The seismometer at Great Barrier Island shows yesterday's
recordings of two quakes in Auckland. Photo / Geonet
Aucklanders have been reassured that a big earthquake is
highly unlikely, although a geologist says the rare pair that
struck yesterday might be a sign of more to come.
The two quakes measuring 3.1 and 3.9 centred near and under
Motutapu Island in the Hauraki Gulf, that struck the region
just after 4pm, were felt from south Auckland to Northland.
More than 10,000 people reported to the GeoNet site that they
felt the 3.9 tremor and emergency services received about 50
calls after the quake, but none for damage or injuries.
GeoNet seismologist Caroline Holden said earthquakes strong
enough to be felt were rare in Auckland - on average fewer
than 10 earthquakes were detected in the region each year.
"There are a lot of faultlines in Auckland because of all the
volcano fields in the region, but the faultlines are really,
really small and can only generally generate quite small
Ms Holden said last night there had not yet been any
aftershocks, and if there were they were unlikely to be large
enough to be felt.
She reassured Aucklanders that earthquakes on the scale that
had rocked Christchurch were highly unlikely in the region.
Small tremors were also not capable of causing volcanic
activity, only earthquakes that reached 8 or more on the
Richter scale could do that.
"[Yesterday's quakes] really were very small earthquakes in
the grand scheme of earthquakes ... very shallow and very
close to populated centres. You have to remember Christchurch
has been through about 10,000 of those earthquakes."
Ms Holden said scientists didn't yet know whether the
eruption was caused by volcanic activity or tectonic plates
"Maybe this is the beginning of something long-term, but at
the moment nothing indicates that this is leading to any
Auckland has two active faults: the Drury Fault and the
Wairoa North Fault. Both of these faults are located in the
southern part of the region and are thought to be capable of
producing earthquakes of magnitudes greater than 6.
Movement on these faults occurs about every 13,000 to 43,000
Meanwhile, the Government has a secret list of 200 of the
country's most earthquake-prone buildings - and it's growing.
But it refuses to reveal details of the structures, which
carry a risk of collapsing like the CTV building, if there
was a similar-sized quake to the fatal shakes in Christchurch
in 2011. The buildings have what are known as non-ductile
columns, which do not have much flexibility.
The CTV building collapse, which killed 115 people, prompted
a Government review of other buildings around the country.
The Herald asked the Ministry of Business, Innovation and
Employment for a list of the buildings.
Adrian Regnault, general manager of the building system
performance branch, confirmed there were 200 buildings on the
list but refused to say where they were.
Auckland Council is assessing the city's most
A spokesperson said buildings to be assessed had been
identified, and more than 4000 buildings could be on its
list, but it had not finished the work.
- Amelia Wade and Anne Gibson of the New Zealand