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On December 26, 2004, a powerful earthquake
occurred on the seafloor just off the coast of northern
Indonesia. The earthquake measured at a magnitude of 9.0 and
led to the worst tsunami that occurred in the past 40 years.
The tsunami raced across the ocean at speeds up to 500 mph
and reached some shores in just a matter of minutes. Some
locations, including those on the other side of the Indian
Ocean, anticipated the arrival of the tsunami for over 8
hours. The huge wave crashed onto the coasts of Indonesia,
Malaysia, Thailand, Myanmar, India, Sri Lanka and other
Asian and African countries.
Total devastation occurred in just minutes as the enormous
wave, measuring between 10 and 40 feet, crashed onto the
shores. Beaches and coastlines were washed away and modified
in shape due to the speed and force of the intense waves and
retreating water. Towns were flattened completely, trees and
other vegetation were ruined, and as of January 5, 2005, the
tsunami led to over 155,000 deaths of those who were
unprepared. Water and airborne diseases were responsible for
even more deaths after the water receded. |

The maximum wave height that
likely occurred when the wave came ashore

(Credit: Dr. Vasily Titov, NOAA Tsunami Research Program,
Pacific Marine Environmental Laboratory)
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The coastline of Sumatra, near
the fault boundary, received waves over 10 meters (33 feet)
tall, while those farther away (Sri Lanka and Thailand) were
caught by waves over 4 meters (13 feet). On the other side
of the Indian Ocean, Somalia and the Seychelles were struck
by waves approaching 4 meters in height (13 feet). |
Wave Travel Time

(Credit: Dr. Vasily Titov, NOAA Tsunami Research Program,
Pacific Marine Environmental Laboratory)
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Although the epicenter of the
earthquake that triggered the tsunami was near the northern
tip of Sumatra, the sea floor shifted along an arc
stretching about 1200 km to the north. This shifting pushes
a mass of water across the Indian Ocean. Wave travel times
ranged from minutes (Sumatra) to 8 hours (Somalia) or more. |
How the wave moved towards the
surrounding coasts.
Click on the image to see an
animation (650 KB)

(Animation provided by Kenji Satake,
National Institute of Advanced Industrial Science and
Technology, Japan)
Indonesia:
Before and After the Tsunami - Aceh, NW Sumatra, Indonesia
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The 'before' image was taken by
Space Imaging's IKONOS satellite on January 10, 2003 and the
'after' image was taken on December 29, 2004, 3 days after
the tsunami event.
These IKONOS images are of Aceh, on the northwestern tip of
Sumatra, Indonesia.
The effects of coastline flooding and strong coastal erosion
can be observed. |
Area 1
: Before Tsunami

Area 1
: After Tsunami

Area 2
: Before Tsunami

Area 2
: After Tsunami

Area 3
: Before Tsunami

Area 3
: After Tsunami

Area 4
: Before Tsunami

Area 4
: After Tsunami

Area 5
: Before Tsunami

Area 5
: After Tsunami

Hi-res Images of Tsunami Aftermath:
Banda Aceh, Indonesia
Banda Aceh: After the Tsunami (Area 1)

Banda Aceh: After the Tsunami (Area 2)

Banda Aceh: Grand Mosque

Before and After Images Showing
Coastal Changes in Northwest Sumatra

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The 'before' image was taken by
NASA's Terra satellite on December 17, 2004 and the 'after'
image was taken on Dec. 29, 2004.
On December 17, the green
vegetation along the west coast appears to reach all the way
to the sea, with only an occasional thin stretch of white
that is likely sand. After the earthquake and tsunamis, the
entire western coast is lined with a noticeable
purplish-brown border.
The brownish border could be
deposited sand, or perhaps exposed soil that was stripped
bare of vegetation when the large waves rushed ashore and
then raced away. Another possibility is that parts of the
coastline may have sunk as the sea floor near the plate
boundary rose.
On a moderate-resolution image
such as this, the affected area may seem small, but each
pixel in the full resolution image is 250 by 250 meters (820
by 820 feet). In places the brown strip reaches inland
roughly 13 pixels, equal to a distance of 3.25 kilometers,
or about 2 miles. |
Tsunami
Destroys Lhoknga, Indonesia
Lhoknga before and after the moment of tsunami impact

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On December 26, 2004, the
Indonesian province of Aceh was hit the hardest by the
earthquake and tsunamis that followed. Sumatra, an island
where Aceh is located, received the largest waves leading to
the flattening of towns and devastating fatalities. |
Zoom-in: Lhoknga before and after the moment of tsunami impact

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The town of Lhoknga, on the west
coast of Sumatra near the capital of Aceh, Banda Aceh, was
completely destroyed by the tsunami. The only building that
was not destroyed was the mosque, the large white feature,
in the center of the city.
Most of the vegetation was wiped
out as the tsunami flattened buildings, trees, and
everything else in its path. Beaches and coastlines were
washed away and modified in shape due to the speed and force
of the intense waves and retreating water. Lakes and
streams were flooded and piers were submerged in water.
The low-lying agricultural areas
remained covered with water and debris several days after
the tsunamis |
Tsunami
Destroys
Gleebruk Village, South Banda
Aceh

[ Top of Page]
Before and After the
Tsunami - Kalutara beach, SW Sri Lanka
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The 'before' image was taken by DigitalGlobe's QuickBird
satellite on January 1, 2004 and the 'after' image was taken
on Dec. 26, 2004, 10:20 a.m. local time, slightly less than
four hours after the 6:28 a.m. earthquake (local Sri Lanka
time) and shortly after the moment of tsunami impact.
This QuickBird image of the southwestern coast of Sri
Lanka--just south of the city of Colombo in a resort area
called Kalutara--was collected shortly after the moment of
tsunami impact. --10:20 local time; slightly less than four
hours after the earthquake.
Coastline flooding was observed
-- High water evident at least a kilometer inland
--Churning ocean noted from the receding water
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Area 1
: Before Tsunami

Area 1
: During Tsunami

Area 2
: Before Tsunami

Area 2
: During Tsunami

Area 3
: Before Tsunami

Area 3
: During Tsunami

Area 4
: Before Tsunami

Area 4
: During Tsunami

[ Top of Page]
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The
high-resolution images, acquired by the IKONOS satellite, show before and after views of the
Male Intl' Airport in the Maldives Islands. Male is the capital of the Maldives. The airport is located
in the center of a small island called Hulule and is the
first point of contact for every visitor coming from
overseas. This image was taken from 423 miles in space as IKONOS moved
from north to south over the Indian Ocean.
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Maldives's Male International
Airport Before and After the Tsunami

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The 'before' image was taken by Space
Imaging's IKONOS satellite on Dec. 3, 2003 and the 'after'
image was taken on Dec. 27, 2004. The 'after' image is
cloudy and hazy so the level of detail is not as good as in
the 'before' image.
The imagery shows sand and debris on the runway, debris and
damage to the coastline and damage to structures on the sand jetties. Other
changes visible in the images may have been produced by human development
along the coast (like the sand bar in the lagoon).
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Damaged Docks and Sand
Pushed Onshore

Sand on the Runway

[ Top of Page]
Before and After the Tsunami - Khao
Lak, SW Thailand
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The 'before' image was taken
by Space Imaging's IKONOS satellite on January 13, 2003
and the 'after' image was taken on December 29, 2004, 3
days after the tsunami event. These IKONOS
images are of Khao Lak, on the southwestern coast of
Thailand, south of the city of Takua Pa and north of
Phuket.
The effects of coastline flooding can be
observed and strong coastal erosion. |
Area 1
: Before Tsunami

Area 1
: After Tsunami

Area 2
: Before Tsunami

Area 2
: After Tsunami

[ Top of Page]
:
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This image from the Ikonos
satellite shows the city of Chennai, a harbor city on the
southeastern Indian coast, located about 350 kilometers (220
miles) north of the Palk Strait, which separates Sri Lanka
and India. The "After" image was captured on December 29,
2004, after the waves' arrival. Although the devastation
captured in this image may not seem as obvious as the damage
to Sri Lanka, parts of Thailand, or northern Sumatra, a
careful eye can see the impacts |
Before and After Images Showing
Damages to Chennai, Southeast India

Area 1
: Destroyed / Damaged Structures

A stretch of houses or other
structures has been wiped out. Where the houses used to be is an
open expanse of beach
Area 2
: Boats Piled on Pier

Boats that were neatly lined up in
their moorings along three piers in the August 14 image are
piled on top of the piers in the image from December 29.
[ Top of Page]
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Supplementary Material:
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Sunday 26 December 2004: at 0100 GMT, an
9.0 magnitude earthquake occurs on the seafloor near Aceh in northern
Indonesia. This earthquake generated a huge tsunami wave, hitting the
coasts of Indonesia, Malaysia, Thailand, Myanmar, India, Sri Lanka,
Maldives and even Somalia.
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StormCenter's Earth and
Oceans expert, Dr. Ellen Prager describes the tsunami as
follows:
"Tsunamis can be
highly variable in the way they strike, some coasts may have been
struck by a towering wall of water while others may have experienced a
tremendous surge of water. Much of this variability depends on the
configuration of the coastline and changes in bathymetry as the waves
approach. The destruction from the tsunamis comes from the onslaught
of the water, the power of the waves and surge, and then the swiftly
flowing currents as the water returns to the sea.
If you live or visit the coast and you feel the earth
shaking, see the ocean's level lower rapidly, or hear a loud rushing
noise or bang from offshore, your immediate reaction should be to run
inland and up as far as possible. Do not go to the shore to
investigate and if a warning is issued, take heed and go to a safe
location inland preferably on higher ground."
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A tsunami (pronounced soo-nahm'ee) is a
series of waves generated by the sudden movement or disturbance of the
seafloor. Tsunamis are fast-moving, low, long waves
that radiate out from a triggering event, such as an undersea
earthquake, volcanic eruption, landslide or asteroid impact. Once one
of these waves reaches shallow water, they change…becoming towering,
powerful walls of water that slam ashore.
Hypothetical Tsunami along the Pacific Northwest Coast
(QuickTime 2.2Mb, Courtesy: USGS )
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Tsunamis or seismic sea
waves differ markedly from typical waves generated by the wind.
Imagine blowing over the surface of a coffee cup…the top surface of
the liquid inside moves in small waves. Now shake the cup and all the
water sloshes back and forth and over the lip – this is a tsunami. In
wind waves only a relatively small portion of the water is in
motion…near the surface. In contrast in a tsunami the entire water
column, from the surface to the sea floor, begins to move and transfer
energy.
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Although tsunamis
travel as low, very fast waves, often over 500 mph, once they reach
shallow water, they slow down and bunch up. It is here that the true
danger lay. Sometimes the water along the beach will recede right
before a tsunami hits. Seconds later, one or more towering walls of
water will crash ashore. And not only is the direct hit of the waves
extremely dangerous, but also the currents created as the water piled
onshore swiftly flows back out to sea.
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The tsunami waves can
travel inland along river beds and can pollute the fresh water rivers
and streams with salt water from the ocean.
Trees, shrubs, and other
vegetation were washed away polluting the cities, destroying food for
animals and adding to the debris that created more destruction around
the towns. Drifting materials, oil and other substances can also lead
to the environmental pollution.
Diseases infect areas
where tsunamis strike as people and animals drink water tainted by
sewage. Other respiratory illnesses occur when people are forced to
cram together in refugee camps.
Other water-carrying
diseases such as dysentery and cholera are also possible to occur as
the water supplies are contaminated.
Space Imaging Logos:
Logo : TIF
TGA
GIF ; Logo with
alpha color: TIF
TGA
GIF
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