Science: Earth Sciences
Audio, Radio New Zealand
Dr Hamish Campbell of GNS Science talks about the Christchurch earthquake and it's subsequent aftershocks.
Dr Hamish Campbell of GNS Science talks about the Christchurch earthquake and it's subsequent aftershocks.
Erosion to earthquakes with geologist and paleontologist Dr Hamish Campbell from GNS science. Chatham Islands geology and it's links with Christchurch and Canterbury.
A video of a press conference with GNS Scientist Kelvin Berryman. Berryman explains the recent aftershocks which have hit Christchurch.
A video of a press conference with GNS Scientist Kelvin Berryman. Berryman explains the recent aftershocks which have hit Christchurch. The end of the video shows the press conference being interrupted by an aftershock.
Blog of Julian, educational outreach facilitator at GNS Science. Includes information on GNS Science field trips; explanations of New Zealand geology; video clips; and sections on the Christchurch earthquakes, and New Zealand fossils.
Senior Siemologist at GNS Science comments on this morning's earthquake in Canterbury.
A paper which details earthquake expectation data, supplied to SCIRT by GNS Science.
Geologist and paleontologist at GNS Science Hamish Campbell discusses the geology behind the Christchurch earthquake.
John Townend is a seismologist for GNS; and an Associate Professor at the School of Geography, Environment and Earth Sciences.
John Townend is a seismologist for GNS; and an Associate Professor at the School of Geography, Environment and Earth Sciences.
John Townend is a seismologist for GNS; and an Associate Professor at the School of Geography, Environment and Earth Sciences.
John Townend is a seismologist for GNS; and an Associate Professor at the School of Geography, Environment and Earth Sciences.
A public talk by Dr Kelvin Berryman, Director of Natural Hazards at GNS Science. This talk, entitled 'What's underneath? Understanding seismic science', formed part of the Plenary Two session, 'Clearing the decks'.
A video of a keynote presentation by Professor David Johnston, Senior Scientist at GNS Science, at the 2016 Seismics in the City Conference. The presentation is titled, "The Trajectory of Post-disaster Recovery and Regeneration: The social dimension".The abstract for the presentation reads, "A consideration of social regeneration and what that means for Canterbury moving forward plus current recovery trajectories and ways of measuring progress."
Scientists from GNS Science have faced tough criticism at the Royal Commission into the Canterbury earthquakes, being accused of funneling resources into the wrong areas and giving vague advice on earthquake risks.
A video of a presentation by Andrew King of GNS Science on "The Natural Hazards Research Platform and National Science Challenge". The presentation was delivered at the Learning from Lifeline Week and Planning Collaborations forum as part of the University of Canterbury's Lifeline Week.
An infographic describing research into historic earthquakes on the Greendale Fault.
A magnitude 5.1 earthquake struck Canterbury Monday night. Four thousand people reportedly felt the quake, which was centred 30 kilometres west of Methven. GNS Science seismologist Dr Jonathan Hanson spoke to Ingrid Hipkiss.
A video of Dr Laurie Johnson of the Pacific Earthquake Engineering Research Centre and Professor David Johnston, Senior Scientist at GNS Science, responding to questions from the floor during the keynote session at the 2016 Seismics in the City Conference. The keynote session is titled, "The Trajectory of Post-disaster Recovery and Regeneration".
A video of a presentation by Dr Rob Buxton of GNS Science on "Modelling interdependencies of critical infrastructure". The presentation was delivered at the learning forum on Interdependencies of Lifeline Systems as part of the University of Canterbury's Lifeline Week.
A video of a presentation by Michelle Daly of GNS Science on the "Economics of Infrastructure Resilience EoRI project". The presentation was delivered at the learning forum on Interdependencies of Lifeline Systems as part of the University of Canterbury's Lifeline Week.
A blog post from US Ambassador to New Zealand and Samoa, David Huebner, titled, "Craig Weaver Remembers February 22nd".
This report provides information on the locations and character of active geological faults and folds in Ashburton District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of permanent fault movement at the ground surface, and where more detailed investigations should be done if development is proposed in that area (depending on the potential activity of the fault and the type of development proposed). See Object Overview for background and usage information. Most of the faults and folds identified at the ground surface in Ashburton District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region.
This report assesses issues and options for preparing an earthquake hazard and risk assessment programme for Canterbury. It outlines investigation options and associated costs in order to better understand Canterbury's earthquake hazard and risk. Although earthquake hazard and risk information needs and investigation priorities within Canterbury have changed over the past 15 years, the majority of the report’s recommended components have been undertaken to some degree either by Environment Canterbury or other organisations. See Object Overview for background and usage information.
The previously unknown Greendale Fault ruptured to the ground surface, causing up to 5 metres horizontal and 1 metre vertical permanent offset of the ground, during the September 2010 Darfield (Canterbury) earthquake. Environment Canterbury commissioned GNS Science, with help from the University of Canterbury, to define a fault avoidance zone and to estimate the fault recurrence interval. There is little evidence for past movement on the fault in the past 16,000 years. However, because of the uncertainties involved, a conservative approach was taken and the fault has been categorised as a Recurrence Interval Class IV fault (a recurrence interval of between 5,000 and 10,000 years). A PhD study by a University of Canterbury student will work towards refining the Recurrence Interval Class over the next three years. Taking a risk-based approach, the Ministry for the Environment Active Fault Guidelines recommend that normal residential development be allowed within the fault avoidance zone for faults of this Recurrence Interval Class, but recommends restrictions for larger community buildings or facilities with post-disaster functions. The report is assisting Selwyn District Council in granting consents for rebuilding houses on or near the Greendale Fault that were damaged by permanent distortion of the ground due to the fault rupture in the September 2010 earthquake. The report provides specific recommendations for building on or close to the Greendale Fault, which are being implemented by Selwyn District Council. See Object Overview for background and usage information.
This study updated the 1999 Earthquake hazard and risk assessment study Stage 1 Part B: Probabilistic seismic hazard assessment and Earthquake scenarios for the Canterbury region, and historic earthquakes in Christchurch report. It incorporated new fault data, a new distributed seismicity model and new methods for estimating Modified Mercalli intensities. See Object Overview for background and usage information.
This report provides information on the locations and character of active geological faults and folds in Mackenzie District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of fault movement, and where more detailed investigations should be done if development is proposed in that area(depending on the potential activity of the fault and the type of development proposed). Most of the faults and folds identified at the ground surface in Mackenzie District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region. See Object Overview for background and usage information.
This study updated the 1999 Earthquake hazard and risk assessment study Stage 1 Part B: Probabilistic seismic hazard assessment and Earthquake scenarios for the Canterbury region, and historic earthquakes in Christchurch report. It incorporated new fault data, a new distributed seismicity model and new methods for estimating Modified Mercalli intensities. See Object Overview for background and usage information.
This report provided information on the location and character of the Ostler Fault Zone near Twizel. The fault traces, and associated recommended fault avoidance zones, were mapped in detail for inclusion in a District Plan Change for the Twizel area. The Ostler Fault Zone was mapped in detail because of the higher likelihood of movement on that fault than others in the district, and the potential for future development across the fault zone because of its proximity to Twizel. See Object Overview for background and usage information. The report recommended that the information be incorporated into the District Plan Change and that site-specific investigations be undertaken before development is allowed within the fault avoidance zones. These recommendations were taken up by Mackenzie District Council.
Topics - The Gettysburg address, the short speech given by Abraham Lincoln 150 years ago today, the finest short speech in the English language, and one of the great political utterances of all time. A strong earthquake that hit Christchurch last night has been upgraded by GNS Science to a magnitude 4.6. It was also shallower than first believed, with GNS reporting it was 8km deep rather than 11km. Wallabies rugby coach Ewen McKenzie has made no apologies for suspending six of his players in what's been described as "a hard-line move designed to set the standards required to win the 2015 World Cup".