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The depth effect of earthquakes on tsunami
The depth effect of earthquakes on tsunami

Workshop 2012 slides lecture
Workshop 2012 slides lecture

... California State University, Sacramento ...
Computing Earthquake Probabilities on Global Scales
Computing Earthquake Probabilities on Global Scales

Plate-wide deformation before the Sumatra
Plate-wide deformation before the Sumatra

IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG)
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG)

conditional probabilities of occurrence of moderate earthquakes in
conditional probabilities of occurrence of moderate earthquakes in

... It is necessary to understand the physical process going on underneath before we try to assess the seismic hazard. Tectonic framework of the Indian subcontinent covering an area of about 3.2 million sq. km is spatio-temporally varied and complex. As a pre requisite for the seismic hazard studies, th ...
Seismic interaction and delayed triggering along the North Anatolian
Seismic interaction and delayed triggering along the North Anatolian

IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X,
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X,

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Research on the Earthquake Disaster Thematic Electric Map

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Earthquake Prediction Model II

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A Multivariate Non-Parametric Hazard Model for Earthquake

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Shallow inland earthquakes in NE Japan possibly triggered

IDENTIFICATION OF SLIDE-GENERATED TSUNAMIS IN THE
IDENTIFICATION OF SLIDE-GENERATED TSUNAMIS IN THE

Literature review of health impact post-earthquakes
Literature review of health impact post-earthquakes

... magnitude between 6.5 and 7.4 in China are similar to earthquakes of that scale outside China.8 Most mortality occurs in the first 6 h after the earthquake. Although limited study has reported on the fate of vulnerable groups such as children and older individuals, post disaster, findings did indicate ...
Get PDF - Wiley Online Library
Get PDF - Wiley Online Library

UGRC 144_Session 3
UGRC 144_Session 3

N. Ambraseys, "Historical earthquakes in Jerusalem – A
N. Ambraseys, "Historical earthquakes in Jerusalem – A

Deaths and Injuries due to the Earthquake in Armenia: A Cohort
Deaths and Injuries due to the Earthquake in Armenia: A Cohort

Earthquake Disaster Simulation in Immersive 3D Environment
Earthquake Disaster Simulation in Immersive 3D Environment

... could be for example awareness or emergency management. It should be noted that these factors influence the formation of a pool of simulation candidates but ultimately the further steps in the process may reject any simulation candidate based on the unsuitability considering other factors. 3.2.2 Sel ...
Geological Survey of Denmark and Greenland Bulletin 31
Geological Survey of Denmark and Greenland Bulletin 31

A SITE AMPLIFICATION STUDY USING OBSERVED RECORDS AT
A SITE AMPLIFICATION STUDY USING OBSERVED RECORDS AT

Why We Need a New Paradigm of Earthquake Occurrence
Why We Need a New Paradigm of Earthquake Occurrence

Chapter 4: Igneous Rocks: Product of Earth`s Internal Fire
Chapter 4: Igneous Rocks: Product of Earth`s Internal Fire

preparing for a new view of u.s. earthquake risk
preparing for a new view of u.s. earthquake risk

< 1 2 3 4 5 6 7 8 ... 13 >

1960 Valdivia earthquake



The 1960 Valdivia earthquake (Spanish: Terremoto de Valdivia) or Great Chilean earthquake (Gran terremoto de Chile) of Sunday, 22 May 1960 was the most powerful earthquake ever recorded, rating a 9.5 on the moment magnitude scale. It occurred in the afternoon (19:11 GMT, 15:11 local time), and lasted approximately 10 minutes. The resulting tsunami affected southern Chile, Hawaii, Japan, the Philippines, eastern New Zealand, southeast Australia, and the Aleutian Islands.The epicenter was near Lumaco (see map), approximately 570 kilometres (350 mi) south of Santiago, with Valdivia being the most affected city. The tremor caused localised tsunamis that severely battered the Chilean coast, with waves up to 25 metres (82 ft). The main tsunami raced across the Pacific Ocean and devastated Hilo, Hawaii. Waves as high as 10.7 metres (35 ft) were recorded 10,000 kilometres (6,200 mi) from the epicenter, and as far away as Japan and the Philippines.The death toll and monetary losses arising from such a widespread disaster are not certain.Various estimates of the total number of fatalities from the earthquake and tsunamis have been published, with the United States Geological Survey citing studies with figures of 2,231, 3,000, or 5,700 killed and another source using an estimate of 6,000 dead. Different sources have estimated the monetary cost ranged from US$400 million to 800 million (or $3.19 billion to $6.38 billion today, adjusted for inflation).
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