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Images, eqnz.chch.2010

A common scene around Christchurch, following the 7.1 magnitude earthquake that hit the city on Saturday September 4, 2010 at around 4:33am. The shake left many roads cracked, buildings demolished, and flooding in the streets.

Images, eqnz.chch.2010

Heaving and subsidence on the faultline left scars where the magnitude 7.1 earthquake on Saturday 4 September 2010 originated.

Images, eqnz.chch.2010

The latest (but temporary) tourist attraction in mid-Canterbury! This was the previously unknown faultline where the Saturday 4 September 2010 earthquake originated.

Images, eqnz.chch.2010

Tension cracks at least 300 mm deep, on the previously unknown faultline from which the Saturday 4 September 2010 earthquake originated.

Images, eqnz.chch.2010

20130808_2296_1D3-40 New Brighton bridge Prior to the earthquakes the stone wall at right was near road level. Now it is about 1.5m (4-5ft) lower. #4075

Images, UC QuakeStudies

A digitally manipulated photograph of a stencilled logo for the Christchurch School of Music. The photographer comments, "The Christchurch School of Music donated several old broken pianos to be placed on Gap Filler sites in Christchurch. Gap Filler make the land where buildings have been demolished into places the local inhabitants can enjoy. As in Maths two negatives make a positive".

Research papers, The University of Auckland Library

On 14 November 2016 a magnitude Mw 7.8 earthquake struck the upper South Island of New Zealand with effects also being observed in the capital city, Wellington. The affected area has low population density but is the largest wine production region in New Zealand and also hosts the main national highway and railway routes connecting the country’s three largest cities of Auckland, Wellington and Christchurch, with Marlborough Port in Picton providing connection between the South and North Islands. These transport facilities sustained substantial earthquake related damage, causing major disruptions. Thousands of landslides and multiple new faults were counted in the area. The winery facilities and a large number of commercial buildings and building components (including brick masonry veneers, historic masonry construction, and chimneys), sustained damage due to the strong vertical and horizontal acceleration. Presented herein are field observations undertaken the day immediately after the earthquake, with the aim to document earthquake damage and assess access to the affected area.

Images, UC QuakeStudies

A photograph of the Domo furniture store, White’s Building and the Edison Building on Tuam Street shortly after the 22 February 2011 earthquake. Members of the public can be seen walking down the road as they attempt to leave the central city.