In 1855 a magnitude 8.2 earthquake – the most powerful ever recorded in New Zealand – shook the southern part of the North Island. Caused by movement along a fault in Palliser Bay, it altered the landscape of the Wellington region.
The evening of 23 January 1855 was the end of a two-day holiday, the 15th anniversary of Wellington’s founding. Shortly after 9 p.m. a violent earthquake began; in Wellington the main shock lasted for at least 50 seconds. People fled outdoors, where they remained for the night in tents and makeshift beds, as continuous aftershocks rocked the area – there were an estimated 250 in the first 11 hours. The aftershocks continued for months. For the first day after the main quake, as far away as New Plymouth an almost continuous vibration could be felt by people sitting, or when leaning against walls.
After the 1848 Marlborough earthquake, many Wellington buildings had been mended in wood. Some new commercial lands, however, were constructed of brick because of fire risk. The 1855 earthquake damaged many of these, including the jail and the bank. The local council chambers and government offices, both two-storey wooden buildings, crumbled.
In 1931, New Zealand’s deadliest earthquake ruined the cities of Napier and Hastings. At least 256 people died in the magnitude 7.8 earthquake – 161 in Napier, 93 in Hastings, and 2 in Wairoa. Many thousands more required medical treatment.
On Tuesday morning, 3 February 1931, at 10.47 a.m., the ground in the Hawke’s Bay region heaved sharply upward and swayed.
Within minutes of the earthquake, fire began in three Napier chemist shops in the business district. Firefighters were almost helpless – water pressure faded to a trickle as the reservoir emptied. Attempts to pump sea water from the beach were short-lived. By mid-afternoon Napier’s business area was totally on fire. Some 36 hours later, after a remarkable attempt by firemen, volunteers and sailors working through the night, the fires were trampled. Almost 11 blocks of central Napier were gutted. Fires also sprang up in Hastings, but water supplies were available there shortly after the earthquake and fire damage was less extensive.
After the earthquake most homes lacked water, electricity, sewerage and chimneys, and people camped in open areas as continuous tremors made it dangerous to stay inside. Within a day the army had set up a tent camp that could house 2,500 people. Women and children were encouraged to leave the area, and refugee camps sprang up in a number of North Island towns.
Ten days after the quake, the region was shaken by the largest aftershock since the initial earthquake, a powerful magnitude 7.3 jolt that did yet more damage to already weakened buildings.