Giant Earthquakes and Their Tsunamis

Total Page:16

File Type:pdf, Size:1020Kb

Giant Earthquakes and Their Tsunamis Giant earthquakes and their tsunamis Tsunami Sand spit American Geophysical Union Chapman Conference Valparaíso, Viña del Mar, and Valdivia, Chile 16–24 May 2010 Chapman Conference on Giant Earthquakes and Their Tsunamis Valparaíso, Viña del Mar, and Valdivia, Chile 16–24 May 2010 Conveners Brian Atwater, U.S. Geological Survey Sergio Barrientos, Universidad de Chile Marco Cisternas, Universidad Católica de Valparaíso Kelin Wang, Geological Survey of Canada The conveners thank Nicolás Gorigoitia, Lynn Hayes, Mario Pino, Rob Wesson, and Cynthia Wilcox for helping to organize the conference. Sponsors The American Geophysical Union and the conference organizers acknowledge financial support from Universidad Católica de Valparaíso, Universidad de Chile, UNESCO/IOC, U.S. Geological Survey, and the municipalities of Viña del Mar and Valparaiso. 1 Chapman Conference on Giant Earthquakes and Their Tsunamis May 16 Sun Talks, posters, and discussion — Hotel Marina del Rey*, Viña del Mar 17 Mon Public presentations — P. Universidad Católica de Valparaíso, Valparaíso 18-20 Tue-Thu Talks, posters, and discussion — Hotel Marina del Rey*, Viña del Mar 20-24 Thu-Mon Field trips — Maullín and Cocotué; Valdivia * Linda Andreani Room SUNDAY, 16 MAY Session 16A Overviews 0900–0930 Welcome 0930–0945 George PLAFKER Overview of the mechanism of the giant 1960 Chile earthquake and near-field tsunami with comparisons to the 1964 Alaska and 2004 Sumatra events 0945-1000 Onno ONCKEN Chile’s seismogenic coupling zones – geophysical and neotectonic observations from the South American subduction zone 1000-1015 Christophe VIGNY Upper plate deformation is dominated by varying coupling on the Chilean subduction zone 1015-1030 Inés CIFUENTES Fifty years after the great 1960 Chilean earthquake: What have we learned and how do we use what we know to reduce human tragedies? 1030-1100 Discussion 1100-1130 Coffee break 1130-1145 Daniel MELNICK Structural control on megathrust rupture: Insights from the 1960 Chile earthquake segment 1145-1200 Rolando ARMIJO Structural partitioning of the Chilean subduction margin: Evidence for a West Andean Thrust 1200-1215 Kenji SATAKE Tsunami warning systems: Impacts of the 1960 and 2004 global tsunamis 1215-1230 Emile OKAL From Nias to Maule: Have we become wiser in the wake of Sumatra? 1230-1300 Discussion 2 SUNDAY, 16 MAY continued Session 16P 1960 earthquakes: Tectonics, source, recurrence 1430-1435 Pedro FEYJÓ On the earthquake that razed Valdivia 1435-1730 Posters: Summaries (1435-1530) and Presentations (1530-1730) 16P-1 Daniel CARRIZO Seismic asperities and barriers related to subducting bathymetric features along the Nazca-South American plate boundary 16P-2 Andrés TASSARA Strength of the megathrust below the Chilean forearc, nature of seismic asperities and model for giant earthquake growth 16P-3 Marcos MORENO Earthquake cycle deformation and its link to upper plate structure in the southern Andes 16P-4 Jan BEHRMANN Differences in composition and strength of subducted sediment define the rupture of the great 1960 Chile earthquake 16P-5 Andreas RIETBROCK Imaging the subduction thrust with passive seismic arrays: A comparison between northern and southern Chile 16P-6 Salvador FARRERAS May 22 1960 earthquake source parameters as derived from tsunami run-ups on Easter Island and alongshore Chile 16P-7 Yushiro FUJII Tsunami source of the 1960 Chilean earthquake inferred from tide gauge data 16P-8 Matthias DORRIES The 1960 Chilean earthquake and the free oscillations of the earth 16P-9 Daniel MELNICK Megathrust earthquakes over the past 1.7 ka at Guafo island, south Chile 16P-10 Lisa ELY Geological evidence of past tsunamis at the boundary between the 1960 and 1835 earthquake rupture areas, south-central Chile 16P-11 Eduard REINHARDT Recovery estimates for the Río Cruces after the May 1960 Chilean earthquake 16P-12 Jorge QUEZADA Holocene coastal uplift in the northern segment of 1960 Chilean earthquakes 16P-13 Jasper MOERNAUT Recurrence of 1960-like earthquake shaking in south- central Chile revealed by lacustrine sedimentary records 1730-1830 Discussion 3 MONDAY, 17 MAY Session 17A Public presentations 0900-0910 Alfonso MUGA Welcome from P. Universidad Católica de Valparaíso 0910-0920 Jorge SEQUEIRA Welcome on behalf of UNESCO-Chile 0920-0930 Inés CIFUENTES Welcome on behalf of the American Geophysical Union 0930-1000 Hiroo KANAMORI Revisiting the 1960 Chilean earthquake 1000-1030 Rodolfo SARAGONI The giant 1960 Chile earthquake: A large magnitude moderate earthquake 1030-1100 Hellmuth SIEVERS The seismic sea wave of 22 May 1960 along the Chilean coast: A personal account 1130-1200 Diana COMTE The 2010 Chile earthquake – variations in the rupture mode 1200-1230 Anne SOCQUET Modelling the source of the maule Mw 8.8 earthquake and early afterslip using GPS and insar data 1230-1300 Marcelo LAGOS Magnitude and impact of the 2010 Chilean tsunami 1300-1400 Conference luncheon Afternoon Outreach Introduced by Inés Cifuentes, Mabel Keller, and Marco Cisternas 4 TUESDAY, 18 MAY Session 18A Chilean earthquake of 27 February 2010 0900-0915 Michael SPRANGER Loss assessment of the Feb 27, 2010 Chile earthquake from a reinsurer’s perspective 0915-0930 Michael BEVIS The 27 February 2010 Maule earthquake: The emergency geodetic response and some of its early results 0930-1200 Posters: Summaries (0930-1010) and Presentations (1010-1200) 18A-1 Marc-Andre GUTSCHER What controls the frequency and size of megathrust earthquakes offshore Chile and Sumatra? Insights from crustal structure and thermal modeling 18A-2 Robert WESSON Long-term inter-seismic subsidence of Santa María Island, Chile (37°S) supported by resurvey of 1835 HMS Beagle soundings 18A-3 Ximena CONTARDO Potential seismogenic faults along the south central Chilean forearc, insight from seismic and bathymetric data 18A-4 Dave CHADWELL Offshore investigations of the 27 Feb. 2010 Maule, Chile earthquake rupture 18A-5 Richard ALLMENDINGER Interseismic strain, continental deformation, and great earthquakes of southern Chile 18A-6 Matthias ROSENAU Did the 27th February 2010 earthquake close the gap? Insights from pre-, co- and postseismic deformation pattern 18A-7 Anthony SLADEN A coseismic distributed-slip model for the 2010 Mw 8.8 Maule (Chile) earthquake 18A-8 Benjamin BROOKS Megathrust seismic events, post-seismic deformation and mountain building: Andean deformation related to the 27 Feb. 2010 Maule, Chile earthquake 18A-9 Christophe VIGNY The Maule Mw 8.8 earthquake monitored by continuous and survey mode GPS 18A-10 Frederick BLUME Rapid GNSS and data communication system deployments in Chile and Argentina following the M 8.8 Maule earthquake 18A-11 Robert SMALLEY High-rate GPS seismograms from the 27 Feb. 2010, M=8.8, Maule Chile earthquake 18A-12 M. Meghan MILLER High-rate low-latency CGPS for science and first responders: Proof-of-concept for a Maule earthquake scenario 1200-1300 Discussion 5 TUESDAY, 18 MAY continued Session 18P 2010 earthquake and its near-field tsunami 1430-1445 Stephen MILLER Modeling of the preparatory processes in the source region and analysis of aftershock decay rates of the 2010 Mw 8.8 Chile earthquake 1445-1500 Marco CISTERNAS Similarities between the great Chilean earthquakes of 1835 and 2010 1500-1730 Posters: Ssummaries (1500-1540) and Presentations (1540-1730) 18P-1 Raul MADARIAGA The Maule Mw 8.8 earthquake: Modelling using 1 hz CGPS and seismic data 18P-2 Sutatcha HONGSRESAWAT Ultra-long period spectrum of the 2010 Maule, Chile earthquake from the Earth's spheroidal modes 18P-3 Mohammad RAEESI Asperity distribution of the 27 Feb. 2010 (Mw = 8.8) Chile earthquake 18P-4 Catherine PETROFF Rapid reconnaissance survey of the february 27, 2010 Chile tsunami - Constitución to Colcura, Quidico to Mehuín 18P-5 Patricio CATALÁN Observations by the international tsunamy survey team, regions VII-VI and V of Chile 18P-6 Rodrigo CIENFUEGOS Observations on morphological changes produced by the impact of the February 27, 2010 tsunami along the coastline of V- VI-VII region 18P-7 Hermann FRITZ Field survey of the 27 February 2010 tsunami in Chile, regions Maule and Biobío (VII and VIII) 18P-8 Jorge QUEZADA The third tsunami wave in Biobío region bays during the Chilean 27th February 2010 earthquake 18P-9 M. Teresa RAMÍREZ Geomorphological effects from the 27 February 2010 tsunami: A post-tsunami survey, central Chile 18P-10 Eduardo JARAMILLO Before and after comparisons of the Chilean coast affected by the earthquake and tsunami of February 27th 18P-11 Ricardo NORAMBUENA International Tsunami Survey Team – Chile 1730-1830 Discussion 6 WEDNESDAY, 19 MAY Session 19A Global perspectives; South America 0900-0915 Kelin WANG What facilitates or hinders giant subduction earthquakes? 0915-1200 Posters: Summaries (0915-1000) and Presentations (1000-1200) 19A-1 Mark SIMONS Spatial heterogeneity and temporal persistence in seismogenic behavior of subduction megathrusts 19A-2 Jim MORI Are asperities persistent features in repeated great earthquakes? 19A-3 Gavin HAYES Applications of a new three-dimensional model of global subduction zone geometries to the understanding of seismogenesis 19A-4 Fabio CORBI Gel-quakes: Laboratory modeling of the subduction interplate seismic behavior 19A-5 Marco CISTERNAS Complex recurrence of large historical earthquakes in central Chile 19A-6 Raul MADARIAGA The M=7.7 Tocopilla earthquake of 14 November 2007, its aftershocks and consequences 19A-7 Sophie PEYRAT Source rupture processes of the 2005 and 2007 earthquakes in northern Chile,
Recommended publications
  • Humboldt Penguin Spheniscus Humboldti Population in Chile: Counts of Moulting Birds, February 1999–2008
    Wallace & Araya: Humboldt Penguin population in Chile 107 HUMBOLDT PENGUIN SPHENISCUS HUMBOLDTI POPULATION IN CHILE: COUNTS OF MOULTING BIRDS, FEBRUARY 1999–2008 ROBERTA S. WALLACE1 & BRAULIO ARAYA2 1Milwaukee County Zoo, 10001 W. Blue Mound Road, Milwaukee, WI 53226, USA ([email protected]) 2Calle Lima 193. Villa Alemana, V Región, Chile Received 19 August 2014, accepted 9 December 2014 SUMMARY WALLACE, R.S. & ARAYA, B. 2015. Humboldt Penguin Spheniscus humboldti population in Chile: counts of moulting birds, February 1999–2008. Marine Ornithology 43: 107–112 We conducted annual counts of moulting Humboldt Penguins roosting on the mainland coast and on offshore islands in north and central Chile during 1999–2008. The census area included the known major breeding colonies in Chile, where many penguins moult, as well as other sites. Population size was relatively stable across years, with an average of 33 384 SD 2 372 (range: 28 642–35 284) penguins counted, but the number of penguins found at any individual site could vary widely. Shifting penguin numbers suggest that penguins tend to aggregate to moult where food is abundant. While many of the major breeding sites are afforded some form of protected status, two sites with sizable penguin populations, Tilgo Island and Pájaros-1 Island, have no official protection. These census results provide a basis upon which future population trends can be compared. Key words: penguin, Spheniscus humboldti, census, Chile INTRODUCTION penguin taking less than three weeks to moult (Paredes et al. 2003). Penguins remain on land during moult, and they return to The Humboldt Penguin Spheniscus humboldti is a species endemic sea immediately after moulting (Zavalaga & Paredes 1997).
    [Show full text]
  • Large Rock Avalanches and River Damming Hazards in the Andes of Central Chile: the Case of Pangal Valley, Alto Cachapoal
    Geophysical Research Abstracts Vol. 21, EGU2019-6079, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Large rock avalanches and river damming hazards in the Andes of central Chile: the case of Pangal valley, Alto Cachapoal Sergio A. Sepulveda (1,2), Diego Chacon (2), Stella M. Moreiras (3), and Fernando Poblete (1) (1) Universidad de O0Higgins, Instituto de Ciencias de la Ingeniería, Rancagua, Chile ([email protected]), (2) Universidad de Chile, Departamento de Geología, Santiago, Chile, (3) CONICET – IANIGLA- CCT, Mendoza, Argentina A cluster of five rock avalanche deposits of volumes varying from 1.5 to 150 millions of cubic metres located in the Pangal valley, Cachapoal river basin in the Andes of central Chile is studied. The landslides are originated in volcanic rocks affected by localised hydrothermal alteration in a short section of the fluvial valley. The largest rock avalanches, with deposit thicknesses of up to about 100 m, have blocked the valley to be later eroded by the Pangal river. Lacustrine deposits can be found upstream. A detailed geomorphological survey of the valley and dating of the landslide deposits is being performed, in order to assess the likelihood of new large volume landslide events with potential of river damming. Such events would endanger hydroelectric facilities and human settlements downstream. A total of eighteen potential landslide source areas were identified, with potential of damming up to 10^7 million cubic metres. This case study illustrates a poorly studied hazard of large slope instabilities and related river damming in the Chilean Andes, extensively covered by large landslide deposits along their valleys.
    [Show full text]
  • Universita' Degli Studi Di Milano Bicocca
    Dipartimento di Scienze Ambiente e Territorio e Scienze della Terra Università degli studi di Milano-Bicocca Dottorato di Ricerca in Scienze della Terra XXVI ciclo Earthquake-induced static stress change in promoting eruptions Tutore: Prof. Alessandro TIBALDI Co-tutore: Dott.ssa Claudia CORAZZATO Fabio Luca BONALI Matr. Nr. 040546 This work is dedicated to my uncle Eugenio Marcora who led my interest in Earth Sciences and Astronomy during my childhood Abstract The aim of this PhD work is to study how earthquakes could favour new eruptions, focusing the attention on earthquake-induced static effects in three different case sites. As a first case site, I studied how earthquake-induced crustal dilatation could trigger new eruptions at mud volcanoes in Azerbaijan. Particular attention was then devoted to contribute to the understanding of how earthquake-induced magma pathway unclamping could favour new volcanic activity along the Alaska-Aleutian and Chilean volcanic arcs, where 9 seismic events with Mw ≥ 8 occurred in the last century. Regarding mud volcanoes, I studied the effects of two earthquakes of Mw 6.18 and 6.08 occurred in the Caspian Sea on November 25, 2000 close to Baku city, Azerbaijan. A total of 33 eruptions occurred at 24 mud volcanoes within a maximum distance of 108 km from the epicentres in the five years following the earthquakes. Results show that crustal dilatation might have triggered only 7 eruptions at a maximum distance of about 60 km from the epicentres and within 3 years. Dynamic rather than static strain is thus likely to have been the dominating “promoting” factor because it affected all the studied unrested volcanoes and its magnitude was much larger.
    [Show full text]
  • "Tectonic Deformation Re Great Subduction Zone Earthquakes
    _ _ _ _ _ _ _ _ _ _ ____ ._ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ . 3 TECTONIC DEFORMATION RELATED TO GREAT SUBDUCTION ZONE EARTliQUAKES George Plafker, U.S. Geological Survey Abstract Vertical and horizontal displacements associated with plate convergence at consuming plate margins are the algebraic sum of interseismic, coseismic, and transient deformat- ions through a complete earthquake cycle on a time scale of tens to thousands of years. Elastic and permanent deformations accumulated during the interseismic period are a function of coupling across the megathrust interface between the underthrusting oceanic crust and the upper plate, and of the direction, rate, and duration of relative plate motions. Coseismic deformations result frbm seaward thrusting of the upper plate and depend upon dip of the megathrust, displacement along the megathrust, and the dip and displacements along subsidiary faults that may break through the upper plate. Transient postseismic displacements may occur that result from relatively slow elastic strain i release or creep deformation following an earthquake, | i Coseismic regional vertical displacements typically involve a central broad asymmetric downwarp elongate parallel to the arc with a flanking zone of marked uplift on the sea- | t ward side, and a zone of relatively minor uplift on the landward side. The major zones I of uplift and subsidence may extend from the trench to its associated volcanic are. In the 1960 Chile earthquake (Mw=9.5] deformation occurred for about 1,050 km parallel to the are over an area of 85,000+ km with shoreline vertical displacements to +5.7 m and -2.3 m.
    [Show full text]
  • Holocene Relative Sea-Level Change Along the Tectonically Active Chilean Coast
    This is a repository copy of Holocene relative sea-level change along the tectonically active Chilean coast. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/161478/ Version: Accepted Version Article: Garrett, Ed, Melnick, Daniel, Dura, Tina et al. (5 more authors) (2020) Holocene relative sea-level change along the tectonically active Chilean coast. Quaternary Science Reviews. 106281. ISSN 0277-3791 https://doi.org/10.1016/j.quascirev.2020.106281 Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 Holocene relative sea-level change along the tectonically active Chilean coast 2 3 Ed Garrett1*, Daniel Melnick2, Tina Dura3, Marco Cisternas4, Lisa L. Ely5, Robert L. Wesson6, Julius 4 Jara-Muñoz7 and Pippa L. Whitehouse8 5 6 1 Department of Environment and Geography, University of York, York, UK 7 2 Instituto de Ciencias de la Tierra, TAQUACh, Universidad Austral de Chile, Valdivia, Chile 8 3 Department of Geosciences, Virginia Tech, Blacksburg, VA, USA 9 4 Instituto de Geografía, Pontificia Universidad Católica de Valparaíso, Valparaíso, Chile 10 5 Department of Geological Sciences, Central Washington University, Ellensburg, WA, USA 11 6 U.S.
    [Show full text]
  • Crustal Deformation Associated with the 1960 Earthquake Events in the South of Chile
    Paper No. CDDFV CRUSTAL DEFORMATION ASSOCIATED WITH THE 1960 EARTHQUAKE EVENTS IN THE SOUTH OF CHILE Felipe Villalobos 1 ABSTRACT Large earthquakes can cause significant subsidence and uplifts of one or two meters. In the case of subsidence, coastal and fluvial retaining structures may therefore no longer be useful, for instance, against flooding caused by a tsunami. However, tectonic subsidence caused by large earthquakes is normally not considered in geotechnical designs. This paper describes and analyses the 1960 earthquakes that occurred in the south of Chile, along almost 1000 km between Concepción and the Taitao peninsula. Attention is paid to the 9.5 moment magnitude earthquake aftermath in the city of Valdivia, where a tsunami occurred followed by the overflow of the Riñihue Lake. Valdivia and its surrounding meadows were flooded due to a subsidence of approximately 2 m. The paper presents hypotheses which would explain why today the city is not flooded anymore. Answers can be found in the crustal deformation process occurring as a result of the subduction thrust. Various hypotheses show that the subduction mechanism in the south of Chile is different from that in the north. It is believed that there is also an elastic short-term effect which may explain an initial recovery and a viscoelastic long-term effect which may explain later recovery. Furthermore, measurements of crustal deformation suggest that a process of stress relaxation is still occurring almost 50 years after the main seismic event. Keywords: tectonic subsidence, 1960 earthquakes, Valdivia, crustal deformation, stress relaxation INTRODUCTION Tectonic subsidence or uplift is not considered in any design of onshore or near shore structures.
    [Show full text]
  • The Mw 8.8 Chile Earthquake of February 27, 2010
    EERI Special Earthquake Report — June 2010 Learning from Earthquakes The Mw 8.8 Chile Earthquake of February 27, 2010 From March 6th to April 13th, 2010, mated to have experienced intensity ies of the gap, overlapping extensive a team organized by EERI investi- VII or stronger shaking, about 72% zones already ruptured in 1985 and gated the effects of the Chile earth- of the total population of the country, 1960. In the first month following the quake. The team was assisted lo- including five of Chile’s ten largest main shock, there were 1300 after- cally by professors and students of cities (USGS PAGER). shocks of Mw 4 or greater, with 19 in the Pontificia Universidad Católi- the range Mw 6.0-6.9. As of May 2010, the number of con- ca de Chile, the Universidad de firmed deaths stood at 521, with 56 Chile, and the Universidad Técni- persons still missing (Ministry of In- Tectonic Setting and ca Federico Santa María. GEER terior, 2010). The earthquake and Geologic Aspects (Geo-engineering Extreme Events tsunami destroyed over 81,000 dwell- Reconnaissance) contributed geo- South-central Chile is a seismically ing units and caused major damage to sciences, geology, and geotechni- active area with a convergence of another 109,000 (Ministry of Housing cal engineering findings. The Tech- nearly 70 mm/yr, almost twice that and Urban Development, 2010). Ac- nical Council on Lifeline Earthquake of the Cascadia subduction zone. cording to unconfirmed estimates, 50 Engineering (TCLEE) contributed a Large-magnitude earthquakes multi-story reinforced concrete build- report based on its reconnaissance struck along the 1500 km-long ings were severely damaged, and of April 10-17.
    [Show full text]
  • The Alaska Earthquake Regional Effects
    The Alaska Earthquake March 27,1964: Regional Effects This volume was published as separate chapters A-J GEOLOGICAL SURVEY PROFESSIONAL PAPER 543 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director CONTENTS [Letters designate the separately published chapters] ('1) Slide-induced waves, seiching, and ground fracturing caused by the earthquake of March 27, 1964, at Kenai Lake, Alaska, by David S. McCulloch. (B) Geomorphic effects of the earthquake of March 27, 1964. in the Martin-Bering Rivers area, Alaska, by Samuel J. Tuthill and Wilson M. Laird. (C) Gravity survey and regional geology of the Prince William Sound, epicentral region. Alaska, by J. E. Case, L). F. Barnes, George Plafker, and S. L. Robbins. (D) Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kadiali and nearby islands, Alaska, by George Plafker and Reuben Kachadooria~~. (E) Effects of the earthquake of Marc11 27. 1964, in the Coljl~erRiver Basin area, Alaska, by Oscar J. Ferrians, Jr. (F) Ground breakage and associated effects ill the Cook Inlet area. Alaska, resulting from the JIarch 27, 1964, earthquake, by Helen L. Foster and Thor x. V. Karlstrorn. (G) Surface faults on Montague Island associated with the 1964 Alahka earthquake, by George Plaflter. (13) Erosion and deposition on a beach raised by the 19ki4 earthyuake. Jfontagne Island, Alaska, by 11. J. Kirkby and Anne V. Kirkby. (I) Tectonics d the March 27,1964, Alaska earthquake. by Grorge I'lafker. (J) Effects of the Alaska earbhquake of March 27. 1964, on shore processes and beach ~norphology, by Kirk W.
    [Show full text]
  • D.5.3 – Status of ICT Policy Development – Country Report Chile
    D.5.3 – Status of ICT Policy Development – Country Report Chile Grant Agreement number: 231730 Project acronym: PRO-IDEAL Project title: PROmotion of an ICT Dialogue between Europe and America Latina Funding Scheme: Support Action Due date: 29/04/2011 Actual date: 29/04/2011 Document Author/s: ADI CHILE Version: 1.0 Dissemination level: PU Status: Final Status of ICT Policy Development – Country Report Chile TABLE OF CONTENTS Page 1 INTRODUCTION .................................................................................................................. 3 2 NATIONAL POLICIES AND STRATEGIES FOR ICT INDUSTRY DEVELOPMENT ......... 4 2.1 Public Policies and Strategies for ICT Development ....................................................... 4 2.2 Active public policies for ICT industry development as cross technology in other value chains 4 2.3 Strategies at corporate or business associations level for ICT industry development..... 6 2.4 Legal framework and other public documents relevant to national ICT policies .............. 7 3 PUBLIC & PRIVATE INSTITUTIONAL STRUCTURE FOR DEVELOPMENT OF ICT ...... 9 3.1 Public and research institutions ....................................................................................... 9 3.2 Universities ....................................................................................................................... 9 3.3 Main private and corporate ICT stakeholders ................................................................ 11 4 NATIONAL POLICIES AND STRATEGIES FOR ICT RESEARCH &
    [Show full text]
  • Crustal Faults in the Chilean Andes: Geological Constraints and Seismic Potential
    Andean Geology 46 (1): 32-65. January, 2019 Andean Geology doi: 10.5027/andgeoV46n1-3067 www.andeangeology.cl Crustal faults in the Chilean Andes: geological constraints and seismic potential *Isabel Santibáñez1, José Cembrano2, Tiaren García-Pérez1, Carlos Costa3, Gonzalo Yáñez2, Carlos Marquardt4, Gloria Arancibia2, Gabriel González5 1 Programa de Doctorado en Ciencias de la Ingeniería, Pontificia Universidad Católica de Chile, Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected]; [email protected] 2 Departamento de Ingeniería Estructural y Geotécnica, Pontificia Universidad Católica de Chile, Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected]; [email protected]; [email protected] 3 Departamento de Geología, Universidad de San Luis, Ejercito de Los Andes 950, D5700HHW San Luis, Argentina. [email protected] 4 Departamento de Ingeniería Estructural y Geotécnica y Departamento de Ingeniería de Minería, Pontificia Universidad Católica de Chile. Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected] 5 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Angamos 0610, Antofagasta, Chile. [email protected] * Corresponding author: [email protected] ABSTRACT. The Chilean Andes, as a characteristic tectonic and geomorphological region, is a perfect location to unravel the geologic nature of seismic hazards. The Chilean segment of the Nazca-South American subduction zone has experienced mega-earthquakes with Moment Magnitudes (Mw) >8.5 (e.g., Mw 9.5 Valdivia, 1960; Mw 8.8 Maule, 2010) and many large earthquakes with Mw >7.5, both with recurrence times of tens to hundreds of years. By contrast, crustal faults within the overriding South American plate commonly have longer recurrence times (thousands of years) and are known to produce earthquakes with maximum Mw of 7.0 to 7.5.
    [Show full text]
  • The Magnitude 8.8 Offshore Maule Region Chile Earthquake of February 27, 2010
    THE MAGNITUDE 8.8 OFFSHORE MAULE REGION CHILE EARTHQUAKE OF FEBRUARY 27, 2010 Public Disclosure Authorized PRELIMINARY SUMMARY OF DAMAGE AND ENGINEERING RECOMMENDATIONS A Report to the World Bank Public Disclosure Authorized by FRANCISCO MEDINA - PETER I. YANEV - ALEXANDER P. YANEV Public Disclosure Authorized Public Disclosure Authorized April 18, 2010 Rev. 01: 07/07/10 Cover: Torre O’Higgins office building in Concepción. Back Cover: Constitución. The Magnitude 8.8 Offshore Maule Region, Chile Earthquake CONTENTS Acknowledgments, iv Executive Summary, v Prologue (by V.V. Bertero), vii 1. Background and Summary of the Investigation .......................................................... 1 2. General Engineering Observations.............................................................................. 3 3. Detailed Engineering Observations............................................................................. 4 3.1. Effects of the earthquake duration on building performance, 4 3.2. Effects of soil conditions on building performance, 5 3.3. Ground motion records, 6 3.4. Low-rise buildings (up to 4 stories), 6 Old and non-engineered buildings Engineered confined-masonry buildings Post-1950 buildings Steel-framed buildings Tsunami effects to buildings 3.5. Mid-rise and high-rise buildings (over 4 stories), 13 Damage to shear wall buildings Damage to exterior building cladding Damage to unusual architectural exterior details 3.6. Interior architectural and equipment damage, 20 3.7. Other structures, 23 Hospitals Historic public buildings
    [Show full text]
  • Lessons from the Chilean Earthquake: How a Human Rights
    How a human rights framework facilitates disaster response MaryCatherine Arbour, MD, Lessons from the Chilean MPH, is Associate Physician Earthquake: How a Human Rights for Research in the Division of Global Health Framework Facilitates Disaster Equity, Department of Response Medicine at Brigham and Women’s Hospital, Boston, MA. MaryCatherine Arbour, Kara Murray, Felipe Arriet, Cecilia Moraga, Miguel Cordero Vega Kara Murray, BA, is an MPH candidate at the Tufts University School of Medicine, Abstract Public Health and Professional Degrees Program, Boston, MA. The earthquake of 2010 in Chile holds important lessons about how a rights-based Felipe Arriet is a psycholo- public health system can guide disaster response to protect vulnerable populations. gist for Chile Crece Contigo, This article tells the story of Chile Grows With You (Chile Crece Contigo), an Ministry of Health, Santiago, Chile. intersectoral system created three years before the earthquake for protection of child rights and development, and its role in the disaster response. The creation of Chile Cecilia Moraga, MA, is a Grows With You with an explicit rights-oriented mandate established intersectoral founding member of the International Association for mechanisms, relationships, and common understanding between governmental groups the Study of Attachment, Chile at the national and local levels. After the earthquake, Chile Grows With You Crece Contigo, Ministry of Health, Santiago, Chile. organized its activities according to its founding principles: it provided universal access and support for all Chilean children, with special attention and services for Miguel Cordero Vega, MSc. those at greatest risk. This tiered approach involved public health and education is National Coordinator to Early Childhood Protection materials for all children and families; epidemiologic data for local planners about System, Ministry of Health, children in their municipalities at-risk before the earthquake; and an instrument Santiago, Chile.
    [Show full text]