A photograph of University of Canterbury Geology students surveying land on the Greendale fault line.
One oblong perspex covered 3-D model of the fault plains that ruptured to cause the 22 February and 13 June 2011 earthquakes; top of the model also acts as a map overlay. This model provides a visual demonstration of the geological forces that caused the 22 February and 13 June 2011 earthquakes. These forces were so strong that parts of the Por...
One oblong perspex covered 3-D model of the fault plains associated with the 4 September 2010 Darfield earthquake; top of the model also acts as a map overlay. Geologists continue to study the 4 September 2010 earthquake and consider it is likely to have been a complex event with several faults rupturing simultaneously. This model provides one ...
A photograph of University of Canterbury Geology staff and students using ground penetrating radar (GPR) to survey land on the Greendale fault line.
A photograph of University of Canterbury Geology student Matt Cockcroft using ground penetrating radar (GPR) to survey land on the Greendale fault line.
A photograph of University of Canterbury Geology staff and students using ground penetrating radar (GPR) to survey land on the Greendale fault line.
A photograph of University of Canterbury Geology student Matt Cockcroft using ground penetrating radar (GPR) to survey land on the Greendale fault line.
A photograph of University of Canterbury Geology students Zach Whitman and Dewiyani Bealing using ground penetrating radar equipment to survey land on the Greendale fault line.
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.
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.
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.
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.
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.
Two huge wrestlers, one representing 'Port Hills fault' and the other 'Greendale fault' struggle together over a broken Christchurch. Another wrestler, representing 'Other faults' appears in the distance yelling 'Is it my turn yet?' Context - Christchurch has now had three major earthquakes and thousands of aftershocks. It now appears likely that the Christchurch quakes resulted from activity on a fault extending directly eastward from the Alpine fault that remained unknown until last year, says Roger Musson, a seismologist at the British Geological Survey in Edinburgh. The new fault first came to light last September (4th) when a stronger but less calamitous quake shook Darfield, 40 kilometres west of Christchurch. Musson says the latest quake (Feb 22, 2011) probably resulted from an eastward continuation of activity on the same fault. "It has probably not moved for tens of thousands of years, so lots of strain built up," says Musson. The third major quake happened on 13th June 2011. (New Scientist - February 22, 2011) Quantity: 1 digital cartoon(s).
Text at top left reads 'Daft things our forefathers did The cartoon shows several nineteenth century gentlemen observing 'volcanic cones', a 'swamp' and 'faultlines underneath' and deciding to build a city. Context - Specifically the Christchurch earthquakes of 4 September 2010 and 22 February 2011 but generally the way many New Zealand cities are built on or near volcanoes, faultlines and swamps. Quantity: 1 digital cartoon(s).
Rolleston/Burnham, South Island, NZ It's been a busy few weeks! Was away on geology fieldtrips all the previous two weeks, then on Saturday morning 4th September 2010 at 4.35 am we got woken in Westport to a reasonable but very long earthquake. My husband was back in Christchurch at the time and texted me saying "are you ok?". I replied, "yes!"...
Under the caption, young people carrying their baggage flutter into the air, away from Canterbury and toward 'Oz'. In September GNS Earth Sciences reported that after the earthquakes, the Greendale and associated faults were still moving as they settled into a new configuration. At the same time the young were leaving Canterbury (and New Zealand) for a better future in Australia. The population of New Zealand was moving into a new configuration. Quantity: 1 digital cartoon(s).