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Freitag, 31. März 2017

EMSC > EARTHQUAKE > M 5.6 - MINAHASA, SULAWESI, INDONESIA

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You are here : EMSC > Earthquake > M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC
    About EMSC

M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC


EMSC

@LastQuake

Independant Scientifc Organization and provider of real-time earthquake warning. Share information with us through our app :
based in Paris, works globally

 I felt this earthquake



Magnitudemb 5.6
RegionMINAHASA, SULAWESI, INDONESIA
Date time2017-03-31 11:21:00.9 UTC
Location0.32 N ; 120.61 E
Depth100 km
Distances618 km N of Makassar, Indonesia / pop: 1,322,000 / local time: 19:21:00.9 2017-03-31
157 km NE of Palu, Indonesia / pop: 283,000 / local time: 19:21:00.9 2017-03-31
Global view
Source parameters reviewed by a seismologist
You felt this earthquake. Tell us!

More information at:

 Badan Meteorologi, Klimatologi, dan Geofisika Djakarta, Indonesia
 Philippine Inst. of Volcanology and Seismology Quezon City, Philippines
 USGS/NEIC Denver, USA
 GeoForschungsZentrum (GFZ) Potsdam, Germany


You are here : EMSC > Earthquake > M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC
    About EMSC

M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC


 I felt this earthquake



 Geoscience Australia, Canberra, ACT, Australia -- Camberra, Australia (AUST)
 National Institute for Earth Physics -- Bucharest, Romania (BUC)
 MTA CSFK GGI Kövesligethy Radó Seismological Observatory -- Budapest, Hungary (BUD)
 Disaster and Emergency Management Presidency, Earthquake Department -- Ankara, Turkey (DDA)
 GeoForschungsZentrum (GFZ) -- Potsdam, Germany (GFZ)
 Geophysical Survey of the Russian Academy of Sciences -- Obninsk, Russia (GSRC)
 Kandilli Observatory and Earthquake Research Institute -- Istanbul, Turkey (KAN)
 Carpathian Seismological Department, Ukraine Academy of Science -- Lviv, Ukraine (LVV)
 National Earthquake Information Center, U.S. Geological Survey -- Golden, USA (NEIR)
 Norwegian Seismic Array -- Kjeller, Norway (NEWS)
You are here : EMSC > Earthquake > M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC
    About EMSC

M 5.6 - MINAHASA, SULAWESI, INDONESIA - 2017-03-31 11:21:00 UTC


 I felt this earthquake



AuthorEMSC
Date/Time UTC2017/03/31 11:21:00.9
Distances to cities618 km N of Makassar, Indonesia / pop: 1,322,000 / local time: 19:21:00.9 2017-03-31
157 km NE of Palu, Indonesia / pop: 283,000 / local time: 19:21:00.9 2017-03-31
Latitude0.32 N
Longitude120.61 E
Depth100.0 Km
Magnitudemb 5.6
RegionMINAHASA, SULAWESI, INDONESIA
rms1.30 s
Nphases, Nstation258, 238
Gap13 °
95% confidence Ellipse Semi major
Semi minor
Azimuth
3.2 Km
3.0 Km
28 °
Location Typemanual
Publication Time2017-03-31 12:33 UTC

Explanation of Parameters


Sta
Dist
EvAz
AM
CD
IE
Phase
Pick Time
Tres
Azim
Slow
T
A
S
Amp
Per
Mag
RN
Operating Network
IRSS
FDSN
MPSI0.71271.1a

P2017/03/31 11:21:16.2-2.2

T



GFZ
DJA
∅
TOLI20.8012.7m

Pn2017/03/31 11:21:18.4-0.8

T



NEIR
∅
∅
TOLI20.8012.7a

P2017/03/31 11:21:18.4-0.8

T



GFZ
∅
∅
MRSI1.3483.5a

P2017/03/31 11:21:25.1-0.1

T



GFZ
DJA
∅
SMSI1.8869.4a

P2017/03/31 11:21:31.6-0.3

T



GFZ
∅
∅
GTOI2.4382.6a

P2017/03/31 11:21:37.9-1.0

T



GFZ
∅
∅
LUWI2.56122.1a

P2017/03/31 11:21:41.00.3

T



KAN
DJA
∅
LUWI2.56122.1m

Pn2017/03/31 11:21:41.10.4

T



NEIR
DJA
∅
SMKI3.49257.3a

P2017/03/31 11:21:52.3-0.7

T



GFZ
∅
∅
BKB4.01247.0m

Pn2017/03/31 11:21:58.7-1.4

T



NEIR
DJA
∅
BKB4.01247.0a

P2017/03/31 11:21:58.8-1.3

T



GFZ
DJA
∅
PMSI4.16204.0a

P2017/03/31 11:22:01.8-0.4

T



GFZ
∅
∅
SPSI4.35191.1a

P2017/03/31 11:22:04.0-0.6

T



GFZ
DJA
∅
KKSI4.59166.8a

P2017/03/31 11:22:06.9-1.0

T



GFZ
∅
∅
MYLDM5.27336.5m

Pn2017/03/31 11:22:18.11.0

T



NEIR
KLM
∅
MYLDM5.27336.5a

P2017/03/31 11:22:18.31.2

T

2917.40.80
GFZ
KLM
∅
KAPI5.38189.1m

Pn2017/03/31 11:22:17.8-0.7

T



NEIR
DJA
∅
KAPI5.38189.1a

P2017/03/31 11:22:18.2-0.3

T

1688.70.80
GFZ
DJA
∅
BKSI5.63184.9a

P2017/03/31 11:22:20.9-1.1

T

1424.60.60
GFZ
DJA
∅
MTKI5.85257.6a

P2017/03/31 11:22:23.7-1.3

T

1874.50.80
GFZ
∅
∅
SANI5.88113.7a

P2017/03/31 11:22:23.6-1.8

T

898.01.10
GFZ
∅
∅
SGSI5.9555.8a

P2017/03/31 11:22:25.2-1.2

T

832.50.60
GFZ
DJA
∅
BSSI6.43181.0a

P2017/03/31 11:22:32.7-0.2

T

645.10.80
GFZ
∅
∅
BBKI6.89236.8a

P2017/03/31 11:22:38.0-1.1

T

1085.20.80
GFZ
DJA
∅
LBMI6.9797.9a

P2017/03/31 11:22:39.4-0.8

T

844.31.20
GFZ
DJA
∅
KKM7.18322.4m

Pn2017/03/31 11:22:43.30.1

T



NEIR
KLM
∅
KKM7.18322.4a

P2017/03/31 11:22:43.70.5

T

677.10.60
GFZ
KLM
∅
OBMI7.24103.2a

P2017/03/31 11:22:42.8-1.0

T

546.40.90
GFZ
∅
∅
NLAI7.40118.6a

P2017/03/31 11:22:47.41.4

T

2577.80.90
GFZ
DJA
∅
DAV8.3536.4m

Pn2017/03/31 11:22:58.7-0.2

T



NEIR
QCP
∅
DAV8.3536.4a

P2017/03/31 11:23:00.92.0

T

1181.60.70
GFZ
QCP
∅
AAI8.58117.8a

P2017/03/31 11:23:04.82.8

T

2150.20.80
GFZ
DJA
∅
AAII8.58117.8a

P2017/03/31 11:23:04.92.9

T

1294.30.80
GFZ
∅
∅
KRAI8.59115.0a

P2017/03/31 11:23:03.91.7

T

1178.40.80
GFZ
∅
∅
SBUM8.66284.2m

Pn2017/03/31 11:23:02.0-1.1

T



NEIR
KLM
CH
SBUM8.66284.2a

P2017/03/31 11:23:03.60.5

T

467.71.40
GFZ
KLM
CH
MMRI9.06169.7m

Pn2017/03/31 11:23:07.8-0.7

T



NEIR
DJA
∅
MMRI9.06169.7a

P2017/03/31 11:23:08.1-0.4

T

166.11.30
GFZ
DJA
∅
MSAI9.09113.7a

P2017/03/31 11:23:11.12.1

T

86.20.60
GFZ
DJA
∅
PLAI9.53197.2a

P2017/03/31 11:23:15.50.6

T

305.10.90
GFZ
∅
∅
RAPI10.2594.1a

P2017/03/31 11:23:24.90.1

T

441.30.90
GFZ
∅
∅
ATNI10.27155.7a

P2017/03/31 11:23:25.70.6

T

195.60.60
GFZ
∅
∅
ABJI10.28218.1a

P2017/03/31 11:23:26.71.6

T

105.31.30
GFZ
DJA
∅
KSM10.37276.4a

P2017/03/31 11:23:26.3-0.1

T

454.02.00
GFZ
KLM
∅
KSM10.37276.4m

Pn2017/03/31 11:23:26.80.4

T



NEIR
KLM
∅
DNP10.44210.9a

P2017/03/31 11:23:29.21.8

T

1489.81.80
GFZ
DJA
∅
BNDI10.47117.5a

P2017/03/31 11:23:29.82.0

T

2461.01.10
GFZ
DJA
∅
BASI10.48180.2a

P2017/03/31 11:23:28.60.7

T

496.41.20
GFZ
∅
∅
BYJI10.54216.2a

P2017/03/31 11:23:31.73.1

T

555.41.60
GFZ
DJA
∅
IGBI10.60210.8a

P2017/03/31 11:23:30.71.3

T

631.21.60
GFZ
DJA
∅
BLJI10.65221.0a

P2017/03/31 11:23:27.9-2.2

T

130.81.00
GFZ
DJA
∅
SOEI10.67160.1m

Pn2017/03/31 11:23:32.82.3

T



NEIR
DJA
∅
SOEI10.67160.1a

P2017/03/31 11:23:34.64.1

T

512.11.00
GFZ
DJA
∅
SIJI10.7896.5a

P2017/03/31 11:23:30.3-1.5

T

196.10.70
GFZ
∅
∅
GRJI10.85228.3a

P2017/03/31 11:23:33.10.3

T

360.71.30
GFZ
DJA
∅
JAGI10.86216.2m

Pn2017/03/31 11:23:33.80.8

T



NEIR
DJA
∅
JAGI10.86216.2a

P2017/03/31 11:23:33.80.8

T

481.72.10
GFZ
DJA
∅
GMJI11.14219.7a

P2017/03/31 11:23:37.20.4

T

151.11.20
GFZ
DJA
∅
NGJI11.91229.9a

P2017/03/31 11:23:49.01.9

T

321.02.20
GFZ
DJA
∅
SWJI11.92227.6a

P2017/03/31 11:23:48.00.7

T

248.70.70
GFZ
∅
∅
PWJI12.09226.4a

P2017/03/31 11:23:50.00.6

T

105.50.70
GFZ
DJA
∅
FAKI12.09105.5m

Pn2017/03/31 11:23:47.7-1.8

T



NEIR
DJA
∅
FAKI12.09105.5a

P2017/03/31 11:23:47.7-1.8

T

214.41.20
GFZ
DJA
∅
SMRI12.52234.0m

Pn2017/03/31 11:23:55.0-0.2

T



NEIR
DJA
∅
SMRI12.52234.0a

P2017/03/31 11:23:56.10.9

T



KAN
DJA
∅
UGM12.98230.6a

P2017/03/31 11:24:01.9-1.8

T



KAN
∅
∅
UGM12.98230.6m

Pn2017/03/31 11:24:02.81.6

T



NEIR
∅
∅
YOGI13.09231.6a

P2017/03/31 11:24:04.6-2.5

T

433.90.90
GFZ
DJA
∅
SAUI13.50128.0m

Pn2017/03/31 11:24:09.21.2

T



NEIR
DJA
∅
SAUI13.50128.0a

P2017/03/31 11:24:09.4-4.2

T

741.31.10
GFZ
DJA
∅
MWPI13.5195.3a

P2017/03/31 11:24:09.2-4.5

T

225.41.00
GFZ
∅
∅
CTJI13.54237.2a

P2017/03/31 11:24:09.5-4.6

T

241.12.20
GFZ
∅
∅
RKPI13.7197.7a

P2017/03/31 11:24:15.5-0.5

T

155.80.80
GFZ
∅
∅
KPJI13.92236.6a

P2017/03/31 11:24:14.7-3.7

T

454.70.70
GFZ
DJA
∅
JCJI14.06241.0a

P2017/03/31 11:24:18.4-1.5

T

300.91.70
GFZ
DJA
∅
CMJI14.57236.1a

P2017/03/31 11:24:23.1-2.4

T

722.00.70
GFZ
DJA
∅
BBJI15.08238.8a

P2017/03/31 11:24:29.2-2.0

T

419.80.70
GFZ
∅
∅
CBJI15.29243.8a

P2017/03/31 11:24:32.6-0.9

T

282.11.70
GFZ
DJA
∅
KLI16.57251.7a

P2017/03/31 11:24:47.1-0.6

T

285.20.90
GFZ
DJA
∅
DLV16.69314.3a

P2017/03/31 11:24:48.1-1.2

T

54.11.90
GFZ
PLV
∅
MTN16.76141.8a

P2017/03/31 11:24:50.10.4

T

598.41.60
GFZ
AUST
∅
MYKOM16.84275.1a

P2017/03/31 11:24:49.5-1.1

T

295.91.60
GFZ
KLM
∅
JMBI17.09263.4a

P2017/03/31 11:24:55.11.7

T

107.00.80
GFZ
∅
∅
KASI17.12249.9a

P2017/03/31 11:24:55.51.7

T

385.20.90
GFZ
DJA
∅
LWLI17.38252.0a

P2017/03/31 11:24:58.82.1

T

540.70.70
GFZ
∅
∅
KDU17.50138.1a

P2017/03/31 11:24:57.7-0.3

T



KAN
AUST
∅
KNRA17.84153.5a

P2017/03/31 11:25:01.80.1

T

335.71.20
GFZ
AUST
∅
SLSI18.23261.4a

P2017/03/31 11:25:06.30.4

T

178.51.60
GFZ
∅
∅
MNAI18.26255.0a

P2017/03/31 11:25:09.22.9

T

489.30.60
GFZ
DJA
∅
SMPI18.2797.3a

P2017/03/31 11:25:10.03.7

T

116.01.50
GFZ
DJA
∅
MASI18.70259.2a

P2017/03/31 11:25:12.81.7

T

351.31.10
GFZ
∅
∅
UBSI18.79257.3a

P2017/03/31 11:25:13.51.5

T

325.90.70
GFZ
∅
∅
SDSI19.24266.3a

P2017/03/31 11:25:17.40.5

T

185.41.50
GFZ
DJA
∅
MKBI19.58261.8a

P2017/03/31 11:25:21.10.5

T

463.61.80
GFZ
∅
∅
BKNI19.59270.1a

P2017/03/31 11:25:22.92.2

T

327.51.40
GFZ
DJA
∅
GENI19.7998.5a

P2017/03/31 11:25:24.51.6

T

122.80.80
GFZ
∅
∅
IPM20.01282.2a

P2017/03/31 11:25:26.10.7

T

251.01.30
GFZ
KLM
∅
PDSI20.20266.5a

P2017/03/31 11:25:28.00.6

T

406.00.70
GFZ
∅
∅
KULM20.55284.3a

P2017/03/31 11:25:31.40.3

T

231.31.40
GFZ
KLM
∅
PPSI20.84261.4a

P2017/03/31 11:25:34.50.3

T

522.00.70
GFZ
DJA
∅
SKLT21.08289.3a

P2017/03/31 11:25:37.20.4

T

163.81.50mb 5.1
GFZ
∅
∅
MBWA21.39182.2a

P2017/03/31 11:25:39.6-0.5

T

138.21.90mb 5.0
GFZ
AUST
∅
PSA0021.80181.9m

P2017/03/31 11:25:42.7-1.8

T



NEIR
∅
∅
TWG22.391.1m

P2017/03/31 11:25:51.50.8

T



NEIR
TATO
∅
SRIT22.50292.0m

P2017/03/31 11:25:52.10.2

T



NEIR
∅
∅
HKPS22.73344.3m

P2017/03/31 11:25:54.90.6

T



NEIR
∅
∅
TPUB22.860.1m

P2017/03/31 11:25:57.92.3

T



NEIR
TATO
∅
YULB22.961.6a

P2017/03/31 11:25:56.80.3

T

109.81.00mb 5.1
GFZ
TATO
∅
KCSI23.07278.2a

P2017/03/31 11:25:56.6-0.8

T

178.21.50mb 5.2
GFZ
∅
∅
GSI23.08272.6a

P2017/03/31 11:25:56.6-0.9

T

556.40.60mb 6.1
GFZ
DJA
∅
SSLB23.350.8a

P2017/03/31 11:26:02.22.1

T

107.91.30mb 5.1
GFZ
TATO
∅
NACB23.752.2m

P2017/03/31 11:26:04.40.7

T



NEIR
TATO
∅
LHMI24.15282.1a

P2017/03/31 11:26:08.41.1

T

351.91.10mb 5.7
GFZ
DJA
∅
YHNB24.241.7a

P2017/03/31 11:26:08.40.2

T

131.51.60mb 5.1
GFZ
TATO
∅
WRA24.25147.0m
iP2017/03/31 11:26:06.8-1.5

T



GSRC
CAN
∅
MLSI24.52279.6a

P2017/03/31 11:26:10.4-0.3

T

200.70.80mb 5.6
GFZ
∅
∅
ASAR27.15152.4a

P2017/03/31 11:26:33.4-1.1

T



NEIR
AUST
∅
CMAR27.91311.5m
iP2017/03/31 11:26:42.31.1

T



GSRC
OBN
∅
CMAR27.91311.5a

PcP2017/03/31 11:29:54.4-0.1

T



NEIR
OBN
∅
CHTO28.13312.1m

P2017/03/31 11:26:44.00.8

T

0.80.80
NEIR
BKK
∅
CHTO28.13312.1m

PcP2017/03/31 11:29:55.60.5

T

0.80.80
NEIR
BKK
∅
PMG28.18110.8m

P2017/03/31 11:26:42.8-0.7

T

115.80.90mb 5.5
NEIR
PMG
∅
OOD31.51153.8a

P2017/03/31 11:27:12.4-0.6

T



KAN
∅
∅
FORT31.76167.7a

P2017/03/31 11:27:13.8-1.4

T



KAN
AUST
∅
RABL31.8998.4a

P2017/03/31 11:27:17.61.4

T

483.10.70mb 6.3
NEIR
AUST
∅
CTA32.32130.4a

P2017/03/31 11:27:20.30.2

T



KAN
BRS
∅
CTAO32.32130.4m

P2017/03/31 11:27:20.70.6

T

68.81.05mb 5.3
NEIR
BRS
∅
JSU32.4115.8m

P2017/03/31 11:27:20.8-0.2

T

41.40.90mb 5.2
NEIR
JMA
∅
MULG33.05158.3a

P2017/03/31 11:27:25.6-0.9

T



KAN
∅
∅
NWAO33.25185.2m

P2017/03/31 11:27:27.8-0.5

T

335.90.85mb 6.2
NEIR
AUST
∅
JCJ33.7736.2a

P2017/03/31 11:27:31.3-1.4

T



KAN
∅
∅
JNU34.0615.5a

P2017/03/31 11:27:36.20.9

T



BUD
JMA
∅
QLP35.16141.4a

P2017/03/31 11:27:45.00.3

T



KAN
AUST
∅
JHS36.4517.4m

P2017/03/31 11:27:55.5-0.3

T

50.81.00mb 5.4
NEIR
JMA
∅
TJN36.449.2mdeP2017/03/31 11:27:56.40.7

T



GSRC
∅
∅
WHYH36.86155.9a

P2017/03/31 11:27:58.7-0.5

T



KAN
∅
∅
SHL37.43314.4m

P2017/03/31 11:28:04.30.1

T

45.80.88mb 5.4
NEIR
NDI
∅
INCN37.427.9a

P2017/03/31 11:28:05.61.6

T

39.40.95mb 5.3
NEIR
SEO
∅
SHL37.43314.4m

PcP2017/03/31 11:30:20.9-0.1

T

45.80.88
NEIR
NDI
∅
KSAR37.579.5m

P2017/03/31 11:28:05.60.4

T



NEIR
USAF
∅
STKA37.72150.1m

P2017/03/31 11:28:06.1-0.4

T

59.20.90mb 5.5
NEIR
AUST
∅
TWOA39.01156.3a

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Sonntag, 19. März 2017

US-GEHEIMDIENSTE

CIA, NSA, NRO, NGA, DIA, DNI:

US-Geheimdienste im Überblick 

Der mächtige graue Staat der USA

Was macht der Geheimdienstdirektor? Wer steuert die Satelliten? Das Netzwerk der US-Geheimdienste ist groß. Ein Überblick.
Von Oliver Hollenstein


U.S. Director of National Intelligence Clapper arrives to testify at a House Intelligence Committee hearing in WashingtonBild: REUTERS

Was macht der Geheimdienstdirektor? Wer steuert die Satelliten? Das Netzwerk der US-Geheimdienste ist groß. Süddeutsche.de stellt sie vor.

Als Lehre aus den Anschlägen vom 11. September 2001 haben die USA 2004 in einer großen Geheimdienstreform den Posten des Director National Intelligence (Direktor der Nachrichtendienste) geschaffen. Aktuell ist das James Clapper (Foto).
Vor der Reform war der CIA-Chef der oberste US-Agent, dann sollte der DNI mit einer eigenen Behörde, dem Office of Director National Intelligence (ODNI), die anderen Geheimdienste beaufsichtigen und koordinieren. Zudem ist der DNI der oberste Geheimdienstberater des Präsidenten und zuständig für dessen tägliches Sicherheitsbriefing.
Laut geheimen Papieren aus dem Fundus des Whistleblowers Edward Snowden, dem sogenannten Black Budget, verfügt das ODNI über ein Budget von 1,7 Milliarden Dollar. Das ist fast dreieinhalb Mal so viel wie bei der Errichtung der Behörde im Jahr 2004. Innerhalb des DNI gibt es verschiedene Abteilungen, die sich um die Koordination der Dienste kümmern: So werden etwa die Terrorismusbekämpfungs-Aktivitäten der Geheimdienste in einem National Counterterrorism Center (NCTC) gesammelt; das National Intelligence Council (NIC) ist für die strategische Weiterentwicklung der Geheimdienste zuständig; auch die Spionageabwehr wird hier koordiniert.
Kritiker sagen, dass der DNI trotz seines umfangreichen Budgets keine Übersicht über die Tätigkeiten der einzelnen Geheimdienste hat - und es dadurch viele doppelte Tätigkeiten gebe.
16. November 2013, 16:302013-11-16 16:30:51 © SZ.de/bbr


Donnerstag, 9. März 2017

ESA/ESRIN

ESA > About Us > ESRIN
International Charter Space & Major Disasters Logo
 
The wealth of Earth Observation data for which ESA is responsible has led to its becoming a founder, and major player, in the International Charter on Space and Natural Disasters. The Charter is a joint effort between member space agencies to place their satellite resources at the disposal of rescue authorities in the event of disasters of both human or natural origin.
An operator is on 24-hour call at ESRIN ready to deal with requests for assistance from civil protection authorities. On receiving a request, they check the identity of the caller and verify that the information needed to respond to the emergency is specified correctly.
This information is then passed by the operator to an on-call officer who analyses the request and the scope of the disaster with the user to establish how to use the satellites that can provide data to the charter to their best abilities. The final step is to prepare an acquisition and processing plan using the available space resources.
Data acquisition and delivery takes place on an emergency basis, and a project manager, qualified in data ordering, handling and application, assists the user throughout the process.
Last update: 26 August 2005

Freitag, 3. März 2017

BOXING DAY TSUNAMI 2004 THAILAND

V: THAILAND TSUNAMI 2004

V: THAILAND TSUNAMI 2004 | RAW FOOTAGE


Veröffentlicht am 23.12.2014
This deadliest tsunami 2004 caused by a 9.0 magnitude earthquake, killing more than 250,000 people in a single day is the most devastating tsunami in modern times, traveled 375 miles (600 km) in a mere 75 min. That’s 300 miles (480 km) per hour, leaving more than 1.7 million homeless affecting 18 countries. Tsunami is an ever-present and real threat for the these islands of the Indian Ocean due to the presence of a tectonic interactive plate. These reviews may help national, regional, and international organizations to prevent such events from occurring again in the future.

The December 2004 earthquake released about enough energy to power the United States for six months, or put another way, it generated the equivalent of a 250-megaton bomb shaking every point of the earth an inch or more. The associated shifts in the ocean floor displaced enough water to fill a tank 1.6 kilometers wide, 1.6 kilometers high and more than 11 kilometers long. The Los Angeles Times reported: “Miles beneath the waters of the Indian Ocean, a massive piece of the Earth’s crust had heaved, buckled and shifted. Along a fracture zone hundreds of miles long, it moved, releasing pent-up energy equivalent to the power of more than 1,000 atomic bombs. The waters above reared up and crashed down, creating a wave that was now racing across the ocean at 500 mph…The records of history and evidence encoded in coral reefs show that tsunamis have hit the Indian Ocean seldom but with great force.”

The 2004 Indian Ocean earthquake was an undersea megathrust earthquake that occurred at 00:58:53 UTC on Sunday, 26 December 2004, with an epicentre off the west coast of Sumatra, Indonesia. The quake itself is known by the scientific community as the Sumatra–Andaman earthquake. The resulting tsunami was given various names, including the 2004 Indian Ocean tsunami, South Asian tsunami, Indonesian tsunami, the Christmas tsunami and the Boxing Day tsunami.

The earthquake was caused when the Indian Plate was subducted by the Burma Plate and triggered a series of devastating tsunamis along the coasts of most landmasses bordering the Indian Ocean, killing 230,000 people in fourteen countries, and inundating coastal communities with waves up to 30 metres (100 ft) high. It was one of the deadliest natural disasters in recorded history. Indonesia was the hardest-hit country, followed by Sri Lanka, India, and Thailand.

With a magnitude of Mw 9.1–9.3, it is the third-largest earthquake ever recorded on a seismograph. The earthquake had the longest duration of faulting ever observed, between 8.3 and 10 minutes. It caused the entire planet to vibrate as much as 1 centimetre (0.4 inches) and triggered other earthquakes as far away as Alaska. Its epicentre was between Simeulue and mainland Indonesia. The plight of the affected people and countries prompted a worldwide humanitarian response. In all, the worldwide community donated more than $14 billion (2004 US$) in humanitarian aid.

Because of the distances involved, the tsunami took anywhere from fifteen minutes to seven hours to reach the coastlines. The northern regions of the Indonesian island of Sumatra were hit very quickly, while Sri Lanka and the east coast of India were hit roughly 90 minutes to two hours later. Thailand was struck about two hours later despite being closer to the epicentre, because the tsunami traveled more slowly in the shallow Andaman Sea off its western coast.