WEBVTT - The Truth About Supervolcanoes

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<v Speaker 1>Brought to you by Toyota. Let's go places. Welcome to

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<v Speaker 1>Forward Thinking. Hey there, welcome to Forward Thinking, the podcast

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<v Speaker 1>that looks at the future and says, I don't know

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<v Speaker 1>where I'm I gonna go when the volcano blow. I'm

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<v Speaker 1>Jonathan Strickland, I'm Lauren, and I'm Joe McCormick. And today, yeah,

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<v Speaker 1>today we're gonna talk about Lauren and something terrifying. Super volcanoes.

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<v Speaker 1>A volcano was super volcano? Yeah? Now is a super

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<v Speaker 1>volcano bigger than an ultra volcano? Or less? I know?

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<v Speaker 1>It has a cape on it and during the day

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<v Speaker 1>it's a mild mannered reporter for a local newspaper. You know,

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<v Speaker 1>people want to know. I feel like we've gotten this

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<v Speaker 1>question before. Is a super volcano going to erupt and

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<v Speaker 1>into the world or at least wipe out a huge

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<v Speaker 1>percentage of species on Earth? And I can understand that

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<v Speaker 1>fear because I actually this, uh, this idea sort of

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<v Speaker 1>entered my mind and infected me with strange fears years

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<v Speaker 1>ago back when I read a book. I read a

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<v Speaker 1>book called The Road by Cormick McCarthy. What a cheerful

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<v Speaker 1>book that was. It is a very good book, but

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<v Speaker 1>It is not a cheerful book. It's sort of a

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<v Speaker 1>I don't want to say too much about it, you know,

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<v Speaker 1>go read it if you're interested, But it's a story

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<v Speaker 1>of a journey in a very desolate post apocalyptic landscape. Um.

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<v Speaker 1>And I was wondering after I read the book, Huh,

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<v Speaker 1>I wonder what it is that the author had in mind,

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<v Speaker 1>because he never said what it is that happened that

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<v Speaker 1>sort of ruined the earth. Frequently in these post apocalyptic

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<v Speaker 1>media's media's, yes, that is totally the way that you

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<v Speaker 1>pluralize that word. Um. You no one ever tells you

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<v Speaker 1>exactly what happened, or if they do, it gets cheesy.

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<v Speaker 1>And I think that's why the rest of them don't sure.

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<v Speaker 1>And so the question is wondering here, like was this

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<v Speaker 1>supposed to be like a nuclear war or was it

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<v Speaker 1>supposed to be like an asteroid impact, some kind of

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<v Speaker 1>a natural, purely earthbound event. Yeah, yeah, I didn't know.

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<v Speaker 1>But it describes a scenario where like all the plant

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<v Speaker 1>life is dead, and it's very cold, and the sky

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<v Speaker 1>is always gray and dark, and there's ash everywhere, and

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<v Speaker 1>and I wondered until I read somewhere on the internet,

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<v Speaker 1>I don't remember where it was now, this was years ago,

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<v Speaker 1>but I read a blog post with somebody having a

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<v Speaker 1>theory that said, oh, well, obviously what has happened in

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<v Speaker 1>this scenario is that it was an eruption of the

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<v Speaker 1>yellow Stone supervolcano. And that makes a lot of sense

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<v Speaker 1>from the as you read the book, if you think

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<v Speaker 1>of it in those terms, the conditions that are mentioned

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<v Speaker 1>in the book seemed to go pretty well. Was something

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<v Speaker 1>like that. Yeah, I think it's a very good possibility.

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<v Speaker 1>I mean, it's also possible that the author didn't actually

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<v Speaker 1>have any one particular thing in mind. But and ultimately

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<v Speaker 1>it doesn't really matter, that's not the point of the story.

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<v Speaker 1>But it is interesting to think that that could have

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<v Speaker 1>been the triggering event. Sure, a caveat. Though it's possible

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<v Speaker 1>that it is the triggering event in this story, it

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<v Speaker 1>is extremely unlikely that this will actually happen, certainly within

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<v Speaker 1>our lifetime. Yeah, we want to be clear that we're

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<v Speaker 1>going to talk about some stuff that is really scary,

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<v Speaker 1>I mean tering you know, and it's it's is legitimately

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<v Speaker 1>scary stuff. However, we also want to point out that

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<v Speaker 1>there is no reason to believe that there is any

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<v Speaker 1>oncoming eruption even within like the century or or several centuries,

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<v Speaker 1>that the likelihood of such an eruption happening in any

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<v Speaker 1>any given years one and seven hundred thousand. That was

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<v Speaker 1>one of the figures I saw. So, uh, let's start

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<v Speaker 1>off by saying, we're going to talk about what could

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<v Speaker 1>happen with a super volcano eruption, but let's also acknowledge

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<v Speaker 1>there's no indication such a thing is going to happen

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<v Speaker 1>in time soon. Yes, and I imagine big friendly letters

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<v Speaker 1>on your screen that just say don't pan. Yes, yes said.

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<v Speaker 1>It definitely makes me feel better. And now I want

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<v Speaker 1>some something that is almost but not quite exactly unlike tea.

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<v Speaker 1>I mean, raining burning ash and lava everywhere, but don't

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<v Speaker 1>panic because it's because yeah, like like you said, it's true.

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<v Speaker 1>I think many, um many people who have explored the

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<v Speaker 1>possibility of a super volcano eruption, especially specifically the eruption

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<v Speaker 1>of the yellow Stone super volcano in North America, have

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<v Speaker 1>sort of pursued it with a kind of like you know,

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<v Speaker 1>playing up the drama and like, oh, this this looming danger.

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<v Speaker 1>We we do want to say at the beginning, it's

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<v Speaker 1>not very likely yeah, it's it's calm yourself down. It's

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<v Speaker 1>kind of the similar look at what would happen with

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<v Speaker 1>the doomsday scenario of an enormous asteroid heading towards Earth.

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<v Speaker 1>It's one of those things that you know, it's important

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<v Speaker 1>to know what you're up against in the unlikely event

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<v Speaker 1>that had happened, because if you play the long game,

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<v Speaker 1>and we're not talking about your lifetime or the lifetime

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<v Speaker 1>of the next like five generations, I'm talking over the

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<v Speaker 1>span of thousands of years. If you play the long game,

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<v Speaker 1>it will happen eventually. But the key word there's eventually.

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<v Speaker 1>And the important thing is to say, all right, well,

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<v Speaker 1>what can we do with this knowledge? And we will

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<v Speaker 1>talk about what some serious science researchers are are planning

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<v Speaker 1>for in in case this happens to happen, um, because

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<v Speaker 1>we'll have some warning, y'all. But in the meanwhile, let

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<v Speaker 1>us define what a super volcano is. Right. We're not

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<v Speaker 1>going to get to what to put in your volcano

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<v Speaker 1>kit yet. Okay, yeah, what is a super volcano? Okay? Well,

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<v Speaker 1>I was curious about this, so I looked it up

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<v Speaker 1>and it seems to me that one of the ways

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<v Speaker 1>that scientists measure the magnitude of a volcanic eruption is

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<v Speaker 1>the volcanic explosivity index or the v I, which sssive

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<v Speaker 1>the index that's so great it sounds to me like

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<v Speaker 1>a Tenacious D album. Yeah, the v E I. So

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<v Speaker 1>it's a numerical score for how bad it done blowed

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<v Speaker 1>up that makes sense, ranging from zero to eight. And

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<v Speaker 1>it's a sign based on a number of criteria, like

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<v Speaker 1>the volume in cubic kilometers of ejected pyroclastic materials, all

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<v Speaker 1>the hot stuff that comes out of the volcano in

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<v Speaker 1>cubic kilometers. Yes, yes, dwell, well, but it's some of

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<v Speaker 1>these scores. It's like point zero zero one cubic kilometers.

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<v Speaker 1>That's somewhat more comforting. I suppose a right, how high

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<v Speaker 1>the eruption column reaches into the sky. And then also

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<v Speaker 1>they're like subjective qualities about the character of the eruption, right,

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<v Speaker 1>I think it was brassy or exactly, you know, classy eruption.

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<v Speaker 1>Right's right. So it's kind of similar to the Richter scale. Actually,

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<v Speaker 1>it's similar to the Richter scale that we use for earthquakes,

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<v Speaker 1>like the Richter scale at the upper level. Also, the

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<v Speaker 1>v e I at least it's the scores are logarithmic,

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<v Speaker 1>meaning that an increase in one number to the next

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<v Speaker 1>is actually an increase in an order of magnitude. So

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<v Speaker 1>from one number to the next could be a dramatic

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<v Speaker 1>increase in the actual output of the volcano. Right, So

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<v Speaker 1>I'm gonna give you the examples of those upper levels.

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<v Speaker 1>So a five on the v I is uh, it

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<v Speaker 1>corresponds to one cubic kilometer. That's a little bit less

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<v Speaker 1>than a quarter of a cubic mile. Yeah, of of

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<v Speaker 1>ejected of what's called ejecta, all this stuff that comes

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<v Speaker 1>out and then settles down on the ground. These words

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<v Speaker 1>are great. Yeah. So the so the nineteen eighty eruption

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<v Speaker 1>of Mount St. Helen's was a five, and that that

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<v Speaker 1>was a big eruption. Yeah, that was huge, But it

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<v Speaker 1>was a five. Okay, wait six? Who here was alive?

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<v Speaker 1>And that during the nineteen eighty amount St Helen's eruption

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<v Speaker 1>just me, okay, let's keep going. It wasn't, but I've

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<v Speaker 1>seen pictures. Yeah, not go on. A six core spunds

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<v Speaker 1>to ten cubic kilometers. That's about two point four cubic miles. Yeah,

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<v Speaker 1>A seven corresponds to about a hundred cubic kilometers twenty

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<v Speaker 1>four cubic miles. You can see how the math is

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<v Speaker 1>working out here, and an eight corresponds to a thousand

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<v Speaker 1>cubic kilometers two miles. Okay, So one way of defining

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<v Speaker 1>a supervolcano is that it's a volcanic eruption that's greater

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<v Speaker 1>than an eight on the v e I eight or

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<v Speaker 1>great so, so a thousand cubic kilometers are more, Yeah,

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<v Speaker 1>which translates to about two hundred forty sometimes people say

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<v Speaker 1>about two hundred fifty cubic miles of ejecta, all this

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<v Speaker 1>hot stuff that comes up out of the volcano and

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<v Speaker 1>then settles down on the Earth. Now, people don't people

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<v Speaker 1>don't always use the v I because it has some limitations,

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<v Speaker 1>like it can't measure equally across all time scales like

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<v Speaker 1>way back into the past. Um. And it does measure

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<v Speaker 1>the release of volcanic gas, which can actually be one

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<v Speaker 1>of the most important effects of volcanic have a very

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<v Speaker 1>long lasting climate effect. Yeah. Um, So a less complicated

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<v Speaker 1>metric is just that level that volume of ejecta we

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<v Speaker 1>were talking about, So a volume greater than a thousand

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<v Speaker 1>cubic kilometers of stuff. But a thousand cubic kilometers I'm

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<v Speaker 1>having trouble picturing in my head. Give me, give me

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<v Speaker 1>a concept here. I tried to come up with a couple. Uh,

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<v Speaker 1>it's a lot, so it doesn't really compare much to like,

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<v Speaker 1>you know, this mini buckets. It's do you remember the

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<v Speaker 1>comment six? And then a couple of Russian names. It's

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<v Speaker 1>the one that the e s a rosette emission and

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<v Speaker 1>ye okay, so yeah, you remember that comment. And then

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<v Speaker 1>that was a wonderful emotional time seeing that lander set

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<v Speaker 1>down on the comet. It was beautiful. But now imagine

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<v Speaker 1>because that comment had a volume of twenty one point

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<v Speaker 1>four cubic kilometers, So the smallest possible supervolcano eruption ejects

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<v Speaker 1>about forty seven of this commet's worth of pyroclastic material.

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<v Speaker 1>So that comment forty seven times burning hot raining down

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<v Speaker 1>on the earth. So we need forties seven probes to

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<v Speaker 1>lent is. I think I might have taken the analogy. Yeah,

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<v Speaker 1>another comparison, A thousand cubic kilometers is more than the

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<v Speaker 1>volume of Lake Titicaka in Peru. If you want to

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<v Speaker 1>look up this lake on the internet, look up a picture.

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<v Speaker 1>It's big. A thousand cubic kilometers is also more than

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<v Speaker 1>double the volume of Lake Erie in North America, which

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<v Speaker 1>is four three cubic kilometers. This is, this is huge,

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<v Speaker 1>and these really big eruptions get bigger than a thousand

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<v Speaker 1>cubic kilometers. But so we should we should put it

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<v Speaker 1>in perspective how often these things happen. Large eruptions are

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<v Speaker 1>much less common than small eruptions. Eruptions that register low

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<v Speaker 1>on the v I scale happen all the time. There's

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<v Speaker 1>one happening right now, They're they're always going on. The

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<v Speaker 1>middle of the scale gets pretty rare, and the top

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<v Speaker 1>of the scale is very rare. In fact, there have

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<v Speaker 1>been exactly zero supervolcano eruptions in recorded human history. Uh,

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<v Speaker 1>there have been no supervolcano eruptions in the entire Holocene epoch.

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<v Speaker 1>But there have been supervolcano eruptions since humans have existed.

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<v Speaker 1>And one example that I thought would be good to

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<v Speaker 1>talk about would be the Toba supervolcano eruption about seventy

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<v Speaker 1>four thousand years ago. Yeah, that happened on the island

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<v Speaker 1>of Sumatra in present day Indonesia, and it included at

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<v Speaker 1>least two thousand, eight hundred cubic kilometers of stuff. That's

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<v Speaker 1>about six hundred and seventy two cubic miles. I did

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<v Speaker 1>not do the calculation for how many comets that is,

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<v Speaker 1>but that's a lot of comments. I did a calcula

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<v Speaker 1>lation of my own in order to put it into

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<v Speaker 1>something vaguely understandable and yet not helpful at all. Uh.

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<v Speaker 1>There are some one point one trillion gallons in a

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<v Speaker 1>single cubic mile, so the stuff that came out of

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<v Speaker 1>this volcano equalled about seven hundred and forty trillion gallons. Wow. Sure,

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<v Speaker 1>it's a bunch um like, like billions of tons of

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<v Speaker 1>hot ash and rock flowing onto the surrounding area, plus

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<v Speaker 1>hundreds of cubic kilometers of of ash and gases spewing

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<v Speaker 1>into the atmosphere. Um. It was so violent that the

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<v Speaker 1>mountain containing the volcano collapsed, uh, leaving what's now Lake Toba,

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<v Speaker 1>which is the largest volcanic lake in the world, with

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<v Speaker 1>a surface area of some one thousand, one hundred thirty

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<v Speaker 1>square kilometers or four d forty square miles in a

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<v Speaker 1>depth of about five or uh feet. That's just fifty

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<v Speaker 1>square miles less than the area of Los Angeles for comparison,

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<v Speaker 1>that's the lake leftover, Yes, that's the crater. Researchers out

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<v Speaker 1>of Oxford University think that the the gases that it

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<v Speaker 1>put out circled the entire globe, and that the ash

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<v Speaker 1>covered a span from the Arabian Sea to the east UM,

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<v Speaker 1>across the entire Indian subcontinent and too into the South

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<v Speaker 1>China Sea in the west UM and then uh some

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<v Speaker 1>like three thousand kilometers south into the Indian Ocean. UM.

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<v Speaker 1>And that's just matter that scientists have collected and confirmed

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<v Speaker 1>as being from this eruption so far. So obviously, an

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<v Speaker 1>eruption like that is not just a negative local event,

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<v Speaker 1>Like it's not just that you'd worry about getting caught

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<v Speaker 1>in the falling ash and hot rock, which would suck.

0:13:49.120 --> 0:13:50.920
<v Speaker 1>But no, but now this is I mean, unless you

0:13:50.960 --> 0:13:54.320
<v Speaker 1>consider a local event a continent um. In that case,

0:13:54.360 --> 0:13:57.240
<v Speaker 1>sure to it's local um. But but no, that this

0:13:57.320 --> 0:14:01.520
<v Speaker 1>was this was big and the result of cooling effect

0:14:01.880 --> 0:14:06.079
<v Speaker 1>as everything that's spewed out started reflecting sunlight, caused global

0:14:06.120 --> 0:14:08.920
<v Speaker 1>weather effects and may have in fact influenced the earth

0:14:09.000 --> 0:14:12.400
<v Speaker 1>slip into a particularly cold era of the ice ages. Yeah.

0:14:12.440 --> 0:14:16.360
<v Speaker 1>In fact, I read about a theory that this event

0:14:16.480 --> 0:14:20.080
<v Speaker 1>may have had something to do with human genetic history. Yeah,

0:14:20.360 --> 0:14:24.720
<v Speaker 1>combined with climate data, some genetic data that researchers have

0:14:24.800 --> 0:14:29.480
<v Speaker 1>been looking into from humans around the time, might indicate

0:14:29.520 --> 0:14:32.400
<v Speaker 1>a huge dip in the number of human people who

0:14:32.400 --> 0:14:36.320
<v Speaker 1>were reproducing around the time of Toba's eruption. Uh, Like

0:14:36.600 --> 0:14:43.160
<v Speaker 1>this eruption might have nearly driven us to extinction. Wow. Well,

0:14:43.360 --> 0:14:47.720
<v Speaker 1>that that's scary and crazy and kind of cool and amazing.

0:14:47.840 --> 0:14:52.200
<v Speaker 1>But it's also like not the only time in history

0:14:52.240 --> 0:14:56.800
<v Speaker 1>that volcanic activity would be associated with extinction. Oh, certainly. Well,

0:14:56.840 --> 0:14:58.400
<v Speaker 1>And I also do want to point out that there

0:14:58.400 --> 0:15:02.040
<v Speaker 1>were a lot fewer humans like Homo sapiens running around

0:15:02.200 --> 0:15:05.240
<v Speaker 1>right seventy four thousand years ago then there are, say today,

0:15:05.320 --> 0:15:09.120
<v Speaker 1>we're in a kound of a vulnerable position anyway, yes, uh.

0:15:09.160 --> 0:15:12.280
<v Speaker 1>And in fact, when you talk about volcanic activity being

0:15:12.320 --> 0:15:16.280
<v Speaker 1>associated with mass extinctions, every single mass extinction has been

0:15:16.320 --> 0:15:21.240
<v Speaker 1>correlated with volcanic activity. Not necessarily that the volcanic activity

0:15:21.440 --> 0:15:25.440
<v Speaker 1>directly caused the mass extinction but likely contributed to it,

0:15:25.840 --> 0:15:30.040
<v Speaker 1>didn't help. Yeah, Now, when you're talking about major volcanic activity,

0:15:30.280 --> 0:15:33.000
<v Speaker 1>help is not something that would immediately spring to mind.

0:15:33.080 --> 0:15:36.200
<v Speaker 1>You might be crying it, but that's not what's certainly

0:15:36.240 --> 0:15:40.160
<v Speaker 1>not aiding the planet. As far as flaming salamander, you're

0:15:40.200 --> 0:15:43.560
<v Speaker 1>probably not excited. So well, first we should say, I mean,

0:15:43.600 --> 0:15:47.440
<v Speaker 1>what is a mass extinction. A mass extinction is basically

0:15:47.560 --> 0:15:53.360
<v Speaker 1>a period um when a huge number of species on

0:15:53.520 --> 0:15:57.640
<v Speaker 1>Earth completely die out all around the same time. And

0:15:57.840 --> 0:16:00.760
<v Speaker 1>this doesn't actually mean it's a like all at once,

0:16:00.840 --> 0:16:02.720
<v Speaker 1>like they all died on the same day. This can

0:16:02.760 --> 0:16:05.840
<v Speaker 1>happen over over many, many years, you know, like thousands

0:16:05.840 --> 0:16:08.760
<v Speaker 1>of years or even millions of years on the geologic scale.

0:16:08.880 --> 0:16:13.160
<v Speaker 1>But looking back across geological history you can see these

0:16:13.240 --> 0:16:17.240
<v Speaker 1>happening very very suddenly. There's sort of like spikes in

0:16:17.440 --> 0:16:21.240
<v Speaker 1>die off on a geologic scale. It's sunden for if

0:16:21.280 --> 0:16:24.040
<v Speaker 1>you were living through it, it would it could be

0:16:24.160 --> 0:16:27.600
<v Speaker 1>an entire it could be multiple lifetimes, multiple multiple lifetimes.

0:16:27.600 --> 0:16:29.640
<v Speaker 1>So uh. In other words, we're not going to say,

0:16:29.640 --> 0:16:32.240
<v Speaker 1>like the dinosaurs died out on a Thursday. That's not

0:16:32.280 --> 0:16:35.120
<v Speaker 1>what we mean. When did Yeah, but not all of

0:16:35.120 --> 0:16:37.960
<v Speaker 1>them all on one Thursday. I would argue that Thursdays

0:16:37.960 --> 0:16:43.240
<v Speaker 1>had not been invented yet, so at any rate, raptors lives,

0:16:44.200 --> 0:16:46.600
<v Speaker 1>they might have been very fond of Thursday. They did

0:16:46.600 --> 0:16:51.240
<v Speaker 1>not call them thursdays, they called them boy those were

0:16:51.240 --> 0:16:54.720
<v Speaker 1>the days at any rate. So at the end of

0:16:54.760 --> 0:16:59.480
<v Speaker 1>the Triassic Period, about half of the species living on Earth,

0:16:59.680 --> 0:17:04.040
<v Speaker 1>both on land and in water, went extinct, and scientists

0:17:04.119 --> 0:17:07.400
<v Speaker 1>found that the cause was likely the massive eruptions that

0:17:07.520 --> 0:17:10.120
<v Speaker 1>had produced enough lava to bury the entire United States

0:17:10.200 --> 0:17:13.720
<v Speaker 1>under three feet of it um. If if you had

0:17:13.760 --> 0:17:16.440
<v Speaker 1>added all all the eject up, that's how much it

0:17:16.480 --> 0:17:18.919
<v Speaker 1>would have. You know, you could have covered uh the

0:17:18.960 --> 0:17:21.280
<v Speaker 1>Earth with three or the United States rather with three

0:17:21.119 --> 0:17:23.560
<v Speaker 1>ft of lava uh. And this happened around the time

0:17:23.600 --> 0:17:26.800
<v Speaker 1>that Pangaea, which is the super continent, was breaking apart.

0:17:26.880 --> 0:17:30.159
<v Speaker 1>So this was all due to tectonic forces. And the

0:17:30.280 --> 0:17:33.119
<v Speaker 1>eruptions themselves weren't a single event. It wasn't like there

0:17:33.200 --> 0:17:37.040
<v Speaker 1>was one massive supervolcanic eruption after which there was this

0:17:37.160 --> 0:17:40.520
<v Speaker 1>massive amount of lava. It was a series of eruptions

0:17:40.520 --> 0:17:46.439
<v Speaker 1>that took course over six hundred thousand years. So again

0:17:46.520 --> 0:17:49.880
<v Speaker 1>not one of those you know, singular events. We as

0:17:49.960 --> 0:17:54.040
<v Speaker 1>humans often think about things as like a singular event.

0:17:54.119 --> 0:17:56.880
<v Speaker 1>For one, it makes it a lot easier to understand

0:17:56.960 --> 0:18:00.520
<v Speaker 1>and talk about and uh and to our lives are

0:18:00.680 --> 0:18:05.000
<v Speaker 1>very short compared to geological time scale, but in truth,

0:18:05.160 --> 0:18:08.600
<v Speaker 1>it happened over hundreds of thousands of years. However, that

0:18:08.800 --> 0:18:12.359
<v Speaker 1>was the event that would lead to the opportunity for

0:18:13.040 --> 0:18:17.480
<v Speaker 1>dinosaurs to spring into certain niches and and take over

0:18:17.480 --> 0:18:19.960
<v Speaker 1>and become the dominant life force for quite some time.

0:18:20.600 --> 0:18:25.200
<v Speaker 1>And then the Cretaceous Tertiary boundary, the KT boundary, that's

0:18:25.240 --> 0:18:27.680
<v Speaker 1>when we talk about how all the dinosaurs all went extinct.

0:18:28.720 --> 0:18:33.000
<v Speaker 1>So the biggest popular theory for a very long time

0:18:33.080 --> 0:18:35.359
<v Speaker 1>was that an asteroid wiped out the dinosaurs. There was

0:18:35.359 --> 0:18:38.840
<v Speaker 1>an asteroid impact which caused global climate change and that

0:18:38.880 --> 0:18:42.240
<v Speaker 1>wiped out the dinosaurs, And that's still very much part

0:18:42.400 --> 0:18:46.840
<v Speaker 1>of the prevailing theory. However, there's also a lot of

0:18:46.880 --> 0:18:50.879
<v Speaker 1>support growing support and in a large consensus building for

0:18:51.119 --> 0:18:56.360
<v Speaker 1>the idea that volcanic eruptions had already created the situation

0:18:56.400 --> 0:18:59.520
<v Speaker 1>where the asteroid was kind of the finishing blow. So

0:18:59.640 --> 0:19:03.080
<v Speaker 1>it was and that the asteroid was solely responsible for

0:19:03.240 --> 0:19:07.080
<v Speaker 1>dinosaurs going extinct. It was that conditions were primed for

0:19:07.119 --> 0:19:09.600
<v Speaker 1>that to happen because of the volcanic activity that had

0:19:09.640 --> 0:19:16.440
<v Speaker 1>already taken place largely in India. So, yes, these these

0:19:16.480 --> 0:19:20.919
<v Speaker 1>volcanic eruptions have been correlated with uh with extinctions, but

0:19:20.960 --> 0:19:23.639
<v Speaker 1>correlation and causation are two different things. Obviously, It's a

0:19:23.680 --> 0:19:26.679
<v Speaker 1>lot more complicated than just pointing at a single source

0:19:26.720 --> 0:19:29.520
<v Speaker 1>and saying this is what caused everything to die out.

0:19:30.000 --> 0:19:32.679
<v Speaker 1>I think a lot of us maybe I'm speaking for

0:19:32.720 --> 0:19:35.200
<v Speaker 1>everybody else. When I think of volcanoes, I often think

0:19:35.200 --> 0:19:38.560
<v Speaker 1>of just the immediate view of you know, the idea

0:19:38.560 --> 0:19:40.520
<v Speaker 1>of lava streaming down the side of the mountain, and

0:19:40.560 --> 0:19:43.639
<v Speaker 1>that that, to me, is represents the the immediate danger.

0:19:44.359 --> 0:19:48.160
<v Speaker 1>But as we've discussed, that's just one of the many

0:19:48.320 --> 0:19:51.040
<v Speaker 1>things that you have to worry about volcanic eruption. Yeah,

0:19:51.080 --> 0:19:53.240
<v Speaker 1>and on a global level, it's it's much more likely

0:19:53.280 --> 0:19:55.640
<v Speaker 1>to I mean the same way that a nuclear blast

0:19:55.720 --> 0:19:58.320
<v Speaker 1>will kill a certain number of people in a certain area,

0:19:58.600 --> 0:20:00.880
<v Speaker 1>but the fallout from that us just a lot more

0:20:00.880 --> 0:20:04.560
<v Speaker 1>wide reaching, right exactly. Yeah, it's a very good analogy.

0:20:04.720 --> 0:20:09.240
<v Speaker 1>So we wanted to talk specifically about the Yellowstone supervolcano.

0:20:09.720 --> 0:20:14.600
<v Speaker 1>This was this was I mean, it'll it'll eventually erupt,

0:20:15.320 --> 0:20:18.800
<v Speaker 1>It'll there'll there will eventually be a super eruption. Whether

0:20:18.880 --> 0:20:21.640
<v Speaker 1>that eventually is like any time within the next few

0:20:21.640 --> 0:20:25.000
<v Speaker 1>thousand years, who can say, Um, it's not likely, and

0:20:25.119 --> 0:20:27.399
<v Speaker 1>if it does happen, we will likely have lots of

0:20:27.880 --> 0:20:32.000
<v Speaker 1>warning signs before it happens. But the reason why we

0:20:32.119 --> 0:20:34.720
<v Speaker 1>are we're specifically focusing on this is one we are

0:20:34.720 --> 0:20:36.680
<v Speaker 1>based in the United States, so it's one of those

0:20:36.720 --> 0:20:39.920
<v Speaker 1>things that, um, is easy for us to focus on.

0:20:40.240 --> 0:20:43.480
<v Speaker 1>To the reason why I even suggested we do supervolcanoes

0:20:43.640 --> 0:20:46.360
<v Speaker 1>is there was a mini series like kind of made

0:20:46.359 --> 0:20:48.920
<v Speaker 1>for TV movie thing that came out in the mid

0:20:48.920 --> 0:20:52.560
<v Speaker 1>two thousand's called Supervolcano and it recently got added to

0:20:52.600 --> 0:20:56.560
<v Speaker 1>Netflix and I watched it, and its specifically deals with

0:20:56.560 --> 0:21:00.040
<v Speaker 1>the Yellowstone supervolcano. And it's interesting. I mean all, a

0:21:00.000 --> 0:21:03.640
<v Speaker 1>lot of the research they did for that is essentially correct,

0:21:04.119 --> 0:21:06.160
<v Speaker 1>or at least was correct based upon what was known

0:21:06.240 --> 0:21:08.520
<v Speaker 1>in the mid two thousand's, so it's not like they

0:21:08.560 --> 0:21:12.280
<v Speaker 1>went crazy with the research. I will say that, Um,

0:21:12.280 --> 0:21:14.920
<v Speaker 1>it's a lot like the articles that we've read where

0:21:15.400 --> 0:21:18.119
<v Speaker 1>you get all the horrible things that will happen, and

0:21:18.160 --> 0:21:20.280
<v Speaker 1>then a sentence at the instinct this probably won't happen.

0:21:21.200 --> 0:21:23.119
<v Speaker 1>It felt like it was an entire mini series that

0:21:23.200 --> 0:21:27.000
<v Speaker 1>was made that way. But at any rate, UM the

0:21:27.080 --> 0:21:30.640
<v Speaker 1>super volcano at Yellowstone has had three major eruptions. I mean,

0:21:30.640 --> 0:21:34.000
<v Speaker 1>there's been lots of different smaller eruptions, but three major ones,

0:21:34.240 --> 0:21:37.399
<v Speaker 1>two of which meet the super volcano criteria of the

0:21:37.440 --> 0:21:40.720
<v Speaker 1>two or two hundred and fifty cubic miles of ojecta.

0:21:40.920 --> 0:21:43.120
<v Speaker 1>So the first happened two point one million years ago,

0:21:44.480 --> 0:21:46.840
<v Speaker 1>so quite some time ago, the second one point two

0:21:46.880 --> 0:21:50.359
<v Speaker 1>million years ago, and the more recent one six hundred

0:21:50.440 --> 0:21:54.720
<v Speaker 1>forty thousand years ago, so not in recent memory certainly.

0:21:55.280 --> 0:21:58.439
<v Speaker 1>And that first eruption was about six thousand times the

0:21:58.480 --> 0:22:00.800
<v Speaker 1>size of the Mount St. Helen's eruption that we talked

0:22:00.800 --> 0:22:04.360
<v Speaker 1>about earlier UH, and the latest one caused the collapse

0:22:04.480 --> 0:22:07.520
<v Speaker 1>of the eruption area. This is actually fairly common. Where

0:22:08.000 --> 0:22:11.960
<v Speaker 1>a a large volcanic eruption, you typically have a a

0:22:12.160 --> 0:22:17.480
<v Speaker 1>chamber beneath the volcanic area that is containing the molten material,

0:22:17.920 --> 0:22:20.720
<v Speaker 1>and when it empties out, often the weight of both

0:22:20.800 --> 0:22:25.240
<v Speaker 1>the the UH surface above it and the ejecta causes

0:22:25.280 --> 0:22:28.720
<v Speaker 1>a collapse. So the latest eruption caused the collapse of

0:22:28.720 --> 0:22:31.240
<v Speaker 1>of this eruption area, which created a sunken crater called

0:22:31.280 --> 0:22:34.879
<v Speaker 1>a caldera, and it's big. It's fift nd square miles

0:22:34.880 --> 0:22:37.560
<v Speaker 1>in area, which is larger than the state of Rhode Island.

0:22:38.000 --> 0:22:41.320
<v Speaker 1>You could fit Rhode Island into the volcanic caldera of

0:22:41.359 --> 0:22:45.679
<v Speaker 1>the Yellowstone Supervolcano. I don't recommend you do it, because

0:22:46.000 --> 0:22:47.959
<v Speaker 1>everyone in Rhode Island would wonder why you pulled them

0:22:47.960 --> 0:22:50.959
<v Speaker 1>off the eastern seaboard. They would be pretty mad. They

0:22:50.960 --> 0:22:54.240
<v Speaker 1>would no longer be called an island unless they're an

0:22:54.280 --> 0:22:56.439
<v Speaker 1>island in the caldera. I mean, they're not technically an

0:22:56.480 --> 0:22:59.320
<v Speaker 1>island anyway, but you'd have even less recent than at

0:22:59.320 --> 0:23:03.640
<v Speaker 1>any rate. Uh So under this park, under the Yelliston

0:23:03.680 --> 0:23:06.520
<v Speaker 1>Park is the magma chamber. Now we've known about the

0:23:07.520 --> 0:23:11.200
<v Speaker 1>initial magma chamber for a really long time, um, and

0:23:11.400 --> 0:23:15.719
<v Speaker 1>it's essentially between three and nine miles beneath the surface.

0:23:15.760 --> 0:23:18.359
<v Speaker 1>It depends upon where you are at any point along

0:23:18.480 --> 0:23:22.000
<v Speaker 1>the area where the magma chamber exists. And it's tough

0:23:22.040 --> 0:23:24.200
<v Speaker 1>to map these things out, you know, we can't really

0:23:24.200 --> 0:23:28.160
<v Speaker 1>dig down to see them. Um. But if you were

0:23:28.200 --> 0:23:31.880
<v Speaker 1>to empty out this chamber, you could fill the one

0:23:31.920 --> 0:23:35.159
<v Speaker 1>thousand cubic mile Grand canyon two point five times with

0:23:35.240 --> 0:23:38.120
<v Speaker 1>the stuff inside it, so two and a half times

0:23:38.160 --> 0:23:41.280
<v Speaker 1>the amount that you would need to completely seal that

0:23:41.400 --> 0:23:45.320
<v Speaker 1>crack uh known as the Grand Canyon. But that's just

0:23:45.440 --> 0:23:50.320
<v Speaker 1>the beginning, because in April two scientists found a second

0:23:50.359 --> 0:23:54.000
<v Speaker 1>magma chamber underneath the first one and well, and this

0:23:54.080 --> 0:23:56.600
<v Speaker 1>actually answered a lot of questions because they were wondering

0:23:56.960 --> 0:24:00.720
<v Speaker 1>how was the magma connecting to the chamber, like where.

0:24:00.760 --> 0:24:04.160
<v Speaker 1>Obviously it's coming from somewhere around in the mantle region

0:24:04.280 --> 0:24:07.840
<v Speaker 1>of Earth, and there's some sort of plume that has

0:24:07.880 --> 0:24:11.399
<v Speaker 1>to connect the mantle to that magma chamber, otherwise you

0:24:11.400 --> 0:24:13.920
<v Speaker 1>wouldn't have it there, right, But they weren't sure how

0:24:13.960 --> 0:24:15.840
<v Speaker 1>that was working. And now they found that there is

0:24:15.880 --> 0:24:19.720
<v Speaker 1>a larger magma chamber underneath the first one, and it's

0:24:19.880 --> 0:24:23.800
<v Speaker 1>it's kind of the way station between the mantle and UH,

0:24:23.960 --> 0:24:27.040
<v Speaker 1>the upper magma chamber. So this one's bigger. It's about

0:24:27.080 --> 0:24:30.800
<v Speaker 1>four point four times larger than the one that's the

0:24:31.280 --> 0:24:35.439
<v Speaker 1>shallow magma chamber, and UH it's somewhere between twelve and

0:24:35.480 --> 0:24:38.200
<v Speaker 1>twenty eight miles beneath the surface again depending upon where

0:24:38.200 --> 0:24:41.520
<v Speaker 1>you're at, and UH it has enough magma to fill

0:24:41.560 --> 0:24:45.240
<v Speaker 1>the Grand Canyon more than eleven times. What I'm picturing

0:24:45.280 --> 0:24:48.520
<v Speaker 1>here is is Thor filling up the Grand Canyon with

0:24:48.600 --> 0:24:50.919
<v Speaker 1>magma and then drinking it down and then shoving it

0:24:50.920 --> 0:24:52.960
<v Speaker 1>off the table, the Grand Canyon right off the table.

0:24:53.000 --> 0:24:58.080
<v Speaker 1>And I got another boy, Thor is a jerk, and uh,

0:24:59.680 --> 0:25:04.119
<v Speaker 1>there's a whole storyline about it actually, So anyway, um, so,

0:25:04.560 --> 0:25:07.000
<v Speaker 1>one thing that scientists do point out, and it is

0:25:07.040 --> 0:25:10.639
<v Speaker 1>important to think on because you know, when I hear

0:25:10.720 --> 0:25:14.119
<v Speaker 1>magma chamber, I think like big gooey chamber filled with

0:25:14.119 --> 0:25:17.159
<v Speaker 1>with lava goo or magma really because lava wants it.

0:25:17.720 --> 0:25:21.200
<v Speaker 1>It is exposed to the atmosphere. But that's not exactly

0:25:21.240 --> 0:25:25.280
<v Speaker 1>what we're looking at. Only about nine of the material

0:25:25.400 --> 0:25:28.040
<v Speaker 1>in the upper magma chamber is actually molten rock, and

0:25:28.119 --> 0:25:32.080
<v Speaker 1>most of it is stored inside of spongy, very hot rock.

0:25:32.720 --> 0:25:35.000
<v Speaker 1>So you've got the spongey hot rock and inside you

0:25:35.000 --> 0:25:37.080
<v Speaker 1>can think of it as having porous cavities to have

0:25:37.119 --> 0:25:42.320
<v Speaker 1>a gooey molten magma center. So yeah, that's great news.

0:25:42.480 --> 0:25:45.359
<v Speaker 1>That's only nine Only nine percent of it is actually

0:25:45.400 --> 0:25:47.800
<v Speaker 1>the molten rock, is what I'm saying. And the lower

0:25:47.880 --> 0:25:51.360
<v Speaker 1>chamber has an even lower percentage of molten rock. Two

0:25:51.960 --> 0:25:54.200
<v Speaker 1>of the material in that is multen rock. It sounds

0:25:54.240 --> 0:26:00.360
<v Speaker 1>like a chocolate lava cake, but but actual lava. Yeah,

0:26:00.400 --> 0:26:05.520
<v Speaker 1>Magma service. Instead of all completely molten rock, there's some

0:26:06.080 --> 0:26:11.560
<v Speaker 1>giant chunks of rock that contain molten stuff. We'll fly

0:26:11.720 --> 0:26:14.919
<v Speaker 1>at your at your face and bust open and if

0:26:14.960 --> 0:26:17.440
<v Speaker 1>it makes you feel better, at Lauren, you probably wouldn't

0:26:17.520 --> 0:26:20.480
<v Speaker 1>be live long enough to notice that. Tell me about

0:26:20.600 --> 0:26:23.959
<v Speaker 1>magma funnels, all right, So so magma funnels this, This

0:26:24.040 --> 0:26:26.000
<v Speaker 1>is the this is the plume. I was talking about

0:26:26.040 --> 0:26:28.720
<v Speaker 1>the way that the way this magma gets funneled up

0:26:28.800 --> 0:26:33.320
<v Speaker 1>from the mantle or perhaps even lower down. So this

0:26:33.359 --> 0:26:36.080
<v Speaker 1>is where we start getting into a lot of estimations.

0:26:36.080 --> 0:26:38.200
<v Speaker 1>I mean, we were already talking about estimations of three

0:26:38.240 --> 0:26:40.400
<v Speaker 1>to nine miles below the service or twelve to twenty

0:26:40.440 --> 0:26:42.760
<v Speaker 1>eight miles below the service, And a lot of this

0:26:42.840 --> 0:26:45.640
<v Speaker 1>is coming to us from seismic information that's been picked

0:26:45.680 --> 0:26:48.080
<v Speaker 1>up over time, and we can learn a lot through

0:26:48.119 --> 0:26:51.240
<v Speaker 1>seismic data. We've talked about how sound travels at different

0:26:51.240 --> 0:26:54.800
<v Speaker 1>speeds through different media, and by measuring that those differences,

0:26:54.840 --> 0:26:57.639
<v Speaker 1>that's how we can figure out a lot of what

0:26:57.920 --> 0:27:03.359
<v Speaker 1>is the composition underneath Yellows Ozone Park. So the Yellowstone

0:27:03.400 --> 0:27:07.560
<v Speaker 1>hot spot plume is what connects the magma in the

0:27:08.160 --> 0:27:11.760
<v Speaker 1>UH in the lower chamber to the mantle UH and

0:27:11.800 --> 0:27:16.080
<v Speaker 1>then the lower chamber is attached to the upper chamber UM.

0:27:16.240 --> 0:27:18.640
<v Speaker 1>And remember the lower ones the bigger one. So the

0:27:18.680 --> 0:27:22.159
<v Speaker 1>hot spot plume is probably around forty miles beneath the

0:27:22.240 --> 0:27:25.720
<v Speaker 1>surface and extends downward to a depth of about four

0:27:25.960 --> 0:27:28.960
<v Speaker 1>d forty miles in the Earth's mantle, although some estimates

0:27:28.960 --> 0:27:31.359
<v Speaker 1>suggest that perhaps it goes all the way down to

0:27:31.400 --> 0:27:35.760
<v Speaker 1>the Earth's core, so one thousand, eight hundred miles UM.

0:27:35.840 --> 0:27:38.480
<v Speaker 1>But it depends upon which model you're looking at. So

0:27:39.720 --> 0:27:42.560
<v Speaker 1>one of the implications of this larger magma chamber that

0:27:42.640 --> 0:27:47.399
<v Speaker 1>was discovered in April is that it could potentially feed

0:27:47.440 --> 0:27:49.560
<v Speaker 1>magma into the upper chamber in the event of a

0:27:49.640 --> 0:27:52.639
<v Speaker 1>large scale eruption. So, in other words, imagine that you

0:27:52.760 --> 0:27:56.280
<v Speaker 1>have a major eruption where that upper magma chamber, which

0:27:56.359 --> 0:27:58.960
<v Speaker 1>can fill the Grand Canyon two and a half times over,

0:27:59.640 --> 0:28:05.879
<v Speaker 1>erupt then gets refilled by the lower chamber, erupts again,

0:28:05.960 --> 0:28:09.679
<v Speaker 1>then gets refilled by the lower because the lower chambers

0:28:09.720 --> 0:28:12.520
<v Speaker 1>four point four times the size of the upper chamber.

0:28:13.359 --> 0:28:16.479
<v Speaker 1>So you can essentially multiply that number by four and

0:28:16.560 --> 0:28:19.760
<v Speaker 1>say that that like super worst case scenario. And keep

0:28:19.800 --> 0:28:22.320
<v Speaker 1>in mind, these eruptions can take place over the course

0:28:22.480 --> 0:28:25.960
<v Speaker 1>of a very long time, like months. We're not talking

0:28:26.000 --> 0:28:28.960
<v Speaker 1>about again, we're not talking about a single explosive event.

0:28:29.480 --> 0:28:32.800
<v Speaker 1>An eruption can take place over a very long amount

0:28:32.800 --> 0:28:37.800
<v Speaker 1>of time. Now, is it possible yes? Is it likely? No?

0:28:38.120 --> 0:28:40.800
<v Speaker 1>So I wanted to mention that again, it is not

0:28:41.000 --> 0:28:46.160
<v Speaker 1>likely to happen. But just for fun, let's talk about

0:28:46.240 --> 0:28:50.560
<v Speaker 1>what a super volcanic eruption would look like. This fun.

0:28:51.600 --> 0:28:56.520
<v Speaker 1>I am using the word fun ironically. Uh So. The

0:28:56.600 --> 0:28:59.840
<v Speaker 1>BBC reported that in the event of a super eruption,

0:29:00.800 --> 0:29:03.600
<v Speaker 1>of people living within a thousand kilometers of the blast

0:29:03.600 --> 0:29:07.920
<v Speaker 1>area could die from the eruptions straightaway. I just looked

0:29:07.960 --> 0:29:10.760
<v Speaker 1>up on Google Maps. If we're within a thousand kilometers,

0:29:11.160 --> 0:29:14.920
<v Speaker 1>we are well outside of a thousand kilometers of yea,

0:29:15.040 --> 0:29:18.080
<v Speaker 1>so no problem. Yeah, because we're we're in Atlanta. That's

0:29:18.200 --> 0:29:21.880
<v Speaker 1>really far away from Yelliston National Park. Uh yeah, no,

0:29:22.000 --> 0:29:25.040
<v Speaker 1>we are well outside of a thousand kilometers. But not

0:29:25.160 --> 0:29:27.200
<v Speaker 1>to gloat or anything. Yeah, yeah, And and and a

0:29:27.280 --> 0:29:30.480
<v Speaker 1>note here about this particular estimation. Uh Tobas seems to

0:29:30.560 --> 0:29:33.800
<v Speaker 1>have been uninhabited by humans and other species of the

0:29:33.840 --> 0:29:36.080
<v Speaker 1>Homo genus at the time of the eruption, So we

0:29:36.120 --> 0:29:39.680
<v Speaker 1>don't have any kind of archaeological record of how a

0:29:39.720 --> 0:29:44.200
<v Speaker 1>super volcanic eruption would directly affect even a proto civilization, right,

0:29:44.960 --> 0:29:47.800
<v Speaker 1>so this is yeah, this is this is a guess.

0:29:47.840 --> 0:29:50.600
<v Speaker 1>And then again it's it's BBC researchers who came up

0:29:50.600 --> 0:29:52.680
<v Speaker 1>with this number. And they I'm sure they consulted with

0:29:52.720 --> 0:29:56.080
<v Speaker 1>lots of geology, right, but this has not come from

0:29:56.120 --> 0:29:59.320
<v Speaker 1>the U S Geological Survey, which is the group that's

0:29:59.480 --> 0:30:03.400
<v Speaker 1>in charge jo of actually looking into this here in

0:30:03.440 --> 0:30:05.400
<v Speaker 1>the United States. Say, what do they have to say

0:30:05.400 --> 0:30:09.760
<v Speaker 1>about this? Well, so they talked more about the ash dispersal,

0:30:09.920 --> 0:30:12.040
<v Speaker 1>Like they don't spend a whole lot of time talking

0:30:12.080 --> 0:30:15.120
<v Speaker 1>about the stuff that would happen in the immediately immediate

0:30:15.200 --> 0:30:19.560
<v Speaker 1>blast zone. But you know, they actually said that they

0:30:19.640 --> 0:30:23.200
<v Speaker 1>ran computer models to see where ash would disperse around

0:30:23.920 --> 0:30:27.520
<v Speaker 1>Yellowstone in the event of a super volcano eruption. And

0:30:27.560 --> 0:30:30.160
<v Speaker 1>the reason they said they did it was they got

0:30:30.200 --> 0:30:35.560
<v Speaker 1>tired of telling people we don't know, like, like, what

0:30:35.600 --> 0:30:38.200
<v Speaker 1>would happen if the super volcano erupted? We don't know.

0:30:38.680 --> 0:30:43.080
<v Speaker 1>Like after a while they said, we should probably find out. Yeah,

0:30:43.160 --> 0:30:47.440
<v Speaker 1>we'll do a couple of models. Will look Yeah. I

0:30:47.480 --> 0:30:49.920
<v Speaker 1>can't imagine what it must be like to work there

0:30:50.000 --> 0:30:53.360
<v Speaker 1>and get these kind of calls from various forms of

0:30:53.360 --> 0:30:56.400
<v Speaker 1>the media, asking because I mean, it is a sensationalized

0:30:56.440 --> 0:30:59.640
<v Speaker 1>story in many ways. And you could say, well, it's

0:30:59.680 --> 0:31:03.200
<v Speaker 1>import because it has the potential to impact the entire world,

0:31:03.640 --> 0:31:07.640
<v Speaker 1>and and it will happen at some point, so therefore,

0:31:08.400 --> 0:31:11.640
<v Speaker 1>isn't it news worthy? The geologists are meanwhile, like I

0:31:11.880 --> 0:31:15.120
<v Speaker 1>need a drink. So in two thousand and fourteen, they

0:31:15.240 --> 0:31:17.160
<v Speaker 1>ran a computer model to look at this, and they

0:31:17.160 --> 0:31:19.880
<v Speaker 1>looked at different versions of the model, like one where

0:31:20.280 --> 0:31:22.520
<v Speaker 1>an eruption would last for maybe a day or two,

0:31:22.560 --> 0:31:24.200
<v Speaker 1>and one where it would last for a week, and

0:31:24.240 --> 0:31:26.760
<v Speaker 1>one where it would last for an entire month, And

0:31:26.800 --> 0:31:30.080
<v Speaker 1>they laid out a map of where the ash would disperse.

0:31:31.200 --> 0:31:36.000
<v Speaker 1>And the good news is their models found that the

0:31:36.040 --> 0:31:39.760
<v Speaker 1>ash accumulation would actually be quote far less end quote

0:31:39.880 --> 0:31:45.280
<v Speaker 1>than that predicted by numerous doomsday scenarios, but still enough

0:31:45.320 --> 0:31:49.880
<v Speaker 1>to kill just about everybody in the United States eventually. Um. So,

0:31:50.560 --> 0:31:54.080
<v Speaker 1>they found that ash from super eruptions gets distributed in

0:31:54.120 --> 0:31:58.040
<v Speaker 1>a different way than ash from normal eruptions, and that's

0:31:58.080 --> 0:32:01.200
<v Speaker 1>because the super eruption creates a number Brella cloud capable

0:32:01.240 --> 0:32:04.320
<v Speaker 1>of pushing ash more than a thousand kilometers up wind,

0:32:04.520 --> 0:32:09.400
<v Speaker 1>so against the wind. Um. So, typically in a volcanic eruption,

0:32:09.440 --> 0:32:11.880
<v Speaker 1>you would see the ash dispersal look like a fan

0:32:12.720 --> 0:32:16.320
<v Speaker 1>extending from the volcano down wind. That's what it would

0:32:16.360 --> 0:32:20.440
<v Speaker 1>normally look like. But with the super volcanoes, it looks

0:32:20.480 --> 0:32:22.960
<v Speaker 1>more like a bull's eye, with the volcano in the center,

0:32:24.040 --> 0:32:26.080
<v Speaker 1>a little bit of an off center bull's eye. It's

0:32:26.120 --> 0:32:29.320
<v Speaker 1>still going to have more dispersal down wind than up wind,

0:32:29.440 --> 0:32:32.320
<v Speaker 1>but the volcano will still be closer to the center

0:32:32.360 --> 0:32:36.560
<v Speaker 1>than at one end of the map. UH. And they

0:32:36.600 --> 0:32:39.160
<v Speaker 1>said that a layer of ash ten centimeters thick or

0:32:39.200 --> 0:32:42.000
<v Speaker 1>more could cover the area within five hundred miles of

0:32:42.040 --> 0:32:46.120
<v Speaker 1>the eruption. UH And even in more distant regions, like

0:32:46.160 --> 0:32:48.160
<v Speaker 1>say New York City, you would still get a dusting

0:32:48.360 --> 0:32:51.000
<v Speaker 1>of volcanic ash. And this is serious stuff, guys. The

0:32:51.280 --> 0:32:53.000
<v Speaker 1>ash is not like the ash you would find in

0:32:53.040 --> 0:32:57.880
<v Speaker 1>your fireplace. Volcanic ash has tiny rocks in it um,

0:32:57.920 --> 0:33:00.000
<v Speaker 1>and these tiny rocks can do a huge amount of damn.

0:33:00.360 --> 0:33:06.200
<v Speaker 1>So let's talk about some of the stuff that could happen. Alright,

0:33:06.280 --> 0:33:10.080
<v Speaker 1>So the eruption would would contain dangerous particles and gases

0:33:10.120 --> 0:33:14.480
<v Speaker 1>like carbon dioxide, sulfur dioxide, hydrochloric acid, and hydrofluoric acid.

0:33:15.000 --> 0:33:16.960
<v Speaker 1>These are not great things for us to come into

0:33:16.960 --> 0:33:19.320
<v Speaker 1>contact with. You don't really want to breathe them. Yeah,

0:33:19.320 --> 0:33:22.840
<v Speaker 1>if you breathe in the particles, then you can have

0:33:23.160 --> 0:33:25.560
<v Speaker 1>a lot of symptoms that are very similar to that

0:33:25.680 --> 0:33:28.040
<v Speaker 1>of the common cold. If it's a short term exposure,

0:33:28.120 --> 0:33:32.800
<v Speaker 1>so we're talking coughing, sneezing, you know, running nose um,

0:33:32.840 --> 0:33:36.320
<v Speaker 1>possibly developing ato bronchitis. If you have long term exposure,

0:33:36.560 --> 0:33:38.239
<v Speaker 1>it can get it much worse. You can actually get

0:33:38.280 --> 0:33:40.640
<v Speaker 1>damaged to your lungs. It can tear up the tissue

0:33:40.640 --> 0:33:42.720
<v Speaker 1>in your lungs um. Also, there are a lot of

0:33:42.720 --> 0:33:45.640
<v Speaker 1>people who talk about how if ash gets UH can

0:33:45.840 --> 0:33:50.120
<v Speaker 1>combined with say uh fluid, it could essentially turn your

0:33:50.160 --> 0:33:54.080
<v Speaker 1>lungs into concrete, which is very lovely to think about.

0:33:54.560 --> 0:33:56.840
<v Speaker 1>But it also can get in your eyes. It can

0:33:56.880 --> 0:33:59.800
<v Speaker 1>cause your eyes to itch. You can also cause corneal abrasions,

0:33:59.800 --> 0:34:03.360
<v Speaker 1>so damaging your eyes. Um, you would obviously if you

0:34:03.400 --> 0:34:05.480
<v Speaker 1>were in an area where volcanic ash was falling, you

0:34:05.480 --> 0:34:08.239
<v Speaker 1>would want a gas mask and goggles. I mean, you

0:34:08.239 --> 0:34:09.680
<v Speaker 1>would want to be able to have some sort of

0:34:09.719 --> 0:34:14.120
<v Speaker 1>filter um to filter out these particles and something protecting

0:34:14.160 --> 0:34:18.360
<v Speaker 1>your eyes in this this sort of environment. Uh. It

0:34:18.440 --> 0:34:23.360
<v Speaker 1>also can contaminate water supplies. Accumulation can lead to structural damage.

0:34:23.719 --> 0:34:27.120
<v Speaker 1>This stuff weighs more than say snow would and ten

0:34:27.200 --> 0:34:29.840
<v Speaker 1>centimeters doesn't sound like a lot, but it's enough to

0:34:30.000 --> 0:34:35.080
<v Speaker 1>collapse certain buildings roofs, so that's a big issue. Also, um,

0:34:35.120 --> 0:34:39.160
<v Speaker 1>it can short out electrical transformers and plunge entire areas

0:34:39.200 --> 0:34:43.080
<v Speaker 1>into blackout status, So that would be a real problem.

0:34:43.160 --> 0:34:46.239
<v Speaker 1>And again, because we're talking about ash dispersing in a

0:34:46.360 --> 0:34:52.560
<v Speaker 1>five hundred mile area around the supervolcano. At ten centimeters

0:34:52.680 --> 0:34:55.800
<v Speaker 1>or so, that's enough to affect a huge amount of

0:34:55.800 --> 0:34:59.439
<v Speaker 1>the United States. Even on outlying areas like where we live,

0:34:59.719 --> 0:35:02.279
<v Speaker 1>we it still get some ash and maybe enough for

0:35:02.320 --> 0:35:04.960
<v Speaker 1>it to cause some serious problems if nothing else, contaminating

0:35:04.960 --> 0:35:08.640
<v Speaker 1>water supplies and making it difficult to grow crops or

0:35:08.719 --> 0:35:13.440
<v Speaker 1>raise livestock. Uh So, lots of effects there throughout the

0:35:13.520 --> 0:35:16.560
<v Speaker 1>entire United States. Even if we were somehow lucky with

0:35:16.600 --> 0:35:20.360
<v Speaker 1>the weather patterns to avoid most of the ash, you

0:35:20.440 --> 0:35:24.160
<v Speaker 1>still have the issue of entire areas of the country

0:35:24.200 --> 0:35:27.600
<v Speaker 1>that we're dedicated to food production would be unable to

0:35:27.600 --> 0:35:32.320
<v Speaker 1>do that for an indeterminate amount of time. Oh sure.

0:35:32.480 --> 0:35:36.400
<v Speaker 1>And then again that the cooling effect of having those

0:35:36.440 --> 0:35:39.400
<v Speaker 1>gases in the air would affect not just the United States,

0:35:39.480 --> 0:35:43.280
<v Speaker 1>but potentially the whole world. Yeah, we're talking global impact

0:35:43.400 --> 0:35:47.400
<v Speaker 1>with this kind of level of eruption. So that cooling

0:35:47.440 --> 0:35:49.719
<v Speaker 1>effect could be as according to the BBC, up to

0:35:49.760 --> 0:35:53.160
<v Speaker 1>ten degrees And since it is the BBC, I'm guessing

0:35:53.160 --> 0:35:56.640
<v Speaker 1>they're talking celsius because it's the BBC. Why would they

0:35:56.640 --> 0:35:59.879
<v Speaker 1>speak in fahrenheit. Um. So, that kind of decrease could

0:35:59.880 --> 0:36:04.000
<v Speaker 1>have that global food production, including things like stopping them

0:36:04.040 --> 0:36:07.680
<v Speaker 1>monsoon season, which we could lead to vast areas of

0:36:07.680 --> 0:36:11.279
<v Speaker 1>of of food just not growing and lead to starvation.

0:36:11.960 --> 0:36:16.560
<v Speaker 1>So we're talking about uh, global devastation. I mean in

0:36:16.600 --> 0:36:20.120
<v Speaker 1>different ways. Like obviously the areas around the volcano would

0:36:20.120 --> 0:36:23.920
<v Speaker 1>be physically devastated, and then other areas would be affected

0:36:23.960 --> 0:36:27.120
<v Speaker 1>in a more long term fashion. Now, granted, this climate

0:36:27.200 --> 0:36:31.880
<v Speaker 1>change would be temporary, particularly in the in the grand

0:36:31.920 --> 0:36:34.719
<v Speaker 1>scheme of things, but we're talking still a period of

0:36:34.760 --> 0:36:38.080
<v Speaker 1>like a decade and ten years. While short on a

0:36:38.120 --> 0:36:40.960
<v Speaker 1>geological scale, that's a long time to go without being

0:36:40.960 --> 0:36:44.400
<v Speaker 1>able to grow food effectively. So it could lead to

0:36:44.680 --> 0:36:48.440
<v Speaker 1>really big problems. And that leads us again to the

0:36:48.520 --> 0:36:52.240
<v Speaker 1>question should we worry about this? And really the answer

0:36:52.440 --> 0:36:57.480
<v Speaker 1>is not really. The odds of it have actually happening

0:36:57.520 --> 0:37:01.120
<v Speaker 1>are so low that they're other things that we need

0:37:01.160 --> 0:37:04.799
<v Speaker 1>to worry about. First. Um, it does mean that, you know,

0:37:04.960 --> 0:37:09.240
<v Speaker 1>being aware of it tells us that eventually it will happen,

0:37:09.320 --> 0:37:11.480
<v Speaker 1>so we have to have some sort of plan in place.

0:37:11.520 --> 0:37:14.920
<v Speaker 1>But it's not like we have a sin submergency of guys,

0:37:15.280 --> 0:37:18.279
<v Speaker 1>we need to figure out our supervolcano plan like tomorrow.

0:37:18.800 --> 0:37:20.360
<v Speaker 1>Yeah yeah. Like, like we said at the top of

0:37:20.400 --> 0:37:24.080
<v Speaker 1>the show, the odds of something like this happening in

0:37:24.120 --> 0:37:27.840
<v Speaker 1>any given year are only one in seven hundred thousand

0:37:28.120 --> 0:37:30.799
<v Speaker 1>and and I know that that even to some people

0:37:30.880 --> 0:37:33.120
<v Speaker 1>might say, well, wow, that's still like those odds. I

0:37:33.120 --> 0:37:35.920
<v Speaker 1>don't like those at all, But that's probably because as

0:37:35.960 --> 0:37:42.600
<v Speaker 1>human beings were really bad at conceptualizing these kind of odds, right,

0:37:42.640 --> 0:37:45.640
<v Speaker 1>I mean, it's it. We're notoriously terrible about it, to

0:37:45.680 --> 0:37:50.319
<v Speaker 1>the point where why people go to casinos. Yeah, it's

0:37:50.440 --> 0:37:55.160
<v Speaker 1>it's why. It's why people, you know, ignore statistics about

0:37:55.280 --> 0:37:57.160
<v Speaker 1>how likely they are to get in a car accident

0:37:57.239 --> 0:37:59.879
<v Speaker 1>versus an airplane accident. You know, it's it's we're bad

0:38:00.000 --> 0:38:03.640
<v Speaker 1>at it because it's difficult for us to think in

0:38:03.680 --> 0:38:06.080
<v Speaker 1>those terms. And when I say we, I mean me too.

0:38:06.120 --> 0:38:08.640
<v Speaker 1>I'm the same way. I I fall into the same

0:38:08.680 --> 0:38:13.200
<v Speaker 1>traps as everybody else. Anything interesting sounds more dangerous to

0:38:13.840 --> 0:38:16.200
<v Speaker 1>essentially Yeah, well, I mean the most interesting man the

0:38:16.200 --> 0:38:18.719
<v Speaker 1>world is pop probably the most dangerous one too. I

0:38:18.760 --> 0:38:22.959
<v Speaker 1>mean I haven't asked him. I'm scared. But uh, yeah,

0:38:23.520 --> 0:38:26.960
<v Speaker 1>so that there are definitely reasons why we need to

0:38:27.120 --> 0:38:30.560
<v Speaker 1>think about it, and we need to plan for things,

0:38:30.600 --> 0:38:32.720
<v Speaker 1>and really we just need to make a better world

0:38:33.200 --> 0:38:36.560
<v Speaker 1>in general, and for multiple reasons. But one of them

0:38:36.640 --> 0:38:38.759
<v Speaker 1>is because it would help us in the in the

0:38:38.840 --> 0:38:42.760
<v Speaker 1>case of a supervolcanic eruption. Uh. In fact, the folks

0:38:42.760 --> 0:38:45.879
<v Speaker 1>that Yellowstone say that it's far more likely that we'll

0:38:45.920 --> 0:38:50.799
<v Speaker 1>see small eruptions ones that would not not even raise

0:38:50.840 --> 0:38:53.400
<v Speaker 1>a blip on on anything beyond the regional scale, And

0:38:53.440 --> 0:38:55.480
<v Speaker 1>even for regional it might just mean that certain parts

0:38:55.480 --> 0:38:58.120
<v Speaker 1>of the park are closed off due to lava flow,

0:38:58.600 --> 0:39:02.120
<v Speaker 1>and that this will probably happen over the course of

0:39:02.160 --> 0:39:05.200
<v Speaker 1>several hundred years where it starts to you know, it

0:39:05.200 --> 0:39:07.560
<v Speaker 1>relieves bits of pressure, and that the pressure does not

0:39:07.640 --> 0:39:11.439
<v Speaker 1>continuously build up to super eruption levels. If that were

0:39:11.480 --> 0:39:14.600
<v Speaker 1>to happen, it would be preceded by earthquakes, likely for

0:39:14.719 --> 0:39:17.920
<v Speaker 1>weeks or maybe even months before any kind of other event,

0:39:18.360 --> 0:39:21.319
<v Speaker 1>So we would have lots of warning signs before there

0:39:21.360 --> 0:39:25.279
<v Speaker 1>was ever any kind of super volcanic eruption. Uh. And

0:39:25.360 --> 0:39:27.680
<v Speaker 1>once those warning sides happened, then it would become really

0:39:27.719 --> 0:39:31.200
<v Speaker 1>important for us to decide what happens next. Because I mean,

0:39:31.960 --> 0:39:36.080
<v Speaker 1>even if you if you discount the global impact, which

0:39:36.239 --> 0:39:39.919
<v Speaker 1>really shouldn't do. But even if if as Americans, we say, look,

0:39:40.080 --> 0:39:42.040
<v Speaker 1>we're just really concerned about what's going to happen to

0:39:42.080 --> 0:39:43.480
<v Speaker 1>us right now. We'll have to worry about the rest

0:39:43.520 --> 0:39:46.320
<v Speaker 1>of the world later, this would be obviously a huge

0:39:46.640 --> 0:39:49.960
<v Speaker 1>blow to national security, right, I mean, the United States

0:39:49.960 --> 0:39:53.120
<v Speaker 1>would effectively not be the US anymore in the wake

0:39:53.160 --> 0:39:56.120
<v Speaker 1>of something like this, if it were to have the uh,

0:39:56.440 --> 0:40:00.960
<v Speaker 1>the far reaching consequences that we've talked about. So if

0:40:01.160 --> 0:40:03.200
<v Speaker 1>we were to see those kind of early warning signs,

0:40:03.239 --> 0:40:06.840
<v Speaker 1>we would have some very serious conversations very very quickly.

0:40:07.480 --> 0:40:10.560
<v Speaker 1>But again, the likelihood of it happening is so low

0:40:10.640 --> 0:40:13.399
<v Speaker 1>that you know, it's I feel pretty comfortable saying it's

0:40:13.400 --> 0:40:15.439
<v Speaker 1>not going to happen within my lifetime, or at least

0:40:15.440 --> 0:40:19.240
<v Speaker 1>the odds are astronomical that it would happen within my lifetime.

0:40:19.680 --> 0:40:23.600
<v Speaker 1>So that's your problem. Guys, who's who's old guy? Now?

0:40:26.880 --> 0:40:28.759
<v Speaker 1>Keep on joking about old I am. I'm going to

0:40:28.840 --> 0:40:30.600
<v Speaker 1>be dead before I have to worry about this. So

0:40:31.160 --> 0:40:35.640
<v Speaker 1>you're the one who makes all the jokes about that. Yeah,

0:40:35.719 --> 0:40:39.400
<v Speaker 1>I mean I've done it, like to come on, see

0:40:39.480 --> 0:40:41.160
<v Speaker 1>you see how it's all coming out. Now. See it's

0:40:41.160 --> 0:40:43.600
<v Speaker 1>a defense mechanism. People. If I make the jokes that

0:40:44.000 --> 0:40:46.040
<v Speaker 1>it heads them off of the pass. How often do

0:40:46.120 --> 0:40:48.839
<v Speaker 1>you dream of us being thrown into a volcano by us?

0:40:48.880 --> 0:40:52.800
<v Speaker 1>I mean the younger generations. Do day dreams count because

0:40:53.520 --> 0:40:56.600
<v Speaker 1>it would make the number higher? Um, all right, So

0:40:56.920 --> 0:40:59.080
<v Speaker 1>it also depends on how long I'm waiting for my tacos.

0:41:00.239 --> 0:41:03.839
<v Speaker 1>There's a lot of imaginary throwing people into volcanoes when

0:41:03.840 --> 0:41:06.879
<v Speaker 1>I'm waiting in line for tacos, all right, So yeah,

0:41:06.920 --> 0:41:09.440
<v Speaker 1>I mean, come on, it's that's hanger right there. It

0:41:09.480 --> 0:41:12.280
<v Speaker 1>can't be. It can't be held responsible for my day dreams.

0:41:13.080 --> 0:41:15.279
<v Speaker 1>But this was actually really interesting to look into. It

0:41:15.320 --> 0:41:17.200
<v Speaker 1>was one of those things I learned a lot looking

0:41:17.200 --> 0:41:20.080
<v Speaker 1>into this, and and after having seen that that mini

0:41:20.120 --> 0:41:24.640
<v Speaker 1>series where I was like, well, that's absolutely terrifying. How

0:41:24.760 --> 0:41:27.160
<v Speaker 1>how realistic is this and looking into it and thinking,

0:41:27.160 --> 0:41:29.319
<v Speaker 1>all right, it's not realistic in the sense of it's

0:41:29.400 --> 0:41:33.280
<v Speaker 1>not likely to happen, but the actual depiction of events

0:41:33.360 --> 0:41:37.279
<v Speaker 1>was pretty interesting and I think fairly accurate. I mean,

0:41:37.280 --> 0:41:41.319
<v Speaker 1>obviously we didn't even cover how the particulates in the

0:41:41.360 --> 0:41:44.680
<v Speaker 1>atmosphere would mean that we would see no no flights,

0:41:45.160 --> 0:41:47.759
<v Speaker 1>like all flights would be grounded across all of North

0:41:47.800 --> 0:41:52.720
<v Speaker 1>America and probably other areas around North America, but definitely

0:41:52.760 --> 0:41:54.840
<v Speaker 1>all of North America. No flights would be going in

0:41:54.840 --> 0:41:58.720
<v Speaker 1>around So I mean, you know, it's it's pretty pretty

0:41:58.719 --> 0:42:02.040
<v Speaker 1>phenomenal when you think about it, but again, not likely

0:42:02.080 --> 0:42:03.879
<v Speaker 1>to happen if you want to hear about other things

0:42:03.920 --> 0:42:06.239
<v Speaker 1>that aren't likely to happen. You should write us and

0:42:06.280 --> 0:42:08.719
<v Speaker 1>tell us, or you just have an idea for a

0:42:08.719 --> 0:42:11.040
<v Speaker 1>future episode. There's something that you've always wanted to learn

0:42:11.120 --> 0:42:12.920
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0:42:12.960 --> 0:42:15.520
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0:42:15.600 --> 0:42:18.800
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0:42:19.040 --> 0:42:22.160
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0:42:22.200 --> 0:42:25.000
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0:42:25.000 --> 0:42:27.520
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0:42:32.080 --> 0:42:38.800
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0:42:38.840 --> 0:42:51.720
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0:42:51.840 --> 0:42:54.640
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