WEBVTT - Geysers: Nature's Innuendo

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<v Speaker 1>Brought to you by the reinvented two thousand twelve Camray.

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<v Speaker 1>It's ready. Are you welcome to Stuff you Should Know?

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<v Speaker 1>From House Stuff Works dot com bloom and welcome to

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<v Speaker 1>the podcast. I'm Josh Clark, There's Charles W. Chuck Bryant,

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<v Speaker 1>and uh, this is stuff you should know. Yeah, just

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<v Speaker 1>a couple of regular guys are sitting around. Check. That

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<v Speaker 1>was good. I know. I genuinely didn't think you were

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<v Speaker 1>going to say Geyser's really a little This was a

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<v Speaker 1>pretty cool article. I thought I knew a lot about Geyser's,

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<v Speaker 1>but I did not know exactly what was going on there. Yeah.

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<v Speaker 1>In fact, I was wrong on a couple of key points.

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<v Speaker 1>Oh really, yes, which I will not point out. Oh

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<v Speaker 1>come on, well, I thought they'd split out lemonade first

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<v Speaker 1>of all. Uh, and I thought that was a little

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<v Speaker 1>guy on there doing it. Oh got lepers Yeah, that's

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<v Speaker 1>what everybody thinks. I was wrong on both of those points.

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<v Speaker 1>Do we have a guyser 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 you're

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<v Speaker 1>trying to be beef up our weather. H this is

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<v Speaker 1>not weather. It's not weather, although it does begin with weather. Yeah,

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<v Speaker 1>I mean when something precipitates, that's weather, and precipitation precipitates

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<v Speaker 1>the explosion of a geyser. That's right. Uh, Chuck, I

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<v Speaker 1>have no guyser introduction. Man, you can't blame me. Though,

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<v Speaker 1>Like I looked, and there is really not a lot

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<v Speaker 1>going on on guysers. I thought you might tell the

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<v Speaker 1>story about the people in nineteen three years that's going

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<v Speaker 1>to but I didn't want to just usurp it. Okay,

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<v Speaker 1>but let's do that though, since you brought it up,

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<v Speaker 1>because I mean I thought about that, I was like,

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<v Speaker 1>whoa hang back, Josh hanging back? Well, apparently guysers can

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<v Speaker 1>kill you. Um. And you know when you see something

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<v Speaker 1>like old Faith will go off. That's why you're three

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<v Speaker 1>ft away watching it. Yeah, you know you're not gonna

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<v Speaker 1>be on top of the thing. But apparently nineteen three

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<v Speaker 1>in New Zealand, which is allowsy with geyser's um, some

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<v Speaker 1>tourists visiting there got caught in a jet at Uh

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<v Speaker 1>why man, why Mangu Valley nice? And uh? It killed

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<v Speaker 1>all four people and carried them more than a mile away. Yes,

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<v Speaker 1>that is sad, and after after we explain how geysers work,

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<v Speaker 1>I think that will well we should mention that again

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<v Speaker 1>because once I understood how guysers worked and I read that,

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<v Speaker 1>I was like, those people met a terrible, terrible demise,

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<v Speaker 1>like 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>bludgeoned to death, which is not related. No, but it's

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<v Speaker 1>pretty bad way to go to geothermal properties. So um chuck. Geysers,

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<v Speaker 1>as I learned from reading this article on how stuff

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<v Speaker 1>works dot com um our beloved site um, are actually

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<v Speaker 1>kind of fragile and there's not that many this this articles,

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<v Speaker 1>there's a thousand guysers roughly in in the world, and

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<v Speaker 1>um I read elsewhere that there's only about fifty guyser

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<v Speaker 1>fields on the planet and about two thirds of those

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<v Speaker 1>have five or fewer guysers, which makes yellow Stone a

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<v Speaker 1>pretty substantial repository of geyser and guys are related activity.

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<v Speaker 1>Because when you're talking guys are you you don't ever

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<v Speaker 1>just talk guys, or you're also talking um fumer roles.

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<v Speaker 1>You're talking hot springs, mud pots, steam vents, and all

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<v Speaker 1>of them are based around the same thing, which is

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<v Speaker 1>there's some sort of geo thermal activity that's relatively close

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<v Speaker 1>to the Earth's surface, right, um. And there's three components

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<v Speaker 1>to a geyser um and they are water supply, plumbing system,

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<v Speaker 1>and heat source. Yeah. And I'm gonna argue with forth

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<v Speaker 1>later on later though, I have to wait. I'm gonna

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<v Speaker 1>call it. We'll just go ahead and say what it is,

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<v Speaker 1>which is a remoteness, all right, and then we'll we'll

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<v Speaker 1>circle back because detached from its family, it comes very remote.

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<v Speaker 1>So a water supply, let's start there, because if you

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<v Speaker 1>ain't got water, you ain't got no geyser. Yeah. And

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<v Speaker 1>I saw in this article that um rivers can often

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<v Speaker 1>um form the water supply. I didn't. I didn't see

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<v Speaker 1>that elsewhere. For the most part, from what I from

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<v Speaker 1>what I can gather is that the water supply is

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<v Speaker 1>um precipitation, rain and snow melt percolating through the Earth's

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<v Speaker 1>crust over five thousand or so years, and then it

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<v Speaker 1>trickles down to the point where it comes in contact with,

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<v Speaker 1>like we said, relatively shallow geo thermal activity, usually very

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<v Speaker 1>very volcano volcano or volcanic activity, or very very old

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<v Speaker 1>like 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 stay close?

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<v Speaker 1>Three miles down it seems like a long way down,

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<v Speaker 1>but if you're talking the planet Earth, it's nothing. That's

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<v Speaker 1>pretty close. If you're talking magma, it's pretty close. We're

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<v Speaker 1>talking tectonic plates, it's pretty close. It's closer than you

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<v Speaker 1>want it to be. Pal, it's a go ahead, okay.

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<v Speaker 1>Number two the plumbing system, right, very important. Um. The

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<v Speaker 1>plumbing system is a series of fissures that run miles

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<v Speaker 1>beneath the surface. And one important aspect of these fissures

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<v Speaker 1>is they're basically sealed shut with silica from rhyolite. It's

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<v Speaker 1>volcanic rock. Um. And like these minerals have sealed this

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<v Speaker 1>rock shut, right, So like really important part of it,

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<v Speaker 1>that water that's percolating down. When it heats up and

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<v Speaker 1>starts to travel back up, it takes that silica that

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<v Speaker 1>riolite with it and then it just kind of acts

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<v Speaker 1>as a ceiling along these pipes. Over five hundred thousand years,

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<v Speaker 1>however long it takes for it to go back up,

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<v Speaker 1>it's it's ceiling and it's making it water tight. Well yeah,

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<v Speaker 1>and I imagine I didn't read this, but I imagine

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<v Speaker 1>that this kind of activity happens elsewhere on the planet,

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<v Speaker 1>but it's not sealed up, so it just disperses, right, Yeah,

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<v Speaker 1>Because one of the key ingredients of a geyser 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 rylelite 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 barries. 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>one like a long vertical shaft coming from hot water

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<v Speaker 1>um up to the top. But there's no obstruction. What

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<v Speaker 1>makes the guys or a geyser is the fact that

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<v Speaker 1>there's an obstruction in the plumbing right where the hot

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<v Speaker 1>spring water can just move freely up and down. There's

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<v Speaker 1>there's just free exchange and you soak around in it

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<v Speaker 1>like a big lazy wall rush, but there's no pressure

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<v Speaker 1>with the guys are there's some sort of obstruction where

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<v Speaker 1>either say, the water on its way back up and

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<v Speaker 1>there's this wide pool that bottlenecks at the top. So

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<v Speaker 1>now you have pressure. There's a bunch of different pipes

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<v Speaker 1>feeding into one pipe and they all connect to the

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<v Speaker 1>same place another bottleneck or this this pipe of water

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<v Speaker 1>is so wide and so deep that the pressure from

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<v Speaker 1>the water above the water at the bottom is so

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<v Speaker 1>tremendous that for all intensive purposes it creates a bottleneck

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<v Speaker 1>just strictly out of pressure without an actual obstruction. Yeah,

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<v Speaker 1>just the weight of the water itself is so great.

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<v Speaker 1>So we have a water supply and a plumbing um

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<v Speaker 1>system that is sealed with rhyolite which makes it water

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<v Speaker 1>tight and pressurized, and then some sort of means for

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<v Speaker 1>pressure to build. Yeah, and uh, I guess we can

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<v Speaker 1>go ahead and liking it to a pressure cooker. Now,

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<v Speaker 1>so you understand what we're talking about. If you've ever

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<v Speaker 1>cooked with a pressure cooker at home, or if you've

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<v Speaker 1>ever eaten it Chick fil A and eating their delicious

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<v Speaker 1>pressure fried chicken, is that how they do it? Oh? Yeah,

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<v Speaker 1>pressure fried? So that's whether so juicy. Um, So water

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<v Speaker 1>is standard water is just gonna boil it like a

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<v Speaker 1>hundred degrees celsius French water. Um. If you're if you're

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<v Speaker 1>cooking with a pressure cooker, which means you know, the

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<v Speaker 1>litt a 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 cooking a

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<v Speaker 1>pressure cooker at like twenty five degrees right, because it's

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<v Speaker 1>just substantial for under a pressure. It takes a lot

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<v Speaker 1>more for what it was boiling water. But it's like

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<v Speaker 1>air bubbles forming and rising to the top. When the

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<v Speaker 1>pressure is too great, it can't boil. So the boiling

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<v Speaker 1>point rises, right, Well, it boils, but it won't it

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<v Speaker 1>can't evaporate. Well, no, it can't. It can't form the

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<v Speaker 1>bubbles that carry to the top. So it can't actually boil.

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<v Speaker 1>So it's just sitting there in this high pressure environment

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<v Speaker 1>at high higher than boiling point temperatures and the same

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<v Speaker 1>things going on in the guyser. Right, You've got the obstruction,

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<v Speaker 1>you've got this heated water, and you have a tremendous

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<v Speaker 1>amount of pressure because again we're talking about miles deep

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<v Speaker 1>um and there's that's quite a bit of pressure at

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<v Speaker 1>the bottom the water at the bottom. It's getting hotter

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<v Speaker 1>and hotter and hotter. Yeah, like, um, I mean, I

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<v Speaker 1>guess it depends. But for guys are to form and start,

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<v Speaker 1>they think the oldest one is between five thousand and

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<v Speaker 1>forty years old. So yeah, so it takes a little

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<v Speaker 1>while because you know, the plumbing has to has to

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<v Speaker 1>steal up in every thing. But as that pressure builds

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<v Speaker 1>and then that heat um increases, you can reach temperatures

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<v Speaker 1>of like four or five degrees fahrenheit of this water

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<v Speaker 1>and it's still not boiling, right, that's right, And then

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<v Speaker 1>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 and it'll just squired a

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<v Speaker 1>little bit of water out and think, wow, that was

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<v Speaker 1>a big relief, and such a big relief that the

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<v Speaker 1>steam all of a sudden expands to times the volume

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<v Speaker 1>of the water. It's like if you're ever boiling, you

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<v Speaker 1>ever steam vegetables in your house, the best way to

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<v Speaker 1>steam vegetables is you don't just set it on a

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<v Speaker 1>massive boil and cover it up. You get it to

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<v Speaker 1>that massive boil and then you turn that heat down low,

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<v Speaker 1>and all of a sudden, that pressure drop creates like

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<v Speaker 1>massive amounts of steam, right. And the reason why is

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<v Speaker 1>because when you increase pressure, you increase the temperature that's

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<v Speaker 1>the boiling point of water. If suddenly you have that

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<v Speaker 1>temperature still but the pressure decreases, that that water and

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<v Speaker 1>this guys are just flash vaporizes. And because there's a

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<v Speaker 1>lot more volume to an equal amount of water and steam,

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<v Speaker 1>that steam, like you said, expands to what times the

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<v Speaker 1>volume And there's your guys are pal Yeah, it's that's

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<v Speaker 1>all of a sudden, all the steam in the water

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<v Speaker 1>just gets shot out. Depending on what kind of guys

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<v Speaker 1>are it is, it's going to take different formations and

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<v Speaker 1>be different heights and last different amounts of time. But um,

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<v Speaker 1>it'll keep going until it either runs out of water

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<v Speaker 1>or it cools down enough for it just start all

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<v Speaker 1>over again. Yeah, and then it just starts all over again,

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<v Speaker 1>which is how you get something like Old Faithful. Right,

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<v Speaker 1>that's right. Once it once it releases that um that

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<v Speaker 1>pressure and it shoots out, it's the whole process just

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<v Speaker 1>begins again, and you have, Um, guys, there's like Old

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<v Speaker 1>Faithful that or run like on a pretty regular schedule.

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<v Speaker 1>I think it's between like sixty and eighty five minutes

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<v Speaker 1>or something like that. Well, I've got the new schedule

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<v Speaker 1>to help schedule because it's been it's been happening with

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<v Speaker 1>greater with less frequency and greater power in recent years.

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<v Speaker 1>I think it's said since two thousand UM. And it's

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<v Speaker 1>a bimodal. They call it bimodal. And if you're going

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<v Speaker 1>to Old Paple and Wyoming, Um. There are generally two

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<v Speaker 1>eruption durations now, either a long one which is over

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<v Speaker 1>four minutes, or a short one, which is about two

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<v Speaker 1>and a half minutes. And if you have just missed

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<v Speaker 1>the short one, there'll be about an hour before your

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<v Speaker 1>next eruption. If you have just missed the long one,

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<v Speaker 1>then there's gonna be about an hour and a half

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<v Speaker 1>until the next one. But either way, it's it's worth

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<v Speaker 1>sticking around for it. Yeah, and it's funny if you

0:12:47.360 --> 0:12:50.080
<v Speaker 1>go to the page and there's obviously a webcam up

0:12:50.080 --> 0:12:51.520
<v Speaker 1>where you can see it and stuff, but that's not

0:12:51.600 --> 0:12:53.560
<v Speaker 1>as fun. But if you go to the web page

0:12:53.559 --> 0:12:55.559
<v Speaker 1>and they ask for tips on you know, seeing it,

0:12:56.200 --> 0:12:58.760
<v Speaker 1>they say, well, if there's a lot of people sitting

0:12:58.840 --> 0:13:02.120
<v Speaker 1>around on the benches, that means there's one upcoming. If

0:13:02.120 --> 0:13:03.839
<v Speaker 1>there's a bunch of people getting up and leaving, that

0:13:03.920 --> 0:13:07.000
<v Speaker 1>means it just happened. It's like, wow, really, yeah, that's

0:13:07.000 --> 0:13:09.640
<v Speaker 1>the best you can do. That sounds like, um, like

0:13:09.800 --> 0:13:15.040
<v Speaker 1>hippie park ranger logic exactly. Um okay, so, uh well,

0:13:15.040 --> 0:13:18.520
<v Speaker 1>I guess we're onto like famous geysers, right, yeah, Actually

0:13:18.559 --> 0:13:21.760
<v Speaker 1>quickly I mentioned I teased about the fourth um thing

0:13:21.840 --> 0:13:26.720
<v Speaker 1>being remoteness. Apparently, in the last fifty years, uh producing

0:13:26.920 --> 0:13:32.079
<v Speaker 1>energy with geothermal energy production is increased so much that

0:13:32.120 --> 0:13:36.720
<v Speaker 1>it's affecting geysers, and so being remote is now believed

0:13:36.760 --> 0:13:38.560
<v Speaker 1>to be one of the requirements to be a geyser

0:13:38.640 --> 0:13:41.880
<v Speaker 1>because geysers are vanishing because of man because so I

0:13:41.960 --> 0:13:44.040
<v Speaker 1>was trying to figure out this out. Maybe you can

0:13:44.400 --> 0:13:48.480
<v Speaker 1>help me. That's because we dig down to these this

0:13:48.840 --> 0:13:52.679
<v Speaker 1>this um, these geysers of this geo thermal activity, and

0:13:52.760 --> 0:13:55.520
<v Speaker 1>in doing so, are we creating like a release valve

0:13:56.040 --> 0:13:58.240
<v Speaker 1>so the pressure camp build as much I think So,

0:13:58.320 --> 0:14:01.640
<v Speaker 1>I mean they're using it to spind turbines to create energy,

0:14:01.720 --> 0:14:03.719
<v Speaker 1>but I know you can also have like a geothermal

0:14:03.800 --> 0:14:07.520
<v Speaker 1>system in your backyard, which I don't think he uses.

0:14:07.600 --> 0:14:09.760
<v Speaker 1>I don't think it like creates steam. So I feel

0:14:09.800 --> 0:14:12.559
<v Speaker 1>like what we're doing then is creating artificial geysers, like

0:14:12.679 --> 0:14:15.600
<v Speaker 1>creating an artificial pipe to let steam out, which would

0:14:15.840 --> 0:14:19.800
<v Speaker 1>impact any natural guys activity because like we said, they're

0:14:19.920 --> 0:14:24.640
<v Speaker 1>very fragile. Earthquakes frequently um cut them off. They also

0:14:24.800 --> 0:14:27.440
<v Speaker 1>bring them back to life to Yeah, that's like there

0:14:27.560 --> 0:14:32.040
<v Speaker 1>was one called the Stroker geyser that that would be

0:14:32.280 --> 0:14:34.520
<v Speaker 1>st r O k K you are, yeah, and that

0:14:34.640 --> 0:14:38.160
<v Speaker 1>stroker like stroker race right right, So stroker geyser um

0:14:38.440 --> 0:14:42.160
<v Speaker 1>is after the Icelandic well, stroker is after the Icelandic

0:14:42.280 --> 0:14:45.960
<v Speaker 1>verb to churn, and actually geysers after the Icelandic verb

0:14:46.480 --> 0:14:51.600
<v Speaker 1>um to gush. So this is all very Icelandic in origin,

0:14:51.720 --> 0:14:53.800
<v Speaker 1>but that would be g e y s I r

0:14:55.640 --> 0:14:59.920
<v Speaker 1>okas in Icelandic. Sure, I won't know how byork pronounced.

0:15:00.640 --> 0:15:03.560
<v Speaker 1>And you've seen Christian Wiggs impression of her. Huh, it's

0:15:03.600 --> 0:15:07.960
<v Speaker 1>really great. Um Okay, So the Stroker Geyser was actually um.

0:15:08.840 --> 0:15:13.920
<v Speaker 1>It was enacted in seventeen nine um because of an earthquake,

0:15:14.400 --> 0:15:19.240
<v Speaker 1>and then another earthquake hit in Ee and it became inactive.

0:15:19.280 --> 0:15:22.400
<v Speaker 1>It went dormant and the local said, we gotta get

0:15:22.400 --> 0:15:24.320
<v Speaker 1>our guys are back. Man, it's all blocked up. So

0:15:24.400 --> 0:15:27.040
<v Speaker 1>they cleared it off and now it's running again. I

0:15:27.120 --> 0:15:32.800
<v Speaker 1>bet that's probably dangerous work. Dangerous. Um. Another way to

0:15:32.960 --> 0:15:36.600
<v Speaker 1>that humans are impacting is a mineral extraction. Apparently in

0:15:36.760 --> 0:15:41.840
<v Speaker 1>two thousand three, uh, they were extracting minerals in Chile,

0:15:42.840 --> 0:15:46.880
<v Speaker 1>the second largest geyser field in South America, and it

0:15:47.480 --> 0:15:52.880
<v Speaker 1>killed it basically from extracting golden stuff. Because basically they

0:15:52.920 --> 0:15:55.800
<v Speaker 1>mess with the plumbing and then you're finished. Because it's

0:15:55.840 --> 0:15:58.720
<v Speaker 1>like you said, like um, in a pressure cooker has

0:15:58.760 --> 0:16:02.360
<v Speaker 1>that little steam, but also it's doesn't explode. The guys

0:16:02.520 --> 0:16:04.600
<v Speaker 1>aren't supposed to have that. If they have that, they

0:16:04.680 --> 0:16:06.600
<v Speaker 1>just don't go off. They're like, well, fine, I'll just

0:16:06.840 --> 0:16:11.760
<v Speaker 1>let some steam off and um, um, that does happen naturally.

0:16:11.840 --> 0:16:16.360
<v Speaker 1>There are steam vents located near geysers, um like yellow stones. Like,

0:16:16.440 --> 0:16:21.680
<v Speaker 1>we have ten thousand um geo thermal um what is

0:16:21.720 --> 0:16:26.080
<v Speaker 1>the word they use, Uh, basically different things. We have

0:16:26.160 --> 0:16:29.200
<v Speaker 1>ten thousands of your thermal different things. Um. But the

0:16:29.320 --> 0:16:33.120
<v Speaker 1>vast majority of those are like steam vents. No, they're

0:16:33.160 --> 0:16:37.600
<v Speaker 1>they're natural, Like they're like little steam releases that come

0:16:37.640 --> 0:16:40.120
<v Speaker 1>up through fissures in the earth. I thought you meant

0:16:40.160 --> 0:16:42.440
<v Speaker 1>we put those in to make old bathele like safers. No,

0:16:42.600 --> 0:16:45.760
<v Speaker 1>they happen naturally. Um. But I think it's the same

0:16:45.840 --> 0:16:48.600
<v Speaker 1>thing as drilling a hole down to a geotherrmal um

0:16:48.960 --> 0:16:53.640
<v Speaker 1>different thing and uh and tapping it to run a turbine. Okay,

0:16:55.000 --> 0:16:58.720
<v Speaker 1>at least you didn't say interesting. Interesting, man, This stuff

0:16:58.800 --> 0:17:02.600
<v Speaker 1>is very interesting. Um, Old people, is a cone geyser?

0:17:03.280 --> 0:17:04.920
<v Speaker 1>I'm not sure I understand the difference. Is it the

0:17:05.119 --> 0:17:08.159
<v Speaker 1>is it the difference? Is it the outlet like the

0:17:08.200 --> 0:17:10.440
<v Speaker 1>shape of the thing above the earth. Yeah, So with

0:17:10.560 --> 0:17:12.960
<v Speaker 1>the cone, guys, where the ryo light bubbles up enough

0:17:13.040 --> 0:17:15.680
<v Speaker 1>over time that it builds up and it forms a

0:17:15.720 --> 0:17:17.760
<v Speaker 1>little cone and that's what the guys are shoots out of.

0:17:17.840 --> 0:17:19.720
<v Speaker 1>And normally with the cone guys or you have a

0:17:20.119 --> 0:17:23.200
<v Speaker 1>big stream going is yet going into the air like

0:17:23.480 --> 0:17:27.879
<v Speaker 1>hundreds of feet That one in um in uh New Zealand,

0:17:28.240 --> 0:17:33.320
<v Speaker 1>the Wyman Geo geyser. Um, that one streamed four d

0:17:33.520 --> 0:17:35.680
<v Speaker 1>seventy ft into the air and for those of you

0:17:35.800 --> 0:17:38.560
<v Speaker 1>in New Zealand, that's four hundred and fifty that's a

0:17:38.640 --> 0:17:43.639
<v Speaker 1>world record, right yeah, yeah, nineteen oh two, yeah, before

0:17:43.640 --> 0:17:45.800
<v Speaker 1>it killed people, right, and then it went dormant in

0:17:45.960 --> 0:17:49.000
<v Speaker 1>nineteen o four because of the landslide, which makes me

0:17:49.119 --> 0:17:51.440
<v Speaker 1>think like this thing is coming back. It just gotta

0:17:51.480 --> 0:17:55.440
<v Speaker 1>bubble back up, kill people and then shut down right afterwards. Yeah,

0:17:55.680 --> 0:17:59.040
<v Speaker 1>it's really had a really chaotic to your career. It's

0:17:59.080 --> 0:18:02.679
<v Speaker 1>like a rock star overdosed on heroin or something. Um.

0:18:02.840 --> 0:18:06.679
<v Speaker 1>But anyway, as I was saying, um, the cone shoots

0:18:06.680 --> 0:18:10.560
<v Speaker 1>a jet into the air. The fountain Um, it shoots

0:18:10.600 --> 0:18:13.200
<v Speaker 1>in a much more like chaotic streme whatever. But it

0:18:13.240 --> 0:18:14.760
<v Speaker 1>doesn't come up from a cone. It comes up from

0:18:14.800 --> 0:18:19.240
<v Speaker 1>a pool. So at the surface the geyser goes into

0:18:19.720 --> 0:18:22.520
<v Speaker 1>a pool of water and then that it will erupt

0:18:22.720 --> 0:18:26.320
<v Speaker 1>out of the water, and that would be the Grand guyser. Um,

0:18:26.800 --> 0:18:29.720
<v Speaker 1>the tall that's the tallest regularly erupting guys are on

0:18:29.760 --> 0:18:32.520
<v Speaker 1>the planet. And that is also a yellowstone. Yeah, the tallest,

0:18:32.560 --> 0:18:34.800
<v Speaker 1>and that it shoots up in the air. Yeah, two

0:18:35.240 --> 0:18:40.320
<v Speaker 1>feet in crazy fountain e hard to predict fashion. Yeah,

0:18:40.359 --> 0:18:43.399
<v Speaker 1>which is pretty surprising too, because the cone geyser shoots

0:18:43.440 --> 0:18:46.280
<v Speaker 1>a jet straight up in the air and this fountain

0:18:46.359 --> 0:18:49.320
<v Speaker 1>geyser is still beating the average one. Yeah. Could you

0:18:49.359 --> 0:18:51.480
<v Speaker 1>imagine if it was a cone guyser, it would be

0:18:51.880 --> 0:18:55.920
<v Speaker 1>mind blowing to the moon. Uh. You mentioned the stroker

0:18:56.080 --> 0:19:00.760
<v Speaker 1>Ace geyser, the steamboat guys Yeah, apparently can sheet water

0:19:00.840 --> 0:19:04.240
<v Speaker 1>up to three hundred feet. But don't bother stopping by

0:19:04.359 --> 0:19:07.520
<v Speaker 1>because it hasn't happened for fifty years. It can go

0:19:07.680 --> 0:19:11.120
<v Speaker 1>fifty years, but yeah, it's finicky. Yeah. Um. There's also

0:19:11.200 --> 0:19:15.680
<v Speaker 1>the geyser, which is the o g geyser because that's

0:19:15.680 --> 0:19:18.280
<v Speaker 1>where the word came from. It's a geyser in Iceland.

0:19:18.600 --> 0:19:23.160
<v Speaker 1>It was discovered in Umour, so it's the oldest known

0:19:23.240 --> 0:19:25.520
<v Speaker 1>guys are on the planet. But they took some samples

0:19:25.600 --> 0:19:28.639
<v Speaker 1>of the silica that forms the cone of the castle

0:19:28.680 --> 0:19:31.200
<v Speaker 1>guys are in Yellowstone. That's the one they think is

0:19:31.560 --> 0:19:35.480
<v Speaker 1>five thousand to forty thousand years old. Apparently silicon dating

0:19:36.800 --> 0:19:40.760
<v Speaker 1>can use some work. I did see one interesting little

0:19:40.840 --> 0:19:44.080
<v Speaker 1>and it wasn't a joke. It was almost like you

0:19:44.160 --> 0:19:47.440
<v Speaker 1>could hear science guys laughing about it. Though. You geysers

0:19:47.480 --> 0:19:52.080
<v Speaker 1>are always called geysers, even if they quit erupting. But

0:19:52.400 --> 0:19:55.159
<v Speaker 1>that ceased to make seeds to be a geyser at

0:19:55.240 --> 0:19:58.240
<v Speaker 1>that point. But once you have erupted, you're always called

0:19:58.240 --> 0:20:02.359
<v Speaker 1>a geyser. The cone formerly known as geyser. Yeah, that's

0:20:02.400 --> 0:20:06.960
<v Speaker 1>what I would call it. Shameful. Uh, listen, do you

0:20:07.080 --> 0:20:11.160
<v Speaker 1>know that whole story about Prince doing that, about changing

0:20:11.240 --> 0:20:13.720
<v Speaker 1>his name. No, I never knew the story behind it.

0:20:13.920 --> 0:20:16.200
<v Speaker 1>So he was locked in a contract with Sony that

0:20:16.280 --> 0:20:20.560
<v Speaker 1>he didn't like, and Sony basically said, you can't release

0:20:20.600 --> 0:20:24.320
<v Speaker 1>an album as Prince. Yes. And but also that had

0:20:24.359 --> 0:20:27.240
<v Speaker 1>something to do with him acting basically crazy, like he

0:20:27.320 --> 0:20:29.600
<v Speaker 1>acted crazy on purpose to get out of his contract

0:20:29.600 --> 0:20:31.439
<v Speaker 1>because there was some sort of clause where like if

0:20:31.480 --> 0:20:33.880
<v Speaker 1>he was if he went nuts or whatever, it would

0:20:33.880 --> 0:20:36.119
<v Speaker 1>avoid his contract. So he did that, and he had

0:20:36.160 --> 0:20:38.800
<v Speaker 1>that font release and I remember he released it to

0:20:38.960 --> 0:20:42.520
<v Speaker 1>the media like, um, his little symbol yes to as

0:20:42.600 --> 0:20:45.480
<v Speaker 1>like a font add on so you could just print

0:20:45.520 --> 0:20:48.359
<v Speaker 1>the symbol when you were writing about him. And his

0:20:48.560 --> 0:20:51.200
<v Speaker 1>contract with Sony was either avoided or they gave it

0:20:51.320 --> 0:20:53.520
<v Speaker 1>up or whatever. But he was basically like, I'll show

0:20:53.600 --> 0:20:56.760
<v Speaker 1>you crazy, but I need to get out of this contract. Boy.

0:20:56.840 --> 0:20:59.480
<v Speaker 1>One of the best concerts I've ever seen. Oh yeah,

0:20:59.480 --> 0:21:01.240
<v Speaker 1>I'll bet and I don't even think I put it

0:21:01.320 --> 0:21:03.880
<v Speaker 1>my top five when we had that listener mail at time,

0:21:03.920 --> 0:21:06.879
<v Speaker 1>but probably forgot. It's probably in my top five. I

0:21:06.920 --> 0:21:09.919
<v Speaker 1>would like to see print. Sometimes he brings it he um.

0:21:10.160 --> 0:21:12.439
<v Speaker 1>He bought you met a bottle of water at um

0:21:12.600 --> 0:21:15.639
<v Speaker 1>a Miles Davis show at the Cotton Club. Really wow.

0:21:16.000 --> 0:21:18.040
<v Speaker 1>Her friends came up to see the lemon Heads and

0:21:18.119 --> 0:21:20.000
<v Speaker 1>she's like, yeah, I'll go with you, and then found

0:21:20.040 --> 0:21:22.000
<v Speaker 1>out that Miles Davis was playing. It's like, I'm gonna

0:21:22.040 --> 0:21:27.919
<v Speaker 1>go over here yourself, bottle of water. Evan Dando, Miles Davis.

0:21:28.640 --> 0:21:32.520
<v Speaker 1>Let me think about that. Sorry, e d um So

0:21:32.800 --> 0:21:38.679
<v Speaker 1>that's uh, that's print. Oh yeah, oh yeah. Guys are too. Um.

0:21:38.720 --> 0:21:40.560
<v Speaker 1>If you want to learn more about guysers, you can

0:21:40.600 --> 0:21:42.920
<v Speaker 1>type that word g E y S e r s.

0:21:43.000 --> 0:21:46.439
<v Speaker 1>That's the English spelling. We didn't do it icelandically. Um,

0:21:46.520 --> 0:21:47.960
<v Speaker 1>but you type that in the search bar at how

0:21:48.040 --> 0:21:50.680
<v Speaker 1>stuff works dot com and it will bring up this fine,

0:21:50.720 --> 0:21:54.080
<v Speaker 1>fine article. And I said search part how stuff works

0:21:54.080 --> 0:21:57.280
<v Speaker 1>dot com, which means it's time for plug fest. It's

0:21:57.280 --> 0:22:01.840
<v Speaker 1>time for listener mail. All right, Josh, I'm gonna call this,

0:22:02.080 --> 0:22:07.400
<v Speaker 1>uh given a local Brooklyn night a plug for his election.

0:22:07.720 --> 0:22:10.600
<v Speaker 1>But that's not how it started. Okay, that was kind

0:22:10.600 --> 0:22:13.320
<v Speaker 1>of a complicated title. Um, guys who just listen to

0:22:13.359 --> 0:22:15.359
<v Speaker 1>your podcast How Labor Unions Work? And I want to

0:22:15.400 --> 0:22:17.960
<v Speaker 1>thank you for trying to give a very balanced a

0:22:18.680 --> 0:22:21.520
<v Speaker 1>story to what is a very complicated and contentious subject.

0:22:22.000 --> 0:22:25.000
<v Speaker 1>As a former New York City union organizer, so this

0:22:25.040 --> 0:22:27.720
<v Speaker 1>guy is the real deal. I am very familiar with

0:22:27.800 --> 0:22:30.560
<v Speaker 1>the arguments against unions, but I truly believe American workers

0:22:30.920 --> 0:22:33.600
<v Speaker 1>in the American economy are better off with unions and

0:22:33.680 --> 0:22:39.240
<v Speaker 1>without when unions are strong, organizing when unions are strong.

0:22:39.320 --> 0:22:42.800
<v Speaker 1>There is some counterpoint to this total acceptance of rampant

0:22:42.880 --> 0:22:46.000
<v Speaker 1>greed that was essentially the cause of the financial meltdown

0:22:46.040 --> 0:22:48.320
<v Speaker 1>in two thousand and eight. At this point, with unions

0:22:48.359 --> 0:22:51.080
<v Speaker 1>at their weakest and a half century, we average Americans

0:22:51.119 --> 0:22:55.359
<v Speaker 1>are being held hostage by corporations. That's what he says. Um,

0:22:55.520 --> 0:22:57.679
<v Speaker 1>I have to say in my line of work, violence

0:22:57.800 --> 0:23:00.800
<v Speaker 1>was not the norm, but intimidation by the employers consant.

0:23:01.359 --> 0:23:04.680
<v Speaker 1>They did everything from threatening workers with being fired, lying

0:23:04.760 --> 0:23:07.400
<v Speaker 1>to them and telling them they did not have collective

0:23:07.440 --> 0:23:10.960
<v Speaker 1>bargaining rights, to telling them the union would only steal

0:23:11.680 --> 0:23:17.040
<v Speaker 1>their dues and not get them a good contract. The

0:23:17.160 --> 0:23:21.000
<v Speaker 1>deceptive HR person right there. Yeah, Or they would tell workers,

0:23:21.240 --> 0:23:23.840
<v Speaker 1>um they would work out individual deals with them, that

0:23:23.920 --> 0:23:27.720
<v Speaker 1>they would vote against the union like, Yeah, that's pretty

0:23:27.960 --> 0:23:31.200
<v Speaker 1>pretty Harry. Even once when we were organizing at a

0:23:31.280 --> 0:23:34.359
<v Speaker 1>Catholic hospital, they told the workers they were going against

0:23:34.400 --> 0:23:37.280
<v Speaker 1>God if they tried to organize. Yeah, can you see

0:23:37.320 --> 0:23:40.720
<v Speaker 1>like those priests like union breaking cracking heads with mental

0:23:40.800 --> 0:23:43.160
<v Speaker 1>to tongue. The only problem I had with your podcast

0:23:43.280 --> 0:23:45.920
<v Speaker 1>was the lack of coverage you gave to the Triangle

0:23:46.160 --> 0:23:49.520
<v Speaker 1>shirtwaist fire. We've mentioned that. He said it could have

0:23:49.560 --> 0:23:52.600
<v Speaker 1>been not more. He said it could deserve its own podcast.

0:23:54.440 --> 0:23:57.640
<v Speaker 1>He said it was one of the deadliest industrial accidents

0:23:57.680 --> 0:24:00.680
<v Speaker 1>in the United States history. Last year hundreds of people

0:24:00.720 --> 0:24:03.680
<v Speaker 1>came out to commemorate the one year anniversary remember of

0:24:03.800 --> 0:24:07.240
<v Speaker 1>the lives lost due to lock stairwells and exits. That

0:24:07.320 --> 0:24:09.280
<v Speaker 1>fire was a major turning point in labor conditions in

0:24:09.280 --> 0:24:12.040
<v Speaker 1>New York City and around the world, as well as

0:24:12.080 --> 0:24:16.880
<v Speaker 1>bringing light to women's terrible working conditions. And I wrote

0:24:16.920 --> 0:24:20.440
<v Speaker 1>them back and it turns out, uh A day e

0:24:20.600 --> 0:24:24.080
<v Speaker 1>d is his name, Fox is running for Brooklyn City Council.

0:24:25.080 --> 0:24:26.960
<v Speaker 1>I said, you know what, dude, we'll plug your campaign.

0:24:27.760 --> 0:24:32.560
<v Speaker 1>Uh www dot e d E f o X dot

0:24:32.640 --> 0:24:36.159
<v Speaker 1>com a a fox dot com and good luck in

0:24:36.280 --> 0:24:39.200
<v Speaker 1>your bid for city council in Brooklyn. Yeah, if you

0:24:39.320 --> 0:24:43.480
<v Speaker 1>wear um sunglasses with Neon arms on them and into

0:24:43.560 --> 0:24:45.800
<v Speaker 1>like your pro union, I would say your vote for this.

0:24:45.920 --> 0:24:48.119
<v Speaker 1>I think we can help guarnering you a little bit

0:24:48.160 --> 0:24:51.520
<v Speaker 1>of the hipster boat, maybe since we are both aging hipsters.

0:24:51.920 --> 0:24:54.760
<v Speaker 1>I am not a hipster, dude. I am not a hipster,

0:24:55.600 --> 0:24:58.120
<v Speaker 1>and I've maybe aging, but I'm not a hipster. Well,

0:24:58.200 --> 0:25:00.359
<v Speaker 1>you look a lot more like a hips wan you

0:25:00.440 --> 0:25:03.359
<v Speaker 1>used to. Well if you, uh, I guess if you

0:25:03.480 --> 0:25:06.240
<v Speaker 1>have a political campaign you're running, Um, we want to

0:25:06.320 --> 0:25:09.760
<v Speaker 1>hear about it. We heard from another guy. Um in, uh,

0:25:10.080 --> 0:25:13.240
<v Speaker 1>was it in Maryland? A state legislator. He's a he's

0:25:13.240 --> 0:25:16.720
<v Speaker 1>a legislator for Maryland who was writing about human trafficking.

0:25:16.800 --> 0:25:19.520
<v Speaker 1>Next guy shout out to that guy as well. UM,

0:25:19.640 --> 0:25:22.080
<v Speaker 1>but if you are a politician that listens to the

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<v Speaker 1>stuff you should Know, we want to hear your viewpoints.

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<v Speaker 1>Let us know what you gotta say, how we're helping you,

0:25:26.960 --> 0:25:29.600
<v Speaker 1>how we can help more that kind of thing you know. Um,

0:25:29.920 --> 0:25:32.359
<v Speaker 1>you can tweet to us, just please don't send us

0:25:32.400 --> 0:25:35.480
<v Speaker 1>a picture of your junk like other politicians. UM to

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<v Speaker 1>s y s K podcast. You can join us on

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<v Speaker 1>Facebook dot com slash Stuff you Should Know, and you

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<v Speaker 1>can send us an email to Stuff Podcast at Discovery

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<v Speaker 1>dot com. Yeah h brought to you by the reinvented

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<v Speaker 1>two thousand twelve camera. It's ready, are you