New Zealand’s White Island volcano eruption ‘could trigger deadly landslides and TSUNAMIS’


The devastating volcanic eruption on New Zealand’s White Island, which has already claimed at least five lives, could trigger subsequent landslides, eruptions and tsunamis, scientists have warned.

Chris Elders, professor of Geology at Curtin University’s School of Earth and Planetary Sciences, told MailOnline that the ash belching out from Volcano Whakaari could trigger a downpour of rain.

Ash particles thrown up into the atmosphere are good at attracting and collecting water droplets in clouds, resulting in heavy rain after an eruption. 

This in turn could cause unstable rock, which formed immediately after the eruption, to be washed down the sides of the volcano in a landslide, with potentially fatal consequences for both rescue workers and the tourists who are still on the island.  

‘It’s still not safe for rescue workers to land on the island,’ Professor Elders said.

‘When you get an eruption like this, the ash deposits very quickly and creates rocks which are extremely unstable. 

‘Any rainfall, which can be triggered by the ash sent into the atmosphere, could cause a landslide if the unstable rocks come loose.’ 

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Ash particles have a high affinity for attracting and keeping hold of water than normal clouds. This results in the clouds becoming ‘full’ and ‘heavy’ quicker than normal, speeding up the natural water cycle. This can lead to landslides and volcanoes, experts warn 

The devastating volcanic eruption on New Zealand's White Island (pictured) has already claimed at least five lives. Scientists also say there is a 'high chance' for the island to try and 're-equilibrate' via a series of smaller volcanic eruptions

The devastating volcanic eruption on New Zealand’s White Island (pictured) has already claimed at least five lives. Scientists also say there is a ‘high chance’ for the island to try and ‘re-equilibrate’ via a series of smaller volcanic eruptions

WHY DOES VOLCANIC ASH CAUSE RAIN AFTER AN ERUPTION?  

The main effect on weather right near a volcano is that there is often a lot of rain, lightning, and thunder during an eruption. 

This is because all the ash particles that are thrown up into the atmosphere are good at attracting/collecting water droplets.   

The smallest particles say in the atmosphere, whereas the larger ones fall out of the sky and come down to Earth quickly.  

Ash particles have a high affinity for attracting and keeping hold of water than normal clouds. 

This results in the clouds becoming ‘full’ and ‘heavy’ quicker than normal, speeding up the natural water cycle. 

If it happens rapidly, precipitation can fall within hours or days of an eruption, and depending on wind and other weather conditions., can happen over an area close to the site of the eruption.   

If this rock reaches the ocean and plunges into the water, it could trigger a tsunami, resulting in further catastrophe.

Large volcanic events such as the White Island eruption can often cause subsequent disasters. 

The eruption of Krakatoa in 1883 caused enormous tsunamis, as did an eruption of Mount Teide on Tenerife in the Canary Islands. 

‘If rock from the mountain slides down into the sea, when that happens it displaces the proportionate amount of water and causes a wave,’ Professor Elders said.  

The violent volcanic eruption on New Zealand’s White Island was caused by ocean crust being ‘subducted’ – or pushed under – another part of the Earth’s crust. 

‘The Pacific Plate is moving westwards, underneath the tectonic plate New Zealand sits on,’ Professor Elders explained. 

This constant movement means sudden explosions can occur at any moment. 

As the Pacific Plate is pushed down further into Earth’s mantle, the rock melts and forms magma.  

The violent volcanic eruption on New Zealand's white Island was caused because ocean crust is being subducted (pictured, the series of events leading to the spontaneous eruption).  This constant movement means sudden explosions can occur at any moment

The violent volcanic eruption on New Zealand’s white Island was caused because ocean crust is being subducted (pictured, the series of events leading to the spontaneous eruption).  This constant movement means sudden explosions can occur at any moment 

Professor Shane Cronin, a volcanologist at the University of Auckland, said: ‘Magma is close to the surface, and the heat and gases from this heat the surface and ground waters to form vigorous hydrothermal systems. 

‘We know hydrothermal and so-called ‘phreatic’ eruptions can occur suddenly and with little or no warning because they are driven by the expansion of super-heated water into steam.’

As pressure builds up in the volcano, eventually the rocks withstanding the forces burst, and the gases are released violently, causing an eruption. 

‘The eruptions are short-lived, but once one occurs, there are high chances for further, generally smaller ones as the system re-equilibrates,’ Professor Cronin said.  

WHAT WAS THE 1914 DISASTER OF WHITE ISLAND?

In the late 1800’s a sulphur mine was established on the island.

The workers lived in a small settlement.

The settlement was decimated in 1914 when an avalanche of rock destroyed the mining buildings. 

Hydrothermally weakened rock collapsed from the crater walls, causing the catastrophe. 

There was significant loss of life and the practice of mining sulphurous rocks on the island was stopped.  

The eruption, which took place at 14:11 local time (01:11 GMT) on Monday, was a ‘short-lived explosive event’ which saw ash catapulted more than 10,000ft (4,000m) into the air. 

Dozens of tourists visiting the volcanically active island 30 miles (48km) off the coast of mainland New Zealand are unaccounted for or injured, according to rescue workers.

Authorities have already confirmed that approximately 100 people were on the island at the time of the eruption. 

Emeritus Professor Ray Cas, from Monash University, said that it has been ‘a disaster waiting to happen for many years’. 

‘I have always felt that it was too dangerous to allow the daily tour groups that visit the uninhabited island volcano by boat and helicopter,’ he said.

In 1914, a small mining community on the island was wiped out after falling rocks weakened by the island’s volcanic activity swept through the village. 

It has been uninhabited now for more than a century, but is a hotspot for tourists hoping to get close to an active volcano.  

Volcano Whakaari, or White Island, (pictured here in a video from New Zealand's Institute of Geological and Nuclear Sciences (GNS))was raised from a level one to a level two for its recent geological activity

Volcano Whakaari, or White Island, (pictured here in a video from New Zealand’s Institute of Geological and Nuclear Sciences (GNS))was raised from a level one to a level two for its recent geological activity 

Emergency services attend to an injured person arriving at the Whakatane Airfield after the volcanic eruption. Adverse weather conditions influenced by the eruption itself could seriously hinder rescue efforts. scientists warn

Emergency services attend to an injured person arriving at the Whakatane Airfield after the volcanic eruption. Adverse weather conditions influenced by the eruption itself could seriously hinder rescue efforts. scientists warn 

New Zealand is home to a preponderance of volcanoes, spanning from the North Island to the South Island and beyond. 

The archipelago nation sits on the boundary between two major tectonic plates — called the Kermadec-Tonga arc — which leaves it vulnerable to natural disasters such as earthquakes, volcanoes and tsunamis. 

They are regularly monitored, but scientific apparatus is still wildly inconsistent at accurately predicting future geological activity. 

White Island, also known as Volcano Whakaari, is one of many in the ‘Ring of Fire’ and forms part of a chain from Ruapehu in the North Island, through numerous submarine volcanoes all the way to the Solomon Islands and the Tonga Chain.

Known as a stratovolcano – similar to Mt St Helens and many other classic cone-shaped volcanoes – it is built up of alternate layers of lava and ash. 

White Island, 48km from the Bay of Plenty region, began erupting about 2.11pm local time

White Island, 48km from the Bay of Plenty region, began erupting about 2.11pm local time

Pictured, a rescue helicopter is pictured arriving at the Whakatane Airport. At least five people have died, several are injured and many more are missing

Pictured, a rescue helicopter is pictured arriving at the Whakatane Airport. At least five people have died, several are injured and many more are missing

Pictures taken by tourists moments after the eruption on White Island pictured) capture the enormous ash cloud sent thousands of feet into the air. Image taken by Micahel Schade from a boat,whohad left the island with his family just 20 minutes before the eruption

Pictures taken by tourists moments after the eruption on White Island pictured) capture the enormous ash cloud sent thousands of feet into the air. Image taken by Micahel Schade from a boat,whohad left the island with his family just 20 minutes before the eruption

Warnings ignored: How persistent tourists travelled to the active volcano against expert advice 

By Charlie Moore for Daily Mail Australia

Tourists have been travelling to White Island for years despite warnings from scientists that it could erupt at any time.

Between 2011 and 2016 the volcano to the north of New Zealand’s north island – which erupted on Monday – had a period of increased activity but still boatloads of tourists arrived.

Volcanologists at the time refused to step foot on the island because it was too dangerous and warned tourists not to go – but still the boats kept landing.

An aerial view of the volcano, which is currently the most active in New Zealand and erupted in 2016 and 2012 before today

An aerial view of the volcano, which is currently the most active in New Zealand and erupted in 2016 and 2012 before today

In recent weeks the volcano has been going through another period of activity but tourism was not stopped.

Last month monitoring outfit GNS Science raised the alert level for the volcano to level two because of increase activity.

‘Volcanic unrest continues at Whakaari/White Island and some monitored parameters show further increases in activity,’ the agency said.

‘Hazards on the island are now greater than during the past few weeks.

‘The patterns of signals are similar to those through the 2011 – 2016 period and suggest that Whakaari/White Island may be entering a period where eruptive activity is more likely than normal.’

Professor Ross Dowling, an Honorary Professor of Tourism in the School of Business and Law at Edith Cowan University, said: ‘The number of tourists visiting active volcanoes is increasing globally as part of an increase in both geological tourism and adventure tourism. 

‘Part of the attraction is to visit an unpredictable natural environment and for most tourists they assume that they will be able to visit such dangerous sites in relative safety. 

‘However, despite the increased science behind predicting volcanic eruptions, the science is not infallible and ‘active’ volcanos may erupt at any time. 

‘Therefore volcanic hazard management guidelines need to be easily understood by the public so that visitors can weigh up their their risks in relation to visiting such sites. 

‘One such strategy is to simply allow visitors to view active volcanoes from a distance and not allow them on to any volcano deemed still in its active phase. 

‘In this way risks to the public will be reduced whilst still allowing adventurous visitors a chance to see and experience those elements of the landscape which are active and dramatic.’

HOW CAN RESEARCHERS PREDICT VOLCANIC ERUPTIONS?

According to Eric Dunham, an associate professor of Stanford University’s School of Earth, energy and Environmental Sciences, ‘Volcanoes are complicated and there is currently no universally applicable means of predicting eruption. In all likelihood, there never will be.’

However, there are indicators of increased volcanic activity, which researchers can use to help predict volcanic eruptions. 

Researchers can track indicators such as: 

  • Volcanic infrasound: When the lava lake rises up in the crater of an open vent volcano, a sign of a potential eruption, the pitch or frequency of the sounds generated by the magma tends to increase.
  • Seismic activity: Ahead of an eruption, seismic activity in the form of small earthquakes and tremors almost always increases as magma moves through the volcano’s ‘plumbing system’.
  • Gas emissions: As magma nears the surface and pressure decreases, gases escape. Sulfur dioxide is one of the main components of volcanic gases, and increasing amounts of it are a sign of increasing amounts of magma near the surface of a volcano. 
  • Ground deformation: Changes to a volcano’s ground surface (volcano deformation) appear as swelling, sinking, or cracking, which can be caused by magma, gas, or other fluids (usually water) moving underground or by movements in the Earth’s crust due to motion along fault lines. Swelling of a volcano cans signal that magma has accumulated near the surface.  

Source: United States Geological Survey



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