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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,

Economic impacts of seismic risk
Economic impacts of seismic risk

... housing was extensive. Out of a total housing stock of approximately 220,000 homes, around 165,000 were impacted, including many that are now uninhabitable. There has also been substantial damage to commercial assets and infrastructure, particularly within Christchurch’s central business district. I ...
Souces and scenarios for tsunami hazard assessment in the
Souces and scenarios for tsunami hazard assessment in the

Azores seismogenic zones
Azores seismogenic zones

... significant differences in strain between the MAR-Terceira and Terceira-Gloria Fault. These differences recently corroborated by Bezzeghoud et al. (2014) using the total seismic moment tensor. Then, we correlate these areas with focal mechanisms, tectonic of the islands and historical seismicity. Th ...
PDF
PDF

... faults in the Azerbaijan area are mostly Cenozoic in or younger. The data presented demonstrate clearly that geological structures are commonly repeated at all scales from outcrop to regional. Several regional earthquakes have been strongly felt and caused damages in and around Tabriz during history ...
Geological Survey of Denmark and Greenland Bulletin 31
Geological Survey of Denmark and Greenland Bulletin 31

Three complementary global earthquakes catalogs were used to
Three complementary global earthquakes catalogs were used to

Auxiliary material for Regional controls on volcano seismicity along
Auxiliary material for Regional controls on volcano seismicity along

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

... is most appropriate in regions with frequent earthquakes, while the response may be highly inappropriate resulting in avoidable casualties in regions with infrequent earthquakes. This is due to better training of the human mind to recognise an earthquake and determine safety actions during an earthq ...
Vol. 20 No. 3 JANUARY 2017 ISSN:1174-3646 Editorial
Vol. 20 No. 3 JANUARY 2017 ISSN:1174-3646 Editorial

Investigation of Expected Seismic Performance on Existing Buildings: A Case Study
Investigation of Expected Seismic Performance on Existing Buildings: A Case Study

Wood-Frame Construction in Past Earthquakes
Wood-Frame Construction in Past Earthquakes

Effect of structural irregularities and short columns on
Effect of structural irregularities and short columns on

Seismic interaction and delayed triggering along the North Anatolian
Seismic interaction and delayed triggering along the North Anatolian

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

1 (a) Explain elastic rebound theory
1 (a) Explain elastic rebound theory

Seismic Assessment of Existing Buildings
Seismic Assessment of Existing Buildings

... 2. Definition of more efficient strategies of intervention; 3. Improvement of seismic strengthening solutions; 4. Formation of a legal framework for rehabilitation actions; 5. Civil and technical education and spread of information; 6. Creation of master-plans for seismic rehabilitation; ...
conditional probabilities of occurrence of moderate earthquakes in
conditional probabilities of occurrence of moderate earthquakes in

... independent seismogenic source zones having individual characteristics. These source zones were chosen on the basis of Khattri et al. (1984) in which the whole country is divided into 24 source zones. Figure 1. shows the source zones considered in the study for seismic hazard assessment. The zone I ...
Earthquake-Tsunami in South Jogjakarta Indonesia
Earthquake-Tsunami in South Jogjakarta Indonesia

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

... Paleoearthquake and fault slip‐rate data are combined with the CIT‐USGS catalog for the period 1944 to 1992 to examine the shape of the magnitude‐frequency distribution along the major strike‐slip faults of southern California. The resulting distributions for the Newport‐Inglewood, Elsinore, Garlock ...
ISNS 4359 Earthquakes and Volcanoes
ISNS 4359 Earthquakes and Volcanoes

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

4 - Earthquakes
4 - Earthquakes

A Multivariate Non-Parametric Hazard Model for Earthquake
A Multivariate Non-Parametric Hazard Model for Earthquake

0. Introduction
0. Introduction

< 1 ... 8 9 10 11 12 13 14 15 16 ... 23 >

2010 Pichilemu earthquake



The 2010 Pichilemu earthquake (Spanish: Terremoto de Pichilemu de 2010), also known as the Libertador O'Higgins earthquake, was a 6.9 MW intraplate earthquake that struck Chile's O'Higgins Region on 11 March 2010. The earthquake was centred 15 kilometres (9.3 mi) northwest of the city of Pichilemu, according to the University of Chile Seismological Service.The earthquake was caused by increased regional stress arising from an earthquake on 27 February, centered offshore Maule Region, which was felt throughout central Chile. The 11 March earthquake was at first thought to be an aftershock from the 27 February event, but University of Chile Seismologist Jaime Campos identified it as an ""independent earthquake"". The Hawaii-based Pacific Tsunami Warning Center pointed out the possibility of local tsunamis within 100 kilometres (62 mi) of the epicentre, although small, but violent waves were seen in the Pichilemu and Bucalemu area. One person was reported dead. At least eleven aftershocks immediately followed, causing panic throughout coastal towns between the Coquimbo and Los Lagos regions.The earthquake was specially destructive in the epicentre town, Pichilemu, capital of Cardenal Caro Province. The city hosts five National Monuments of Chile, of which two, the Agustín Ross Park and the Agustín Ross Cultural Centre, were seriously damaged by the earthquake. It also damaged the villages of La Aguada and Cardonal de Panilonco. Rancagua, the capital of O'Higgins Region, was also damaged, leading President Sebastián Piñera to declare a catastrophe state in O'Higgins Region.
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