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Earthquakes
.
Kota Vamshi
 Introduction
 Types
 Earthquake measuring devices
 Seismic zones of India
 Earthquakes in India
 Hazards and Impacts
 Risk Mitigation
 Events During an Earthquake
 Role of EMS
.
.
.
.
Agenda
Introduction:
PlateTectonics
.
Plate tectonics, theory dealing with
the dynamics of Earth’s outer shell—
the lithosphere—that
revolutionized Earth sciences by
providing a uniform context for
understanding mountain-building
processes, volcanoes, and earthquakes
as well as the evolution of Earth’s
surface and reconstructing its past
continents and oceans.
Some major tectonic plates are:
• African plate
• Antarctic plate
• Eurasian plate.
• IndoAustralian plate.
• NorthAmerican plate.
• Pacific plate.
• South American plate.
An earthquake (quake, tremor or temblor) is the
shaking of the surface of the Earth resulting from a
sudden release of energy in
the Earth's lithosphere that creates seismic waves.
Earthquakes can range in intensity, from those that
are so weak that they cannot be felt, to those violent
enough to propel objects and people into the air,
damage critical infrastructure, and wreak destruction
across entire cities.
The seismic activity of an area is the frequency,
type, and size of earthquakes experienced over a
particular time.
When the epicenter of a large earthquake is located
offshore, the seabed may be displaced sufficiently to
cause a tsunami. Earthquakes can also
trigger landslides.
Introduction:Earthquake
TypesofFaults
(Earthquakemovements)
A fault is a planar
fracture or discontinuity in a
volume of rock across which
there has been significant
displacement as a result of
rock-mass movements.
Faults
A reverse fault is one in
which one side of the
fault, the hanging wall,
moves up and over the
other side, the foot
wall.
Reverse faults
faults are inclined
fractures where the
blocks have mostly
shifted vertically.
Normal faults
Strike-slip faults
are vertical (or nearly
vertical) fractures
where the blocks have
mostly moved
horizontally.
Strike-slip faults
WhatareDevicestoMeasurethe
magnitudeofearthquake?
Richter
Magnitude
Scale
• .
• .
• .
• .
The Richter scale is used to rate the magnitude of an earthquake,
that is the amount of energy released during an earthquake.
Seismometers
Seismographs
Seismograms
• .
• .
• .
• .
Seismographs are instruments used to record the
motion of the ground during an earthquake.
A Seismogram is the recording of the ground
shaking at the specific location of the instrument.
A Seismometer is the internal part of the
seismograph, which may be a pendulum, or a mass
mounted on a spring; however, it is often used
synonymously with "seismograph".
This region is liable to lower and is
classified as the Low Damage Risk
Zone. It is the zone with low
chances of having earthquakes.
This zone is classified as a Moderate
Damage Risk Zone. The IS code
assigns a zone factor of 0.16 for
Zone 3.
This zone is called the High Damage
Risk Zone. The IS code assigns a
zone factor of 0.24 for Zone 4.
Zone 5 covers the areas with the
highest risk of suffering earthquakes.
It is referred to as the Very High
Damage Risk Zone.
Seismiczonesof
India
.
Earthquake-prone regions of the country have
been identified on the basis of scientific inputs
related to seismicity, earthquakes that
occurred in the past and the tectonic setup of
the region. On the basis of these inputs, the
Bureau of Indian Standards (BIS) has grouped
the country into four seismic zones viz. zones
V, IV, III and II. Zone V being the highest and
Zone II being lowest
SomeFatalEarthquakesinIndia
•Magnitude: 9.1–9.3
•Epicenter: West coast of
Sumatra, Indonesia (3.316°N
95.854°E)
•Deaths: >283,106 (Includes
deaths in Indonesia, Sri Lanka,
India,Thailand, Maldives, and
Somalia)
Indian Ocean Earthquake, 2004
•Magnitude: 8.7
•Epicenter: South of Mount
Everest (27.55°N 87.09°E)
•Deaths: > 30,000
Great Bihar-Nepal Earthquake,
1934
•Magnitude: 7.6
•Epicentre: Muzaffarabad,
Pakistan-administered Kashmir
(34.45°N 73.65°E)
• Deaths: 130,000
Kashmir Earthquake, 2005
•Magnitude: 7.7-
•Epicentre: Bhuj, Kutch,
Gujarat (23.419°N 70.232°E)
•Deaths: 20,000
Gujarat Earthquake,2001
Hazardswithanearthquake
•
Various hazards associated with an earthquake can be grouped
as:
Primary hazards: These are the effects, which occur
simultaneously along with the natural phenomenon of the
earthquake.
~Ground Shanking
~Fault rupture
~Tectonic deformities
Secondary hazards: These affects are those, which occur at the
end or after the earthquake phenomenon.
~Soil liquefaction
~Land and Mud slides
~Submarine avalanches
~Snow avalanches
~Tsunamis
Primary Impacts :
~Building and bridge collapse
~Rupture Of water and pipelines and Other utilities
~Changes in underground water sources
~Changes in courses of rivers
~Disappearance and/or creation of new islands.
Secondary Impacts :
~Death and damage due to collapse of including buildings.
~Fire and explosions
~Disease and epidemics
~Floods from dam failure
~Floods from tsunami.
Impacts due to Earthquake
Earthquakes : Risk
Mitigation
.
• Hazard resistant construction or
retrofitting of Buildings/ Houses
to reduce the vulnerability of the
structures
• Proper land use planning to avoid
potentially high hazard zones.
• Community preparedness through
awareness generation, mutual
assistance, and adherence to a set
of Do's and Don'ts.
.
.
.*
.*
Role of Healthcare/Medicine(EMS) in
Earthquakes
Common Injuries for the victims of an Earthquake are:
• Lacerations
• Contusions
• Simple Fractures. etc.,.
EDs will experience an increase in patients with these
diagnoses like
• ChronicObstructive Pulmonary Disease(COPD),
• Cardiac arrest
• Myocardial Infarctions,
• Possibly childbirth. etc.,.
The second group includes those with conditions or issues more
unique to earthquakes, such as
• Crush injury
• The need to use ketamine,
• Indications for hypertonic saline treatment. etc.,.
Conclusion
•
• .
• .
• An earthquake is a natural phenomenon. It is difficult to make accurate prediction about
the time, location and magnitude of an earthquake.
• The movement of tectonic plates due to the mantle leads to earthquakes. On according
based on few assumptions we divide the geographical area into Seismic zones and MSK
scale.
• One should be ready after knowing about the warning signs and move to safer places.
The highest authority should note about the hazards and impacts and be ready to
excavate the victims and calculate the disaster damage.
• Taking precautions can save one from the natural calamities. Community should try to
participate in the rescue programme and doesn't spread any kind of chaotic rumours.
• The responsible department should concentrate on the events before-during-after the
event.
• The role of medical services is the most important, it should include keen assessment
,Face unique unexpected situation, they should try to understand, treat and prevent the
mental and physical state of patient .
References:
• Britannica
• Geological survey of India
• India today
• The Hindu
• David E. Hogan (Disaster Medicine)
• Textbook of Community Medicine
• NCERT Grade 11 Geography
• Natural Disasters (Deanna Romero)
Thank

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Earthquakes

  • 2.  Introduction  Types  Earthquake measuring devices  Seismic zones of India  Earthquakes in India  Hazards and Impacts  Risk Mitigation  Events During an Earthquake  Role of EMS . . . . Agenda
  • 3. Introduction: PlateTectonics . Plate tectonics, theory dealing with the dynamics of Earth’s outer shell— the lithosphere—that revolutionized Earth sciences by providing a uniform context for understanding mountain-building processes, volcanoes, and earthquakes as well as the evolution of Earth’s surface and reconstructing its past continents and oceans. Some major tectonic plates are: • African plate • Antarctic plate • Eurasian plate. • IndoAustralian plate. • NorthAmerican plate. • Pacific plate. • South American plate.
  • 4. An earthquake (quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can also trigger landslides. Introduction:Earthquake
  • 5. TypesofFaults (Earthquakemovements) A fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Faults A reverse fault is one in which one side of the fault, the hanging wall, moves up and over the other side, the foot wall. Reverse faults faults are inclined fractures where the blocks have mostly shifted vertically. Normal faults Strike-slip faults are vertical (or nearly vertical) fractures where the blocks have mostly moved horizontally. Strike-slip faults
  • 7. Richter Magnitude Scale • . • . • . • . The Richter scale is used to rate the magnitude of an earthquake, that is the amount of energy released during an earthquake.
  • 8. Seismometers Seismographs Seismograms • . • . • . • . Seismographs are instruments used to record the motion of the ground during an earthquake. A Seismogram is the recording of the ground shaking at the specific location of the instrument. A Seismometer is the internal part of the seismograph, which may be a pendulum, or a mass mounted on a spring; however, it is often used synonymously with "seismograph".
  • 9. This region is liable to lower and is classified as the Low Damage Risk Zone. It is the zone with low chances of having earthquakes. This zone is classified as a Moderate Damage Risk Zone. The IS code assigns a zone factor of 0.16 for Zone 3. This zone is called the High Damage Risk Zone. The IS code assigns a zone factor of 0.24 for Zone 4. Zone 5 covers the areas with the highest risk of suffering earthquakes. It is referred to as the Very High Damage Risk Zone. Seismiczonesof India . Earthquake-prone regions of the country have been identified on the basis of scientific inputs related to seismicity, earthquakes that occurred in the past and the tectonic setup of the region. On the basis of these inputs, the Bureau of Indian Standards (BIS) has grouped the country into four seismic zones viz. zones V, IV, III and II. Zone V being the highest and Zone II being lowest
  • 10.
  • 11. SomeFatalEarthquakesinIndia •Magnitude: 9.1–9.3 •Epicenter: West coast of Sumatra, Indonesia (3.316°N 95.854°E) •Deaths: >283,106 (Includes deaths in Indonesia, Sri Lanka, India,Thailand, Maldives, and Somalia) Indian Ocean Earthquake, 2004 •Magnitude: 8.7 •Epicenter: South of Mount Everest (27.55°N 87.09°E) •Deaths: > 30,000 Great Bihar-Nepal Earthquake, 1934 •Magnitude: 7.6 •Epicentre: Muzaffarabad, Pakistan-administered Kashmir (34.45°N 73.65°E) • Deaths: 130,000 Kashmir Earthquake, 2005 •Magnitude: 7.7- •Epicentre: Bhuj, Kutch, Gujarat (23.419°N 70.232°E) •Deaths: 20,000 Gujarat Earthquake,2001
  • 12. Hazardswithanearthquake • Various hazards associated with an earthquake can be grouped as: Primary hazards: These are the effects, which occur simultaneously along with the natural phenomenon of the earthquake. ~Ground Shanking ~Fault rupture ~Tectonic deformities Secondary hazards: These affects are those, which occur at the end or after the earthquake phenomenon. ~Soil liquefaction ~Land and Mud slides ~Submarine avalanches ~Snow avalanches ~Tsunamis
  • 13. Primary Impacts : ~Building and bridge collapse ~Rupture Of water and pipelines and Other utilities ~Changes in underground water sources ~Changes in courses of rivers ~Disappearance and/or creation of new islands. Secondary Impacts : ~Death and damage due to collapse of including buildings. ~Fire and explosions ~Disease and epidemics ~Floods from dam failure ~Floods from tsunami. Impacts due to Earthquake
  • 14. Earthquakes : Risk Mitigation . • Hazard resistant construction or retrofitting of Buildings/ Houses to reduce the vulnerability of the structures • Proper land use planning to avoid potentially high hazard zones. • Community preparedness through awareness generation, mutual assistance, and adherence to a set of Do's and Don'ts. . . .* .*
  • 15.
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  • 17. Role of Healthcare/Medicine(EMS) in Earthquakes Common Injuries for the victims of an Earthquake are: • Lacerations • Contusions • Simple Fractures. etc.,. EDs will experience an increase in patients with these diagnoses like • ChronicObstructive Pulmonary Disease(COPD), • Cardiac arrest • Myocardial Infarctions, • Possibly childbirth. etc.,. The second group includes those with conditions or issues more unique to earthquakes, such as • Crush injury • The need to use ketamine, • Indications for hypertonic saline treatment. etc.,.
  • 18. Conclusion • • . • . • An earthquake is a natural phenomenon. It is difficult to make accurate prediction about the time, location and magnitude of an earthquake. • The movement of tectonic plates due to the mantle leads to earthquakes. On according based on few assumptions we divide the geographical area into Seismic zones and MSK scale. • One should be ready after knowing about the warning signs and move to safer places. The highest authority should note about the hazards and impacts and be ready to excavate the victims and calculate the disaster damage. • Taking precautions can save one from the natural calamities. Community should try to participate in the rescue programme and doesn't spread any kind of chaotic rumours. • The responsible department should concentrate on the events before-during-after the event. • The role of medical services is the most important, it should include keen assessment ,Face unique unexpected situation, they should try to understand, treat and prevent the mental and physical state of patient .
  • 19. References: • Britannica • Geological survey of India • India today • The Hindu • David E. Hogan (Disaster Medicine) • Textbook of Community Medicine • NCERT Grade 11 Geography • Natural Disasters (Deanna Romero)
  • 20. Thank

Editor's Notes

  1. Sometimes Indo-Australian plate is considered as one . The tectonic plates are further divided into smaller based on convinence. There are approximately 160 tectonic plates on the planet
  2. Zone 5 covers the areas with the highest risk of suffering earthquakes of intensity MSK IX (Medvedev–Sponheuer–Karnik scale) or more significantly. The IS code assigns a zone factor of 0.36 for Zone 5. Structural designers use this factor for the earthquake-resistant design of structures in Zone 5. The zone factor of 0.36 (the maximum horizontal acceleration that a structure can experience) is indicative of effective (zero period) level earthquakes in this zone. It is referred to as the Very High Damage Risk Zone. Generally, the areas having trap rock or basaltic rock are prone to earthquakes
  3. Not perceivable 1/ Hardly perceivable 2/ Weak 3/ Largely Observed 4 Fairly Strong 5/Strong 6 Very Strong 7/ Damaging 8 Destructive 9 / devastating 10 / Catastrophic 11
  4. The biggest earthquake ever recorded, of magnitude 9.5, happened on May 22, 1960, in Chile Gujarat January 26, 2001, August 15, 1950.
  5. Ketamine (ketamine hydrochloride) : (severe pain) : trauma, Head Injury,fractures, abdominal and flank pain, low back pain, and extremity pain. has been approved for general anesthesia either alone or in combination with other medications. It is a superb drug for use in short-term medical procedures that do not require skeletal muscle relaxation 1981 Athens earthquake resulted 50% cardiac arrests cases in 3 days of disaster