INDONESIAN TSUNAMI
26TH
DECEMBER 2004
At GMT 00.59 a magnitude 9 undersea
earthquake shook the sea bed off the north west
coast of Sumatra. Within hours multiple tsunamis
had swept across the Indian Ocean ravaging
coastal regions and killing over 120,000 people.
Two tectonic plates, the
Australian and
Eurasian plates, meet
just off Sumatra's
south-west coast,
grinding together and
sending periodic
seismic tremors
through the region.
violent rupture occurred
on the sea floor along a
fault about 1,000km
long.
Source:-BNPB,2005
Area affected
The 9.0 magnitude quake, which
was the strongest in the world for at
least 40 years, wreaked havoc
across the whole region.
Walls of water, tens of metres high,
slammed into coastal resorts
thousands of miles apart.
Surging seas and floods were
reported as far away as east Africa.
Source:-BNPB,2005
Deadly wave
All along the rupture
the seafloor was
shunted vertically by
about 10 metres.
This movement
displaced the overlying
water, generating a
massive tsunami, or
tidal wave.
The wave then fanned
out across the Indian
Ocean at enormous
speed.
Source:-BNPB,2005
“Scale of
devastation
Thousands are reported
to have been killed, but
there has been little
news from the worst-hit
areas where all
transport and
communication links
were destroyed. “
bbc.co.uk 27.12.04
The Aftermath
Early reports gave no
hint of the scale of the
disaster…….
Whole villages were flattened as here in indonesia
BANDA
ACEH
CITY,
SUMART
A
DIGITAL
GLOBE
SATELLIT
E
PHOTOS
Before
After
Damage map of Banda Aceh showing the impact of tsunamis wave fronts from two
directions. The numerals indicate the tsunami elevation in meters near the beach (white)
and flow depth inland (black).
Source :- UNOSAT, Tsunami data: Borrero et al.
2006, Jaffe et al., 2006, Matsutomi et al., 2006).
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Source:-International strategy for disaster management ISDR,2004
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
Indonesian earthquake and tsunami val 2015
CONCLUSIONS
• The Tsunami caused in indonesia killed >300,000 people because there was no
Warning System.
• Source region for Tsunami extends from Banda Aceh through the Nicobar Islands.
• We need a method for estimating size of great earthquakes within a time frame useful
to the Tsunami Warning System.
References:-
Geocities, web page: www.geocities.com
Goda Y., Random Seas and Design of Maritime Structures, University of Tokyo
Press,Tokyo, Japan, 323 pp.
Mapsoftworld, web page: www.mapsoftworld.com
USGS, Geological Survey web:http://earthquake.usgs.gov/eqinthenews/2004/usslav/
"Tsunamis and Earthquakes: Tsunami Generation from the 2004 Sumatra Earthquake —
. Walrus.wr.usgs.gov. Retrieved 12 August2010

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Indonesian earthquake and tsunami val 2015

  • 1. INDONESIAN TSUNAMI 26TH DECEMBER 2004 At GMT 00.59 a magnitude 9 undersea earthquake shook the sea bed off the north west coast of Sumatra. Within hours multiple tsunamis had swept across the Indian Ocean ravaging coastal regions and killing over 120,000 people.
  • 2. Two tectonic plates, the Australian and Eurasian plates, meet just off Sumatra's south-west coast, grinding together and sending periodic seismic tremors through the region. violent rupture occurred on the sea floor along a fault about 1,000km long. Source:-BNPB,2005
  • 3. Area affected The 9.0 magnitude quake, which was the strongest in the world for at least 40 years, wreaked havoc across the whole region. Walls of water, tens of metres high, slammed into coastal resorts thousands of miles apart. Surging seas and floods were reported as far away as east Africa. Source:-BNPB,2005
  • 4. Deadly wave All along the rupture the seafloor was shunted vertically by about 10 metres. This movement displaced the overlying water, generating a massive tsunami, or tidal wave. The wave then fanned out across the Indian Ocean at enormous speed. Source:-BNPB,2005
  • 5. “Scale of devastation Thousands are reported to have been killed, but there has been little news from the worst-hit areas where all transport and communication links were destroyed. “ bbc.co.uk 27.12.04 The Aftermath Early reports gave no hint of the scale of the disaster…….
  • 6. Whole villages were flattened as here in indonesia
  • 8. Damage map of Banda Aceh showing the impact of tsunamis wave fronts from two directions. The numerals indicate the tsunami elevation in meters near the beach (white) and flow depth inland (black). Source :- UNOSAT, Tsunami data: Borrero et al. 2006, Jaffe et al., 2006, Matsutomi et al., 2006).
  • 16. Source:-International strategy for disaster management ISDR,2004
  • 20. CONCLUSIONS • The Tsunami caused in indonesia killed >300,000 people because there was no Warning System. • Source region for Tsunami extends from Banda Aceh through the Nicobar Islands. • We need a method for estimating size of great earthquakes within a time frame useful to the Tsunami Warning System.
  • 21. References:- Geocities, web page: www.geocities.com Goda Y., Random Seas and Design of Maritime Structures, University of Tokyo Press,Tokyo, Japan, 323 pp. Mapsoftworld, web page: www.mapsoftworld.com USGS, Geological Survey web:http://earthquake.usgs.gov/eqinthenews/2004/usslav/ "Tsunamis and Earthquakes: Tsunami Generation from the 2004 Sumatra Earthquake — . Walrus.wr.usgs.gov. Retrieved 12 August2010