Named ‘the most damaging earthquake since Hawke's Bay Earthquake in 1931’ the epicentre was 40 km west of Christchurch City, and the depth of the quake was at 10 km below the surface of Canterbury Plains. It would result in 156,619 insurance claims according to the Earthquake Commission, costing $2.487 billion. A major feature of the surface fault rupture was the large dextral displacements. Commemoration is an important part of healing and growing, but also of learning lessons, some of which are especially relevant today, he says. many aftershocks were recorded along the Greendale Fault indicates the readjustment process of the earth’s crust to a major fracture. The epicentre was close to the town of Darfield.

A must see when you come to New Zealand is the beautiful heritage buildings. Read more about the 2010 Canterbury earthquakes on NZHistory.
“You only need to scratch the surface in conversation with Selwyn residents and others across Canterbury to realise that damage done in those 40 seconds has etched itself in to the memories of all those that were jolted awake that morning.

Photo: Selwyn District Council, Lincoln Uni win premier netball bragging rights, New motorway on-ramp an 'issue' concedes NZTA, Compulsory micro-chipping of cats out of draft animal bylaw, Soldier sentenced over assaults still serving at Burnham Military Camp, Golf course goes for $6.6m after owner's death, Serious crash between car and milk tanker in Dunsandel, Govt green lights new Lincoln Uni science centre, Person critical after incident at Christchurch Adventure Park, Baby Daxton fights for life after four brain surgeries, Two Covid cases reported, no new community cases, Kiwi police officer killed in line of duty in London.
Collapsed brick walls in Worcester Street (1st of 2), Aftershocks, 4 September 2010 to 21 February 2011, Flickr exhibition: earthquake damage in Christchurch, September 2010. © Crown Copyright. All text licensed under the Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence unless otherwise stated. Cracks opened up close to rivers and streams where the ground moved down towards the water, causing damage to man-made structures – a process known as lateral spreading. The earthquake began on the (also unknown) Charing Cross Fault several kilometres to the north of the Greendale Fault, and the entire rupture involved at least six fault segments.

This is exactly how it must of waking up in the epicentre of the Darfield earthquake in New Zealand. Over the past couple of years, there have been measures put in place to help protect utilities, these include; flexible joints or ductile pipes have been used for water pipelines across unstable ground to prevent bursts. Darfield is a town in the Selwyn District of the South Island of New Zealand. The ground above the liquidised layers subsided unevenly, cracking footpaths, roads and houses. It was a relatively shallow earthquake – about 10 kilometres below the surface of the Canterbury Plains. © Copyright Star Media Network 2019.

All of these items have been created in the last 50 years, who knows what else there is to come? The area north of the fault rupture moved eastwards and the area south of it westwards.

An early Treasury estimate of the cost of the earthquake was $4 billion.

Named ‘the most damaging earthquake since Hawke's Bay Earthquake in 1931’ the epicentre was 40 km west of Christchurch City, and the depth of the quake was at 10 km below the surface of Canterbury Plains. The Darfield War Memorial will be lit up on Thursday and Friday. You are not permitted to download, save or email this image. Visit image gallery to purchase the image.

It was a relatively shallow earthquake – about 10 kilometres below the surface of the Canterbury Plains. Create your own unique website with customizable templates.

In its place, a commemorative video featuring Mayor Sam Broughton, The New Zealand Army Brass Band and a Darfield High School student, will be released tomorrow (Friday 4 September) on the Council website, Facebook and YouTube Channel.

The 2011 Christchurch earthquake, Creative Commons Attribution-NonCommercial 3.0 New Zealand Licence. Of those, EQC said 276 claims relating to the September 2010 event were still open as of this week. GeoNet earthquake reports were sent out using both Twitter and Facebook after each major aftershock. New support and connections were made as we rebuilt our lives together. The aftershocks were mainly clustered along the Greendale Fault, reflecting gradual readjustment of the earth’s crust to a major rupture.


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