University of Otago geologist Prof David Prior, pictured
beside an electron microscope, displays greatly magnified
images of the structure of ice (at left) and quartz. Photo
by Peter McIntosh.
By studying the microstructure of ice, University of
Otago scientists hope to gain new insights into the origin of
earthquakes, deep below the Southern Alps.
Otago scientists are focusing on the similarity of ice to
rock, both being crystalline solids, and both being deformed
- changing shape in response to force - in similar ways.
The research is headed by Prof David Prior, who has become a
world leader in a technique linked to the use of electron
microscopes and used to study the microstructure of ice.
Prof Prior has spent about 18 months applying the laboratory
technique, known as ''electron back-scatter diffraction
(EBSD)'', to ice, at the university's Otago Centre for
''We have made the technique routine and reliable and are the
only lab worldwide that can do this,'' he said.
The technique provided ''maps of the microstructure of the
ice'', which helped boost understanding of how the ice
developed, and of its physical properties.
''This is the first research of this kind in the world as
nobody else has our capabilities of microstructural imaging
of ice through EBSD.''
The Otago research had been going ''spectacularly well'' and
several international groups, including from MIT in the
United States, had recently used the Otago facilities.
Rocks found at New Zealand's alpine fault zone were
''probably the best in the world to tell us about what
happens around and beneath big earthquakes'', he said.
And such processes might, in fact, control earthquake
''nucleation'' - the initial rock rupture involved.
The post-quake record of what had happened had remained in
the rock microstructure, but scientists ''lacked the tools''
to read this. The Otago experiments could help ''decode the
macrostructural record in rocks'', he said.
Matthew Vaughan and Meike Seidemann are doctoral students
undertaking ice research under Prof Prior's supervision.
Mr Vaughan, who was born in Canada, said ice had many
It could be readily produced to order, including with fine
crystalline microstructure, and did not require the equipment
needed to generate the much higher pressures needed for
deforming rocks, he said.