The Utility of Earth Science Information in Post-Earthquake Land- Use Decision-Making: the 2010-2011 Canterbury Earthquake Sequence in Aotearoa New Zealand
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Geology of the Wairarapa Area
GEOLOGY OF THE WAIRARAPA AREA J. M. LEE J.G.BEGG (COMPILERS) New International NewZOaland Age International New Zealand 248 (Ma) .............. 8~:~~~~~~~~ 16 il~ M.- L. Pleistocene !~ Castlecliffian We £§ Sellnuntian .~ Ozhulflanl Makarewan YOm 1.8 100 Wuehlaplngien i ~ Gelaslan Cl Nukumaruan Wn ~ ;g '"~ l!! ~~ Mangapanlan Ql -' TatarianiMidian Ql Piacenzlan ~ ~;: ~ u Wai i ian 200 Ian w 3.6 ,g~ J: Kazanlan a.~ Zanetaan Opoitian Wo c:: 300 '"E Braxtonisn .!!! .~ YAb 256 5.3 E Kunaurian Messinian Kapitean Tk Ql ~ Mangapirian YAm 400 a. Arlinskian :;; ~ l!!'" 500 Sakmarian ~ Tortonisn ,!!! Tongaporutuan Tt w'" pre-Telfordian Ypt ~ Asselian 600 '" 290 11.2 ~ 700 'lii Serravallian Waiauan 5w Ql ." i'l () c:: ~ 600 J!l - fl~ '§ ~ 0'" 0 0 ~~ !II Lillburnian 51 N 900 Langhian 0 ~ Clifdenian 5e 16.4 ca '1000 1 323 !II Z'E e'" W~ A1tonian PI oS! ~ Burdigalian i '2 F () 0- w'" '" Dtaian Po ~ OS Waitakian Lw U 23.8 UI nlan ~S § "t: ." Duntroonian Ld '" Chattian ~ W'" 28.5 P .Sll~ -''" Whalngaroan Lwh O~ Rupelian 33.7 Late Priabonian ." AC 37.0 n n 0 I ~~ ~ Bortonian Ab g; Lutetisn Paranaen Do W Heretauncan Oh 49.0 354 ~ Mangaorapan Om i Ypreslan .;;: w WalD8wsn Ow ~ JU 54.8 ~ Thanetlan § 370 t-- §~ 0'" ~ Selandian laurien Dt ." 61.0 ;g JM ~"t: c:::::;; a.os'"w Danian 391 () os t-- 65.0 '2 Maastrichtian 0 - Emslsn Jzl 0 a; -m Haumurian Mh :::;; N 0 t-- Campanian ~ Santonian 0 Pragian Jpr ~ Piripauan Mp W w'" -' t-- Coniacian 1ij Teratan Rt ...J Lochovlan Jlo Turonian Mannaotanean Rm <C !II j Arowhanan Ra 417 0- Cenomanian '" Ngaterian Cn Prldoli -
Public Health Response to the February 22 Christchurch Earthquake
Public Health Response to the February 22 Christchurch Earthquake Progress Report Rebecca Dell Public Health Medicine Registrar Daniel Williams Medical Officer of Health, Incident Controller 30 March 2011 CONTENTS 1. Abbreviations 3 2. Background 3 3. Intelligence 4 4. Communications 6 5. Liaison 7 6. Operations 9 a. CPH Emergency Operations Centre 9 b. Water quality and technical advice 9 c. Welfare centres 11 d. Outbreak control 12 e. Community Welfare Recovery 12 f. Health In All Policies 13 7. Logistics 13 a. Staff 13 b. Building 14 c. Equipment 14 d. Staff welfare 14 8. Recovery 15 9. Assessment 17 10. Appendices 18 Appendix 1 Intelligence and surveillance inputs for earthquake response 18 Appendix 2 Enteric disease notifications for Canterbury 23 Appendix 3 E. coli transgressions mapping 26 Appendix 4 Free Associated Chlorine concentration mapping 28 Appendix 5 Enteric disease Episurv notifications by census area unit 29 Appendix 6 Campylobacter notifications following 22 February 30 Appendix 7 Draft results for Wave 1 of Christchurch Health Survey 31 Appendix 8 Latest public health key messages 45 Appendix 9 Public health guidelines for reopening of schools and early childhood centres 46 Appendix 10 Public health advice for early childhood centres 48 Appendix 11 Public health advice about asbestos dust 49 Appendix 12 Health Assessment Form for Welfare Centres 51 Page 2 of 54 1. ABBREVIATIONS CCC Christchurch City Council CDHB Canterbury District Health Board CPH Community and Public Health (public health division of CDHB) ECC Emergency Co-ordination Centre (at Christchurch Art Gallery) EOC Emergency Operations Centre EQRC Earthquake Recovery Centre (Civil Defence recovery phase at Christchurch Art Gallery HPO Health Protection Officer MOH Medical Officer of Health NZFSA New Zealand Food Safety Authority PHS Public Health South (Southern District Health Board) 2. -
The 2016 Kaikōura Earthquake
Earth and Planetary Science Letters 482 (2018) 44–51 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl The 2016 Kaikoura¯ earthquake: Simultaneous rupture of the subduction interface and overlying faults ∗ Teng Wang a, Shengji Wei a,b, , Xuhua Shi a, Qiang Qiu c, Linlin Li a, Dongju Peng a, Ray J. Weldon a,d, Sylvain Barbot a,b a Earth Observatory of Singapore, Nanyang Technological University, Singapore b Asian School of the Environment, Nanyang Technological University, Singapore c School of Earth and Environment, University of Leeds, United Kingdom d Department of Geological Science, University of Oregon, United States a r t i c l e i n f o a b s t r a c t Article history: The distribution of slip during an earthquake and how it propagates among faults in the subduction Received 2 August 2017 system play a major role in seismic and tsunami hazards, yet they are poorly understood because Received in revised form 22 October 2017 offshore observations are often lacking. Here we derive the slip distribution and rupture evolution during Accepted 26 October 2017 the 2016 Mw 7.9 Kaikoura¯ (New Zealand) earthquake that reconcile the surface rupture, space geodetic Available online xxxx measurements, seismological and tsunami waveform records. We use twelve fault segments, with eleven Editor: P. Shearer in the crust and one on the megathrust interface, to model the geodetic data and match the major Keywords: features of the complex surface ruptures. Our modeling result indicates that a large portion of the finite rupture model moment is distributed on the subduction interface, making a significant contribution to the far field strong motion surface deformation and teleseismic body waves. -
Transpressional Rupture Cascade of the 2016 Mw 7.8
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Transpressional Rupture Cascade of the 2016 Mw 10.1002/2017JB015168 7.8 Kaikoura Earthquake, New Zealand Key Points: Wenbin Xu1 , Guangcai Feng2, Lingsen Meng3 , Ailin Zhang3, Jean Paul Ampuero4 , • Complex coseismic ground 5 6 deformation can be explained by slip Roland Bürgmann , and Lihua Fang on six crustal fault segments 1 2 • Rupture process across multiple faults Department of Land Surveying and Geo-informatics, Hong Kong Polytechnic University, Hong Kong, China, School of 3 likely resulted from a triggering Geosciences and Info-Physics, Central South University, Changsha, China, Department of Earth Planetary and Space cascade between crustal faults Sciences, University of California, Los Angeles, CA, USA, 4Seismological Laboratory, California Institute of Technology, • Rupture speed was overall slow, but Pasadena, CA, USA, 5Department of Earth and Planetary Science, University of California, Berkeley, CA, USA, 6Institute of locally faster along individual fault segments Geophysics, China Earthquake Administration, Beijing, China Supporting Information: Abstract Large earthquakes often do not occur on a simple planar fault but involve rupture of multiple • Supporting Information S1 • Data Set S1 geometrically complex faults. The 2016 Mw 7.8 Kaikoura earthquake, New Zealand, involved the rupture of • Data Set S2 at least 21 faults, propagating from southwest to northeast for about 180 km. Here we combine space • Data Set S3 geodesy and seismology techniques to study subsurface fault geometry, slip distribution, and the kinematics of the rupture. Our finite-fault slip model indicates that the fault motion changes from predominantly Correspondence to: W. Xu, G. Feng, and L. Meng, right-lateral slip near the epicenter to transpressional slip in the northeast with a maximum coseismic surface [email protected]; displacement of about 10 m near the intersection between the Kekerengu and Papatea faults. -
Late Quaternary Faulting in the Kaikoura Region, Southeastern Marlborough, New Zealand
AN ABSTRACT OF THE THESIS OF Russell J. Van Dissen for the degree of Master of Science in Geology presented on February 15, 1989. Title: Late Quaternary Faulting in the Kaikoura Region, Southeastern Marlborough, New Zealand Redacted for privacy Abstract approved: Dr. Robert 8.0eats Active faults in the Kaikoura region include the Hope, Kekerengu, and Fidget Faults, and the newly discovered Jordan Thrust, Fyffe, and Kowhai Faults. Ages of faulted alluvial terraces along the Hope Fault and the Jordan Thrust were estimated using radiocarbon-calibrated weathering-rind measurements on graywacke clasts. Within the study area, the Hope Fault is divided, from west to east, into the Kahutara, Mt. Fyffe, and Seaward segments. The Kahutara segment has a relatively constant Holocene right-lateral slip rate of 20-32 mm/yr, and an earthquake recurrence interval of 86 to 600 yrs: based on single-event displacements of 3 to 12 m. The western portion of the Mt. Fyffe segment has a minimum Holocene lateral slip rate of 16 + 5 mm/yr .(southeast side up); the eastern portion has horizontal and vertical slip rates of 4.8+ 2.7 mm/yr and 1.7 + 0.2 mm/yr, respectively (northwest side up). There is no dated evidence for late Quaternary movementon the Seaward segment, and its topographic expression is much more subdued than that of the two western segments. The Jordan Thrust extends northeast from the Hope Fault, west of the Seaward segment. The thrust has horizontal and vertical slip rates of 2.2 + 1.3 mm/yr and 2.1 + 0.5 mm/yr, respectively (northwest side up), and a maximum recurrence interval of 1200 yrs: based on 3 events within the last 3.5 ka. -
Kaikoura Earthquake Response – a Controller's Perspective
Kaikoura Earthquake Response – A Controller’s Perspective John Mackie, Christchurch City Council Abstract Having just dealt with the tsunami alert and the overnight evacuation of 20,000 people from coastal areas of Christchurch, following the 7.8 magnitude earthquake at two minutes past midnight on 14 November 2016, key Civil Defence personnel from Christchurch were requested to assist with the response effort in Kaikoura who had suffered severe damage as a result of the quake. This paper outlines the priorities and challenges presented to emergency personnel that were deployed to assist the community and meet their immediate needs in response to one of New Zealand's largest recorded earthquakes. The first wave of responders from Christchurch included a Controller, Emergency Operations Centre (EOC) staff including operations manager, engineering support, planning and intelligence, welfare manager and staff, building and structural engineers, who were booked to fly to Kaikoura at first light on Tuesday 15 November. In a very short space of time after arrival on Tuesday morning, the team were briefed to gain a situational awareness from the local EOC team on the extent of the known damage, emerging issues and welfare needs in the community, which they had identified over the gruelling 34 hours since the event. We understood already that there was no road or rail access to the town due to landslips and cliff collapses, but the boat harbour had been rendered almost useless due to the seismic upheaval of the coast line. One of the short term priorities was to restore a temporary water supply as it was reported that three of the town's five reservoirs were damaged and there was one day of storage remaining at normal demand. -
Submission on Selwyn District Council Draft Long Term Plan 2018-2028
Submission on Selwyn District Council Draft Long Term Plan 2018-2028 To: Selwyn District Council Submitter: Community & Public Health A division of the Canterbury District Health Board Attn: Kirsty Peel Community and Public Health C/- Canterbury District Health Board PO Box 1475 Christchurch 8140 Proposal: Selwyn District Council is consulting on their long-term plan to ascertain views on how best to manage infrastructure and services in the district over the next 10 years. Page 1 of 9 Template File Pathway: Y:\CFS\CPHGroups\RMC\SDC\LTP\2018\SelwynLTPSubmissionFinal180503.docx SUBMISSION ON SELWYN DISTRICT COUNCIL DRAFT LONG TERM PLAN Details of submitter 1. Canterbury District Health Board (CDHB) 2. The CDHB is responsible for promoting the reduction of adverse environmental effects on the health of people and communities and to improve, promote and protect their health pursuant to the New Zealand Public Health and Disability Act 2000 and the Health Act 1956. 3. These statutory obligations are the responsibility of the Ministry of Health and, in the Canterbury District, are carried out under contract by Community and Public Health under Crown funding agreements on behalf of the Canterbury District Health Board. General comments 4. Health and wellbeing (overall quality of life) is influenced by a wide range of factors beyond the health sector. These influences can be described as the conditions in which people are born, grow, live, work and age, and are impacted by environmental, social and behavioural factors. They are often referred to as the ‘social determinants of health1. Barton and Grant’s Health Map2 shows how various influences on health are complex and interlinked. -
Contest 2015 Title: “Slip Rate and Paleoseismicity of the Kekerengu Fault: an Anchor Point for Deformation Rates and Seismic H
Contest 2015 Title: “Slip Rate and Paleoseismicity of the Kekerengu Fault: An anchor point for deformation rates and seismic hazard through central New Zealand” Leader: Timothy A. Little Organisation: Victoria University of Wellington Total funding (GST ex): $182,778 Title: Slip Rate and Paleoseismicity of the Kekerengu Fault: An anchor point for deformation rates and seismic hazard through central New Zealand Programme Leader: Timothy A. Little Affiliation: Victoria University of Wellington Co-P.I.: Russ Van Dissen (GNS Science) A.I.: Kevin Norton (VUW) Has this report been peer reviewed? Provide name and affiliation. Part of it: the paper by Little et al. was published in 2018 in the Bulletin of Seismological Society of America, which is a peer-reviewed international journal. Table of Contents: 1. Key Message for Media 2. Abstract 3. Introduction/ Background 4. Research Aim 1: Determining Kekerengu Fault Paleoseismic History 5. Research Aim 2: Determining the Late Quaternary Slip Rate of the Kekerengu Fault 6. Conclusions & Recommendations 7. Acknowledgments 8. References 9. Appendices Key Message for Media: [Why are these findings important? Plain language; 5 sentences.] Prior to this study, little scientific data existed about the rate of activity and earthquake hazard posed by the active Kekerengu Fault near the Marlborough coast in northeastern South Island. Our study was designed to test the hypothesis that this fault carries most of the Pacific-Australia plate motion through central New Zealand, and is a major source of seismic hazard for NE South Island and adjacent regions straddling Cook Strait—something that had previously been encoded in the NZ National Seismic Hazard Model. -
Landslides Triggered by the MW 7.8 14 November 2016 Kaikoura Earthquake, New Zealand
This is a repository copy of Landslides Triggered by the MW 7.8 14 November 2016 Kaikoura Earthquake, New Zealand. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/128042/ Version: Accepted Version Article: Massey, C, Petley, D.N., Townsend, D. et al. (25 more authors) (2018) Landslides Triggered by the MW 7.8 14 November 2016 Kaikoura Earthquake, New Zealand. Bulletin of the Seismological Society of America, 108 (3B). ISSN 0037-1106 https://doi.org/10.1785/0120170305 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. 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/ Manuscript Click here to download Manuscript BSSA_Kaikoura_Landslides_revised_FINAL.docx 1 Landslides Triggered by the MW 7.8 14 November 2016 Kaikoura Earthquake, New 2 Zealand 3 C. Massey1; D. Townsend1; E. Rathje2; K.E. Allstadt3; B. Lukovic1; Y. Kaneko1; B. Bradley4; J. 4 Wartman5; R.W. Jibson3; D.N. Petley6; N. Horspool1; I. Hamling1; J. Carey1; S. -
GEOTECHNICAL RECONNAISSANCE of the 2011 CHRISTCHURCH, NEW ZEALAND EARTHQUAKE Version 1: 15 August 2011
GEOTECHNICAL RECONNAISSANCE OF THE 2011 CHRISTCHURCH, NEW ZEALAND EARTHQUAKE Version 1: 15 August 2011 (photograph by Gillian Needham) EDITORS Misko Cubrinovski – NZ Lead (University of Canterbury, Christchurch, New Zealand) Russell A. Green – US Lead (Virginia Tech, Blacksburg, VA, USA) Liam Wotherspoon (University of Auckland, Auckland, New Zealand) CONTRIBUTING AUTHORS (alphabetical order) John Allen – (TRI/Environmental, Inc., Austin, TX, USA) Brendon Bradley – (University of Canterbury, Christchurch, New Zealand) Aaron Bradshaw – (University of Rhode Island, Kingston, RI, USA) Jonathan Bray – (UC Berkeley, Berkeley, CA, USA) Misko Cubrinovski – (University of Canterbury, Christchurch, New Zealand) Greg DePascale – (Fugro/WLA, Christchurch, New Zealand) Russell A. Green – (Virginia Tech, Blacksburg, VA, USA) Rolando Orense – (University of Auckland, Auckland, New Zealand) Thomas O’Rourke – (Cornell University, Ithaca, NY, USA) Michael Pender – (University of Auckland, Auckland, New Zealand) Glenn Rix – (Georgia Tech, Atlanta, GA, USA) Donald Wells – (AMEC Geomatrix, Oakland, CA, USA) Clint Wood – (University of Arkansas, Fayetteville, AR, USA) Liam Wotherspoon – (University of Auckland, Auckland, New Zealand) OTHER CONTRIBUTORS (alphabetical order) Brady Cox – (University of Arkansas, Fayetteville, AR, USA) Duncan Henderson – (University of Canterbury, Christchurch, New Zealand) Lucas Hogan – (University of Auckland, Auckland, New Zealand) Patrick Kailey – (University of Canterbury, Christchurch, New Zealand) Sam Lasley – (Virginia Tech, Blacksburg, VA, USA) Kelly Robinson – (University of Canterbury, Christchurch, New Zealand) Merrick Taylor – (University of Canterbury, Christchurch, New Zealand) Anna Winkley – (University of Canterbury, Christchurch, New Zealand) Josh Zupan – (University of California at Berkeley, Berkeley, CA, USA) TABLE OF CONTENTS 1.0 INTRODUCTION 2.0 SEISMOLOGICAL ASPECTS 3.0 GEOLOGICAL ASPECTS 4.0 LIQUEFACTION AND LATERAL SPREADING 5.0 IMPROVED GROUND 6.0 STOPBANKS 7.0 BRIDGES 8.0 LIFELINES 9.0 LANDSLIDES AND ROCKFALLS 1. -
Plunket Annual Report 2016/17
ANNUAL REPORT The2017 Royal New Zealand Plunket Society Inc. a Our vision 3 From our New Zealand President 4 From our Chief Executive 6 Plunket by the numbers 8 Our heart 12 Our people 16 Our approach 18 Our insights 20 Our funding 22 Plunket Board and Leadership 26 Financials 28 Funding Partners 34 Principal Partner 36 ISSN 0112-7004 (Print) ISSN 2537-7671 (Online) 1 OUR VISION OUR GOALS OUR MĀORI PRINCIPLES Our vision, Healthy tamariki – We make sure every Mana Atua – Mana Atua is the most Whānau tamariki/child has the opportunity to be important foundation pillar, enabling āwhina as healthy and well as they can be. Māori to reconnect to the source of Confident whānau – We build the creation, based on their realities as goals, In the first 1000 confidence and knowledge of whānau/ tangata whenua. The disconnection families across New Zealand. of tangata whenua from their Mana days we make Atua (resulting in a state of Wairua Connected communities – We make Matangaro) is a source of ‘haumate’ the difference sure no whānau/family is left isolated, strategic (unwellness). disconnected or unable to cope. of a lifetime Mana Tūpuna – Acknowledging OUR STRATEGIC THEMES the ancestral dimension, a person’s Tamariki, their whānau/family and connection to their ancestry through themes whakapapa (genealogy). communities are at the heart of everything we do. Mana Whenua – Mana Whenua High performing Plunket people. recognises the physical, spiritual and emotional connection to the land. This & Māori Integrated, collaborative and includes forests, swamps, pa sites, connected approach. rivers and other geographical entities, Plunket is a learning organisation elements each in their own right able to principles fuelled by knowledge, data and define a person’s tūrangawaewae (place insights. -
Presentation of September 4, 2010 Canterbury Earthquake
Presentation of September 4, 2010 Canterbury Earthquake William Godwin, PG, CEG AEG Vice President, 2019-20 Webinar – May 6, 2020 Introduction ► This presentation is on the 2010 Mw 7.1 Canterbury Earthquake. The earthquake occurred as I was traveling from San Francisco to Auckland, New Zealand to attend the IAEG Congress. Upon arrival I was asked to join the Geotechnical Extreme Events Reconnaissance (GEER) team to document damage from the event in the Christchurch area of the South Island. Little did I know that another smaller (Mw 6.2), yet deadlier earthquake would strike 5 months later in close to the same area. Introduction ► The purpose of the GEER is to observe and record earthquake induced phenomena and impacts to infrastructure before evidence is removed or altered as part of cleanup efforts. ► The reconnaissance was conducted by a joint USA-NZ-Japan team with the main funding for the USA contingent coming from GEER and partial support from PEER and EERI. ► This presentation includes my photographs from Sept. 8-10 supplemented with a few photos and observations noted in the GEER report, Nov. 2010. I also describe other seismic events from 2011-16. Sept 4th Darfield Earthquake ► At 4:35 am on September 4th NZ Standard Time (16:35 Sept 3rd UTC) the rupture of a previously unrecognized strike-slip fault (Greendale Fault) beneath the Canterbury Plains of New Zealand’s South Island produced a Mw 7.1 earthquake that caused widespread damage throughout the region. Surprisingly only two people were seriously injured, with approximately 100 total injuries. This compares with 185 deaths in the 2011 event Canterbury Earthquake Sequence Greendale Fault Rupture Characteristics Epicenter (focal) depth: 10.8km Tectonic Setting Ground Motion (pga) Geographical Setting Preliminary Observations ► Rock Avalanche, Castle Rock Reserve, Littleton, Christchurch ► Fault Offset, Telegraph Rd at Grange Rd.