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Deep beneath Washington State, something ancient is stirring. After thousands of years of silence, the region’s largest volcano is showing signs of life again — subtle tremors, rising heat, and shifts scientists can’t ignore. In this video, we’re diving into what’s waking it up, how experts detected the changes, and what could happen if the magma system continues to grow restless. For decades, this massive giant slept quietly under forests and snow. Now it’s whispering, and researchers are rushing to understand what comes next. If this awakening continues, the Pacific Northwest may be facing a chapter it hasn’t seen in millennia. Animation is created by Bright Side.
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00:00These ominous rumbling sounds, the ground shaking under your feet, wait a minute, that's my tummy!
00:07Or it might be Washington State's Mount Adams waking up!
00:11It's the largest volcano in the state by both area and volume,
00:15and it's recently started to show signs of life after staying silent for thousands of years.
00:21Scientists have noticed an alarming uptick in seismic activity around the mountain.
00:25And since the last eruption here happened between 3,800 and 7,600 years ago,
00:31humanity was still in the Stone Age at that time.
00:34This sudden chattiness has scientists, let's say, curious.
00:38The U.S. Geological Survey has hurriedly installed temporary seismic stations around Mount Adams
00:43to keep an eye on the situation.
00:46At the same time, they reassure the public there's no need to panic.
00:50Mount Adams doesn't reach the height of the better-known Mount Rainier.
00:54And still, it covers a massive area, making it Washington's largest active volcano.
01:00Interestingly, records show that before September of this year,
01:04Mount Adams had experienced an average of just one small earthquake every 2-3 years since 1982.
01:11And then, the Cascades Volcano Observatory and the Pacific Northwest Seismic Network
01:16detected a staggering 6 earthquakes in just one month, September.
01:20These quakes were all rather tiny, with magnitudes ranging between 0.9 and 2 on the Richter scale.
01:28It means they were so weak you wouldn't feel them at the surface.
01:31Plus, satellite imagery confirmed there was no ground deformation in the area.
01:37Now, at the moment, the USGS keeps Mount Adams' alert level at green or normal.
01:42So, we shouldn't worry about the ground opening and swallowing towns and cities.
01:47But the most recent seismic blips have encouraged the agency to install additional equipment
01:52for more precise monitoring.
01:54Such an expanded network will help scientists notice even the smallest earthquakes,
01:59which will help them understand what's happening under Mount Adams.
02:03This extra equipment might also shed light on whether this recent activity
02:07is a signal of future eruptions or just a random anomaly.
02:12If Mount Adams eventually erupted, it would likely produce slow-moving lava flows
02:17rather than explosive eruptions like Mount St. Helens.
02:21After all, past eruptions have only led to lava flows that travel just a few miles from the volcano.
02:27So, that's not what we'd need to worry about.
02:30A much more dangerous thing would be lahars.
02:32These are mud flows that can happen when volcanic ash, rock, and melted ice mix during eruptions.
02:38Lahars have occurred near Mount Adams without even eruptions.
02:42Rock, weakened by hydrothermal processes at the volcano's summit,
02:46suddenly broke loose, creating fast-moving, destructive mud flows.
02:51Exactly for this reason, the USGS categorizes Mount Adams as a high-threat volcano.
02:57While it doesn't erupt frequently, it still poses serious risks to nearby settlements.
03:04Another volcano we should carefully watch is Kattla in Iceland.
03:08It's one of the country's most powerful and dangerous volcanoes.
03:12It last erupted over a century ago in 1918.
03:15But if it erupts again, it could be 10 times as powerful as another Icelandic volcano,
03:22whose name I can't pronounce.
03:23See?
03:24That one erupted in 2010, completely disrupting air travel all over Europe.
03:30An eruption of Kattla could release large amounts of sulfur dioxide,
03:34which could form sulfate aerosols in the atmosphere.
03:37Such aerosols reflect sunlight, which could even cause temporary global cooling.
03:42This phenomenon often followed catastrophic volcanic eruptions in the past.
03:47Although eruptions are common in Iceland,
03:50Kattla's ash cloud would likely shoot higher into the sky
03:53and cover larger areas of Europe than that other one did.
03:57It would ground flights and negatively affect economies.
04:01If Kattla erupted, it would also harm agriculture, water supplies, and air quality.
04:07In 2014, scientists noted that a large eruption could even cause a tsunami
04:11that might travel along Iceland's south coast and out to sea.
04:15But the potential impact of such a tsunami is still unclear.
04:20Kattla tends to erupt on a regular schedule every 40 to 80 years,
04:24which means that another eruption is statistically very likely soon.
04:29That's why Kattla remains under close scientific observation.
04:32The Canary Islands' Cumbra Vieja erupted recently in 2021,
04:40reminding people of its destructive potential.
04:42The lava flow from this eruption was devastating.
04:46It covered whole neighborhoods and flowed into the ocean,
04:49destroying more than 3,000 homes.
04:52Thousands of people had to be evacuated.
04:54But the craziest thing?
04:56Even though the damage was significant,
04:58scientists believe it could have been far worse.
05:00A massive eruption of Cumbra Vieja could have caused the volcano's entire western flank
05:06to collapse into the Atlantic Ocean, triggering a mega-tsunami.
05:11This hypothetical tsunami could have potentially created waves
05:14hundreds or even thousands of feet high.
05:17They could have flooded coastlines around the Atlantic Basin,
05:20including parts of the U.S. and Europe.
05:23Luckily, recent studies claim that a collapse of that scale is unlikely.
05:27But even though the chance of a mega-tsunami is low,
05:31scientists still think it's wise to prepare for possible eruptions
05:35because there's a chance of extensive damage.
05:38The lava flows that occur at this volcano tend to be extensive and dangerous
05:42to both human life and the infrastructure on the island.
05:46If you decide to travel to Ecuador, you should be wary of Cotopaxi,
05:53one of the most active volcanoes in this country.
05:56It's been rumbling with minor eruptions since 2022.
06:00While these eruptions have been relatively small,
06:03Cotopaxi has a great potential for a major eruption.
06:06And it has scientists on high alert.
06:08If Cotopaxi erupted on a large scale,
06:12it could produce a massive ash cloud over 12 miles high,
06:16threatening the lives of around 200,000 people in the neighboring area.
06:20A serious danger is Cotopaxi's snow-capped summit.
06:24It would melt super rapidly in a major eruption.
06:28It could lead to destructive floods and landslides
06:30that would flow down the mountain and potentially reach populated areas.
06:34This combination of volcanic activity and glacial floods
06:38makes Cotopaxi a high-risk volcano.
06:42A powerful eruption could occur soon,
06:44or it could be years or even decades away.
06:47But monitoring efforts are in place to catch any warning signs.
06:53The next volcano we should watch out for is already infamous,
06:57Mount Vesuvius.
06:59Its catastrophic eruption in 79 CE
07:02destroyed the Roman cities of Pompeii and Herculaneum.
07:06Its last eruption occurred in 1944.
07:09But Vesuvius remains highly active
07:11and poses a great risk to nearby Naples,
07:15one of Italy's largest cities.
07:17A large eruption would threaten over 3 million people.
07:20Many of them live in the vicinity
07:22or even directly on the slopes of the volcano.
07:25If Vesuvius erupted,
07:26it would be an explosive event
07:28with ash, rocks, and volcanic gas
07:31ejected at extremely high speeds.
07:34And even though such a destructive event
07:36isn't expected for a few hundred years,
07:39Vesuvius remains one of the world's
07:41most closely watched volcanoes.
07:43After all,
07:44it has a real potential to cause catastrophic damage
07:47in a densely populated area.
07:51Then, we have Popocatépetl,
07:54often called El Popo.
07:55It's one of North America's tallest active volcanoes,
07:59which lies about 40 miles from Mexico City.
08:02Exactly this proximity to a metropolitan area
08:05with a population of 22 million people
08:08makes Popocatépetl especially hazardous.
08:11A large eruption could send a massive ash cloud
08:14over Mexico City,
08:15causing widespread disruptions.
08:17Ash could clog the city's drainage systems,
08:20contaminate water supplies,
08:21and even cause power outages
08:23by short-circuiting electrical systems.
08:26Plus, Lahars could rush down the volcano,
08:29reaching nearby towns.
08:31Popocatépetl has been showing
08:33near-constant seismic activity
08:35since the early 2000s,
08:37and smaller eruptions are pretty common here.
08:40In early 2024,
08:41there were 13 recorded minor eruptions,
08:44which alarmed nearby towns.
08:46At the same time,
08:47volcanologists consider such eruptions
08:49normal for Popocatépetl.
08:53While talking about super-dangerous volcanoes,
08:56we can't skip Yellowstone National Park.
08:59It houses one of the world's largest super-volcanoes.
09:03Its last massive eruption
09:04occurred about 640,000 years ago.
09:07But if this monster were to erupt today,
09:10the impact would be much more devastating
09:12for the entire planet.
09:14States closest to Yellowstone,
09:16including Montana, Idaho, and Wyoming,
09:19would be most affected,
09:20likely experiencing disastrous pyroclastic flows.
09:24These flows,
09:25which are made of a dangerous mix
09:27of lava, ash, and gases,
09:29can obliterate everything in their path.
09:32Large parts of the country
09:33would also be blanketed in volcanic ash,
09:36over 3 feet in some areas.
09:38On a global scale,
09:39an eruption at Yellowstone
09:41would send tons of ash and gases
09:43into the stratosphere,
09:45potentially blocking sunlight
09:46and causing global temperatures
09:48to drop for a few years.
09:50This would disrupt agriculture,
09:52collapse transportation systems,
09:54and create food shortages
09:55on a massive scale.
09:57Still, even though there's a popular myth
09:59that Yellowstone is overdue for an eruption,
10:03geologists clarify that this isn't true.
10:06Volcanoes don't follow precise timetables,
10:08and the activity at Yellowstone
10:10doesn't indicate an imminent eruption.
10:13So, yeah, that's good news.
10:18Wow! Earth's surface is shaking.
10:20Long cracks split the ground open.
10:22Lava rivers are rapidly flowing down the slopes.
10:26Deafening noise is filling the air.
10:28Rocks and other debris are flying high up.
10:30Clouds of volcanic gas and ash cover the sky.
10:34Now, this is not a plot
10:35of a blockbuster disaster movie.
10:37It's what happens when supervolcanoes decide to erupt.
10:41But this is likely not the scenario
10:43that will take place
10:44when the world's largest volcano,
10:46Mauna Loa,
10:47decides to finish its long, long nap.
10:50In 2021,
10:51scientists were sure it would happen soon.
10:54But, so far, nothing.
10:56The volcano's seismicity keeps increasing
10:58and then going back to normal.
11:00But you never know
11:02when this giant will finally come back to life.
11:04That's why experts have been monitoring
11:06geological activity
11:08on Hawaii's largest island
11:10for quite some time.
11:11The Big Island of Hawaii
11:13is made up of five volcanoes,
11:15including the most active on the planet,
11:17Kilauea,
11:18and the largest,
11:19Mauna Loa.
11:20This gigantic thing
11:22makes up almost half the landmass
11:23of the island.
11:24And what Lava Kilauea
11:26emits in one day,
11:28Mauna Loa could spew out
11:29within 20 minutes.
11:31That's what it did in 1984.
11:33While Mauna Loa's smaller sibling
11:35has been throwing tantrums for a while,
11:38the giant has been slumbering
11:40ever since its last eruption.
11:42But very recently,
11:43the Hawaii Volcano Observatory
11:45has recorded more than 200 mini-earthquakes
11:48below Mauna Loa.
11:49It likely means
11:50an increased flow of magma down there.
11:53Good morning!
11:54The volcano might be waking up.
11:56Or not.
11:57If Mauna Loa did suddenly erupt,
12:00lava flows could reach the ocean
12:02and the most populated
12:03and touristy places,
12:05like Captain Cook,
12:06very, very quickly,
12:07in a matter of hours.
12:08In 1984,
12:10the last time
12:11the volcano erupted,
12:12lava got as far
12:13as the outskirts of Hilo
12:15on the other side of the island.
12:17That's where a campus
12:18of the University of Hawaii
12:19is found.
12:20Luckily,
12:20people had a few weeks' warning
12:22to get ready for the disaster.
12:24These days,
12:25locals have special go-bags
12:27ready with the most important stuff,
12:29including documents and money.
12:31Such precautions
12:32can come in handy
12:33in case of an emergency evacuation.
12:36Even though most Mauna Loa eruptions
12:38have so far
12:39only affected the summit area,
12:41several of them
12:41sent lava
12:42all the way down to the ocean.
12:44And you never know
12:45how powerful
12:46the next eruption will be.
12:48Now,
12:49what is the highest mountain on Earth?
12:50Mount Everest, you say?
12:52Well, it depends.
12:54From seafloor to the summit,
12:55Mauna Loa
12:56is a thousand feet taller
12:58than the famous Himalayan peak.
13:00The volcano is so big,
13:01it makes the Pacific plate
13:03it's sitting on
13:04literally slump
13:05under its wake.
13:06Scientists say
13:07that when this monster
13:08of a volcano erupts,
13:10the volume of lava
13:11coming out per unit
13:12will be life-threatening.
13:14Over its recorded history,
13:16Mauna Loa
13:16has been erupting regularly,
13:18almost every six years.
13:20And even though
13:20the last eruption
13:21of the volcano
13:22occurred about 40 years ago,
13:25scientists are certain
13:25it'll happen again.
13:28Now,
13:28remember the scene
13:29I showed you
13:30at the beginning?
13:31Well,
13:31you can relax.
13:32It's not likely
13:33to happen with Mauna Loa.
13:35The thing is,
13:36big island volcanoes,
13:37including Mauna Loa,
13:39aren't very volatile.
13:40That's because
13:41they're shield volcanoes.
13:43These volcanoes
13:43got such a name
13:44because they aren't
13:45really very high
13:46and resemble
13:47a warrior's shield
13:48placed flat on the ground.
13:50Shield volcanoes
13:51get formed
13:52by very fluid lava.
13:54It travels farther
13:55and forms much thinner flows.
13:57Then lava erupted
13:58from a stratovolcano,
13:59which is conically shaped
14:01and tall,
14:02like the infamous
14:03Krakatoa in Indonesia.
14:05So if,
14:06or should I say when,
14:07Mauna Loa erupts,
14:08there probably won't be
14:10ash clouds
14:10and tons of debris.
14:12The most dangerous thing
14:13will be lava.
14:14Since Mauna Loa
14:15is a shield volcano,
14:17its lava is extremely
14:18fluid and voluminous,
14:20which allows it
14:20to flow far and fast.
14:23Using theoretical
14:24vent maps,
14:25experts from
14:26the Hawaii Volcano Observatory
14:28have made charts
14:29of possible lava flows.
14:31They're kind of worried
14:32about earthquakes
14:33clustering at high rates.
14:35It likely means
14:36that lava is on the move
14:37under the surface.
14:39500 to 600 earthquakes
14:41per day
14:41are a serious reason
14:43to be on high alert.
14:44On the other hand,
14:46it doesn't necessarily
14:47mean a disaster
14:48or inevitable eruption.
14:50Around a decade ago,
14:52several earthquakes
14:53that happened
14:53at the same time
14:54signaled that something
14:55was happening
14:56under Mauna Loa.
14:58But an eruption
14:59didn't occur.
15:00Instead,
15:01half the volcano
15:02shifted a bit
15:02to the south.
15:04This way,
15:04it probably gave
15:05more room to magma
15:06so that it had
15:07enough space
15:08to stay beneath
15:09the surface.
15:10Now,
15:11let's get back
15:11to the catastrophic
15:12eruption we saw
15:13at the beginning
15:14of the video.
15:15That's what often
15:15happens when
15:16a supervolcano erupts.
15:18Those are volcanoes
15:19that have at least
15:20once had an eruption
15:21with a volcanic
15:22explosivity index
15:24of 8,
15:25which is the largest
15:25recorded number
15:26on the index.
15:28Supervolcanoes
15:29are often extremely large
15:30with no cone at all.
15:32That's because
15:33they're typically
15:33the remains
15:34of gigantic magma
15:35chambers
15:36that once flared up,
15:37leaving behind
15:38a caldera.
15:39They're usually found
15:40over hot spots.
15:42Supervolcanoes
15:43can produce
15:43supereruptions,
15:45and when they do,
15:46they blow
15:46more than 240 cubic miles
15:49of ash,
15:50molten rock,
15:50and hot gases
15:51up into the air.
15:53In other words,
15:54four supereruptions
15:55could fill
15:56the Grand Canyon
15:57to the brim.
15:58Supervolcanoes
15:59get formed
16:00when gigantic volumes
16:01of scorching hot magma
16:02are trying to escape
16:04from deep underground.
16:05This magma
16:06rises close
16:07to the surface,
16:08but can't break
16:08through Earth's crust.
16:10That's why
16:10a huge pressurized
16:12pool of bubbling magma
16:13gathers at a depth
16:15of only several miles.
16:17The pressure
16:17keeps growing
16:18because more magma
16:19is trying to get
16:20to the surface
16:20until, bam,
16:22a supereruption occurs.
16:24The most recent
16:26supereruption
16:26happened in New Zealand.
16:28Well,
16:28when I say recent,
16:30I mean around
16:3026,500 years ago.
16:33Nah,
16:33I wasn't around then.
16:35That's when
16:35a supervolcano
16:36beneath the surface
16:37of Lake Taubo
16:38spewed into the air
16:39more than 300 cubic miles
16:41of ash and pumice.
16:43Imagine 500,000
16:45great pyramids
16:46of Giza
16:46flying up
16:47at the same time.
16:49That's how incredibly
16:50powerful that eruption was.
16:52But the most exciting
16:53and confusing thing
16:54about the eruption
16:55was that the Taubo volcano
16:57simply didn't go off
16:59like many others.
17:00At first,
17:01everything was going
17:02as usual.
17:03More than 200 square miles
17:04of magma
17:05had built up
17:06under the surface
17:06and the pressure
17:07was getting higher
17:08and higher.
17:09But after the rock
17:10cracked
17:11and the first part
17:12of lava
17:12rushed out of the crater,
17:14something went wrong
17:15and the supervolcano
17:16took a break.
17:18Only several months later,
17:19the disastrous eruption
17:21shook the ground
17:22and thousands of tons
17:23of lava,
17:24rocks,
17:25and ash
17:25flew high
17:26into the atmosphere.
17:27But the age
17:28of supervolcanoes
17:30isn't over.
17:31The most infamous
17:31of them all
17:32is probably the one
17:34in Yellowstone National Park.
17:36This giant
17:37handles at least
17:37three mega-powerful eruptions,
17:40and who knows
17:41how many smaller ones.
17:42If this monster
17:43erupted anywhere
17:44as strongly
17:45as it did
17:452.1 million years ago,
17:47it would spit out
17:48more than 588 cubic miles
17:51of red-hot material.
17:53You can probably
17:53picture it more vividly
17:55if I tell you
17:55that this volume
17:56is comparable
17:57to 65 million
17:59capital rotundas
18:00in Washington, D.C.
18:02piled together.
18:03Wow.
18:04Anyway,
18:05scientists are sure
18:05that Yellowstone
18:06doesn't present
18:07any danger these days.
18:09For an eruption
18:10to happen,
18:11magma inside
18:12must be at least
18:1250% molten.
18:14With the Yellowstone caldera,
18:16this number
18:16is just 5-15%.
18:18But of course,
18:20Yellowstone
18:20isn't the only
18:21supervolcano
18:22on our planet.
18:23There's also
18:24New Zealand's
18:25Taubo
18:25you already know about,
18:26Japan's
18:27Eri Cauldre,
18:28California's
18:29Long Valley,
18:30Indonesia's Toba,
18:31any of them
18:32can one day
18:33produce a supereruption.
18:35There are also
18:36several so-called
18:37supervolcanoes
18:38that haven't lived up
18:40to this name yet
18:41because they've never
18:42produced anything
18:43like a supereruption.
18:44For example,
18:45in 1883,
18:47Indonesian volcano
18:48Krakatoa
18:49went off.
18:50The power of the eruption
18:51tore the volcano's
18:52walls open.
18:53And cold seawater
18:55rushed into
18:56its molten insides.
18:57The difference
18:58in temperature
18:58made the volcano
18:59blow up
19:00with a deafening boom.
19:02It was clearly heard
19:032,000 miles away
19:04in Australia.
19:06It earned the blast
19:07the title
19:07of the loudest sound
19:09in history.
19:10But even though
19:11the consequences
19:11of this event
19:12were truly catastrophic,
19:14it still turned out
19:15not powerful enough
19:16to be called
19:17a supereruption.
19:18That's it for today.
19:20So hey,
19:21if you pacified
19:22your curiosity,
19:23then give the video
19:23a like
19:24and share it
19:24with your friends.
19:25Or if you want more,
19:26just click on these videos
19:28and stay on the bright side.
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