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Images, UC QuakeStudies

Dried liquefaction in North New Brighton. The photographer comments, "This shape formed as the liquefaction after the 23 December earthquake in Christchurch started to dry out".

Images, Canterbury Museum

One landscape colour digital photograph taken on 19 November 2011 showing part of the north side of London Street. The properties visible in the photograph are (from left to right) Tommy Changs Café, Canterbury Street, site of theatre erected for the Loons Circus Theatre Company production of Macbeth (being dismantled), Lyttel Arthouse (closed),...

Images, Canterbury Museum

One landscape colour digital photograph taken on 19 November 2011 showing part of the north side of London Street. The properties visible from left to right are Lyttel Piko Organic and Wholefoods, and Satchmo Café Pizzabar The Lyttelton streetscape has changed dramatically from its pre-earthquake appearance and will continue to change as new bu...

Images, Canterbury Museum

One landscape colour digital photograph taken on 19 November 2011 showing part of the north side of London Street. The properties visible from left to right are: Himalaya Design (obscured), Coffee Culture (downstairs), J Voyce and Co Ships Providore (upstairs), empty shop, and Lyttel Piko Organic and Wholefoods The Lyttelton streetscape has cha...

Images, Canterbury Museum

One landscape colour digital photograph taken on 19 November 2011 showing part of the north side of London Street. The properties visible from left to right are: part of Lyttel Piko Organic and Wholefoods, Satchmo Café Pizzabar, Milly May and Snoclothes New Zealand. The empty section was formerly occupied by No. 6 Cafe. The Lyttelton streetsc...

Images, Canterbury Museum

One landscape colour digital photograph taken on 19 November 2011 showing buildings on London Street. Visible in the photograph (left to right) are Bells Pharmacy - relocated into a converted house with law firm MacTodd on the upper floor, Portico (gift shop), Tommy Changs Cafe, and the edge of the Lyttelton Petanque Club Gap Filler initiative. ...

Research papers, University of Canterbury Library

Geomorphic, structural and chronological data are used to establish the late Quaternary paleoseismicity of the active dextral-oblique Northern Esk Fault in North Canterbury, New Zealand. Detailed field mapping of the preserved c. 35 km of surface traces between the Hurunui River and Ashley Head reveals variations in strike ranging from 005° to 057°. Along with kinematic data collected from fault plane striae and offset geomorphic markers along the length of the fault these variations are used to distinguish six structural subsections of the main trace, four dextral-reverse and two dextral-normal. Displacements of geomorphic markers such as minor streams and ridges are measured using differential GPS and rangefinder equipment to reveal lateral offsets ranging from 3.4 to 23.7 m and vertical offsets ranging from < 1 to 13.5 m. Characteristic single event displacements of c. 5 m and c. 2 m have been calculated for strike-slip and reverse sections respectively. The use of fault scaling relationships reveals an anomalously high displacement to surface rupture length ratio when compared to global data sets. Fault scaling relationships based on width limited ruptures and magnitude probabilities from point measurements of displacement imply earthquake magnitudes of Mw 7.0 to 7.5. Optically Stimulated Luminescence (OSL) ages from displaced Holocene alluvial terraces at the northern extent of the active trace along with OSL and radiocarbon samples of the central sections constrain the timing of the last two surface rupturing events (11.15 ±1.65 and 3.5 ± 2.8 ka) and suggest a recurrence interval of c. 5612 ± 445 years and late Quaternary reverse and dextral slip rates of c. 0.31 mm/yr and 0.82 mm/yr respectively. The results of this study show that the Northern Esk Fault accommodates an important component of the c. 0.7 – 2 mm/yr of unresolved strain across the plate boundary within the North Canterbury region and affirm the Esk Fault as a source of potentially damaging ground shaking in the Canterbury region.