
What are the strongest earthquakes ever recorded?
The 8.8-magnitude temblor set off warnings in Hawaii, North and Central America and Pacific islands south toward New Zealand.
Here's a glance at some of the most powerful earthquakes recorded previously, according to the US Geological Survey.
1. Biobío, Chile
A 9.5-magnitude earthquake struck in a central region of Chile in 1960. Known as the Valdivia earthquake or Great Chilean earthquake, the largest ever recorded temblor resulted in more than 1,600 deaths in the country and beyond, most of which were caused by the resulting large tsunami. Thousands of people were injured.
2. Alaska
In 1964, a 9.2-magnitude earthquake jolted the Alaska's Prince William Sound, lasting for almost five minutes. More than 130 people were killed in the largest recorded earthquake in the US and subsequent tsunami. There were huge landslides and towering waves that caused severe flooding. The event was followed by thousands of aftershocks for weeks after the initial quake.
3. Sumatra, Indonesia
A 9.1-magnitude earthquake and resulting tsunami devastated south-east and south Asia and east Africa in 2004, killing 230,000 people. Indonesia alone recorded more than 167,000 deaths as entire communities were wiped out.
4. Tohoku, Japan
A 9.1-magnitude earthquake struck off the coast of north-eastern Japan in 2011, triggering a towering tsunami that smashed into the Fukushima nuclear plant. It knocked out power and cooling systems and triggered meltdowns in three reactors. More than 18,000 people were killed in the quake and tsunami, some of whom have never been recovered.
5. Kamchatka, Russia
In 1952, a 9.0-magnitude quake caused significant damage but no reported deaths despite a tsunami that hit Hawaii with 9.1-metre (30ft) waves.
6. Biobío, Chile
A huge 8.8-magnitude earthquake hit central Chile in 2010, shaking the capital for a minute and half and setting off a tsunami. More than 500 people were killed in the disaster.
7. Esmeraldas, Ecuador
In 1906, an 8.8-magnitude earthquake and resulting tsunami killed 500 to 1,500 people. Its effects were felt for miles along the Central American coast and as far as San Francisco and Japan.
8. Alaska
In 1965, an 8.7-magnitudequake struck Alaska's Rat Islands, causing a tsunami with waves 11-metres (35ft) high. There was some relatively minor damage, including cracks in buildings and an asphalt runway.
9. Tibet
At least 780 people were killed when an 8.6-magnitude earthquake struck in 1950. Dozens of villages were destroyed, including at least one that slid into a river. There were also major landslides that jammed the Subansiri River in India. When the water eventually broke through, it resulted in a deadly 7-metre (23) wave.
10. Sumatra, Indonesia
In 2012, a powerful 8.6-magnitude earthquake struck off the west coast of northern Sumatra in Indonesia. Though the quake caused little damage, it increased pressure on a fault that was the source of the devastating 2004 tsunami.

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The Sun
an hour ago
- The Sun
‘Ring of Fire' roars again as THIRD volcano rumbles to life in wake of 8.8 megaquake after first eruption in 600 years
SCIENTISTS have warned of the growing number of volcanic eruptions along the Pacific "Ring of Fire" triggered by an enormous earthquake. A chain of three volcanoes has now been set off - with the first roaring back to life with its first eruption in 600 years on Sunday evening. 4 The Krasheninnikov volcano in the Kamchatka Peninsula, Russia, spewed a colossal column of ash nearly 4 miles into the sky in the "historic" eruption. A second, Klyuchevskaya Sopka, the largest in the region, exploded with a stream of scalding lava just hours later. And the alarm was raised on Monday evening local time over rumbling at a third site, the Mutnovsky volcano. The public has been strongly warned against visiting the volcano after a "thermal anomaly" was picked up by the Kamchatka Volcanic Eruption Response Team (KVERT). The string of geological detonations was ignited by a monster 8.8 magnitude earthquake last Wednesday - the sixth-strongest ever recorded. Its epicentre was around 84 miles southeast of the Kamchatka Peninsula and triggered tsunami warnings across a wide area around the Pacific. Whilst the destructive tsunami waves feared thankfully did not materialise, heartbreaking videos did emerge of whales killed by the quake washing up on beaches. 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. The volcanoes being activated lie along the "Ring of Fire" - an enormous horseshoe-shaped strip surrounding the Pacific Ocean which contains hundreds of volcanoes. Dr Ozerov said: "We associate the eruptions with the earthquake, which activated magmatic centres, and 'pumped' additional energy into them." Scientists explain that the powerful earthquake likely destabilised the earth's crust and created fracturs which magma can push through. Dr Jonathan Paul, a volcanologist from Royal Holloway University of London, told the 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." He said the delay between the initial earthquake and the eruption of Krasheninnikov was likely due to the fact that cracks in the rock take time to develop. In the interim period, magma would have been forcing itself through new lines of weakness and building up enough pressure to break through, he said. The succession of eruptions has sparked fears that more are on the way along the Ring of Fire volcanoes - 160 of which are in Kamchatka. Michael Manga, a geoscientist at the University of California, Berkeley, previously said: "The volcanoes in volcanic arcs, including Chile, the US Cascades, Japan, Indonesia and Kamchatka, are prone to erupt after earthquakes." 4 The last time Krasheninnikov erupted was sometime between 1423 and 1503. KVERT issued an aviation "red alert" warning of significant levels of ash in the air. As of Monday evening local time, the eruption remained active with the emergency group warning that ash explosions of up to 10 km could occur at any time. Russian volcanologist Alexei Ozerov said of the Krasheninnikov eruption: "A crack opened up along the volcano from the top of the crater, and a steam-gas mixture is currently rising from this crack. "Emissions are occurring, and a large amount of ash was ejected during the opening of the crater crack. "This ash reached the Valley of Geysers, and the smell of gas. "A question is immediately raised about the evacuation of the Valley of Geysers, those tourists who are there." What is the Ring of Fire? THE Ring of Fire is an enormous horseshoe-shaped band around the Pacific Ocean which experiences extremely elevated tectonic activity. Around 90 percent of the world's earthquakes occur within the bounds of the 25,000 mile-long, 300 mile-wide zone. And somewhere between 750 and 915 volcanoes lie in the zone, depending on which areas are included. The density of earthquakes and volcanoes along the Ring of Fire is created by the borders of various tectonic plates meeting. Primarily, it is the Pacific Plate interacting with others - such as the the Eurasian, North American, and Australian plates. These are constantly moving past, colliding with and sliding beneath one another, creating an immense amount of stress and pressure in the earth's crust. The Ring of Fire traces the Pacific coast up from the southern tip of South America, along the coast of North America, across to Asia and down the coasts of Japan, the Philippines and Indonesia before reaching New Zealand.


Daily Mail
4 hours ago
- Daily Mail
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
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.


BBC News
4 hours ago
- BBC News
The quest to make an ice cream that doesn't melt
Ice cream is a staple of summer – but melts quickly when the mercury rises. Can scientists help it keep its cool? Few things delight on a summer day like an ice cream cone. Few things cause such despair, however, like the total disintegration of said ice cream, running down one's fingers, sagging from the cone, heading earthwards before you can say "toddler meltdown". Any number of rhapsodies could be written about the pleasures of something so short-lived, all the sweeter for their brevity. But you would have to go to another story to find them, because here we will not tolerate such masochism. Reports of Japanese manufacturer Kanazawa Ice's ice pops, and, later on, soft-serve ice cream, withstanding numerous heat-based assaults without melting, went viral some years ago, however. The scientists behind this ice cream had pumped it full of polyphenols, a class of antioxidant molecules found in many fruits. The result was a curious stability, a notable lack of creamy liquid running over fingers. How did it work? Ice cream is composed primarily of cream and sugar. Machines for producing the stuff churn the sweet slurry in a refrigerated drum, and when it forms a frozen film on the drum's interior, a scraper chips it off. This keeps the ice crystals from growing to a distasteful size, the phenomenon behind the slightly jagged texture of some ice cream when you bring it home from the grocery store. When ice cream, somewhere in the long trip between factory and your freezer, heats up slightly, melts, and then is refrozen, chunky, unpleasant crystals result. This is a known problem with taking ice cream from its first freezer into a world full of temperatures greater than zero. Ice cream manufacturers already use a number of stabilisers, such as carrageenan, from seaweed, and guar gum (from guar seeds), to try to keep ice cream from suffering too much from its journeys. When Cameron Wicks, a food scientist then studying at the University of Wisconsin who now works at food producer General Mills, saw the video of Kanazawa Ice's no-melt ice cream, she wondered how the polyphenols had their stabilising effect. The molecules are known for their potential health-promoting traits, not necessarily their engineering qualities. In the lab, she began to experiment with cream mixtures using higher and higher levels of one particular polyphenol: tannic acid. In experiments where she mixed cream with 0.75%, 1.5%, and 3% tannic acid, she noticed that almost immediately, the higher concentrations began to thicken. After chilling the mixtures for 24 hours, she took measurements and noted that tannic acid had caused them to gel, so strongly that the 3% mixture could be cut with a knife or turned upside down without falling out of a cup. Putting the cream under the microscope, Wicks saw that the higher concentrations had more distinct fat globules. The tannic acid, she and her colleagues surmised, was interacting with the proteins in the cream, creating a supportive network or barrier to the merging of the fat globs. That would explain why ice cream made from such a substance is resistant to melting: the liberated fats from the melted crystals of cream would not be able to run down, thanks to the addition of the polyphenol. More like this:• Should you avoid dairy when you have a cold?• Why not all comfort food is the same• The explosive potential of custard powder That said, this chemical trick is not a way to freeze time and break the physical laws of the Universe. It's more like a bra for your ice cream – or a nice, supportive pair of dessert hosiery. As the hours pass, Wicks found in later experiments, ice cream made this way acquires a pudding-like texture, although it will continue more or less in its previous shape. And polyphenols do not, of course, keep the ice cream cold. Ice cream that does not melt, that instead warms up into a rubbery monolith, is not really what most of us expect from a frozen dessert. Expectation matters more than you think when it comes to food. If you expect vanilla ice cream, and discover upon taking a bite that it is mashed potatoes, it is a profound readjustment. Perhaps polyphenols will join the ranks of more established stabilisers, helping to keep ice cream more or less at it should be through the travails of long-distance travel. But will high-dose polyphenol desserts, designed to withstand a hair dryer's blast or to hold their shape for hours make their way to an ice cream stand near you? Only time will tell. -- For more science, technology, environment and health stories from the BBC, follow us on Facebook and Instagram.