![]() Earthquake damage in Masterton following the 24th June 1942 earthquake. | Earthquakes |
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| On Tuesday 23rd of January 1855, as the sky slowly darkened to twilight at the end of a summer's day, Wellington was preparing to go to bed. In a small 4-roomed house in Te Aro, the Darcy family sat playing dominoes by oil lamp. At 9.15 pm, without warning, the house began to move like 'waves on a sea'. The family were thrown to the floor and the chimney crashed through the roof, covering everything with bricks and dust. Pictures leaped from walls, tables overturned and their upright piano came down with a crash. In the Hutt Valley, Arthur Ludlam reported that the first shock lifted his house clean off the ground and shook it from side to side before it came crashing down. On Lambton Quay, Baron von Alzdolf was killed when his house of brick, one of the very few brick structures in Wellington, collapsed in on him. Wellington had just been struck by the most devastating earthquake since human occupation began. Though the 1855 earthquake was the most dramatic earthquake ever recorded in Wellington, many larger (and smaller) quakes have had a role in shaping our geography, our building practices, the lay-out of our city, and our social history. They have even led to the creation of urban myths - such as how until 1855, ships used to sail up what is now Kent and Cambridge Terrace, to dock at what is today the Basin Reserve. (a canal to the Basin Reserve was once planned but was never built!) Wellington is prone to earthquakes because it rests on the point where two tectonic plates meet. Kilometres beneath Wellington the light, thick Australian plate rides over the heavier, but thinner Pacific plate. These plate movements have resulted in three major fault-lines running either through or very close to Wellington City - the Ohariu Fault, the Wairarapa Fault, and the Wellington Fault. It is when one of these faults shifts suddenly that earthquakes occur. The number of earthquakes which occur in Wellington has led to our city becoming one of the world's leading centres for the study and research of earthquake activity and for the development of seismic strengthening techniques in buildings.
![]() Earthquake damage in upper Manners Street following the 1942 earthquake
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BOOKSNote that some of these are available as reference items only. You will find them within the New Zealand Reference Collection on the 2nd floor of the Central Library. Ask at the reference desk if you need help locating any of this material. Earthquakes / by G.A. Eiby. 551.22 EIB First published in 1957, G.A. Eiby's classic book has undergone several expansions and revisions. Though it is not Wellington specific, it remains one of the best introductions to earthquakes in New Zealand ever written. It covers what happens inside the earth to cause earthquakes, why and where they occur in New Zealand, the different types of seismographs available and how they work, and how buildings are affected by earthquakes.
A night of terror : Wairarapa's 1942 earthquake / Jan McLaren. (Reference Only)
Caught in the Crunch : Earthquakes and Volcanoes in New Zealand / by Rebecca Ansell and John Taber.
Magnitude Eight Plus : New Zealand's Biggest Earthquake / by Rodney Grapes.
Wellington's Restless Coast : Changes in Land and Sea at Turakirae Head / by G.R. Stevens.
More Earthquakes Explained / by J.J Aitken and M.A. Lowry
Earthquakes and Uplift History of the Miramar Peninsular, Wellington / by Brad Pillans and Phil Huber
NEWSPAPERS
The library has been collecting newspaper clippings for a number of years and storing them in a vertical file. Please ask the Reference Desk staff on the 2nd floor of the Library if you would like to see the file. In addition to this, the library has microfilmed copies of the major Wellington daily newspapers back to 1865. Here are some dates of larger earthquakes which were felt in Wellington. Some of these resulted in considerable damage to buildings and property in the Wellington region. You can look up microfilmed copies of the newspapers from around these dates to see how these quakes were reported.
9th August 1904
The Institute of Geological and Nuclear Sciences.
GeoNet.
The Wellington Emergency Management Office (WEMO)
The Earthquake Commission.
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