Lahar Researchers Capture Flood Of Information
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Dr Shane Cronin of Massey University and post-graduate student Suzy Cole examining lahar deposits at the OnTrack
warning tower, Whangaehu River, on Wednesday. (Photo: Vern Manville, GNS Science)
Researchers from GNS Science and Massey University have spent the last three days gathering a flood of data about
Sunday’s spectacular lahar as part of a $1 million research programme to gather maximum scientific value from the event.
The digital information was captured by instruments that were installed along the Whangaehu Valley in advance of the
predicted break-out from Ruapehu’s summit Crater Lake.
It will take months to sift through and interpret all of the data, but initial results suggest that the lahar was 25
percent bigger than the 1953 Tangiwai flow. There is a 25 percent margin of error in this estimate.
“All of our years of effort have paid off. We have collected a world-class dataset that will make this the best-studied
lahar ever,” said project leader Dr Vern Manville of GNS Science.
A terrestrial laser scan survey of the breach is planned for later this week.
Shane Cronin, leader of Massey University’s lahar science programme, mobilised 16 staff and student volunteers on Sunday
to track the lahar downstream and collect eye-witness records of its behaviour as it poured down the Whangaehu Valley.
“Although the lahar is over, the real work is just beginning for us,” Dr Cronin said.
Teams from Massey University have been on the mountain all week surveying the deposits and taking samples for analysis.
Information is being shared between all of the agencies that had measuring equipment and observers along the river,
including the Department of Conservation, Horizons Regional Council, OnTrack, and Genesis. Video and still images
captured by media organisations and members of the public will also be a valuable contribution.
The lahar has also attracted considerable interest from overseas researchers, with groups from Hawai’i, Japan, France,
and Britain taking part in the scientific response. The research programme is funded by a Marsden grant from the Royal
Society of New Zealand, the Foundation for Research Science and Technology, and the Earthquake Commission.
ENDS