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(ASEMINARREPORTFORPARTIALFULFILLMENTOFM.SC.DEGREEINZOOLOGY)
Submittedby– GhanshyamYadav
M.Sc.(zoology)sem-II
Rollno.-1989011
Guide–Dr.A.K.SHRIVASTAVA
Department of zoology
AffiliatedToThe University of Rajasthan
EL-NINO
Defination-
over pacific ocean(Non- El Nino
year):
NoramlYear El-Nino year
Effects of El-Nino
LA-NINA
Effects of LA-Nina
•EARTHQUAKE
Introduction
Earthquakes constitute one of the worst natural hazards
which often turn into disaster causing widespread
destruction and loss to human life.
The effects of earthquake vary upon the magnitude and
intensity. Earthquakes occur every now and then all
round the world. except in some places where
earthquakes occur rarely. The devastation of cities and
towns is one of the effects of earthquake.
An Earthquake is the result of a sudden release of
energy in the earth's crust that creates seismic waves.
The seismic activity of an area refers to the frequency.
type and size of earthquakes experienced over a period
of time.
For example
If you throw stone in a pond of still water. Series of
waves are produced on the surface of water. These
waves spread out in all directions from the point where
the stone strikes the water.
Similarly any sudden disturbances in the earth's crust
may produce vibration in the crust which travel in all
direction from point of disturbances.
The primary cause of an earthquake is faults on the crust of the
earth.
"A Fault is a break or fracture b/w two blocks of rocks in
response to stress."
 This movement may occur rapidly, in the form of an
earthquake or may occur slowly, in the form of creep.
Earth scientists use the angle of the fault with respect tot eh
surface (known as the dip) and the direction of slip along the fault
to classify faults.
Some major causes of earthquakes on basic of its causes
are :
Surface causes
Volcanic causes
Tectonic causes
Surface Cause :
Great explosion, landslides, slips on steep coasts, dashing
of sea waves, avalanches, railway trains, heavy trucks, some
large engineering projects cause minor tremors. Some of them
are man made, other are natural.
Volcanic Cause :
Volcanic eruptions produce
earthquakes. Earthquakes may
precede, accompany and frequently
follow volcanic eruptions.
They are caused by sudden
displacements of lava within or
beneath the earth crust.
There are two general categories of
earthquakes that can occur at a
volcano :
volcano-tectonic earthquakes
Long period earthquakes.
Tectonic Cause :
Structural disturbances resulting in the parts of the
lithosphere is the main cause of this type of earthquake.
Most of the disastrous earthquakes belong to this
category and occur in areas of great faults and fractures.
Sudden yielding to strain produced on the rocks of
accumulating stress causes displacements especially
along old fault zones known as great transform faults.
Seismic waves produced due to earthquake are
basically divided into two major types :
 Body waves
 Surface waves
Body waves :
Body waves travels through the interior
(body) of earth as they leave the focus. Body
waves are further divided into following types
:
 Primary (P) waves
 Secondary (s) waves
Waves produced due to Earthquake
Surface Wave :
Surface waves travels parallel to the earth's surface and
these waves are slowest and most damaging. Surface
wave are divided into following types :
 Love waves
 Rayleigh waves
Seismometer-The measurement of
earthquake
 Seismometers are instruments
that unmeasured motions of the
ground, including those of
seismic waves generated by
earthquakes, volcanic eruptions,
and other seismic sources.
 Seismometers may be
deployed at Earth's surface, in
shallow vaults, in boreholes, or
underwater.
Earthquake Prediction
Earthquake prediction is usually defined as the
specification of the time, location, and magnitude of a
future earthquake within stated limits.
But some evidence of upcoming Earthquake are
following :
 Unusual animal behavior
 Water level in wells
 Large scale of fluctuation of oil flow from oil wells
 Foreshocks or minor shocks before major
earthquakes
 Temperature change
 Uplifting of earth surface
 Change in seismic wave velocity
Effect of Earthquake
 Loss of life and property
 Damage to transport system i.e. roads. railways,
highways, airports, marine
 Damage to infrastructure.
 Chances of Floods - Develop cracks in Dams
 Chances of the fire short-circuit
 Communications such as telephone wires are
damaged
 Water pipes, sewers are disrupted
 Economic activities like agriculture, industry, trade
and transport are severely affected.
Landslides Floods
Fire Soil liquefaction
Shaking and ground rupture Tsunami
Earthquake Safety Rules
If you are in house :
 Don't use lift for getting down from building.
 Be prepared to move with your family.
If you are in shop school or office :
 Don't run for an exit.
 Take cover under a disk/table.
 Move away from window glass.
 Do not go near electric point and cable. Keep away from weak Portion of the building and false
ceiling.
If you are outside :
 Avoid high buildings, walls, power lines and other objects that could fall and create block.
 Don't run through streets.
 If possible, move on to an open area away from hazard including trees.
If you are in vehicle :
 Stop in a safe open place.
 Remain inside vehicle.
 Close window, doors and vents.
Bhuj Earthquake- 26th January 2001
 Date : 26th January 2001
 Origin line : 08 hrs. 46 min. 42.9 sec. IST
 Epicenter : Latitude 23.40 N Longitude 70.28 E
 Magnitude : 7.7
 Focal Depth : 25 kms.
• On the morning of January 26, 2001, the Nation's
52nd Republic Day, a devastating earthquake occurred
in the Kutchh district of the state of Gujarat.
• The earthquake was felt as far away as Delhi in the
north, Kolkata in the east.
• Bhuj town and the village Bhachau, 60 km east of
Bhuj, were the worst affected and many other areas of
Gujarat including its state headquarters Ahmedabad,
were badly affected.
TSUNAMI
When the wave enters shallow water, it slows down and its
amplitude (height) increases.
• Tidal wave
• Seismic sea wave
seismic
landslides
CAUSES
VOLCANO-GENERATED TSUNAMI
Diagram of how a volcanic eruption can generate a tsunami.
LANDSLIDE-GENERATED TSUNAMI
Tsunami caused due to landslides
Tsunami generated by Earthquake
MeasurestakenbeforeTsunami
 When in coastal areas, stay
alert for tsunami warnings.
 Plan an evacuation route that
leads to higher ground.
 Know the warning sings of
tsunami like, rapidly rising or
falling coastal waters &
rumblings of an offshore
earthquake.
 Never stay near shore to
watch a tsunami come in
MajorTsunami of World
Climate Prediction Center (19 December 2005). "FrequentlyAsked
Questions about El Niño and La Niña". National Centers for
Environmental Prediction. Retrieved 17 July 2009.
"Historical El Niño and La Niña Events"
Significant Earthquake Database National
Geophysical Data Center NOAA

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Climatic changes el nino and la nina

  • 3. over pacific ocean(Non- El Nino year):
  • 9. Introduction Earthquakes constitute one of the worst natural hazards which often turn into disaster causing widespread destruction and loss to human life. The effects of earthquake vary upon the magnitude and intensity. Earthquakes occur every now and then all round the world. except in some places where earthquakes occur rarely. The devastation of cities and towns is one of the effects of earthquake.
  • 10. An Earthquake is the result of a sudden release of energy in the earth's crust that creates seismic waves. The seismic activity of an area refers to the frequency. type and size of earthquakes experienced over a period of time. For example If you throw stone in a pond of still water. Series of waves are produced on the surface of water. These waves spread out in all directions from the point where the stone strikes the water. Similarly any sudden disturbances in the earth's crust may produce vibration in the crust which travel in all direction from point of disturbances.
  • 11. The primary cause of an earthquake is faults on the crust of the earth. "A Fault is a break or fracture b/w two blocks of rocks in response to stress."  This movement may occur rapidly, in the form of an earthquake or may occur slowly, in the form of creep. Earth scientists use the angle of the fault with respect tot eh surface (known as the dip) and the direction of slip along the fault to classify faults.
  • 12. Some major causes of earthquakes on basic of its causes are : Surface causes Volcanic causes Tectonic causes Surface Cause : Great explosion, landslides, slips on steep coasts, dashing of sea waves, avalanches, railway trains, heavy trucks, some large engineering projects cause minor tremors. Some of them are man made, other are natural.
  • 13. Volcanic Cause : Volcanic eruptions produce earthquakes. Earthquakes may precede, accompany and frequently follow volcanic eruptions. They are caused by sudden displacements of lava within or beneath the earth crust. There are two general categories of earthquakes that can occur at a volcano : volcano-tectonic earthquakes Long period earthquakes.
  • 14. Tectonic Cause : Structural disturbances resulting in the parts of the lithosphere is the main cause of this type of earthquake. Most of the disastrous earthquakes belong to this category and occur in areas of great faults and fractures. Sudden yielding to strain produced on the rocks of accumulating stress causes displacements especially along old fault zones known as great transform faults.
  • 15. Seismic waves produced due to earthquake are basically divided into two major types :  Body waves  Surface waves Body waves : Body waves travels through the interior (body) of earth as they leave the focus. Body waves are further divided into following types :  Primary (P) waves  Secondary (s) waves Waves produced due to Earthquake
  • 16. Surface Wave : Surface waves travels parallel to the earth's surface and these waves are slowest and most damaging. Surface wave are divided into following types :  Love waves  Rayleigh waves
  • 17. Seismometer-The measurement of earthquake  Seismometers are instruments that unmeasured motions of the ground, including those of seismic waves generated by earthquakes, volcanic eruptions, and other seismic sources.  Seismometers may be deployed at Earth's surface, in shallow vaults, in boreholes, or underwater.
  • 18. Earthquake Prediction Earthquake prediction is usually defined as the specification of the time, location, and magnitude of a future earthquake within stated limits. But some evidence of upcoming Earthquake are following :  Unusual animal behavior  Water level in wells  Large scale of fluctuation of oil flow from oil wells  Foreshocks or minor shocks before major earthquakes  Temperature change  Uplifting of earth surface  Change in seismic wave velocity
  • 19. Effect of Earthquake  Loss of life and property  Damage to transport system i.e. roads. railways, highways, airports, marine  Damage to infrastructure.  Chances of Floods - Develop cracks in Dams  Chances of the fire short-circuit  Communications such as telephone wires are damaged  Water pipes, sewers are disrupted  Economic activities like agriculture, industry, trade and transport are severely affected.
  • 20. Landslides Floods Fire Soil liquefaction Shaking and ground rupture Tsunami
  • 21. Earthquake Safety Rules If you are in house :  Don't use lift for getting down from building.  Be prepared to move with your family. If you are in shop school or office :  Don't run for an exit.  Take cover under a disk/table.  Move away from window glass.  Do not go near electric point and cable. Keep away from weak Portion of the building and false ceiling. If you are outside :  Avoid high buildings, walls, power lines and other objects that could fall and create block.  Don't run through streets.  If possible, move on to an open area away from hazard including trees. If you are in vehicle :  Stop in a safe open place.  Remain inside vehicle.  Close window, doors and vents.
  • 22. Bhuj Earthquake- 26th January 2001  Date : 26th January 2001  Origin line : 08 hrs. 46 min. 42.9 sec. IST  Epicenter : Latitude 23.40 N Longitude 70.28 E  Magnitude : 7.7  Focal Depth : 25 kms. • On the morning of January 26, 2001, the Nation's 52nd Republic Day, a devastating earthquake occurred in the Kutchh district of the state of Gujarat. • The earthquake was felt as far away as Delhi in the north, Kolkata in the east. • Bhuj town and the village Bhachau, 60 km east of Bhuj, were the worst affected and many other areas of Gujarat including its state headquarters Ahmedabad, were badly affected.
  • 24. When the wave enters shallow water, it slows down and its amplitude (height) increases.
  • 25. • Tidal wave • Seismic sea wave seismic landslides
  • 26.
  • 28. VOLCANO-GENERATED TSUNAMI Diagram of how a volcanic eruption can generate a tsunami.
  • 30. Tsunami generated by Earthquake
  • 31.
  • 32. MeasurestakenbeforeTsunami  When in coastal areas, stay alert for tsunami warnings.  Plan an evacuation route that leads to higher ground.  Know the warning sings of tsunami like, rapidly rising or falling coastal waters & rumblings of an offshore earthquake.  Never stay near shore to watch a tsunami come in
  • 33.
  • 35. Climate Prediction Center (19 December 2005). "FrequentlyAsked Questions about El Niño and La Niña". National Centers for Environmental Prediction. Retrieved 17 July 2009. "Historical El Niño and La Niña Events" Significant Earthquake Database National Geophysical Data Center NOAA