapid summary for last-minute revision before your exam.

Geomorphology — Key Facts for BPSC Examination

Endogenic Forces (Internal):

ForceEffectProcess
Tectonic movementsMountain buildingFolding, faulting
Volcanic activityNew landformsLava flows, volcanic cones
Seismic activityEarthquakesFault rupture

Exogenic Forces (External):

ForceEffectProcess
WeatheringRock breakdownPhysical, chemical, biological
ErosionMaterial removalWater, wind, ice
TransportationMaterial movementRivers, glaciers, wind
DepositionMaterial accumulationDeltas, alluvial fans

BPSC Tip: The distinction between endogenic (building) and exogenic (wearing down) forces is frequently asked — remember that endogenic forces are generally stronger!


🟡 Standard — Regular Study (2d–2mo)

Standard content for students with a few days to months.

Geomorphology — BPSC Study Guide

Earth’s Internal Structure

Layers by Composition:

LayerDepthComposition
Crust0-35 kmSilicates (SIAL/SIMA)
Mantle35-2900 kmIron, magnesium silicates
Outer Core2900-5150 kmLiquid iron, nickel
Inner Core5150-6371 kmSolid iron, nickel

Layers by Physical Properties:

LayerProperties
LithosphereRigid, broken into plates
AsthenospherePlastic, convective flow
MesosphereStronger than asthenosphere
Outer coreLiquid, generates magnetic field

Mohorovičić Discontinuity (Moho): Boundary between crust and mantle

Plate Tectonics

Major Plates:

PlateTypeMajor Features
EurasianContinentalEurope, Asia, Indian subcontinent
Indo-AustralianMixedIndia, Australia, surrounding ocean
PacificOceanicPacific Ocean floor
AfricanMixedAfrica, Arabian Peninsula
North AmericanContinentalNorth America, Greenland
South AmericanMixedSouth America
AntarcticMixedAntarctica

Plate Boundaries:

Boundary TypeFeaturesExample
DivergentMid-ocean ridges, seafloor spreading, volcanismMid-Atlantic Ridge
ConvergentSubduction zones, deep trenches, volcanic arcsHimalayas, Andes
TransformFault lines, earthquake zonesSan Andreas Fault
CollisionMountain building, no subductionHimalayas

Evidence for Plate Tectonics:

  1. Continental drift (Alfred Wegener, 1912)
  2. Seafloor spreading (Harry Hess, 1960s)
  3. Paleomagnetic stripes
  4. Fossil distribution patterns
  5. Climate zone anomalies
  6. Earthquake and volcano distribution

Landforms Created by Geomorphic Processes

Fluvial (River) Landforms:

StageLandforms
YouthV-shaped valleys, waterfalls, rapids
MaturityMeanders, oxbow lakes, natural levees
Old ageFloodplains, deltas, point bars

Erosional vs Depositional Fluvial Features:

TypeErosionalDepositional
YouthGorges, canyons, waterfallsAlluvial fans (mountain fronts)
MaturityMeanders, oxbow lakesPoint bars, natural levees
Old ageCut-off featuresDeltas, distributaries

Glacial Landforms:

TypeFeatures
ErosionalCirques, U-shaped valleys, aretes, hanging valleys
DepositionalMoraines (lateral, medial, terminal), drumlins, eskers

Wind (Aeolian) Landforms:

TypeFeatures
ErosionalMushroom rocks, ventifacts, yardangs
DepositionalSand dunes (barchan, longitudinal, transverse), loess

Coastal Landforms:

TypeFeatures
ErosionalSea cliffs, wave-cut platforms, sea caves, stacks
DepositionalBeaches, spits, bars, tombolos

Weathering Types:

TypeProcessExample
Physical/Frost wedgingWater freezes, expands, splits rockMountain regions
Thermal expansionTemperature changes cause expansion/contractionDeserts
Chemical/HydrolysisWater + CO₂ forms carbonic acidFeldspar → clay
Chemical/OxidationIron combines with oxygenRust-colored rocks
BiologicalPlant roots, acids from organismsTree roots splitting rocks

BPSC PYQ: “Explain the theory of plate tectonics with suitable examples” Answer: Earth’s lithosphere is divided into plates that move due to convection currents in the asthenosphere. At divergent boundaries, seafloor spreading occurs; at convergent boundaries, subduction or collision creates mountains and trenches; at transform boundaries, plates slide past each other causing earthquakes.


🔴 Extended — Deep Study (3mo+)

Comprehensive coverage for students on a longer study timeline.

Geomorphology — Comprehensive BPSC Notes

Mountain Building (Orogenesis)

Fold Mountains:

CharacteristicFeatures
FormationCompression, horizontal crustal shortening
StructureAnticlines (upward folds), synclines (downward folds)
ExamplesHimalayas, Alps, Andes, Rockies

Himalayan Orogeny:

  • Collision between Indian and Eurasian plates (50 million years ago)
  • Still rising ~1 cm per year
  • Contains: Mount Everest (8849m), K2, Kangchenjunga
  • Features: Nappe structures, thrust faults, deep gorges

Fault-Block Mountains:

  • Due to tension or compression on fractured crust
  • Uplifted blocks (horsts) and sunken blocks (grabens)
  • Examples: Sierra Nevada (USA), Vosges (France), Black Forest (Germany)

Earthquakes and Volcanoes

Earthquake Properties:

PropertyDescriptionMeasurement
FocusOrigin point undergroundDepth categories: shallow (<70km), intermediate (70-300km), deep (>300km)
EpicenterPoint on surface directly above focusLocated by triangulation
Seismic wavesP-waves, S-waves, Surface wavesTravel at different speeds

Richter Scale:

  • Logarithmic: M = log₁₀(A/A₀)
  • Each unit increase = 10× ground motion, ~31× energy
  • Modified Mercalli Intensity measures shaking effects

Volcanoes:

TypeShapeEruptionExamples
ShieldFlat, broadGentle, fluid lavaMauna Loa (Hawaii)
Composite/StratovolcanoSteep, conicalExplosive, alternating lava/ashMount Fuji, Mount St. Helens
Cinder coneSmall, steepSingle vent, pyroclasticParicutin (Mexico)
CalderaLarge basinCollapse after massive eruptionCrater Lake (Oregon)

Distribution of Volcanoes:

  • Pacific Ring of Fire (75% of world’s volcanoes)
  • Mediterranean-Himalayan belt
  • Mid-Atlantic ridge

Drainage Systems and River Basins

Drainage Patterns:

PatternCharacteristicsExample
DendriticTree-like, uniform rockMost rivers
TrellisRectangular, folded rocksAppalachian rivers
RadialOutward from central high pointMount Vesuvius rivers
CentripetalInward to central basinInland drainage basins
DerangedRandom, youthful topographyGlaciated areas

River Basin Morphology:

ZoneFeatures
Upper courseSteep gradient, vertical erosion, V-shaped valleys
Middle courseMixed erosion/deposition, meandering begins
Lower courseGentle gradient, deposition dominates, floodplains

Delta Formation:

  • Conditions: Strong deposition, weak tides/currents, subsiding coast
  • Types: Arcuate (Nile), Bird’s foot (Mississippi), Estuarine (Seine)

Applications and Human Geography

Geomorphology and Human Activity:

IssueConsideration
SettlementsAvoid earthquake zones, volcanic hazard areas, floodplains
AgricultureAlluvial soils, terracing for slope cultivation
TransportationRoad routing around steep terrain
MiningResource extraction from geological formations

Bihar-specific Geomorphology:

  • Part of the Indo-Gangetic Plain
  • Alluvial deposits from Himalayan rivers
  • Flood-prone due to multiple river systems (Ganga, Kosi, Gandak)
  • Seismic vulnerability (Zone III-IV)

Important Concepts for BPSC:

  1. Isostasy: Equilibrium of crust floating on mantle (post-glacial rebound)
  2. Wilson Cycle: Opening and closing of ocean basins
  3. Epeirogenic movements: Continental uplift/subsidence without deformation

BPSC Strategy: Map-based questions frequently combine geomorphology with Indian geography. Practice identifying mountain ranges, plate boundaries, and major river systems on blank maps.

Common BPSC Questions:

  1. “Discuss the theory of plate tectonics and its supporting evidence” (10 marks)
  2. “Explain the landforms produced by river erosion and deposition” (10 marks)
  3. “Describe the distribution of earthquakes and volcanoes worldwide” (8 marks)
  4. “Discuss the formation of the Himalayas and its significance” (15 marks)

Map Work: Be able to locate and describe: Himalayas, Indo-Gangetic Plain, Thar Desert, Western Ghats, Eastern Ghats, Deccan Plateau, major rivers (Ganga, Brahmaputra, Indus, Mahanadi, Godavari, Krishna, Kaveri)


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