Port Hills Fault

E784232

The Port Hills Fault is an active geological fault beneath the Port Hills near Christchurch, New Zealand, believed to have generated the devastating 2011 Christchurch earthquake.

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Statements (35)

Predicate Object
instanceOf active fault
geological fault
seismogenic structure
associatedWith 2011 Christchurch earthquake
believedToHaveGenerated 2011 Christchurch earthquake
country New Zealand
coveredBy Quaternary sediments
dipDirection northward
discoveredBy seismological investigations after 2010–2011 Canterbury earthquakes
displacementStyle compressional
faultType oblique-slip fault
reverse fault
identifiedUsing aftershock distribution
geodetic data
strong-motion records
locatedIn Port Hills NERFINISHED
locatedInRegion Canterbury NERFINISHED
South Island NERFINISHED
locatedNear Christchurch NERFINISHED
maximumMagnitudeEstimate approximately 7.0 Mw
nearbyCity Christchurch NERFINISHED
nearbyPort Port of Lyttelton NERFINISHED
orientation approximately east–west striking
overlies Canterbury Plains basement rocks
partOf Canterbury active fault system NERFINISHED
relatedTo Canterbury earthquake sequence
Greendale Fault NERFINISHED
riskCategory significant local seismic source
seismicHazardTo Christchurch urban area
Lyttelton NERFINISHED
studiedBy GNS Science NERFINISHED
University of Canterbury NERFINISHED
tectonicSetting Pacific–Australian plate boundary zone NERFINISHED
timeZone UTC+12
timeZoneDST UTC+13

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.