Commemoration stone of the 1987 earthquake in Edgecumbe.
The Edgecumbe earthquake of 1987 was an earthquake measuring 6.3 on the Richter scale that struck the Bay of Plenty region of New Zealand on 2 March 1987 just after 1.42 pm, centred on the town of Edgecumbe. The earthquake was very shallow, being centred approximately 8 km from the Earth's surface. The earthquake was one of the most damaging New Zealand's North Island has experienced in recent decades, with approximately 50% of the houses in Edgecumbe being damaged by the quake. There was extensive damage to a local milk factory, with large storage tanks toppled. Kawerau was another nearby town that suffered damage and Whakatane was also badly shaken. An 80-tonne New Zealand Railways DC class locomotive was thrown onto its side.
The earthquake caused no fatalities;[1][2][3] one person died at the time as a result of a heart attack, possibly due to the quake.[4] A foreshock just minutes before had cut the power supply and many people had moved away from heavy machinery and out of their houses. The largest aftershock was measured at 5.2 and struck at 1.52 pm.
A crack 7 kilometres (4.3 mi) long opened in the Rangitaiki Plains near Edgecumbe as a result of the earthquake. It is now known as the 'Edgecumbe Fault'. At one point, the land close to the fault dropped 2 metres (6.6 ft).
The epicentre of the quake was approximately 2.24 kilometres (1.39 mi) south-south-east of the town of Matata, or 15 kilometres (9.3 mi) north-north-west of Edgecumbe.[5] The intense ground shaking caused by the earthquake led to a large number of ground surface failures, including sand boils, ridge-top shatters and debris avalanches on steeper slopes.[6]
See also
References
|
|---|
| | Pre-colonisation |
- 1100 Alpine Fault
- 1460 Wellington
- 1600s Alpine Fault
- 1717 Alpine Fault
- 1815 New Plymouth
- 1817 Fiordland
- 1826 Fiordland
- 1835 Manukau
- 1838 Waitotara Forest
|
|---|
| | Modern | |
|---|
| | Related articles | |
|---|
|
New Zealand