WEBVTT - SYSK Selects: Geysers: Nature's Innuendo

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<v Speaker 1>Hello there, Hello, Hello. It's me Josh, and this week's

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<v Speaker 1>s Y s K Select is a little episode from

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<v Speaker 1>two thousand twelve called Geysers Colon Nature's Innuendo. I thought

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<v Speaker 1>of that title myself, and I still love it to

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<v Speaker 1>this day, so I hope you enjoy it. It's one

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<v Speaker 1>of those really cool Earth sciences bio geochemical ones that

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<v Speaker 1>really get me jazzed, and I hope it gets you

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<v Speaker 1>jazz too. Let's all get jazz. Welcome to Stuff You

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<v Speaker 1>Should Know, a production of My Heart Radios How Stuff Works,

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<v Speaker 1>Good Bloom, and welcome to the podcast. I'm Josh Clark.

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<v Speaker 1>There's Charles W. Chuck Bryant, and uh, this is Stuff

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<v Speaker 1>you should Know. Yeah, just a couple of regular guys

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<v Speaker 1>are sitting around chat. That was good. I know, I

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<v Speaker 1>genuinely didn't think you were going to say, guys, really

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<v Speaker 1>a little um. This was a pretty cool article. I

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<v Speaker 1>thought I knew a lot about Geyser's, but I did

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<v Speaker 1>not know exactly what was going on there. Yeah. In fact,

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<v Speaker 1>I was wrong on a couple of key points. Oh really, yes,

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<v Speaker 1>which I will not point out. Oh come on, well,

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<v Speaker 1>I thought they spit out lemonade first of all. Uh,

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<v Speaker 1>and I thought there was a little guy down there

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<v Speaker 1>doing it. Oh got lepre cons Yeah, yeah, that's what

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<v Speaker 1>everybody thinks. I was wrong on both of those points.

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<v Speaker 1>Do we have a geyser myth sound effect? I don't

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<v Speaker 1>think so. Um does this count as weather? Now? This

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<v Speaker 1>is earth science, biogeochemical processes. Okay, I just know what

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<v Speaker 1>you're trying to be beef up our weather. Uh. This

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<v Speaker 1>is not whether it's not weather, although it does begin

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<v Speaker 1>with weather. Yeah, I mean when something precipitates, that's weather,

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<v Speaker 1>and precipitation precipitates the explosion of a geyser, that's right.

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<v Speaker 1>Uh chuck, Yes, I have no guys are introduction. Man,

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<v Speaker 1>you can't blame me though, Like I looked, and there

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<v Speaker 1>is really not a lot going on on geysers. I

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<v Speaker 1>thought you might tell the story about the people in

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<v Speaker 1>nineteen o three. He was going to, but I didn't

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<v Speaker 1>want to just usurp it. Okay, but let's do that though,

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<v Speaker 1>since you brought it up, Because I mean I thought

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<v Speaker 1>about that too, I was like, whoa hang back, Josh

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<v Speaker 1>hanging back? Well, apparently guysers can kill you. Um, and

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<v Speaker 1>you know when you see something like old faithful go off.

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<v Speaker 1>That's why you're three ft away watching it. Yeah, you

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<v Speaker 1>know you're not gonna be on top of the thing.

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<v Speaker 1>But apparently in nineteen o three in New Zealand, which

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<v Speaker 1>is allowsy with geysers, um, some tourists visiting there got

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<v Speaker 1>caught in a jet at uh wy man Wymani valley

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<v Speaker 1>nice good and uh it killed all four people and

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<v Speaker 1>carried them more than a mile away. Yes, that is sad.

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<v Speaker 1>And after after we explain how guysers work, I think

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<v Speaker 1>that will well we should mention that again because once

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<v Speaker 1>I understood how guysers worked and I read that, I

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<v Speaker 1>was like, those people met a terrible, terrible demise, like

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<v Speaker 1>they that was terrible way to go. Yeah, I mean,

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<v Speaker 1>it's tantamount to getting thrown into a volcano or caught

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<v Speaker 1>in dropping into the cracks of an earthquake, and they're

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<v Speaker 1>all kind of related, as it turns out, or being

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<v Speaker 1>blood into death, which is not related. No, but it's

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<v Speaker 1>pretty bad way to go to the geothermal earth properties.

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<v Speaker 1>So um chuck geysers, as I learned UM from reading

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<v Speaker 1>this article on how stuff works dot com um our

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<v Speaker 1>beloved site, UM, are actually kind of fragile and there's

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<v Speaker 1>not that many this this article, there's a thousand guysers

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<v Speaker 1>roughly in in the world. And um, I read elsewhere

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<v Speaker 1>that there's only about fifty geyser fields on the planet,

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<v Speaker 1>and about two thirds of those have five or fewer guysers,

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<v Speaker 1>which makes yellow Stone a pretty substantial repository of geyser

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<v Speaker 1>and guys are related activity. Because when you're talking guyser,

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<v Speaker 1>you you you don't ever just talk guys or you're

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<v Speaker 1>also talking um fumer roles. You're talking hot springs, mud pots,

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<v Speaker 1>steam vents, and all of them are based around the

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<v Speaker 1>same thing, which is there's some sort of geo thermal

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<v Speaker 1>activity that's relatively close to the Earth's surface, right, Um.

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<v Speaker 1>And there's three components to a geyser um and they

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<v Speaker 1>are water supply, plumbing system, and heat source. Yeah, and

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<v Speaker 1>I'm gonna argue with fourth later on later though, I

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<v Speaker 1>have to wait. I'm gonna call it. We'll just go

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<v Speaker 1>ahead and say what it is, which is a remoteness,

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<v Speaker 1>all right, and then we'll we'll circle back because detached

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<v Speaker 1>from its family, right, it comes very remote. So a

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<v Speaker 1>water supply, let's start there, because if you ain't got water,

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<v Speaker 1>you ain't got no guyser. Yeah, and I saw in

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<v Speaker 1>this article that um rivers can often um form the

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<v Speaker 1>water or supply. I didn't. I didn't see that elsewhere.

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<v Speaker 1>For the most part, from what I from what I

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<v Speaker 1>can gather is that the water supply is um precipitation,

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<v Speaker 1>rain and snow melt percolating through the Earth's crust over

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<v Speaker 1>five thousand or so years, and then it trickles down

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<v Speaker 1>to the point where it comes in contact with like

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<v Speaker 1>we said, relatively shallow geothermal activity, usually very very young

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<v Speaker 1>volcano volcano or volcanic activity, or very very old like

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<v Speaker 1>on in the throes of death volcanic activity. Yeah. Um,

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<v Speaker 1>and it can be anything from magma to um cool magma.

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<v Speaker 1>But it's very hot rock and it's close enough to

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<v Speaker 1>the surface that this water doesn't evaporate, it starts to

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<v Speaker 1>trickle back up. Yeah. And when do you say close?

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<v Speaker 1>Three miles down seems like a long way down. But

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<v Speaker 1>if you're talking the planet Earth, it's nothing. That's pretty close. Yeah,

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<v Speaker 1>if you're talking magma, it's pretty close. We're talking techtonic plates,

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<v Speaker 1>it's pretty close. It's closer than you on it to

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<v Speaker 1>be pale. It's a go ahead, okay, Number two of

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<v Speaker 1>the plumbing system, right, very important. Um. The plumbing system

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<v Speaker 1>is a series of fissures that run miles beneath the surface.

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<v Speaker 1>And one important aspect of these fissures is they're basically

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<v Speaker 1>sealed shut with silica from rhyolite. It's volcanic rock, um

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<v Speaker 1>and like these minerals have sealed this rock shut. Right, So,

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<v Speaker 1>like really important part of it. That water that's percolating down,

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<v Speaker 1>when it heats up and starts to travel back up,

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<v Speaker 1>it takes that silica that rhyolite with it, and then

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<v Speaker 1>it just kind of acts as a ceiling along these

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<v Speaker 1>pipes over five hundred thousand years, however long it takes

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<v Speaker 1>for it to go back up. It's it's ceiling and

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<v Speaker 1>it's making it water tight. Well yeah, and I imagine

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<v Speaker 1>I didn't read this, but I imagine that this kind

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<v Speaker 1>of activity happens elsewhere on the planet, but it's not

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<v Speaker 1>sealed up, so it just disperses, right. Yeah. Because one

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<v Speaker 1>of the key ingredients of a guy's or is pressure,

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<v Speaker 1>high pressure, that's right. And to get that pressure in

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<v Speaker 1>these pipes, you have to have ryolite coated sealed pipes.

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<v Speaker 1>That's right. Okay, so there's the plumbing system and it

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<v Speaker 1>can the plumbing system varies. All guysers are different. Sometimes

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<v Speaker 1>it's just like a huge, long vertical chaft. Sometimes it

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<v Speaker 1>binds and turns and winds around. Okay, so this is

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<v Speaker 1>this is something that actually differentiates guys are from a

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<v Speaker 1>hot spring. So a hot spring is just like a

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<v Speaker 1>like a long vertical chaft coming from hot water um

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<v Speaker 1>up to the top, but there's no obstruction. What makes

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<v Speaker 1>the guys or a geyser is the fact that there's

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<v Speaker 1>an obstruction in the plumbing right where the hot spring

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<v Speaker 1>water can just move freely up and down. There's there's

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<v Speaker 1>just free exchange and you soak around in it like

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<v Speaker 1>a big lazy wall rush. But there's no pressure. With

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<v Speaker 1>the guys are, there's some sort of obstruction where either say,

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<v Speaker 1>the water on its way back up and there's this

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<v Speaker 1>wide pool that bottlenecks at the top, so now you

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<v Speaker 1>have pressure. There's a bunch of different pipes feeding into

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<v Speaker 1>one pipe and they all connect to the same place

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<v Speaker 1>another bottleneck or this this pipe of water is so

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<v Speaker 1>wide and so deep that the pressure from the water

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<v Speaker 1>above the water at the bottom is so tremendous that

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<v Speaker 1>for all intensive purposes, it creates a bottleneck just strictly

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<v Speaker 1>out of pressure without an actual obstruction. Yeah. Just the

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<v Speaker 1>weight of the water itself is so great. So we

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<v Speaker 1>have a water supply and a plumbing um system that

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<v Speaker 1>is sealed with rhyolite which makes it water tight and pressurized,

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<v Speaker 1>and then some sort of means for pressure to build. Yeah,

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<v Speaker 1>and uh, I guess we can go ahead and liking

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<v Speaker 1>it to a pressure cooker now, so you understand we're

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<v Speaker 1>talking about if you've ever cooked with a pressure cooker

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<v Speaker 1>at home, or if you've ever eaten it Chick fil

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<v Speaker 1>A and eating their delicious pressure fried chicken. Is that

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<v Speaker 1>how they do it? Oh yeah, let's explain pressure. So

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<v Speaker 1>that's why there so juicy man um. So water is

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<v Speaker 1>standard water is just gonna boil it like a hundred

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<v Speaker 1>degrees celsius in the fancy French water. Um, if you're

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<v Speaker 1>if you're cooking with a pressure cooker, which means you know,

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<v Speaker 1>the littue sealed shut it lets out some steam or

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<v Speaker 1>else it would explode obviously, Um, it will actually take

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<v Speaker 1>a lot more energy to boil and bubble up, which

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<v Speaker 1>means more heat and so you can actually cook in

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<v Speaker 1>a pressure cooker at like twenty five degrees, right, because

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<v Speaker 1>it's just substantial for under that pressure. It takes a

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<v Speaker 1>lot more for what it was boiling water. But it's

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<v Speaker 1>like air bubbles forming and rising to the top. When

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<v Speaker 1>the pressure is too great, it can't boil. So the

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<v Speaker 1>boiling point rises, right, Well, it boils, but it won't

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<v Speaker 1>it can't evaporate. Well, no, it can't. It can't form

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<v Speaker 1>the bubbles that carry to the top, so it can't

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<v Speaker 1>actually boil. So it's just sitting there in this high

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<v Speaker 1>pressure environment at high higher than boiling point temperatures, and

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<v Speaker 1>the same things going on in a geyser. Right, You've

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<v Speaker 1>got the obstruction, you've got this heated water, and you

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<v Speaker 1>have a tremendous amount of pressure because again we're talking

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<v Speaker 1>about miles deep, um, and there's that's quite a bit

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<v Speaker 1>of pressure at the bottom the water at the bottom,

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<v Speaker 1>and it's getting hotter and hotter and hotter. Yeah, like, um,

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<v Speaker 1>I mean, I guess it depends. But for guys are

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<v Speaker 1>to form and start, they think the oldest one is

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<v Speaker 1>between five thousand and forty years old. So yeah, so

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<v Speaker 1>it takes a little while because you know, the plumbing

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<v Speaker 1>has to has to steal up and everything. But as

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<v Speaker 1>that pressure builds and then that heat um increases, you

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<v Speaker 1>can reach temperatures of like four or five degrees fahrenheit

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<v Speaker 1>of this water and it's still not boiling, right, that's right.

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<v Speaker 1>And then eventually it does boil. It overcomes that pressure threshold. Well,

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<v Speaker 1>it finds its way through to to the escape route,

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<v Speaker 1>which is the top of the surface, and it'll just

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<v Speaker 1>and that's not the eruption, it'll just scored a little

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<v Speaker 1>bit of water out. You'll go and think, wow, that

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<v Speaker 1>was a big relief, and such a big relief that, uh,

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<v Speaker 1>the steam all of a sudden expands to fundred times

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<v Speaker 1>the volume of the water. It's like if you're ever boiling,

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<v Speaker 1>uh you ever steam vegetables in your house. The best

0:11:10.720 --> 0:11:12.760
<v Speaker 1>way to steam vegetables is you don't just set it

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<v Speaker 1>on a massive boil and cover it up. You get

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<v Speaker 1>it to that massive boil and then you turn that

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<v Speaker 1>heat down low, and all of a sudden, that pressure

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<v Speaker 1>drop creates like massive amounts of steam. Right. And the

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<v Speaker 1>reason why is because when you increase pressure, you increase

0:11:27.040 --> 0:11:30.320
<v Speaker 1>the temperature. That's the boiling point of water. If suddenly

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<v Speaker 1>you have that temperature still, but the pressure decreases that

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<v Speaker 1>that water and this guys are just flash vaporizes. And

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<v Speaker 1>because there's a lot more volume to an equal amount

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<v Speaker 1>of water and steam, that steam, like you said, expands

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<v Speaker 1>to what times of volume? Yeah, and there's your guys

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<v Speaker 1>are how Yeah, it's that's all of a sudden, all

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<v Speaker 1>the steam in the water just gets shot out. Depending

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<v Speaker 1>on what kind of guys are it is, it's going

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<v Speaker 1>to take different formations and be different heights and last

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<v Speaker 1>different amounts of time. But um, it'll keep going until

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<v Speaker 1>it either runs out of water or it cools down

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<v Speaker 1>enough for it just start all over again. Yeah, and

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<v Speaker 1>then it just starts all over again, which is how

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<v Speaker 1>you get something like Old Faithful. All right, that's right.

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<v Speaker 1>Once it once it releases that um that pressure and

0:12:39.840 --> 0:12:42.800
<v Speaker 1>it shoots out, it's the whole process just begins again,

0:12:43.320 --> 0:12:46.440
<v Speaker 1>and you have, um, guys are's like Old Faithful that

0:12:46.880 --> 0:12:49.160
<v Speaker 1>erupt like on a pretty regular schedule. I think it's

0:12:49.200 --> 0:12:52.600
<v Speaker 1>between like sixty and eighty five minutes or something like that. Well,

0:12:52.640 --> 0:12:56.440
<v Speaker 1>I've got the new schedule schedule because it's been it's

0:12:56.440 --> 0:13:00.960
<v Speaker 1>been happening with greater with less frequency in greater power

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<v Speaker 1>in recent years, I think it's said since two thousand

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<v Speaker 1>UM and it's a bimodal. They call it bimodal. And

0:13:08.000 --> 0:13:11.880
<v Speaker 1>if you're going to Old Faithful in Wyoming, Um there

0:13:11.880 --> 0:13:14.960
<v Speaker 1>are generally two eruption durations now, either a long one

0:13:15.320 --> 0:13:17.880
<v Speaker 1>which is over four minutes, or a short one, which

0:13:17.880 --> 0:13:20.240
<v Speaker 1>is about two and a half minutes. And if you

0:13:20.440 --> 0:13:23.120
<v Speaker 1>have just missed the short one, there'll be about an

0:13:23.120 --> 0:13:26.720
<v Speaker 1>hour before your next eruption. If you have just missed

0:13:26.760 --> 0:13:29.040
<v Speaker 1>the long one, then there's gonna be about an hour

0:13:29.080 --> 0:13:31.200
<v Speaker 1>and a half until the next one. But either way,

0:13:31.240 --> 0:13:33.839
<v Speaker 1>it's it's worth sticking around for it. Yeah, And it's

0:13:33.880 --> 0:13:36.640
<v Speaker 1>funny if you go to the page and there's obviously

0:13:36.640 --> 0:13:38.319
<v Speaker 1>a webcam up where you can see it and stuff,

0:13:38.320 --> 0:13:40.160
<v Speaker 1>but that's not as fun. But if you go to

0:13:40.200 --> 0:13:42.160
<v Speaker 1>the web page and they ask for tips on you know,

0:13:42.360 --> 0:13:45.400
<v Speaker 1>seeing it, they say, well, if there's a lot of

0:13:45.400 --> 0:13:48.600
<v Speaker 1>people sitting around on the benches, that means there's one upcoming.

0:13:49.160 --> 0:13:50.920
<v Speaker 1>If there's a bunch of people getting up and leaving,

0:13:51.000 --> 0:13:53.800
<v Speaker 1>that means it just happened. It's like, wow, really, yeah,

0:13:54.000 --> 0:13:56.600
<v Speaker 1>that's the best you can do. That sounds like um,

0:13:56.800 --> 0:14:01.720
<v Speaker 1>like hippie park ranger logic exactly like um. Okay, so,

0:14:01.880 --> 0:14:05.320
<v Speaker 1>uh well, I guess we're onto like famous geysers, right, yeah,

0:14:05.400 --> 0:14:08.760
<v Speaker 1>Actually quickly I mentioned I teased about the fourth um

0:14:08.840 --> 0:14:14.000
<v Speaker 1>thing remoteness. Apparently, in the last fifty years, uh, producing

0:14:14.120 --> 0:14:18.880
<v Speaker 1>energy with geo thermal energy production has increased so much

0:14:19.240 --> 0:14:22.880
<v Speaker 1>that it's affecting geysers, and so being remote is now

0:14:23.520 --> 0:14:25.800
<v Speaker 1>believed to be one of the requirements to be a geyser,

0:14:25.880 --> 0:14:29.160
<v Speaker 1>because geysers are vanishing because of man. Because so I

0:14:29.200 --> 0:14:31.600
<v Speaker 1>was trying to figure out this out, maybe you can

0:14:31.640 --> 0:14:36.080
<v Speaker 1>help me. That's because we dig down to these this

0:14:36.080 --> 0:14:39.960
<v Speaker 1>this um, these geysers of this geo thermal activity, and

0:14:39.960 --> 0:14:42.760
<v Speaker 1>in doing so, are we creating like a release valve

0:14:43.280 --> 0:14:45.520
<v Speaker 1>so the pressure camp build as much I think so.

0:14:45.560 --> 0:14:48.920
<v Speaker 1>I mean they're using it to spind turbines to create energy.

0:14:48.960 --> 0:14:50.600
<v Speaker 1>But I know you can also have like a geo

0:14:50.640 --> 0:14:54.800
<v Speaker 1>thermal system in your backyard, which I don't think uses

0:14:54.840 --> 0:14:57.000
<v Speaker 1>I don't think it like creates steam. So I feel

0:14:57.000 --> 0:14:59.840
<v Speaker 1>like what we're doing then is creating artificial geysers, like

0:15:00.040 --> 0:15:02.880
<v Speaker 1>eating an artificial pipe to let steam out, which would

0:15:03.040 --> 0:15:06.840
<v Speaker 1>impact any natural guys activity. I because like we said,

0:15:06.840 --> 0:15:11.600
<v Speaker 1>they're very fragile. Earthquakes frequently um cut them off. They

0:15:11.640 --> 0:15:13.880
<v Speaker 1>also bring them back to life too. Yeah, that's true.

0:15:14.040 --> 0:15:18.760
<v Speaker 1>Like there was one called the Stroker Geyser that that

0:15:18.960 --> 0:15:21.640
<v Speaker 1>would be str o k K you are, yeah, and

0:15:21.680 --> 0:15:25.040
<v Speaker 1>that's stroker like stroker race right right. So Stroker geyser

0:15:25.280 --> 0:15:28.800
<v Speaker 1>um is after the Icelandic well, Stroker is after the

0:15:28.840 --> 0:15:32.880
<v Speaker 1>Icelandic verb to churn, and actually geyser's after the Icelandic

0:15:32.960 --> 0:15:37.920
<v Speaker 1>verb um to gush. So this is all very Icelandic

0:15:37.960 --> 0:15:40.560
<v Speaker 1>in origin. But that would be g e y s

0:15:40.600 --> 0:15:46.240
<v Speaker 1>i R geyser okay in Icelandic. Sure, I own how

0:15:46.280 --> 0:15:50.160
<v Speaker 1>Buyork pronounces guyser. Have you seen Kristen Wiggs impression of her?

0:15:50.240 --> 0:15:54.200
<v Speaker 1>Huh that's really great? Um okay, So the Stroker Geyser

0:15:54.320 --> 0:16:00.440
<v Speaker 1>was actually um it was enacted in nine um because

0:16:00.480 --> 0:16:05.240
<v Speaker 1>of an earthquake, and then another earthquake hit in and

0:16:05.280 --> 0:16:08.680
<v Speaker 1>it became inactive. It went dormant and the local said,

0:16:09.040 --> 0:16:10.760
<v Speaker 1>we got to get our guys are back, man, it's

0:16:10.760 --> 0:16:13.040
<v Speaker 1>all blocked up. So they cleared it off and now

0:16:13.120 --> 0:16:16.080
<v Speaker 1>it's running again. I bet that was probably dangerous work

0:16:16.520 --> 0:16:21.520
<v Speaker 1>dangerous um. Another way to that humans are impacting is

0:16:21.560 --> 0:16:26.160
<v Speaker 1>a mineral extraction. Apparently in two thousand three, Uh, they

0:16:26.160 --> 0:16:31.880
<v Speaker 1>were extracting minerals in Chile, the second largest geyser field

0:16:32.280 --> 0:16:37.120
<v Speaker 1>in South America, and it killed it basically from extracting

0:16:37.120 --> 0:16:41.560
<v Speaker 1>golden stuff. Because basically they mess with the plumbing and

0:16:41.600 --> 0:16:44.280
<v Speaker 1>then you're finished. Because it's like you said, like, um,

0:16:44.600 --> 0:16:46.960
<v Speaker 1>in a pressure cooker has that little steam val so

0:16:47.080 --> 0:16:51.080
<v Speaker 1>it doesn't explode. The guys aren't supposed to have that, right.

0:16:51.120 --> 0:16:53.560
<v Speaker 1>If they have that, they just don't go off. They're like, well, fine,

0:16:53.560 --> 0:16:57.880
<v Speaker 1>I'll just let some steam off and um, um, that

0:16:57.960 --> 0:17:02.000
<v Speaker 1>does happen. Naturally, there are steam it's located near geysers.

0:17:02.680 --> 0:17:05.720
<v Speaker 1>Um like yellow stones. Like we have ten thousand um

0:17:05.920 --> 0:17:11.040
<v Speaker 1>geo thermal um what is the word they use, Uh,

0:17:11.280 --> 0:17:14.560
<v Speaker 1>basically different things. We have ten thousands of your thermal

0:17:14.600 --> 0:17:17.600
<v Speaker 1>different things. Um. But the vast majority of those are

0:17:17.640 --> 0:17:21.560
<v Speaker 1>like steam vents. Oh they're man made. No, they're they're natural. Like. Oh,

0:17:21.800 --> 0:17:25.640
<v Speaker 1>they're like little steam releases that come up through fissures.

0:17:25.960 --> 0:17:27.680
<v Speaker 1>Okay in the earth. I thought you meant we put

0:17:27.720 --> 0:17:29.960
<v Speaker 1>those in to make old faithful like safers. No, they

0:17:30.000 --> 0:17:33.200
<v Speaker 1>happen naturally. Um, but I think it's the same thing

0:17:33.240 --> 0:17:36.560
<v Speaker 1>as drilling a hole down to a geothermal um different

0:17:36.560 --> 0:17:40.880
<v Speaker 1>thing and uh and tapping it to run a turbine. Okay,

0:17:42.240 --> 0:17:45.960
<v Speaker 1>at least you didn't say interesting. Interesting, man, this stuff

0:17:46.000 --> 0:17:49.800
<v Speaker 1>is very interesting. Um, old Faithful is a cone geyser?

0:17:50.480 --> 0:17:52.159
<v Speaker 1>I'm not sure I understand the difference? Is it the

0:17:52.320 --> 0:17:55.239
<v Speaker 1>is it the good difference? Is it the outlet like

0:17:55.320 --> 0:17:57.479
<v Speaker 1>the shape of the thing above the earth. Yeah, So

0:17:57.600 --> 0:17:59.920
<v Speaker 1>with the cone guys or, the rhyolite bubbles up and

0:18:00.040 --> 0:18:02.879
<v Speaker 1>enough over time that it builds up and it forms

0:18:02.880 --> 0:18:04.760
<v Speaker 1>a little cone and that's what the guys are shoots

0:18:04.760 --> 0:18:06.600
<v Speaker 1>out of. And normally with the cone guys or you

0:18:06.640 --> 0:18:10.280
<v Speaker 1>have a big stream going jet going into the air

0:18:10.400 --> 0:18:14.320
<v Speaker 1>like hundreds of feet. That one in um in uh

0:18:14.520 --> 0:18:19.720
<v Speaker 1>New Zealand, the Wyman ge geyser. Um, that one streamed

0:18:20.720 --> 0:18:22.960
<v Speaker 1>seventy ft into the air and for those of you

0:18:23.000 --> 0:18:27.960
<v Speaker 1>in New Zealand, that's four hundred fifty that's a world record, right, yeah,

0:18:28.160 --> 0:18:31.960
<v Speaker 1>nineteen oh two, Yeah, before it killed people, right, and

0:18:32.000 --> 0:18:34.600
<v Speaker 1>then it went dormant in nineteen o four because of

0:18:34.640 --> 0:18:37.720
<v Speaker 1>a landslide, which makes me think like this thing's coming back.

0:18:38.119 --> 0:18:40.879
<v Speaker 1>I just gotta bubble back up and then shut down

0:18:41.000 --> 0:18:45.359
<v Speaker 1>right afterwards. Yeah, it's really had a really chaotic to

0:18:45.560 --> 0:18:47.960
<v Speaker 1>your career. It's like a rock star that overdosed on

0:18:48.040 --> 0:18:52.119
<v Speaker 1>heroin or something. Um. But anyway, as I was saying, um,

0:18:52.320 --> 0:18:57.160
<v Speaker 1>the cone shoots a jet into the air. The fountain, Um,

0:18:57.280 --> 0:18:59.919
<v Speaker 1>it shoots in a much more like chaotic streme whatever.

0:19:00.240 --> 0:19:01.680
<v Speaker 1>But it doesn't come up from a cone. It comes

0:19:01.720 --> 0:19:05.360
<v Speaker 1>up from a pool. So at the surface, the geyser

0:19:05.560 --> 0:19:09.280
<v Speaker 1>goes into a pool of water and then that will

0:19:09.440 --> 0:19:11.760
<v Speaker 1>erupt out of the water, and that would be the

0:19:11.800 --> 0:19:16.560
<v Speaker 1>grand geyser. Um, the tall that's the tallest regularly erupting

0:19:16.560 --> 0:19:19.240
<v Speaker 1>guys are on the planet. And that is also a yellowstone. Yeah,

0:19:19.240 --> 0:19:21.840
<v Speaker 1>the tallest in that it shoots up in the air. Yeah,

0:19:21.880 --> 0:19:27.520
<v Speaker 1>two hundred feet in crazy fountain e hard to predict fashion. Yeah,

0:19:27.560 --> 0:19:30.639
<v Speaker 1>which is pretty surprising too, because the cone geyser shoots

0:19:30.640 --> 0:19:33.520
<v Speaker 1>a jet straight up in the air, and this fountain

0:19:33.560 --> 0:19:36.560
<v Speaker 1>geyser is still beating the average one. Yeah. Could you

0:19:36.560 --> 0:19:38.800
<v Speaker 1>imagine if it was a cone geyser, it would be

0:19:39.080 --> 0:19:43.200
<v Speaker 1>mind blowing to the moon. Uh. You mentioned the stroker

0:19:43.280 --> 0:19:47.800
<v Speaker 1>ace geyser the steamboat guys are. Yeah, apparently can choo

0:19:47.800 --> 0:19:51.280
<v Speaker 1>water up to three hundred feet, but don't bother stopping

0:19:51.280 --> 0:19:54.680
<v Speaker 1>by because it hasn't happened for fifty years. It can

0:19:54.680 --> 0:19:58.359
<v Speaker 1>go fifty years between. It's finicky. Yeah. Um there's also

0:19:58.440 --> 0:20:02.920
<v Speaker 1>the geyser. We to the o G geyser because that's

0:20:02.920 --> 0:20:05.480
<v Speaker 1>where the word came from. It's a geyser in Iceland.

0:20:05.840 --> 0:20:10.400
<v Speaker 1>It was discovered in um so it's the oldest known

0:20:10.440 --> 0:20:12.800
<v Speaker 1>guys are on the planet. But they took some samples

0:20:12.800 --> 0:20:15.879
<v Speaker 1>of the silica that forms the cone of the castle

0:20:15.920 --> 0:20:18.439
<v Speaker 1>guys are in Yellowstone. That's the one they think is

0:20:18.760 --> 0:20:22.680
<v Speaker 1>five thousand to forty thousand years old. Apparently silicon dating

0:20:24.000 --> 0:20:28.040
<v Speaker 1>can use some work. I did see one interesting little

0:20:28.080 --> 0:20:31.320
<v Speaker 1>and it wasn't a joke. It was almost like you

0:20:31.359 --> 0:20:34.680
<v Speaker 1>could hear science guys laughing about it. Though. You geysers

0:20:34.680 --> 0:20:39.359
<v Speaker 1>are always called geysers, even if they quit erupting, but

0:20:39.600 --> 0:20:42.399
<v Speaker 1>that ceased to make seats to be a geyser at

0:20:42.440 --> 0:20:45.440
<v Speaker 1>that point. But once you have erupted, you're always called

0:20:45.480 --> 0:20:49.600
<v Speaker 1>a geyser. The cone formerly known as geyser. Yeah, that's

0:20:49.600 --> 0:21:16.560
<v Speaker 1>what I would call it. Shameful, uh, let's do you

0:21:16.600 --> 0:21:20.760
<v Speaker 1>know that whole story about Prince doing that about changing

0:21:20.760 --> 0:21:23.280
<v Speaker 1>his name. No, I never knew the story behind it.

0:21:23.440 --> 0:21:25.760
<v Speaker 1>So he was locked in a contract with Sony that

0:21:25.800 --> 0:21:30.080
<v Speaker 1>he didn't like, and Sony basically said, you can't release

0:21:30.119 --> 0:21:33.840
<v Speaker 1>an album as Prince. Yes. And but also that had

0:21:33.880 --> 0:21:36.800
<v Speaker 1>something to do with him acting basically crazy, like he

0:21:36.880 --> 0:21:39.119
<v Speaker 1>acted crazy on purpose to get out of his contract

0:21:39.119 --> 0:21:41.000
<v Speaker 1>because there was some sort of clause where like if

0:21:41.000 --> 0:21:43.400
<v Speaker 1>he was if he went nuts or whatever, it would

0:21:43.400 --> 0:21:45.679
<v Speaker 1>avoid his contract. So he did that, and he had

0:21:45.720 --> 0:21:48.399
<v Speaker 1>that font release and I remember he released it to

0:21:48.480 --> 0:21:52.080
<v Speaker 1>the media like, um, his little symbol yes to as

0:21:52.119 --> 0:21:55.040
<v Speaker 1>like a font add on so you could just print

0:21:55.040 --> 0:21:57.959
<v Speaker 1>the symbol when you were writing about him. And his

0:21:58.080 --> 0:22:00.959
<v Speaker 1>contract with Sony was either avoided they gave it up

0:22:01.040 --> 0:22:03.199
<v Speaker 1>or whatever. But he was basically like, I'll show you

0:22:03.280 --> 0:22:06.320
<v Speaker 1>crazy if I need to get out of this contract. Boy.

0:22:06.359 --> 0:22:09.040
<v Speaker 1>One of the best concerts I've ever seen. Oh yeah,

0:22:09.040 --> 0:22:10.800
<v Speaker 1>I'll bet. And I don't even think I put it

0:22:10.800 --> 0:22:13.040
<v Speaker 1>in my top five when we had that listener mail

0:22:13.080 --> 0:22:16.160
<v Speaker 1>that time, but probably forgot. It's probably in my top five.

0:22:16.359 --> 0:22:18.719
<v Speaker 1>I would like to see print sometimes he brings it

0:22:19.040 --> 0:22:21.399
<v Speaker 1>he um, he bought you me a bottle of water

0:22:21.560 --> 0:22:24.000
<v Speaker 1>at um a Miles Davis show at the Cotton Club.

0:22:24.440 --> 0:22:27.280
<v Speaker 1>Really wow. Her friends came up to see the lemon

0:22:27.280 --> 0:22:29.080
<v Speaker 1>Heads and she's like, yeah, I'll go with you, and

0:22:29.080 --> 0:22:31.119
<v Speaker 1>then found out that Miles Davis was playing. It's like,

0:22:31.160 --> 0:22:36.360
<v Speaker 1>I'm gonna go over here, bottle of water, Evan Dando,

0:22:36.680 --> 0:22:39.879
<v Speaker 1>Miles Davis exactly. Let me think about that. Sorry, e

0:22:40.040 --> 0:22:46.480
<v Speaker 1>d um So that's uh, that's print. Oh yeah, and guys,

0:22:46.840 --> 0:22:48.720
<v Speaker 1>oh yeah, guys are too. Um. If you want to

0:22:48.760 --> 0:22:50.920
<v Speaker 1>learn more about guysers, you can type that word g

0:22:51.080 --> 0:22:53.640
<v Speaker 1>E Y S E r S. That's the English spelling.

0:22:54.160 --> 0:22:56.639
<v Speaker 1>We didn't do it icelandically. Um, but you type that

0:22:56.680 --> 0:22:58.840
<v Speaker 1>in the search bar at how stuff Works dot com

0:22:58.920 --> 0:23:01.560
<v Speaker 1>and it will bring up this fine, fine article. And

0:23:01.680 --> 0:23:04.200
<v Speaker 1>I said search part host of works dot com, which

0:23:04.280 --> 0:23:09.119
<v Speaker 1>means it's time for listener mail. All right, Josh, I'm

0:23:09.119 --> 0:23:13.280
<v Speaker 1>gonna call this, uh given a local Brooklyn night, a

0:23:13.320 --> 0:23:17.480
<v Speaker 1>plug for his election. But that's not how it started. Okay,

0:23:18.000 --> 0:23:20.840
<v Speaker 1>that's kind of a complicated title. Um, guys who just

0:23:20.880 --> 0:23:22.960
<v Speaker 1>listen to your podcast How Labor Unions Work, And I

0:23:22.960 --> 0:23:25.000
<v Speaker 1>want to thank you for trying to give a very balanced,

0:23:25.800 --> 0:23:29.400
<v Speaker 1>uh story to what is a very complicated and contentious subject.

0:23:29.840 --> 0:23:32.840
<v Speaker 1>As a former New York City union organizer, so this

0:23:32.880 --> 0:23:35.560
<v Speaker 1>guy was the real deal. I am very familiar with

0:23:35.600 --> 0:23:38.440
<v Speaker 1>the arguments against unions, but I truly believe American workers

0:23:38.760 --> 0:23:41.399
<v Speaker 1>in the American economy are better off with unions and

0:23:41.520 --> 0:23:46.679
<v Speaker 1>without when unions are strong. Typical union organizing when unions

0:23:46.680 --> 0:23:49.720
<v Speaker 1>are strong, there is some counterpoint to this total acceptance

0:23:50.080 --> 0:23:52.960
<v Speaker 1>of rampant greed that was essentially the cause of the

0:23:53.000 --> 0:23:55.600
<v Speaker 1>financial meltdown in two thousand and eight. At this point,

0:23:55.600 --> 0:23:58.000
<v Speaker 1>with unions at their weakest and a half century, we

0:23:58.119 --> 0:24:01.879
<v Speaker 1>average Americans are being held hostage by operations. This is

0:24:01.920 --> 0:24:04.439
<v Speaker 1>what he says. Um, I have to say. In my

0:24:04.560 --> 0:24:06.959
<v Speaker 1>line of work, violence was not the norm, but intimidation

0:24:07.000 --> 0:24:10.720
<v Speaker 1>by the employer was constant. They did everything from threatening

0:24:10.720 --> 0:24:13.400
<v Speaker 1>workers with being fired, lying to them and telling them

0:24:13.400 --> 0:24:17.440
<v Speaker 1>they did not have collective bargaining rights, to telling them

0:24:17.440 --> 0:24:22.240
<v Speaker 1>the union would only steal their dues and not get

0:24:22.320 --> 0:24:27.720
<v Speaker 1>them a good contract. The deceptive HR person right there. Yeah.

0:24:27.840 --> 0:24:30.160
<v Speaker 1>Or they would tell workers, um, they would work out

0:24:30.200 --> 0:24:33.119
<v Speaker 1>individual deals with them if they would vote against the union,

0:24:33.800 --> 0:24:37.720
<v Speaker 1>like trying to Yeah, that's pretty pretty, Harry. Even once

0:24:37.760 --> 0:24:40.720
<v Speaker 1>when we were organizing at a Catholic hospital, they told

0:24:40.720 --> 0:24:43.440
<v Speaker 1>the workers they were going against God if they tried

0:24:43.440 --> 0:24:45.919
<v Speaker 1>to organize. Yeah, can you see like those priests like

0:24:46.359 --> 0:24:50.040
<v Speaker 1>union breaking cracking heads with metal baton. The only problem

0:24:50.040 --> 0:24:52.560
<v Speaker 1>I had with your podcast was the lack of coverage

0:24:52.600 --> 0:24:56.240
<v Speaker 1>you gave to the triangle shirtwaist fire. We mentioned that.

0:24:56.520 --> 0:24:58.440
<v Speaker 1>He said it could have been none more. He said

0:24:58.440 --> 0:25:01.479
<v Speaker 1>it could deserve its own podcast. Well, that's true, we

0:25:01.520 --> 0:25:04.320
<v Speaker 1>mentioned it. He said it was one of the deadliest

0:25:04.440 --> 0:25:08.159
<v Speaker 1>industrial accidents in the United States history. Last year, hundreds

0:25:08.160 --> 0:25:10.679
<v Speaker 1>of people came out to commemorate the one year anniversary

0:25:10.960 --> 0:25:13.960
<v Speaker 1>remember of the lives lost due to lock stairwells and

0:25:14.000 --> 0:25:16.600
<v Speaker 1>exits that fire was a major turning point in labor

0:25:16.640 --> 0:25:19.480
<v Speaker 1>conditions in New York City and around the world, as

0:25:19.520 --> 0:25:24.240
<v Speaker 1>well as bringing light to women's terrible working conditions. And

0:25:24.400 --> 0:25:27.600
<v Speaker 1>I wrote him back, and it turns out, uh A

0:25:27.720 --> 0:25:30.879
<v Speaker 1>day e d is his name. Fox is running for

0:25:30.960 --> 0:25:33.960
<v Speaker 1>Brooklyn City Council. I said, you know what, dude, we'll

0:25:33.960 --> 0:25:39.159
<v Speaker 1>plug your campaign. Uh www dot e d E f

0:25:39.359 --> 0:25:43.239
<v Speaker 1>o X dot com, ad a fox dot com and

0:25:43.359 --> 0:25:46.760
<v Speaker 1>good luck in your bid. For city council in Brooklyn. Yeah,

0:25:46.800 --> 0:25:50.720
<v Speaker 1>if you wear um sunglasses with Neon arms on them

0:25:50.760 --> 0:25:53.200
<v Speaker 1>and into like your pro union, I would say, God,

0:25:53.240 --> 0:25:55.199
<v Speaker 1>vote for this. I think we can help garner you

0:25:55.480 --> 0:25:58.280
<v Speaker 1>a little bit of the hipster vote maybe, since we

0:25:58.280 --> 0:26:01.639
<v Speaker 1>are both aging hipsters. I not a hipster, dude, I

0:26:01.680 --> 0:26:05.000
<v Speaker 1>am not a hipster, and I've maybe aging, but I'm

0:26:05.000 --> 0:26:07.399
<v Speaker 1>not a hipster. Well you look a lot more like

0:26:07.440 --> 0:26:10.520
<v Speaker 1>a hipster than you used to. Well if you, uh,

0:26:10.640 --> 0:26:13.640
<v Speaker 1>I guess if you have a political campaign you're running, Um,

0:26:13.720 --> 0:26:15.520
<v Speaker 1>we want to hear about it. We heard from another

0:26:15.600 --> 0:26:20.399
<v Speaker 1>guy um in uh was it in Maryland, a state legislator.

0:26:20.440 --> 0:26:23.480
<v Speaker 1>He's a he's a legislator for Maryland who was writing

0:26:23.480 --> 0:26:26.160
<v Speaker 1>about human trafficking. That's right. Shout out to that guy

0:26:26.200 --> 0:26:29.399
<v Speaker 1>as well. Um, but if you are a politician that

0:26:29.440 --> 0:26:31.200
<v Speaker 1>listens to stuff, you should know we want to hear

0:26:31.240 --> 0:26:34.040
<v Speaker 1>your viewpoints. Let us know what you gotta say, how

0:26:34.080 --> 0:26:36.120
<v Speaker 1>we're helping you, how we can help more that kind

0:26:36.160 --> 0:26:38.800
<v Speaker 1>of thing, you know. Um, you can tweet to us,

0:26:39.080 --> 0:26:41.240
<v Speaker 1>just please don't send us a picture of your junk

0:26:41.320 --> 0:26:45.119
<v Speaker 1>like other politicians. UM to s y s K podcast.

0:26:45.600 --> 0:26:48.480
<v Speaker 1>You can join us on Facebook, dot com, slash stuff

0:26:48.520 --> 0:26:51.800
<v Speaker 1>you Should Know, and you can send us an email

0:26:52.280 --> 0:26:59.000
<v Speaker 1>to stuff podcast at how stuff works dot com. Stuff

0:26:59.040 --> 0:27:00.960
<v Speaker 1>you Should Know is a production of iHeart Radio's How

0:27:01.000 --> 0:27:03.760
<v Speaker 1>Stuff Works. For more podcasts for my heart Radio, visit

0:27:03.760 --> 0:27:06.480
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<v Speaker 1>to your favorite shows. H