Scientists claim to have developed system to predict cataclysmic SUPERVOLCANO eruptions that could end life on Earth

It is a discovery that could save the life of million, and safeguard entire species.

Researchers claim to have worked out how to accurately predict the eruption of 'supervolcanoes' that blanket the earth in giant ash clouds triggering a 'nuclear winter'.

They say the discovery could reveal exactly when giant pools of magma greater than 100 cubic miles in volume and formed a few miles below the surface will erupt. 

WHAT MAKES A MEGAERUPTION? 

The most recent supervolcanic eruption on Earth occurred 27,000 years ago at Taupo located at the center of New Zealand's north island. 

They occur when giant pools of magma greater than 100 cubic miles in volume form a few miles below the surface and erupt.

They throw 100 times more superheated gas, ash and rock into the atmosphere than run-of-the-mill eruptions - enough to blanket continents and plunge the globe into decades-long volcanic winters. 

Repeatedly throughout Earth's history,when they become a super-eruption, the resulting gigantic volcanic outbursts that throw 100 times more superheated gas, ash and rock into the atmosphere than run-of-the-mill eruptions - enough to blanket continents and plunge the globe into decades-long volcanic winters.

The most recent super-eruption took place about 27,000 years ago in New Zealand, well before humans kept records of volcanic eruptions and their aftermath. 

Geologists today are studying deposits from past super-eruptions to try and understand where and how rapidly these magma bodies develop and what causes them to eventually erupt. 

Despite considerable study, geologists are still debating how quickly these magma pools can be activated and erupted, with estimates ranging from millions to hundreds of years.

Now a team of geologists have developed a new 'geospeedometer' that they argue can help resolve this controversy by providing direct measurements of how long the most explosive types of magma existed as melt-rich bodies of crystal-poor magma before they erupted. 

They have applied their new technique to two super-eruption sites and a pair of very large eruptions and found that it took them no more than 500 years to move from formation to eruption.

These results are described in the article 'Melt inclusion shapes: Timekeepers of short-lived giant magma bodies' appearing in the November issue of the journal Geology.

Geologists have developed a number of different 'timekeepers' for volcanic deposits. 

Quartz crystal that developed in molten magma. Black dots are blebs of molten rock captured in the crystal when it formed. Using advanced 3-D X-ray tomography, the researchers were able to measure the size and shape of the melt inclusions with unprecedented precision.

The fact that these techniques measure different processes and have different resolutions, has contributed to this lack of consensus.

'Geologists have developed a number of different 'timekeepers' for volcanic deposits,' said Guilherme Gualda, associate professor of earth and environmental sciences at Vanderbilt University, who directed the project.

'The fact that these techniques measure different processes and have different resolutions, has contributed to this lack of consensus. 

'Our new method indicates that the process can take place within historically relevant spans of time,'

The method was developed as part of the doctoral thesis of Ayla Pamukcu, who is now a post-doctoral researcher at Brown and Princeton Universities.

'The hot spot under Yellowstone National Park has produced several super-eruptions in the past.

'The measurements that have been made indicate that this magma body doesn't currently have a high-enough percentage of melt to produce a super-eruption. 

But now we know that, when or if it does reach such a state, we will only have a few hundred years to prepare ourselves for the consequences,' Gualda said.

The researchers' geospeedometer is based on millimeter-sized quartz crystals that grew within the magma bodies that produced these giant eruptions. 

Quartz crystals are typically found in magmas that have a high percentage of silica. 

This type of magma is very viscous and commonly produces extremely violent eruptions. Mount St. Helens was a recent example.

The geologists use image process method that describe the edges of a melt inclusion by set of points. Next they use these points to create a 3-D polyhedron (red) that represents the final shape of the melt inclusion.

When the crystals form, they often capture small blobs of molten magma – known as blebs or melt inclusions. Blebs are initially round. 

While the crystal is floating in hot magma, diffusion causes them to gradually acquire the polygonal shape of the crystal void that they occupy. But this faceting process can be halted if eruption occurs before complete faceting is achieved.

Using advanced 3-D X-ray tomography, the researchers were able to measure the size and shape of the melt inclusions with exquisite precision. 

In cases where the inclusions had not become completely faceted, the researchers could determine how much time had elapsed since they were enclosed.

SCIENTISTS FIND MASSIVE NEW MAGMA CHAMBER UNDER YELLOWSTONE 

In the heart of Yellowstone National Park, a supervolcano releases around 45,000 metric tonnes of carbon dioxide each day. 

But the magma chamber lying directly beneath its surface is not considered large enough to produce such levels, so researchers have been searching for an alternative source for years.

In April, by tracking seismic waves, geophysicists discovered a huge secondary chamber deeper underground that's so large its partly-molten rock could fill the Grand Canyon 11 times over.

Previous research found a relatively small magma chamber, known as the upper-crustal magma reservoir, directly beneath the surface in 2013 that measures 2,500 cubic miles (10,420 cubic km). 

To discover the latest chamber, Hsin-Hua Huang from the University of Utah and his colleagues tracked seismic waves from almost 5,000 earthquakes.

These readings combined data from the University of Utah Seismograph Stations, which collected shallow readings from nearby quakes in Utah, Idaho, the Teton Range and Yellowstone, and from the Earthscope array, which revealed deeper readings from temblors from more further afield.

Each of these quakes created waves that echoed around the supervolcano. 

The movement and structure of these waves could then be used to map the earth beneath. 

The researchers said in their paper: 'The Yellowstone magmatic system from the mantle plume to the upper crust', published in the journal Science, that the reservoir contains around 98 per cent hot rock. 

The remaining 2 per cent is molten rock and is too deep to directly cause an eruption, they added.

'Previous studies provided us with the data we needed to calculate the rate of the faceting process. We then used this rate, in combination with our shape measurements, to calculate how long the crystal existed in the magma before the eruption,' said Pamukcu.

In addition, the researchers compared the results obtained with faceting with results obtained using other techniques. 

Crystallization may cause variations in concentration of certain elements. In quartz, the element titanium can vary sharply between different zones or layers within the crystal. 

Over time, however, the process of diffusion gradually smooths out these variations. 

This process also stops at the eruption, so the shallower the slope of titanium concentrations across these boundaries today, the longer the crystal spent in magmatic conditions.