Tag Archives: Underwater

Majority Of Dogecoin Holders In Profit, While 67% Of Shiba Inu Owners Are Underwater – Benzinga

  1. Majority Of Dogecoin Holders In Profit, While 67% Of Shiba Inu Owners Are Underwater Benzinga
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  3. Most Dogecoin (DOGE) Holders in Profit As Over 65% of Shiba Inu (SHIB) Owners Languish Underwater: IntoTheB… The Daily Hodl
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Space Shuttle Challenger remnants discovered underwater



CNN
 — 

Explorers trudged the Atlantic Ocean searching for World War II artifacts lost at sea, but they stumbled on something else — a 20-foot-long piece of debris from the Space Shuttle Challenger, which was destroyed shortly after takeoff in 1986.

The History Channel and NASA revealed Thursday that the Challenger segment was discovered off Florida’s east coast during the filming of a new series called “The Bermuda Triangle: Into Cursed Waters.” The series is set to premiere this month on the History Channel.

The Challenger broke apart after its launch on January 28, 1986, killing all seven crew members aboard, including a teacher was set to become the first civilian in space. TV viewers, especially students in schools across the US, watched a live broadcast of the blast in horror that morning.

“NASA currently is considering what additional actions it may take regarding the artifact that will properly honor the legacy of Challenger’s fallen astronauts and the families who loved them,” the space agency said in a news release.

Mike Barnette, an underwater explorer who led the crew that found the shuttle artifact, remembers watching the tragedy on TV in his high school classroom. He called it “sobering” to realize that his team found a scrap from the spacecraft — the first debris to be discovered since pieces from the shuttle washed ashore in 1996.

“I can almost smell the smells of that day,” Barnette told CNN in a phone interview Thursday, referring to the day the Challenger exploded. “It was just so burned into my brain.”

Barnette and his team of investigators set off in March to search suspected shipwreck sites in the Bermuda Triangle, a swath of the northern Atlantic Ocean said to be the site of dozens of shipwrecks and plane crashes. The team also set its sights on one area outside the triangle, just off Florida’s Space Coast, where NASA has launched rockets since its inception.

The team was searching for a WWII-era rescue plane that mysteriously disappeared in December 1945, but a more modern object partially covered by sand on the seafloor sparked interest and further investigation from the dive team, according to the History Channel.

During the first dive, Barnette said a storm caused the water to turn so murky it was like swimming in Guinness beer. “We had terrible visibility,” he said.

The divers carried out a second excursion in May and finally captured clear footage of the wreckage. They brought evidence of their discovery to retired NASA astronaut Bruce Melnick, a longtime friend of Barnette’s, who immediately suggested it could be detritus from the Challenger disaster.

Distinctive square tiles from the Challenger tipped the explorers off, suggesting they had uncovered a large chunk of the orbiter’s underbelly. The underbelly was coated in thousands of silicon tiles protecting the shuttle from heat as it returned into the Earth’s atmosphere from space.

The team turned its findings over to NASA in August, and the space agency recently confirmed the origins of the debris after reviewing footage from the dive, according to a news release.

The final Challenger mission was set to carry seven people into space — NASA astronauts Francis “Dick” Scobee, Michael Smith, Ronald McNair, Ellison Onizuka, Judith Resnik and Gregory Jarvis as well as Christa McAuliffe, a New Hampshire schoolteacher who was set to become the first citizen space shuttle passenger as part of a new NASA program.

But 73 seconds after takeoff from its Florida launch site, the Challenger exploded, killing everyone on board. A NASA investigation later revealed a rubber “O-ring” seal on one of Challenger’s solid rocket boosters had failed because it was exposed to unusually low temperatures while the space shuttle sat on the launchpad. It caused a leak of highly explosive gases, which ultimately led to the catastrophic explosion.

“While it has been nearly 37 years since seven daring and brave explorers lost their lives aboard Challenger, this tragedy will forever be seared in the collective memory of our country. For millions around the globe, myself included, Jan. 28, 1986, still feels like yesterday,” NASA Administrator Bill Nelson said in a statement.

“This discovery gives us an opportunity to pause once again, to uplift the legacies of the seven pioneers we lost, and to reflect on how this tragedy changed us. At NASA, the core value of safety is — and must forever remain — our top priority, especially as our missions explore more of the cosmos than ever before.”

The six-part series “The Bermuda Triangle: Into Cursed Waters” premieres at 10 p.m. ET on November 22 on the History Channel.

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Soaked passenger basically ‘went underwater’ during Splash Mountain ride: ‘Did him dirty’

There’s a reason Disneyland named it Splash Mountain — and it’s not because you leave the ride dry.

“You will get wet,” Disney warns of the famous ride on its website. Splash Mountain includes 950,000 gallons of water, three dips and a five-story drop.

TikToker @bozoztok posted footage of a group of passengers on the ride. But it wasn’t the big drop that left a man in the front with a particularly memorable experience.

“Splash Mountain did him dirty,” the video text read.

The incident happened during the indoor portion of the ride. As the boat made a small dip down an incline, the man in the front seat went directly into the water.

People screamed in shock and excitement in the background. When the boat came up and stabilized, the man was completely soaked in water.

According to Disney, how drenched you get depends on where you’re seated. Riders in the back may only get a “splash or spray,” while those in the front “can expect to get soaked.”

People in the TikTok comments shared their experiences on the ride.

“It’s never the big drop on the outside, it’s always the dark drop on the inside that gets everyone,” someone commented.

“No but the Disneyland version gets you drenched for no reason,” a user said.

“I always get soaked on this drop. Always more than the big drop,” a TikToker wrote.

“The man basically went underwater,” a person replied.

“I love that drop omg. It’s so funny watching the person in the front,” another added.

The post Soaked passenger basically ‘went underwater’ during Splash Mountain ride appeared first on In The Know.

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Powerful Underwater Volcano Sets New Record for Highest Debris Cloud in Recorded History

Debris from the January eruption of the Tonga-Hunga Ha’apai volcano in the South Pacific was blasted into the air with such force that it actually reached the mesosphere, according to the results of a new scientific study.

On January 15 earlier this year, the underwater Hunga Tonga-Hunga Ha’apai volcano erupted with a cataclysmic force, roughly 65 km (40 miles) off the coast of the Kingdom of Tonga. The violence of the explosion blasted an enormous cloud of debris skyward and gave rise to a gigantic tsunami that tragically claimed the lives of six.

According to the results of a new scientific study published in the journal Science, the plume of ash and gas from this powerful explosion may be the tallest of its kind since records began.

Google Earth Timelapse – 1985 vs. 2020

Volcanic eruptions are known for spewing out vast clouds of debris that are capable of causing widespread disruption and damage, halting air travel, and, in extreme events, noticeably affecting the climate.

Whilst there have been numerous eruptions forceful enough to loft volcanic material high into the sky, very few were powerful enough to launch debris to an altitude 30 km (19 miles) above the Earth. According to the new research, the plume ejected from the Hunga Tonga-Hunga Ha’apai volcano was blasted much higher than this, and may have even reached up into the mesosphere.

Ordinarily, scientists are able to determine the height of a plume by taking measurements of its temperature and comparing it to the temperatures of pockets of air at various altitudes. This method works because the gas in Earth’s atmosphere is known to get increasingly colder at higher altitudes.

A zoomed-in view of the eruption, taken by Japan’s Himawari-8 satellite at 05:40 UTC on 15 January 2022, about 100 minutes after the eruption started. (Photo credit: Simon Proud / Uni Oxford, RALSpace NCEO / Japan Meteorological Agency)

However, when material is pushed very high into the atmosphere, this method ceases to be effective, as the air temperature actually starts to increase with altitude.

In order to accurately measure the height of Hunga Tonga-Hunga Ha’apai’s plume, the scientists behind the study instead turned to data collected by a trio of satellites in geosynchronous orbit.

Each of the weather satellites observed the eruption from a vantage point roughly 36,000 km above Earth’s surface. Despite sharing similar orbital heights, each spacecraft imaged the cloud from a different perspective. The images were captured in 10-minute intervals throughout the eruption.

By observing the cloud from multiple perspectives and combining the images with known quantities such as the distances between points on the planet’s surface, the team was able to determine the true height of the plume, thanks to a phenomenon known as the parallax effect.

The analysis revealed that the power of Hunga Tonga-Hunga Ha’apai’s eruption sent volcanic material soaring an incredible 57 km (35 miles) above the planet’s surface. That means the debris was blasted well into the third layer of Earth’s atmosphere known as the mesosphere, where fast-moving meteorites end their lives in fiery displays as shooting stars.

Moving forward, the team hopes to discover why the underwater eruption created such a high-altitude plume, and to develop an automated system for determining the height of volcano plumes via the parallax effect.

Stay tuned to IGN for all the weirdest and most important developments from around the scientific world.

Anthony is a freelance contributor covering science and video gaming news for IGN. He has over eight years experience of covering breaking developments in multiple scientific fields and absolutely no time for your shenanigans. Follow him on Twitter @BeardConGamer.

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‘Avatar: Way of Water’ Trailer Draws You Into Gorgeous Underwater World

A new trailer for Avatar: The Way of Water came out Wednesday, taking fans back to the world of the blue-skinned Na’vi for the first time since 2009. The full Avatar 2 trailer follows a teaser trailer that came out in May and drew 25 million views in five months.

The movie hits theaters Dec. 16.

Wednesday’s trailer gives us a fresh look at the visually spectacular world that director James Cameron crafted for his sequel, along with hints of the trials Jake Sully, Neytiri and their family face.

Cameron shot many sequences underwater, using new cameras developed for that purpose.

Sam Worthington, Zoe Saldaña, Stephen Lang, CCH Pounder and Giovanni Ribisi are among those reprising their roles from the  original film, with Sigourney Weaver back in a different part. Worthington plays Jake Sully, who left his human body to wed Saldaña’s Neytiri and join her in life on Pandora. 

Weaver played a human, Dr. Grace Augustine, in the first film, but returns as Jake and Neytiri’s daughter Kiri. Kate Winslet joins the cast as a free diver named Ronal. Winslet learned free diving for the film and reportedly held her breath for a whopping seven minutes.

The film has been rumored to top three hours, though the final length is still not public. Cameron told Empire in May: “I don’t want anybody whining about length when they sit and binge-watch [television] for eight hours…. It’s OK to get up and go pee.”

Get used to seeing the lush world of Pandora again because three sequels to this film are planned, coming in 2024, 2026 and 2028.

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Tonga underwater volcanic eruption produced the highest plume on RECORD, study reveals 

The Tonga volcanic eruption in January produced the highest ever recorded plume, scientists have confirmed.

Hunga Tonga-Hunga Ha’apai, an underwater volcano in the South Pacific, released an ash cloud that was 187,000 feet (57 km/35 miles) high.

Its colossal eruption on January 15 this year was also the first recorded to have broken through into the third layer of the atmosphere – the mesosphere.

The mesosphere starts about 160,000 feet (48 km) above us, and is where passing meteors start to burn up and form shooting stars.

Researchers from the University of Oxford and RAL Space used three geostationary weather satellites to accurately measure the massive plume’s height.

The previous record-holder, the 1991 eruption of Mount Pinatubo in the Philippines, caused a plume that was recorded as 131,000 feet (40 km/ 25 miles) high.

‘It’s an extraordinary result as we have never seen a cloud of any type this tall before,’ said lead author Dr Simon Proud.

‘Furthermore, the ability to estimate the height in the way we did, using the parallax method, is only possible now that we have good satellite coverage. 

‘It wouldn’t have been possible a decade or so ago.’

Parallax-based retrievals of plume altitude at 04:30 GMT on 15 January 2022 overlaid on Himawari-8 data for the same time frame

WHAT IS THE ‘PARALLAX EFFECT’? 

The parallax effect is the difference in the apparent location of an object viewed along two different lines of sight.

You can see this effect by closing your right eye, and holding out one hand with the thumb raised upwards. 

If you then switch eyes, so that your left is closed and your right is open, your thumb will appear to shift slightly against the background.

Astronomers use this effect to measure large distances, like between the Earth and stars.

The parallax effect

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The Hunga Tonga-Hunga Ha’apai eruption took place in the southern Pacific Ocean, around 40 miles (65km) from Tonga’s main island.

It triggered a 7.4 magnitude earthquake, sending tsunami waves crashing into the island that were felt as far away as Russia, the United States and Chile.

The eruption released more energy than the Tsar Bomba – the most powerful nuclear bomb ever detonated – and blasted 20,000 Olympic swimming pools-worth of water into the stratosphere.

For the study, published today in Science, scientists wanted to accurately measure how far the towering column of ash and water produced stretched into the atmosphere.

Normally, this is done by measuring the temperature of the top of the plume using infrared-based satellites and comparing it to standard temperatures at different known altitudes.

This can be done because previous plumes have only extended into the troposphere, the first layer of the atmosphere, where temperature decreases with height.

However, the Hunga Tonga-Hunga Ha’apai cloud went into the third layer of the atmosphere, the mesosphere.

Due to the ozone layer absorbing solar ultraviolet radiation, temperatures in the stratosphere and mesosphere actually increase with height.

So, to measure the plume, Dr Proud’s team developed a different technique that utilises the ‘parallax effect’ – the difference in the apparent location of an object viewed along two different lines of sight.

This technique allows researchers to calculate the distance between the object and both viewers.

The location of the Tonga volcano is covered by three weather satellites, all 22,000 miles (36,000 km) up in space – the GOES-17 from the US, Himawari-8 from Japan and GeoKompSat-2A from South Korea.

Aerial shots taken by these satellites of known location were used to gauge the plume’s height.

On top of that, they recorded images every ten minutes, meaning the researchers could document rapid changes in the plume’s trajectory.

Dr Proud said: ‘Thirty years ago, when Pinatubo erupted, our satellites were nowhere near as good as they are now. They could only scan the earth every 30 minutes. Or maybe even every hour.’

Evolution of volcanic plume altitude over time. Infrared (IR) heights are derived from Himawari-8 satellite measurements and known temperature standards from the European Centre for Medium-Range Weather Forecasts. The blue lines indicate altitudes estimated by the stereoscopic method across the entire plume, and the green markers are parallax heights derived from a manual analysis of data from Himawari-8, GK-2A, and GOES-17 satellites

An animation showing the evolution of the height of the Hunga Tonga-Hunga Ha’apai eruption plume, measured using the stereoscopic method applied to images from three weather satellites.

Dr Proud also speculates that the estimation for the Mount Pinatubo eruption could be incorrect as a result of the reduced satellite data available at the time.

He said: ‘We think for Pinatubo we actually missed the peak of the activity and the points where it went the highest – it fell between two of the satellite images and we missed it.’

The researchers now intend to construct an automated system to compute the heights of volcano plumes using the parallax method. 

They hope that a dataset of plume heights will help other scientists model the dispersion of volcanic ash in the atmosphere.

The Hunga Tonga-Hunga Ha’apai eruption took place in the southern Pacific Ocean, around 40 miles (65km) from the country’s main island 

Its colossal eruption on January 15 this year was the first recorded to have broken through into the third layer of the atmosphere – the mesosphere. It also caused many effects, like atmospheric waves, extreme winds and unusual electric currents, that were felt around the world and into space

The previous record-holder, the 1991 eruption of Mount Pinatubo in the Philippines, caused a plume that was recorded as 131,000 feet (40 km/ 25 miles) high (pictured)

WHAT HAPPENED DURING THE JANUARY TONGA ERUPTION? 

Hunga Tonga-Hunga Ha’apai, an underwater volcano in the South Pacific, spewed debris as high as 25 miles into the atmosphere when it erupted on January 15.

It triggered a 7.4 magnitude earthquake, sending tsunami waves crashing into the island, leaving it covered in ash and cut off from outside help. 

It also released somewhere between 5 to 30 megatons (5 million to 30 million tonnes) of TNT equivalent, according to NASA Earth Observatory.  

Digital elevation maps from the NASA Earth Observatory also show the dramatic changes at Hunga Tonga-Hunga Ha’apai, the uppermost part of a large underwater volcano. 

Prior to the explosion earlier this month, the twin uninhabited islands Hunga Tonga and Hunga Ha’apai were merged by a volcanic cone to form one landmass.

Hunga Tonga and Hunga Ha’apai are themselves remnants of the northern and western rim of the volcano’s caldera – the hollow that forms shortly after the emptying of a magma chamber. 

NASA said the eruption ‘obliterated’ the volcanic island about 41 miles (65km) north of the Tongan capital Nuku’alofa, on the island of Tongatapu (Tonga’s main island).

It blanketed the island kingdom of about 100,000 in a layer of toxic ash, poisoning drinking water, destroying crops and completely wiping out at least two villages.

It also claimed at least three lives in Tonga and resulted in the drowning deaths of two beachgoers in Peru after freak waves hit the South American country.  

Peruvian authorities have declared an environmental disaster after the waves hit an oil tanker offloading near Lima, creating a huge slick along the coast.

 

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Internet cable reveals the source of underwater vibrations

Credit: Pixabay/CC0 Public Domain

Scientists have harnessed Internet-transmitting fiber-optic cables to overcome a long-standing geophysical challenge: identifying where seismic noise in the ocean originates. Tiny vibrations of Earth called microseisms are ubiquitous, yet researchers have not had a way to pinpoint their sources in the sea. An innovative use of telecommunications equipment has changed that.

In the research now published in Geophysical Research Letters, Xiao et al. sent laser pulses through a commercially operated fiber-optic cable linking Valencia, Spain, to Palma on the Mediterranean island of Mallorca. The researchers then measured the small amount of light that bounced back through the cable, a technique called distributed acoustic sensing (DAS). When seismic vibrations disturbed the cable, they changed how the light returned to the source and let the researchers identify the origins of microseisms.

The researchers found that the microvibrations emanated from source regions between a few kilometers and about 10 kilometers across, but this source region migrated within a band between 7 and 27 kilometers from the coast, where the ocean was between 25 and 100 meters deep. Where the vibrations were strongest was not always near the source of the microseisms, however. Sometimes they were strongest in areas closer to or farther from shore.

The researchers hypothesize that this constantly shifting behavior is possible because wave-wave interactions at the sea surface are what cause microseisms, and the variable nature of local winds means that wave action also shifts.

Meanwhile, properties of the underwater environment such as depth, seafloor slope, and the seismic velocity of the subsurface structure might also influence microseisms, perhaps explaining why they were not always strongest near the source and suggesting that excitation of microseisms likely differs depending on bathymetry. The authors say their results reveal the potential of DAS for understanding microseism activity.


Waves in lakes make waves in the Earth


More information:
Han Xiao et al, Locating the Precise Sources of High‐Frequency Microseisms Using Distributed Acoustic Sensing, Geophysical Research Letters (2022). DOI: 10.1029/2022GL099292
Provided by
American Geophysical Union

This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original story here.

Citation:
Internet cable reveals the source of underwater vibrations (2022, October 3)
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This underwater camera operates wirelessly without batteries

Enlarge / MIT engineers built a battery-free, wireless underwater camera that could help scientists explore unknown regions of the ocean, track pollution, or monitor the effects of climate change.

Adam Glanzman

MIT engineers have built a wireless, battery-free underwater camera, capable of harvesting energy by itself while consuming very little power, according to a new paper published in the journal Nature Communications. The system can take color photos of remote submerged objects—even in dark settings— and convey the data wirelessly for real-time monitoring of underwater environments, aiding the discovery of new rare species or monitoring ocean currents, pollution, or commercial and military operations.

We already have various methods of taking underwater images, but according to the authors, “Most of the ocean and marine organisms have not been observed yet.” That’s partly because most existing methods require being tethered to ships, underwater drones, or power plants for both power and communication. Those methods that don’t use tethering must incorporate battery power, which limits their lifetime. While it’s possible in principle to harvest energy from ocean waves, underwater currents, or even sunlight, adding the necessary equipment to do so would result in a much bulkier and more expensive underwater camera.

So the MIT team set about developing a solution for a battery-free, wireless imaging method. The design goal was to minimize the hardware required as much as possible. Since they wanted to keep power consumption to a minimum,  for instance, the MIT team used cheap off-the-shelf imaging sensors. The trade-off is that such sensors only produce grayscale images. The team also needed to develop a low-power flash as well, since most underwater environments don’t get much natural light.

Enlarge / Overview of how the underwater backscatter imaging system works.

S.S. Afzal et al., 2022

The solution to both challenges turned out to incorporate red, green, and blue LEDs. The camera uses the red LED for in situ illumination and captures that image with its sensors, then repeats the process with the green and blue LEDs. The image might look black-and-white, per the authors, but the three colors of light from the LEDs are reflected in the white part of each image. So a full-color image can be reconstructed during post-processing.

“When we were kids in art class, we were taught that we could make all colors using three basic colors,” said co-author Fadel Adib. “The same rules follow for color images we see on our computers. We just need red, green, and blue—these three channels—to construct color images.”

Instead of a battery, the sensor relies on piezo-acoustic backscatter for ultra-low-power communication after the image data has been encoded as bits. This method doesn’t need to generate its own acoustic signal (as with sonar, for instance), relying instead on modulating reflections of incident underwater sounds to transmit data one bit at a time. That data is picked up by a remote receiver capable of recovering the modulated patterns, and the binary information is then used to reconstruct the image. The authors estimate that their underwater camera is about 100,000 times more energy-efficient than its counterparts, and could run for weeks on end.

Naturally, the team built a proof-of-concept prototype and did some testing to demonstrate that their method worked. For instance, they imaged pollution (in the form of plastic bottles) in Keyser Pond in southeastern New Hampshire, as well as imaging an African starfish (Protoreaster lincklii) in “a controlled environment with external illumination.” The resolution of the latter image was good enough to capture the various tubercles along the starfish’s five arms.

Enlarge / Sample images obtained using underwater backscatter imaging.

S.S.. Afzal et al., 2022

The team was also able to use their underwater wireless camera to monitor the growth of an aquatic plant (Aponogeton ulvaceus) over several days, and to detect and locate visual tags often used for underwater tracking and robotic manipulation. The camera achieved high detection rates and high localization accuracy up to a distance of about 3.5 meters (about 11 and a half feet); the authors suggest longer detection ranges could be achieved with higher-resolution sensors. Distance is also a factor in the camera’s energy harvesting and communication capabilities, per tests conducted in the Charles River in eastern Massachusetts. As expected, both those critical capabilities decrease with distance, although the camera successfully transmitted data 40 meters (131 feet) away from the receiver.

In short, “The tetherless, inexpensive, and fully-integrated nature of our method makes it a desirable approach for massive ocean deployments,” the authors wrote. Scaling up their approach requires more sophisticated and efficient transducers, as well as higher-power underwater acoustic transmissions. It’s possible that one could also make use of existing mesh networks of buoys on the ocean surface, or networks of underwater robots like Argo floats, to remotely power the energy-harvesting cameras.

“One of the most exciting applications of this camera for me personally is in the context of climate monitoring,” said Adib. “We are building climate models, but we are missing data from over 95 percent of the ocean. This technology could help us build more accurate climate models and better understand how climate change impacts the underwater world.”

DOI: Nature Communications, 2022. 10.1038/s41467-022-33223-x  (About DOIs).

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New Pacific island rises after underwater volcanic blast | Volcanoes News

The tiny island came into existence 11 hours after a volcanic eruption and grew to 24,000-square metres in size.

A new island has emerged in the southwest Pacific Ocean after a Home Reef underwater volcano erupted  oozed lava and ejected ash and steam.

The island came into existence 11 hours after the eruption on September 10, which discoloured the surrounding water, the US-based space agency NASA said in a statement.

NASA was able to photograph the new land mass with satellites. The volcano is situated in the Home Reef seamount near the central Tonga island.

“The Operational Land Imager-2 (OLI-2) on Landsat 9 captured this natural-color view of the young island on September 14, 2022, as plumes of discolored water circulated nearby,” the statement said.

“Previous research suggests that these plumes of superheated, acidic seawater contain particulate matter, volcanic rock fragments, and sulfur.”

On September 14, Tonga Geological Services estimated the size of the island to be 4,000 square metres (43,055 square feet), with an elevation of 10.1 metres (33 feet) above sea level. However, by September 20 the agency said the island had grown substantially to 24,000 square metres (258,333 square feet).

The new island in the southwest Pacific Ocean [NASA Earth Observatory]

NASA said while islands created from underwater volcanos do not last long, some can go on to exist for years.

“The volcano poses low risks to the aviation community and the residents of Vava‘u and Ha‘apai… All mariners are, however, advised to sail beyond 4 kilometers (2.49 miles) away from Home Reef until further notice,” TGS noted.

Seismic activity is a common occurrence around Tonga, an archipelago nation with 171 islands and a population of 100,000.

Previously, Home Reef volcanos erupted in 1852, 1857, 1984 and 2006 – with the last two eruptions producing islands 50 to 70 metres (164-229 feet) high, NASA said.

The Home Reef, a seafloor ridge from Tonga to New Zealand, has the highest concentration of underwater volcanos in the world, according to the space agency.

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A New Island Has Arisen in The Pacific Following Underwater Eruption : ScienceAlert

A submerged volcano on the seamount known as the Home Reef in the central Tonga Islands has awoken after 16 years of deep sleep to poke its head out of the blue.

On 10 September 2022, lava and rock fragments began to ooze into the ocean 25 kilometers (15 miles) southwest of Late Island, while plumes of steam and ash burst through the surface of the waves.

Slowly the debris gathered into a whole new island, covering 4,000 square meters (one acre) and reaching a height of 10 meters (33 feet) within a few days.

Though it would barely grow much taller, on September 20 officials from the Tonga Geological Services (TGS) announced that the island had swelled six times in size, expanding to 24,000 square meters.

Like a phoenix rising from the ashes, this ephemeral, unnamed structure will probably sink back down into the Pacific Ocean’s burning ‘Ring of Fire’ long before any seafarer might hope to set foot on its rocky shore.

The last time Home Reef gave birth to a new island, in 2006, it took a year for the ocean’s waves to erode its crest. This time, the crest is much shorter.

So much debris was produced by the submerged Tonga volcano in the 2006 event, an expansive raft of the frothy volcanic glass known as pumice was set adrift across the South Pacific, giving the eery appearance of land.

You can see footage of that raft below:

frameborder=”0″ allow=”accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture” allowfullscreen>

Since 1852, Home Reef has produced islands on five occasions, some reaching between 50 and 70 meters in height. In 1984, the island even bore a small lagoon.

The seamount responsible for these short-lived structures sits in a region of the Pacific Ocean known as the Tonga-Kermadec subduction zone, which holds some of the fastest converging tectonic plates in the world.

Here, the Pacific Plate is rapidly slipping under two other plates (the Kermadec and Tonga) at a rate of about 24 centimeters a year (9 inches), forming the second deepest trench in the world and an extremely active volcanic arc.

In fact, this long stretch of seafloor ridge, which spreads from Tonga to New Zealand, is home to the highest density of underwater volcanos found anywhere on Earth.

Satellite images of the Home Reef’s recent eruption capture the formation of its newest island in stunning detail. The image below was released by NASA using US Geological Survey data on September 14.

It shows not only a long trail of smoke but an intense discoloration of the surrounding ocean.

A submerged volcano erupting to form Home Reef. (Lauren Dauphin/NASA Earth Observatory/USGS)

A follow-up image taken on September 18 using USGS data and shared by the TGS on Facebook zooms in on the volcanic fall-out, as can be seen below.

The eruption that formed Home Reef in September, 2022. (USGS)

The clouding of the water is probably a result of superheated acidic seawater, mixed with chunks of volcanic rock and debris, according to a recent press release from NASA.

“The volcano poses low risks to the aviation community and the residents of Vava’u and Ha’apai,” TGS announced on September 20.

“All mariners are, however, advised to sail beyond 4 kilometers away from Home Reef until further notice.”

Since September 25, there have been no more sightings of volcanic ash or steam from this slice of the Pacific. Home Reef is probably done for now, leaving us to appreciate its latest gift to the sea while we can.

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