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Earthquake
Terminologies
• Earthquake – it is a motion of ground surface
ranging from a faint tremor to a wild motion
capable of shaking buildings apart and causing
gaping fissures to open in the ground.
• Seismic waves – waves generated by the
earthquake
• Focus – place of origin of the earthquake
• Epicentre – place on the surface of the earth,
perpendicular to focus
• Richter scale is used to measure the intensity of
earthquake
Cause of earthquake
• Due to disequilibrium caused by different
factors like
• Vulcanicity, folding, faulting, gaseous
expansion &contraction inside the earth etc
• Plate movements
• Hydrostatic pressure of manmade
waterbodies like dams, lakes etc
• Weaker zones on earth are more prone to
seismic activity
Classification of earthquakes
• On the basis of causative factors
1. NATURAL- caused by natural processes like
endogenetic forces.
Volcanic earthquake – caused by volcanic
eruptions- fissure or explosive. And this is
dependent on intensity &magnitude of the
earthquake
Tectonic earthquake – caused by dislocation
of rockblocks during faulting
• Isostatic earthquake – due to sudden
disturbances in the isostatic balance at regional
level
• Plutonic earthquake – focus at greater depths
ranging from 240 km to 670 km
2.ARTIFICIAL
Man induced – caused by human activities like
pumping of water &mineral oil from underground
Deep ground mining, nuclear explosion, storage
of he volume of water in reservoirs etc
Distribution of earthquakes
• Mostly occur in:
• Zones of young folded mountains
• Zones of faulting and fracturing
• At the junction of continental and oceanic margins
• Zones of active volcanoes
• Along different plate boundaries
• Major regions are:
• Circum-Pacific belt surrounding the pacific ocean
• Mid continental belt- Alpine – Himalayan chain,Northern
Africa &epicentre of East African fault zones
• Mid Atlantic belt
Seismic waves and tremors
• Primary waves- P waves, longitudinal waves are
analogous to sound waves. faster peed in solid &
in liquid at slower speed
• Secondary waves – transverse waves, S waves are
analogous to light waves. Cannot pass through
liquid matter
• Surface waves – long period waves, L waves.
Affects only the surface of the earth & covers
longest distances. Speed is lower than S&P waves
but more destructive & violent.
Seismic waves
seismograph Path of seismic waves

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Earthquake

  • 2. Terminologies • Earthquake – it is a motion of ground surface ranging from a faint tremor to a wild motion capable of shaking buildings apart and causing gaping fissures to open in the ground. • Seismic waves – waves generated by the earthquake • Focus – place of origin of the earthquake • Epicentre – place on the surface of the earth, perpendicular to focus • Richter scale is used to measure the intensity of earthquake
  • 3. Cause of earthquake • Due to disequilibrium caused by different factors like • Vulcanicity, folding, faulting, gaseous expansion &contraction inside the earth etc • Plate movements • Hydrostatic pressure of manmade waterbodies like dams, lakes etc • Weaker zones on earth are more prone to seismic activity
  • 4. Classification of earthquakes • On the basis of causative factors 1. NATURAL- caused by natural processes like endogenetic forces. Volcanic earthquake – caused by volcanic eruptions- fissure or explosive. And this is dependent on intensity &magnitude of the earthquake Tectonic earthquake – caused by dislocation of rockblocks during faulting
  • 5. • Isostatic earthquake – due to sudden disturbances in the isostatic balance at regional level • Plutonic earthquake – focus at greater depths ranging from 240 km to 670 km 2.ARTIFICIAL Man induced – caused by human activities like pumping of water &mineral oil from underground Deep ground mining, nuclear explosion, storage of he volume of water in reservoirs etc
  • 6. Distribution of earthquakes • Mostly occur in: • Zones of young folded mountains • Zones of faulting and fracturing • At the junction of continental and oceanic margins • Zones of active volcanoes • Along different plate boundaries • Major regions are: • Circum-Pacific belt surrounding the pacific ocean • Mid continental belt- Alpine – Himalayan chain,Northern Africa &epicentre of East African fault zones • Mid Atlantic belt
  • 7.
  • 8. Seismic waves and tremors • Primary waves- P waves, longitudinal waves are analogous to sound waves. faster peed in solid & in liquid at slower speed • Secondary waves – transverse waves, S waves are analogous to light waves. Cannot pass through liquid matter • Surface waves – long period waves, L waves. Affects only the surface of the earth & covers longest distances. Speed is lower than S&P waves but more destructive & violent.