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The earthquake caused widespread damage across Christchurch, especially in the central city and eastern suburbs, with damage exacerbated by buildings and infrastructure already being weakened by the 4 September 2010 earthquake and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The shallow earthquake was reported to be felt across the South Island and the lower and central North Island. While the initial quake only lasted around 10 seconds, the vicinity and depth of its location to Christchurch in addition to the previous quakes were the reason for so much destruction.
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