WEBVTT - When Mount St. Helens Blew Its Top

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<v Speaker 1>Welcome to Stuff you Should Know, a production of I

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<v Speaker 1>Heart Radio. Hey, and welcome to the podcast. I'm Josh

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<v Speaker 1>and there's Chuck and sitting in for Jerry today is

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<v Speaker 1>our great friend and co producer Dave c and the

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<v Speaker 1>sea stands for cool. Say hello, David, everybody, that's pretty.

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<v Speaker 1>That's a really great Dave impression. He's a he's a troll. Yes,

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<v Speaker 1>I always hear him is wal wal wal walt wal Uh.

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<v Speaker 1>Dave is great. I wish you all knew him, but

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<v Speaker 1>we do, and so he's ours. You're gonna have to

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<v Speaker 1>take our word for it. That's right, speaking of take

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<v Speaker 1>our word for it, Chuck, I have to say to

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<v Speaker 1>all the people who don't know much about Mount St.

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<v Speaker 1>Helen's prepared to have your socks knocked off, or your

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<v Speaker 1>lid blown or your skin seared off of your your muscle. Yeah,

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<v Speaker 1>this is a good one. This is uh. I mean,

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<v Speaker 1>this is so bread and butter stuff you should know

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<v Speaker 1>it is. I don't know why it took us almost

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<v Speaker 1>sixteen years to get to it. And none of that

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<v Speaker 1>margarine stuff are low fat. It's like full milk fat butter.

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<v Speaker 1>Bread and butter stuff you should know salted butter, even

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<v Speaker 1>you like salted Huh. It depends on what you're using

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<v Speaker 1>it for. I like just plain unsalted butter, even on

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<v Speaker 1>a bread and butter piece of like bread with butter. Yeah,

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<v Speaker 1>mainly with like baking and cooking. It's like that's when

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<v Speaker 1>it matters. Yeah, I got too. Um, what's your brand?

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<v Speaker 1>Oh boy? It depends. I mean I love to get

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<v Speaker 1>the hate to be that guy, but I dude, love

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<v Speaker 1>to get the local butter when we get to our

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<v Speaker 1>farmer's market and get it from our c s A.

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<v Speaker 1>What's wrong with that? Well, I don't know. Can't you

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<v Speaker 1>say parquake? Can you right? You must be a social

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<v Speaker 1>justice warrior you buy local butter? Do you like that?

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<v Speaker 1>What's the stuff? The Irish butter in the grocery store?

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<v Speaker 1>That's my brand? Uh? Carry Gold? Carry Gold. That's good too,

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<v Speaker 1>Like I've I've reached arched it, like I've literally researched

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<v Speaker 1>but the butter because I want to get the most

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<v Speaker 1>bang from my buck, and it is at the top

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<v Speaker 1>of basically every list. It's of like any butter of

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<v Speaker 1>any kind. It's really really good butter. Yeah, I totally agree.

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<v Speaker 1>I love carry Gold. I take that stuff camping. Yeah,

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<v Speaker 1>I carried it out in my pocket. Well, I like

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<v Speaker 1>that you can get a tub. It's a smaller tub,

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<v Speaker 1>but I do like a spreadable tub as opposed to

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<v Speaker 1>a stick. I haven't seen the tub. We have a

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<v Speaker 1>stick because we have a cute little butter dish, so

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<v Speaker 1>we have we used the sticks. So anyway back to um,

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<v Speaker 1>Mount St. Helen's the episode today. I was four years

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<v Speaker 1>old when this happened, so I mean I didn't know

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<v Speaker 1>what was going on, but I imagine you were like,

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<v Speaker 1>holy cow, this is one of the most amazing things

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<v Speaker 1>I've ever seen on my TV. Yeah, I was nine

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<v Speaker 1>and I remember it being a big deal. But it's

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<v Speaker 1>funny when I was researching this and then watching, UM,

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<v Speaker 1>there's a really really great thing on YouTube that I

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<v Speaker 1>recommend that A and He put out, You're ago it

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<v Speaker 1>had to be. It was called minute by Minute Colin. Uh,

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<v Speaker 1>the eruption of Mount St. Helen's really gripping stuff as

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<v Speaker 1>a any used to do. You know, they probably still

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<v Speaker 1>do that kind of stuff, but I don't know. Um,

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<v Speaker 1>all of the media around it, I was thinking, like man,

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<v Speaker 1>and I don't know if it was more regional or

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<v Speaker 1>if it truly was nationwide. But I remember the eruption,

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<v Speaker 1>but I didn't remember like the six weeks leading up

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<v Speaker 1>to it, which was a very big deal. Yeah, although

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<v Speaker 1>I think it was more of like a yeah, a

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<v Speaker 1>regional thing for this the lead up. And then also

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<v Speaker 1>if you were a geologist, a vulcanologists, a seismologist, anything

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<v Speaker 1>that had to do with volcanoes erupting or mountains, then

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<v Speaker 1>it would have been a big deal to you two.

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<v Speaker 1>And it definitely attracted them from far and wide. And

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<v Speaker 1>because there was so much warning, um, and it was

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<v Speaker 1>able to buy it. I mean, Mount St. Helens was

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<v Speaker 1>able to kind of draw to it like a magnet.

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<v Speaker 1>All of these amazingly well trained researchers, Um, they were

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<v Speaker 1>there when it went off. And it's probably the most

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<v Speaker 1>best documented volcano in history because of that. Yeah, I mean,

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<v Speaker 1>because like you said, the Mount st. Helens is basically

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<v Speaker 1>saying it's coming everyone. Would you like to document this? Yeah,

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<v Speaker 1>I'm telling you again, it's coming, and I'll show you

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<v Speaker 1>in lots of different scary ways that it's coming. And

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<v Speaker 1>people left, people stayed, people came there, people like tourists

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<v Speaker 1>came to see this thing. So let's get into it. Okay,

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<v Speaker 1>so just a real quick refresher, we've done um volcanoes,

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<v Speaker 1>and I think we've done super volcanoes too, because that

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<v Speaker 1>sounds like us. Yeah, was volcanoes, seventeen super volcanoes. Okay.

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<v Speaker 1>So we talked a lot about how volcanoes work in

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<v Speaker 1>those episodes, So if you want to know a lot

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<v Speaker 1>more in depth, go check those out. But just as

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<v Speaker 1>a refresher for the specific kind of volcano that Mount St.

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<v Speaker 1>Helens is. It's a strato volcano, and it's created when

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<v Speaker 1>one younger plate is subducted under an older plate, and

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<v Speaker 1>as the younger plate goes down into the bowels of

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<v Speaker 1>the Earth, all of the rocket carries with it gets

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<v Speaker 1>heated up. The same with water too, and that stuff

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<v Speaker 1>travels upward because it's less dense than the surrounding mantle

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<v Speaker 1>down below, and as it gets closer and close to

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<v Speaker 1>the crust, it wants to pop out of there, but

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<v Speaker 1>it can't necessarily, sometimes it can, and when it can,

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<v Speaker 1>it just spews out all sorts of molten lava and

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<v Speaker 1>that builds the volcano in a kind of a cone shape,

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<v Speaker 1>which is what Mount Saint Helen's was up until May. Yeah. Um,

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<v Speaker 1>it's a part of the cascade arc arranged there in

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<v Speaker 1>the Pacific Northwest, and all of this happened, and you know,

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<v Speaker 1>geologically speaking, pretty quickly. It happened over the course of

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<v Speaker 1>about forty years in the case of Mountain St. Helens,

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<v Speaker 1>which is pretty speedy. And uh, Ed helped us out

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<v Speaker 1>with this. We did a great job on this article. Um.

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<v Speaker 1>And Ed points out that you know in the Northwest,

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<v Speaker 1>that's why you see so many you know, uh sort

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<v Speaker 1>of coney mountains like that is because of this cascade

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<v Speaker 1>arc and how these mountains were formed, you know, not

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<v Speaker 1>too long ago, right, Yeah, forty thousand years ago, maybe

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<v Speaker 1>less St Helens And I think the whole arc is

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<v Speaker 1>less than a hundred right, um, so the whole thing

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<v Speaker 1>that's driving Mount St. Helens. And apparently also there's some other, um,

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<v Speaker 1>I guess volcanic mountains in the area, like Atoms. I

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<v Speaker 1>think Mount Adams is one as well. But there's a

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<v Speaker 1>there's a magma chamber somewhere under there, I think, um

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<v Speaker 1>possibly miles and miles below the surface. But under normal circumstances,

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<v Speaker 1>like I said, when a Stratto volcanoes formed, the the

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<v Speaker 1>lava just kind of is able to find cracks in

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<v Speaker 1>the crust and like it's it's released through there and

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<v Speaker 1>it builds the mountain up slowly and slowly. But if

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<v Speaker 1>there's not a crack in the crust, as in the

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<v Speaker 1>case where Mount st Helens is um, that magma starts

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<v Speaker 1>to back up. It hits the crust and it starts

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<v Speaker 1>to back up below and all of a sudden you

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<v Speaker 1>have a lot of stuff going on. That um makes

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<v Speaker 1>things go kaboom when the right set of circumstances happens. Yeah,

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<v Speaker 1>this is this is pretty notable. This magma chamber is uh,

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<v Speaker 1>well I is in was quite large and like you said,

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<v Speaker 1>it's it's looking for a place to go. But if

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<v Speaker 1>it doesn't have a place to go, what will happen?

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<v Speaker 1>And as you'll see, this is what happened in the

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<v Speaker 1>case of Mount st Helens is it starts bulging, and

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<v Speaker 1>like the mountain, if you're a geologist, it's super exciting

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<v Speaker 1>to see this happen. Um, even though it's very scary

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<v Speaker 1>and dangerous. But when a geologist sees an actual mountains

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<v Speaker 1>start to bulge out in a direction and we're talking

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<v Speaker 1>you know, hundreds of feet of bulge over the course

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<v Speaker 1>of a pretty short period of time. Then it's pretty like, Uh,

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<v Speaker 1>it's it's a pretty notable thing. And that's exactly what

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<v Speaker 1>was happening in the case of the magma chamber there

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<v Speaker 1>in UH in Washington. Yeah, like this pressure is building

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<v Speaker 1>up so much it's causing a boil on the mountain.

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<v Speaker 1>The mountain grows a goiter basically, and that's just full

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<v Speaker 1>of pressure and magma just waiting to go off. It

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<v Speaker 1>doesn't always go off. And in fact Mount St. Helen's

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<v Speaker 1>had two bulges also called crypto domes, which is pretty

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<v Speaker 1>awesome UM, from previous volcanic eruptions. One was called Goat

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<v Speaker 1>Rocks Bulge UM, and then the other one was called

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<v Speaker 1>the Sugar Bowl bulge, and they just never like the

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<v Speaker 1>magma found its way out other ways, but the bulge

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<v Speaker 1>was left. This is a new bulge, and like you said,

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<v Speaker 1>it was growing I think about six ft a day.

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<v Speaker 1>Every day it kept growing another six ft, which is

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<v Speaker 1>really fast for a mountain to grow. Uh. And that

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<v Speaker 1>was one of the big signs initially that that something

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<v Speaker 1>was going on. And and one more thing before we

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<v Speaker 1>started to get into um Mount St. Helens itself, Chuck,

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<v Speaker 1>I think we need to say like Mount St. Helens

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<v Speaker 1>was big. It was a big eruption, but it was

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<v Speaker 1>not the biggest eruption Mountain St. Helens has ever had.

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<v Speaker 1>Apparently the biggest eruption it's ever came just about four

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<v Speaker 1>thousand years ago, which is within um traditional like folk

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<v Speaker 1>tale memory. Yeah, I mean it had been an active

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<v Speaker 1>volcano for forty thousand years, but the big one before

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<v Speaker 1>nineteen eighty was. Yeah, like you said, four, I was

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<v Speaker 1>trying to look at a specific year, but let's just

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<v Speaker 1>say four thousand years ago, because once you get back

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<v Speaker 1>that far, you know who cares? Who cares? But it became,

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<v Speaker 1>like you said, part of folklore. The indigenous people there,

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<v Speaker 1>especially the pulla Up people, called the mountain LeWitt l

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<v Speaker 1>O O w I T and there was a Lout's

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<v Speaker 1>brewing company, so shout them out. This is one of

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<v Speaker 1>those things where, uh, I thought, I wonder why, because

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<v Speaker 1>there's been such a push to change names of things

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<v Speaker 1>over the past like a decade or so, this is

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<v Speaker 1>one that was. It seems so like sort of egregious

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<v Speaker 1>that we should call it LeWitt and not Mount st.

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<v Speaker 1>Helens that I'm pretty curious. I'm sure there's been pushes

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<v Speaker 1>over the years to get it changed, but the Europeans,

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<v Speaker 1>of course named it Mountain St. Helen's in after Captain

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<v Speaker 1>George Vancouver. If that name rings a bell, it should

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<v Speaker 1>gave the name of it because of a diplomat name,

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<v Speaker 1>Alan fits Herbert didn't call it fits Herbert peak or

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<v Speaker 1>anything like that because his noble title was Baron St.

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<v Speaker 1>Helen's God. But here's the rub is that Allan fitz

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<v Speaker 1>Herbert never even saw Mountain St. Helen's the mountain named

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<v Speaker 1>after him, So like, I don't know, maybe maybe let's

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<v Speaker 1>call this one LeWitt. Yeah, I think that's a great

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<v Speaker 1>idea actually, And the reason they call it lewe It

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<v Speaker 1>that that was she was named after Um, a like

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<v Speaker 1>a famous volcanic fire tender woman, Um and low Itt

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<v Speaker 1>and a couple of other men who fell in love

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<v Speaker 1>with her and fought for her. Um became low it

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<v Speaker 1>became Mount St. Helen's or lou It if you want

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<v Speaker 1>to call it, at and then the other the other

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<v Speaker 1>men who were fighting for became mount Hood and mount Atoms.

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<v Speaker 1>They were smited by the creator God and turned into

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<v Speaker 1>mountains for fighting Um. And there's legends not just from

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<v Speaker 1>the pool up, but other indigenous tribes around the area

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<v Speaker 1>that something really big happened, and it looks like what

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<v Speaker 1>it is is a geo myth, which we've talked about before.

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<v Speaker 1>And I think the Great Floods episode that has been

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<v Speaker 1>handed down generation after generation that describes this enormous eruption

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<v Speaker 1>four thousand years ago pretty good stuff. Yeah, for sure.

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<v Speaker 1>And it was a big eruption too. There's just one

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<v Speaker 1>other thing. There is a layer of tefra of basically

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<v Speaker 1>volcanic ash and debris and stuff that is so thick

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<v Speaker 1>and so wide it goes up into British Columbia and

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<v Speaker 1>sixty two miles away from Mount St. Helen. It's still

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<v Speaker 1>twenty inches thick, almost two ft thick of ash sixty

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<v Speaker 1>two miles away. That's how big that four thousand year

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<v Speaker 1>ago eruption was. That's huge. And all this to say

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<v Speaker 1>that Mount Helen's uh which has an asked, by the way,

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<v Speaker 1>did you know that? Uh? Yeah, I did, you keep saying, Helen.

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<v Speaker 1>I just wondered. I'm I'm being short because I don't

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<v Speaker 1>want to take up too much time talking about Certainly

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<v Speaker 1>that's good. That reminds me of the guy in college

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<v Speaker 1>who fell on the sidewalk and his books splayed out

0:12:20.120 --> 0:12:22.800
<v Speaker 1>and then he acted like he was reading. Yeah, I

0:12:22.960 --> 0:12:25.880
<v Speaker 1>love that story. I forgot about him. Um, all of

0:12:25.960 --> 0:12:27.959
<v Speaker 1>us to say is that Mount St Helen's had been,

0:12:28.360 --> 0:12:30.959
<v Speaker 1>you know, active, had a long history of activity. So

0:12:31.240 --> 0:12:33.960
<v Speaker 1>it's not like anyone ever thought, well, well, that thing

0:12:34.080 --> 0:12:37.199
<v Speaker 1>is done and it's never gonna happen again. No, definitely not.

0:12:37.920 --> 0:12:40.320
<v Speaker 1>Because also in the nineteenth century there was a lot

0:12:40.440 --> 0:12:43.120
<v Speaker 1>of um eruptions too. There's a painting by a Canadian

0:12:43.200 --> 0:12:47.200
<v Speaker 1>artist named Paul Kane who painted in eighteen forty seven eruption.

0:12:47.800 --> 0:12:50.840
<v Speaker 1>So I mean start starting in the nineteenth century. Um,

0:12:50.880 --> 0:12:56.640
<v Speaker 1>Mount St Helen's was documented pretty pretty clearly scientifically too,

0:12:56.760 --> 0:13:00.120
<v Speaker 1>as as being an eruptive volcano, disruptive volcan you know

0:13:00.200 --> 0:13:04.520
<v Speaker 1>you can almost say, all right, shall we take a break. Yeah,

0:13:04.640 --> 0:13:07.080
<v Speaker 1>that's a nice prelude, I think so too. All right,

0:13:07.120 --> 0:13:34.000
<v Speaker 1>we'll be back right after this geo. Okay, So we

0:13:34.040 --> 0:13:36.280
<v Speaker 1>got a nice background on Mount St Helen's that had

0:13:36.320 --> 0:13:39.640
<v Speaker 1>been very active for about or on a off, active

0:13:39.679 --> 0:13:43.800
<v Speaker 1>for forty thousand years, uh, including I believe the last

0:13:44.640 --> 0:13:48.120
<v Speaker 1>sort of big one was in eighteen fifty seven. Um,

0:13:48.480 --> 0:13:50.800
<v Speaker 1>not too long after that, in nineteen o eight, about

0:13:50.840 --> 0:13:54.839
<v Speaker 1>a million acres of land became part of Columbia National Forest,

0:13:54.920 --> 0:13:58.280
<v Speaker 1>which was hence renamed Gifford. Uh a pin shot or

0:13:58.320 --> 0:14:00.199
<v Speaker 1>pin show. I never know how to say that the

0:14:00.360 --> 0:14:03.599
<v Speaker 1>Bronson Pinchot National Forest National forest, and that was in

0:14:03.679 --> 0:14:08.240
<v Speaker 1>nine and Mount St. Helens is inside that National Forest.

0:14:08.920 --> 0:14:10.920
<v Speaker 1>Um all this uh, this sort of a long way

0:14:10.960 --> 0:14:13.880
<v Speaker 1>of saying. It wasn't like super populated. It didn't have

0:14:14.120 --> 0:14:16.800
<v Speaker 1>wasn't surrounded by neighborhoods and suburbs and stuff like that.

0:14:17.960 --> 0:14:20.880
<v Speaker 1>But there was something or is still something called Spirit

0:14:20.960 --> 0:14:23.600
<v Speaker 1>Lake there um near the base of the mountain, which

0:14:23.880 --> 0:14:27.360
<v Speaker 1>is uh, they have like youth camps there. People had

0:14:27.440 --> 0:14:32.560
<v Speaker 1>cabins here and there. There were recreational activities that all

0:14:32.640 --> 0:14:34.600
<v Speaker 1>over the place. So it's not like no one was there,

0:14:34.960 --> 0:14:39.480
<v Speaker 1>but it wasn't heavily populated right well put so, Um,

0:14:39.960 --> 0:14:42.760
<v Speaker 1>the whole thing starts. Actually even before the whole thing started,

0:14:42.840 --> 0:14:46.160
<v Speaker 1>and I saw in nineteen seventy five the two volcanologists

0:14:46.240 --> 0:14:49.920
<v Speaker 1>published a paper UM saying that it was very likely

0:14:50.040 --> 0:14:52.960
<v Speaker 1>Mount St. Helen's was going to erupt in the twentieth

0:14:53.000 --> 0:14:56.400
<v Speaker 1>century at some point, like a big one and five

0:14:56.480 --> 0:14:59.720
<v Speaker 1>years later, in March eighty, the whole thing was kicked

0:14:59.760 --> 0:15:03.240
<v Speaker 1>off by h four point oh earthquake, which is nothing

0:15:03.280 --> 0:15:05.520
<v Speaker 1>to sneeze at, and it was at the mountain. Like

0:15:05.600 --> 0:15:08.320
<v Speaker 1>this earthquake took place at the mountain, and all of

0:15:08.360 --> 0:15:12.280
<v Speaker 1>a sudden, within five days there were quake storms. There

0:15:12.400 --> 0:15:15.720
<v Speaker 1>was twenty four quakes of four point oh or greater

0:15:16.120 --> 0:15:20.400
<v Speaker 1>within eight hours. When a volcano starts doing that and

0:15:20.480 --> 0:15:23.760
<v Speaker 1>you're detecting it, you you, that's when the geologists come

0:15:23.840 --> 0:15:26.640
<v Speaker 1>running from far and wide. Yeah, so they you know,

0:15:26.720 --> 0:15:29.240
<v Speaker 1>the word gets out, and they did come running from

0:15:29.280 --> 0:15:31.240
<v Speaker 1>foreig and wide and they you know, set up camp

0:15:31.320 --> 0:15:36.080
<v Speaker 1>there at various places. Other just sort of um, as

0:15:36.120 --> 0:15:39.800
<v Speaker 1>I learned from watching this uh any special that um

0:15:39.920 --> 0:15:43.680
<v Speaker 1>there are like volcano chasers even that um, they hear

0:15:43.680 --> 0:15:46.120
<v Speaker 1>about this stuff. They're fascinated by it. I guess it's

0:15:46.160 --> 0:15:50.560
<v Speaker 1>just sort of amateur geo enthusiasts. And people started kind

0:15:50.600 --> 0:15:53.000
<v Speaker 1>of coming in there because they got wind that something

0:15:53.080 --> 0:15:56.640
<v Speaker 1>may be brewing at Mount St. Helen's including and this

0:15:56.840 --> 0:15:58.800
<v Speaker 1>is you know, they're all kinds of people we could

0:15:58.840 --> 0:16:01.960
<v Speaker 1>feature story wise, but one gentleman we are going to feature.

0:16:01.960 --> 0:16:04.360
<v Speaker 1>His name was David Johnston UH, and he was a

0:16:05.040 --> 0:16:08.120
<v Speaker 1>volcanologist at the U s g S, the United States

0:16:08.240 --> 0:16:11.880
<v Speaker 1>Geographical Survey, and he was one of the UM. There

0:16:11.920 --> 0:16:13.480
<v Speaker 1>were some great interviews with him in this A and

0:16:13.560 --> 0:16:17.040
<v Speaker 1>E special. He was very young guy, UM, super excited

0:16:17.080 --> 0:16:18.600
<v Speaker 1>to be there, and he was one of the ones

0:16:18.720 --> 0:16:21.760
<v Speaker 1>kind of sounding the alarm along with his partner and

0:16:21.800 --> 0:16:25.720
<v Speaker 1>this guy named Don Swanson about hey, like, you know,

0:16:25.840 --> 0:16:29.280
<v Speaker 1>the s is getting real here everybody, and it looks

0:16:29.320 --> 0:16:32.760
<v Speaker 1>like things like people need to start leaving. Yeah, like

0:16:33.720 --> 0:16:35.600
<v Speaker 1>the thing is is there are the people who did

0:16:35.680 --> 0:16:37.520
<v Speaker 1>live on the mountain were not the kind of folk

0:16:37.600 --> 0:16:41.120
<v Speaker 1>who listened to like, you know, the governmentcil neton college

0:16:41.160 --> 0:16:44.840
<v Speaker 1>boys or the government to be told like leave your home.

0:16:45.440 --> 0:16:48.560
<v Speaker 1>And then also there was um those youth groups that

0:16:48.680 --> 0:16:52.280
<v Speaker 1>were like you're going to ruin our week at Spirit Lake. UM.

0:16:52.400 --> 0:16:57.640
<v Speaker 1>There was also Weyerhauser the first base exactly it's like

0:16:57.720 --> 0:17:00.480
<v Speaker 1>a roller rink over there. UM. And then there was

0:17:00.560 --> 0:17:03.120
<v Speaker 1>Weyerhauser who had a contract to be able to log

0:17:03.600 --> 0:17:06.520
<v Speaker 1>on the on the mountain. They definitely didn't want to

0:17:06.560 --> 0:17:09.040
<v Speaker 1>have to shut down operations. So there's a lot of pressure,

0:17:09.640 --> 0:17:11.879
<v Speaker 1>a surprising amount of pressure, you know, more than you

0:17:11.920 --> 0:17:15.080
<v Speaker 1>would think to keep them outain open, and David Johnston

0:17:15.400 --> 0:17:17.879
<v Speaker 1>and Don Swanson and some of the other colleagues were like,

0:17:18.480 --> 0:17:21.080
<v Speaker 1>you really can't do this, and they managed to convince

0:17:21.200 --> 0:17:23.800
<v Speaker 1>the governor of Washington that it was the right move.

0:17:24.040 --> 0:17:26.840
<v Speaker 1>And then later on, as we'll see, there was even

0:17:26.920 --> 0:17:30.000
<v Speaker 1>more pressure to reopen because things didn't go as fast

0:17:30.080 --> 0:17:33.320
<v Speaker 1>as everyone thought, and they managed to push that back

0:17:33.359 --> 0:17:36.240
<v Speaker 1>as well, and as a result, David Johnston is frequently

0:17:36.320 --> 0:17:40.680
<v Speaker 1>credited for saving thousands of lives potentially, which is pretty cool.

0:17:40.840 --> 0:17:42.600
<v Speaker 1>I mean, and everything I've seen about and he was

0:17:42.680 --> 0:17:47.640
<v Speaker 1>a genuinely great person and also like a really great

0:17:47.760 --> 0:17:51.719
<v Speaker 1>pioneer in volcanology too. Yeah. Absolutely, um yeah. They did

0:17:51.760 --> 0:17:54.320
<v Speaker 1>eventually set up what they called a red zone, and

0:17:54.720 --> 0:17:57.399
<v Speaker 1>a lot of people did evacuate. Uh, there were some

0:17:57.560 --> 0:18:01.200
<v Speaker 1>notable people who didn't. Um. Certainly, we need to mention

0:18:01.280 --> 0:18:05.560
<v Speaker 1>Harry Truman. Um obviously not the president, but he was

0:18:05.680 --> 0:18:09.000
<v Speaker 1>this old kajer who ran the lodge there and he

0:18:09.240 --> 0:18:12.520
<v Speaker 1>became a folk hero because he famously thumbed his nose

0:18:12.720 --> 0:18:15.600
<v Speaker 1>and stayed and said, you know, I'm I'm a part

0:18:15.640 --> 0:18:17.760
<v Speaker 1>of this place. It's a part of me. If the

0:18:17.840 --> 0:18:21.840
<v Speaker 1>mountain goes, I'm gonna go with it. Art Carney played

0:18:21.960 --> 0:18:24.280
<v Speaker 1>him in the movie version. He was He got a

0:18:24.480 --> 0:18:29.240
<v Speaker 1>lot of media attention along with his sixteen cats. Um,

0:18:29.840 --> 0:18:32.840
<v Speaker 1>which is the only part of the story. Like, hey man,

0:18:33.359 --> 0:18:35.760
<v Speaker 1>I'm I'm all for people evacuating and keep people safe,

0:18:35.800 --> 0:18:40.280
<v Speaker 1>but I'm also like some old old mountain man wants

0:18:40.320 --> 0:18:42.480
<v Speaker 1>to stay up there and go go down with a volcano.

0:18:42.640 --> 0:18:46.440
<v Speaker 1>Like that's his right, but send the cats away. Don't

0:18:46.520 --> 0:18:49.520
<v Speaker 1>say like I'm gonna go down and kill these sixteen

0:18:49.560 --> 0:18:52.240
<v Speaker 1>cats at the same time. Yeah, it's kind of like

0:18:52.359 --> 0:18:55.280
<v Speaker 1>being buried in like you know, medieval times and having

0:18:55.359 --> 0:18:57.600
<v Speaker 1>your live horse buried with you. Yeah. I just I

0:18:57.640 --> 0:18:59.359
<v Speaker 1>don't know. Man. Once I heard about the cats, because

0:18:59.400 --> 0:19:01.359
<v Speaker 1>I was all into the sky, right, and then I

0:19:01.440 --> 0:19:03.280
<v Speaker 1>heard about the cat I was like, oh, dude, you

0:19:03.280 --> 0:19:06.240
<v Speaker 1>should have at least set the cats away. Yeah, no way,

0:19:06.440 --> 0:19:16.040
<v Speaker 1>not not a lodge cajure. So um, Harry Truman will

0:19:16.080 --> 0:19:18.280
<v Speaker 1>come back in. This is Harry Ard Truman, by the way,

0:19:18.320 --> 0:19:21.960
<v Speaker 1>everybody said his middle initial to differentiate him. He'll come

0:19:21.960 --> 0:19:24.800
<v Speaker 1>back in later. But so this mark the last thing

0:19:24.840 --> 0:19:28.600
<v Speaker 1>that we happened on the mountain. March in eight hours,

0:19:28.680 --> 0:19:32.399
<v Speaker 1>there's twenty four four point or greater magnitude earthquakes, and

0:19:32.520 --> 0:19:35.760
<v Speaker 1>that brought everybody running. Um. This whole thing was so

0:19:36.000 --> 0:19:39.520
<v Speaker 1>perfectly planned that on the day of the eruption there

0:19:39.680 --> 0:19:44.440
<v Speaker 1>was the mineral and gem show in Yakima, like I think,

0:19:44.560 --> 0:19:46.960
<v Speaker 1>less than a hundred miles away from Mount St. Helen's,

0:19:47.200 --> 0:19:49.560
<v Speaker 1>So anybody who has any had anything to do with

0:19:49.720 --> 0:19:53.080
<v Speaker 1>geology just happened to be in the area or was

0:19:53.200 --> 0:19:57.520
<v Speaker 1>purposefully in the area. And then on March that's just

0:19:57.600 --> 0:20:02.200
<v Speaker 1>getting more and more and more. There was an actual eruption, right, yeah,

0:20:02.320 --> 0:20:05.080
<v Speaker 1>So this was I mean, compared to what eventually ended

0:20:05.119 --> 0:20:07.840
<v Speaker 1>up happening, you could call this sort of many eruption.

0:20:08.680 --> 0:20:12.280
<v Speaker 1>Even though it sent it made a big boom. Apparently

0:20:12.320 --> 0:20:15.080
<v Speaker 1>it was a pretty cloudy day so it wasn't super visible,

0:20:15.160 --> 0:20:19.080
<v Speaker 1>but the ash column went up sixty feet into the air,

0:20:19.680 --> 0:20:22.600
<v Speaker 1>it's nothing to sneeze, and a new crater formed at

0:20:22.640 --> 0:20:25.960
<v Speaker 1>the summit, which grew to about six hundred feet wide,

0:20:26.960 --> 0:20:29.399
<v Speaker 1>so it was a major thing. There was another one

0:20:29.440 --> 0:20:34.080
<v Speaker 1>on again throwing ash into the air, and this is

0:20:34.160 --> 0:20:37.920
<v Speaker 1>like basically from that point through the big one in

0:20:38.080 --> 0:20:46.159
<v Speaker 1>mid May, it was just constant uh warning, constant upheaval, mudslides, avalanches,

0:20:46.720 --> 0:20:50.400
<v Speaker 1>craters growing, and like the mountain is saying like it's

0:20:50.440 --> 0:20:54.080
<v Speaker 1>gonna happen people. This is not a false alarm until

0:20:54.240 --> 0:20:57.520
<v Speaker 1>things calmed down, and that's what you were talking about earlier,

0:20:57.560 --> 0:21:00.680
<v Speaker 1>Like things kind of settled down on what was that

0:21:00.840 --> 0:21:06.800
<v Speaker 1>like May around around may to where the people got

0:21:06.840 --> 0:21:09.239
<v Speaker 1>Auntie that were evacuated and said, hey, listen, we want

0:21:09.280 --> 0:21:11.639
<v Speaker 1>to go back and check on our stuff. And the

0:21:11.720 --> 0:21:14.000
<v Speaker 1>governor eventually was like, all right, I think it, you

0:21:14.080 --> 0:21:15.800
<v Speaker 1>know at the time, and I think Washington still is

0:21:15.880 --> 0:21:18.639
<v Speaker 1>a little bit of one of those like uh, not

0:21:18.800 --> 0:21:21.800
<v Speaker 1>quite live free or die, but you know, like all right, listen,

0:21:21.840 --> 0:21:23.480
<v Speaker 1>these people pay taxes, they want to go back to

0:21:23.520 --> 0:21:27.040
<v Speaker 1>their homes, sign a waiver that you're not gonna sue us,

0:21:27.560 --> 0:21:29.720
<v Speaker 1>and let him go back there. And that's what they did.

0:21:30.320 --> 0:21:34.000
<v Speaker 1>They did. There's footage of them signing um waivers on

0:21:34.080 --> 0:21:36.760
<v Speaker 1>the hood of a car with some obvious state lawyer

0:21:36.800 --> 0:21:39.320
<v Speaker 1>in a three piece suit of canning people a pen

0:21:39.920 --> 0:21:43.280
<v Speaker 1>being like signed here. It's really hilarious, but um they did.

0:21:43.359 --> 0:21:46.119
<v Speaker 1>They started some people started to trickle in um and

0:21:46.240 --> 0:21:50.040
<v Speaker 1>that's actually why there were you know, I think, and

0:21:50.240 --> 0:21:54.480
<v Speaker 1>we ended up with fifty seven casualties. Seven people died,

0:21:55.400 --> 0:21:58.200
<v Speaker 1>and that was one reason why it was actually that high.

0:21:58.400 --> 0:22:00.720
<v Speaker 1>Could have could have been less, but bowl were allowed

0:22:00.720 --> 0:22:03.600
<v Speaker 1>to trickle back in. They still kept like a perimeter,

0:22:04.080 --> 0:22:07.280
<v Speaker 1>but I think it was kind of porous. If you

0:22:07.400 --> 0:22:09.520
<v Speaker 1>wanted to get through, you could get through. And there

0:22:09.560 --> 0:22:13.200
<v Speaker 1>are stories in that minute by minute episode of People.

0:22:13.359 --> 0:22:17.080
<v Speaker 1>There's this one backpacker who is probably hilarious at parties

0:22:17.080 --> 0:22:19.680
<v Speaker 1>because he makes like a funny a funny voice for

0:22:19.760 --> 0:22:22.400
<v Speaker 1>the police when the police is talking, when he's recreating

0:22:22.400 --> 0:22:26.159
<v Speaker 1>a conversation. Um, he's he's stuck through with friends. There

0:22:26.160 --> 0:22:27.960
<v Speaker 1>are a lot of people on the mountain that otherwise

0:22:28.040 --> 0:22:30.480
<v Speaker 1>might not have been had they kept it closed. But

0:22:30.560 --> 0:22:32.520
<v Speaker 1>they did open it up a little bit, and it

0:22:32.680 --> 0:22:35.159
<v Speaker 1>was because nothing had happened for a little while, and

0:22:35.200 --> 0:22:39.080
<v Speaker 1>then about three days later everything happened. You said, you

0:22:39.160 --> 0:22:41.560
<v Speaker 1>said S was getting real. This is when the S

0:22:41.680 --> 0:22:46.240
<v Speaker 1>hit the fan. Yeah, well, I mean just prior to this,

0:22:46.359 --> 0:22:48.159
<v Speaker 1>I guess let's let's back up one half second and

0:22:48.280 --> 0:22:50.840
<v Speaker 1>let you know about what happened when David Johnson and

0:22:50.920 --> 0:22:54.800
<v Speaker 1>Don Swanson, they had moved from their initial base at

0:22:54.840 --> 0:22:58.680
<v Speaker 1>cold Water one, which was about I think eight or

0:22:58.800 --> 0:23:02.840
<v Speaker 1>nine miles away. Uh, took their second station, which was

0:23:02.920 --> 0:23:05.680
<v Speaker 1>called cold Water two, which is about five to six

0:23:05.760 --> 0:23:08.399
<v Speaker 1>miles from the mountain. UM and notably it was on

0:23:08.440 --> 0:23:11.080
<v Speaker 1>the northeast side of the mountain, which turned out to

0:23:11.119 --> 0:23:13.800
<v Speaker 1>be the wrong spot to be UM. But you know,

0:23:13.960 --> 0:23:16.800
<v Speaker 1>these guys knew what was going on. Uh. They know

0:23:16.920 --> 0:23:20.600
<v Speaker 1>it's a dangerous job. And apparently they were swapping UM

0:23:20.840 --> 0:23:24.440
<v Speaker 1>taking shifts. And Don Swanson got the call from Johnston

0:23:24.520 --> 0:23:26.640
<v Speaker 1>and he said, hey, listen, I've got tonight and tomorrow

0:23:26.920 --> 0:23:29.200
<v Speaker 1>if you come and relieve me the next day. And

0:23:29.359 --> 0:23:33.159
<v Speaker 1>then on May eighteenth, nineteen eighty is when Johnston was

0:23:33.240 --> 0:23:36.119
<v Speaker 1>there when everything went boom. Yeah, and I think there

0:23:36.160 --> 0:23:39.560
<v Speaker 1>have been other colleagues and grad students and everything around

0:23:39.600 --> 0:23:41.840
<v Speaker 1>cold Water too, and Johnston sent him away. He's like,

0:23:41.920 --> 0:23:45.000
<v Speaker 1>this is outside the red zone, it's still potentially dangerous.

0:23:45.200 --> 0:23:47.199
<v Speaker 1>There's no reason for more than just one of us

0:23:47.240 --> 0:23:48.639
<v Speaker 1>to be here at a time, So you guys go.

0:23:49.640 --> 0:23:53.080
<v Speaker 1>So at eight thirty two am on May eighteenth night,

0:23:53.920 --> 0:23:58.480
<v Speaker 1>Mount St. Helen's like blew up. And there's like a

0:23:58.640 --> 0:24:02.120
<v Speaker 1>typical idea that people have of a volcano going off,

0:24:02.200 --> 0:24:05.359
<v Speaker 1>and most of the time it's shooting like a huge

0:24:05.440 --> 0:24:08.040
<v Speaker 1>thing at ash and magma straight into the air from

0:24:08.080 --> 0:24:11.640
<v Speaker 1>its top. But that is not what happened with Mount

0:24:11.720 --> 0:24:14.800
<v Speaker 1>st Helens. Mount st Helens was a very specific and

0:24:15.000 --> 0:24:18.000
<v Speaker 1>unusual type of eruption because it didn't go out of

0:24:18.040 --> 0:24:21.080
<v Speaker 1>the top. It came out of the side, and it

0:24:21.240 --> 0:24:26.080
<v Speaker 1>came out in what was known as a lateral blast eruption. Yeah,

0:24:26.240 --> 0:24:28.840
<v Speaker 1>so you know, like we said earlier, that pressure is

0:24:28.920 --> 0:24:32.600
<v Speaker 1>building up uh a lot under the surface. There's a

0:24:32.680 --> 0:24:35.320
<v Speaker 1>lot of moisture down there. Some of it was um,

0:24:35.400 --> 0:24:38.920
<v Speaker 1>like you mentioned, from that initial uh plate subduction. That's

0:24:38.920 --> 0:24:42.360
<v Speaker 1>called magmatic water. Some of it is just regular groundwater

0:24:42.560 --> 0:24:44.560
<v Speaker 1>from from rain and snow and everything. Because it is

0:24:44.600 --> 0:24:47.920
<v Speaker 1>the mountains, that's called meteoric water. And all of that

0:24:48.000 --> 0:24:50.679
<v Speaker 1>stuff is just heating up. It's got pressure from below

0:24:51.119 --> 0:24:54.160
<v Speaker 1>because it's heating, It's got pressure from above because all

0:24:54.200 --> 0:24:56.280
<v Speaker 1>of that weight of the rock is just pushing it down,

0:24:57.160 --> 0:25:01.280
<v Speaker 1>and all of this magma is just like boiling under there.

0:25:01.480 --> 0:25:03.200
<v Speaker 1>But and I don't know we talked about this before.

0:25:03.200 --> 0:25:05.520
<v Speaker 1>I guess it was in one of the volcano episodes.

0:25:05.640 --> 0:25:08.520
<v Speaker 1>But it's it's not allowed to turn to steam because

0:25:08.600 --> 0:25:11.520
<v Speaker 1>there's no room for it. Like steam is expansive and

0:25:12.200 --> 0:25:16.960
<v Speaker 1>it can't expand. So it's just this superheated beyond the

0:25:17.040 --> 0:25:21.959
<v Speaker 1>boiling point level of liquid that's just distributed all throughout

0:25:22.080 --> 0:25:25.160
<v Speaker 1>the upper half and notably sort of the north side

0:25:25.200 --> 0:25:28.400
<v Speaker 1>of this mountain. Yeah, and that that created that bulge

0:25:28.520 --> 0:25:31.600
<v Speaker 1>that kept growing by about six ft a day. UM.

0:25:31.920 --> 0:25:35.040
<v Speaker 1>That was the bultree. It is because like it's as

0:25:35.359 --> 0:25:38.520
<v Speaker 1>violent as it as you can imagine that a bulge,

0:25:38.720 --> 0:25:40.320
<v Speaker 1>and it's something that can make a bulge on the

0:25:40.359 --> 0:25:43.840
<v Speaker 1>side of the mountain would be. And so under under

0:25:43.880 --> 0:25:48.920
<v Speaker 1>other circumstances a plenty in eruption where where volcano explodes

0:25:48.960 --> 0:25:51.560
<v Speaker 1>out of the top, like you typically think of that

0:25:51.760 --> 0:25:54.840
<v Speaker 1>pressure that magma is going to basically force the top

0:25:54.920 --> 0:25:58.680
<v Speaker 1>of the mountain open and that's how it's going to explode.

0:25:59.200 --> 0:26:01.280
<v Speaker 1>This is not what how been with Mount St Helen's

0:26:01.520 --> 0:26:04.440
<v Speaker 1>that kind of UM. I guess the hump was on

0:26:04.760 --> 0:26:06.680
<v Speaker 1>one side. It was on the north flank, wasn't it.

0:26:07.600 --> 0:26:09.679
<v Speaker 1>So it was on the north flank, And the thing

0:26:09.800 --> 0:26:13.280
<v Speaker 1>that kicked off Mount St Helen's eruption wasn't the volcano.

0:26:13.400 --> 0:26:16.720
<v Speaker 1>It was actually an earthquake in the volcano, and that

0:26:17.240 --> 0:26:21.959
<v Speaker 1>that that earthquake caused the largest landslide and recorded history

0:26:22.200 --> 0:26:26.399
<v Speaker 1>on Earth. More than half of a square mile of

0:26:26.520 --> 0:26:31.440
<v Speaker 1>Mount St. Helen's suddenly vanished away. It just suddenly dropped

0:26:31.520 --> 0:26:34.040
<v Speaker 1>off the side, the north side of the mountain. Yeah,

0:26:34.119 --> 0:26:36.679
<v Speaker 1>and it's um like, you should really go check out

0:26:36.720 --> 0:26:39.320
<v Speaker 1>the footage of this stuff. It's some of the most

0:26:39.359 --> 0:26:44.440
<v Speaker 1>amazing like natural geologic disaster footage I've ever seen, just

0:26:44.560 --> 0:26:46.600
<v Speaker 1>to see this mountain and then that you know, especially

0:26:46.640 --> 0:26:50.560
<v Speaker 1>in the Anything to see people interviewed, uh describing like

0:26:50.640 --> 0:26:53.560
<v Speaker 1>seeing this with their eyeballs that was it was just

0:26:53.720 --> 0:26:56.440
<v Speaker 1>like it was incomprehensible what they were witnessing, like a

0:26:56.600 --> 0:27:00.240
<v Speaker 1>mountain that large and and part of it just going

0:27:00.280 --> 0:27:03.479
<v Speaker 1>away immediately again. And one of the reasons they were

0:27:03.520 --> 0:27:06.040
<v Speaker 1>able to witness it, and we have such great documentations

0:27:06.080 --> 0:27:09.360
<v Speaker 1>because at eight thirty two am, a pair of geologists,

0:27:09.480 --> 0:27:12.240
<v Speaker 1>husband and wife geologists, happened to be flying in a

0:27:12.359 --> 0:27:15.080
<v Speaker 1>plane because they had hired a plane to go look

0:27:15.119 --> 0:27:17.119
<v Speaker 1>at Mount St. Helen's because they'd heard that, you know,

0:27:17.359 --> 0:27:20.560
<v Speaker 1>it was there's some stuff going on, and they happened

0:27:20.600 --> 0:27:23.680
<v Speaker 1>to make one more pass right as the mountain that

0:27:23.800 --> 0:27:26.119
<v Speaker 1>earthquake dropped the side of the mountain. They were like

0:27:26.480 --> 0:27:28.640
<v Speaker 1>right above it in a plane. As a matter of fact,

0:27:28.760 --> 0:27:31.240
<v Speaker 1>you know, what's where's your quote? Should we read that? Yeah,

0:27:31.680 --> 0:27:35.840
<v Speaker 1>this is Dorothy Dorothy Stoffel Uh in twenty nineteen. She said,

0:27:35.880 --> 0:27:38.000
<v Speaker 1>the whole north half of the mountain that we were

0:27:38.040 --> 0:27:41.320
<v Speaker 1>flying just five feet above, began churning, and a mile

0:27:41.440 --> 0:27:45.520
<v Speaker 1>long fracture shot across the mountain faster than our minds

0:27:45.560 --> 0:27:48.119
<v Speaker 1>could absorb. The north half of the mountain just became

0:27:48.200 --> 0:27:52.640
<v Speaker 1>like fluid and slid away. Amazing. I saw somebody else

0:27:52.680 --> 0:27:56.520
<v Speaker 1>describe as like a zipper opening along the mountain. Yeah.

0:27:56.680 --> 0:27:59.480
<v Speaker 1>And and you know there there were amateur photographers around

0:27:59.600 --> 0:28:01.760
<v Speaker 1>for some of the stuff. Um, some of these hikers

0:28:01.840 --> 0:28:04.440
<v Speaker 1>like that guy you mentioned that was telling the story

0:28:04.520 --> 0:28:09.520
<v Speaker 1>and finding voices, UM and volcano chasers like they got

0:28:09.680 --> 0:28:12.320
<v Speaker 1>some some like some One guy got like twenty two

0:28:12.359 --> 0:28:14.320
<v Speaker 1>pictures in a row and this is when it eventually blew.

0:28:14.480 --> 0:28:17.320
<v Speaker 1>The other guy got like six or eight pictures. Uh.

0:28:17.480 --> 0:28:20.760
<v Speaker 1>There was a family uh camping with their two young

0:28:20.880 --> 0:28:24.480
<v Speaker 1>daughters and that guy they were you know on the

0:28:24.560 --> 0:28:27.479
<v Speaker 1>north side, Um, you know, well below it but uh,

0:28:27.760 --> 0:28:30.280
<v Speaker 1>you know, within the range. And he was like, you know,

0:28:31.200 --> 0:28:33.000
<v Speaker 1>speaking to how it didn't blow from the top, he said,

0:28:33.040 --> 0:28:35.920
<v Speaker 1>it looked like somebody shot a shotgun out of the

0:28:35.960 --> 0:28:39.320
<v Speaker 1>side of this mountain pointed at us. So ash ash

0:28:39.440 --> 0:28:42.200
<v Speaker 1>was raining down, but it was raining like at people

0:28:42.400 --> 0:28:46.120
<v Speaker 1>and less down from the sky right exactly. It wasn't

0:28:46.120 --> 0:28:47.880
<v Speaker 1>going up and then coming back down. It was coming

0:28:48.000 --> 0:28:51.160
<v Speaker 1>straight at you if you were anywhere north of the mountain. Yea.

0:28:51.840 --> 0:28:53.640
<v Speaker 1>And the reason why the north of the mountain was

0:28:53.680 --> 0:28:56.360
<v Speaker 1>so dangerous because that's where that hump had been. That's

0:28:56.400 --> 0:28:59.800
<v Speaker 1>also where the earthquake moved a good portion of the mountain,

0:29:00.080 --> 0:29:04.000
<v Speaker 1>which meant that all that pressure that was keeping that pressurized,

0:29:04.040 --> 0:29:09.280
<v Speaker 1>superheated water from boiling under the mountain was suddenly exposed.

0:29:09.720 --> 0:29:12.120
<v Speaker 1>It was that pressure was gone, and so all of

0:29:12.200 --> 0:29:18.160
<v Speaker 1>that incredibly hot water flash heated into steam. And when

0:29:18.240 --> 0:29:20.760
<v Speaker 1>that happens, that expands. Like you said, the reason that

0:29:20.880 --> 0:29:24.120
<v Speaker 1>one of the reasons steam can't exist in that situation

0:29:24.240 --> 0:29:27.960
<v Speaker 1>is because it's too expansive. When it does have the

0:29:28.080 --> 0:29:32.320
<v Speaker 1>chance to expand, uh, it does so with incredible force.

0:29:33.200 --> 0:29:36.040
<v Speaker 1>And that's what happened. That's why Mount Saint Helen's blew

0:29:36.120 --> 0:29:38.960
<v Speaker 1>out the side rather than the top because there had

0:29:39.000 --> 0:29:41.720
<v Speaker 1>been a weakening and the pressure that allowed all that

0:29:41.880 --> 0:29:45.480
<v Speaker 1>to just blow out and blow out it did. Yeah,

0:29:45.600 --> 0:29:48.480
<v Speaker 1>I mean it was um. If you look at it,

0:29:48.560 --> 0:29:52.920
<v Speaker 1>it looks almost like a controlled demolition blast or something. Um.

0:29:53.040 --> 0:29:55.320
<v Speaker 1>It definitely doesn't look like any kind of volcano blast

0:29:55.400 --> 0:29:57.760
<v Speaker 1>that you might think of in your head. Um. It

0:29:57.840 --> 0:30:00.520
<v Speaker 1>happened kind of all at once, and it was twenty

0:30:00.640 --> 0:30:05.040
<v Speaker 1>four megaton blast, which I know everyone always tries to

0:30:05.040 --> 0:30:08.840
<v Speaker 1>compare it to like Hiroshima. It was six hundred times

0:30:09.800 --> 0:30:14.200
<v Speaker 1>as powerful as the Hiroshima atomic bomb. Good lord, But

0:30:14.320 --> 0:30:16.600
<v Speaker 1>I mean that's what it would take to move point

0:30:16.800 --> 0:30:20.240
<v Speaker 1>six square or cubic miles of mountain all of a

0:30:20.280 --> 0:30:24.160
<v Speaker 1>sudden too, you know, And that that blast chuck that

0:30:24.440 --> 0:30:28.000
<v Speaker 1>that twenty four megaton blast. It was described as like

0:30:28.640 --> 0:30:33.479
<v Speaker 1>a fast moving cloud of heat and stones moving at

0:30:33.720 --> 0:30:36.160
<v Speaker 1>at some points pretty close to the mountain three hundred

0:30:36.240 --> 0:30:39.640
<v Speaker 1>miles an hour, heated to like six hundred and sixty

0:30:39.720 --> 0:30:43.680
<v Speaker 1>degrees fahrenheit. I think that's like three degrees celsius, just

0:30:44.120 --> 0:30:49.400
<v Speaker 1>blowing northward away from the mountain and everything within eight

0:30:49.520 --> 0:30:54.200
<v Speaker 1>miles of that of the Mountain was in that blast zone,

0:30:54.520 --> 0:30:58.840
<v Speaker 1>and if you recall correctly, David Johnston's um cold Water

0:30:59.360 --> 0:31:04.280
<v Speaker 1>to camp was within about five miles. Yeah, he obviously

0:31:04.360 --> 0:31:07.000
<v Speaker 1>didn't make it. Uh, they found I think they found

0:31:07.000 --> 0:31:09.920
<v Speaker 1>pieces of his trailer like a decade later. H he

0:31:10.000 --> 0:31:13.720
<v Speaker 1>had time to send out one signal which was over

0:31:13.800 --> 0:31:18.520
<v Speaker 1>his radio Vancouver, Vancouver, this is it. The only person

0:31:18.600 --> 0:31:21.400
<v Speaker 1>to pick that up was a Ham radio operator nearby,

0:31:22.320 --> 0:31:27.040
<v Speaker 1>and they renamed that Arie Johnston Ridge in his honor. Um. Obviously,

0:31:27.160 --> 0:31:31.520
<v Speaker 1>Harry Truman perished along with those sixteen cats, and he

0:31:31.760 --> 0:31:34.920
<v Speaker 1>was close enough, uh to where I saw that. They

0:31:34.960 --> 0:31:40.400
<v Speaker 1>said that he and everything around him was basically instantly vaporized,

0:31:40.480 --> 0:31:42.880
<v Speaker 1>Like he wouldn't have felt anything. It would have happened

0:31:43.320 --> 0:31:46.400
<v Speaker 1>his death and vaporization would have happened in like less

0:31:46.400 --> 0:31:49.120
<v Speaker 1>than a second. Yeah, I have the impression the same

0:31:49.160 --> 0:31:52.200
<v Speaker 1>thing happened to David Johnston. And also that rad that

0:31:52.360 --> 0:31:56.280
<v Speaker 1>Ham radio operator who was volunteering to kind of document it.

0:31:56.680 --> 0:32:01.240
<v Speaker 1>He documented David Johnston. Um get covered up, he said,

0:32:01.720 --> 0:32:05.280
<v Speaker 1>Um the he said, gentleman, the camper in the car

0:32:05.440 --> 0:32:07.240
<v Speaker 1>that's sitting over to the south of me. He was

0:32:07.280 --> 0:32:10.280
<v Speaker 1>talking about David Johnston is covered is going to hit

0:32:10.360 --> 0:32:13.680
<v Speaker 1>me too. And that was Jerry Martin, that Ham radio operator,

0:32:13.840 --> 0:32:16.920
<v Speaker 1>and that was his last transmission. He was vaporized as well.

0:32:17.040 --> 0:32:22.440
<v Speaker 1>Essentially everything everything north of the mountain within eight miles

0:32:22.800 --> 0:32:28.160
<v Speaker 1>was just destroyed, just destroyed, like entire hundred foot trees

0:32:28.240 --> 0:32:32.200
<v Speaker 1>that were like ten twelve feet in diameter, just completely

0:32:32.280 --> 0:32:35.400
<v Speaker 1>flattened and also denuded of any bark on the way

0:32:35.440 --> 0:32:39.520
<v Speaker 1>as well. UM. And this was just a blast that UM.

0:32:40.040 --> 0:32:44.080
<v Speaker 1>The landslide that was created from that, the the earthquake

0:32:44.160 --> 0:32:48.080
<v Speaker 1>that initially triggered the eruption UM that had in some

0:32:48.240 --> 0:32:51.680
<v Speaker 1>incredible effects as well. Yeah, because what you've got, you know,

0:32:51.840 --> 0:32:54.479
<v Speaker 1>beyond this avalanche happening, is you've got all of a sudden,

0:32:54.840 --> 0:32:56.760
<v Speaker 1>all this heat happens in a place where there's a

0:32:56.800 --> 0:33:01.240
<v Speaker 1>lot of snow, so that snow melts, that glacier ice melts,

0:33:01.800 --> 0:33:05.400
<v Speaker 1>and you have flooding, and you have mud slides, and

0:33:05.680 --> 0:33:07.360
<v Speaker 1>you have a word that I had never even heard

0:33:07.400 --> 0:33:10.360
<v Speaker 1>of before Ed included it in here, which was lahar,

0:33:11.200 --> 0:33:14.880
<v Speaker 1>which sounds like just a mud slide on steroids, like

0:33:14.960 --> 0:33:19.200
<v Speaker 1>a mudside carrying ammunition with it. And this is just

0:33:19.720 --> 0:33:23.320
<v Speaker 1>raining down everywhere and and like causing a path of

0:33:23.360 --> 0:33:26.160
<v Speaker 1>destruction that hasn't been seen in like modern times in

0:33:26.200 --> 0:33:28.520
<v Speaker 1>this country. Yeah, it was like it had so much

0:33:28.600 --> 0:33:32.000
<v Speaker 1>power chuck that that that slide did that one part

0:33:32.040 --> 0:33:35.600
<v Speaker 1>of it was carrying chunks of rock as big as

0:33:35.720 --> 0:33:38.240
<v Speaker 1>five hundred and fifty eight feet or seven hundred and

0:33:38.320 --> 0:33:43.000
<v Speaker 1>seventy across. That's as big as a fifty story building.

0:33:43.240 --> 0:33:46.760
<v Speaker 1>It was moving rocks that size just fast as you

0:33:46.800 --> 0:33:49.560
<v Speaker 1>can imagine, down the mountain into the valleys. And I

0:33:49.640 --> 0:33:52.360
<v Speaker 1>saw it described as if you were watching it from

0:33:52.400 --> 0:33:55.440
<v Speaker 1>a ridge, as some people were, like far away, you

0:33:55.480 --> 0:33:59.000
<v Speaker 1>would see the cloud or the debris starting to come

0:33:59.480 --> 0:34:02.040
<v Speaker 1>at you. It would disappear into a valley, and then

0:34:02.040 --> 0:34:03.440
<v Speaker 1>all of a sudden it would come up over the

0:34:03.560 --> 0:34:06.680
<v Speaker 1>ridge and keep keep going. It would. It was just

0:34:06.920 --> 0:34:10.359
<v Speaker 1>filling valleys with rocks and debris. It's just it's it's

0:34:10.480 --> 0:34:15.960
<v Speaker 1>unimaginable trying to grasp what happened. And it's even crazier

0:34:16.120 --> 0:34:20.120
<v Speaker 1>that some people are actually they're watching this happen crazy.

0:34:20.960 --> 0:34:24.120
<v Speaker 1>It is crazy. You want to take a break, Yeah,

0:34:24.160 --> 0:34:25.680
<v Speaker 1>we'll take a break and talk a little bit more

0:34:25.719 --> 0:34:54.160
<v Speaker 1>about the after effects right after this. Okay, we're back,

0:34:54.440 --> 0:34:58.600
<v Speaker 1>and as Chuck promised everyone, it's after effect time. Well,

0:34:58.680 --> 0:35:01.880
<v Speaker 1>we talked a little bit about it. Um. Obviously, Spirit Lake,

0:35:01.920 --> 0:35:03.600
<v Speaker 1>which we mentioned at the beginning, which was at the

0:35:03.640 --> 0:35:08.160
<v Speaker 1>base of the mountain UM, has a very strange effects

0:35:08.239 --> 0:35:10.879
<v Speaker 1>on bodies of water. It Uh, it did two things.

0:35:10.960 --> 0:35:14.719
<v Speaker 1>It made the lake larger, but it also made it shallower,

0:35:14.880 --> 0:35:18.040
<v Speaker 1>because it just flooded all this water down there and

0:35:18.200 --> 0:35:21.319
<v Speaker 1>raised it such that the outlet was basically dammed up,

0:35:21.800 --> 0:35:23.400
<v Speaker 1>and so the lake got a whole lot bigger, but

0:35:23.480 --> 0:35:26.440
<v Speaker 1>it reduced its depth by about eight feet. Um. I

0:35:26.520 --> 0:35:29.520
<v Speaker 1>think five years later they built a spillway tunnel to

0:35:30.280 --> 0:35:33.839
<v Speaker 1>control the depth of the lake. Um. Two hundred homes

0:35:33.880 --> 0:35:37.160
<v Speaker 1>and cabins and about two hundred miles of road and

0:35:37.320 --> 0:35:41.839
<v Speaker 1>railways were completely obliterated. Yeah. I also saw that lake

0:35:42.239 --> 0:35:45.560
<v Speaker 1>was now two hundred feet higher in elevation than it

0:35:45.640 --> 0:35:48.560
<v Speaker 1>had been before, as if like there was so much debris.

0:35:49.120 --> 0:35:52.200
<v Speaker 1>It like raised the lake two hundred feet even though

0:35:52.239 --> 0:35:54.600
<v Speaker 1>it also made it shallower. It's nuts, And I think

0:35:54.640 --> 0:35:58.520
<v Speaker 1>it lowered the ultimate height of Mount Saint Helen's right. Yeah, Um,

0:35:58.920 --> 0:36:02.200
<v Speaker 1>I can't remember. I think by like six meters or

0:36:02.280 --> 0:36:06.200
<v Speaker 1>something like that. Some ridiculous amount of height just blown off.

0:36:06.920 --> 0:36:09.720
<v Speaker 1>And that was another thing too, like the after effects

0:36:09.800 --> 0:36:12.040
<v Speaker 1>of it um if you look at Mount St. Helen's

0:36:12.080 --> 0:36:15.839
<v Speaker 1>today or especially like right afterward, UM, it was turned

0:36:15.840 --> 0:36:18.680
<v Speaker 1>into like an amphitheater, Like the north side was blown

0:36:18.719 --> 0:36:20.880
<v Speaker 1>out and the other sides were kind of curved around

0:36:21.440 --> 0:36:23.520
<v Speaker 1>and what was neat is one of the huge after

0:36:23.640 --> 0:36:25.720
<v Speaker 1>effects of Mount St. Helen's. One of the more positive

0:36:25.760 --> 0:36:28.080
<v Speaker 1>ones is I saw it described as like a crash

0:36:28.200 --> 0:36:32.920
<v Speaker 1>course um for vulcanologists and seismologists and everybody who are

0:36:32.960 --> 0:36:37.040
<v Speaker 1>now just had this amazing natural laboratory to study in.

0:36:37.560 --> 0:36:40.480
<v Speaker 1>And that the eruption, because it was the lateral blast,

0:36:40.880 --> 0:36:44.120
<v Speaker 1>opened up like basically a cross section of the mountain

0:36:44.440 --> 0:36:47.759
<v Speaker 1>that they could study. Now it's it's past history from

0:36:47.800 --> 0:36:50.200
<v Speaker 1>the inside out, which I thought was pretty neat. And

0:36:50.280 --> 0:36:53.120
<v Speaker 1>a young Trey Anastasia said, one day I shall play

0:36:53.320 --> 0:36:57.520
<v Speaker 1>at the base of that amphitheater and bore people with noodling.

0:36:59.760 --> 0:37:02.120
<v Speaker 1>They they there, No, I don't think so. I don't

0:37:02.120 --> 0:37:04.399
<v Speaker 1>think there's anything there. How was this kidding? Oh wow,

0:37:04.480 --> 0:37:07.520
<v Speaker 1>that was just completely made. I never will miss a

0:37:07.719 --> 0:37:11.400
<v Speaker 1>chance to take a ticket fish with you. Uh so,

0:37:12.360 --> 0:37:16.080
<v Speaker 1>ash is raining down and out. Uh, it literally darkened

0:37:16.080 --> 0:37:19.080
<v Speaker 1>the skies. Um. When this ash, if you were close

0:37:19.200 --> 0:37:22.880
<v Speaker 1>enough to it, it would literally burn you alive. Um.

0:37:23.000 --> 0:37:25.560
<v Speaker 1>If you're far away, it can just create a lot

0:37:25.600 --> 0:37:29.400
<v Speaker 1>of problems everything from uh, you know, just equipment not working,

0:37:29.520 --> 0:37:35.960
<v Speaker 1>electrical outages and blackouts and brown outs. Visibility is obviously terrible. Um.

0:37:36.120 --> 0:37:39.120
<v Speaker 1>As far as crops go, certain crops were wiped out

0:37:39.760 --> 0:37:42.799
<v Speaker 1>by this ash and the toxic gases. Some of them

0:37:43.320 --> 0:37:45.560
<v Speaker 1>did a little bit better because they just got a

0:37:45.600 --> 0:37:47.919
<v Speaker 1>little bit of the ash and it um ash will

0:37:47.960 --> 0:37:51.200
<v Speaker 1>help promote rainfall and hold moisture in the ground better.

0:37:51.280 --> 0:37:55.520
<v Speaker 1>So apparently wheat crops and apple crops fared pretty well. Yeah,

0:37:55.600 --> 0:37:58.080
<v Speaker 1>that was surprising. Yeah. I also saw and there was

0:37:58.160 --> 0:38:01.040
<v Speaker 1>a lot of devastation. Any any big game animal in

0:38:01.120 --> 0:38:04.880
<v Speaker 1>the blast zone. Was I said, big game animal by

0:38:04.920 --> 0:38:07.640
<v Speaker 1>the way, was it was in the blast zone? Was

0:38:08.000 --> 0:38:11.640
<v Speaker 1>was killed without question, But they were They were very surprised.

0:38:11.680 --> 0:38:15.160
<v Speaker 1>Biologists who went in to investigate shortly afterward found they

0:38:15.200 --> 0:38:18.960
<v Speaker 1>were like entire communities and ecosystems of smaller animals and

0:38:19.040 --> 0:38:23.200
<v Speaker 1>plants and microbes. Fun. Guy that had survived just fine.

0:38:23.680 --> 0:38:26.359
<v Speaker 1>And we're among the first to recallonize and we're part

0:38:26.400 --> 0:38:31.120
<v Speaker 1>of the reason why um Mount St. Helen's ecosystem started

0:38:31.160 --> 0:38:34.319
<v Speaker 1>to rebound so quickly. I mean, that's what will happen,

0:38:34.440 --> 0:38:37.200
<v Speaker 1>right if if if the Earth ever just burns up

0:38:37.200 --> 0:38:40.239
<v Speaker 1>into a fiery ball, that'll just become a big mushroom field,

0:38:40.320 --> 0:38:44.000
<v Speaker 1>right probably, and then the animals that lived underground will

0:38:44.040 --> 0:38:47.200
<v Speaker 1>come above ground and say it's our time, baby, I

0:38:47.280 --> 0:38:52.239
<v Speaker 1>look forward to for some um what else happened? Oh?

0:38:52.320 --> 0:38:55.800
<v Speaker 1>I saw that the ash cloud that that um that

0:38:56.000 --> 0:38:58.320
<v Speaker 1>blew finally out of the top. We should say that

0:38:58.960 --> 0:39:01.880
<v Speaker 1>the lateral blast was followed by a plenty in blast

0:39:02.680 --> 0:39:05.120
<v Speaker 1>and that shot, like you know, that was the money

0:39:05.200 --> 0:39:08.680
<v Speaker 1>volcano shot that everybody was looking for. A plume of

0:39:08.800 --> 0:39:11.960
<v Speaker 1>ash and smoke rose eighty thousand feet into the air,

0:39:12.640 --> 0:39:14.840
<v Speaker 1>and it was moving so fast that it circled the

0:39:14.880 --> 0:39:17.759
<v Speaker 1>globe in fifteen days, came back to square one in

0:39:17.880 --> 0:39:21.440
<v Speaker 1>fifteen days. And of course that was like affecting air traffic.

0:39:21.600 --> 0:39:25.520
<v Speaker 1>Do you remember the icelandic Uh volcano that affected air

0:39:25.560 --> 0:39:28.080
<v Speaker 1>traffic in Europe for like weeks. Weren't you stranded by

0:39:28.120 --> 0:39:34.239
<v Speaker 1>that or something? Okay? Okay? Um it like they knew

0:39:34.320 --> 0:39:38.120
<v Speaker 1>what to do in part because of how Mount St.

0:39:38.200 --> 0:39:40.400
<v Speaker 1>Helen's affected air travel. At the time, they were like,

0:39:40.960 --> 0:39:43.920
<v Speaker 1>this is brand new to us, um, but it helped

0:39:44.040 --> 0:39:46.680
<v Speaker 1>lay the groundwork for understanding what to look for how

0:39:46.760 --> 0:39:49.359
<v Speaker 1>to deal with that kind of stuff later on. Yeah,

0:39:49.440 --> 0:39:51.080
<v Speaker 1>the um. The other thing I wanted to point out

0:39:51.120 --> 0:39:53.360
<v Speaker 1>to about Spirit Lake was if you look at footage

0:39:54.040 --> 0:39:57.239
<v Speaker 1>of the lake and now these kind of rivers that

0:39:57.400 --> 0:40:00.320
<v Speaker 1>were just happening, and it literally like re out it

0:40:00.920 --> 0:40:05.080
<v Speaker 1>you know, the Columbia River and the Cowlitz River in sections, um,

0:40:05.239 --> 0:40:08.200
<v Speaker 1>but it looks like it looks like a logging operation

0:40:08.360 --> 0:40:11.719
<v Speaker 1>is happening, um, and like you could almost and may

0:40:11.800 --> 0:40:14.000
<v Speaker 1>have been able. Well obviously it has been too dangerous,

0:40:14.000 --> 0:40:17.120
<v Speaker 1>but it looks like you could have walked over these logs.

0:40:17.239 --> 0:40:20.120
<v Speaker 1>They were so like packed and these were just trees

0:40:20.360 --> 0:40:23.719
<v Speaker 1>you know, an hour before. Yeah, if you could do

0:40:23.880 --> 0:40:27.920
<v Speaker 1>that lumberjack log rolling thing, you could have probably made

0:40:27.960 --> 0:40:30.840
<v Speaker 1>it across the lake. But there in that minute by

0:40:30.920 --> 0:40:33.760
<v Speaker 1>minute episode, there was a pair of like high school

0:40:33.800 --> 0:40:36.800
<v Speaker 1>sweethearts who have been camping and they had a harrowing

0:40:36.880 --> 0:40:40.279
<v Speaker 1>experience because they they both got thrown into Spirit Lake,

0:40:40.800 --> 0:40:43.960
<v Speaker 1>and um, the boyfriend was able to rescue the girlfriend.

0:40:44.080 --> 0:40:46.279
<v Speaker 1>Is like the logs were starting to close in on him.

0:40:46.360 --> 0:40:48.880
<v Speaker 1>He pulled her out from the lake and they were

0:40:48.960 --> 0:40:51.719
<v Speaker 1>hanging onto logs when they finally made it out and

0:40:51.800 --> 0:40:55.960
<v Speaker 1>were rescued. That happened like that happened to somebody. They

0:40:56.000 --> 0:40:58.560
<v Speaker 1>were in their car. Oh is that how? And that's

0:40:58.600 --> 0:41:00.680
<v Speaker 1>how they got in the lake. They were in their car. Yeah,

0:41:00.760 --> 0:41:02.239
<v Speaker 1>they said it just picked him up and all that

0:41:02.360 --> 0:41:05.040
<v Speaker 1>they were driving and then they were floating and they

0:41:05.080 --> 0:41:06.960
<v Speaker 1>said that there you know there she said, like my

0:41:07.080 --> 0:41:08.799
<v Speaker 1>instinct was to get out of the car, but there

0:41:08.880 --> 0:41:11.640
<v Speaker 1>was like nowhere to go, right yeah, because there were

0:41:11.880 --> 0:41:15.160
<v Speaker 1>trees everywhere floating around beside him, right yeah. And this

0:41:15.360 --> 0:41:17.120
<v Speaker 1>is you know, these are just sort of That's what

0:41:17.239 --> 0:41:19.640
<v Speaker 1>was so cool about the special is it really brought

0:41:19.719 --> 0:41:22.200
<v Speaker 1>in the human element of these people that were around there.

0:41:22.880 --> 0:41:25.160
<v Speaker 1>Um and they you know, they all survived because they

0:41:25.200 --> 0:41:29.320
<v Speaker 1>were being interviewed obviously UM Dorothy Stoffel, who was the

0:41:30.000 --> 0:41:33.480
<v Speaker 1>the geologist that was flying with UM. I guess it

0:41:33.560 --> 0:41:36.279
<v Speaker 1>was her husband, Keith. Was that her brother her her

0:41:36.360 --> 0:41:40.560
<v Speaker 1>husband Keith? Okay, Um they survived that plane flight, like

0:41:40.719 --> 0:41:43.160
<v Speaker 1>they got out of there. There were stories of people

0:41:43.239 --> 0:41:46.840
<v Speaker 1>that literally it was like from a movie. Drove, you know,

0:41:47.000 --> 0:41:50.320
<v Speaker 1>a hundred and ten miles an hour, like out running

0:41:50.400 --> 0:41:55.320
<v Speaker 1>this ash debris slide coming at right. Yeah, and some

0:41:55.480 --> 0:41:57.719
<v Speaker 1>people didn't make it. So there was one guy who

0:41:57.840 --> 0:42:00.759
<v Speaker 1>was chronicled in that that was driving as fast as

0:42:00.800 --> 0:42:03.920
<v Speaker 1>you can in the blasts just caught up with him

0:42:04.000 --> 0:42:07.719
<v Speaker 1>and buried him um in the in the ash um

0:42:08.360 --> 0:42:11.840
<v Speaker 1>and he probably died pretty much instantly. But like again,

0:42:11.960 --> 0:42:14.800
<v Speaker 1>that happened to people. There's very famous footage of a

0:42:14.920 --> 0:42:20.000
<v Speaker 1>house just flowing down like a newly engorged mud slide

0:42:20.040 --> 0:42:23.120
<v Speaker 1>e river moving so fast that you probably could have

0:42:23.239 --> 0:42:26.280
<v Speaker 1>towed water skiers from the house. Essentially it was moving

0:42:26.360 --> 0:42:29.720
<v Speaker 1>that fast just down the river. So I mean again,

0:42:29.960 --> 0:42:33.960
<v Speaker 1>it was one of the most documented um volcanic eruptions

0:42:34.040 --> 0:42:36.759
<v Speaker 1>of all times. So there's really amazing footage on there

0:42:37.080 --> 0:42:39.480
<v Speaker 1>or just on the internet, is what I mean. Um,

0:42:39.840 --> 0:42:42.600
<v Speaker 1>But that wasn't the last time that that Mount St.

0:42:42.640 --> 0:42:46.840
<v Speaker 1>Helen's has erupted. I think it erupted a few times

0:42:46.920 --> 0:42:52.279
<v Speaker 1>between nineteen eighty and maybe I think, yeah, and then

0:42:52.360 --> 0:42:55.360
<v Speaker 1>the biggest one recently was between two thousand four and

0:42:55.440 --> 0:42:58.400
<v Speaker 1>two thousand eight. Yeah, it started sort of getting a

0:42:58.440 --> 0:43:01.880
<v Speaker 1>little more active again. Uh this time though, you know,

0:43:02.000 --> 0:43:04.960
<v Speaker 1>one of the things that um to the benefit of

0:43:05.000 --> 0:43:07.800
<v Speaker 1>the surrounding area when a volcano blows like that is

0:43:07.840 --> 0:43:11.080
<v Speaker 1>that pressure is released and it's gonna take a long

0:43:11.160 --> 0:43:13.879
<v Speaker 1>time to build back up to that level again kind

0:43:13.880 --> 0:43:16.320
<v Speaker 1>of depending on what how it reforms on top of it.

0:43:17.000 --> 0:43:20.160
<v Speaker 1>But this time apparently there are, uh, there are more

0:43:20.440 --> 0:43:23.680
<v Speaker 1>ways for this pressure to be released. So I think

0:43:23.719 --> 0:43:26.040
<v Speaker 1>it's just sort of the pressure is being released a

0:43:26.080 --> 0:43:30.600
<v Speaker 1>little more gradually since the two thousand foursion too. But

0:43:30.800 --> 0:43:33.160
<v Speaker 1>there they do say that like, oh no, like it

0:43:33.280 --> 0:43:37.000
<v Speaker 1>will happen again, like things are uh, there is a

0:43:37.040 --> 0:43:40.320
<v Speaker 1>new lava dome growing and the pressure is going to

0:43:40.400 --> 0:43:43.239
<v Speaker 1>build up, and it could be in a thousand years

0:43:43.320 --> 0:43:45.920
<v Speaker 1>or it could be in ten years. Yeah, we just

0:43:46.040 --> 0:43:48.319
<v Speaker 1>don't know now, but they are studying it. Like there

0:43:48.719 --> 0:43:51.960
<v Speaker 1>there's a lot of active research and study going on

0:43:52.040 --> 0:43:54.360
<v Speaker 1>at Mount Saint Helen's now. Yeah, I believe, you know,

0:43:54.440 --> 0:43:56.520
<v Speaker 1>the eruption was such a big deal that they've they've

0:43:56.600 --> 0:43:59.240
<v Speaker 1>opened the U s g S opened a research station

0:43:59.360 --> 0:44:04.560
<v Speaker 1>nearby UM and also that that two thousand four activity

0:44:05.080 --> 0:44:07.840
<v Speaker 1>basically ran from two thousand four to two eight. Like

0:44:07.960 --> 0:44:10.479
<v Speaker 1>you said, they've been studying the mountain closely. So there's

0:44:10.640 --> 0:44:15.480
<v Speaker 1>amazing time laps footage of those four years, and it's

0:44:15.520 --> 0:44:19.239
<v Speaker 1>astounding how fast and how big Mount St. Helen's just

0:44:19.400 --> 0:44:23.520
<v Speaker 1>grows from that eruption activity. It's called time laps Images

0:44:23.560 --> 0:44:29.480
<v Speaker 1>of Mount St Helen's um dome growth. It's on YouTube, UM,

0:44:29.760 --> 0:44:32.759
<v Speaker 1>and I recommend checking that out as well. Yeah, I

0:44:32.760 --> 0:44:37.320
<v Speaker 1>would just be careful when you google dome growth or

0:44:37.440 --> 0:44:42.800
<v Speaker 1>bulge growth. Boy. So, man, we are so juvenile sometimes,

0:44:42.840 --> 0:44:46.799
<v Speaker 1>aren't we? And by we I mean me too. Um.

0:44:47.000 --> 0:44:49.960
<v Speaker 1>But like we said, Mount St Helens bounced back, Spirit

0:44:50.080 --> 0:44:52.520
<v Speaker 1>Lake open back up and the cold Water two station

0:44:52.680 --> 0:44:56.080
<v Speaker 1>has been renamed after David Johnston and there's an amazing

0:44:56.120 --> 0:44:58.600
<v Speaker 1>memorial too. I saw on some trip Advisor posts that

0:44:58.640 --> 0:45:01.399
<v Speaker 1>somebody so I was like, the one of the best, um,

0:45:02.320 --> 0:45:05.800
<v Speaker 1>like not welcome center, but you know, information centers that

0:45:05.960 --> 0:45:08.360
<v Speaker 1>the person's ever been to. So I would like to

0:45:08.400 --> 0:45:12.400
<v Speaker 1>go there. Some cookies are en real? All right? You

0:45:12.480 --> 0:45:15.480
<v Speaker 1>got anything else? I got nothing else? All right, We'll

0:45:15.520 --> 0:45:19.120
<v Speaker 1>go forth and research um Mount St Helen's with an

0:45:19.280 --> 0:45:22.800
<v Speaker 1>s UM. And you can start doing that by watching

0:45:22.880 --> 0:45:26.080
<v Speaker 1>Dante's Peak. Since I said Dante's peak, it's time for

0:45:26.160 --> 0:45:30.400
<v Speaker 1>listener mail. This is following up on an email that

0:45:30.520 --> 0:45:34.760
<v Speaker 1>you particularly liked from our speectacular. Okay, hey, guys, thoroughly

0:45:34.880 --> 0:45:37.920
<v Speaker 1>enjoying the most recent spectacular. The accents are comedy genius.

0:45:38.640 --> 0:45:44.720
<v Speaker 1>Uh Meagle, do you want to pop in and say Hi, Hello, perfect?

0:45:45.440 --> 0:45:47.239
<v Speaker 1>I'm gonna bring Megle back every now and then. By

0:45:47.239 --> 0:45:49.440
<v Speaker 1>the way, I just want to prepare you in the audience.

0:45:50.360 --> 0:45:52.719
<v Speaker 1>I wanted to address a couple of eighteen hundreds diction

0:45:52.800 --> 0:45:55.439
<v Speaker 1>issues that call some puzzlement. Uh. When you got talked

0:45:55.480 --> 0:45:58.600
<v Speaker 1>about toilet it's basically what Josh said. I've always thought

0:45:58.640 --> 0:46:01.440
<v Speaker 1>of it as a refreshing as freshening up in the bathroom,

0:46:01.520 --> 0:46:03.960
<v Speaker 1>washing your face and hands when first waking up, or

0:46:03.960 --> 0:46:06.440
<v Speaker 1>going to bed. A double check with Marion Webster, though,

0:46:06.480 --> 0:46:12.120
<v Speaker 1>and it's more generally dressing and grooming. That makes sense. Yeah. Sure.

0:46:12.400 --> 0:46:15.759
<v Speaker 1>On the other hand, the strangers in the beverage from

0:46:15.800 --> 0:46:18.120
<v Speaker 1>the toll House is a lot more puzzling. I had

0:46:18.280 --> 0:46:20.560
<v Speaker 1>no idea what it meant, And although Josh's guests that

0:46:20.640 --> 0:46:23.359
<v Speaker 1>beverage meant the pub was clever, it doesn't really make

0:46:23.440 --> 0:46:26.440
<v Speaker 1>sense just as a reminder of the sentence is talking

0:46:26.480 --> 0:46:29.480
<v Speaker 1>about some men drinking tea in an end and pausing

0:46:29.640 --> 0:46:33.440
<v Speaker 1>to quote discover the sex and dates of arrival of

0:46:33.520 --> 0:46:36.960
<v Speaker 1>the strangers, which floated in some numbers in the beverage

0:46:37.080 --> 0:46:39.919
<v Speaker 1>end quote. I think I found the answer, though, guys,

0:46:40.000 --> 0:46:43.440
<v Speaker 1>in a Dictionary of Scottish dialect, we love this stuff

0:46:43.440 --> 0:46:46.160
<v Speaker 1>by them, this is amazing. Tea leaves floating on the

0:46:46.200 --> 0:46:48.839
<v Speaker 1>surface of your drink are considered omens that you will

0:46:48.880 --> 0:46:51.920
<v Speaker 1>meet someone new, So these tea leaves are called strangers.

0:46:52.280 --> 0:46:54.719
<v Speaker 1>If you pick up a stranger and bite it, the

0:46:54.880 --> 0:46:57.160
<v Speaker 1>toughness will tell you whether the new acquaintance will be

0:46:57.320 --> 0:47:01.239
<v Speaker 1>male or female. Amazing. I'm gonna guess there's also a

0:47:01.280 --> 0:47:03.560
<v Speaker 1>way to predict the date you meet this person, although

0:47:03.560 --> 0:47:05.640
<v Speaker 1>I didn't see reference to that. So that's what the

0:47:05.719 --> 0:47:08.320
<v Speaker 1>characters are doing, guys, using tea leaves to predict the future.

0:47:09.120 --> 0:47:11.320
<v Speaker 1>By the way, other omens can also be strangers, like

0:47:11.400 --> 0:47:14.839
<v Speaker 1>unburned candlewicks or sit on greats. I've loved the show

0:47:14.920 --> 0:47:18.400
<v Speaker 1>for years, look forward to anymore. That is a great email.

0:47:18.640 --> 0:47:23.760
<v Speaker 1>Nat Jacob's fantastic uh sleuthing and we are super grateful.

0:47:24.120 --> 0:47:27.640
<v Speaker 1>Top to bottom start to finish. Wonderful email. Also just

0:47:27.920 --> 0:47:31.319
<v Speaker 1>put so nicely to not like you big dummies. Yeah,

0:47:31.800 --> 0:47:34.240
<v Speaker 1>because I got it pretty wrong. It was a terrible guess,

0:47:35.880 --> 0:47:38.759
<v Speaker 1>but I mean that was really hard. Like you was obscure,

0:47:39.320 --> 0:47:42.120
<v Speaker 1>you know very much? Anyway, I love knowing that now.

0:47:42.239 --> 0:47:44.480
<v Speaker 1>That was one of my favorite emails. So thanks a lot, Nat.

0:47:44.760 --> 0:47:46.120
<v Speaker 1>And if you want to be like Nat and get

0:47:46.200 --> 0:47:48.400
<v Speaker 1>in touch with us in the best way possible, you

0:47:48.560 --> 0:47:51.880
<v Speaker 1>can send us an email to Stuff podcast at iHeart

0:47:51.960 --> 0:47:58.360
<v Speaker 1>radio dot com. Stuff you Should Know is a production

0:47:58.440 --> 0:48:01.319
<v Speaker 1>of I Heart Radio from our podcasts My heart Radio,

0:48:01.600 --> 0:48:04.520
<v Speaker 1>visit the i heart Radio app, Apple Podcasts, or wherever

0:48:04.600 --> 0:48:12.640
<v Speaker 1>you listen to your favorite shows. H m hm