The fault runs along the Hutt River.at the foot of the Western Hills |
View across Lower Hutt to the Wellington Fault scarp |
Regional Faults in the Lower North Island |
You can find out information about all of New Zealand's known active faults on the GNS Science Active Faults Database, but in this image you can see a screen grab of those known in the Wellington area, some of them labelled:
As you can see there are many other faults in the region, each of which is capable of rupturing, so that the real possibility of a large earthquake occurring at some point from one or other of the faults is something that should inspire everyone to be prepared. (Make some time to go to https://getready.govt.nz/ )
Here is an aerial view of the Wellington Fault trace passing through California Park in Upper Hutt and along California Drive beyond - centre top to bottom right of the photo. The fault is an oblique slip fault, with mostly horizontal movement but some vertical displacement as well when it ruptures.
The entrance to Wellington City at Thorndon is a bottleneck, where the Wellington Fault passes underneath the railway, State Highway and Ferry Terminal, as well as the water supply. This makes Wellington vulnerable to being cut off by a rupture of the Wellington Fault.
This video gives you more information and shows you various locations that you can visit to learn about the Wellington Fault and some of its features:
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