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Earthquakes


🧾 1. Definition and Causes

  • An earthquake is the shaking of the Earth caused by the release of energy in the Earth's crust.

  • The energy release generates seismic waves that travel in all directions.

  • Most earthquakes occur along faults due to tectonic movements.

🔄 Causes of Earthquakes

CauseDetails
Tectonic movementSudden slip along faults due to crustal stress.
Volcanic activityDuring violent eruptions, e.g., in volcanic regions (volcanic earthquakes).
Collapse of underground minesCalled collapse earthquakes.
Explosion earthquakesResult from nuclear or chemical explosions.
Reservoir-induced earthquakesLarge man-made reservoirs create pressure changes in Earth's crust.
Folding, faultingMovement or displacement in rock strata.

📍 2. Focus and Epicentre

TermDefinition
Focus / HypocentrePoint inside the Earth where energy is released (origin of quake). Usually ≤60 km deep.
EpicentrePoint on Earth's surface directly above the focus. Most severe shaking occurs here.
  • Earthquakes occur in the lithosphere (up to 200 km deep).

  • Seismic waves radiate outward from the focus in all directions.


🌊 3. Earthquake Waves

A. Types of Seismic Waves

Wave TypeSub-TypeDescription
Body WavesP-wavesPrimary waves, fastest, travel through solids, liquids, gases. Vibration is parallel to wave direction.
S-wavesSecondary waves, slower, travel only through solids. Vibration is perpendicular to wave direction.
Surface Waves-Slowest but most destructive. Cause horizontal and vertical ground motion.

📊 4. Seismograph and Wave Recording

  • A seismograph is an instrument that records earthquake waves.

  • It displays three distinct wave sections: P, S, and Surface waves.

  • Seismographs help determine the epicentre and magnitude of an earthquake.


🚫 5. Shadow Zones

ZoneWave Behavior
Within 105°Both P and S waves detected.
Between 105°–145°No P or S waves recorded (shadow zone).
Beyond 145°Only P-waves recorded; S-waves blocked (they can’t pass through liquids).
  • Shadow zones helped confirm the liquid nature of the Earth’s outer core.

📏 6. Measuring Earthquakes

ScaleMeasuresRangeType
Richter ScaleEnergy released (magnitude)0 to 10Logarithmic
Mercalli ScaleDamage and effect (intensity)I to XIISubjective, visual

⚠️ 7. Effects of Earthquakes

A. On Ground and Landscape

  • Ground shaking and displacement

  • Landslides, mudslides, avalanches

  • Soil liquefaction

  • River course changes and reservoir formation

B. On Man-Made Structures

  • Collapse of buildings, bridges, roads

  • Damage to dams, pipelines, railways

  • Fire outbreaks due to gas leaks

  • Disruption of electricity, communication, and transport

C. On Water Bodies

  • Tsunamis: Triggered if epicentre is under ocean floor (Richter 5+).

  • Cause sea-floor displacement and powerful waves.

  • Can travel thousands of km at high speed.

D. Socio-Environmental Impact

  • Homelessness, fear, trauma

  • Epidemics due to poor sanitation

  • Destruction of infrastructure and socio-economic losses


🌐 8. Global Distribution of Earthquakes

🔥 Earthquake Belts

RegionCharacteristics
Circum-Pacific Belt“Ring of Fire”; around the Pacific Ocean; many volcanoes and deep quakes.
Alpine-Himalayan BeltIncludes Himalayas and Alps; high seismicity due to plate collisions.
Mid-Oceanic RidgesShallow earthquakes; divergent boundaries in oceans like Atlantic and Indian.

🇮🇳 9. Earthquakes in India

📍 Seismic Zones of India (Zone V to Zone II)

ZoneRisk LevelRegions
Zone VVery High RiskNorth-east India, Northern Bihar (Darbhanga, Araria), Uttarakhand, Kashmir Valley, Kutch
Zone IVHigh RiskRemaining J&K, Himachal Pradesh, Delhi, Northern UP, Eastern Haryana, Punjab
Zone IIIModerate RiskParts of Gujarat, Maharashtra, Goa, Kerala, West Bengal
Zone II & ILow/Very Low RiskParts of Central and Southern India (Peninsular region)
  • Himalayan arc and Northeast India are most active due to Indian Plate movement.

🛠️ 10. Earthquake Hazard Mitigation

Preparedness Measures

StrategyDetails
Seismological CentresFor monitoring and early warning.
Vulnerability MappingIdentify and educate at-risk zones.
Building Design ModificationsEncourage earthquake-resistant structures.
Construction RegulationDiscourage high-rise, heavy construction in high-risk areas.
Lightweight MaterialsUse in buildings to reduce damage risk.
Public Awareness & DrillsCommunity education for evacuation and safety.

PhenomenonLink to Earthquakes
TsunamiUndersea earthquakes displace ocean floor → water displacement → massive sea waves.
LandslidesTriggered by ground shaking in hilly terrain (Himalayas, Western Ghats).
Volcanic ActivityOften linked, especially in tectonic zones like the Pacific Ring of Fire.