A photograph of a crowd of students listening to a band on the UCSA lawn. The photograph was taken during an Orientation Week in the 2000s.
A photograph of University of Canterbury students, including Babul Hasan (centre) dressed in graduation regalia.
A photograph of University of Canterbury alumnus Babul Hasan dressed in graduation regalia inside the University central library.
A photograph of University of Canterbury alumnus Babul Hasan being presented with his degree at a graduation ceremony.
A photograph of University of Canterbury alumnus Babul Hasan dressed in graduation regalia in Cathedral Square.
A PDF copy of a submission for the University of Canterbury student-run magazine, CANTA, written by UC alumnus Mike Gibbs.
A photograph of University of Canterbury alumnus Babul Hasan dressed in graduation regalia outside the Commerce building at the University of Canterbury.
Recurrent liquefaction in Christchurch during the 2010-2011 Canterbury earthquake sequence created a wealth of shallow subsurface intrusions with geometries and orientations governed by (1) strong ground motion severity and duration, and (2) intrinsic site characteristics including liquefaction susceptibility, lateral spreading severity, geomorphic setting, host sediment heterogeneity, and anthropogenic soil modifications. We present a suite of case studies that demonstrate how each of these characteristics influenced the geologic expressions of contemporary liquefaction in the shallow subsurface. We compare contemporary features with paleo-features to show how geologic investigations of recurrent liquefaction can provide novel insights into the shaking characteristics of modern and paleo-earthquakes, the influence of geomorphology on liquefaction vulnerability, and the possible controls of anthropogenic activity on the geologic record. We conclude that (a) sites of paleo-liquefaction in the last 1000-2000 years corresponded with most severe liquefaction during the Canterbury earthquake sequence, (b) less vulnerable sites that only liquefied in the strongest and most proximal contemporary earthquakes are unlikely to have liquefied in the last 1000-2000 years or more, (c) proximal strong earthquakes with large vertical accelerations favoured sill formation at some locations, (d) contemporary liquefaction was more severe than paleoliquefaction at all study sites, and (e) stratigraphic records of successive dike formation were more complete at sites with severe lateral spreading, (f) anthropogenic fill suppressed surface liquefaction features and altered subsurface liquefaction architecture.
Back in 2011, a slightly rusty three speed bike abandoned after the September earthquake on a demolition site in Christchurch caught the attention of John Smithies. He's 72, only slightly older than the bike, and he decided it would be just the bicycle to take on a epic, 2000 kilometre journey from Cape Reinga to Bluff. He started in September and expects to reach Bluff on Friday. He's making the epic journey in memory of his wife, Alison who died two years ago of a form of non-Hodgkin lymphoma. The ride down State Highway One is raising money for leukemia and blood cancer.
Greater Christchurch has been through a lot over the past 25 years, and its public transport is no exception. This paper aims to understand the broader factors that have influenced public transport patronage growth from 1999-2025. This is split into two periods, 1999-2010 and 2015-2025, before and after the 2010-2011 Canterbury Earthquake Sequence which fundamentally changed Greater Christchurch. Patronage grew from 9.7 to 17.2 million per year in this first period, unprecedented growth for this network, during a time of significant investment into the network. In contrast, 2015-2025 saw stagnation in growth, or even decreases, only growing after the COVID-19 pandemic. Patronage could not keep up with population growth after the earthquakes with growth mostly occurring in the outer areas of Christchurch and its satellite towns. People are less likely to bus from these areas due to long travel times into much of Christchurch, significantly longer than by car. Additionally, many businesses and employees moved outside of Central Christchurch, the main employment area for Greater Christchurch, after the earthquakes, into areas with relatively low bus routes. Significantly less people were willing to bus to work in these areas, apart from Riccarton and Papanui. However, businesses have been returning to Central Christchurch, with more people willing to bus to work there. These past determinants of growth are important to understand so that their effects can be individually researched more in-depth in future, to provide greater clarity on what have been successful factors for public transport growth in Greater Christchurch, and find out if they can be reimplemented or expanded to reignite some of the growth experienced in the 2000’s.
DAVID BENNETT to the Minister of Finance: How is the Government's economic programme helping to keep interest rates lower during this economic cycle, compared to the previous economic cycle in the mid-2000s? Dr RUSSEL NORMAN to the Minister of Energy and Resources: How much more is an average New Zealand household that uses 8,000kwh of power annually paying for electricity per year as of November 2013 compared to November 2008, according to the Ministry of Business, Innovation, and Employment's latest Quarterly Survey of Domestic Electricity Prices? Hon DAVID PARKER to the Minister of Finance: What will he do to "spread some of the benefits of growth" when hourly wage rates have only grown by 1.6 percent in the year to December 2013, which is close to 0 percent in real terms, when 45 percent of listed corporates have double-digit profit growth? JACQUI DEAN to the Minister for the Environment: What recent announcements has the Government made on the classification for drilling for oil and gas in New Zealand's Exclusive Economic Zone? GRANT ROBERTSON to the Minister of Justice: When she told the House yesterday "I had previously told Oravida that it could not use my name or photograph to endorse or promote its business products or services" when was that and what specific circumstances did it relate to? COLIN KING to the Minister for Tertiary Education, Skills and Employment: How is the Youth Guarantee Scheme helping the Government achieve the Better Public Services target of 85 percent of all 18-year-olds achieving NCEA Level two or an equivalent qualification in 2017? CAROL BEAUMONT to the Minister of Women's Affairs: Does she have confidence in the Ministry of Women's Affairs given their 2013 Annual Report shows that six out of seven policy outcomes have stayed the same or gone backwards in the last past year; if so, why? SCOTT SIMPSON to the Minister for Courts: How is the Government improving the way the Disputes Tribunal works to make it easier for New Zealanders to resolve civil disputes? Hon TREVOR MALLARD to the Minister of Internal Affairs: What action, if any, has he taken this year to show the Prime Minister that he has met the highest ethical standards required by Section 2.53 of the Cabinet Manual? ALFRED NGARO to the Minister of Pacific Island Affairs: What steps is the Government taking to lift the skills of Pacific people in New Zealand? DENIS O'ROURKE to the Minister for Canterbury Earthquake Recovery: Does he accept the conclusion in the Human Rights Commission's report Monitoring Human Rights in the Canterbury Earthquake Recovery that "many people affected by the earthquakes continue to experience deteriorating standards of living and impacts on their quality of life that go beyond the immediate effects of the disaster"? CATHERINE DELAHUNTY to the Minister of Energy and Resources: Has he had any discussions with any Indian Government Ministers about selling Solid Energy assets?