Media Release
20 March 2009
Scientists To Probe Alpine Fault
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Scientists from around the world will descend on the West Coast of the South Island next week to discuss an ambitious
plan to drill into the Alpine Fault and learn more about earthquakes.
The project, the first of its kind in New Zealand, aims to drill several kilometres into the Earth’s crust and examine
physical and chemical conditions inside the fault. This will provide an important insight into how big faults such as
the Alpine Fault evolve and generate earthquakes.
The Alpine Fault extends for more than 650km from south of Fiordland through Milford Sound and along the spine of the
South Island into Marlborough. It forms part of the boundary between the Pacific and Australian tectonic plates, which
are moving past each other and colliding, forcing up the Southern Alps.
It is one of the world’s major active faults and is visible from space. Geological evidence suggests it ruptures every
200 to 400 years producing earthquakes of about magnitude 8. Scientists believe it last ruptured in 1717.
The Alpine Fault moves at a rate of about 25m every 1000 years - fast by global standards. In between its major
ruptures, it is locked and produces few sizeable earthquakes.
From Sunday, 60 scientists from seven countries will gather at Franz Josef for a five-day workshop that will start with
a review of the latest geological and geophysical knowledge about the Alpine Fault. They will then develop a drilling
plan that meets an agreed set of objectives.
Project Leader, John Townend of Victoria University in Wellington, said the project would involve expertise and funding
from many countries and organisations.
A key feature of the Alpine Fault was that it exhumed rocks from within the earthquake generating zone very rapidly in
geological terms. This brought rocks associated with earthquake processes within reach of deep drill holes, Dr Townend
said.
This provided a globally unique opportunity to study earthquake and other land deformation processes through a
combination of surface studies and scientific drilling.
At major plate boundary faults in most other parts of the world, the earthquake generating zone was deep and therefore
largely beyond the reach of present drilling technology.
“A key motivation for this project is to provide new understanding of how large faults evolve and generate earthquakes
in what is an amazing natural laboratory.
“Potentially, it also offers the chance to develop deep-fault monitoring techniques that could operate for many years,”
Dr Townend said.
As well as penetrating the earthquake zone and extracting rocks for analysis, scientists hope to install a variety of
underground instruments that may shed light on the timing and severity of earthquakes and other forms of tectonic
deformation on the Alpine Fault.
Lowering instruments into the heart of the fault would enable scientists to investigate a range of processes not
normally accessible to them. Measurements would include pressure, temperature, rock fracturing, and the chemistry of
fluids, rocks and gases.
Dr Townend said a large earthquake on the Alpine Fault could strike this century, and there was a compelling case to
install instruments at depth to better understand and monitor the South Island’s most dangerous fault.
Monitoring equipment had been successfully installed deep inside major faults in several countries including Japan,
Taiwan, and the United States. Scientists who led the San Andreas Fault Observatory at Depth (SAFOD) deep drilling
project will attend the workshop to share their knowledge.
The workshop has been made possible through funding awarded by the International Continental Scientific Drilling
Programme.
END