earthquakes and faults ppt.pptx

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.

What is 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
disurbances in the earth’s crust
may produce vibration in the
crust which travel in all direction
from point of disturbances.

Focus(Hypocenter):
Focus is the point on the fault
where rupture occurs and the
location from which seismic
waves are released.
Epicenter:
Epicenter is the point on the
earth’s surface that is directly
above the focus ,the point where
an earthquake or underground
explosion originates.

Cont…
Fault Line:
A Fault line is the surface trace of
a fault, the line of intersection
between the earth’s surface.
Fault plane:
Fault plane are the crackes or
sudden slips of the land .
Fault Scrap:
A Fault scrap is the topographic
expression of faulting attributed
to the displacement of the land
surface by movement along
faults.

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 to the
surface (known as the dip) and the direction of slip along the
fault to classify faults.

Classification Of Faults
Normal fault:
a dip-slip fault in which the
block above the fault has
moved downward relative to
the block below.
1.Thrust (reverse)fault:
Thrust (reverse)fault:
a dip-slip fault in which the
upper block, above the fault
plane, moves up and over the
lower block.

Strike-slip fault:
A left-lateral strike-slip
fault :
It is one on which the
displacement of the far block is
to the left when viewed from
either side.
A right-lateral strike-slip
fault:
It is one on which the
displacement of the far block is
to the right when viewed from
either side.

Some major causes of earthquakes on basic of its causes are:
Surface causes
Volcanic causes
Tectonic causes
Surface cause:
Great explosions, 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.
Plate Boundary Overview.flv

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

Primary Waves (P-waves) Secondary Waves(S-wave)
High frequency High frequency
Short Wavelength Short Wavelength
Longitudinal waves Transverse waves
Pass trough both solids and
liquids
Can not move through liquids
Move forwards and
backwards as it compressed
and decompressed
Move in all direction from
their source
P-wave is faster S-wave is more slower than P-
wave
First P-wave arrive After P-wave,S-wave is arrive

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

Love Waves Rayleigh wave
Guided waves Guided waves
Displacement is parallel to the
free surface
Displacement is perpendicular
to love-wave displacement
Love wave is faster Rayleigh wave is slower
Causes horizontal shifting of
the earth surface.
Ground move in circular
motion.

The intensity and strength of an earthquake is measured on
Richter scale,the scale invented by Charles Richter California
,USA in 1935.which categories earthquake on the basis of
energy released.
Defintion:
“the logarithm to base ten of the maximum seismic-wave
amplitude recorded on a standard seismograph at a distance of
100 kilometers from the earthquake epicenter.”
Scientists measure the strength of earthquakes using
machines known as seismographs.
Seismology is the scientific study of earthquakes and the
propagation of elastic waves through the Earth.

Amount of energy released during different
Earthquake:
Intensity Of Earthquake
On Richter Scale:
Energy Release (Amount Of
TNT):
1.0 170 Grams
2.0 6 Kilogram
3.0 179 Kilogram
4.0 5 Metric Tons
5.0 179 Metric Tons
6.0 5643 Metric Tons
7.5 1 Mega Tons

Seismometers are instruments
that measure motions of the
ground, including those
of seismic waves generated
by earthquakes, volcanic
eruptions, and otherseismic
sources.
Seismometers may be
deployed at Earth's surface, in
shallow vaults, in boreholes, or
underwater.

 Zone - II: This is said to be the least active seismic zone.
 Zone - III: It is included in the moderate seismic zone.
 Zone - IV: This is considered to be the high seismic zone.
 Zone - V: It is the highest seismic zone.
The earthquake zoning map of India divides India into 4 seismic
zones Based on the observations of the affected area due to
Earthquake india divided into four types of zones:

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 earthquake
Temperature change
Uplifting of earth surface
Change in seismic wave velocity

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 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.

Cont…
Landslides
Shaking and
ground rapture

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.

Keep calm, switch on the transistor radio and obey
instructions.
Keep away from beaches and low banks of river. A huge
wave may sweep in
Do not re enter badly damaged buildings and do not go
near damage structures.
Turn off the water, gas and electricity.
Do not smoke, light match or use a cigarette lighter
Do not turn on switches there may be gas leak or short
circuit
If there is any fire, try to put it out or call fire brigade.

Do not drink water from open containers without having
examined it.
If you aware of people have been buried, tell the rescue team. Do
not rush and try not to worsen the situation.
Avoid places where there are loose electric wires and do not
come in contact with any metal object.
Eat something. You will better and more capable of helping
other.
Do not walk around the streets to see what is happening. Keep
the streets clear so rescue vehicles can access the roads easily.

Date Place Scale Damage
Sept 2,
1993
Latur
(maharashtra)
6.3 Large areas of Maharashtra
rocked. 10,000 people lost
lives.
May 22,
1997
Jabalpur
(Maharashtra)
6.0 40 person killed and over
100 injured.
March 29,
1999
Nandprayag 6.8 widespread destruction in
chamoli , rudraprayag and
other areas. Massive loss of
human life.
Jan. 26,
2001
Bhuj (gujrat) 7.8 Tremors left by India and its
neighboring countries. Over
1 lakh people killed. Huge
loss to property and
infrastructure.
Oct. 8,
2005
Muzzaffarabad
in Pakistan
occupied
Kashmir
7.4 Heavy damage to life and
property.
Death toll about one lakh in
Pakistan and nearly 2000 in
India.

Helpless man being trapped under debris

disaster picture from Kashmir earthquake
2005

 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.

There were more than 20,000 deaths and 167,000 people injured
Four districts of Gujarat lay in ruin and altogether, 21 districts were
affected.
Around 300,000 families and at least 3 million children under 14
aged were affected.
Around 600,000 people were left homeless.
In the city of Bhuj, more than 3,000 Population of the city lost
their lives; the main hospital was crushed and close to 90% of the
buildings was destroyed.
There was significant damage to infrastructure with facilities such
as hospitals, schools, electric power and water systems, bridges and
roads damaged or destroyed.

Damage to high rise building in Bhuj

5 year old girl recovers
at a hospital in Bhuj on
Monday after Friday's
massive earthquake.

The response within India was immediate. The
national and state governments quickly provided
assistance in many forms including cash, medical
supplies, communications teams, shelters, food,
clothing, transport and relief workers.
There were more than 185 non-government
organizations (NGOs), mostly Indian charities, which
undertook earthquake-related activities

Search and Rescue teams soon arrived from
Switzerland, United Kingdom, Russia and Turkey to
find and rescue survivors buried under debris.
Relief teams and supplies soon followed from 38
countries as well as United Nations agencies and
many international NGOs such as the Red Cross.
The world bank and Asian development bank
sanction loans in less than three months after the
earthquake.

Gujarat earthquake emergency reconstruction
project (GEERP) was started by GSDMA(Gujrat State
Disaster Management Authority), with financial help
from world bank, Asian development bank, govt of
India and other donor agencies.
Several state governments came forward to
participate in, the reconstruction work in different
villages.
The UN system, multilateral and bilateral agencies,
NGOs and the corporate sector participated in the
relief and reconstruction work.

Government of Gujarat provided assistance in the form
of materials and cash to about 218,000 families.
NGOs supplemented the efforts by providing shelter to
about 7000 families.
About 65 NGOs were active in kutch alone who
adopted 211 villages and constructed 32,297 houses at the
cost of Rs. 185.80 crores.
The technical support was made available to the
owners who were provided loan to reconstruct the
houses.

earthquakes and faults ppt.pptx

earthquakes and faults ppt.pptx

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earthquakes and faults ppt.pptx