Transcript ppt

Earthquake Information
European-Mediterranean Seismological Centre
Summary:
Magnitude
Mw 8.0
Region
NEAR COAST OF CENTRAL PERU
Date time
2007-08-15 at 23:40:57.2 UTC
Location
13.28 S ; 76.74 W
Depth
40 km
Distances
67 km W Chincha alta (pop 153,076 ; local time 18:40 2007-08-15)
42 km SW San vicente de cañete (pop 25,517 ; local time 18:40 2007-0815)
Credit EMSC
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Taiwan
Credit EMSC
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全球的岩石圈之主要大板塊
MAJOR TECTONIC PLATES OF THE WORLD
歐亞板塊
Eurasian
北美板塊
North American
加勒比海板塊
Caribbean
太平洋板塊
Pacific
非洲板塊
African
20070815’s quake
南美板塊
South American
納薩卡板塊
Nazca
菲律賓板塊
Philippines
太平洋板塊
Pacific
印度-澳洲板塊
Indian/Australian
南極板塊
Antarctica
Peru, like much of the west coast of North and South America, lies above an area of intense seismic activity and is
no stranger to earthquakes. The nearby Nazca tectonic plate, which lies under the Pacific Ocean, is forced
underneath the South American continental plate at a rate of about 4 cm a year. That may not sound a lot but it is
enough to put huge strain on the earth's crust. The pressures are periodically released through earthquakes.
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'The earth was like jelly' - hundreds die in Peru quake, but Lima escapes
Scientists said the quake was a "megathrust" - the largest of earthquakes - similar to the Indian Ocean
temblor in 2004 that generated a deadly tsunami.
At least 200 people in the town of Pisco were reported trapped under a church which caved in during a
service. "So much effort and our city is destroyed," the town's mayor, Mendoza Uribe, told local radio.
About 70% of the port city of 60,000 people had been levelled, he said, weeping. "We don't have lights,
water, communications. Most houses have fallen, churches, stores, hotels, everything is destroyed."
Witnesses from the nearby town of Chincha said there were at least 30 bodies at the badly damaged hospital.
With the weather being cold many of the homeless appealed for blankets.
Damage to the city and province of Ica was "dramatic", according to the deputy health minister, José
Calderón.
The government declared a state of emergency in the affected areas, appealed for blood donations and
mobilised thousands of police, soldiers and medical staff. It promised an "air bridge" to shuttle the most
badly injured to Lima.
Hospital doctors called off a planned strike. Telephone companies appealed to people to make emergency
calls only.
A quarter of Ica's buildings were said to have collapsed and several churches were badly damaged, with local
media reporting that in one church falling masonry killed 17 worshippers.
At least 57 bodies were brought to the morgue, and injured people crowded into a hospital which resembled
a war zone, with blood on the floor, screaming children and overwhelmed medical staff, according to
reports.
Rory Carroll, Latin America correspondent
Friday August 17, 2007
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Yesterday, Peru's national disaster management authority estimated at least 450 were dead and 1,500 injured.
The Red Cross said the toll was expected to rise.
However the doomsday scenario did not happen: Lima, a vast metropolis of poorly built concrete which has
suffered cataclysmic earthquakes in the past, shook violently but escaped with minor damage and only one
recorded death.
"It made waves and the earth was like jelly," Antony Falconi, 27, told the Associated Press. "Who isn't going
to be frightened? The Earth moved differently this time." Another Lima resident, María Pilar Mena, 47, said
it was the strongest tremor she had ever felt. "When the quake struck, I thought it would never end."
The US Geological Survey said the epicentre was beneath the Pacific coast about 90 miles south-east of the
capital. Four strong aftershocks ranging from 5.4 to 5.9 followed, the organisation said.
In 1970 a 7.9-magnitude earthquake in the Andes north of Lima triggered a landslide which buried the
town of Yungay, killing up to 66,000 people.
Many people were forced to
spend the night in local parks.
Photograph: Karel Navarro/AP
Rory Carroll, Latin America correspondent
Friday August 17, 2007
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Research animations of the August 15, 2007 Peru tsunami propagation created with
experimental runs of the MOST tsunami forecast model and including DART™ buoy data.
Yellow squares indicate DART™ buoy locations. Click the image to animate (left) or enlarge
(right).
The animation and graphic display qualitative and quantitative information about the tsunami propagation
including tsunami wave interaction with ocean floor bathymetric features, and neighboring coastlines. The
tsunami radiation pattern is indicated with color coded information about the maximum wave amplitude at
different locations throughout the Pacific Ocean.
The timer and moving yellow squares indicate time elapsed since time of the earthquake, providing an
estimate of tsunami arrival time at different locations (left).
credit NOAA / PMEL / Center for Tsunami Research
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Peru Earthquake (8/15/2007)
Animation of the tsunami propagation over the Pacific Ocean.
USC modeled the first 2 hours of the tsunami waves showing an energy distribution with a
predominantly SSW orientation.
Maximum wave height
distribution 10 hours after
the earthquake in the
vicinity of Peru.
Credit Tsunami Research Center, University of Southern California
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The particle velocities recorded at 101B (near Taipei 101) with a depth of 100 meters
EW
NS
V
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10 min.