1855 Wairarapa earthquake

1855 Wairarapa earthquake
Date 23 January 1855 (1855-01-23)
Magnitude 8.2–8.3 Mw
Depth 33 km
Epicenter 41°12′S 175°12′E / 41.20°S 175.20°E / -41.20; 175.20Coordinates: 41°12′S 175°12′E / 41.20°S 175.20°E / -41.20; 175.20
Areas affected New Zealand, North Island
Casualties 5–9 deaths

The 1855 Wairarapa earthquake occurred on 23 January at about 9 p.m., affecting much of the Cook Strait area of New Zealand, including Marlborough in the South Island and Wellington and Wairarapa in the North Island. In Wellington, close to the epicenter, shaking lasted for at least 50 seconds. The moment magnitude is estimated to have been in the range 8.2–8.3, the most powerful recorded in New Zealand since systematic European colonisation began in 1840.[1] This earthquake was associated with the largest observed movement on a strike-slip fault, maximum 18 metres (59 ft). It has been suggested that the surface rupture formed by this event helped influence Charles Lyell to link earthquakes with rapid movement on faults.[2]

Tectonic setting

New Zealand lies along the boundary between the Australian and Pacific Plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In the North Island the displacement is mainly taken up along the Kermadec subduction zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS).[3] A group of dextral strike-slip structures, known as the Marlborough Fault System, transfer displacement between the mainly transform and convergent type plate boundaries in a complex zone at the northern end of the South Island.[4] The earthquake occurred on the Wairarapa Fault which is part of the NIFS.

Earthquake characteristics

Map of the North Island Fault System showing the Wairarapa Fault
See also: Marine terrace

The earthquake was associated with the rupturing of approximately 150 km (93 mi) of the Wairarapa Fault. A horizontal displacement of up to 18 metres (59 ft) was accompanied by uplift and tilting of the Rimutaka Range on the northwestern side of the fault with vertical offsets of about 6 metres near the fault reducing to almost nothing on the western coast of the Wellington Peninsula. The estimated magnitude of about 8.2 is unusually large for an earthquake associated with movement on a mainly strike-slip fault, and the coseismic offset would have been the largest known for such an event. It has been suggested that this was caused by the rupture propagating down to where the fault links through to the top of the subducting Pacific Plate.[5] Geomorphological evidence, particularly the uplifted beach ridges observed at Turakirae Head, appears to record three previous coseismic uplifts of the Rimutaka Range caused by earthquakes similar in magnitude to the 1855 event, with a recurrence interval of about 2200 years.[6]


Wellington experienced severe shaking but the resulting damage was reduced as the city had been extensively rebuilt following the 1848 Marlborough earthquake using mainly wooden structures; only one recorded fatality (in a brick building) occurred. [7] Reports identify at least another four people (possibly as many as eight) as having died in the surrounding countryside during the earthquake. Numerous landslides were reported along the slopes of the Rimutaka Range. Minor damage was recorded in places as far away as Lyttelton and Christchurch.[8] The uplift of the northwestern side of Wellington Harbour rendered many of the jetties in the harbour unusable, although this new area of land provided a new rail and road route to the north.


The earthquake generated New Zealand’s largest historical locally generated tsunami, with a maximum run-up of 10–11 m (33–36 ft).[9] New Zealand's National Institute of Water and Atmospheric Research created an animated tsunami simulation model based on the 1855 Wairarapa event, which was screened on the television tele-drama "Aftershock" [10]

See also


  1. M 8.2 - 8.3, Wairarapa, 23 January 1855. GeoNet.
  2. Sibson, R.H. (2006). "Charles Lyell and the 1855 Wairarapa earthquake in New Zealand: Recognition of fault rupture accompanying an earthquake". Seismological Research Letters. 77 (3): 358–363.
  3. Mouslopoulou, V., Nicol, A., Little, T.A. & Walsh, J.J. (2007). "Terminations of large strike-slip faults: an alternative model from New Zealand". In: Cunningham, W.D. & Mann, P (eds). Tectonics of Strike-Slip Restraining and Releasing Bends. Geological Society of London, Special Publication, 290; p. 387–415.
  4. Van Dissen, R. & Yeats, R.S. (1991). "Hope Fault, Jordan Thrust, and uplift of the Seaward Kaikoura Range, New Zealand". Geology, 19, 393–396.
  5. Rodgers, D.W.; Little T.A. (2006). "World's largest coseismic strike-slip offset: The 1855 rupture of the Wairarapa Fault, New Zealand, and implications for displacement/length scaling of continental earthquakes". Journal of Geophysical Research. 111 (B12408). Bibcode:2006JGRB..11112408R. doi:10.1029/2005JB004065.
  6. McSaveney, M.J.; Graham, I.J.; Begg, J.G.; Beu, A.G.; Hull, A.G.; Kyeong, K. & Zondervan, A. (2006). "Late Holocene uplift of beach ridges at Turakirae Head, south Wellington coast, New Zealand". New Zealand Journal of Geology and Geophysics. 49 (3): 337–358. doi:10.1080/00288306.2006.9515172. Retrieved 3 September 2016.
  7. "The Earthquake of 1855", Early Wellington, 1928, Louis E. Ward
  8. "Effects of the Shock in other Parts". The Press. LVIII (11126). 19 November 1901. p. 5. Retrieved 6 June 2012.
  9. "Wairarapa tsunami, 23 January 1855". GeoNet. Retrieved 15 November 2013.
  10. NIWA tsunami animation – National Institute of Water and Atmospheric Research

Further reading

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