Broken globe and fallen ornaments in an office in the Locke Building at the University of Canterbury.
Canta Magazine Volume 81 Issue 23 from 20 October 2010.
Canta Magazine Volume 81 Issue 21 from 6 October 2010.
Canta Magazine Volume 81 Issue 20 from 29 September 2010.
Canta Magazine Volume 81 Issue 19 from 20 September 2010.
Broken picture frame and fallen ornaments in an office in the Locke building at the University of Canterbury.
Fallen bookshelf and scattered books in a postgrad common room in the Locke Building at the University of Canterbury.
Provides information for students and staff of University of Canterbury in relation to the Canterbury earthquake of 22nd February 2011. Contains re-start timetable, transport options, latest announcements, FAQs, video and photo galleries, messages of support and sections devoted to the Library and the College of Education.
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Photograph captioned by Fairfax, "Dr Mark Quigley is a lecturer in the department of Geological Sciences at the University of Canterbury. His lecture on the Canterbury earthquake drew such interest that 600 were turned away".
Briefing for a University of Canterbury Staff Working Bee held in a lecture theatre before the cleanup begins on campus.
Briefing for a University of Canterbury Staff Working Bee held in a lecture theatre before the cleanup begins on campus.
At 4.35 a.m. on the 4th of September 2010 Christchurch residents were shaken awake by a magnitude 7.1 earthquake, the largest earthquake to hit urban New Zealand for nearly 80 years. It was a large earthquake. On average the world only has 17 earthquakes a year larger than magnitude seven. Haiti’s earthquake in January 2010 was magnitude 7.1 and Chile’s earthquake in February was magnitude 8.8. Although it was a big quake, Christchurch was lucky. In Haiti’s earthquake over 230,000 people were killed and in Chile 40,000 homes were destroyed. Happily this was not the situation in Christchurch, however the earthquake has caused considerable damage. The challenge for the Landscape Architecture community is to contribute to the city’s reconstruction in ways that will not only fix the problems of housing, and the city’s urban, suburban and neighbourhood fabric but that will do so in ways that will help solve the landscape problems that dogged the city before the earthquake struck.
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.
Photograph captioned by Fairfax, "Tim Stahl from Canterbury University maps the fault line west of Rolleston with GPS equipment after Saturday's earthquake".
The Resilient Organisations Research Programme and the University of Canterbury are undertaking a longitudinal study to examine the resilience and recovery of organisations within the Canterbury region following the 4 September Canterbury earthquake. The preliminary data suggest the physical, economic and social effects of the earthquake were varied across industry sectors within Canterbury. These preliminary results catalogue organisations’ perceptions of the: - disruptions to their ability to do business - challenges faced in the aftermath of the earthquake - factors that have helped mitigate the effects of the earthquake - revenue changes and projections for the duration of this change - financing options for recovery
Among the deformation features produced in Christchurch by the September 4th Darfield Earthquake were numerous and widespread “sand volcanoes”. Most of these structures occurred in urban settings and “erupted” through a hardened surface of concrete or tarseal, or soil. Sand volcanoes were also widespread in the Avon‐ Heathcote Estuary and offered an excellent opportunity to readily examine shallow subsurface profiles and as such the potential appearance of such structures in the rock record.
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.