WEBVTT - How Supervolcanoes Work

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<v Speaker 1>Welcome to Stuff you Should Know from how Stuff Works

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<v Speaker 1>dot Com. Hey, and welcome to the podcast. I'm Josh Clark,

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<v Speaker 1>and there's Charles W. Chuck Bryant, and there's Jerry So

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<v Speaker 1>Stuff you Should Know. Super Bowl, okay, supervolcano? Was that?

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<v Speaker 1>What was that? Do you know what that was? Oh? Geez,

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<v Speaker 1>you and that song. I can't help it. For nine

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<v Speaker 1>years you've been Holman the Final Countdown by Europe. Not

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<v Speaker 1>every oh, I don't know, every three months or so,

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<v Speaker 1>it's the world years. It's the world's most effective earworm.

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<v Speaker 1>Do you do that to you? Me? With the final Countdown?

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<v Speaker 1>She's like, it doesn't get to her. It bounces right off.

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<v Speaker 1>She's like, try your worst. Um, super volcanoes. If you

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<v Speaker 1>listen to volcanoes, well we did that one, yeah, or

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<v Speaker 1>our Yellowstone or I guess it was Geyser's Nature's Innuendo.

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<v Speaker 1>That was a great title. Um. Then some of this

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<v Speaker 1>might seem a little bit familiar, but why not to

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<v Speaker 1>cover it as its own thing? Well, it is its

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<v Speaker 1>own thing. They're starting to figure out. Yeah, Like this

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<v Speaker 1>article even says don't even think of it as a

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<v Speaker 1>amped up volcano. It says stop stop. They should call

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<v Speaker 1>it something else, then they really should. I mean that

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<v Speaker 1>you can make a case that, yes, it's calling it

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<v Speaker 1>a super volcano. It does make sense in a way, um,

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<v Speaker 1>because it is obviously magma pushing up through the earth. Uh.

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<v Speaker 1>But that's pretty much where the comparisons end, and that

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<v Speaker 1>that's that's a pretty deep comparison between a volcano and

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<v Speaker 1>a super volcano. But there's a lot of different stuff

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<v Speaker 1>going on. And the more we look into these things that, frankly,

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<v Speaker 1>the scarier they become. Yeah, I mean, right out of

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<v Speaker 1>the gate. One of the big things that is different

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<v Speaker 1>from a volcano is a volcano is usually like a

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<v Speaker 1>mountain that you can look at with smoke coming out

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<v Speaker 1>of it and point to you can keep an eye

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<v Speaker 1>on it. In other words, yeah, and whereas a super

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<v Speaker 1>volcano is usually categorized by a big depression in the

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<v Speaker 1>earth from a past explosion, like a crater or something. Yeah,

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<v Speaker 1>or it might be like nothing, that crater might be

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<v Speaker 1>fully filled in by this point, might be a forest,

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<v Speaker 1>It could be Um, it could be a hot spot

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<v Speaker 1>like a yellow Stone as we'll see, where there are

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<v Speaker 1>is a lot of geysers and hot springs. But the

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<v Speaker 1>point is is it's a A super volcano is a

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<v Speaker 1>massive amount of magma, a chamber, a magma chamber, possibly

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<v Speaker 1>a magma reservoir feeding the magma chamber, something even bigger

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<v Speaker 1>um and it's it's connected or near a thin spot

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<v Speaker 1>in the mantle that it may or may not have

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<v Speaker 1>created itself in the Earth's sor this and that. Eventually

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<v Speaker 1>something's going like the pressure inside is going to build up,

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<v Speaker 1>there's gonna be enough magma and then kaboom. Things are

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<v Speaker 1>gonna go south pretty quick. Because these things are so

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<v Speaker 1>big and so explosive that they could they can change

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<v Speaker 1>the global climate, possibly irreversibly on a human time scale. Yeah,

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<v Speaker 1>whenever I read about stuff like this or even your

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<v Speaker 1>garden variety natural disaster, it just feels like the Earth

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<v Speaker 1>is like, you know, one day, I'm going to kill

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<v Speaker 1>all the people. You realize this slowly, like all humans

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<v Speaker 1>will be gone. I want to just explode you all. Yeah,

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<v Speaker 1>that's so gaya guy. A hypothesis is it kind of

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<v Speaker 1>all right? But it's not gonna be anytime soon. In

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<v Speaker 1>the case of a super volcano, Well, we hope, I saw,

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<v Speaker 1>I saw. It's been calculated that they go off every

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<v Speaker 1>Oh no, a hundred thousand or so years. The most

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<v Speaker 1>recent one was something like um four thousand, twenty six

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<v Speaker 1>thousand years ago. It's not too bad. Yeah, and we

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<v Speaker 1>got a little time from New Zealand. Yeah, so we

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<v Speaker 1>should say this is spelled t a u p o.

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<v Speaker 1>Here in the States, we would typically pronounce that like

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<v Speaker 1>taupo maybe, but based on our Maori episode, I would

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<v Speaker 1>guess that it's actually pronounced Could you repeat that again?

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<v Speaker 1>So let's talk about how big these things can be. Uh,

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<v Speaker 1>Sumatra seventy four thousand years ago. That was a super

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<v Speaker 1>eruption that some say, and of course we don't know

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<v Speaker 1>because it was seventy four thousand years ago. That's all

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<v Speaker 1>we can do is kind of make our best guess.

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<v Speaker 1>But some people think that that this almost was an

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<v Speaker 1>extinction level event in full. It all most wiped out

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<v Speaker 1>the entire human race. It could have jumped started a

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<v Speaker 1>ten thousand year ice age, leaving behind a crater or

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<v Speaker 1>a CAULDERA that was about nineteen by sixty two miles.

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<v Speaker 1>That is huge. That's a yeah, that was Mount Toba,

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<v Speaker 1>the Toba super eruption, right, Yes, six seventy cubic miles

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<v Speaker 1>yea of ejecta. Yeah, and that ten thousand year ice

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<v Speaker 1>age thing, that's noteworthy. They think that this whole thing

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<v Speaker 1>was bad enough that it reduced humans down to several

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<v Speaker 1>thousand people, and that there were plenty more humans before then,

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<v Speaker 1>but that the the effects from shooting um gases the ejecta,

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<v Speaker 1>but gases that flowed up into the atmosphere and actually

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<v Speaker 1>reflect sunlight cooling the earth below it. UM really disrupted

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<v Speaker 1>a lot of normal processes here on Earth, cooled it

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<v Speaker 1>and made it really tough to survive. Five. That's the

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<v Speaker 1>hallmark of super volcanoes. Is there their global effect? Yeah,

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<v Speaker 1>like a nuclear winter, basically changing the temperature of the Earth,

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<v Speaker 1>maybe not permanently, but long enough to where your s

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<v Speaker 1>O l right ten thousand year. I said, you're you're

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<v Speaker 1>not gonna be happy during those years. Uh, these days, UM,

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<v Speaker 1>North America, South American Asia are the greatest risks and

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<v Speaker 1>there's one. Um. Actually it says we're those three places

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<v Speaker 1>of the greatest risk. But there's one in Europe in Italy. Yeah,

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<v Speaker 1>that supposedly, and this was from Geez. Just like four

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<v Speaker 1>months ago, I read an article that said that the

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<v Speaker 1>one in Italy, it's in Naples, what's it called the

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<v Speaker 1>Compy Flagray or, as we say in the United States,

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<v Speaker 1>the Flagrian Fields area, the burning Fields. Yeah, that that

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<v Speaker 1>should give you an indication of what we're talking about.

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<v Speaker 1>Didn't get that name for nothing, No, but it's right

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<v Speaker 1>beneath Naples. Yeah. But apparently that one is based on

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<v Speaker 1>computer modeling and physical measurements. Uh. One of the scientists said,

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<v Speaker 1>we proposed that magma could be approaching the critical degassing

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<v Speaker 1>pressure level at Camp Flegria. Uh. And basically what that

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<v Speaker 1>means is it's not gonna happen like next year, but

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<v Speaker 1>they have raised the volcano threat level from green to yellow,

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<v Speaker 1>which means we need to kind of really start monitoring

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<v Speaker 1>and study. Is studying this thing a lot more. The

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<v Speaker 1>thing is that they don't know like how to predict

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<v Speaker 1>like it could happen next year. They're saying it's probably

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<v Speaker 1>not going to but it could because we know so

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<v Speaker 1>little about volcanoes and supervolcanoes in particular, that like it

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<v Speaker 1>could just happen. Yeah, Like we don't even know for

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<v Speaker 1>sure how many there are underneath us, but they say

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<v Speaker 1>like six to ten maybe potentially active ones around the

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<v Speaker 1>globe right now, and then a total of maybe thirty

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<v Speaker 1>to forty that have ever been right. Um, but yeah,

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<v Speaker 1>that one. I don't understand why this article overlooked that

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<v Speaker 1>one Europe, but it's it's like Europe's toast, basically, it's inevitable.

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<v Speaker 1>Probably the next month or two, there was one I

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<v Speaker 1>think the biggest ever UM happened here in the States

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<v Speaker 1>in Colorado, long before anybody called it Colorado. It was

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<v Speaker 1>twenty million years ago, and the Fish Canyon Tough Event.

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<v Speaker 1>So here's where super volcanoes really kind of come into

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<v Speaker 1>um their own, just the massive amount of damage and

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<v Speaker 1>stuff they spew out. Right, the Fish Canyon Tough event

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<v Speaker 1>shot out twelve d cubic miles. So you know what

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<v Speaker 1>a cube is, right, It's like a three dimensional square.

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<v Speaker 1>And by Mr Rubick, you can write exactly you can

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<v Speaker 1>take a little like an inch by an inch by

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<v Speaker 1>an inch and create a little cubic kitch. You can

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<v Speaker 1>do that with feet, you can do that with a meter,

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<v Speaker 1>and you just keep going bigger and bigger and bigger,

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<v Speaker 1>and eventually you're going to get to a cubic mile

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<v Speaker 1>or a cubic kilometer. And this Fish Canyon Tough event

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<v Speaker 1>spewed out twelve hundred cubic miles or five thousand cubic

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<v Speaker 1>kilometers of rock, of dust, of ash, of molten lava

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<v Speaker 1>shot it out and that nuts. That's so much stuff

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<v Speaker 1>that literally changes the geography of an entire region when

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<v Speaker 1>something like that happens, that's crazy. Um all right, I'm

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<v Speaker 1>gonna contemplate the Cube and uh, we'll be back right

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<v Speaker 1>after this to talk a little bit more about Yellowstone.

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<v Speaker 1>Did you ever watch Jim Henson's The Cube? Remember when

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<v Speaker 1>we talked about did you ever watch it? Bizarre? Yes,

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<v Speaker 1>very weird. We love our friends with the handsome company. Um,

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<v Speaker 1>all right, well we're gonna talk about Yellowstone a little bit.

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<v Speaker 1>But defining these and when we talked about volcanoes, Defining

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<v Speaker 1>volcanoes and what makes a volcano or super volcano is

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<v Speaker 1>not an exact science. They don't have strict definitions, but um,

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<v Speaker 1>they do try to look at a couple of different

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<v Speaker 1>things when they're categorizing these these bad Mama jamas um

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<v Speaker 1>Magne said, did I just say that magnitude which is

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<v Speaker 1>the volume of the magma or the mass of magma

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<v Speaker 1>that's erupted, and then intensity, which is the rate that

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<v Speaker 1>that happens. Um, so if you're looking at magnitude intensity um,

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<v Speaker 1>Like I said, they don't have it like a number.

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<v Speaker 1>They say once it gets over this number. But um,

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<v Speaker 1>so I wonder how they do categorize it. They don't.

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<v Speaker 1>It's just up in the air, like they just do

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<v Speaker 1>not have it set out so that you can say, well,

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<v Speaker 1>once it hits this and this, it's it's officially a

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<v Speaker 1>super volcano. That's just not laid out like that. As

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<v Speaker 1>bad as writers of articles want it to be like that,

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<v Speaker 1>it's just not at that point. There's just but there

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<v Speaker 1>are factors where it's like, yeah, I would qualify that

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<v Speaker 1>as a supervolcano. I'm Joe volcanologist or Jane volcanologists or

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<v Speaker 1>versus a volcano um. And they usually do it by comparison, right,

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<v Speaker 1>So like as far as intensity goes, that's how fast

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<v Speaker 1>magma erupts. Right. Yeah. And Mount Vesuvius back in seventy nine,

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<v Speaker 1>see with that very famous eruption that covers Pompeii and Herculaneum. Um.

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<v Speaker 1>If you believe that kind of thing, right, I've seen

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<v Speaker 1>it with my own eyes. Yeah, Um, Mountain Vesuvius shot

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<v Speaker 1>out magma uh and ojecta at a rate of a

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<v Speaker 1>hundred thousand cubic meters a second. Wow, that's a lot, right,

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<v Speaker 1>that's some fast magma. So super volcanoes erupted it's something

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<v Speaker 1>like tens of millions or hundreds of millions of cubic

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<v Speaker 1>meters per second. That's a lot too. Yeah, you don't

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<v Speaker 1>want to be standing on that road. No, you don't

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<v Speaker 1>want to be anywhere near it. So that's typically how

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<v Speaker 1>they're figuring out what constitutes a super volcano. They look

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<v Speaker 1>at this volcano and they say that's bad, and then

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<v Speaker 1>they go, but what about this, and they go, that's

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<v Speaker 1>a super volcano. There is another categorization they use, which

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<v Speaker 1>is also a great band name, Volcano explosivity index. Yeah.

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<v Speaker 1>See the index just kind of throws it off, you know, yeah,

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<v Speaker 1>maybe an album title, okay, ejecta not bad, not bad

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<v Speaker 1>at all. So this is when they measure ash column

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<v Speaker 1>height and the quantity of that ash promise and lava ejected.

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<v Speaker 1>So not the volume, but how high it goes. I

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<v Speaker 1>don't know why they just can't combine all that into

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<v Speaker 1>one big formula Claven scale, but supervolcanoes there, it is

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<v Speaker 1>a scale, and the highest of the EI category is

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<v Speaker 1>a magnitude eight, which means more than two fifty cubic

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<v Speaker 1>miles and a plume more than sixteen miles high. Sixteen miles, dude,

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<v Speaker 1>that's amazing. It is it's super It is um. So

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<v Speaker 1>you kind of put all this stuff together. They don't

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<v Speaker 1>have it in a single index, but if you combine

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<v Speaker 1>all the stuff, you start to get an idea of

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<v Speaker 1>just how much damage a supervolcano can do. Just how

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<v Speaker 1>massive in huge it is so um And again going

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<v Speaker 1>back to comparisons, Krakatoa was a very famous volcano that

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<v Speaker 1>erupted in eight three, and it created what's regarded as

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<v Speaker 1>the loudest sound ever recorded here on Earth. It traveled

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<v Speaker 1>around the world four times over five days. And we

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<v Speaker 1>know that it did because by three there were um

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<v Speaker 1>weather stations that had barometers all over the world and

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<v Speaker 1>they would record the shock wave from the sound every

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<v Speaker 1>thirty four hours like clockwork. For five days. It just

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<v Speaker 1>kept traveling around the world from this explosion, this volcanic explosion.

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<v Speaker 1>It was heard by human ears three thousand miles away.

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<v Speaker 1>It was one of the most as sounding events that's

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<v Speaker 1>ever happened in recorded history. And there's a really cool

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<v Speaker 1>article just about the sound it made, called the sound

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<v Speaker 1>so loud that it circled the Earth four times on Nautilus.

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<v Speaker 1>So go check it out. I think everybody should read

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<v Speaker 1>this article. It's really cool article. And didn't it killed

0:15:04.400 --> 0:15:06.960
<v Speaker 1>like thirty six thousand people? Yeah, and it just and

0:15:07.000 --> 0:15:10.640
<v Speaker 1>that wasn't a very populated area. No, huh, No, Krakato

0:15:10.720 --> 0:15:16.280
<v Speaker 1>was um in uh Java, Indonesia. Yeah, I guess Krakato

0:15:16.360 --> 0:15:20.320
<v Speaker 1>in the eighties was probably not you know, New York City. No, No,

0:15:20.480 --> 0:15:23.040
<v Speaker 1>it wasn't. So yeah, the idea that it killed thirty

0:15:23.040 --> 0:15:26.160
<v Speaker 1>six thousand people, Yeah, it wasn't a densely populated area

0:15:26.240 --> 0:15:28.280
<v Speaker 1>right around the mountain. It killed a lot of people

0:15:28.320 --> 0:15:31.680
<v Speaker 1>spread out like Naples. Yeah, they're talking about I think

0:15:31.720 --> 0:15:35.239
<v Speaker 1>like five thousand people live in just that immediate area.

0:15:35.320 --> 0:15:38.040
<v Speaker 1>It would be just devastating. That would not be good man.

0:15:38.920 --> 0:15:42.600
<v Speaker 1>Um Alright, So we talked about it's it's kind of

0:15:42.600 --> 0:15:47.080
<v Speaker 1>tough two predicting these things, kind of tough to pin

0:15:47.160 --> 0:15:50.000
<v Speaker 1>down where they are and to study them. And Yellowstone,

0:15:50.000 --> 0:15:58.800
<v Speaker 1>which we've kind of danced around a little bit, not literally, Uh,

0:15:59.080 --> 0:16:02.880
<v Speaker 1>Yellowstone and particular is a big deal because um of

0:16:03.040 --> 0:16:07.400
<v Speaker 1>just how big this thing could be Uh, they're talking

0:16:07.960 --> 0:16:15.120
<v Speaker 1>thirty by forty five miles underground, stretching from northern Nevada

0:16:15.480 --> 0:16:19.280
<v Speaker 1>through southern Idaho to northwest Wyoming. Um, it's basically a

0:16:19.360 --> 0:16:23.760
<v Speaker 1>system three fifty miles long and about eighteen million years old.

0:16:24.200 --> 0:16:28.920
<v Speaker 1>That's just man, it's just bubbling underground. That's the trail

0:16:29.360 --> 0:16:34.760
<v Speaker 1>of volcanic activity that's taken place, which ends at Yellowstone, right.

0:16:34.800 --> 0:16:38.600
<v Speaker 1>And the one that's actually the supervolcano beneath Yellowstone is

0:16:38.640 --> 0:16:42.040
<v Speaker 1>like thirty miles by forty five miles, which is huge.

0:16:42.080 --> 0:16:44.560
<v Speaker 1>The one in in Europe at the Burning Fields is

0:16:44.560 --> 0:16:48.600
<v Speaker 1>about seven seven miles wide, which is enormous in and

0:16:48.640 --> 0:16:51.960
<v Speaker 1>of itself, but you know, thirty to forty five that's

0:16:52.040 --> 0:16:55.280
<v Speaker 1>way bigger. I'm afraid to stay. Um. And it's made

0:16:55.360 --> 0:17:00.520
<v Speaker 1>up of a magma chamber beneath the surface, few miles

0:17:00.520 --> 0:17:02.960
<v Speaker 1>beneath the surface. And they thought that that was the

0:17:03.000 --> 0:17:06.159
<v Speaker 1>extent of super volcano. Apparently they did a survey in

0:17:06.240 --> 0:17:09.360
<v Speaker 1>two thousand and fifteen they figured out that this chamber

0:17:09.400 --> 0:17:15.560
<v Speaker 1>has about cubic miles worth of magma in it. There's

0:17:15.600 --> 0:17:20.199
<v Speaker 1>also a reservoir beneath that magma chamber, and that that

0:17:20.320 --> 0:17:24.080
<v Speaker 1>reservoir has eleven thousand, two hundred cubic miles all this

0:17:24.200 --> 0:17:28.480
<v Speaker 1>magma poised right beneath yellow Stone, and the pressure is

0:17:28.560 --> 0:17:31.760
<v Speaker 1>just building and building and building. And that's the other

0:17:31.800 --> 0:17:35.120
<v Speaker 1>thing about super volcanoes. They seem to erupt, not slowly

0:17:35.200 --> 0:17:38.760
<v Speaker 1>where lava just spills out like and say like Hawaii

0:17:38.800 --> 0:17:42.560
<v Speaker 1>at Kilauea, where it's very famously just this pretty steady flow.

0:17:42.640 --> 0:17:46.800
<v Speaker 1>But it's not explosive. These things blow up, and when

0:17:46.840 --> 0:17:50.640
<v Speaker 1>they do, they can bury areas around them in hundreds

0:17:50.640 --> 0:17:55.119
<v Speaker 1>and hundreds of meters of of ash that solidifies and

0:17:55.160 --> 0:17:57.920
<v Speaker 1>turns into the new crust of the earth, that turns

0:17:57.960 --> 0:18:01.199
<v Speaker 1>us all into statues. It does. So that was my

0:18:01.240 --> 0:18:03.680
<v Speaker 1>own eyes too. All right, well, let's take our final

0:18:03.720 --> 0:18:06.239
<v Speaker 1>break and we'll talk a little bit more about what

0:18:06.320 --> 0:18:34.160
<v Speaker 1>lies beneath Yellowstone Park right after this. Alright, So Yellowstone

0:18:34.160 --> 0:18:37.760
<v Speaker 1>has had um, I mean, it's had events in the past.

0:18:37.880 --> 0:18:39.320
<v Speaker 1>That's why they know there's going to be one in

0:18:39.320 --> 0:18:42.840
<v Speaker 1>the future. About two point one million years ago, the

0:18:42.960 --> 0:18:47.600
<v Speaker 1>Huckleberry Ridge event um name, I don't think they called

0:18:47.600 --> 0:18:50.800
<v Speaker 1>it that two point one million years ago, but that

0:18:51.680 --> 0:18:56.600
<v Speaker 1>I had a five cubic mile blast and it created

0:18:56.640 --> 0:19:02.320
<v Speaker 1>a crater about the size of four um Manhattan's and

0:19:02.400 --> 0:19:06.199
<v Speaker 1>I assume they mean everybody knows exactly what manhattans. Sure,

0:19:06.320 --> 0:19:09.680
<v Speaker 1>just put four New York City's side by side on

0:19:09.720 --> 0:19:11.960
<v Speaker 1>top of each other. However you want to arrange them, Yeah,

0:19:12.080 --> 0:19:14.679
<v Speaker 1>maybe in a little spin spinning pin wheel, mush them

0:19:14.720 --> 0:19:21.760
<v Speaker 1>together in a ball like use soap bars remnants, you know. Yeah. Uh,

0:19:21.960 --> 0:19:24.000
<v Speaker 1>one point three million years ago they had one at

0:19:24.000 --> 0:19:28.000
<v Speaker 1>Masa Falls and that was only about sixty seven cubic

0:19:28.040 --> 0:19:31.439
<v Speaker 1>miles of ejecta. That was tiny, but they still consider

0:19:31.440 --> 0:19:33.400
<v Speaker 1>that a super volcano because no one seems to care

0:19:33.600 --> 0:19:37.760
<v Speaker 1>that it has no definition. Right. What else? Uh, six

0:19:37.880 --> 0:19:40.680
<v Speaker 1>hundred forty thousand years ago at Lava Creek, that one

0:19:40.760 --> 0:19:43.480
<v Speaker 1>spit out two hundred and forty cubic miles about a

0:19:43.520 --> 0:19:48.600
<v Speaker 1>thousand cubic kilometers and apparently it's ash pillar hit a

0:19:48.680 --> 0:19:53.160
<v Speaker 1>hundred thousand feet. That's pretty awesome, right, Yeah. So yeah,

0:19:53.160 --> 0:19:56.200
<v Speaker 1>they're looking at these things and they're saying, um, this

0:19:56.280 --> 0:19:58.920
<v Speaker 1>is probably a pretty decent map of what's going to

0:19:59.040 --> 0:20:02.160
<v Speaker 1>happen at Yellows Owned eventually. Yeah. We have an article

0:20:02.160 --> 0:20:04.560
<v Speaker 1>on our site too called what if the Yellowstone supervolcano

0:20:04.560 --> 0:20:07.960
<v Speaker 1>were erupted, and they said it could kill as many

0:20:07.960 --> 0:20:11.960
<v Speaker 1>as ninety thousand people immediately and put a ten foot

0:20:12.040 --> 0:20:14.679
<v Speaker 1>layer of molten ash as far as a thousand miles

0:20:14.720 --> 0:20:20.720
<v Speaker 1>around the park. Ten Yeah, that would cover your one

0:20:20.800 --> 0:20:24.000
<v Speaker 1>story house. Yeah, for a thousand miles. And um they

0:20:24.000 --> 0:20:27.920
<v Speaker 1>said that nuclear winter would probably almost be a certainty,

0:20:28.320 --> 0:20:34.800
<v Speaker 1>probably be a certainty almost probably. Uh. It would basically

0:20:34.840 --> 0:20:38.560
<v Speaker 1>blot out the sun and cool the earth, um, which

0:20:38.560 --> 0:20:41.680
<v Speaker 1>would kill our crops. It would be really really bad.

0:20:42.640 --> 0:20:45.640
<v Speaker 1>But they said, do you remember do you remember um

0:20:45.680 --> 0:20:50.399
<v Speaker 1>in two thousand and fourteen fifteen when that Icelandic volcano

0:20:50.840 --> 0:20:53.320
<v Speaker 1>went off, to the effect that it had, was it two?

0:20:54.160 --> 0:20:58.160
<v Speaker 1>The effect that it had on air travel in Europe. Yeah,

0:20:58.240 --> 0:21:00.400
<v Speaker 1>and it was just air travel and everybody he kept

0:21:00.440 --> 0:21:03.199
<v Speaker 1>waiting for it to clear up in it for weeks,

0:21:03.200 --> 0:21:07.399
<v Speaker 1>like flights were getting delayed, canceled, rerouted, like Europe was

0:21:07.480 --> 0:21:10.880
<v Speaker 1>just off the map as far as plane travel was going.

0:21:11.200 --> 0:21:14.600
<v Speaker 1>There's just plane travel. And that was a pretty small volcano.

0:21:15.000 --> 0:21:17.480
<v Speaker 1>It was in no way, shape or form a super volcano.

0:21:18.119 --> 0:21:23.560
<v Speaker 1>So just just that one aspect of transportation being affected,

0:21:23.800 --> 0:21:26.000
<v Speaker 1>let alone the fact that this could like kick off

0:21:26.000 --> 0:21:30.240
<v Speaker 1>an ice age. There's just so many, so many factors

0:21:30.240 --> 0:21:32.560
<v Speaker 1>that could come into play that could get us in

0:21:32.600 --> 0:21:34.480
<v Speaker 1>this way, get us in that way, get us. It

0:21:34.480 --> 0:21:37.359
<v Speaker 1>could affect our crops through sunlight and through temperature. It

0:21:37.400 --> 0:21:40.680
<v Speaker 1>could make as super cold, make our toes fall off.

0:21:40.720 --> 0:21:43.160
<v Speaker 1>There's just so many different ways it could. It could

0:21:43.200 --> 0:21:47.159
<v Speaker 1>affect us. Um that we just the average person is

0:21:47.200 --> 0:21:49.159
<v Speaker 1>not walking around thinking about this, and they should be

0:21:49.320 --> 0:21:52.280
<v Speaker 1>well true, but um not to be alarmist. They the

0:21:52.359 --> 0:21:56.280
<v Speaker 1>U S Geological Survey said that the probability that UM

0:21:56.520 --> 0:22:00.080
<v Speaker 1>that Yellowstone will blow its top is point zero ro

0:22:00.240 --> 0:22:04.880
<v Speaker 1>zero zero each year. Yeah, so one in seven hundred thousand,

0:22:05.200 --> 0:22:09.720
<v Speaker 1>which is on par of any given individual UM being

0:22:09.760 --> 0:22:13.320
<v Speaker 1>struck by lightning. So that makes me feel better. There's

0:22:13.320 --> 0:22:16.360
<v Speaker 1>still plenty of lightning out there. Yeah, and you never

0:22:16.400 --> 0:22:19.800
<v Speaker 1>know what's gonna happen. So apparently this the hot spot

0:22:20.640 --> 0:22:23.720
<v Speaker 1>causes the earth above it to dome once in a while,

0:22:23.760 --> 0:22:26.800
<v Speaker 1>and it feels like it showing off right. Yeah. I

0:22:26.800 --> 0:22:28.359
<v Speaker 1>bet the park rangers of the LA Zone when they

0:22:28.359 --> 0:22:31.760
<v Speaker 1>see that are like, man, is this it. There was

0:22:31.800 --> 0:22:35.480
<v Speaker 1>a two thousand three temperature increase just a few inches

0:22:35.520 --> 0:22:37.600
<v Speaker 1>below the soil and some spots that was hitting like

0:22:37.640 --> 0:22:41.640
<v Speaker 1>two hundred degrees fahrenheit, boiling the sap in trees nearby.

0:22:42.400 --> 0:22:44.720
<v Speaker 1>It was getting hot and then apparently it's already cool

0:22:44.760 --> 0:22:48.480
<v Speaker 1>down again. And what's probably going on in these processes

0:22:48.680 --> 0:22:52.200
<v Speaker 1>there's a process called incubation right where they're just sitting there.

0:22:52.440 --> 0:22:58.080
<v Speaker 1>Because the reservoir and the chamber are they have finite space.

0:22:58.680 --> 0:23:01.080
<v Speaker 1>So the more magma that builds up in it, the

0:23:01.480 --> 0:23:04.760
<v Speaker 1>higher the pressure builds. And if that pressure starts to

0:23:04.840 --> 0:23:07.600
<v Speaker 1>build and all of a sudden escapes a little bit,

0:23:08.040 --> 0:23:10.640
<v Speaker 1>that magma is gonna shoot up. And as that magma

0:23:10.720 --> 0:23:14.520
<v Speaker 1>shoots up, it starts to form air bubbles. Because the

0:23:14.600 --> 0:23:18.360
<v Speaker 1>change in elevation we're talking is traveling miles very quickly upward,

0:23:18.840 --> 0:23:22.160
<v Speaker 1>so bubbles start to form. As those bubbles breakup, they explode.

0:23:22.160 --> 0:23:25.239
<v Speaker 1>It's very much like champagne, and it shoots out and

0:23:25.280 --> 0:23:28.320
<v Speaker 1>it allows more magnet to follow behind it and follows

0:23:28.359 --> 0:23:33.200
<v Speaker 1>the same process. So there's huge explosion and it can

0:23:33.359 --> 0:23:37.640
<v Speaker 1>actually be hastened by earthquakes, or it can also be

0:23:37.920 --> 0:23:42.960
<v Speaker 1>um delayed by earthquakes. Yeah, um, so there's a lot

0:23:42.960 --> 0:23:46.159
<v Speaker 1>of different factors involved. But during this period where the

0:23:46.200 --> 0:23:50.000
<v Speaker 1>pressure is building and building and building. It's the incubation period.

0:23:50.320 --> 0:23:53.040
<v Speaker 1>And the reason it changes from say one year to

0:23:53.119 --> 0:23:55.760
<v Speaker 1>the next is if it's not getting as much magma,

0:23:56.000 --> 0:23:59.000
<v Speaker 1>then some of that magma higher up has the chance

0:23:59.119 --> 0:24:01.920
<v Speaker 1>to kind of cool and solidify and fall back down

0:24:02.160 --> 0:24:05.760
<v Speaker 1>and pressures relieved. But we have no way of tracking that.

0:24:05.800 --> 0:24:08.040
<v Speaker 1>We can just be like, oh my god, the ground

0:24:08.119 --> 0:24:11.520
<v Speaker 1>is bowing up. That's that's about where we're at right now.

0:24:11.640 --> 0:24:14.159
<v Speaker 1>But don't they generally think that dormancy is like the

0:24:14.200 --> 0:24:16.320
<v Speaker 1>longer it sits, the worst it's going to be when

0:24:16.320 --> 0:24:18.680
<v Speaker 1>it eventually does go off. That's what I read. Interesting.

0:24:18.960 --> 0:24:21.440
<v Speaker 1>Do you have anything else? Yeah, apparently one other thing.

0:24:21.760 --> 0:24:25.560
<v Speaker 1>Um if you were around a volcano then went off,

0:24:25.800 --> 0:24:28.639
<v Speaker 1>and I would guess any volcano, it would be like

0:24:28.680 --> 0:24:33.600
<v Speaker 1>breathing tiny glass needles thanks to all of the um

0:24:33.840 --> 0:24:37.800
<v Speaker 1>silicates that were ejected into the air. And I have

0:24:37.880 --> 0:24:42.720
<v Speaker 1>even one more other thing. There was a an volcano

0:24:42.800 --> 0:24:47.720
<v Speaker 1>that went off in eighteen fifteen, Tambora. I believe, I'm

0:24:47.720 --> 0:24:50.440
<v Speaker 1>not sure exactly where that was, but the Tambora earth

0:24:50.560 --> 0:24:56.639
<v Speaker 1>or volcano is credited with the creation of Frankenstein. Yeah,

0:24:56.720 --> 0:25:00.280
<v Speaker 1>it was the the year without a summer, and in

0:25:00.560 --> 0:25:06.159
<v Speaker 1>the northern and Northern Europe the summer was super super cool.

0:25:06.440 --> 0:25:09.440
<v Speaker 1>Elsewhere there was basically no summer. It was no the

0:25:09.480 --> 0:25:13.480
<v Speaker 1>whole the whole time. Um. But because of that, Mary

0:25:13.520 --> 0:25:19.320
<v Speaker 1>Shelley and uh Byron Right and her husband Percy by

0:25:19.400 --> 0:25:23.760
<v Speaker 1>Shelly Um all were stuck inside for during a summer vacation.

0:25:24.160 --> 0:25:26.480
<v Speaker 1>And that was when she came up with Frankenstein because

0:25:26.480 --> 0:25:29.720
<v Speaker 1>they had a scary story contest. There was a movie

0:25:29.760 --> 0:25:33.400
<v Speaker 1>about that. Yeah, but that that contest may never have happened,

0:25:33.400 --> 0:25:36.159
<v Speaker 1>and Frankenstein may never have been created had it not

0:25:36.280 --> 0:25:39.560
<v Speaker 1>been for that volcano going off. Yeah, that was a

0:25:39.600 --> 0:25:41.480
<v Speaker 1>freaky movie. I can't remember the name of it, The

0:25:41.880 --> 0:25:44.600
<v Speaker 1>Lost Summer. It wasn't that, man have been more than one.

0:25:46.160 --> 0:25:48.200
<v Speaker 1>I just remember the whole time. There was a lot

0:25:48.200 --> 0:25:50.880
<v Speaker 1>of drugs and Mary Shelley was like, Percy, why can't

0:25:50.880 --> 0:25:52.840
<v Speaker 1>you be more like Lord Byron And he's it because

0:25:52.840 --> 0:25:57.760
<v Speaker 1>I'm Percy. Who is in it? I'm just kidding? No, man,

0:25:57.920 --> 0:26:00.760
<v Speaker 1>was it called Gothic? I don't know. I seem to

0:26:00.800 --> 0:26:02.960
<v Speaker 1>remember that it was kind of a Why do I

0:26:03.000 --> 0:26:05.800
<v Speaker 1>think Julian Sands was in it? This sounds like a

0:26:05.880 --> 0:26:09.080
<v Speaker 1>Julian Sands. Movie's all very much in the very nineteenth

0:26:09.119 --> 0:26:12.640
<v Speaker 1>century drugs. It's in the back of my head. We'll

0:26:12.680 --> 0:26:16.200
<v Speaker 1>find out buried deep. Uh. If you want to know

0:26:16.640 --> 0:26:20.320
<v Speaker 1>more about volcanoes and Frankenstein and all that stuff, type

0:26:20.359 --> 0:26:22.960
<v Speaker 1>those words in the search bar how stuff works dot Com.

0:26:23.000 --> 0:26:25.160
<v Speaker 1>Since I said search bar, it's time for listener mail.

0:26:28.040 --> 0:26:33.160
<v Speaker 1>I'm gonna call this uh cool uncle from Katie. Hey, guys,

0:26:33.280 --> 0:26:36.200
<v Speaker 1>is about free speech. In ninety ninety, my uncle, Dennis

0:26:36.280 --> 0:26:40.600
<v Speaker 1>Barry was a director of Contemporary Art Center in Cincinnata, Ohio.

0:26:41.320 --> 0:26:44.359
<v Speaker 1>The museum brought in the Robert Maplethorpe UH Robert and

0:26:44.400 --> 0:26:48.359
<v Speaker 1>Maplethorp art exhibit titled The Perfect Moment, which resulted in

0:26:48.359 --> 0:26:51.439
<v Speaker 1>an uproar as seven of the photographs for seeing as

0:26:51.440 --> 0:26:55.439
<v Speaker 1>pornographic from some conservative folks. My uncle defended the artwork

0:26:55.760 --> 0:26:59.879
<v Speaker 1>this freedom of speech, and was subsequently arrested, charged with obscenity,

0:27:00.000 --> 0:27:02.480
<v Speaker 1>and went to trial, the first time in history that

0:27:02.520 --> 0:27:05.240
<v Speaker 1>a museum was actually taking the trial with criminal charges

0:27:05.280 --> 0:27:07.840
<v Speaker 1>over the contents of an exhibition. UH. He spent a

0:27:07.880 --> 0:27:11.240
<v Speaker 1>few nights in jail, received death threats, and was harassed

0:27:11.280 --> 0:27:13.560
<v Speaker 1>all over town, but he stuck to his firm beliefs

0:27:13.560 --> 0:27:16.159
<v Speaker 1>that artists had the right to express themselves freely in

0:27:16.200 --> 0:27:20.440
<v Speaker 1>American furthermore, deserved to have their work exhibited. During the trial,

0:27:20.520 --> 0:27:22.840
<v Speaker 1>art experts were brought in to help the jury decide

0:27:23.240 --> 0:27:26.880
<v Speaker 1>if they were pornographic in nature. They can you see

0:27:26.920 --> 0:27:31.119
<v Speaker 1>Matt like being, like I say, is a bull whip

0:27:31.119 --> 0:27:34.480
<v Speaker 1>in a man's rectum art? I never saw that show

0:27:34.520 --> 0:27:37.680
<v Speaker 1>as he Southern? No, that was falk Horn Leghorn. Yeah,

0:27:37.720 --> 0:27:41.480
<v Speaker 1>he was definitely Southern. Ultimately, the jury concluded that Maplethorpe's

0:27:41.520 --> 0:27:44.639
<v Speaker 1>work was in fact art and that my uncle, um

0:27:44.840 --> 0:27:51.680
<v Speaker 1>Northern Museum was not guilty of obscenity charges. Very cool.

0:27:51.720 --> 0:27:55.280
<v Speaker 1>Do you remember that? I remember that case? Oh really? Yeah? Man,

0:27:55.320 --> 0:27:58.320
<v Speaker 1>when maple Thorpe like, oh yeah, it was a huge deal.

0:27:59.119 --> 0:28:01.159
<v Speaker 1>Maybe it's because I was Toledo at the time, so

0:28:01.240 --> 0:28:02.840
<v Speaker 1>they made a big deal out of it. But it

0:28:02.880 --> 0:28:05.360
<v Speaker 1>was pretty big, she said. To this day, it's still

0:28:05.400 --> 0:28:07.119
<v Speaker 1>the most famous trial of freedom of speech in the

0:28:07.240 --> 0:28:10.040
<v Speaker 1>art world. Uh. And as an artist myself, I'm pretty

0:28:10.080 --> 0:28:12.800
<v Speaker 1>darn proud of my uncle's actions. Way back when he

0:28:12.840 --> 0:28:16.040
<v Speaker 1>admits himself that the events and effects of that trial

0:28:16.119 --> 0:28:18.480
<v Speaker 1>never really go away. He's still recognized for his actions.

0:28:18.800 --> 0:28:20.960
<v Speaker 1>The museums and galleries across the country have been able

0:28:21.000 --> 0:28:24.200
<v Speaker 1>to show challenging artwork that perhaps would have been cast

0:28:24.240 --> 0:28:27.439
<v Speaker 1>aside had my uncle and as awesome First Amendment lawyer H.

0:28:27.600 --> 0:28:33.720
<v Speaker 1>Lewis Serkin uh And not won that trial. Ultimately, the

0:28:33.720 --> 0:28:36.080
<v Speaker 1>result of the trial left the positive legacy for Contemporary

0:28:36.160 --> 0:28:38.240
<v Speaker 1>Arts Center, and my uncle went on to become the

0:28:38.280 --> 0:28:40.360
<v Speaker 1>founding director of the Rock and Roll Hall of Fame,

0:28:41.160 --> 0:28:43.880
<v Speaker 1>where he had to defend offensive song lyrics as art

0:28:44.200 --> 0:28:46.640
<v Speaker 1>in order to get them displayed in the museum. That

0:28:46.880 --> 0:28:49.080
<v Speaker 1>is such a great email. I love that email. He's

0:28:49.120 --> 0:28:50.640
<v Speaker 1>a pretty interesting guy to say the least. And that

0:28:50.680 --> 0:28:54.800
<v Speaker 1>is from Katie Barry and Katie Boy. Tell your uncle

0:28:54.960 --> 0:28:58.360
<v Speaker 1>Dennis that we have a lot of respect for him

0:28:58.520 --> 0:29:03.160
<v Speaker 1>for real, like not fake respect like but usually don't laugh, no,

0:29:03.440 --> 0:29:07.200
<v Speaker 1>like seriously, it's a it's a great story. Heads off

0:29:07.240 --> 0:29:09.920
<v Speaker 1>to your uncle. You know one thing, um, I'm sad

0:29:09.960 --> 0:29:12.959
<v Speaker 1>about that we didn't mention in the First Amendment episode

0:29:12.960 --> 0:29:16.480
<v Speaker 1>was that whole two Live Crew episode. You remember that

0:29:17.040 --> 0:29:18.920
<v Speaker 1>they all went to like I think they was a

0:29:18.960 --> 0:29:23.080
<v Speaker 1>Supreme Court over their lyrics. Didn't they Yeah, it was

0:29:23.120 --> 0:29:25.760
<v Speaker 1>a big deal. Everybody expected him to just lay down

0:29:25.840 --> 0:29:28.720
<v Speaker 1>and roll over. Nope, too, Life Crew, don't roll over

0:29:28.720 --> 0:29:31.239
<v Speaker 1>for nobody. Uh. You know we're going to do one

0:29:31.240 --> 0:29:33.160
<v Speaker 1>on the PMRC at some point, so we'll probably cover

0:29:33.160 --> 0:29:35.720
<v Speaker 1>it in that. Okay, good. Uh. If you want to

0:29:35.760 --> 0:29:38.800
<v Speaker 1>get in touch with us, you can tweet to us.

0:29:38.880 --> 0:29:41.400
<v Speaker 1>We're at s Y s K Podcast where at josh

0:29:41.520 --> 0:29:44.440
<v Speaker 1>um Clark. You can hang out on Facebook dot com

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<v Speaker 1>Stuff you Should Know. Send us an email to Stuff

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<v Speaker 1>Podcast at how stuff Works dot com, and as always,

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<v Speaker 1>other topics, visit how stuff Works dot com. M