Because so much of the City of Christchurch and surrounding suburbs were built on loose sand and silt deposits, there was an unprecedented amount of damage from liquefaction following the February 2011 M6.2 earthquake. The severest of those events were the earthquake (magnitude from 7.0 to … The earthquake occurred on a conservative plate margin where the Pacific Plate slid past the Australian Plate in the opposite direction. E n v … Background . Effects. The epicenter of the quake … Many people are still missing. The earthquake occurred on New Zealand’s South Island 10km to the West of Christchurch, Canterbury. "However all earthquakes in the Christchurch region will be shallow, so the effect of a given earthquake will be worse than from a deeper plate boundary earthquake of the same magnitude." An interview with Dr Chris Leathart, GP, Christchurch and a member of the bpac nz Clinical Advisory Group. Loose soils behaved like quicksand, causing structures to suddenly sink, tilt, or even topple.
The epicentre was 6 miles South East of Christchurch and the focus was very shallow at 3.1 miles. The earthquake in February 2011 occurred at 12:51 p.m. and just 10 kilometers (6 miles) from the center of Christchurch. The Christchurch earthquake, February 2011. Initial effects: The economic heart of Christchurch is shut down. These events caused a small number of fatalities and considerable damage. It damaged or destroyed thousands of homes and buildings. Some of the secondary effests are: - uncertainty for the residents as to whether their homes are going to be condemned An effective plan … Infrastructure is damaged as are buildings and factories. The earthquake was caused by the two plates being forced together for a long time. On February 22, 2011, residents of the then-second-largest city in New Zealand – Christchurch, located on the South Island's Canterbury Plains – were hit hard by a magnitude 6.3 earthquake. Scientists find rare mix of factors exacerbated the Christchurch quake - 17/03/2011. (This is 23:51 21 February UTC). Christchurch being New Zealand’s second most populated city, there were many casualties caused by the earthquake. It was a 6.3 magnitude earthquake and the focus was very shallow at 4.99 km deep. It had a magnitude of 6.3, though was officially classified—scientifically speaking—as an aftershock of the 2010 quake. During 2010 and 2011, major earthquakes caused widespread damage and the deaths of 185 people in the city of Christchurch. This event was catastrophic in terms of impact, ... • Effects of the earthquake were reported by older people across different regions of New Zealand and these effects persisted over three years following the events. Media Animal welfare impact following the 4 September 2010 Canterbury (Darfield) earthquake 1 This survey was part of a Master of Emergency Management research report to develop recommendations to enhance companion animal emergency management in New Zealand. The earthquake, which was … The 2011 Christchurch earthquake was a 6.3 magnitude earthquake which struck the South Island of New Zealand at 12:51 pm on 22 February 2011 NZT. A key reason for this is that a double blow often occurs. Both schools were affected by the 2010 and 2011 Christchurch earthquakes. Cost: Like any other natural disaster it costs millions>billions of dollars. Following the quake, the central city was cordoned off, leaving it eerily quiet. Outcome measurement was mostly undertaken between 19 and 26 days after the September earthquake. This clip shows how central Christchurch looked after the earthquake of 22 February 2011. The earthquake struck the city of Christchurch in New Zealand on 22 February 2011. Outside of New Zealand, the earthquake became known as the "Christchurch Earthquake", and it resulted in the deaths of 185 people and injuries of several thousand. The primary effects of course are the loss of lives in the February 2011 quake, and the loss of and damage to property. The total economic loss caused by the 2010-2011 Christchurch earthquakes is currently estimated to be in the range between 25 and 30 billion NZ dollars (or 15% to 18% of New Zealand’s GDP). Then, more than five months after the mainshock, on 22 February 2011, a M6.3 aftershock occurred 5 km south-east of Christchurch at a depth of only 5 km. 2011 with its epicentre in Christchurch city. There is a case study sheet students can then complete which summarises this information. On the 22nd of February 2011, 12:51 pm a catastrophic earthquake hit Christchurch, New Zealand. On 22 February 2011, Christchurch was struck by a magnitude 6.3 earthquake which caused 185 deaths, thousands of injuries, and the destruction of the central business district. People are dislocated, injured, or busy trying to get their personal lives together. The earthquake … The epicentre was 6 miles South East of Christchurch and the focus was very shallow at 3.1 miles. Christchurch earthquake: Effects and responses A sorting resource covering the effects of and responses to the Christchurch earthquake, New Zealand. The Australian Plate and the Pacific Plate share a convergent plate boundary. In the Christchurch earthquakes there were a number of large-scale rock collapses in the areas to the south-east of the city. The 22 February 2011 earthquake caused 185 fatalities, injured 3,129 people, and 1,293 were injured in the aftermath. Primary effects of the March 2011 earthquake included over 15,000 people dead and 6,114 injured. On February the 2nd 2011 at 12:51 pm an aftershock of the September earthquake struck with a magnitude of 6.3 on the Richter scale. A significant earthquake hit Christchurch, in New Zealand’s South Island, at 12.51 pm local time (23:51 GMT) on Tuesday 22 February 2011. It was technically an aftershock from a larger earthquake in 2010 but the impacts were more severe. 2011 Christchurch earthquake. 16/03/2011 11:03 am Four seismic effects, including one that is rarely documented, combined to produce unusually strong ground-shaking in February’s magnitude 6.3 earthquake in Christchurch, scientists have found. The Christchurch earthquake of February 2011 .

It is possible that these initiatives were protective and prevented more significant adverse consequences being observed. The earthquake happened on a conservative plate margin between the Pacific Plate and the Australian Plate. One month on from the magnitude 6.3 earthquake that hit Christchurch on February 23, the physical and psycholigical effects are still being felt. It was a 6.3 magnitude earthquake and the focus was very shallow at 4.99 km deep. New Zealand is on the edge of a tectonic plate and is prone to earthquakes, same as Japan & California. An earthquake-damaged home stands at the edge of a cliff in Christchurch The earthquake struck on 22 February 2011. Many buildings were damaged or destroyed, while others appear untouched. However, many more people were displaced and homes destroyed. Christchurch Cathedral showing the effects of the February 2011 earthquake. It was the largest aftershock of … Effects: Devastation, continuous aftershocks, Trauma & Loss of life, Devastation, how much more descriptive do I need to be. It lasted only 10 seconds. Aftershocks were concentrated at the east end of the fault towards Christchurch as rock distorted by the original earthquake adjusted to new stresses. This earthquake had little effect causing some structural damage, only two people were injured. In the first place, there have been over 1000 earthquakes since the September 4th 2010 7.1 earthquake. As a comparison, the March 2011 earthquake and tsunami in Japan is estimated to have caused damage equivalent to around 3 to 4 percent of Japan’s annual GDP. A powerful 6.3-magnitude earthquake has struck the city of Christchurch on New Zealand's South Island, killing at least 65 people. Damaged school buildings resulted in state intervention which required amendment of the Education Act of 1989, and the development of ‘site sharing agreements’ in undamaged schools to cater for the needs of students whose schools had closed. One result of this readjustment was a damaging aftershock (magnitude 6.3) on 22 February 2011, when a fault ruptured very close to Christchurch. Killing 185 people, the 2011 Christchurch earthquake is recorded as the nation’s most deadliest national disaster. On 11 March 2011, Japan was hit by an earthquake of magnitude 9.0 on the Richter scale. Burwood was one of the hardest hit areas with over 50 per cent of the school zone designated "Red Zone" and a loss to the school roll in excess of 200 children. Apart from physical injuries, international literature suggests that psychosocial recovery after a disaster can take five to ten years. It struck the Canterbury region of the island and caused a lot of damage and many deaths in Christchurch, New Zealand's second largest city.. The epicentre was 10km away from Christchurch with a shallow focus of 5km. People needing elective surgery are unable to get it. Christchurch earthquakes of 2010–11, series of tremors that occurred within and near the city of Christchurch, New Zealand, and the Canterbury Plains region from early September 2010 to late December 2011. The Christchurch rebuild is forecast to start in earnest during the second half of 2012, continuing through to at least 2016. Students are asked to colour code the primary and secondary effects and the immediate and long-term responses. On Tuesday 22 February, 2011 at 12.51 pm the lives of hundreds of thousands of Cantabrians were changed forever. The June 2011 Christchurch earthquake was a shallow magnitude 6.0 M w earthquake that occurred on 13 June 2011 at 14:20 NZST (02:20 UTC).It was centred at a depth of 7 km (4.3 mi), about 5 km (3 mi) south-east of Christchurch, which had previously been devastated by a magnitude 6.2 M W earthquake in February 2011. It has an X rating on the Mercalli scale, signifying that it was an intense earthquake. This earthquake caused much more damage and had a greater impact on the area. At least 166 people died, and the city of Christchurch was devastated structurally and emotionally. About $2 billion worth of damage has been done, much of this damage will impede economic activity. These effects generally decreased with greater distance from the most directly affected regions of NZ and over time. Christchurch's Catholic cathedral damaged after the earthquake, in 2011. It was about 5 km underground.
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