Dr Simon Cox, of GNS Science, Dunedin, at the Department of
Conservation's Haast Visitor Information Centre on
Wednesday night. Photo by Marjorie Cook.
When the long overdue major Southern Alps faultline
rupture occurs, Haast residents may experience an 8m shift of
the ground beneath their feet.
If they survive, they will need to be prepared to
wait for a long time for help to come.
Geologist Dr Simon Cox, of GNS Sciences, Dunedin, presented a
frightening scenario to more than 50 people at a seminar in
Haast on Wednesday night, held as part of the Department of
Conservation's summer programme.
His seminar updated residents and visitors on earthquake
research developments before going on to describe the rich
and varied geology of the area caused by the alpine fault.
Haast is home to 297 permanent residents, according to Census
2006 data, and can have up to 700 visitors a day.
The population lives right on top of the faultline in a 50km
stretch of small coastal villages between the Haast River and
Jackson Bay.
The faultline starts hundreds of kilometres up the coast and
continues down to the Jackson River, through the Cascade
Valley to Milford Sound.
An earthquake of magnitude 7 or 8 could devastate large parts
of the South Island, Dr Cox said.
Haast residents could expect to lose at least their power
supply and hydro scheme.
They might also have to head for the hills to avoid coastal
tsunamis.
Large rock landslips would block the alpine highways
providing access out of Haast.
Rivers would also be dammed, creating the potential for
dam-burst floods of sediment down the river valleys -
presenting another threat to residents as they fled the
coast.
Intense shaking of the ground could also cause "sand
volcanoes" - where sand liquefies - that would "burst out
everywhere", Dr Cox said.
Scientists from New Zealand and overseas have studied the
alpine fault and collected data showing major ruptures
occurred at Haast about 1430, 1620 and 1717.
In 1717, the Haast River channel was offset by at least 8m.
They have also discovered the rate of movement between the
Australian and Pacific plates - which creates the fault line
- is 35mm a year.
Scientists thought the alpine fault was sliding along quietly
but after analysing tests on soil age, they realised a grand
shake was more likely.
Scientists have been warning of the destructive impact a
large rupture would have on the South Island population and
environment.
"The current thinking [is] that the 8m shift will happen in
one motion.
That could be a reasonably small earthquake, believe it or
not, to get 8m.
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