Tampilkan postingan dengan label Earthquake. Tampilkan semua postingan
Tampilkan postingan dengan label Earthquake. Tampilkan semua postingan

Selasa, 22 Maret 2011

JAPAN TOHOKO EARTHQUAKE

JAPAN TOHOKO EARTHQUAKE

JAPAN EARTHQUAKE 2011 literally in wikipedia called “The 2011 Tōhoku earthquake and tsunami” was a 9.0-magnitude megathrust earthquake off the coast of Japan that occurred at 14:46 JST (local time) on Friday 11 March 2011, followed by a severely destructive tsunami. Epicenter was 130 km of the east coast Peninsula Tohoku near Sendai (wikipedia.com).



Tectonic Summary
Occurred as thrust faulting on or near the subduction zone interface plate boundary between the Pacific and North America plates. The Pacific plate thrusts underneath Japan at the Japan Trench, and dips to the west beneath Eurasia.This thrust faulting associated with subduction along this plate boundary (Jorge en, 2011). Acording to Ross Stein : Blok 400 km length, vertically thrusting 0.6 m, while Pacific Plate moved 20 meters until 40 m to Westward with 100km width. One of the biggest faulting connected to Earthquake.




Scientific data about the earthquake, from USGS




Pic Sources USGS

11/03/11 5:46:23

Epicenter: 38.321 142.369

MW 8.9

USGS/WPHASE CENTROID MOMENT TENSOR

11/03/11 05:46:23.00

Centroid: 37.321 141.769

Depth 24 No. of sta: 89

Moment Tensor; Scale 10**22 Nm

Mrr= 1.16 Mtt= 0.18

Mpp=-1.34 Mrt= 1.33

Mrp= 2.17 Mtp=-0.10

Principal axes:

T Val= 2.88 Plg=55 Azm=313

N = -0.08 11 205

P = -2.79 32 108

Best Double Couple:Mo=2.8*10**22

NP1:Strike=162 Dip=17 Slip= 45

NP2: 28 78 102

Sources : http://earthquake.usgs.gov/earthquakes/eqinthenews/2011/usc0001xgp/#details



Date 14:46:23, 11 March 2011 (+09:00)
Duration 6 minutes Magnitude 9.0 MW Depth 32 km (19.9 mi)
Epicenter location :
38°19′19″N 142°22′08″E/38.322°N 142.369°E

(Tsunami).
Total damage Flooding, landslides, fires, building and infrastructure damage, nuclear incidents Peak ground acceleration 2.99 g (vector sum)
Tsunami Yes
Landslides Yes
Foreshocks 7+ (4+ above 6.0 MW)
Aftershocks 656+ (44+ above 6.0 MW)
Casualties: 8,928 deaths, 2,628 injured, 12,664 people missing (all figures preliminary)

Library Sources:

Jorge en “Honshu earthquake and tsunami in Japan, 8.9 Mw “ at http://www.structuralgeology.org/2011/03/honshu-earthquakein-japan-89-mw.html

Wikipedia

BGS at http://www.bgs.ac.uk/research/highlights/earthquakes/honshuMarch2011.html

USGS



Video :

http://www.youtube.com/watch?feature=player_embedded&v=LU_QTr5-eTU
BGS marine geologist Prof Dave Tappin interviewed by BGS minerals geologist Clive Mitchell.
They discuss what conditions are necessary for a tsunami to occur,
how far it may travel and what size the wave height may reach.



http://www.youtube.com/watch?feature=player_embedded&v=7Ij-EW7EBuI
BGS seismologist Dr Brian Baptie compares recent earthquakes from Haiti 2010 (7.1),
Christchurch, New Zealand 2011 (6.3) and Honshu, Japan (9.0).




http://www.youtube.com/watch?feature=player_embedded&v=I4M6OX16Yco
Dr David Kerridge, BGS, explains how they recorded the recent earthquakes in Japan.
The seismic waves take about 10-12 minutes to arrive at our
Edinburgh-based seismometers from their source off the coast of Japan.


Link Pictures before and after tsunami :
http://www.abc.net.au/news/events/japan-quake-2011/beforeafter.htm

Minggu, 18 Oktober 2009

September-October 2009 Large Earthquake in Indonesia Plus Field Important Information Map Equipment on This Area


  1. September-October 2009 Large Earthquake in Indonesia
  2. Plus Field Important Information Equipment on This Area
1. Large 7,6 SR Earthquake in West Sumatra Province Indonesia

A. News Source from ESDM News

Location:










The Earthquake Disaster in Padang Indonesia at September 29th-30th 2009, has main earthquake 7,6 SR and the next following earthquake in 6,2 SR. As a Fact this earthquake didn't followed by a tsunami (overlarge wave) disaster.

From DESDM Institution announced this earthquake happened because subduction (in area of crash zone from two big plate tectonic) of Indonesian Sea Plate (Australian Plate) under Asian Plate which located along West Coast of Sumatra Island, according USGS it's in subduction zone between Australian Plate and Sunda Plate. (note this Formation of collide is Subduction Form because the two plate which is Sea Plate and Continent Plate, has a Large Differentiation of Density between them. The lower density plate later subducts under the higher density plate).

This Earthquake didnot have ability to produce Tsunami because the epicentre (earthquake source point) deep enought location, and as the result didn't produce Large Power to made a tsunami.

Information from Indonesian Meterolog, Climate and Geophysist Institution (BMKG), this earthquake appeared in afternoon (30/9), at 17:16:09 WIB in 7,6 Scala Richter (SR). Epicentre (earthquke source point) layed on coordinate 0.84 LS - 99.65 BT, 71 Km depth from water sea level, 57 Km far from South West Pariaman, Sumatera Barat. The Second (following) earthquake
appear 22 minutes later, on 17:38:52 WIB in 6,2 SR, Epicentre location on 72 LS - 99.94 BT, at 110 Km depth, 22 Km SouthWest Pariaman, Sumatera Barat.


Other Large Earthquke in September - October in Island Arc Java-Sumatra is on Sukabumi South Java and Later in Sunday October 17th 2009 at Ujung Kulon, Sunda Strait. Both of them caused by Tectonic Plate movement.

see more informations about West Padang Earthquake from The Field in:
http://www.theage.com.au/world/second-quake-hits-sumatra-as-death-toll-soars-20091001-gd43.html

B.USGS Report Padang earthquake

Earthquake Details

Magnitude7.6
Date-Time
Location 0.725°S, 99.856°E
Depth81 km (50.3 miles) set by location program
RegionSOUTHERN SUMATRA, INDONESIA
Distances60 km (35 miles) WNW of Padang, Sumatra, Indonesia
225 km (140 miles) SW of Pekanbaru, Sumatra, Indonesia
470 km (295 miles) SSW of KUALA LUMPUR, Malaysia
975 km (600 miles) NW of JAKARTA, Java, Indonesia
Location Uncertaintyhorizontal +/- 4.2 km (2.6 miles); depth fixed by location program
ParametersNST=405, Nph=405, Dmin=534.3 km, Rmss=0.92 sec, Gp= 18°,
M-type=teleseismic moment magnitude (Mw), Version=A
Source
  • USGS NEIC (WDCS-D)
Event IDus2009mebz

From USGS Report (write as in original text) about Padang Earthquake September 30th 2009

Felt Reports

At least 1100 people were killed, 2181 were injured and thousands are still unaccounted for in the Padang area. More than 2650 buildings have been damaged in the area and landslides have disrupted power and communications. Felt (VII) at Padang. Widely felt throughout Sumatra and Java, Indonesia, Malaysia, Singapore and Thailand. A small local tsunami with wave heights of 27 centimeters (amplitude measured relative to normal sea level) was generated.

Tectonic Summary

The southern Sumatra earthquake of September 30, 2009 occurred as a result of oblique-thrust faulting near the subduction interface plate boundary between the Australian and Sunda plates. At the location of this earthquake, the Australian Plate moves north-northeast with respect to the Sunda plate at a velocity of approximately 60 mm/yr. On the basis of the currently available fault mechanism information and earthquake depth of 80 km, it is likely that this earthquake occurred within the subducting Australian Plate rather than on the plate interface itself. The recent earthquake was deeper than typical subduction thrust earthquakes that generally occur at depths less than 50 km. The subduction zone surrounding the immediate region of this event has not witnessed a megathrust earthquake in the recent past, rupturing last in an earthquake of M 8.5 or larger in 1797. Approximately 350 km to the south, a 250 km section of the plate boundary slipped during an Mw 8.4 earthquake in September 2007, while approximately 300 km to the north, a 350 km section slipped during the Mw 8.7 earthquake of March 2005. In early 2008, the plate boundary updip of today’s earthquake was active in a sequence of Mw 5-6 earthquakes. It is not clear how today’s earthquake is related to the sequence of megathrust subduction zone events on the shallower section of the plate boundary.



2. Important Maps to Equipt if you want to go to Padang Earthquake area in Indonesia

With the exception of public UN sources, reproduction or redistribution of the above text, in whole, part or in any form, requires the prior consent of the original source.

For Fund emergency Disaster conect to UNOCHA.

Your Important maps to equipt in Padang............

1. Map from reliefweb "The Temporary Map about region Damage because disaster in Padang Source Ocha, Reliefweb, and rovicky.wordpress.com and

2. Map from USG Humanitarian Assistance to Indonesia Earthquake, September 30th, 2009

Klick on Image

Small view

3. Indonesia: Population Map – Padang North [with building damages] (as of 01 Oct 2009)

klick on image

4. Potential Building Damage
Source(s):
- German Aerospace Center (DLR)
- International Charter Space and Major Disasters
Klick:
Potential Buiding Damage

5. Free Bakorsurtanal Earthquake Location Maps (Basic Maps of The Location)


http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0614.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0712.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0713.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0714.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0715.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0716.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0812.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0813.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0814.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0815.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0816.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0913.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0914.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/0915.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/1013.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/1014.jpg
http://www.bakosurtanal.go.id/upl_images/gempasumbar2009/rbi250k/1015.jpg