WEBVTT - Sailor on a Sea of Lava

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<v Speaker 1>My La. Welcome to Stuff to Blow Your Mind, the

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<v Speaker 1>production of My Heart Radio. Hey, welcome to Stuff to

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<v Speaker 1>Blow your Mind. My name is Robert Lamb and I'm

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<v Speaker 1>Joe McCormick and Robert. Are we gonna be talking about

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<v Speaker 1>hot lava today? Oh? Yeah, yeah, We're definitely gonna be

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<v Speaker 1>talking about hot lava. Um, this was. This is an

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<v Speaker 1>episode that I was inspired for us to put together

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<v Speaker 1>because I mean, lava is always cool. Was we'll get

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<v Speaker 1>into in a minute. They're like lava, lakes of lava,

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<v Speaker 1>rivers of lava. It pops up in a lot of

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<v Speaker 1>our favorite uh science fiction and fantasy franchises, but of

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<v Speaker 1>course in the real world, it's also incredibly interesting. It's uh,

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<v Speaker 1>it's it's there's something almost kind of holy about being

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<v Speaker 1>either in the presence of lava or being in places

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<v Speaker 1>where lava has recently been And standard terminology insert the

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<v Speaker 1>term for molten rock when it's still bottled up below

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<v Speaker 1>the Earth's surface is magma, and the exact same stuff

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<v Speaker 1>is called lava once it breaches the surface in an eruption.

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<v Speaker 1>So if it's on the surface of the Earth, basically

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<v Speaker 1>if you're looking at it, if you're watching it form

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<v Speaker 1>a river across the black fields of rock. It is

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<v Speaker 1>now lava right, yes, now, I recently had the privilege

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<v Speaker 1>this just was just last weekend. Actually, um, just a

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<v Speaker 1>little over a week ago. I had the privilege of

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<v Speaker 1>getting to hike the Kilauea Ekey Trail in Volcano National

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<v Speaker 1>Park in Hawaii with my family and with some friends. Uh.

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<v Speaker 1>This is a hike that I'd done twenty years ago

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<v Speaker 1>and I always wanted to do again. I always wanted

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<v Speaker 1>to you know, be able to bring my my wife

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<v Speaker 1>on the trip, and then you know, bring my son

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<v Speaker 1>on the trip. And Uh, if anyone out there is

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<v Speaker 1>considering going to the island of Hawaii, I highly recommend

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<v Speaker 1>this particular walk. It's it's very popular. It's not not

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<v Speaker 1>a trade secret or anything. It's a three point three

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<v Speaker 1>mile loop. It takes you around down and then straight

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<v Speaker 1>across Kilauea Ekey Crater. Uh. Today it just just like

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<v Speaker 1>you know it was twenty years ago. It's this beautiful

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<v Speaker 1>landscape of black cracked volcanic terrain, um with with vegetation. Uh,

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<v Speaker 1>you know at the top. So the hike itself gives

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<v Speaker 1>you this this wonderful transformation. You get to walk through

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<v Speaker 1>almost this kind of rainforest setting. Uh. Then you you know,

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<v Speaker 1>you go down uh the edge of the crater, and

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<v Speaker 1>then you go into the bottom of the crater, where

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<v Speaker 1>it's like another planet. It's it's truly unlike anywhere else

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<v Speaker 1>I've been, just a really unique and beautiful place. One

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<v Speaker 1>of the things I remember that we talked about in

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<v Speaker 1>our episodes on the eruption of Mount Vesuvius was about

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<v Speaker 1>how you can track sort of the length of time

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<v Speaker 1>since the last eruption or or major disturbance by how

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<v Speaker 1>far vegetation has re encroached on the on the volcano

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<v Speaker 1>and that you know, so there's this horrible eruption in

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<v Speaker 1>what was of Vesuvius, and it turned the area there

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<v Speaker 1>and too, I'm sure you know, eliminated most life within

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<v Speaker 1>a certain radius from the uh from the eruption site.

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<v Speaker 1>But then you get to see just like over the years,

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<v Speaker 1>the trees and all the vegetation just pours back in

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<v Speaker 1>the greening of the of the cone. And and there's

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<v Speaker 1>something I always found beautiful about that because it's like

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<v Speaker 1>the trees don't know, yeah, the tree that it's it's

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<v Speaker 1>always it's it's kind of interesting in both directions. Because

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<v Speaker 1>you see footage of of of the volcanic activity that

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<v Speaker 1>took place in this crater back in nine and you know,

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<v Speaker 1>you see the plant the plants are just hanging out

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<v Speaker 1>that they don't you know, they don't care. They're like,

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<v Speaker 1>I don't know. I'm still doing Okay, I haven't been

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<v Speaker 1>the leaves have not been burnt from me yet, so

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<v Speaker 1>you will sue me in the foreground. And then likewise,

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<v Speaker 1>you go back there today and you see the you know,

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<v Speaker 1>the plants making their comeback. Um, right at the fissure point,

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<v Speaker 1>right at the place where where all of this volcanic

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<v Speaker 1>activity was was happening, where this lava fountain was shooting

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<v Speaker 1>high into the sky. It's beautiful. Yeah. So, like I said,

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<v Speaker 1>if you go to to Ikey Crater today, Kilauea Ekey Crater,

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<v Speaker 1>you can you can walk across it. Uh, you know,

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<v Speaker 1>all perfectly safe. Um, the lava that was underneath your feet,

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<v Speaker 1>it's all completely solid now we're thought to be probably

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<v Speaker 1>has been completely solid since the I think the mid nineties,

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<v Speaker 1>they say, But but all this was different in the past.

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<v Speaker 1>Hawaii is, of course a young island formed from five

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<v Speaker 1>separate shield volcanoes. If you were to travel back in

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<v Speaker 1>time a million years, the island wouldn't be there at all.

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<v Speaker 1>Travel back to the mid nineteen fifties, and this particular

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<v Speaker 1>crater was there, but it contained an entire forest at

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<v Speaker 1>the bottom of it. Um and this would have been

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<v Speaker 1>roughly eight hundred feet or two hundred and forty four

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<v Speaker 1>meters down into the crater. But then in nineteen fifty nine, UH,

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<v Speaker 1>there was this um this eruption event, spectacular eruption from

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<v Speaker 1>a half mile fissure in the crater wall. And then

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<v Speaker 1>in seventeen separate episodes, lava gushed from this event, lasting

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<v Speaker 1>five weeks total, flooding the crater with lava halfway up

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<v Speaker 1>that eight d foot crater wall, so forming the the

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<v Speaker 1>iconic set piece of many wonderful movies and video games,

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<v Speaker 1>especially to the Lake of Lava. That's right, um And

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<v Speaker 1>there's some stunning images of this uh UM. I included

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<v Speaker 1>one in our notes here, Joe. These just come from

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<v Speaker 1>the UH from MPs dot gov. You can you can

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<v Speaker 1>look up all sorts of information there about the eruption

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<v Speaker 1>of Kilauea ekey. UH. There's some great photography. UH. There's

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<v Speaker 1>also some wonderful footage If you go on YouTube and

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<v Speaker 1>you look for the eruption of kilawaa n nineteen sixty.

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<v Speaker 1>This is like a wonderfully old school documentary piece about

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<v Speaker 1>uh this event with all sorts of just glorious unreal

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<v Speaker 1>footage of of of you know, churning lava, spewing lava

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<v Speaker 1>fountains and so for work, which is wonderful to watch

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<v Speaker 1>either before or after you, you know, physically visit the crater.

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<v Speaker 1>I also love the dragnet style department of interior seal

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<v Speaker 1>that appears right at the beginning. Yeah, and the narrator

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<v Speaker 1>reminds me of the narrator from a lot of the

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<v Speaker 1>old Walt Disney Goofy shorts, where like Goofy is doing

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<v Speaker 1>different sports, so you expect Goofy to show up at

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<v Speaker 1>some point as a volcanologist, but he does not gorsh

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<v Speaker 1>that would shore your bones. So anyway, this is a

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<v Speaker 1>spectacular event. A fountain of lava shot nine feet into

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<v Speaker 1>the air, dropping gouts of magna at times the size

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<v Speaker 1>of bathtubs. Are described as being the size of bathtubs,

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<v Speaker 1>and the resulting like a lava was was most impressive

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<v Speaker 1>I've seen it described in Park literature as a quote

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<v Speaker 1>churning lava lake. Eventually enough lava filled the crater that

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<v Speaker 1>the crack was covered up. Then the molten lava drain

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<v Speaker 1>back into the vent at a speed four times faster

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<v Speaker 1>than it filled. The National Park Service describes this occurrence

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<v Speaker 1>as quote a noisy whirlpool of red hot liquid lava

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<v Speaker 1>and black slabs of solid rock metal. Yeah, I mean,

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<v Speaker 1>it didn't get any more metal than this. Um. And

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<v Speaker 1>there's actually footage in that video I mentioned where you

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<v Speaker 1>get to see a shot of a of a lava

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<v Speaker 1>of vortex um and it's it's it's pretty, it's pretty impressive.

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<v Speaker 1>So even though if you visit this particular location today

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<v Speaker 1>you don't get to um, you know, you don't get

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<v Speaker 1>to see this this impressive lake of lava any greater,

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<v Speaker 1>you can you can imagine it, like the landscape still

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<v Speaker 1>speaks of it. Uh. The landscape looks like the top

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<v Speaker 1>of of of of a sheet of brownies, you know

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<v Speaker 1>that is cooled and has therefore um um you know

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<v Speaker 1>broken as it's kind of collapse, because that's essentially what

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<v Speaker 1>happened with the with the lake of lava as this uh,

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<v Speaker 1>as the surface drops down and cracks open. Uh, it's

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<v Speaker 1>it's just a wonderful, dynamic landscape that that not only

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<v Speaker 1>I mean, on one level it feels like a place

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<v Speaker 1>that is not Earth, But on another level, it's like

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<v Speaker 1>it's this wonderful, almost holy insight into like just how

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<v Speaker 1>dynamic the planet is and how alive our planet is.

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<v Speaker 1>Now to to sort of get to the point of

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<v Speaker 1>the episode, though, I guess, yeah, the idea of a

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<v Speaker 1>lake of lava, a sea of lava, or you know,

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<v Speaker 1>certainly think of any footage you've you've seen of lava

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<v Speaker 1>flows when when rock becomes more or less like a liquid,

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<v Speaker 1>we can't help but imagine the fantastic possibilities, right ships, uh,

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<v Speaker 1>sailing on a sea of lava, boats riding rivers of fire,

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<v Speaker 1>cartoon characters surfing down lava on some sort of fantastic surfboard.

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<v Speaker 1>I think one of the most um you know, obvious

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<v Speaker 1>and perhaps outrageous examples that I can think too, comes

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<v Speaker 1>from the first season of The Mandalorian, the Star Wars

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<v Speaker 1>television series, in which we see our heroes ride a

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<v Speaker 1>droid piloted large down a subterranean canal of lava, which

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<v Speaker 1>I think is also supposed to be part of like

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<v Speaker 1>the sewage system. I'm not sure exactly how this uh,

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<v Speaker 1>how this planet um is really using. It's it's lava here,

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<v Speaker 1>but it's it's a fun it's a fun steement like

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<v Speaker 1>within the fantasy of the show. It's it's really cool.

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<v Speaker 1>It's very you know, it's very hellish. It's kind of like,

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<v Speaker 1>you know, the river sticks meets lava and and and

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<v Speaker 1>here's here's some sort of a ridiculous droid, you know,

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<v Speaker 1>in the in the back of the barge pushing it along.

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<v Speaker 1>Um And then I guess this sort of thing happens

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<v Speaker 1>in a lot of video games. I'm thinking, like, surely

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<v Speaker 1>this happens in Mario, right, Oh yeah, yeah, definitely. In

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<v Speaker 1>Super Mario sixty four there's there's at least a couple

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<v Speaker 1>of levels with things floating around in lava, and the

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<v Speaker 1>one for the Super Nintendo I think also when you

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<v Speaker 1>get towards the end, closer to Bowser's Palace, there's there's

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<v Speaker 1>stuff floating around in lava a lot. Yeah, it just

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<v Speaker 1>makes sense. You gotta have your you gotta have your

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<v Speaker 1>lava levels, and just about any video game it's bad stuff. Yeah,

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<v Speaker 1>it's bad, guys said, Yeah, I mean, you look at

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<v Speaker 1>other movies where where does the bad guy build his

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<v Speaker 1>layer and it's in a volcano of course, right. Um.

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<v Speaker 1>We even talked about one recently on the Weird House Cinema.

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<v Speaker 1>There was the Hercules movie where we had we had

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<v Speaker 1>the villain uh using a hideout in a volcano, and

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<v Speaker 1>of course the final showdown takes place within the volcano

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<v Speaker 1>over a lake of lava. Oh yeah, what was the

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<v Speaker 1>funny thing about the sword there or something? Oh, there

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<v Speaker 1>were multiple funny things going on, but yeah, that they

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<v Speaker 1>had that was where the rainbow sword. You know, he

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<v Speaker 1>had a rainbow sword, and then there was the sword

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<v Speaker 1>that could that was holding the phoenix in place. There

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<v Speaker 1>was a lot going on in that particular volcanic layer.

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<v Speaker 1>Now I was looking around for other examples of this

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<v Speaker 1>sort of trope. I went to TV tropes dot com,

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<v Speaker 1>which is always a fun place to bruse this sort

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<v Speaker 1>of thing. I was reminded that, Um, in The Hobbit

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<v Speaker 1>The Desolation of Smog, this being the second Hobbit film

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<v Speaker 1>from Peter Jackson, there's a scene where Thorn rides a

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<v Speaker 1>wheelbarrow on molten gold um sort of surfing in it.

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<v Speaker 1>I I had completely forgotten about this whole this whole

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<v Speaker 1>sequence in the movie where they add this bit where

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<v Speaker 1>they try to defeed the dragon by um covering him

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<v Speaker 1>with molten gold. Oh, I don't remember that either. I

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<v Speaker 1>did see that movie somehow. Yeah, I just saw it

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<v Speaker 1>last year, and I kind of blanked out on all this,

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<v Speaker 1>But then after I read about it, like, okay, I

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<v Speaker 1>vaguely remember that because it's kind of a pretty scene

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<v Speaker 1>where the dragon gets covered in gold, but then it

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<v Speaker 1>cracks the gold and he's free from the gold. They

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<v Speaker 1>ripped that straight out of the end of Alien three,

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<v Speaker 1>that's right. Yeah, what do they cover liquid lead or something? Yeah, yeah,

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<v Speaker 1>it's the lead works and they covered the alien and

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<v Speaker 1>I guess it's lead. It's some kind of molten metal,

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<v Speaker 1>and then you think it's dead, but then it just

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<v Speaker 1>jumps out. Oh yeah, it certainly wasn't in the book.

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<v Speaker 1>I don't remember that in the Hobbit novel at all. No. Well,

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<v Speaker 1>I also don't remember in the Hobbit novel. In the novel,

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<v Speaker 1>did they like ride barrels down the river? Is that

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<v Speaker 1>in there? Yeah, they did ride barrels. I do remember

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<v Speaker 1>the barrel the row where they rode in barrels. They

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<v Speaker 1>were kind of I think everybody was corrected everybody, but

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<v Speaker 1>the Bilbo was like sealed up and then I think

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<v Speaker 1>they were all, you know, pretty seasick in there. But

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<v Speaker 1>um but I do remember that happening now. I also

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<v Speaker 1>read on TV Tropes that there's a there's a book

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<v Speaker 1>in the Culture series by n In Banks that Look

0:12:13.480 --> 0:12:15.760
<v Speaker 1>to Windward, which is what I have, but I haven't

0:12:15.760 --> 0:12:19.040
<v Speaker 1>read yet. It's apparently mentioned that lava rafting is an

0:12:19.040 --> 0:12:23.000
<v Speaker 1>extreme sport that citizens of the Culture participate in on

0:12:23.200 --> 0:12:27.600
<v Speaker 1>unfinished habitats. So it sounds that sounds on brand with

0:12:27.679 --> 0:12:30.160
<v Speaker 1>the sort of thing that people of the culture would do.

0:12:30.520 --> 0:12:35.080
<v Speaker 1>It's a moderately extreme sport. Yeah, yeah. Now, one thing

0:12:35.120 --> 0:12:37.559
<v Speaker 1>that's worth pointing out about about these examples and plenty

0:12:37.559 --> 0:12:41.280
<v Speaker 1>of other examples, is that very often, whether you're playing

0:12:41.280 --> 0:12:44.280
<v Speaker 1>a video game or watching a movie, you find something

0:12:44.320 --> 0:12:47.720
<v Speaker 1>kind of interesting about molten lava. In in fiction, molten

0:12:47.840 --> 0:12:51.360
<v Speaker 1>lava only seems dangerous if you come into physical contact

0:12:51.440 --> 0:12:54.880
<v Speaker 1>with it. So if you fall into it or um

0:12:55.000 --> 0:12:57.960
<v Speaker 1>or it's poured over you that sort of resinc you know,

0:12:58.040 --> 0:13:01.080
<v Speaker 1>into the lake of lava, then you're oomed. But if

0:13:01.120 --> 0:13:04.119
<v Speaker 1>you're just standing next to it or in close proximity

0:13:04.160 --> 0:13:06.480
<v Speaker 1>to it, you're fine, which of course would not be

0:13:06.520 --> 0:13:09.600
<v Speaker 1>the case because lava is extremely hot, as we'll get

0:13:09.600 --> 0:13:13.120
<v Speaker 1>into in this episode. Yeah, that is funny. So they

0:13:13.200 --> 0:13:15.719
<v Speaker 1>treated as like it's like Hollywood acid. It's as if

0:13:15.760 --> 0:13:19.200
<v Speaker 1>it only harms you by direct contact chemical reaction. But

0:13:19.240 --> 0:13:21.760
<v Speaker 1>of course, you know, a real lake of lava or

0:13:21.840 --> 0:13:25.800
<v Speaker 1>river of flowing molten lava that would be so hot

0:13:25.880 --> 0:13:29.199
<v Speaker 1>that it is superheating the air directly above it. So

0:13:29.360 --> 0:13:32.000
<v Speaker 1>like that would be, you know, being above a lake

0:13:32.040 --> 0:13:34.040
<v Speaker 1>of lava. I don't know exactly how hot it would be,

0:13:34.080 --> 0:13:36.520
<v Speaker 1>but it would be to some extent like getting right

0:13:36.559 --> 0:13:39.800
<v Speaker 1>next to a heating element of a broiler. Yeah. Yeah,

0:13:39.800 --> 0:13:42.160
<v Speaker 1>we're talking pretty hot, and we'll bust out some temperatures

0:13:42.200 --> 0:13:44.440
<v Speaker 1>here in a bit, but it's it's a fire chive

0:13:44.520 --> 0:13:47.040
<v Speaker 1>from sort of the floor is lava scenario, whether you're

0:13:47.040 --> 0:13:50.880
<v Speaker 1>talking about the Netflix game show or just the the

0:13:50.920 --> 0:13:54.880
<v Speaker 1>good old fashioned childhood version of this where the floor

0:13:55.000 --> 0:13:58.319
<v Speaker 1>is now we're imagining it is lava, and you can

0:13:58.400 --> 0:14:00.520
<v Speaker 1>as long as you don't touch it, you're mine. If

0:14:00.559 --> 0:14:03.280
<v Speaker 1>you make the jump from from the love seat to

0:14:03.280 --> 0:14:06.240
<v Speaker 1>the couch without touching the floor. Then you're fine. I

0:14:06.280 --> 0:14:07.880
<v Speaker 1>think the more act. If you want to play the

0:14:07.920 --> 0:14:09.720
<v Speaker 1>same game, but you want it to be more accurate,

0:14:09.720 --> 0:14:12.240
<v Speaker 1>it should be like the floor is spikes. There you go,

0:14:12.400 --> 0:14:14.320
<v Speaker 1>You know, like spikes. They don't hurt you unless you

0:14:14.400 --> 0:14:17.040
<v Speaker 1>actually like get on them and put your weight on them.

0:14:17.679 --> 0:14:20.440
<v Speaker 1>What kind of gory kids are playing the floor is spikes? Though,

0:14:20.680 --> 0:14:26.760
<v Speaker 1>you know somehow it's worse. It's worse. I want my

0:14:26.920 --> 0:14:31.560
<v Speaker 1>kids imagining wholesome charring down to the bone, complete just

0:14:31.720 --> 0:14:35.320
<v Speaker 1>incineration of their flesh turning into a puff of carbon

0:14:35.440 --> 0:14:37.320
<v Speaker 1>that goes up into the air. You know. One of

0:14:37.360 --> 0:14:39.600
<v Speaker 1>the weird things about this is that I know that

0:14:39.800 --> 0:14:42.160
<v Speaker 1>Flora's Lava is the most popular of the childhood games.

0:14:42.160 --> 0:14:44.880
<v Speaker 1>Did you play Flora's Lava as a child? Oh? Absolutely?

0:14:44.920 --> 0:14:48.040
<v Speaker 1>I mean I don't know if most often we said

0:14:48.080 --> 0:14:49.960
<v Speaker 1>it was lava or we said that it was like,

0:14:50.320 --> 0:14:53.720
<v Speaker 1>you know, swamp water with alligators in it, or or whatever.

0:14:53.760 --> 0:14:56.840
<v Speaker 1>But we definitely played the games of can't touch the floor,

0:14:56.920 --> 0:14:58.760
<v Speaker 1>got to stay on the furniture because it is some

0:14:58.880 --> 0:15:01.840
<v Speaker 1>kind of hazard. See, we would often do and I

0:15:01.880 --> 0:15:03.560
<v Speaker 1>have no idea where we got this. We would do

0:15:03.600 --> 0:15:05.600
<v Speaker 1>the floor as an never ending pit. And I'm not

0:15:05.640 --> 0:15:07.680
<v Speaker 1>sure where we got the idea of a never ending

0:15:07.680 --> 0:15:11.359
<v Speaker 1>pit from. I'm trying to think back on well, what

0:15:11.360 --> 0:15:13.280
<v Speaker 1>what would I have been watching at the time, Like

0:15:13.320 --> 0:15:16.000
<v Speaker 1>what movies had a never ending pit in them? And

0:15:16.360 --> 0:15:19.640
<v Speaker 1>I don't really remember what specifically we could be referring

0:15:19.640 --> 0:15:21.960
<v Speaker 1>to their this the version of the game played by

0:15:21.960 --> 0:15:25.000
<v Speaker 1>a philosopher's child, you know, the real threat to them

0:15:25.040 --> 0:15:27.080
<v Speaker 1>is that they'll fall forever and be a left alone

0:15:27.080 --> 0:15:29.400
<v Speaker 1>with their thoughts. Well, I would think about this. Maybe

0:15:29.400 --> 0:15:31.360
<v Speaker 1>it had something, you know, maybe it had something to

0:15:31.400 --> 0:15:34.200
<v Speaker 1>do with the Masters of the Universe movie, where there's

0:15:34.200 --> 0:15:36.840
<v Speaker 1>like a never ending pit underneath Eternea, or it's supposed

0:15:36.880 --> 0:15:38.320
<v Speaker 1>to be a never ending pit. I don't know even

0:15:38.320 --> 0:15:40.520
<v Speaker 1>though if they describe it as such, or maybe I

0:15:40.800 --> 0:15:42.640
<v Speaker 1>just had this idea of a never ending pit in

0:15:42.720 --> 0:15:44.920
<v Speaker 1>my head and just assume that that's what it was.

0:15:45.320 --> 0:15:46.880
<v Speaker 1>You know, we're really getting on a tangent. But I

0:15:46.920 --> 0:15:48.640
<v Speaker 1>will say I think a lot of the terror of

0:15:48.680 --> 0:15:51.480
<v Speaker 1>the idea of a bottomless pit comes at the idea

0:15:51.560 --> 0:15:54.440
<v Speaker 1>of people imagining the very beginning of a fall where

0:15:54.480 --> 0:15:58.040
<v Speaker 1>you're accelerating towards terminal velocity, and it's that feeling of

0:15:58.120 --> 0:16:00.280
<v Speaker 1>you're going faster and faster as you followed out and

0:16:00.280 --> 0:16:03.400
<v Speaker 1>it's really scary. But actually, pretty quickly you hit terminal

0:16:03.440 --> 0:16:05.960
<v Speaker 1>velocity and then you would you would basically equalize, so

0:16:06.000 --> 0:16:08.640
<v Speaker 1>the acceleration stops, and then you're just floating in the

0:16:08.680 --> 0:16:11.200
<v Speaker 1>air forever. So it is like a it is like

0:16:11.200 --> 0:16:13.880
<v Speaker 1>a sensory deprivation tank that you just get to stay

0:16:13.920 --> 0:16:17.080
<v Speaker 1>in for for the rest of your life. Well, anyway,

0:16:17.120 --> 0:16:19.480
<v Speaker 1>we could keep going on this, but uh, but I

0:16:19.520 --> 0:16:21.200
<v Speaker 1>thought that this all might be a good place to

0:16:21.280 --> 0:16:24.560
<v Speaker 1>jump off and talk about the idea of lava boats,

0:16:25.400 --> 0:16:27.920
<v Speaker 1>both in terms of what we might loosely think of

0:16:27.960 --> 0:16:30.120
<v Speaker 1>as actual lava boats, and we'll break that down a

0:16:30.160 --> 0:16:33.440
<v Speaker 1>little bit, but we'll also even get into some considerations

0:16:33.440 --> 0:16:36.680
<v Speaker 1>of what could be possible if you were just really

0:16:36.760 --> 0:16:41.160
<v Speaker 1>insistent on on creating a human constructed vessel that can

0:16:41.200 --> 0:16:43.800
<v Speaker 1>withstand a lake of lava. Well, how might you go

0:16:43.840 --> 0:16:52.560
<v Speaker 1>about that? We'll get into that as well. Thank now, Rob,

0:16:52.640 --> 0:16:54.960
<v Speaker 1>I know that what you have in mind when you

0:16:55.000 --> 0:16:57.680
<v Speaker 1>say a lava boat is what we're talking about is

0:16:57.720 --> 0:17:00.840
<v Speaker 1>a boat that can float on lava. But my brain

0:17:00.880 --> 0:17:04.239
<v Speaker 1>went in a different direction with this, which was not

0:17:04.400 --> 0:17:08.520
<v Speaker 1>a boat floating in lava, but a boat made of lava,

0:17:08.680 --> 0:17:12.200
<v Speaker 1>or more specifically, of a type of volcanic rock known

0:17:12.240 --> 0:17:15.919
<v Speaker 1>as pummice. Will you go on this strange journey with me?

0:17:16.280 --> 0:17:17.840
<v Speaker 1>Oh yeah, I mean, when you decided to do a

0:17:17.840 --> 0:17:20.760
<v Speaker 1>whole episode about lava boats, you take what you can get.

0:17:21.320 --> 0:17:22.720
<v Speaker 1>This is kind of this is kind of the This

0:17:22.800 --> 0:17:28.040
<v Speaker 1>American Life, um uh principle of podcasting. You know, you

0:17:28.040 --> 0:17:30.960
<v Speaker 1>know an American and This American Life. You know, they're

0:17:30.960 --> 0:17:33.000
<v Speaker 1>gonna have a certain theme, and not every segment of

0:17:33.040 --> 0:17:35.879
<v Speaker 1>the episode is going to really match up with whatever

0:17:35.880 --> 0:17:38.960
<v Speaker 1>that theme happens to be. But but you know, it's

0:17:38.960 --> 0:17:41.320
<v Speaker 1>a it's a guiding principle for the episode. Well, I

0:17:41.320 --> 0:17:43.480
<v Speaker 1>think this one puts us in places that are that

0:17:43.520 --> 0:17:45.960
<v Speaker 1>are just as awesome and weird as looking at the

0:17:46.040 --> 0:17:48.919
<v Speaker 1>lake of lava and imagining floating on it. Let's do it,

0:17:48.960 --> 0:17:53.399
<v Speaker 1>Let's go there. Okay. So pummis is a very unique

0:17:53.440 --> 0:17:57.600
<v Speaker 1>and interesting rock which has the strange distinction of being

0:17:57.720 --> 0:18:01.640
<v Speaker 1>so low in density that it can often actually float

0:18:01.720 --> 0:18:04.280
<v Speaker 1>on the surface of water. If you you may have

0:18:04.320 --> 0:18:07.400
<v Speaker 1>observed this yourself, if you ever had like a pumice

0:18:07.400 --> 0:18:10.080
<v Speaker 1>stone in the bathtub or something. But if you've never

0:18:10.119 --> 0:18:11.840
<v Speaker 1>seen this, you can look up plenty of video. It

0:18:12.160 --> 0:18:14.720
<v Speaker 1>exists all over the internet. Or you can even try

0:18:14.720 --> 0:18:17.040
<v Speaker 1>it for yourself. You can get a handful of pumice stones,

0:18:17.280 --> 0:18:20.040
<v Speaker 1>throw them into a bathtub or you know, tub of water,

0:18:20.160 --> 0:18:22.800
<v Speaker 1>sink full of water, and there's a very good chance

0:18:22.840 --> 0:18:26.240
<v Speaker 1>that they will float like styrofoam, though you may get

0:18:26.280 --> 0:18:28.960
<v Speaker 1>some duds. I think not all pumice stones float, but

0:18:29.000 --> 0:18:33.760
<v Speaker 1>a lot do. Now quite famously, almost all rocks sink

0:18:33.880 --> 0:18:36.480
<v Speaker 1>in water. So how why is this one different? How

0:18:36.480 --> 0:18:38.960
<v Speaker 1>does this rock end up being the one that is

0:18:39.000 --> 0:18:43.159
<v Speaker 1>able to float on the water surface. Well, pummice is

0:18:43.200 --> 0:18:46.959
<v Speaker 1>a type of igneous rock, igneous meaning formed in fire.

0:18:47.160 --> 0:18:50.280
<v Speaker 1>So this is a rock that's usually a byproduct of

0:18:50.680 --> 0:18:54.760
<v Speaker 1>violent or explosive volcanic eruptions. And I say violent or

0:18:54.800 --> 0:18:59.840
<v Speaker 1>explosive as opposed to the slower, more gentle volcanic eruptions

0:19:00.119 --> 0:19:02.639
<v Speaker 1>that you would typically see producing the things we've been

0:19:02.640 --> 0:19:05.000
<v Speaker 1>talking about, you know, the rivers of molten lava on

0:19:05.040 --> 0:19:07.680
<v Speaker 1>the surface, or the stuff you'd see in the famous

0:19:07.760 --> 0:19:10.160
<v Speaker 1>lava lake footage from Hawaii. A lot of the Hawaiian

0:19:10.240 --> 0:19:13.760
<v Speaker 1>eruptions we picture are are the more gentle types of eruptions,

0:19:14.280 --> 0:19:17.719
<v Speaker 1>but more explosive or violent volcanic eruptions, which those are

0:19:17.720 --> 0:19:19.800
<v Speaker 1>the ones you'll typically see producing more of a kind

0:19:19.800 --> 0:19:23.160
<v Speaker 1>of uh an ash cloud like a column rising into

0:19:23.160 --> 0:19:27.439
<v Speaker 1>the sky. Very sudden eruptions um these are more likely

0:19:27.480 --> 0:19:30.920
<v Speaker 1>to release a lot of pummice. I think. Another characteristic

0:19:31.040 --> 0:19:34.200
<v Speaker 1>of pumice forming eruptions is that they tend to happen

0:19:34.680 --> 0:19:38.600
<v Speaker 1>in places where the magma is richer in silica, which

0:19:38.640 --> 0:19:41.080
<v Speaker 1>tends to make it more viscous. So you can think

0:19:41.119 --> 0:19:44.359
<v Speaker 1>about the different kinds of magma here. The magma that

0:19:44.440 --> 0:19:48.119
<v Speaker 1>leads to a highly pummus forming eruption is usually going

0:19:48.160 --> 0:19:52.479
<v Speaker 1>to be thicker or stickier magma. But how does it

0:19:52.520 --> 0:19:56.320
<v Speaker 1>turn into a rock that can float? So if you

0:19:56.359 --> 0:20:00.760
<v Speaker 1>imagine molten rock trapped underneath the Earth's surface, this magma

0:20:00.800 --> 0:20:04.840
<v Speaker 1>down there is actually not just composed of melted rock.

0:20:05.280 --> 0:20:09.800
<v Speaker 1>It also contains various fluids in solution, so it might

0:20:09.840 --> 0:20:13.639
<v Speaker 1>contain dissolved water, vapor or c O two sometimes I

0:20:13.680 --> 0:20:19.320
<v Speaker 1>think sulfur dioxide, and these gases are are all kept

0:20:19.359 --> 0:20:23.000
<v Speaker 1>dissolved in the magma because the magma is under very

0:20:23.080 --> 0:20:26.200
<v Speaker 1>high pressure. It's underneath the ground. So you can think

0:20:26.200 --> 0:20:28.960
<v Speaker 1>about the way that the CEO two dissolved in a

0:20:29.080 --> 0:20:33.560
<v Speaker 1>carbonated beverage stays in solution until the can or the

0:20:33.600 --> 0:20:37.280
<v Speaker 1>bottle is opened, and then the release of pressure allows

0:20:37.320 --> 0:20:40.080
<v Speaker 1>some of that CEO too to start coming out of solution,

0:20:40.520 --> 0:20:43.320
<v Speaker 1>turning back into gas, and to start, you know, it

0:20:43.359 --> 0:20:45.159
<v Speaker 1>starts floating to the top of the drink in the

0:20:45.200 --> 0:20:48.760
<v Speaker 1>form of bubbles. That's because you have undone the pressure

0:20:48.800 --> 0:20:51.560
<v Speaker 1>of the closed container. And it turns out that the

0:20:51.600 --> 0:20:54.440
<v Speaker 1>process leading to the formation of pumus during a volcanic

0:20:54.520 --> 0:20:57.439
<v Speaker 1>eruption is actually pretty similar to what happens when you

0:20:57.520 --> 0:21:01.960
<v Speaker 1>open a carbonated beverage, except it involves an extra step,

0:21:01.960 --> 0:21:05.400
<v Speaker 1>which is sort of the freezing of that that frothing

0:21:05.480 --> 0:21:08.760
<v Speaker 1>foamy product. So the process goes like this. You've got

0:21:08.760 --> 0:21:11.760
<v Speaker 1>magma trapped beneath the earth surface and it's got all

0:21:11.800 --> 0:21:14.480
<v Speaker 1>this gas dissolved in it, and the gas again is

0:21:14.520 --> 0:21:17.320
<v Speaker 1>kept in solution by high pressure, and then there is

0:21:17.359 --> 0:21:20.720
<v Speaker 1>a volcanic eruption in effect that the soda can is opened,

0:21:21.200 --> 0:21:24.000
<v Speaker 1>the magma rushes to the surface where there is rapid

0:21:24.080 --> 0:21:28.320
<v Speaker 1>depressurre ization. And now because the pressure is lower, the

0:21:28.440 --> 0:21:32.720
<v Speaker 1>dissolved CO two and water and other gases they bolt

0:21:32.800 --> 0:21:35.800
<v Speaker 1>from solution and they start wanting to turn into gas,

0:21:35.840 --> 0:21:39.040
<v Speaker 1>forming into bubbles. But at the very same time that

0:21:39.040 --> 0:21:41.479
<v Speaker 1>the pressure is relieved and the gas wants to come

0:21:41.480 --> 0:21:44.399
<v Speaker 1>out of solution and turn into bubbles, the magma is

0:21:44.440 --> 0:21:48.760
<v Speaker 1>also cooling really rapidly. In effect, it is freezing the

0:21:48.880 --> 0:21:51.840
<v Speaker 1>rock in place, and so what you end up with

0:21:52.160 --> 0:21:55.800
<v Speaker 1>is a rock that is filled with what geologists called vesicles.

0:21:56.200 --> 0:21:59.760
<v Speaker 1>These are little bubbles and hollows created by the deep

0:21:59.760 --> 0:22:03.200
<v Speaker 1>pre surized to gases that are sort of locked into

0:22:03.240 --> 0:22:07.040
<v Speaker 1>crystal and form because the rock was cooling rapidly at

0:22:07.040 --> 0:22:09.919
<v Speaker 1>the same time that all these bubbles were forming. And

0:22:09.960 --> 0:22:11.840
<v Speaker 1>what you get is a rock that's sort of the

0:22:12.200 --> 0:22:15.159
<v Speaker 1>rock equivalent of if you took the foamy head of

0:22:15.160 --> 0:22:17.959
<v Speaker 1>a beer and froze it. Yeah, and you know this

0:22:18.040 --> 0:22:21.880
<v Speaker 1>is this is something you can actually if you were

0:22:21.920 --> 0:22:25.520
<v Speaker 1>to pick up various lava rocks, you'll find that they

0:22:25.520 --> 0:22:28.479
<v Speaker 1>are lighter than you might think for this very reason,

0:22:28.560 --> 0:22:31.320
<v Speaker 1>because they have all of these little little hollow pockets

0:22:31.320 --> 0:22:33.960
<v Speaker 1>in them. Uh, you know, there were essentially you know,

0:22:34.000 --> 0:22:36.760
<v Speaker 1>little pockets of gas. Yes, though though of course you

0:22:36.800 --> 0:22:39.240
<v Speaker 1>can end up with very different kinds of lava rock,

0:22:39.359 --> 0:22:41.000
<v Speaker 1>but a lot of them are like this, yeah, that

0:22:41.040 --> 0:22:44.040
<v Speaker 1>they they've got this this lower density than other types

0:22:44.080 --> 0:22:46.360
<v Speaker 1>of rock, I think, But it depends on a lot

0:22:46.359 --> 0:22:48.680
<v Speaker 1>of It depends on like the composition of the magma,

0:22:49.119 --> 0:22:53.600
<v Speaker 1>the conditions under which the lava cooled once it was

0:22:53.640 --> 0:22:55.639
<v Speaker 1>on the surface, and things like that. So so you

0:22:55.680 --> 0:22:58.000
<v Speaker 1>can end up with a lot of different products. But

0:22:58.400 --> 0:23:01.280
<v Speaker 1>pummus is one of these, and pummice is is very

0:23:01.320 --> 0:23:03.800
<v Speaker 1>low density, so you can end up with this very

0:23:03.840 --> 0:23:06.440
<v Speaker 1>low density rock that it's that's full of these little

0:23:06.520 --> 0:23:08.760
<v Speaker 1>vesicles that allow it to float on the surface of

0:23:08.760 --> 0:23:11.760
<v Speaker 1>the water. Uh though though I do think over time

0:23:12.280 --> 0:23:15.560
<v Speaker 1>pummice tends to get water logged and lose its buoyancy,

0:23:15.600 --> 0:23:17.280
<v Speaker 1>but that can take a long time, so you can

0:23:17.680 --> 0:23:20.320
<v Speaker 1>get a pummice rock that you know, it remains buoyant

0:23:20.359 --> 0:23:23.840
<v Speaker 1>for for years after after the time it's created. But anyway,

0:23:24.000 --> 0:23:27.480
<v Speaker 1>coming back around to the idea of lava boats, I

0:23:27.520 --> 0:23:30.680
<v Speaker 1>think the really amazing thing about the ability of pummice

0:23:30.720 --> 0:23:34.840
<v Speaker 1>to float is that when large masses of pummice are

0:23:34.840 --> 0:23:39.080
<v Speaker 1>all formed together, they can all float together, leading to

0:23:39.400 --> 0:23:44.200
<v Speaker 1>a phenomenon known as pummice rafts. So as one example

0:23:44.240 --> 0:23:46.560
<v Speaker 1>of this, I was looking at a BBC article from

0:23:46.600 --> 0:23:53.160
<v Speaker 1>twenty nineteen called vast pummice raft found drifting through Pacific Ocean. Yeah,

0:23:53.400 --> 0:23:56.639
<v Speaker 1>this is really incredibly includes footage that is also quite

0:23:57.359 --> 0:23:59.560
<v Speaker 1>quite fascinating. Oh yeah, well we'll get to that in

0:23:59.600 --> 0:24:02.720
<v Speaker 1>a second. So in August of twenty nineteen, there were

0:24:02.760 --> 0:24:07.440
<v Speaker 1>some Australian sailors that reported the discovery of a gigantic

0:24:08.080 --> 0:24:12.359
<v Speaker 1>raft of floating pummice stones in the Pacific Ocean. This

0:24:12.480 --> 0:24:16.120
<v Speaker 1>was out on the open sea east of Fiji, and

0:24:16.160 --> 0:24:18.760
<v Speaker 1>the story is that it was a couple of Australian

0:24:18.840 --> 0:24:23.119
<v Speaker 1>sailors who were traveling between islands in a catamaran and

0:24:23.200 --> 0:24:27.800
<v Speaker 1>they accidentally piloted into this field of floating stones in

0:24:27.840 --> 0:24:29.719
<v Speaker 1>the middle of the night. So I think that they

0:24:29.760 --> 0:24:32.320
<v Speaker 1>didn't see what they were getting into, but then they

0:24:32.359 --> 0:24:36.400
<v Speaker 1>realized something was up and the raft of stones apparently

0:24:36.440 --> 0:24:40.120
<v Speaker 1>slowed the vessel down and greatly reduced the wave action

0:24:40.280 --> 0:24:44.160
<v Speaker 1>on the surface of the water. And the sailors investigated.

0:24:44.200 --> 0:24:46.320
<v Speaker 1>They looked out in the moonlight and they shine their

0:24:46.359 --> 0:24:49.359
<v Speaker 1>spotlight to try to see what was going on, and

0:24:49.600 --> 0:24:53.359
<v Speaker 1>saw this rock field in the water that extended as

0:24:53.400 --> 0:24:56.959
<v Speaker 1>far as they could see. And at first the pummice

0:24:57.080 --> 0:24:59.119
<v Speaker 1>jammed their rudder, so it made it hard for them

0:24:59.160 --> 0:25:01.119
<v Speaker 1>to steer, and they thought there might be stuck. But

0:25:01.160 --> 0:25:03.720
<v Speaker 1>eventually they were able to get out of the raft zone.

0:25:04.640 --> 0:25:06.840
<v Speaker 1>And when you hear the dimensions of this thing, and

0:25:06.920 --> 0:25:10.560
<v Speaker 1>especially when you see what a giant pumice raft looks like,

0:25:10.920 --> 0:25:14.600
<v Speaker 1>you can imagine how strange and frightening of an experience

0:25:14.640 --> 0:25:17.800
<v Speaker 1>this might have been. So at the time of the article,

0:25:18.000 --> 0:25:20.679
<v Speaker 1>it was estimated that this pumice raft was about a

0:25:20.720 --> 0:25:25.160
<v Speaker 1>hundred and fifty square kilometers or fifty eight square miles,

0:25:25.200 --> 0:25:28.959
<v Speaker 1>which the article says is roughly equivalent to twenty thousand

0:25:29.040 --> 0:25:32.439
<v Speaker 1>football fields. Though this is BBC, so I think that

0:25:32.520 --> 0:25:35.320
<v Speaker 1>is what we would we would call soccer, not football.

0:25:35.480 --> 0:25:40.479
<v Speaker 1>It's still soccer fields and amazing. I was looking up

0:25:40.520 --> 0:25:44.800
<v Speaker 1>countries by land area for comparison, and so this raft

0:25:44.840 --> 0:25:46.800
<v Speaker 1>would indeed be larger than a bunch of the world's

0:25:46.840 --> 0:25:50.960
<v Speaker 1>smallest countries. It's roughly the same area as the British

0:25:51.000 --> 0:25:57.399
<v Speaker 1>Virgin Islands or Lichtenstein, but There are various videos you

0:25:57.440 --> 0:26:00.680
<v Speaker 1>can look up taken from people on boats who have

0:26:00.760 --> 0:26:02.600
<v Speaker 1>gotten into one of these rafts, and by the way,

0:26:02.600 --> 0:26:05.119
<v Speaker 1>that is not recommended. Multiple sources I was looking at

0:26:05.160 --> 0:26:08.800
<v Speaker 1>were saying that sailing into a pumus raft area can

0:26:08.840 --> 0:26:11.560
<v Speaker 1>be dangerous and advising people not to try it. But

0:26:11.880 --> 0:26:15.560
<v Speaker 1>people had taken video of this, and it's almost too

0:26:15.560 --> 0:26:18.520
<v Speaker 1>weird to describe. One video I found that was, you know,

0:26:18.960 --> 0:26:22.440
<v Speaker 1>relinked all over the internet. It looks like the ship

0:26:22.680 --> 0:26:27.560
<v Speaker 1>is sitting in an enormous desert or gravel parking lot,

0:26:28.040 --> 0:26:31.040
<v Speaker 1>except the parking lot extends all the way to the

0:26:31.080 --> 0:26:36.040
<v Speaker 1>horizon and it is undulating with waves like the ocean,

0:26:36.359 --> 0:26:41.640
<v Speaker 1>because it is the ocean. Just absolutely hallucinogenic apocalyptic imagery.

0:26:41.640 --> 0:26:45.320
<v Speaker 1>If you can just imagine a moving, rippling parking lot

0:26:45.440 --> 0:26:48.399
<v Speaker 1>that goes as far as you can see. Yeah, I mean,

0:26:48.440 --> 0:26:50.720
<v Speaker 1>it's almost it's like they sailed into a tool video

0:26:50.800 --> 0:26:53.879
<v Speaker 1>or something. It's and it does seem to stretch to

0:26:53.880 --> 0:26:56.120
<v Speaker 1>the horizon. It's just yeah, it's like it's it's if

0:26:56.200 --> 0:26:58.760
<v Speaker 1>you can imagine the sun coming up and you find

0:26:58.760 --> 0:27:01.320
<v Speaker 1>yourself in this boat on such a sea, It's like

0:27:01.359 --> 0:27:03.680
<v Speaker 1>something out of a rhyme of the ancient mariner. Oh

0:27:03.720 --> 0:27:06.080
<v Speaker 1>totally like, yeah, you just want to get out of here,

0:27:06.200 --> 0:27:09.760
<v Speaker 1>unhand me gray beard loon um. But according to this

0:27:09.880 --> 0:27:13.679
<v Speaker 1>BBC report, the geoscientists that they consulted said that the

0:27:13.680 --> 0:27:18.600
<v Speaker 1>pumice raft discovered in August nineteen was probably created by

0:27:18.680 --> 0:27:23.919
<v Speaker 1>the eruption of an underwater volcano near Tonga earlier that month,

0:27:24.880 --> 0:27:28.119
<v Speaker 1>and the rocks in this raft very greatly in size.

0:27:28.160 --> 0:27:30.439
<v Speaker 1>A lot of them appear to be sort of marble

0:27:30.640 --> 0:27:33.480
<v Speaker 1>or pebble sized, but others are big, you know, the

0:27:33.520 --> 0:27:36.840
<v Speaker 1>size of basketballs. And another weird thing is that this

0:27:36.880 --> 0:27:41.000
<v Speaker 1>is apparently not even that unusual. The article sitesay professor

0:27:41.080 --> 0:27:45.760
<v Speaker 1>named Scott Brian of the Queensland University of Technology saying

0:27:45.800 --> 0:27:49.720
<v Speaker 1>that big pummice rafts like this appear roughly once every

0:27:49.800 --> 0:27:53.639
<v Speaker 1>five years or so in the area due to volcanic eruptions,

0:27:54.600 --> 0:27:59.800
<v Speaker 1>and he interestingly links pumice rafts to historical reports of

0:28:00.440 --> 0:28:04.080
<v Speaker 1>islands in the ocean that people spot on one journey,

0:28:04.119 --> 0:28:06.240
<v Speaker 1>but then later say they can't find again when they

0:28:06.240 --> 0:28:09.320
<v Speaker 1>returned to the same place, So possibly some of these

0:28:09.359 --> 0:28:13.360
<v Speaker 1>observations were actually not land but floating rafts of low

0:28:13.400 --> 0:28:17.399
<v Speaker 1>density rock. That's fascinating because we we've discussed on past

0:28:17.480 --> 0:28:22.720
<v Speaker 1>in past episodes about how various mirages and optical effects

0:28:23.080 --> 0:28:27.400
<v Speaker 1>can can lead to the mis identification of of islands

0:28:27.400 --> 0:28:30.879
<v Speaker 1>where there are no islands. But but here's another possibility,

0:28:30.880 --> 0:28:33.199
<v Speaker 1>at least for for some reasons of the world, right,

0:28:33.320 --> 0:28:37.600
<v Speaker 1>especially in the Pacific, and like these these volcanic chain areas. Yeah, now,

0:28:37.600 --> 0:28:41.400
<v Speaker 1>these rafts don't last forever. They disintegrate over time. They

0:28:41.440 --> 0:28:44.800
<v Speaker 1>probably break up into smaller and smaller clusters and then

0:28:44.920 --> 0:28:49.360
<v Speaker 1>end up either sinking or being deposited on shores. But yeah,

0:28:49.400 --> 0:28:54.800
<v Speaker 1>it's a truly stunning active planet Earth to to see

0:28:54.840 --> 0:28:57.680
<v Speaker 1>these things. And I know what you're all wondering. And

0:28:57.760 --> 0:28:59.920
<v Speaker 1>I know you're thinking, Okay, since we're on the subject

0:29:00.040 --> 0:29:04.120
<v Speaker 1>of lava boats, you're thinking, could a pumice raft function

0:29:04.360 --> 0:29:07.440
<v Speaker 1>as an actual raft function as a boat? For me? Like?

0:29:07.680 --> 0:29:09.880
<v Speaker 1>Could I walk on it? Could I travel on it?

0:29:10.320 --> 0:29:14.160
<v Speaker 1>And I think generally like that would be the It

0:29:14.200 --> 0:29:17.880
<v Speaker 1>seems like they're the perfect scenario, right right, So from

0:29:17.920 --> 0:29:20.280
<v Speaker 1>everything I can tell, the answer to this is almost

0:29:20.360 --> 0:29:25.160
<v Speaker 1>always no. I did find a few pictures of scientists,

0:29:25.280 --> 0:29:28.680
<v Speaker 1>uh the sort of appearing to trudge around on a

0:29:28.720 --> 0:29:32.400
<v Speaker 1>pumice raft and what looks like very shallow water, but

0:29:32.520 --> 0:29:34.240
<v Speaker 1>I couldn't tell what was going on. There may be

0:29:34.320 --> 0:29:37.120
<v Speaker 1>some kind of special condition involved in this one scenario.

0:29:37.640 --> 0:29:40.560
<v Speaker 1>In general, I think most pumice rafts will no more

0:29:40.640 --> 0:29:43.800
<v Speaker 1>support your weight than would a floating clump of cheetos

0:29:43.840 --> 0:29:46.120
<v Speaker 1>on the surface of a swimming pool. It's just like

0:29:46.160 --> 0:29:48.120
<v Speaker 1>you just go right through it, so don't try it.

0:29:48.520 --> 0:29:50.920
<v Speaker 1>I think what would really be necessary in order for

0:29:50.960 --> 0:29:52.800
<v Speaker 1>it to support you would be some way for it

0:29:52.840 --> 0:29:55.640
<v Speaker 1>to like all be held together into a single mass.

0:29:55.680 --> 0:29:58.960
<v Speaker 1>But this is like, you know, it's like floating packing peanuts.

0:29:59.040 --> 0:30:01.720
<v Speaker 1>It's just like there's nothing to like form a solid

0:30:01.720 --> 0:30:04.959
<v Speaker 1>floor for you. M yeah, you'd have to somehow like

0:30:04.960 --> 0:30:08.040
<v Speaker 1>like lash it all together. I guess, right. Yeah, And well,

0:30:08.080 --> 0:30:09.760
<v Speaker 1>even if you were able to do that, I might

0:30:09.840 --> 0:30:14.680
<v Speaker 1>worry that it's not rigid enough, so like it could

0:30:14.680 --> 0:30:16.880
<v Speaker 1>turn into like a death trap, like you just jump

0:30:16.920 --> 0:30:19.120
<v Speaker 1>into a tarp that's on the water surface and it

0:30:19.280 --> 0:30:23.640
<v Speaker 1>closes around you. Yeah that sounds that sounds horrifying. But

0:30:23.640 --> 0:30:26.800
<v Speaker 1>but but just because the raft won't support anything the

0:30:26.840 --> 0:30:30.240
<v Speaker 1>size and density of a human being doesn't mean that

0:30:30.320 --> 0:30:34.280
<v Speaker 1>these don't carry other biological passengers. And in fact, there

0:30:34.400 --> 0:30:37.680
<v Speaker 1>is plenty of evidence that pumice rafts do exactly that,

0:30:37.680 --> 0:30:42.120
<v Speaker 1>that they may serve as a fast dispersal mechanism for

0:30:42.280 --> 0:30:46.880
<v Speaker 1>many kinds of smaller life forms, especially marine life, spreading

0:30:46.880 --> 0:30:50.640
<v Speaker 1>between different zones of the ocean and UH from coastal

0:30:50.720 --> 0:30:53.760
<v Speaker 1>regions to other coastal regions, sort of island to island.

0:30:54.400 --> 0:30:57.120
<v Speaker 1>For example. I was looking at one paper by Brian

0:30:57.200 --> 0:30:59.080
<v Speaker 1>at All. I think this is actually Scott Bran, the

0:30:59.120 --> 0:31:01.880
<v Speaker 1>same research u who was cited in that BBC article,

0:31:02.600 --> 0:31:05.760
<v Speaker 1>but a bunch of other authors published in pl Os

0:31:05.840 --> 0:31:11.480
<v Speaker 1>one in called rapid long distance dispersal by pumice rafting.

0:31:12.080 --> 0:31:16.240
<v Speaker 1>And here the authors note that actually pumice rafts make

0:31:16.400 --> 0:31:21.680
<v Speaker 1>a wonderful agent for transporting a big variety of marine

0:31:21.800 --> 0:31:25.360
<v Speaker 1>organisms from one place to another, uh for a number

0:31:25.360 --> 0:31:27.920
<v Speaker 1>of reasons. I mean, they've got these little vesicles in them, all,

0:31:27.920 --> 0:31:31.200
<v Speaker 1>these little hollows and holes and bubbles which make a

0:31:31.240 --> 0:31:34.760
<v Speaker 1>great place for tiny organisms and larvae of of larger

0:31:34.880 --> 0:31:39.560
<v Speaker 1>organisms to hide from predators while they're being transported across

0:31:39.600 --> 0:31:43.360
<v Speaker 1>the water. But anyway, they write, quote here we report

0:31:43.400 --> 0:31:47.400
<v Speaker 1>on a significant recent pumice rafting and long distance dispersal

0:31:47.440 --> 0:31:50.440
<v Speaker 1>event that occurred across the southwest Pacific following the two

0:31:50.520 --> 0:31:55.680
<v Speaker 1>thousand six explosive eruption of home Reef Volcano in Tonga Uh.

0:31:55.720 --> 0:31:58.520
<v Speaker 1>And they say according to their their research, they found

0:31:58.720 --> 0:32:02.760
<v Speaker 1>more than eighty species ease and a substantial biomass underwent

0:32:02.880 --> 0:32:06.120
<v Speaker 1>a more than five thousand kilometer journey in seven to

0:32:06.200 --> 0:32:09.720
<v Speaker 1>eight months by by way of this pumice raft. And

0:32:09.800 --> 0:32:12.920
<v Speaker 1>so that they include like some photos of pieces of

0:32:12.920 --> 0:32:16.880
<v Speaker 1>pumice salvage from from some of these floating rafts. And

0:32:17.040 --> 0:32:20.040
<v Speaker 1>it's funny how much life that they're just coated with

0:32:20.160 --> 0:32:22.560
<v Speaker 1>by the end. Like, so they have these photos where

0:32:22.600 --> 0:32:25.440
<v Speaker 1>they identify all the different life forms that are clinging

0:32:25.440 --> 0:32:36.240
<v Speaker 1>to these floating rocks. They've got braz Owen's anemones, mollusks, goose, barnacles, corals, cyanobacteria, macroalgae, uh,

0:32:36.760 --> 0:32:39.200
<v Speaker 1>some other things. I don't even know how to pronounce it.

0:32:39.400 --> 0:32:42.680
<v Speaker 1>Like these can become sort of these these rafts of

0:32:42.800 --> 0:32:46.080
<v Speaker 1>life going from place to place. Yeah, these are these

0:32:46.120 --> 0:32:49.520
<v Speaker 1>are impressive, Like all this just acreated life on the rock.

0:32:49.880 --> 0:32:53.400
<v Speaker 1>And I found another interesting relationship. This one just hypothetical,

0:32:53.440 --> 0:32:55.600
<v Speaker 1>I mean the previous like, it is clear that these

0:32:55.600 --> 0:32:59.120
<v Speaker 1>pumice rafts actually do harbor plenty of life forms and

0:32:59.160 --> 0:33:03.240
<v Speaker 1>transport them around in the ocean. But another interesting hypothesis

0:33:03.440 --> 0:33:07.280
<v Speaker 1>is that floating rafts of pumice could possibly have been

0:33:07.840 --> 0:33:12.720
<v Speaker 1>a good environment for the the origins of life on Earth.

0:33:13.200 --> 0:33:16.000
<v Speaker 1>This has argued, for example, in a paper I was

0:33:16.000 --> 0:33:19.520
<v Speaker 1>looking at from the journal Astrobiology by Martin D. Brazier.

0:33:19.600 --> 0:33:24.080
<v Speaker 1>At All Brazier, I think, is a professor at Oxford University,

0:33:24.280 --> 0:33:27.720
<v Speaker 1>and the paper is called pummics as a Remarkable substrate

0:33:27.800 --> 0:33:30.160
<v Speaker 1>for the Origin of life, And essentially the authors here

0:33:30.240 --> 0:33:32.880
<v Speaker 1>argue that floating rafts of pumice actually meet a lot

0:33:32.880 --> 0:33:35.840
<v Speaker 1>of the criteria that we would expect for the place

0:33:35.880 --> 0:33:39.240
<v Speaker 1>for life to first evolve on Earth. Uh. They give

0:33:39.240 --> 0:33:42.560
<v Speaker 1>a number of reasons, they say, uh related to the

0:33:42.560 --> 0:33:46.600
<v Speaker 1>physical properties of pummice itself. So just reading from their abstract,

0:33:46.680 --> 0:33:50.120
<v Speaker 1>they give four reasons. They say, first, during eruption, it

0:33:50.200 --> 0:33:54.120
<v Speaker 1>develops the highest surface area to volume ratio for any

0:33:54.240 --> 0:33:57.640
<v Speaker 1>rock type. Second, it is the only known rock type

0:33:57.680 --> 0:34:00.360
<v Speaker 1>that floats as rafts on the air water inner face

0:34:00.400 --> 0:34:03.320
<v Speaker 1>and then becomes beached in the title zone for long

0:34:03.400 --> 0:34:06.920
<v Speaker 1>periods of time. Third, it is exposed to an unusually

0:34:07.000 --> 0:34:12.400
<v Speaker 1>wide variety of conditions, including dehydration. Finally, from rafting to burial,

0:34:12.520 --> 0:34:16.319
<v Speaker 1>it has a remarkable ability to add sorb metals, organics,

0:34:16.360 --> 0:34:19.839
<v Speaker 1>and phosphates, as well as to host organic catalysts such

0:34:19.880 --> 0:34:23.359
<v Speaker 1>as zeolites and titanium oxides. And then they say these

0:34:23.360 --> 0:34:26.239
<v Speaker 1>remarkable properties now deserve to be rigorously explored in the

0:34:26.280 --> 0:34:29.600
<v Speaker 1>laboratory and the early rock record. So this would sort

0:34:29.640 --> 0:34:32.319
<v Speaker 1>of match with some of the other interesting ideas we've

0:34:32.360 --> 0:34:35.680
<v Speaker 1>talked about how um a lot of researchers are thinking

0:34:36.040 --> 0:34:39.560
<v Speaker 1>good candidate areas for the origins of life on Earth

0:34:39.800 --> 0:34:43.960
<v Speaker 1>would be like areas that repeatedly got wet and dry

0:34:43.960 --> 0:34:47.319
<v Speaker 1>in cycles, or areas that were right at the interface

0:34:47.880 --> 0:34:51.960
<v Speaker 1>of water and dry land, because that that kind of change,

0:34:52.000 --> 0:34:57.480
<v Speaker 1>like hydration and dehydration of of sort of gatherings of

0:34:57.600 --> 0:35:02.120
<v Speaker 1>organic molecules could have triggered some of the chemical evolution

0:35:02.280 --> 0:35:05.680
<v Speaker 1>that gave rise to you know, the organic molecules you're

0:35:05.680 --> 0:35:08.360
<v Speaker 1>looking for for the origins of life and possibly for

0:35:08.400 --> 0:35:12.680
<v Speaker 1>the structural formations of cells themselves. Yeah, and if and

0:35:12.760 --> 0:35:14.480
<v Speaker 1>if this, if this were the case too. This would

0:35:14.480 --> 0:35:18.320
<v Speaker 1>be another example of volcanoes being both you know, creator

0:35:18.320 --> 0:35:22.000
<v Speaker 1>and destroyer. You know, known for their their very destructive properties,

0:35:22.000 --> 0:35:25.319
<v Speaker 1>but also we have numerous examples of how they bring

0:35:25.360 --> 0:35:28.600
<v Speaker 1>new things into being being be at the creation of

0:35:28.600 --> 0:35:32.120
<v Speaker 1>of whole island chains or uh you know, creating more

0:35:32.239 --> 0:35:36.600
<v Speaker 1>land on existing volcanic islands, or just creating fertile soil

0:35:37.400 --> 0:35:41.920
<v Speaker 1>from which you know, all sorts of of plants can grow. Totally. Yeah,

0:35:42.080 --> 0:35:44.160
<v Speaker 1>So anyway, I like this idea. Maybe in the future

0:35:44.160 --> 0:35:47.319
<v Speaker 1>will come back to more more of the relationship or

0:35:47.360 --> 0:35:57.879
<v Speaker 1>the possible relationship between pumus and the origins of life. Now,

0:35:58.200 --> 0:36:02.400
<v Speaker 1>another example of of what we might call lava boats

0:36:02.480 --> 0:36:06.240
<v Speaker 1>or or lava rafts are sometimes referred to as such. Uh.

0:36:06.600 --> 0:36:10.000
<v Speaker 1>You can also find in the in the real world. UM.

0:36:10.040 --> 0:36:13.600
<v Speaker 1>And there's there's actually some fabulous footage of this of

0:36:13.640 --> 0:36:18.320
<v Speaker 1>this phenomenon that that came out in in recent years, UM,

0:36:18.360 --> 0:36:23.520
<v Speaker 1>particularly in regard to two thousand eighteen UH volcanic activity

0:36:23.520 --> 0:36:27.640
<v Speaker 1>at Kilauea. Uh. What we're talking about here with lava boats,

0:36:27.719 --> 0:36:32.279
<v Speaker 1>lava rafts are simply a created lava masses that move

0:36:32.440 --> 0:36:36.239
<v Speaker 1>downstream and lava flows. Uh. They look sort of like

0:36:36.400 --> 0:36:40.000
<v Speaker 1>rafts or boats um and as they move more lava

0:36:40.040 --> 0:36:43.880
<v Speaker 1>can adhere to them, and they accreed into bigger lava balls.

0:36:44.120 --> 0:36:46.600
<v Speaker 1>And to be clear, the official terminology here is not

0:36:47.000 --> 0:36:50.040
<v Speaker 1>lava boats or lava rafts. It is lava balls or

0:36:50.080 --> 0:36:54.640
<v Speaker 1>accretionary balls. But lava boats kind of took social media

0:36:54.680 --> 0:36:57.600
<v Speaker 1>by storm, especially uh in regard to some of the

0:36:57.640 --> 0:36:59.720
<v Speaker 1>footage that was making the rounds, which is quite impressive.

0:36:59.760 --> 0:37:02.960
<v Speaker 1>It looks like this big black sort of star destroyer

0:37:03.239 --> 0:37:07.359
<v Speaker 1>type shape in the lava flow making its way sort

0:37:07.400 --> 0:37:10.320
<v Speaker 1>of towards the camera. You're wanting to recreate your Revenge

0:37:10.320 --> 0:37:13.280
<v Speaker 1>of the Sixth scene, this is exactly what you're looking for, yeah,

0:37:13.400 --> 0:37:16.040
<v Speaker 1>or you can you can imagine like a burning skeleton

0:37:16.280 --> 0:37:19.640
<v Speaker 1>like jamming on a metal guitar like this standing on

0:37:19.719 --> 0:37:23.000
<v Speaker 1>top of this thing. It's it's very impressive. It should

0:37:23.000 --> 0:37:27.319
<v Speaker 1>have its own due warrior. Yeah. So this is this

0:37:27.360 --> 0:37:29.480
<v Speaker 1>is awesome footage. You know, definitely try to look it

0:37:29.560 --> 0:37:31.920
<v Speaker 1>up if you're you're interested. And it also can help

0:37:32.000 --> 0:37:35.160
<v Speaker 1>sort of illustrate what sometimes we sometimes encounter with lava

0:37:35.200 --> 0:37:39.480
<v Speaker 1>fields in which an upper rigid crust rests or you

0:37:39.520 --> 0:37:42.480
<v Speaker 1>could even say floats on a layer of fluid lava.

0:37:42.760 --> 0:37:44.960
<v Speaker 1>But this would be, you know, an even more stark

0:37:45.160 --> 0:37:49.839
<v Speaker 1>example of that of that that situation. Now, from here,

0:37:49.880 --> 0:37:52.239
<v Speaker 1>I thought we might move on into the discussion of

0:37:52.320 --> 0:37:55.640
<v Speaker 1>sort of I guess, speculative lava boats and you you

0:37:55.640 --> 0:37:58.480
<v Speaker 1>mean boats more literally? Now, Yes, now we're getting into

0:37:58.520 --> 0:38:02.240
<v Speaker 1>the idea of like a a vessel that humans made,

0:38:02.719 --> 0:38:05.480
<v Speaker 1>and in this case, that humans make and then like

0:38:05.600 --> 0:38:09.240
<v Speaker 1>set adrift in a lake of lava and then attempt

0:38:09.320 --> 0:38:12.400
<v Speaker 1>to climb into said vessel and maybe make a voyage

0:38:12.560 --> 0:38:15.719
<v Speaker 1>halfway across the lake. Take me there, Yeah, perhaps to

0:38:15.800 --> 0:38:19.799
<v Speaker 1>defeat Bowser or something. I don't know. But so, if

0:38:19.800 --> 0:38:22.399
<v Speaker 1>you haven't watched the two thousand and sixteen documentary Into

0:38:22.440 --> 0:38:25.880
<v Speaker 1>the Inferno, I think we we we both would highly

0:38:25.880 --> 0:38:28.520
<v Speaker 1>recommend this. It's It was written and directed by Werner

0:38:28.600 --> 0:38:34.000
<v Speaker 1>Herzog and featured British volcanologists Clive Oppenheimer. Both of these

0:38:34.040 --> 0:38:36.160
<v Speaker 1>gentlemen were guests on our show back And I believe

0:38:36.280 --> 0:38:40.600
<v Speaker 1>this was like late in promotion of their documentary Fireball

0:38:40.920 --> 0:38:44.560
<v Speaker 1>Visitors from Darker Worlds. Yeah, I think, uh, Into the

0:38:44.600 --> 0:38:47.839
<v Speaker 1>Inferno was the documentary they had done right before this one,

0:38:48.360 --> 0:38:52.520
<v Speaker 1>right yeah, dealing with with the volcanoes and uh, it's

0:38:52.560 --> 0:38:55.040
<v Speaker 1>it's it's wonderful. If you get a chance to watch it,

0:38:55.120 --> 0:38:58.200
<v Speaker 1>you definitely should if you're interested in volcanoes or you know,

0:38:58.200 --> 0:39:01.040
<v Speaker 1>it's the work of Verna Herzog. Uh, you know, definitely

0:39:01.040 --> 0:39:04.960
<v Speaker 1>worth picking. Picking up Um Into the Inferno features footage

0:39:05.040 --> 0:39:09.719
<v Speaker 1>of volcanologist Maurice and Kadia Kraft Uh, French husband and

0:39:09.760 --> 0:39:14.320
<v Speaker 1>wife duo. The Crafts were pioneers in the film documentation

0:39:14.360 --> 0:39:18.120
<v Speaker 1>of volcanoes, notable for there's sometimes very you know, close

0:39:18.200 --> 0:39:22.719
<v Speaker 1>proximity UM filming of lava flows, a lot of very

0:39:22.800 --> 0:39:26.799
<v Speaker 1>dangerous at times looking footage. Uh and Saturday they did

0:39:26.840 --> 0:39:32.240
<v Speaker 1>both perish in a pyroclastic flow on mountains and in Japan.

0:39:33.400 --> 0:39:36.120
<v Speaker 1>But these were these were this was a couple that

0:39:36.200 --> 0:39:38.600
<v Speaker 1>that loved volcanoes, and I was reading a little bit

0:39:38.640 --> 0:39:42.000
<v Speaker 1>about them in Fire in the Earth, Fire in the Soul.

0:39:42.080 --> 0:39:45.440
<v Speaker 1>The Final Moments of Maurice and Katia Craft by John

0:39:45.920 --> 0:39:50.840
<v Speaker 1>uh Caldarazzo, published in Interdisciplinary Studies in Literature and Environment

0:39:51.120 --> 0:39:56.200
<v Speaker 1>in and In this the the author notes the following

0:39:56.560 --> 0:39:59.680
<v Speaker 1>quote and this is speaking of Maurice here he loved

0:39:59.680 --> 0:40:02.279
<v Speaker 1>to say how fantastic. It would be to one day

0:40:02.320 --> 0:40:06.200
<v Speaker 1>build a special boat, a kind of titanium arc to

0:40:06.320 --> 0:40:09.799
<v Speaker 1>put in on a lava flow off. They'd ride down

0:40:09.800 --> 0:40:13.759
<v Speaker 1>a steaming mountain, flying the French flag and waving to

0:40:13.840 --> 0:40:17.320
<v Speaker 1>all their friends as they rode a glowing river into

0:40:17.360 --> 0:40:20.000
<v Speaker 1>the sea. Well, on one hand, that's beautiful, but I'm

0:40:20.040 --> 0:40:23.640
<v Speaker 1>also amused by the though the addition of the French flag.

0:40:23.880 --> 0:40:27.960
<v Speaker 1>Well you know they were French, why not. But now

0:40:28.000 --> 0:40:29.719
<v Speaker 1>I don't think we're supposed to to take this quick

0:40:29.800 --> 0:40:34.479
<v Speaker 1>claim this lava for France. Um vegan is you've gotta

0:40:34.480 --> 0:40:36.720
<v Speaker 1>get on. It's literally getting on on the ground floor

0:40:36.760 --> 0:40:41.399
<v Speaker 1>of new uh of of New Land. Now, I don't

0:40:41.400 --> 0:40:43.719
<v Speaker 1>think we're meant to take this, you know, real seriously,

0:40:43.840 --> 0:40:48.759
<v Speaker 1>these were two individuals who simply loved volcanoes, loved volcanic activity.

0:40:49.040 --> 0:40:53.240
<v Speaker 1>They lived for volcanoes. Uh Caldaraso quotes them is saying

0:40:53.280 --> 0:40:56.759
<v Speaker 1>that volcanoes were like are like blind wild animals that

0:40:56.880 --> 0:41:00.800
<v Speaker 1>one must observe, like a quote mad witch doctor. I

0:41:00.880 --> 0:41:03.040
<v Speaker 1>think the idea is like it's it's got indigestion. You

0:41:03.080 --> 0:41:04.719
<v Speaker 1>need to watch it for a very long time to

0:41:04.760 --> 0:41:08.200
<v Speaker 1>see what what's what's going on with it? Um. They

0:41:08.239 --> 0:41:11.960
<v Speaker 1>also talked about how normal mountains are dead and that

0:41:12.000 --> 0:41:15.359
<v Speaker 1>they prefer the living mountains of volcanoes. When you love

0:41:15.480 --> 0:41:20.040
<v Speaker 1>volcanoes so much, you have to slag normal mountains, right, So,

0:41:20.239 --> 0:41:21.640
<v Speaker 1>you know, I think it's safe to, you know, to

0:41:21.680 --> 0:41:23.359
<v Speaker 1>say that they could just be you know, they're being

0:41:23.360 --> 0:41:26.400
<v Speaker 1>a little poetic, like we love volcano so much that

0:41:26.440 --> 0:41:28.160
<v Speaker 1>if we could ride a ship on the on the

0:41:28.160 --> 0:41:30.719
<v Speaker 1>flow of lava, we would. But at the same time,

0:41:30.719 --> 0:41:33.479
<v Speaker 1>it's still a terrific vision. Uh, you know, this high

0:41:33.480 --> 0:41:37.279
<v Speaker 1>tech vessel sailing across lava. I was looking around. I

0:41:37.280 --> 0:41:41.160
<v Speaker 1>imagine somebody has has explored this more in science fiction,

0:41:41.239 --> 0:41:44.400
<v Speaker 1>especially like pulp science fiction of the old days, Like

0:41:44.400 --> 0:41:46.840
<v Speaker 1>there has to be some story about like a uh,

0:41:46.880 --> 0:41:49.200
<v Speaker 1>you know, a volcanic planet and there being some sort

0:41:49.200 --> 0:41:52.239
<v Speaker 1>of a volcanic ship. I would be shocked if this

0:41:52.320 --> 0:41:54.879
<v Speaker 1>is not shown, if this neess not appeared in uh

0:41:55.000 --> 0:41:58.480
<v Speaker 1>in Doctor Who at some point or another. So so

0:41:58.600 --> 0:42:00.880
<v Speaker 1>if if you're wondering what could this exists? Could we

0:42:00.920 --> 0:42:04.560
<v Speaker 1>make something like this? Well? Luckily, volcanologist and science writer

0:42:04.719 --> 0:42:08.200
<v Speaker 1>Robin Andrews chimed in on this very topic for a

0:42:08.920 --> 0:42:12.200
<v Speaker 1>seventeen Forbes dot Com article titled Here's how to make

0:42:12.200 --> 0:42:15.480
<v Speaker 1>a boat to sail over deadly lava and and he

0:42:15.480 --> 0:42:19.800
<v Speaker 1>he uses, uh, the dreams of the crafts of particularly

0:42:19.840 --> 0:42:21.880
<v Speaker 1>Maurice Craft is kind of the jumping off point for

0:42:21.920 --> 0:42:25.759
<v Speaker 1>this as well. Okay, what's his plan here? Okay, so, um,

0:42:25.880 --> 0:42:28.040
<v Speaker 1>he points out, there's, first of all, you've got to

0:42:28.040 --> 0:42:31.000
<v Speaker 1>take into account those temperatures, like like first and foremost.

0:42:31.239 --> 0:42:33.680
<v Speaker 1>They may ignore the temperatures in the movies, but you

0:42:33.719 --> 0:42:35.879
<v Speaker 1>need to be aware of them. Uh. First of all,

0:42:36.480 --> 0:42:39.480
<v Speaker 1>he writes that lava flows tend to run one thousand

0:42:39.520 --> 0:42:43.200
<v Speaker 1>degrees celsius or one thousand, eight hundred thirty two degrees

0:42:43.200 --> 0:42:46.840
<v Speaker 1>fahrenheit on average, and lava lakes can exceed that to

0:42:46.880 --> 0:42:51.080
<v Speaker 1>a max of of of of somewhere around eleven hundred

0:42:51.120 --> 0:42:55.080
<v Speaker 1>degrees celsius or two thousand and twelve degrees fahrenheit. So

0:42:55.120 --> 0:42:58.520
<v Speaker 1>it's it's really hot. You can if you're gonna be

0:42:58.600 --> 0:43:01.880
<v Speaker 1>anywhere anywhere close to at for you, certainly for a

0:43:01.880 --> 0:43:04.279
<v Speaker 1>boat ride. If you're gonna build a boat, you have

0:43:04.320 --> 0:43:07.759
<v Speaker 1>to take into account that, Um, it's gonna be that hot.

0:43:07.800 --> 0:43:10.399
<v Speaker 1>You're gonna need physical protection, You're also going to need

0:43:10.440 --> 0:43:13.760
<v Speaker 1>some sort of containment suit or uh, you know, oxygen

0:43:13.880 --> 0:43:16.400
<v Speaker 1>just supply so that you're not just breathing in toxic

0:43:16.480 --> 0:43:19.520
<v Speaker 1>gases that are either going to kill you dead out

0:43:19.560 --> 0:43:23.319
<v Speaker 1>there on the lake or just like permanently damage your body.

0:43:23.400 --> 0:43:25.720
<v Speaker 1>So he says, Okay, if you're gonna build this boat,

0:43:25.800 --> 0:43:28.919
<v Speaker 1>it probably needs to be steel, as steel melts at

0:43:29.560 --> 0:43:32.920
<v Speaker 1>one thousand, three seventy degrees celsius or two thousand, five

0:43:32.960 --> 0:43:35.680
<v Speaker 1>hundred degrees fahrenheit. So you know, you don't want to

0:43:35.719 --> 0:43:38.000
<v Speaker 1>be in a boat that melts in the lava lake.

0:43:38.320 --> 0:43:40.720
<v Speaker 1>You want to be in a boat that that doesn't

0:43:40.760 --> 0:43:46.000
<v Speaker 1>quite melt and almost well, yes, by the way, so

0:43:46.160 --> 0:43:48.920
<v Speaker 1>some of this may may sound from like familiar territory.

0:43:49.400 --> 0:43:51.239
<v Speaker 1>Of of course, we did an episode on the one

0:43:51.360 --> 0:43:54.560
<v Speaker 1>Ring from from the Lord of the Rings discussing just

0:43:54.600 --> 0:43:57.040
<v Speaker 1>what sort of metal would melt or be destroyed in

0:43:57.160 --> 0:44:00.040
<v Speaker 1>Mount Doom but would not melt or be destroyed in

0:44:00.080 --> 0:44:03.719
<v Speaker 1>a medieval forge. So if you want more metallurgy, uh,

0:44:04.000 --> 0:44:06.839
<v Speaker 1>that's that's episode to go back to. Okay, all right,

0:44:06.880 --> 0:44:09.799
<v Speaker 1>but going back here to the work of Robin Andrews. Next,

0:44:09.840 --> 0:44:12.200
<v Speaker 1>he points out that you need an interior lining in

0:44:12.239 --> 0:44:15.680
<v Speaker 1>that boat that's non flammable and also highly heat resistant.

0:44:15.920 --> 0:44:18.640
<v Speaker 1>Otherwise the boat would just simply cook you. I think

0:44:18.640 --> 0:44:22.399
<v Speaker 1>you your skin would stick to it, which is which

0:44:22.400 --> 0:44:25.440
<v Speaker 1>sounds horrifying. Yeah, even if the boat didn't melt, it

0:44:25.440 --> 0:44:28.280
<v Speaker 1>would essentially turn into a frying pan. Right, you're writing

0:44:28.320 --> 0:44:31.960
<v Speaker 1>in a frying pan on the heating element. Yes, So

0:44:32.040 --> 0:44:36.040
<v Speaker 1>he writes the following about possible lining options here. Quote,

0:44:36.440 --> 0:44:38.600
<v Speaker 1>there are a variety of plastics you can use, and

0:44:38.640 --> 0:44:42.680
<v Speaker 1>if you aren't worried about fire started by rogue lava blebs,

0:44:43.120 --> 0:44:46.319
<v Speaker 1>you could even use wet wood. If you want to

0:44:46.320 --> 0:44:50.480
<v Speaker 1>be particularly high tech, grab some halfneum carbide with a

0:44:50.520 --> 0:44:53.920
<v Speaker 1>melting point of around four thousand degrees celsius seven thousand

0:44:53.960 --> 0:44:59.000
<v Speaker 1>two trees fahrenheit and very high thermal resistance. These would

0:44:59.080 --> 0:45:02.000
<v Speaker 1>ensure you don't get a little sizzled inside your boat.

0:45:02.400 --> 0:45:05.200
<v Speaker 1>You could even use half carbide to make the boat,

0:45:05.560 --> 0:45:09.640
<v Speaker 1>but seeing as it's unfathomably expensive, steals a far cheaper

0:45:09.680 --> 0:45:12.520
<v Speaker 1>option here, just looked it up. Half neum carbide is

0:45:12.520 --> 0:45:15.880
<v Speaker 1>said to have a melting point of thirty degrees celsius,

0:45:15.920 --> 0:45:20.480
<v Speaker 1>So you're really good to go there. Yeah, and he

0:45:20.520 --> 0:45:22.920
<v Speaker 1>also mentioned that you'd probably need to paddle with similar

0:45:22.960 --> 0:45:24.880
<v Speaker 1>material you know you'd have you'd have to make your

0:45:24.880 --> 0:45:27.719
<v Speaker 1>paddle or your your your pole out of that as well.

0:45:27.760 --> 0:45:29.759
<v Speaker 1>I guess it depends on how ambitious you are. You're

0:45:29.800 --> 0:45:33.480
<v Speaker 1>just happy to be floating um on or down the

0:45:33.719 --> 0:45:35.640
<v Speaker 1>you know, the lake or flow of lava, or do

0:45:35.719 --> 0:45:37.800
<v Speaker 1>you do you feel like you need to actually build

0:45:37.840 --> 0:45:40.440
<v Speaker 1>up speed? Where do you end up? Does this mean

0:45:40.480 --> 0:45:42.520
<v Speaker 1>you just ride this thing until it dumps you out

0:45:42.560 --> 0:45:45.160
<v Speaker 1>into the ocean? Um? Well, I guess it depends. I mean,

0:45:45.200 --> 0:45:47.640
<v Speaker 1>if you're just in a lake of of of lava,

0:45:47.800 --> 0:45:52.000
<v Speaker 1>like in a crater like um kilaueaikey, then you might

0:45:52.000 --> 0:45:54.640
<v Speaker 1>just be floating out there until the like the vortex

0:45:54.680 --> 0:45:57.920
<v Speaker 1>sucks you down or until or if it's if there's

0:45:57.960 --> 0:46:00.360
<v Speaker 1>a fountain of of lava going on and told like

0:46:00.400 --> 0:46:02.759
<v Speaker 1>that burns you up or or drops a bunch of

0:46:02.800 --> 0:46:07.279
<v Speaker 1>bathtub sized blobs of lava on top of you. Or

0:46:07.560 --> 0:46:09.360
<v Speaker 1>yeah it's a flow going into the ocean. Maybe you

0:46:09.480 --> 0:46:11.719
<v Speaker 1>ride that out, but that's gonna be there. There's gonna

0:46:11.719 --> 0:46:14.399
<v Speaker 1>be some rapids in there. Well. Another hazard we haven't

0:46:14.440 --> 0:46:17.160
<v Speaker 1>even mentioned yet is that if you actually do ride

0:46:17.200 --> 0:46:19.640
<v Speaker 1>this all the way down to the water's edge, and

0:46:19.640 --> 0:46:22.960
<v Speaker 1>then you plunge into the water where the molten lava

0:46:23.040 --> 0:46:25.600
<v Speaker 1>is hitting the water. Uh. You need to be careful

0:46:25.600 --> 0:46:29.000
<v Speaker 1>there because another totally separate thing I was reading about

0:46:29.040 --> 0:46:31.120
<v Speaker 1>that we haven't even gotten to yet is this stuff

0:46:31.160 --> 0:46:33.720
<v Speaker 1>called las If you have you've read about this rob

0:46:33.840 --> 0:46:36.959
<v Speaker 1>the so called lava haze, No, no, tell me about

0:46:37.000 --> 0:46:41.000
<v Speaker 1>the lays. Well. Unfortunately this has actually led to at

0:46:41.040 --> 0:46:43.200
<v Speaker 1>least a few human deaths in the past. But it's

0:46:43.239 --> 0:46:46.640
<v Speaker 1>this type of steam or haze or mist that billows

0:46:46.719 --> 0:46:50.520
<v Speaker 1>up when molten lava falls into the ocean. I think

0:46:50.560 --> 0:46:53.000
<v Speaker 1>I was reading about it directly in connection with Kilauea.

0:46:53.040 --> 0:46:57.800
<v Speaker 1>Actually it's dangerous for multiple reasons. Number one that these clouds,

0:46:57.800 --> 0:47:00.880
<v Speaker 1>because of some kind of chemical reaction that happens, the

0:47:00.960 --> 0:47:04.840
<v Speaker 1>clouds are full of hydrochloric acid, is like stomach acid,

0:47:04.880 --> 0:47:07.560
<v Speaker 1>which you don't want getting into your lungs. But I

0:47:07.600 --> 0:47:10.960
<v Speaker 1>think it may also have like other types of highly

0:47:10.960 --> 0:47:15.400
<v Speaker 1>corrosive acids, hydrofluoric acid. Of course, lots of carbon dioxide.

0:47:15.400 --> 0:47:18.200
<v Speaker 1>But then the another part is that it's full of

0:47:18.640 --> 0:47:23.920
<v Speaker 1>tons of extremely tiny little shards of volcanic glass. That

0:47:24.000 --> 0:47:27.200
<v Speaker 1>get carried up in the steam. So basically, you don't

0:47:27.200 --> 0:47:28.879
<v Speaker 1>want to get anywhere near this stuff. If you ever

0:47:28.880 --> 0:47:32.320
<v Speaker 1>see lava dripping into the water, it's beautiful to observe

0:47:32.400 --> 0:47:34.680
<v Speaker 1>from a distance, but you don't want to go near it.

0:47:35.400 --> 0:47:38.359
<v Speaker 1>So if you're listening to this episode and you're you're

0:47:38.440 --> 0:47:40.120
<v Speaker 1>if you're thinking, well, I could do this, I could

0:47:40.120 --> 0:47:42.280
<v Speaker 1>pull this off. Now, do not, please do not attempt

0:47:42.360 --> 0:47:46.359
<v Speaker 1>this at home, or or or in Volcano National Park,

0:47:46.480 --> 0:47:49.080
<v Speaker 1>or anywhere near any volcano you have you happen to

0:47:49.120 --> 0:47:52.319
<v Speaker 1>be visiting. Please keep a respectful distance. And that's just

0:47:52.400 --> 0:47:56.640
<v Speaker 1>respecting yourself, right right though, Certainly, if you have a

0:47:56.719 --> 0:48:00.520
<v Speaker 1>chance to to to get within a safe distance of

0:48:00.560 --> 0:48:03.440
<v Speaker 1>any kind of volcanic activity to visit you know, Volcano

0:48:03.520 --> 0:48:07.920
<v Speaker 1>National Park or really any any volcanic location, uh, definitely

0:48:08.000 --> 0:48:10.600
<v Speaker 1>check it out. I mean, these these are the living mountains,

0:48:10.640 --> 0:48:12.680
<v Speaker 1>These are these are amazing places. And even if you're

0:48:12.719 --> 0:48:16.759
<v Speaker 1>visiting a place that's not quite alive anymore, uh, you know,

0:48:16.960 --> 0:48:21.839
<v Speaker 1>sort of recently dead mountains like that alone haunted by

0:48:21.840 --> 0:48:24.799
<v Speaker 1>a particular energy that you just don't necessarily encounter it.

0:48:25.200 --> 0:48:27.920
<v Speaker 1>Uh in in other parts of the world, totally yea,

0:48:28.280 --> 0:48:30.719
<v Speaker 1>but obviously we'd love to hear from everyone out there. Um,

0:48:30.760 --> 0:48:35.239
<v Speaker 1>have you visited some volcanic locations and you have additional

0:48:35.320 --> 0:48:38.080
<v Speaker 1>sightings you would like to share if you seen anything, uh,

0:48:38.160 --> 0:48:41.560
<v Speaker 1>you know, like these these the floating pumas or these

0:48:41.680 --> 0:48:45.080
<v Speaker 1>uh or these these lava balls? Uh, let us know,

0:48:45.840 --> 0:48:48.719
<v Speaker 1>you know, what are some volcanic terrains that you've explored,

0:48:49.239 --> 0:48:53.640
<v Speaker 1>And likewise, what are some volcanic situations you've explored in

0:48:54.120 --> 0:48:56.839
<v Speaker 1>fantasy and fiction that match up with what we've been

0:48:56.840 --> 0:48:58.640
<v Speaker 1>talking about. What are we missing out there in the

0:48:58.680 --> 0:49:04.080
<v Speaker 1>world the why the wide wild world of sci fi exploration?

0:49:04.160 --> 0:49:06.920
<v Speaker 1>If there are some some tremendous scenes of ships sailing

0:49:06.920 --> 0:49:09.719
<v Speaker 1>on a sea of lava and so forth, right in

0:49:09.800 --> 0:49:11.400
<v Speaker 1>and let us know. We'd love to hear from you.

0:49:11.840 --> 0:49:15.080
<v Speaker 1>Huge thanks as always to our excellent audio producer Seth

0:49:15.160 --> 0:49:17.680
<v Speaker 1>Nicholas Johnson. If you would like to get in touch

0:49:17.719 --> 0:49:19.920
<v Speaker 1>with us with feedback on this episode or any other,

0:49:20.000 --> 0:49:22.319
<v Speaker 1>to suggest topic for the future, to tell us about

0:49:22.400 --> 0:49:25.719
<v Speaker 1>your love about fantasies, or just to say hello, you

0:49:25.760 --> 0:49:28.399
<v Speaker 1>can email us at contact at stuff to Blow Your

0:49:28.400 --> 0:49:38.800
<v Speaker 1>Mind dot com. Stuff to Blow Your Mind. It's production

0:49:38.840 --> 0:49:41.239
<v Speaker 1>of I Heart radio for more podcasts, for my heart

0:49:41.320 --> 0:49:44.480
<v Speaker 1>Radio because the iHeart Radio app, Apple podcasts, or wherever

0:49:44.480 --> 0:50:01.400
<v Speaker 1>you're listening to your favorite shows. I D had a

0:50:01.480 --> 0:50:03.560
<v Speaker 1>time about about movie