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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.

Images, UC QuakeStudies

A photograph looking north down Colombo Street, from the intersection of Armagh Street. In the distance, rubble from the partially-collapsed Winnie Bagoes building can be seen on the road.

Images, UC QuakeStudies

A photograph of the earthquake-damaged Stone Chamber of the Canterbury Provincial Council Buildings on Durham Street North. Large sections of the Chamber have collapsed and the masonry and other rubble has spilled onto the footpath in front. To the left scaffolding constructed up the side of the building has also collapsed and twisted out of shape. Wire fences have been placed along the side of the building as a cordon.

Images, UC QuakeStudies

Dried liquefaction silt in North New Brighton. The photographer comments, "Here you can see the very fine surface layer of liquefaction starting to shrink, crack and then curl up on itself".

Images, UC QuakeStudies

Residents working to clear liquefaction from their properties in north-east Christchurch. The liquefaction has been piled on the side of the road where it will be collected by road maintenance contractors.

Images, UC QuakeStudies

The Christ Church Cathedral viewed from north Colombo Street. The collapsed tower can be seen as well as emergency personnel, including members of the police and the fire service, working in the rubble.

Images, UC QuakeStudies

Damage to TJ's Kazbah in New Brighton. The east and north walls and part of the upper floor have collapsed, tipping rubble and the contents of the rooms out onto the street. The photographer comments, "The occupants of the business and rooms all managed to escape alive. A digger was used to make the building safe and then used to sift through the rubble for any surviving belongings. It was a very emotional time for the ex-occupants".

Images, UC QuakeStudies

A collapsed section of road in north-east Christchurch. In the background, residents have piled liquefaction from their properties on the side of the road where it will be collected by road maintenance contractors.

Images, UC QuakeStudies

A collapsed section of road in north-east Christchurch. In the background, residents have piled liquefaction from their properties on the side of the road where it will be collected by road maintenance contractors.

Images, UC QuakeStudies

A photograph looking north up Colombo Street from near the intersection with Tuam Street. Building rubble litters the left side of the road, as well as the right in some places in the distance.

Images, UC QuakeStudies

A photograph looking north along Manchester Street from near the intersection with St Asaph Street. Badly-damaged buildings can be seen on each side of the street and the road has been closed off.

Images, UC QuakeStudies

A photograph of the north side of the ChristChurch Cathedral. The tower has been partially demolished with a large pile of rubble in front. The Citizens' War Memorial can be seen to the left.

Images, UC QuakeStudies

Dried liquefaction silt in North New Brighton. The photographer comments, "The liquefaction after the 23 December earthquake in Christchurch started to dry out and the thicker deposits started to curl up like broken drain pipe".

Images, UC QuakeStudies

A photograph of the north side of the ChristChurch Cathedral. The tower has been partially demolished leaving a large pile of rubble in front. The Citizens' War Memorial can be seen to the left.