Building Code compliance document E2/AS1 (2011) includes an exposure zone E, which is beachfront regions subject to rough seas and surf beaches. New Zealand lies along the boundary of the Australian Plate and the Pacific Plate. (GNS Science). The zones relate to the severity of exposure to wind-driven salt, with B being low risk, C medium risk and D high risk. About 20 percent of the region’s population live on soils prone to movement during earthquakes. New Zealand Earthquake fault zones including Kaikoura Area, Livingstone, Porters Pass-Amberly, Medbury, Cant Range Front, Spey-Mica Burn and Porters Pass-Amberly Fault Zone. According to GeoNet, over 2500 people have reported feeling it. A maximum of 100 earthquakes are displayed. Expert advice may be required in specific circumstances. a medium seismic risk if the area has a Z factor that is greater than or equal to 0.15 and less than 0.3; and; a high seismic risk if the area has a Z factor that is greater than or equal to 0.3. The colours on this map indicate the likely severity of shaking in different areas – in technical terms, the ground motion which has a 10% chance of occurring within 50 years. Earthquakes occur frequently in New Zealand as the country is situated in the collision zone between the Indo-Australian and Pacific tectonic plates, part of the Pacific Basin Ring of Fire, where many earthquakes and volcanoes occur. with a Weathertight Services claim, it is published under section 12 of the Weathertight Homes Resolution Services Act 2006. The interaction as these plates collide is responsible for much of New Zealand’s geography. For example, an up-to-date council-wide wind zone map would be considered higher-resolution data, and a site-specific wind zone calculation would be higher still. A = zone of intense earthquake activity, B = hot liquid basaltic magmas, C = andesitic, dacitic or rhyolitic magmas. Special considerations for suspended ceilings. The area in which a building is located has: Source: NZS 1170.5:2004 (Incorporating Amendment No 1). 18 Oct 02:24 : Magnitude recalculated from 3.9 to 4.2. the area within 100 m of tidal estuaries and sheltered inlets. Reproduced with permission from Standards New Zealand. The 1848 earthquake, centred in Marlborough, caused great damage to the brick and masonry buildings in Wellington, and the city was rebuilt mainly in wood; consequently it suffered comparatively little damage in the 8.2 magnitude earthquake of 1855, which lifted the land 2–3m. The corrosion zones in BRANZ Maps are our interpretation of the exposure zones in NZS 3604:2011. Find out how to build within the rules. Some parts of New Zealand are more likely to experience severe earthquakes than others. A maximum of 100 earthquakes are displayed. Evidence rests on a single report that has so far not been verified, Doublet earthquake: damaging in Oamaru & neighbouring settlements, Felt throughout North Island, Strong in Wanganui, Felt through North Island, chimney throughout Tairawhiti, Felt throughout Upper half of the South Island, Felt throughout lower half of the North Island, Felt throughout North Island & upper South Island. Microclimatic factors need to be considered in all locations. [2] Early settlers learned fairly quickly the importance of using appropriate building methods in an earthquake-prone country. For safe, healthy and durable buildings, all building work in New Zealand must meet certain standards. “No place in New Zealand is truly free of earthquakes,” he said. New building regulations meant that any new buildings constructed afterwards attempted to take earthquake shaking into account in building design.[3]. Special considerations for suspended ceilings. Most events occur along the main ranges running from Fiordland in the southwest to East Cape in the northeast. BRANZ Maps also include the changes to the zone boundaries in the Canterbury region introduced by the New Zealand Building Code clause B1 compliance document published in August 2011.

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