Search

found 158 results

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of unstable and damaged buildings in the area. In the background is the Empire Hotel on London Street in Lyttelton. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of the unstable and damaged buildings in the area. On the left is the Empire Hotel where bracing has been placed on the front of the building. On the right is a shipping container in front of the damaged Wunderbar. The word 'coffee' has been spray painted on the side.

Images, UC QuakeStudies

A view down London Street in Lyttelton. The road has been closed to traffic because of unstable and damaged buildings in the area. In the background is the Empire Hotel on London Street in Lyttelton. Bracing has been placed on the front of the building to keep it together and limit further damage from aftershocks. The building has been cordoned off with fencing.

Videos, UC QuakeStudies

A video about Whare, a gift and homeware store which relocated several times after the 4 September 2010 earthquake. Whare originally had two stores, one in Beckenham, and another on Lichfield Street in the central city. Both stores were closed as a result of the 22 February 2011 earthquake. The store reopened temporarily in a garage and then in the Snowride Store on Lincoln Road. This video was part of The Press's 'Up and Running' series which showcases businesses which have stayed up and running despite the challenges posed by the 2010 and 2011 Canterbury earthquakes.

Images, eqnz.chch.2010

The permanent closure (to motor vehicles) of the Bexley red zone streets has started. This was once the main south-north route just west of the Avon River in the New Brighton area, till an expressway (ring road) was built about 80m to the west (right) about 12-13 years ago. Then it became just another suburban street, but now all the houses ...

Videos, UC QuakeStudies

A video of a protest against the merging of Phillipstown and Woolston Schools. Staff and students from Phillipstown School lead a march down Ferry Road to highlight the dangers children will face walking to school if Phillipstown is closed. The video also includes interviews with Phillipstown Principal Tony Simpson and Christchurch City Councillors Peter Beck and Makere Hubbard, about the protest and the merger.

Research papers, University of Canterbury Library

At 00:02 on 14th November 2016, a Mw 7.8 earthquake occurred in and offshore of the northeast of the South Island of New Zealand. Fault rupture, ground shaking, liquefaction, and co-seismic landslides caused severe damage to distributed infrastructure, and particularly transportation networks; large segments of the country’s main highway, State Highway 1 (SH1), and the Main North Line (MNL) railway line, were damaged between Picton and Christchurch. The damage caused direct local impacts, including isolation of communities, and wider regional impacts, including disruption of supply chains. Adaptive measures have ensured immediate continued regional transport of goods and people. Air and sea transport increased quickly, both for emergency response and to ensure routine transport of goods. Road diversions have also allowed critical connections to remain operable. This effective response to regional transport challenges allowed Civil Defence Emergency Management to quickly prioritise access to isolated settlements, all of which had road access 23 days after the earthquake. However, 100 days after the earthquake, critical segments of SH1 and the MNL remain closed and their ongoing repairs are a serious national strategic, as well as local, concern. This paper presents the impacts on South Island transport infrastructure, and subsequent management through the emergency response and early recovery phases, during the first 100 days following the initial earthquake, and highlights lessons for transportation system resilience.

Research papers, University of Canterbury Library

At 00:02 on 14th November 2016, a Mw 7.8 earthquake occurred in and offshore of the northeast of the South Island of New Zealand. Fault rupture, ground shaking, liquefaction, and co-seismic landslides caused severe damage to distributed infrastructure, and particularly transportation networks; large segments of the country’s main highway, State Highway 1 (SH1), and the Main North Line (MNL) railway line, were damaged between Picton and Christchurch. The damage caused direct local impacts, including isolation of communities, and wider regional impacts, including disruption of supply chains. Adaptive measures have ensured immediate continued regional transport of goods and people. Air and sea transport increased quickly, both for emergency response and to ensure routine transport of goods. Road diversions have also allowed critical connections to remain operable. This effective response to regional transport challenges allowed Civil Defence Emergency Management to quickly prioritise access to isolated settlements, all of which had road access 23 days after the earthquake. However, 100 days after the earthquake, critical segments of SH1 and the MNL remain closed and their ongoing repairs are a serious national strategic, as well as local, concern. This paper presents the impacts on South Island transport infrastructure, and subsequent management through the emergency response and early recovery phases, during the first 100 days following the initial earthquake, and highlights lessons for transportation system resilience.