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Why Taranaki big Mt just got more dangerous



A large Mt Taranaki option could launch devastating pyroclastic flows across a wider area than first thought – putting more people at risk.

A pyroclastic flow is a super-heated hurricane of gas, and rock particles that are fired from an erupting volcano and scorches everything in its path

At Mt Taranaki and other volcanoes like it around the world, scientists have long assumed that these flows could only spread about 1

0km to 15km.

But a new study, led by University of Auckland researchers, has pushed this limit out to 25km, with serious implications for populated areas within the danger zones.

The new estimates put many Taranaki towns at risk, although the main areas of New Plymouth were protected by the edifice of The older Pouakai volcano.

Mt Taranaki was probably the most likely New Zealand to cause national-scale impacts on our lifetimes, with a 50 per cent probability of an eruption in the next 50 years. 02] According to existing estimates, more than 85,000 people live within 30km of the mountain and 40,000 in high-priority evacuation areas.

The fresh findings have been presented to the joint Taranaki Volcano Scientific Advisory Group and work was now underway to revisit local hazard plans

MAGNETIC CLUES

The new study's leader, PhD student Geoff Lerner, was able to get fresh light on this explosive history by applying methods of paleomagnetism – or the record of magnetic signals stored in volcanic rocks.

"Due to the difficulties of understanding, the deposits far from volcanoes, scientists in the past that Taranaki had never been able to conclusively identify hot pyroclastic flow deposits," Lerner said.

"We tried a paleomagnetic method that had attempted at Mt Taranaki before, targeting some deposits with other characteristics consistent with hot flows."

When rocks cooled after being erupted from a volcano, they recorded a signal from the Earth's magnetic field at that time, leaving scientists some important about the direction the rocks had traveled in.

"If they tumble about after cooling, for example in a volcanic flood or lahar, the directions become jumbled, "Lerner explained.

" If they travel while still very hot and are deposited together, such as within a pyroclastic flow, then they are cool and all of the particles are magnetically lined-up. ] "We can later test whether particles are lined up or not, which can tell us if the deposit was from a pyroclastic flow or not."

 This map shows the distribution of samples from a volcanic formation (Warea) the study drew one. The rings depict the run-out distance of expected possible pyroclastic density currents based on previous studies (white) and minimum possible distances based on the new study (ed). Source / Supplement / Basemap imagery from Planet Team
This map shows the distribution of samples from a volcanic formation (Warea) the study drew on. The rings depict the run-out distance of expected possible pyroclastic density currents based on previous studies (white) and minimum possible distances based on the new study (ed). Source / Supplement / Basemap imagery from Planet Team

Using sophisticated lab equipment to heat and measure rock samples many times, Lerner and his colleagues were able to reconstruct the temperature at which the rocks were deposited.

"We found that the magnetic directions at several different sites between 15 km to 20 km from the volcano did line up, which means that these were from pyroclastic flows. "

The team also collected new samples from the deposits for radiocarbon dating, which put them at around 11,500 years old – and linked them to one of Taranaki's biggest eruptions in 30,000 years.

"We estimate that these are only possible in the largest 15 per cent of Taranaki eruptions, the varieties of events that occur on average every 1000 years. "

'WIDESPREAD DISRUPTION'

Lerner's supervisor, Auckland University volcanologist Professor Shane Cronin, said a big large eruption would disrupt a ir and surface transport, tourism, power and water supplies across the north island.

Although could be expected in the relatively near future, the dormancy since Taranaki's last big blow, at around 1790, had been one of its longest.

The same research team recently revealed how Mt Taranaki was in its second-longest break between eruptions in more than 1200 years of records.

"Thus, we have a modern experience of typically very long eruptions," Cronin said.

"Past research shows that once Mt Taranaki starts erupting, it continues for years, decades, or centuries."

The volcano began erupting about 130,000 years ago, with large eruptions occurring on average every 500 years and narrower eruptions about 90 years apart.

A recent estimate of the net losses in economic activity from a letter Taranaki was estimated at between $ 1.7 billion and $ 4 billion – or between $ 13 billion and $ 26 billion over a dec. ade of volcanism.

Cronin, who is director of a national science collaboration aimed at making New Zealand more resilient to natural hazards, said a wider research program at Taranaki was offering scientific insights that were also important for engineering and socio-economic issues

"Using a novel integration of volcanic scientific knowledge, experimentation and advanced mathematical and economic simulation, we aim to radically cut down uncertainty that hinders decisive hazard and mitigation planning."

Cronin said the new study, about to published in the [GeologicalSocietyofAmericaBulletin]potential implications for other volcanoes in New Zealand and overseas

Approximately 29 million people worldwide live within a 10 km radius of an active volcano, while 229 million live within a 30km radius.


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