Greendale Land Survey Photograph 05

Images, UC QuakeStudies

A photograph of University of Canterbury Geology staff and students using a dynamic cone penetrometer to measure soil strength of a paddock on the Greendale fault line.

Greendale Land Survey Photograph 10

Images, UC QuakeStudies

A photograph of University of Canterbury Geology students using ground penetrating radar equipment to survey land on the Greendale fault line. From left: Matt Cockcroft, Zach Whitman and Dewiyani Bealing.

Greendale Land Survey Photograph 08

Images, UC QuakeStudies

A photograph of University of Canterbury Geology students using ground penetrating radar equipment to survey land on the Greendale fault line. From left: Matt Cockcroft, Zach Whitman and Dewiyani Bealing.

Greendale Land Survey Photograph 09

Images, UC QuakeStudies

A photograph of University of Canterbury Geology students using ground penetrating radar equipment to survey land on the Greendale fault line. From left: Matt Cockcroft, Zach Whitman and Dewiyani Bealing.

Greendale Land Survey Photograph 18

Images, UC QuakeStudies

A photograph of University of Canterbury Geology staff and students using ground penetrating radar (GPR) to survey land on the Greendale fault line. From left: Thomas Wilson, Zach Whitman and Matt Cockcroft.

Kim Wright WEMO Photograph 062

Images, UC QuakeStudies

A photograph of volunteers from the Wellington Emergency Management Office taking photographs of the lateral shifting and cracks in a road after the 4 September 2010 earthquake.

MVI_2430

Videos, eqnz.chch.2010

At Greendale Faultline on Highfield Road in mid-Canterbury, where the magnitude 7.1 earthquake on 4 September 2010 originated.

MVI_2425

Videos, eqnz.chch.2010

At Greendale Faultline on Highfield Road in mid-Canterbury, where the magnitude 7.1 earthquake on 4 September 2010 originated.

MVI_2424

Videos, eqnz.chch.2010

At Greendale Faultline on Highfield Road in mid-Canterbury, where the magnitude 7.1 earthquake on 4 September 2010 originated.

Executive Summary: Assessment of fault scarp rehabilitation on farms affec…

Articles, UC QuakeStudies

A report by Thomas Wilson, Zach Whitman, Matt Cockcroft, Mike Finnemore, Peter Almond, Derrick Moot, et al on various remediation techniques for farms on the Greendale fault scarp. The purpose of the report was to brief the Rural Recovery Group on 20 September 2010.

Executive Summary: Damage and Rehabilitation Survey of "On-Fault" Farms Af…

Articles, UC QuakeStudies

A report by Thomas Wilson, Peter Almond, Derrick Moot, Zach Whitman, Rose Turnbull, et al summarising a reconnaissance survey of farms on the Greendale fault. The purpose of the report was to inform farm and societal recovery. It was presented at a Rural Recovery Group meeting on 13 September 2010.

IMG_2437

Images, eqnz.chch.2010

This originally straight farm fence has been laterally displaced at least 2 metres where it crosses the previously unknown Greendale Faultline from which the Saturday 4 September 2010 earthquake originated.

The national seismic hazard model for New Zealand, and the Mw7.1 4 Septemb…

Research papers, University of Canterbury Library

A team of earthquake geologists, seismologists and engineering seismologists from GNS Science, NIWA, University of Canterbury, and Victoria University of Wellington have collectively produced an update of the 2002 national probabilistic seismic hazard (PSH) model for New Zealand. The new model incorporates over 200 new onshore and offshore fault sources, and utilises newly developed New Zealand-based scaling relationships and methods for the parameterisation of the fault and subduction interface sources. The background seismicity model has also been updated to include new seismicity data, a new seismicity regionalisation, and improved methodology for calculation of the seismicity parameters. Background seismicity models allow for the occurrence of earthquakes away from the known fault sources, and are typically modelled as a grid of earthquake sources with rate parameters assigned from the historical seismicity catalogue. The Greendale Fault, which ruptured during the M7.1, 4 September 2010 Darfield earthquake, was unknown prior to the earthquake. However, the earthquake was to some extent accounted for in the PSH model. The maximum magnitude assumed in the background seismicity model for the area of the earthquake is 7.2 (larger than the Darfield event), but the location and geometry of the fault are not represented. Deaggregations of the PSH model for Christchurch at return periods of 500 years and above show that M7-7.5 fault and background source-derived earthquakes at distances less than 40 km are important contributors to the hazard. Therefore, earthquakes similar to the Darfield event feature prominently in the PSH model, even though the Greendale Fault was not an explicit model input.