logo
Fears over 'Ring of Fire' eruptions as Russian volcano roars into life for the first time in 500 years following huge 8.8-magnitude earthquake

Fears over 'Ring of Fire' eruptions as Russian volcano roars into life for the first time in 500 years following huge 8.8-magnitude earthquake

Daily Mail​a day ago
Scientists have warned that a string of volcanic eruptions along the volatile 'Ring of Fire' could have been caused by an enormous earthquake.
The Krasheninnikov Volcano in Kamchatka, Russia, roared into life in a 'historic' eruption on Sunday.
As it erupted for the first time in over 500 years, the volcano sent a plume of ash 3.7 miles (6 km) into the sky.
According to experts, this destructive blast was likely triggered by the huge 8.8-magnitude earthquake which struck last week.
Last Wednesday, Russia was hit by the sixth-largest earthquake ever recorded, sending people fleeing from tsunami warnings as far away as Chile and Hawaii.
Shortly after the tremor, another volcano in the Kamchatka region also erupted, sending streams of lava pouring down its slopes.
Dr Alexey Ozerov, Director of the Russian Institute of Volcanic and Seismic Sciences, said that there was a 'direct connection' between the powerful earthquake and these eruptions.
Dr Ozerov says: 'We associate the eruptions with the earthquake, which activated magmatic centres, and "pumped" additional energy into them.'
Last Wednesday, data from the US Geological Survey (USGS) showed an earthquake struck about 84 miles east-southeast of Kamchatka, Russia, at around 7:24 pm EST, marking the sixth strongest earthquake ever.
Just hours later, Klyuchevskaya Sopka, the largest volcano in the Kamchatka Peninsula, exploded with a stream of lava and ash.
On Sunday, the Krasheninnikov Volcano became the second volcano to suddenly erupt following the earthquake.
The Kamchatka Volcanic Eruption Response Team (KVERT) called the eruption 'historic' and reported that clouds of ash travelled 46 miles (75 km) from the blast.
The last time Krasheninnikov erupted was sometime between 1423 and 1503.
Roughly nine hours after the eruption, KVERT issued an aviation 'red alert' warning of significant levels of ash being sent into the atmosphere.
As of Monday evening local time, the eruption remained ongoing with KVERT warning that 'ash explosions up to 10 km (32,800 ft) a.s.l. could occur at any time'.
Following the eruption, the region was hit by another 7.0 magnitude earthquake, which triggered tsunami warnings all across the peninsula.
What would happen if the Ring of Fire erupted?
If the Ring of Fire erupted, the most immediate effects would be felt by areas close to volcanoes.
Eruptions up to a ranking of seven on the Volcanic Explosivity Index, as large as Krakatoa, would occur all along the chain of volcanoes.
Ash injected into the atmosphere could cause planes to crash and trigger global travel chaos.
The injection of dust and sulphur into the atmosphere would then lead to global cooling.
This could drop temperatures as much as 1°C (1.8°F), leading to widespread crop failure.
Scientists now say that all three of these events could have been caused by Sunday's earthquake.
Dr Jonathan Paul, a volcanologist from Royal Holloway University of London, told Daily Mail: 'The earthquake released a huge amount of stress in the crust, which could have made an eruption easier by opening up new lines of weakness through which magma could travel upwards.'
Dr Paul says that the delay between the initial earthquake and the eruption of Krasheninnikov is likely due to the fact that the fractures in the rock took time to develop.
In the days between the events, magma would have been forcing itself through new lines of weakness and building up enough pressure to erupt.
These events have sparked concerns that more volcanic activity may be on its way.
Russia's Kamchatka Peninsula has an exceptionally high density of active volcanoes because it is situated directly above the Ring of Fire - a 25,000-mile chain of volcanoes that stretches around the Pacific Ocean.
Made up of numerous faults between shifting tectonic plates, the Ring of Fire is home to over 425 volcanoes, making up 75 per cent of all active volcanic sites on Earth.
This includes some of the most destructive volcanoes ever to erupt, including Krakatoa, Mount Tambora, and Hunga Tonga-Hunga Ha'apai.
Could the Ring of Fire erupt?
Scientists say that an earthquake could never cause the entire Ring of Fire to erupt.
Earthquakes can only trigger eruptions in volcanoes that were going to erupt anyway.
The Ring of Fire is made up of too many plate borders with different geometries and rock types for this to ever occur.
Some scientists have suggested that a sufficiently large earthquake could trigger more volcanic activity along the Ring of Fire.
Michael Manga, a geoscientist at the University of California, Berkeley, previously told the Daily Mail: 'The volcanoes in volcanic arcs, including Chile, the US Cascades, Japan, Indonesia and Kamchatka, are prone to erupt after earthquakes.'
Were the Ring of Fire to erupt, the results could be extremely dangerous.
People in the vicinity of a volcano would be at risk from falling rocks, toxic gases, deadly mudslides, and boiling hot pyroclastic flows.
The bigger danger would come from the fact that, as volcanoes erupt, they inject huge quantities of sulphur and dust into the upper atmosphere.
This could block out the sun and cause global temperatures to plummet as much as 1°C (1.8°F) for several years.
Dr Paul says: 'Both the eruption and earthquake are bound together by plate tectonics.
'Earthquakes are always a likelihood around the Ring of Fire because of localised plate tectonic activity.
'Earthquakes are triggered because the movement of tectonic plates with respect to each other isn't a continuous process; it takes place in fits and starts, because of the build-up and release of friction and pressure.'
However, although scientists say that more eruptions and earthquakes are possible, a mass eruption event is extremely unlikely.
Dr Paul says: 'Earthquakes can only trigger volcanic eruptions when the volcano is "ready"; in other words, there is a sufficiently high build-up of pressure beneath the ground.
'An analogy might be a can of Coke that has been shaken up; the earthquake would be lifting the ring-pull that leads to an eruption.'
Since this 'ready' condition isn't very common in nature, earthquakes like those in Russia are unlikely to cause multiple eruptions.
WHAT IS EARTH'S RING OF FIRE?
The Ring of Fire is a horseshoe-shaped geological disaster zone and hotbed of tectonic and volcanic activity.
Roughly 90 per cent of the world's earthquakes occur in the belt, which is also home to more than 450 volcanoes.
The seismic region stretches along the Pacific Ocean coastlines, where the Pacific Plate grinds against other plates that form the Earth's crust.
It loops from New Zealand to Chile, passing through the coasts of Asia and the Americas on the way.
In total, the loop makes up a 25,000-mile-long (40,000km) zone prone to frequent earthquakes and eruptions.
The region is susceptible to disasters because it is home to a vast number of 'subduction zones', areas where tectonic plates overlap.
Earthquakes are triggered when these plates scrape or slide underneath one another. When that happens at sea it can spawn tsunamis.
Orange background

Try Our AI Features

Explore what Daily8 AI can do for you:

Comments

No comments yet...

Related Articles

Research into Australian skinks' resistance to snake venom could streamline design of antivenoms
Research into Australian skinks' resistance to snake venom could streamline design of antivenoms

The Guardian

time3 hours ago

  • The Guardian

Research into Australian skinks' resistance to snake venom could streamline design of antivenoms

Australian skinks have evolved the means to resist snake venom by shutting down their muscles, suggests new research which could help to inform future treatments for snakebites. Research led by the University of Queensland has found that multiple species of Australian skink have evolved venom resistance through changes to a critical muscle receptor. In other animals, the receptor is the target of venom neurotoxins, which cause rapid paralysis and death. Sign up: AU Breaking News email Study co-author Prof Bryan Fry, who leads UQ's adaptive biotoxicology lab, said that when venomous snakes arrived in Australia 25 to 30m years ago from Asia that skinks would have been their prey, resulting in evolutionary pressure to evolve venom resistance. 'What was fascinating was that with the kind of mutations that we documented in the Australian … skinks that gave rise to resistance are the kind of mutations that we've seen in other animals outside Australia,' Fry said. Mongooses, which feed on cobras, are one such example. The researchers showed that the Australian major skink, Bellatorias frerei had the same mutation that gave the honey badger its resistance to cobra venom. The researchers looked at 47 skink species and found that 13 of these were resistant to snake venom. Of these 13 species, some had multiple types of resistance, leading the researchers to discover that the skinks had developed independent mutations conferring resistance on 25 occasions. Fry said the researchers used tissue banks from museums across Australia rather than testing venom on live skinks. Study co-author and UQ researcher Dr Uthpala Chandrasekara said in a statement: 'We used synthetic peptides and receptor models to mimic what happens when venom enters an animal at the molecular level and the data was crystal clear, some of the modified receptors simply didn't respond at all.' 'It's fascinating to think that one tiny change in a protein can mean the difference between life and death when facing a highly venomous predator. Sign up to Breaking News Australia Get the most important news as it breaks after newsletter promotion 'The more we learn about how venom resistance works in nature, the more tools we have for the design of novel antivenoms.' Dr Andrew Amey, collection manager of amphibians, reptiles and herpetology at Queensland Museum, who was not involved in the research, said that there were more than 470 currently recognised species of Australian skink, with more being discovered all the time – with little known about them. 'It is great to see research looking into how they deal with such an important predator that just might tell us more about how we can manage the effects of snakebite ourselves,' Amey said. The study was published in the International Journal of Molecular Sciences.

Kamchatka is moving AWAY from Russia: Scientists are baffled as peninsula shifts 6.5ft southeast following magnitude 8.8 earthquake
Kamchatka is moving AWAY from Russia: Scientists are baffled as peninsula shifts 6.5ft southeast following magnitude 8.8 earthquake

Daily Mail​

time4 hours ago

  • Daily Mail​

Kamchatka is moving AWAY from Russia: Scientists are baffled as peninsula shifts 6.5ft southeast following magnitude 8.8 earthquake

Last week, Russia 's Kamchatka Peninsula was hit by a magnitude 8.8 earthquake –the sixth–largest ever recorded. The tremor released enormous amounts of destructive energy, triggering tsunami warnings as far away as Chile and the western United States. But when the activity had subsided, scientists from the Russian Academy of Sciences were baffled to find that the peninsula had actually moved away from the mainland. In some places towards the peninsula's southern tip, the landmass had drifted as much as 6.5ft (two metres) to the southeast. That is similar to the movement caused by Japan 's 9–magnitude Tohoku earthquake in 2011 – the fifth–largest earthquake ever recorded. In a post on Telegram, the Russian Academy of Sciences wrote: 'We made a preliminary calculation based on the results of geodynamic observations. 'It turned out that we all went quite well to the southeast. 'The maximum coseismic displacements after the earthquake of July 30 were observed in the southern part of the peninsula.' Earthquakes occur along Earth's faultlines - points where the tectonic plates meet and move past one another. On average, the tectonic plates only move about 0.6 inches (1.5 centimetres) per year, but that movement isn't even and steady. In places like the Kamchatka Peninsula, where the Eurasian and Pacific plates meet, the plates become caught and lock against one another. When this happens, huge amounts of pressure are built up in the rocks along the faultline, which is ultimately released in the form of an earthquake. Scientists call this process elastic rebound, and it explains why landmasses move so quickly during periods of intense seismic activity. As the tectonic plates release pressure in the form of an earthquake, the two plates can slip past each other and often move several metres at a time. This process can actually continue for days or even weeks following the initial earthquake as the plates settle and adjust their positions. In the Kamchatka Peninsula earthquake last Wednesday, the release of such a large amount of built–up pressure allowed the entire peninsula to move up to 6.5 feet southeast. The earthquake released enormous amounts of energy, which triggered tsunamis that swept the nearby area (pictured), and led to tsunami warnings as far away as Chile and the western United States This process also explains why large earthquakes rarely arrive as isolated incidents but, rather, as sequences. The Kamchatka earthquake followed a 10–day sequence made up of 50 magnitude 5.0 or larger earthquakes, including three magnitude 6.6 tremors and a magnitude 7.4 earthquake on July 20. Similarly, large earthquakes are almost always followed by aftershocks – smaller earthquakes which follow in the wake of the main event. Professor David Tappin, lead tsunami expert at the British Geological Survey, told Daily Mail: 'They result from the sudden change in stress within and between rocks after the principal earthquake, as the displaced crust adjusts to the effects of the main shock. 'Aftershocks can happen in the days, months, or even years after the initial earthquake and are typically smaller than the main shock.' According to the United States Geological Survey (USGS), the Kamchatka earthquake has already been followed by magnitude 6.9 and 6.2 aftershocks. The USGS says that the sequence remains active and that more aftershocks remain likely. The USGS predicts there is a 47 per cent chance of there being at least one magnitude 7.0 or larger earthquake in the month following the Kamchatka earthquake. These slips mean the aftershocks remain likely. This graph shows the likelihood that at least one earthquake of a given magnitude will occur within a month of last week's activity Within a year, there is a 13 per cent chance that the region will be hit by a magnitude 8.0 or larger event. Scientists believe that the flurry of activity following the initial earthquake has now also triggered two volcanic eruptions in the region. The Kamchatka Peninsula is situated directly above the Ring of Fire, a 25,000–mile chain of volcanoes that stretches around the Pacific Ocean. The Ring of Fire is home to over 425 active volcanoes, including 22 within the peninsula itself. Just hours after the earthquake, Klyuchevskaya Sopka, the largest volcano in the region, exploded with a stream of lava and ash. On August 3, the Krasheninnikov Volcano then became the second volcano to suddenly erupt following the earthquake. As it erupted for the first time in over 500 years, the volcano sent a plume of ash 3.7 miles (6 km) into the sky. Scientists believe that these eruptions were triggered by the earthquake, which opened new faults in the rock and allowed more magma to escape towards the surface. Those changes in structural integrity and pressure may have pushed Klyuchevskaya Sopka and Krasheninnikov into erupting. This has sparked concerns that Russia's recent earthquakes could trigger a wave of devastating volcanic eruptions along the Ring of Fire. However, earthquakes will only trigger eruptions in volcanoes which are close to eruption. That means scientists do not expect to see significantly increased rates of volcanic activity along the geological fault. The Earth is moving under our feet: Tectonic plates move through the mantle and produce Earthquakes as they scrape against each other Tectonic plates are composed of Earth's crust and the uppermost portion of the mantle. Below is the asthenosphere: the warm, viscous conveyor belt of rock on which tectonic plates ride. The Earth has fifteen tectonic plates (pictured) that together have moulded the shape of the landscape we see around us today Earthquakes typically occur at the boundaries of tectonic plates, where one plate dips below another, thrusts another upward, or where plate edges scrape alongside each other. Earthquakes rarely occur in the middle of plates, but they can happen when ancient faults or rifts far below the surface reactivate. These areas are relatively weak compared to the surrounding plate, and can easily slip and cause an earthquake.

How the ‘Little Boy' Hiroshima nuclear bomb transformed modern warfare forever
How the ‘Little Boy' Hiroshima nuclear bomb transformed modern warfare forever

The Independent

time4 hours ago

  • The Independent

How the ‘Little Boy' Hiroshima nuclear bomb transformed modern warfare forever

Eighty years ago, a weapon was used which would transform modern warfare and the entire world forever. Hiroshima, in Japan, was the target of the first ever nuclear weapon, dropped by the US Air Force on 7 August 1945 - killing more than 150,000 people in the months afterwards, according to some estimates. Although victory had been declared in Europe four months earlier, American forces continued to fight Japan over the summer, in what would be the final months of the protracted Pacific War. Just three days after the catastrophic nuclear attack on Hiroshima, Nagasaki met a similar fate. It had been just weeks since the first successful test of a nuclear weapon was masterminded by J. Robert Oppenheimer. Eighty years later, The Independent takes a look at the direction nuclear warfare took after that seminal day - and how different nuclear weapons are now How has the nuclear bomb developed since 1945? Nicknamed 'Little Boy', the bomb dropped on Hiroshima exploded some 1,800 feet above the city, where it delivered around 12.5 kilotons of TNT. Large sections of the city - five square miles - were razed to ashes. Within just four days, 120,000 people were killed, many instantly vaporised and others dying due to the impact of the burns and radiation in the days afterwards. ''Little Boy' was a gun-type weapon, which detonated by firing one mass of uranium down a cylinder into another mass to create a self-sustaining nuclear reaction,' the National Museum of the US Air Force explains. 'Weighing about 9,000 pounds (4.5 tons), it produced an explosive force equal to 20,000 tons of TNT [explosive].' Delivered by the USAAF B29 bomber `Enola Gay', 'Little Boy' has now been entirely taken out of operational use - but its creation had set US and Russian scientists into a frantic race to develop the largest and most powerful nuclear weapons, in the largest quantities. Seven years after the two Japanese cities were decimated by the atomic bomb, the US tested a brand new type of nuclear weapon: the hydrogen bomb. First tested at Enewetak Atoll in the Marshall Islands, the hydrogen bomb was 500 times more powerful than the one used in Hiroshima. It is believed that many if not all current nuclear weapons in America's stockpile are hydrogen - or thermonuclear - weapons. The largest ever bomb test was conducted by the Soviet Union, who tested a 58-megaton atmospheric nuclear weapon nicknamed the 'Tsar Bomb' near northern Russia. In recent decades, following many years of international efforts to prevent the production of new nuclear weapons, the US has focussed on modernising its existing stockpile. According to the Bulletin of the Atomic Scientists (BAS), the US has begun a modernisation programme which will 'ultimately see every nuclear delivery system replaced with newer versions over the coming decades'. How large have nuclear arsenals grown? The Hiroshima bomb was dropped a mere three weeks after the Trinity test, the first successful test of a nuclear weapon the world had ever seen. At the time, the American nuclear arsenal consisted of two weapons: the bombs which were used to destroy large areas of Hiroshima and Nagasaki, a catastrophe for the Japanese people, hundreds of thousands of whom were killed. But it was seen by some as one of the main reasons World War Two came to an end when it did. Fast forward five years and the US had developed 299 more nuclear weapons, a nuclear arsenal nearly 60 times larger than that of the Soviet Union, which contained five, having tested its first nuclear bomb just one year earlier in 1949. After a rapid period of dramatically increasing stockpiles during the Cold War saw the US stockpile hit a peak of 31,255 in 1961 and the Russian stockpile peak at 45,000 in 1986 - according to BAS estimates - numbers steadily decreased for decades. The International Campaign to Abolish Nuclear Weapons (ICAN) says the US has approximately 5,044. Russia is estimated to have around 5,580, making it the world's largest stockpile. In descending order of the size of their arsenal, the other seven countries believed to have nuclear weapons are China, France, United Kingdom, Pakistan, India, Israel, North Korea. Not all of these countries openly admit they possess the weapons. In the eight decades since the catastrophes in Hiroshima and Nagasaki, nuclear weapons have never been used in combat - but the incomparable destructiveness of hydrogen bombs and the sheer number of nuclear weapons in the world makes their risk far greater.

DOWNLOAD THE APP

Get Started Now: Download the App

Ready to dive into a world of global content with local flavor? Download Daily8 app today from your preferred app store and start exploring.
app-storeplay-store