↑ "Strong earthquake rocks New Zealand's South Island"."Marlborough, Kaikoura escape worst of quake". ↑ Van Der Heide, Maike (4 September 2010).Archived from the original on 6 September 2010. ↑ "New Zealand Earthquake Report - at 11:12 am (NZST)".Archived from the original on 7 September 2010. ↑ "New Zealand Earthquake Report - at 4:56 am (NZST)".↑ "New Zealand Earthquake 2010: Strong Quake Shakes Christchurch".Archived from the original on 25 August 2011. ↑ 2.0 2.1 2.2 "Magnitude 7.0 - South Island of New Zealand: Details".The 2010 earthquake was centred about 80–90 km to the southeast of the plate boundary through the island, probably on one of a network of smaller faults linked to the main faults that mark the plate boundary itself. In the South Island, these plates mainly slide past each other horizontally, producing earthquakes along fault lines such as the Alpine fault. New Zealand sits on the boundary between the Australian and Pacific plates. Ī state of emergency was declared by Civil Defence for Christchurch and the Selwyn District. The total cost of damages may be as high as NZ$2 billion. Businesses in the city centre were closed the day of the quake. The quake caused damage to historic buildings in Lyttelton, near Christchurch, including a church and parts of a hotel. It caused a lot of damage and cut off power and water supply, mainly in the city of Christchurch. The main quake was felt widely across the South Island, and in the North Island as far north as New Plymouth. Strong aftershocks were reported, including ones of magnitude 5.3. It was centred 40 km west of Christchurch, near the town of Darfield, at a depth of 10 km. The 2010 Canterbury earthquake was a powerful 7.1 magnitude earthquake, which struck the South Island of New Zealand at 4:35 am Septemlocal time (16:35 3 September UTC). It seeks to provide a sense of the experiences and the potential meanings that were derived from being part of this 'moment in time'.Įxamples of innovations in practice emerged during the earthquake response and a number of recommendations for nursing practice are identified. This paper presents an overview of the earthquakes and experiences of nurses working during this time, identifying a range of issues that will benefit from further exploration and research. However, little is known regarding the impact of this, either in personal or professional terms. Nurses played a significant role in the response to the earthquakes and its aftermath. The establishment of an injury database allowed for an accurate picture to emerge of the injury burden, and each of the authors was present and worked in a clinical capacity during the earthquake. SOURCES OF EVIDENCE: This paper developed following interviews with nurses who worked during this period, and draws on literature related to healthcare responses to earthquakes and natural disasters. Staff working in the only emergency department in the city were faced with an external emergency while also being directly affected as part of the disaster. While the highest magnitude quake occurred in September 2010, registering 7.1 on the Richter scale, it was the magnitude 6.3 event on 22 February 2011 which was associated with the greatest injury burden and loss of life. The location of these, around and within the major city of Christchurch, was unexpected and associated with previously unknown fault lines. NZ has experienced earthquakes and aftershocks centred in the Canterbury region of the South Island. To outline the impact of the Canterbury, New Zealand (NZ) earthquakes on Christchurch Hospital, and the experiences of emergency nurses during this time.
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