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Earthquake engineering

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Tarun kumar
Tarun kumar

An earthquake is caused by rapid shaking of the ground due to movement of tectonic plates or volcanic activity underground. Earthquakes are measured using seismometers which record seismic waves on instruments called seismographs. The location and magnitude of earthquakes are determined from these recordings. The Richter scale is used to describe earthquake magnitude, with greater magnitudes indicating stronger shaking. Major effects of earthquakes include damage to buildings and structures, landslides, tsunamis, and changes to the land surface like cracks and fissures. The most active seismic belts are around the Pacific Ocean, along the Alps and Himalayas, and along mid-ocean ridges.

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EARTHQUAKE
Definition: • An Earthquake is a sudden and rapid shaking of the ground due to passage of vibrations beneath caused by transient disturbance of elastic or gravitational equilibrium of rocks. • The scientific study of earthquakes is called Seismology. • Earthquakes are measured using observations from seismometers. • Seismic waves are recorded on instruments called seismographs. • The time, locations, and magnitude of an earthquake can be determined from the data recorded by seismograph stations.
Earthquake engineering
RICHTER MAGNITUDE SCALE: • The Richter magnitude scale was developed in 1935 by Charles F. Richter. • Earthquakes with magnitude of about 2.0 or less are usually called micro earthquakes; are generally recorded only on local seismographs. • Events with magnitudes of about 4.5 or greater, are strong enough to be recorded by sensitive seismographs all over the world. • Great earthquakes have magnitudes of 8.0 or higher. • On the average, one earthquake of such size occurs somewhere in the world each year.
Earthquake engineering
CAUSES : Natural Causes of Earthquake: • Tectonic Movement • Volcanic Activity • Pressure of gases in the interior • Landslides and avalanches • Faulting and folding in the rock beds are responsible for causing minor earthquakes.
Man-made Earthquakes: • The impounding of large quantities of water behind dams disturbs the crustal balance. • The shock waves through rocks set up by the underground testing of Atom bombs or Hydrogen bombs may be severe to cause earthquake.
EFFECTS: Destructive Effects: • Earthquake causes dismantling of buildings, bridge and other structures at or near epicenter. • Rails are folded, underground wires broken. • Earthquakes originate sea waves called Tsunamis. • Earthquakes result in the formation of cracks and fissures on the ground formation. • The earthquakes cause landslides. • Landslide due to earthquake may block valleys to form lakes.
SEISMIC BELT: • Narrow geographic zone on the Earth's surface along which most earthquake activity occurs. • The outermost layer of the Earth (lithosphere) is made up of several large tectonic plates. There are three main seismic belts in the world ： 1. Circum-Pacific seismic belt 2. Alpine-Himalayan seismic belt 3. Ridge seismic belt
Earthquake engineering

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Earthquake engineering

  • 2. Definition: • An Earthquake is a sudden and rapid shaking of the ground due to passage of vibrations beneath caused by transient disturbance of elastic or gravitational equilibrium of rocks. • The scientific study of earthquakes is called Seismology. • Earthquakes are measured using observations from seismometers. • Seismic waves are recorded on instruments called seismographs. • The time, locations, and magnitude of an earthquake can be determined from the data recorded by seismograph stations.
  • 4. RICHTER MAGNITUDE SCALE: • The Richter magnitude scale was developed in 1935 by Charles F. Richter. • Earthquakes with magnitude of about 2.0 or less are usually called micro earthquakes; are generally recorded only on local seismographs. • Events with magnitudes of about 4.5 or greater, are strong enough to be recorded by sensitive seismographs all over the world. • Great earthquakes have magnitudes of 8.0 or higher. • On the average, one earthquake of such size occurs somewhere in the world each year.
  • 6. CAUSES : Natural Causes of Earthquake: • Tectonic Movement • Volcanic Activity • Pressure of gases in the interior • Landslides and avalanches • Faulting and folding in the rock beds are responsible for causing minor earthquakes.
  • 7. Man-made Earthquakes: • The impounding of large quantities of water behind dams disturbs the crustal balance. • The shock waves through rocks set up by the underground testing of Atom bombs or Hydrogen bombs may be severe to cause earthquake.
  • 8. EFFECTS: Destructive Effects: • Earthquake causes dismantling of buildings, bridge and other structures at or near epicenter. • Rails are folded, underground wires broken. • Earthquakes originate sea waves called Tsunamis. • Earthquakes result in the formation of cracks and fissures on the ground formation. • The earthquakes cause landslides. • Landslide due to earthquake may block valleys to form lakes.
  • 9. SEISMIC BELT: • Narrow geographic zone on the Earth's surface along which most earthquake activity occurs. • The outermost layer of the Earth (lithosphere) is made up of several large tectonic plates. There are three main seismic belts in the world ： 1. Circum-Pacific seismic belt 2. Alpine-Himalayan seismic belt 3. Ridge seismic belt