Model: Liquefaction Volcano

Images, Canterbury Museum

Plastic and wood model of three liquefaction volcanoes. The working model pumps water over the grey surface which is decorated with a basket of laundry, a bucket of pegs and a football. The model is surrounded by artificial green grass and rests atop a black wooden base.

Memorial Guitar: Kia Kaha

Images, Canterbury Museum

One white over-painted hand-made electric guitar made primarily from ash and maple timbers, also incorporating wood from a variety of historic buildings in Canterbury damaged or destroyed in the 2010 - 2011 earthquakes including the Arts Centre, Kutwell’s Warehouse, Lyttleton main street pub, Timeball Station, Carlton Hotel, Merivale shops, bui...

Christchurch Press 29 June 2012: Section A, Page 2

Articles, UC QuakeStudies

Page 2 of Section A of the Christchurch Press, published on Friday 29 June 2012.

Bike Ride in the East Side - Photograph 55

Images, UC QuakeStudies

Tree stumps and wood chips from trees that were removed from the South Brighton pine forest. The photographer comments, "A Sunday afternoon ride to New Brighton, then back via Aranui, Wainoni, Dallington, and Richmond. Not a cheerful experience. South Brighton pine forest - gone! The pines had become poisoned by the rising saline water table, so they've all had to come out".

Geotechnical aspects of the Mw6.2 2011 Christchurch New Zealand Earthquake

Research papers, University of Canterbury Library

The 22 February 2011, Mw6.2 Christchurch earthquake is the most costly earthquake to affect New Zealand, causing an estimated 181 fatalities and severely damaging thousands of residential and commercial buildings. This paper presents a summary of some of the observations made by the NSF-sponsored GEER Team regarding the geotechnical/geologic aspects of this earthquake. The Team focused on documenting the occurrence and severity of liquefaction and lateral spreading, performance of building and bridge foundations, buried pipelines and levees, and significant rockfalls and landslides. Liquefaction was pervasive and caused extensive damage to residential properties, water and wastewater networks, high-rise buildings, and bridges. Entire neighborhoods subsided, resulting in flooding that caused further damage. Additionally, liquefaction and lateral spreading resulted in damage to bridges and to stretches of levees along the Waimakariri and Kaiapoi Rivers. Rockfalls and landslides in the Port Hills damaged several homes and caused several fatalities.