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•An earthquake (also known as a quake,
tremor or temblor) is the result of a
sudden release of energy in the Earth's
crust that creates seismic waves.
•The seismicity, seismism or seismic
activity of an area refers to the frequency,
type and size of earthquakes experienced
over a period of time.
• Magnitude 3 or lower earthquakes are
mostly almost imperceptible or weak and
magnitude 7 and over potentially cause
serious damage over larger areas, depending
on their depth.
• The largest earthquakes in historic times
have been of magnitude slightly over 9,
although there is no limit to the possible
magnitude.
•The most recent large earthquake of magnitude
9.0 or larger was a 9.0 magnitude earthquake in
Japan in 2011 (as of October 2012), and it was the
largest Japanese earthquake since records began.
• Intensity of shaking is measured on the modified
Mercalli scale.
•The shallower an earthquake, the more damage
to structures it causes, all else being equal.
• In its most general sense, the word
earthquake is used to describe any seismic
event — whether natural or caused by humans
— that generates seismic waves.
• Earthquakes are caused mostly by rupture
of geological faults, but also by other events
such as volcanic activity, landslides, mine
blasts, and nuclear tests.
• An earthquake's point of initial rupture is
called its focus or hypocenter. The epicenter is
the point at ground level directly above the
hypocenter.
Earthquakes are caused by tectonic movements in
the Earth's crust.
The main cause is that when tectonic plates collide,
one rides over the other, causing progeny
(mountain building), earthquakes and volcanoes.
Causes of earthquakes
Earthquakes are caused by
tectonic movements in the Earth's
crust.
The main cause is that when
tectonic plates collide, one rides
over the other, causing progeny
(mountain building), earthquakes
and volcanoes.
• The boundaries between moving plates form
the largest fault surfaces on Earth.
• When they stick, relative motion between
the plates leads to increasing stress.
• This continues until the stress rises and
breaks, suddenly allowing sliding over the
locked portion of the fault, releasing the stored
energy.
•Earthquake clusters
•Most earthquakes form part of a
sequence, related to each other in
terms of location and time.
•Most earthquake clusters consist of
small tremors which cause little to no
damage, but there is a theory that
earthquakes can recur in a regular
pattern.
Earthquake fault types
There are three main types of fault that
may cause an earthquake: normal, reverse
(thrust) and strike-slip.
Normal faults occur mainly in areas
where the crust is being extended. Reverse
faults occur in areas where the crust is being
shortened.
Strike-slip faults are steep structures
where the two sides of the fault slip
horizontally past each other.
Aftershocks
An aftershock is an earthquake that occurs
after a previous earthquake, the main shock.
An aftershock is in the same region of the
main shock but always of a smaller
magnitude.
Aftershocks are formed as the crust adjusts to
the effects of the main shock.
Date January 26, 2001
Magnitude 7.7 Mw
[1]
Depth 16 kilometres (10 mi)
Epicenter
Yellow star marks
epicentre 23°25′08″N
70°13′55″E / 23.419°N
70.232°E[2]
Countries or regions India, Pakistan
Max. intensity X (Intense)
Casualties
19,727 believed dead,
166,001 injured[3]
•The 2001 Gujarat earthquake occurred on January
26, 2001, India's 51st Republic Day, at 08:46 AM
local time (3:16 UTC) and lasted for over two
minutes.
•The epicenter was about 9 km south-southwest of
the village of Chobar in BacheToluca of Kutch
District of Gujarat, India.
•The earthquake reached a magnitude of between
7.6 and 7.7 on the moment magnitude scale and
had a maximum felt intensity of X (Intense) on the
Mercalli intensity scale.
•The quake killed around 20,000 people (including
18 in South eastern Pakistan), injured another
167,000 and destroyed nearly 400,000 homes.
intraplate earthquake
Relief poured in from all over the world and
over a longer period of time, the affected area
was re-equipped with all the basic facilities
along with state-of-the-art upgrades.
The result being that Bhuj, along with
several small towns and villages, is now
complete with a better hospital, town and first-
aid center.
Also, several guidelines and rules were put
into place by the Gujarat government for real-
estate and construction businesses in foresight
of another such event.
Earthquake

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Earthquake

  • 1.
  • 2. •An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. •The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.
  • 3.
  • 4. • Magnitude 3 or lower earthquakes are mostly almost imperceptible or weak and magnitude 7 and over potentially cause serious damage over larger areas, depending on their depth. • The largest earthquakes in historic times have been of magnitude slightly over 9, although there is no limit to the possible magnitude.
  • 5. •The most recent large earthquake of magnitude 9.0 or larger was a 9.0 magnitude earthquake in Japan in 2011 (as of October 2012), and it was the largest Japanese earthquake since records began. • Intensity of shaking is measured on the modified Mercalli scale. •The shallower an earthquake, the more damage to structures it causes, all else being equal.
  • 6.
  • 7. • In its most general sense, the word earthquake is used to describe any seismic event — whether natural or caused by humans — that generates seismic waves. • Earthquakes are caused mostly by rupture of geological faults, but also by other events such as volcanic activity, landslides, mine blasts, and nuclear tests. • An earthquake's point of initial rupture is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter.
  • 8. Earthquakes are caused by tectonic movements in the Earth's crust. The main cause is that when tectonic plates collide, one rides over the other, causing progeny (mountain building), earthquakes and volcanoes.
  • 9. Causes of earthquakes Earthquakes are caused by tectonic movements in the Earth's crust. The main cause is that when tectonic plates collide, one rides over the other, causing progeny (mountain building), earthquakes and volcanoes.
  • 10. • The boundaries between moving plates form the largest fault surfaces on Earth. • When they stick, relative motion between the plates leads to increasing stress. • This continues until the stress rises and breaks, suddenly allowing sliding over the locked portion of the fault, releasing the stored energy.
  • 11. •Earthquake clusters •Most earthquakes form part of a sequence, related to each other in terms of location and time. •Most earthquake clusters consist of small tremors which cause little to no damage, but there is a theory that earthquakes can recur in a regular pattern.
  • 12. Earthquake fault types There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal faults occur mainly in areas where the crust is being extended. Reverse faults occur in areas where the crust is being shortened. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other.
  • 13. Aftershocks An aftershock is an earthquake that occurs after a previous earthquake, the main shock. An aftershock is in the same region of the main shock but always of a smaller magnitude. Aftershocks are formed as the crust adjusts to the effects of the main shock.
  • 14. Date January 26, 2001 Magnitude 7.7 Mw [1] Depth 16 kilometres (10 mi) Epicenter Yellow star marks epicentre 23°25′08″N 70°13′55″E / 23.419°N 70.232°E[2] Countries or regions India, Pakistan Max. intensity X (Intense) Casualties 19,727 believed dead, 166,001 injured[3]
  • 15. •The 2001 Gujarat earthquake occurred on January 26, 2001, India's 51st Republic Day, at 08:46 AM local time (3:16 UTC) and lasted for over two minutes. •The epicenter was about 9 km south-southwest of the village of Chobar in BacheToluca of Kutch District of Gujarat, India. •The earthquake reached a magnitude of between 7.6 and 7.7 on the moment magnitude scale and had a maximum felt intensity of X (Intense) on the Mercalli intensity scale. •The quake killed around 20,000 people (including 18 in South eastern Pakistan), injured another 167,000 and destroyed nearly 400,000 homes.
  • 16.
  • 18. Relief poured in from all over the world and over a longer period of time, the affected area was re-equipped with all the basic facilities along with state-of-the-art upgrades. The result being that Bhuj, along with several small towns and villages, is now complete with a better hospital, town and first- aid center. Also, several guidelines and rules were put into place by the Gujarat government for real- estate and construction businesses in foresight of another such event.