Alpine Fault

E612005

The Alpine Fault is a major geological fault in New Zealand that marks the boundary between the Pacific and Australian tectonic plates and is responsible for much of the uplift of the Southern Alps.

All labels observed (1)

Label Occurrences
Alpine Fault canonical 4

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf geological fault ⓘ
plate boundary ⓘ
transform fault ⓘ
age Cenozoic ⓘ
associatedProcess oblique convergence of Pacific and Australian plates ⓘ
associatedRange Southern Alps ⓘ
connectsTo Marlborough Fault System ⓘ
Puysegur Trench region ⓘ
continent Zealandia ⓘ
country New Zealand ⓘ
displacementSinceFormation hundreds of kilometres of lateral offset ⓘ
earthquakeRecurrenceInterval about 200–400 years ⓘ
exposes high-grade metamorphic rocks ⓘ
mylonites ⓘ
formedDuring Miocene ⓘ
hazardLevel major seismic hazard for South Island ⓘ
lastMajorRupture around 1717 CE ⓘ
length about 600 km ⓘ
locatedIn South Island ⓘ
maximumHistoricalMagnitude about magnitude 8 ⓘ
monitoredBy GPS networks ⓘ
seismographs ⓘ
movementType dextral strike-slip ⓘ
reverse faulting component ⓘ
nearbyCity Greymouth ⓘ
Queenstown ⓘ
Wanaka ⓘ
orientation southwest–northeast ⓘ
orogeny Southern Alps orogeny ⓘ
overlainBy Quaternary sediments in many places ⓘ
partOf plate boundary between Pacific and Australian plates around New Zealand ⓘ
passesNear Fox Glacier ⓘ
Franz Josef Glacier ⓘ
Hokitika ⓘ
Milford Sound ⓘ
region West Coast of the South Island ⓘ
responsibleFor uplift of the Southern Alps ⓘ
runsAlong western edge of the Southern Alps ⓘ
separates Australian Plate ⓘ
Pacific Plate ⓘ
slipRate about 20–30 mm per year ⓘ
studiedBy GNS Science ⓘ
University of Otago ⓘ
Victoria University of Wellington ⓘ
tectonicSetting convergent plate boundary ⓘ
terminusNear Fiordland ⓘ
Marlborough Fault System ⓘ
verticalUpliftRate about 5–10 mm per year ⓘ

How these facts were elicited

Referenced by (4)

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