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Wellington Fault information


Wellington Fault
The Wellington Fault runs under California Drive in Totara Park, Upper Hutt. The road has been built extra wide with a central median to keep houses back from the fault line.
Map
 
Map of active Wellington Fault traces (red)
EtymologyDuke of Wellington
CountryNew Zealand
RegionWellington Region
CitiesWellington
Characteristics
RangeUp to 8 Mw[1]
Segmentsmultiple
Length170 km (110 mi)[2]
DisplacementUp to 7.6 mm (0.30 in)/year[2]
Tectonics
PlateAustralian
StatusActive
TypeDextral fault
AgeMiocene-Holocene
New Zealand geology database (includes faults)
Wellington Fault (blue) in context main strands of the North Island Fault System.

The Wellington Fault is an active seismic fault in the southern part of the North Island of New Zealand. It is a dextral (right-lateral) strike-slip fault with variable amounts of vertical movement causing uplift to the northwest, as expressed by a series of ranges. It forms part of the North Island Fault System, which accommodates the transfer of displacement along the oblique convergent boundary between the Indo-Australian Plate and Pacific Plate.

  1. ^ Cite error: The named reference van Dissen was invoked but never defined (see the help page).
  2. ^ a b Cite error: The named reference Langridge was invoked but never defined (see the help page).

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Wellington Fault

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The Wellington Fault is an active seismic fault in the southern part of the North Island of New Zealand. It is a dextral (right-lateral) strike-slip fault...

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North Island Fault System

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subduction. The faults include the Wairarapa Fault and Wellington Fault to the southwest, the Ruahine and Mohaka Faults in the central section and the Waimana...

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Wellington

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considerable damage in Wellington. The area has high seismic activity even by New Zealand standards, with a major fault, the Wellington Fault, running through...

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Geology of the Wellington Region

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Ohariu Fault, Wellington Fault, Wairarapa Fault, Reikorangi Fault, Otaki Forks Fault, and Wairangi Fault in the North Island. The Wairarapa Fault has an...

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List of fault zones

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This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...

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Wellington Harbour

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and a major earthquake fault line (the Wellington Fault) lies along its western shore. In 2014 another fault line (the Aotea Fault) was discovered extending...

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Wairarapa Fault

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earthquake. Geology of New Zealand Geology of the Wellington Region North Island Fault System Wellington Fault Rodgers, D.W.; Little T.A. (2006). "World's largest...

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Alpine Fault

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The Alpine Fault is a geological fault that runs almost the entire length of New Zealand's South Island, being about 600 km (370 mi). long, and forms...

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Geography of New Zealand

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"Defining the geometric segmentation and Holocene slip rate of the Wellington Fault, New Zealand: the Pahiatua section". New Zealand Journal of Geology...

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Maungaraki

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development on the Hutt Valley's western escarpment that runs along the Wellington Fault. Maungaraki translated from Māori means "northern mountain". This may...

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List of geological faults of England

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types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Many faults may have acted as both normal faults at one time and...

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Water supply in the Wellington region

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Wellington region involves the provision of drinking water services in the Greater Wellington region of New Zealand. Water supplies to the Wellington...

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Aro Valley

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active today. Aro Valley formed from fault activity. One kilometre to the west of Aro Valley is the Wellington Fault running north-east along the foot of...

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Wellington Region

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Greater Wellington, also known as the Wellington Region (Māori: Te Upoko o te Ika), is a non-unitary region of New Zealand that occupies the southernmost...

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Mangahao River

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Stream, which feeds the Mangatainoka River. The crush zone of the Wellington Fault probably assisted the capture. The capture has deepened the gorge cut...

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1934 Pahiatua earthquake

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(2007). "Late Holocene paleoseismicity of the Pahiatua section of the Wellington fault, New Zealand". New Zealand Journal of Geology and Geophysics. 50 (3):...

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1855 Wairarapa earthquake

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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...

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Te Ara Tupua

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are larger than usual because the site is on reclaimed land near the Wellington Fault. The bridge design also needed to take into account overhead electric...

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Battle of New Orleans

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entrenched enemy, caused lopsided British casualties.The Duke of Wellington faulted Cochrane and held that the attack could have succeeded were it not...

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Lifeline utility

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Wellington Lifelines Group published a report in 2019 examining the potential effects on Wellington of a magnitude 7.5 earthquake on the Wellington Fault...

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Southern Alps

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earthquakes on the Alpine Fault and other nearby faults. Despite the substantial uplift, most of the relative motion along the Alpine Fault is transverse, not...

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DEV Aratere

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moored fishing vessel in Wellington Harbour. 1 October 2004 – "30 seconds of potential disaster" after Aratere had a steering fault in the Marlborough Sounds...

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Lower Hutt

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city in the Wellington Region of New Zealand. Administered by the Hutt City Council, it is one of the four cities that constitute the Wellington metropolitan...

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1848 Marlborough earthquake

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Marlborough earthquake, Awatere Fault, New Zealand. New Zealand Journal of Geology and Geophysics 49, 375–382. "Damaged Wellington buildings (sketches by Robert...

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