Images may be subject to copyright laws and are therefore not of reproduction quality. 2012.I.21 The south side of the fault moved generally up and west, while the north side moved down and east. These forces were so strong that parts of the Port Hills have risen by more than 40 cm. If you would like to participate, you can choose to edit this article, or visit the project page for more information.
(There is a lot of basalt above much of it.) When it ruptured, the energy shot northwest straight across the city.Layers of sediment below Christchurch also separated under the intense vertical acceleration, an example of the recently discovered "trampoline effect".Weaker upper layers bounced up further than stronger layers lower down, then slapped back down against the lower layers as they came up, producing very high impacts, Fry said. Please contact the Museum with any queries on this matter This model provides a visual demonstration of the geological forces that caused the 22 February and 13 June 2011 earthquakes.
These forces were so strong that parts of the Port Hills have risen by more than 40 cm.
In comparison, the 6.4 magnitude 13 June 2011 earthquake had a maximum slip of 1.5 m at 4-5 km underground.
No surface fault trace has been found for the Port Hills fault.
As a direct result of the fault slip, the Bexley, Aranui, Wainoni, Avondale and New Brighton areas have gone down, mostly by less than 15 centimetres. The south side of the fault moved generally up and west, while the north side moved down and east. See what jobs are currently available and how to hire the Museum as a venue for your event. Stub This article has been rated as Stub-Class on the project's quality scale. The information on this page was created from historic documentation and may not reflect the best available knowledge about the item. The Hollywood fault extends ENE for a distance of 14 km through Beverly Hills, West Hollywood, and Hollywood to the Los Angeles River and Interstate 5. Please email
To order a copy of this image please contact Canterbury Museum Find out more about the people and the organisation behind Canterbury Museum. During the 6.3 magnitude 22 February 2011 earthquake, slip of more than 2.5 m occurred 4 km underground. Researchers are using techniques never used before in New Zealand to study the history of ancient earthquakes around the Port Hills.
It runs from an area close to Riccarton, under the Central City, through the eastern suburbs off the coast of New Brighton.It runs parallel to the more destructive Port Hills Fault that lies 5 km to the south of the Christchurch Fault. During the 6.3 magnitude 22 February 2011 earthquake, slip of more than 2.5 m occurred 4 km underground. Christchurch earthquake. "Think of jumping on a trampoline. If you have information or questions about the objects on this website, please contact us.
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port hills fault