A sign on a cordon fence. It says 'The number 1 hazard is you! Put the Hazard Board at front of site. All visitors must read the Hazard Board. Induct all visitors with Induction Cards'.
Photograph captioned by BeckerFraserPhotos, "792 Colombo Street".
A photograph of the entrance to Ballantynes on Cashel Street. A sign by the door that states the building is a construction site and a multiple hazards area.
A photograph of a sign on the RAD Bikes bike shed on Gloucester Street. The sign reads "RAD Bikes Recycle A Dunger. This is an ex-demolition site. Hazards may exist. Please take care".
A photograph of organisers of LUXCITY on the corner of Manchester Street and Gloucester Street. A site hazards board is leaning against a white van, in front of students in high-visibility vests who are setting up the Pavilions & Lighting Devices market.
This report provided information on the location and character of the Ostler Fault Zone near Twizel. The fault traces, and associated recommended fault avoidance zones, were mapped in detail for inclusion in a District Plan Change for the Twizel area. The Ostler Fault Zone was mapped in detail because of the higher likelihood of movement on that fault than others in the district, and the potential for future development across the fault zone because of its proximity to Twizel. See Object Overview for background and usage information. The report recommended that the information be incorporated into the District Plan Change and that site-specific investigations be undertaken before development is allowed within the fault avoidance zones. These recommendations were taken up by Mackenzie District Council.
This study analysed liquefaction susceptibility and estimated ground settlements for two earthquake scenarios (foothills and Alpine Fault) for eastern Waimakariri District. The report was later partially superseded by Earthquake hazard assessment for Waimakariri District (Yetton and McCahon, 2009), which while not using such detailed analytical methods as the 2000 Beca report, reviewed new information available since 2000 (including that collected as part of the Pegasus Town development). This showed that the liquefaction susceptibility in eastern Waimakariri district was in fact much more variable than suggested in the 2000 Beca maps, and that liquefaction susceptibility was extremely difficult to predict without a site-specific investigation. See Object Overview for background and usage information.