WEBVTT - From the Vault: Mud, Part 1

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<v Speaker 1>Hey, welcome to Stuff to Blow Your Mind. My name

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<v Speaker 1>is Robert Lamb. It's Saturday. We're venturing back into the vault.

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<v Speaker 1>This is going to be part one of our let's see,

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<v Speaker 1>this was a four part series that we did on mud.

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<v Speaker 1>You know, if you listened recently, you may have heard

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<v Speaker 1>our series on dust. Well, similar we're talking about mud

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<v Speaker 1>and there so we get into all sorts of different

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<v Speaker 1>angles here in these four episodes. So it might seem

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<v Speaker 1>mundane on the surface, but once you sync into it,

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<v Speaker 1>I think you'll find it as fascinating as we did.

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<v Speaker 1>This episode originally published on seven six, twenty twenty three.

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<v Speaker 1>Here we go.

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<v Speaker 2>Welcome to Stuff to Blow Your Mind, a production of iHeartRadio.

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<v Speaker 1>Hey, welcome to Stuff to Blow your Mind. My name

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<v Speaker 1>is Robert.

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<v Speaker 3>Lamb, and I am Joe McCormack. And today we are

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<v Speaker 3>going to be starting a series of episodes on mud,

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<v Speaker 3>a topic that I promise is more interesting than you

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<v Speaker 3>might think. And to get us started today, I wanted

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<v Speaker 3>to talk about a section from an English epic poem

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<v Speaker 3>that endorses the belief that mud just happens to give

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<v Speaker 3>rise to monsters or monstrous creatures of various shapes. So

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<v Speaker 3>the poem in question is a late sixteenth century epic

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<v Speaker 3>poem by the English poet Edmund Spencer called The Fairy Queen.

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<v Speaker 3>I took a class in college where we read this,

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<v Speaker 3>or we read part of it. To be honest, there's

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<v Speaker 3>a lot that I forget about it. But it's very

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<v Speaker 3>much your classic epic poem, with heroic knights, the Red

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<v Speaker 3>Cross Knight, and damsels in distress and witches and ogres

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<v Speaker 3>and all that. And there's an interesting passage toward the

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<v Speaker 3>beginning of The Fairy Queen. I think it's in book one,

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<v Speaker 3>Canto one, where Spencer implies a belief about the way

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<v Speaker 3>nature works, a belief that the mud, specifically the mud

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<v Speaker 3>of the Nie River, spawns monsters, and Spencer writes quote

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<v Speaker 3>as when old father Nilus gins to swell with timely

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<v Speaker 3>pride above the Egyptian veil, his fatty waves do fertile

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<v Speaker 3>slime out well and overflow each plane and lowly dale.

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<v Speaker 3>But when his later spring gins to a veil, huge

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<v Speaker 3>heaps of mud he leaves wherein their breed ten thousand

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<v Speaker 3>kinds of creatures, partly male and partly female, of his

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<v Speaker 3>fruitful seed, such ugly, monstrous shapes elsewhere may no man read.

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<v Speaker 3>And then Spencer later cites the same belief again as

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<v Speaker 3>a kind of illustration of a general principle. He writes,

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<v Speaker 3>but reason teacheth that the fruitful seeds of all things

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<v Speaker 3>living through impression of the sunbeams in moist complexion, do

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<v Speaker 3>life conceive and quickened are by kind. So after Nilus inundation,

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<v Speaker 3>infinite shapes of creatures men do find inform in the

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<v Speaker 3>mud on which the sun hath shined. So I think

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<v Speaker 3>he seems to be saying like mud plus sunshine equals monsters,

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<v Speaker 3>or at least creatures of infinite shapes, which in some

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<v Speaker 3>passages he seems to think might be monsters. Maybe among

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<v Speaker 3>infinite variation there will necessarily be some monsters. And I'm

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<v Speaker 3>interested in this belief because, on one hand, it just

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<v Speaker 3>sort of reflects some ancient beliefs that are carried over

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<v Speaker 3>into the Medieval and Renaissance period about where life comes from,

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<v Speaker 3>ideas now obsolete theories like spontaneous generation that you know

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<v Speaker 3>that life forms, which is sort of like arise in

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<v Speaker 3>the mud or in like a wet bag of flower

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<v Speaker 3>or something. But I also like it because it imagines

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<v Speaker 3>the mud in the floodplain of a great river like

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<v Speaker 3>the Nile as a source of both like sort of

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<v Speaker 3>mystery and danger but also great possibility. And this does

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<v Speaker 3>correspond to the kind of the double nature of mud

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<v Speaker 3>and of a river like the Nile. So you think

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<v Speaker 3>of the Nile River delta, it is a place of

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<v Speaker 3>incredibly fertile soil that you know, that supplies food and

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<v Speaker 3>crops for all of the areas around. But also if

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<v Speaker 3>you know, you get stuck in the mud, that's a

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<v Speaker 3>place you don't want to be. And it is a

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<v Speaker 3>place where you will find lots of life that is

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<v Speaker 3>maybe life that's kind of strange to you. You don't

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<v Speaker 3>usually go wading into the mud, and if you do,

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<v Speaker 3>I don't know, all kinds of weird little mollusks and

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<v Speaker 3>creepy crawleys and critters are in there, and you don't

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<v Speaker 3>know what you might find.

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<v Speaker 1>Yeah, yeah, this is really interesting. We should also note,

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<v Speaker 1>you know, it does accurately, though monstrously refer to the

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<v Speaker 1>the the inundation of the Nile, which is a topic

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<v Speaker 1>we did an entire episode at least one episode on

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<v Speaker 1>in the past. I mean, the Nile overflows its banks

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<v Speaker 1>and it brings life and has this this very prominent

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<v Speaker 1>role in especially in ancient Egyptian belief and mythology. But yeah,

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<v Speaker 1>this dual nature of mud is quite interesting and something

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<v Speaker 1>that that we're going to be talking about quite a

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<v Speaker 1>bit in these episodes because it at once it is

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<v Speaker 1>like you want to build something, well, you're gonna need

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<v Speaker 1>something like mud or mud itself. But of course it's

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<v Speaker 1>also the place where you know, many a famous military

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<v Speaker 1>campaign has perished in the mud, so you know, it's

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<v Speaker 1>the thing from which monsters emerge, but it's all you know,

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<v Speaker 1>it's the thing where you might find a pig, but

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<v Speaker 1>you also will find gleaming butterflies, you know, cascading and

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<v Speaker 1>swirling around something some stinking pile of mud. So yeah,

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<v Speaker 1>it does seem to have this dual nature, at least

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<v Speaker 1>from the human vantage point.

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<v Speaker 3>So our goal is after we're done with this series,

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<v Speaker 3>you will never think about mud the same way. And

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<v Speaker 3>when it gets stuck to your shoes, you might still

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<v Speaker 3>be mad, but there will also be a part of

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<v Speaker 3>you that that's kind of reflective and stops to be

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<v Speaker 3>amazed at what it is. Your dog has just gotten

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<v Speaker 3>all over your couch.

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<v Speaker 1>Yeah, and if you're like me too. Just even thinking

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<v Speaker 1>about this topic, it means that you've had the Primus

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<v Speaker 1>song my Name is Mud just flipped on in your brain.

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<v Speaker 1>I haven't even listened to it to encourage or extinguish it,

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<v Speaker 1>but it's just there as I read these various papers

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<v Speaker 1>about mud or mummama mud, Right, I guess that's the way.

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<v Speaker 3>It's said, and so I'll take your word for it.

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<v Speaker 1>It's a solid jam. It's got some colossal bass and

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<v Speaker 1>drums on there.

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<v Speaker 3>Oh yeah, that's primus. They rattle the furniture. But anyway,

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<v Speaker 3>we should go straight to the question what is mud?

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<v Speaker 3>What is it made of? In general, mud seems to

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<v Speaker 3>have a kind of loose definition. We all know it

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<v Speaker 3>when we see it, but there may not be strict

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<v Speaker 3>scientific criteria about what counts, except maybe in certain contexts,

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<v Speaker 3>like when you're talking when you get to some things

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<v Speaker 3>we'll get to in a minute about like particle size

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<v Speaker 3>and what solidifies into certain kinds of rock. But just generally,

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<v Speaker 3>I mean, mud is some sort of wet soil, but

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<v Speaker 3>exactly how wet, Exactly what are the properties of the

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<v Speaker 3>soil for it to count as mud versus just being

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<v Speaker 3>kind of like I don't know, damp, gross stuff that

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<v Speaker 3>might be in the eye of the beholder, of the

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<v Speaker 3>beat or of the bee treader.

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<v Speaker 1>Yeah, I would. I would. I think that sometimes we

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<v Speaker 1>know it when we see it, but we definitely know

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<v Speaker 1>it when we step on it or step in it.

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<v Speaker 1>I guess that's the thing, right. If I'm able to

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<v Speaker 1>step on it, well maybe it's not fully mud. But

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<v Speaker 1>if I'm in it, well I am in mud now.

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<v Speaker 1>But I think the other Yeah. The other interesting thing

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<v Speaker 1>about mud is a lot of it does depend on

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<v Speaker 1>where you're coming from, you know, like if you were

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<v Speaker 1>a domesticated hog, well, mud is just simply good. There's

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<v Speaker 1>not much else to say about that, though. We will

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<v Speaker 1>get into how various animals use mud later on in

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<v Speaker 1>a subsequent episode, but just from the human perspective, it's

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<v Speaker 1>kind of interesting. One of the books I was looking at,

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<v Speaker 1>and we'll come back to later when we get more

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<v Speaker 1>in depth on this is a book titled Mud, a

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<v Speaker 1>Military History by ce Wood, which, if you haven't thought

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<v Speaker 1>about it much before, or you haven't you're not like

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<v Speaker 1>a military history enthusiast, you might not realize that, oh yeah, mud.

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<v Speaker 1>Mud is the sort of thing that you could write

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<v Speaker 1>an entire book about just from the perspective of war

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<v Speaker 1>and military operations. But that's what this book is.

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<v Speaker 3>When I think of mud and armed conflict. Obviously, you know,

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<v Speaker 3>terrain and especially mud have played a big role in

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<v Speaker 3>worse throughout history, but I think especially of Eastern Europe

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<v Speaker 3>for some reason.

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<v Speaker 1>Yeah, big big war machines, big tanks stuck in the mud,

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<v Speaker 1>or as as Wood mentions a time or two, the

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<v Speaker 1>idea of one of these colossal tanks just going down

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<v Speaker 1>a muddy hill, as if it were like a sled

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<v Speaker 1>on a snowfield or something, you know, just out of control.

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<v Speaker 1>Things like that. Occurring mud changes what you can and

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<v Speaker 1>can't do in many instances with any with things ranging

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<v Speaker 1>from infantry to horses to modern industrial war machines. But

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<v Speaker 1>like I said, we'll get back to that more in

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<v Speaker 1>the future. But I thought it was interesting that Wood

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<v Speaker 1>opens just dealing with his basic ambiguity concerning mud and

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<v Speaker 1>writes that, Okay, if we're going to be just very

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<v Speaker 1>broad about it, it comes down to soil consisting of

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<v Speaker 1>mineral and organic matter combined with moisture at such a

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<v Speaker 1>level relative to the exact compositions of the soil to

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<v Speaker 1>make it unstable and likely to move and flow underfoot

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<v Speaker 1>or underhoof or under wheeler track, etc. Wood points out

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<v Speaker 1>that while many military minds have considered mud and other

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<v Speaker 1>soil issues beneath their strategic consideration, but they have always

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<v Speaker 1>done so at their peril, because mud, as we'll get

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<v Speaker 1>into later, does make a difference in war has come

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<v Speaker 1>to very famously define certain war zones. He points out

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<v Speaker 1>that not everyone has certainly ignored this fact, and in

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<v Speaker 1>nineteen forty four, the US Army conducted a series of

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<v Speaker 1>tests regarding mud. They're like, all right, let's get down

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<v Speaker 1>to it. Let's classify some mud. Because we have only

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<v Speaker 1>so many resources for our rubber tires, so we needed

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<v Speaker 1>to decide where we need to send them, where we

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<v Speaker 1>need to prioritize our best tires. And so this is

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<v Speaker 1>a situation where we're dealing with sort of a narrowed

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<v Speaker 1>perspective concerning mud. This is just mud concerning like, let

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<v Speaker 1>me roll some vehicles across it. But they classified mud

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<v Speaker 1>into two types and two subtypes. Okay, Type one bottomless mud. Now,

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<v Speaker 1>this just means that the MUD's consistency cannot support a

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<v Speaker 1>vehicle with tires that have twenty pounds of pressure, or

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<v Speaker 1>that the underlying hard layer of earth beneath the mud

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<v Speaker 1>beneath the layer of mud is too far beneath the

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<v Speaker 1>vehicle's ground clearance.

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<v Speaker 3>Okay, so this sounds like dangerous mud.

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<v Speaker 1>Yeah, this is the mud that your vehicle is going

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<v Speaker 1>to get stuck in and or sink into. And then

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<v Speaker 1>type two is just all other types of mud. But

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<v Speaker 1>this does feature two subtypes, Type A and type B.

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<v Speaker 1>Type A has a quote unquote cleaning quality, meaning that

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<v Speaker 1>it contains enough moisture to work as a liquid. So

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<v Speaker 1>like this, like type A mud gets on your vehicle

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<v Speaker 1>and you know, it kind of flows off. I mean

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<v Speaker 1>it's I don't think cleaning quality means that your tank

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<v Speaker 1>or your truck is going to be clean after the

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<v Speaker 1>mud has a rent stock a little bit. Yeah, it

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<v Speaker 1>flows away, but it's it's this a cleaning quality. Type

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<v Speaker 1>B is adhesive or sticky. So this is the the

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<v Speaker 1>mudd in type of mud. This is the type of

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<v Speaker 1>mud that the the big pickup pickup truck driver seeks

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<v Speaker 1>out when they go out into the wilderness to make

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<v Speaker 1>sure that they return to city life with a vehicle

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<v Speaker 1>completely encased in mud. Okay, So more on the military

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<v Speaker 1>angle later on. So this is not necessarily a helpful

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<v Speaker 1>way to understand mud as a whole, but rather to

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<v Speaker 1>a way to underline that the meaning of mud kind

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<v Speaker 1>of depends on what you're trying to do in it

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<v Speaker 1>or through it, and mud therefore could be your threat

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<v Speaker 1>or your treasure, depending on what you're looking to get

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<v Speaker 1>out of the situation.

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<v Speaker 3>Very true. Now, I found an article that I thought

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<v Speaker 3>was helpful. It was from two thousand and three in

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<v Speaker 3>the Washington Post, and being in the Washington Post, I

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<v Speaker 3>would say a little overly concerned with these specific types

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<v Speaker 3>of mud found around the Washington d C. Metro area.

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<v Speaker 3>But I'm mostly ignoring those parts because it does helpfully

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<v Speaker 3>consult a bunch of soil scientists on the definitions and

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<v Speaker 3>categories of mud. So it was called a World Gone

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<v Speaker 3>Mud by Joel Aikenbach from June fifteenth, two thousand and three.

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<v Speaker 3>First of all, it consults a researcher named Trish Steinhilbert

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<v Speaker 3>from the University of Maryland Agricultural Nutrient Management Program, who says,

0:13:00.280 --> 0:13:03.319
<v Speaker 3>you know, we would just call it wet soil. So

0:13:03.320 --> 0:13:06.199
<v Speaker 3>that's one perspective. It's just wet soil, But then the

0:13:06.320 --> 0:13:10.920
<v Speaker 3>article cites another soil physicist, or sorry, another soil researcher,

0:13:11.000 --> 0:13:13.520
<v Speaker 3>this time a soil physicist also from the University of

0:13:13.520 --> 0:13:18.080
<v Speaker 3>Maryland named Robert Hill, who says mud should be differentiated

0:13:18.120 --> 0:13:22.160
<v Speaker 3>from merely wet soil because it has different physical properties.

0:13:22.160 --> 0:13:26.360
<v Speaker 3>As commonly understood, like we've been saying, mud is sticky

0:13:26.679 --> 0:13:29.800
<v Speaker 3>in a way that not all wet soils are, and

0:13:30.080 --> 0:13:33.679
<v Speaker 3>this stickiness is due to the presence of a higher

0:13:33.720 --> 0:13:40.920
<v Speaker 3>proportion of smaller particles, especially clay particles. So, as you

0:13:41.000 --> 0:13:44.960
<v Speaker 3>probably know, soil is made from a mixture of different materials.

0:13:45.040 --> 0:13:47.800
<v Speaker 3>Some of those materials are organic, so they can be

0:13:47.880 --> 0:13:51.720
<v Speaker 3>you know, decaying organic matter or decaying bits of plants

0:13:51.760 --> 0:13:55.160
<v Speaker 3>and animals and all that, but also inorganic matter, and

0:13:55.200 --> 0:13:58.160
<v Speaker 3>we're going to focus on the inorganic matter for the moment.

0:13:58.600 --> 0:14:03.319
<v Speaker 3>The inorganic solid particles that make up soil are generally

0:14:03.360 --> 0:14:07.920
<v Speaker 3>produced by the erosion and breakdown of larger rocks over time,

0:14:08.440 --> 0:14:11.720
<v Speaker 3>which can happen due to physical forces like wind, rain,

0:14:11.840 --> 0:14:14.400
<v Speaker 3>and ice, or it can be due to break down

0:14:14.400 --> 0:14:18.240
<v Speaker 3>by organisms like fungi and bacteria. And we all know

0:14:18.320 --> 0:14:21.440
<v Speaker 3>soil can have different consistencies you stick your hands into

0:14:21.440 --> 0:14:24.560
<v Speaker 3>the soil in one place, it just feels different than

0:14:24.560 --> 0:14:27.640
<v Speaker 3>the soil in another place. One of the major factors

0:14:27.680 --> 0:14:30.720
<v Speaker 3>that you can use to sort soil into different categories

0:14:30.840 --> 0:14:35.680
<v Speaker 3>is the average particle size in the soil. So if

0:14:35.880 --> 0:14:40.280
<v Speaker 3>particles are bigger than two millimeters, that's gravel. You know

0:14:41.360 --> 0:14:44.600
<v Speaker 3>that's going to pop under your car tire. Particles of

0:14:45.320 --> 0:14:49.280
<v Speaker 3>less than two millimeters in diameter but more than zero

0:14:49.400 --> 0:14:54.800
<v Speaker 3>point zero five millimeters are sand. Then smaller than sand,

0:14:55.120 --> 0:14:58.400
<v Speaker 3>you've got silt, which is made of particles less than

0:14:58.560 --> 0:15:01.960
<v Speaker 3>zero point zero five million meters in diameter. And then

0:15:02.000 --> 0:15:05.680
<v Speaker 3>at the very bottom, the finest grain soil is clay,

0:15:05.800 --> 0:15:10.600
<v Speaker 3>which means particles smaller than zero point zero zero two

0:15:11.040 --> 0:15:15.240
<v Speaker 3>millimeters in diameter. Now, apart from particle size, there are

0:15:15.280 --> 0:15:19.400
<v Speaker 3>also some at least common chemical properties you'll find at

0:15:19.440 --> 0:15:23.000
<v Speaker 3>these different areas, like they tend to derive from different

0:15:23.000 --> 0:15:27.160
<v Speaker 3>types of minerals, like clay typically features a standard mineral constituent,

0:15:27.240 --> 0:15:31.840
<v Speaker 3>which is hydrous aluminum philosilicates. But for the moment, we

0:15:31.840 --> 0:15:34.680
<v Speaker 3>can just think about these as particles of different sizes.

0:15:35.120 --> 0:15:39.160
<v Speaker 3>So by one definition, any sufficiently wet soil made of

0:15:39.360 --> 0:15:43.120
<v Speaker 3>any mixture of these particles could be mud. But if

0:15:43.120 --> 0:15:46.600
<v Speaker 3>you're going with the definition of mud as sticky slop

0:15:46.720 --> 0:15:48.760
<v Speaker 3>that kind of sucks to the bottom of your shoes

0:15:48.800 --> 0:15:51.840
<v Speaker 3>and you might get stuck in it usually means it's

0:15:51.880 --> 0:15:56.320
<v Speaker 3>made up of mostly silt and clay sized particles. Silt

0:15:56.360 --> 0:16:00.400
<v Speaker 3>sized and clay sized particles, and things get especially sticky

0:16:00.480 --> 0:16:02.120
<v Speaker 3>if it has a lot of clay.

0:16:02.760 --> 0:16:05.560
<v Speaker 1>And again there's this fine line, Like I know, I

0:16:05.640 --> 0:16:09.120
<v Speaker 1>instantly think back to some cave environments that I've been in,

0:16:09.680 --> 0:16:14.800
<v Speaker 1>and mud at just the right consistency, it's like it's sticky,

0:16:15.000 --> 0:16:17.600
<v Speaker 1>but you're not slipping in it. It's almost something you

0:16:17.640 --> 0:16:21.200
<v Speaker 1>want to walk on. But that line is very thin

0:16:21.520 --> 0:16:25.400
<v Speaker 1>between between that and like the treacherous mud that you

0:16:25.480 --> 0:16:29.680
<v Speaker 1>will slip in. So it's fascinating when you start getting

0:16:29.680 --> 0:16:30.840
<v Speaker 1>into the way this breaks down.

0:16:31.400 --> 0:16:34.960
<v Speaker 3>Yeah, is the mud grippy like maybe rubber? Or will

0:16:34.960 --> 0:16:37.080
<v Speaker 3>it fly out from under you like a banana peel?

0:16:37.800 --> 0:16:41.560
<v Speaker 3>And that does, I think come down to something having

0:16:41.600 --> 0:16:44.120
<v Speaker 3>to do with the water content as well as the

0:16:44.160 --> 0:16:48.360
<v Speaker 3>particle size. So if mud is wet soil or sticky

0:16:48.360 --> 0:16:51.640
<v Speaker 3>wet soil, we've explained the soil part. It tends to

0:16:51.680 --> 0:16:55.240
<v Speaker 3>be the smaller particle sizes clay sized and silt sized

0:16:55.240 --> 0:16:58.160
<v Speaker 3>particles that make mud. But there's also the wetness angle.

0:16:58.280 --> 0:17:00.840
<v Speaker 3>How wet does soil have to be for it to

0:17:00.880 --> 0:17:04.320
<v Speaker 3>be mud. Here we get to the concept of cohesive

0:17:04.440 --> 0:17:09.720
<v Speaker 3>soil and what are called Aderberg limits. So cohesive soils

0:17:09.800 --> 0:17:13.880
<v Speaker 3>are soils that tend to stick or clump together as

0:17:13.920 --> 0:17:18.119
<v Speaker 3>opposed to crumbling. Cohesive soils tend to have again more

0:17:18.280 --> 0:17:23.480
<v Speaker 3>clay sized particles. Smaller particles stick together better, and cohesive

0:17:23.520 --> 0:17:27.240
<v Speaker 3>soils can be in three states, depending on how wet

0:17:27.280 --> 0:17:32.240
<v Speaker 3>they are. These states are non plastic, plastic, and viscous.

0:17:32.880 --> 0:17:37.560
<v Speaker 3>Non Plastic means hard, you know, difficult to mold or deform.

0:17:37.840 --> 0:17:41.320
<v Speaker 3>This is usually when they're dry. Cohesive soils dry up

0:17:41.440 --> 0:17:44.359
<v Speaker 3>kind of hard like bricks, and they form tough earth,

0:17:44.440 --> 0:17:47.560
<v Speaker 3>so you can think about like hard clay ground, you

0:17:47.600 --> 0:17:51.200
<v Speaker 3>know what that's like. When cohesive soils get wet, though,

0:17:51.240 --> 0:17:54.119
<v Speaker 3>they can cross one of these Aderberg limits, that the

0:17:54.119 --> 0:17:57.840
<v Speaker 3>plastic limit and become plastic, so this means they become

0:17:58.040 --> 0:18:03.240
<v Speaker 3>soft or moldable, think about wet clay, and then beyond

0:18:03.400 --> 0:18:06.160
<v Speaker 3>that limit there's another limit, another limit which is the

0:18:06.200 --> 0:18:09.960
<v Speaker 3>liquid limit, and this is the viscous stage where there's

0:18:10.000 --> 0:18:12.919
<v Speaker 3>sort of like a liquid goop. So you can add

0:18:12.960 --> 0:18:16.639
<v Speaker 3>water to non plastic soil until it crosses the plastic limit,

0:18:16.720 --> 0:18:19.879
<v Speaker 3>becomes soft and mouldable, you can add more water until

0:18:19.920 --> 0:18:23.800
<v Speaker 3>it crosses the liquid limit. Where the liquid limit is

0:18:23.800 --> 0:18:27.280
<v Speaker 3>explained in this Washington Post article as if you cut

0:18:27.320 --> 0:18:30.520
<v Speaker 3>a groove in the mud, the mud will flow back

0:18:30.560 --> 0:18:34.120
<v Speaker 3>in to fill it. That's the liquid limit, which actually

0:18:34.240 --> 0:18:38.399
<v Speaker 3>has some analogies in the culinary world, like if you

0:18:38.440 --> 0:18:41.080
<v Speaker 3>ever did the back of the spoon test for the

0:18:41.200 --> 0:18:43.840
<v Speaker 3>thickness of a sauce in the kitchen. The French term

0:18:43.880 --> 0:18:46.280
<v Speaker 3>for that is nape, where if you like wipe your

0:18:46.560 --> 0:18:48.960
<v Speaker 3>the tip of your finger along the back of a

0:18:49.000 --> 0:18:52.199
<v Speaker 3>spoon coated in the sauce, it should leave a trail

0:18:52.400 --> 0:18:54.680
<v Speaker 3>rather than having the sauce flow back in to fill

0:18:54.760 --> 0:18:56.280
<v Speaker 3>the gap. That's nape.

0:18:56.800 --> 0:18:59.080
<v Speaker 1>One of the many culinary techniques in you just like

0:18:59.200 --> 0:19:01.160
<v Speaker 1>jab your finger into things like.

0:19:01.200 --> 0:19:03.520
<v Speaker 3>Yeah, stick, yeah, stick your finger in the food.

0:19:03.840 --> 0:19:06.680
<v Speaker 1>Yeah, let the meat touch your face, and that will

0:19:06.680 --> 0:19:08.520
<v Speaker 1>determine if it is the right temperature.

0:19:08.880 --> 0:19:11.040
<v Speaker 3>But so the definition of the liquid limit is that

0:19:11.119 --> 0:19:13.120
<v Speaker 3>it does not pass the back of the spoon test

0:19:13.160 --> 0:19:14.760
<v Speaker 3>if you cut a groove in it, it will flow

0:19:14.800 --> 0:19:17.560
<v Speaker 3>back in to fill the gap. So it sounds to

0:19:17.600 --> 0:19:22.119
<v Speaker 3>me like the definitional sweet spot for mud is a

0:19:22.160 --> 0:19:26.440
<v Speaker 3>wet cohesive soil. It's made primarily of silt or clay

0:19:26.440 --> 0:19:29.200
<v Speaker 3>sized particles, especially if there's a lot of clay sized

0:19:29.240 --> 0:19:34.320
<v Speaker 3>particles that is above the plastic limit and below the

0:19:34.359 --> 0:19:39.040
<v Speaker 3>liquid limit. Somewhere in there, though, I was thinking that

0:19:39.920 --> 0:19:43.320
<v Speaker 3>even sort of fully liquid glop we do sometimes call mud,

0:19:43.359 --> 0:19:45.679
<v Speaker 3>don't we, But that's not usually the first kind of

0:19:45.720 --> 0:19:46.880
<v Speaker 3>substance I think of.

0:19:47.400 --> 0:19:50.639
<v Speaker 1>Right, right, Like, I come back to the example of

0:19:51.440 --> 0:19:54.600
<v Speaker 1>mud pies. You know, I think a lot of us

0:19:54.600 --> 0:19:56.720
<v Speaker 1>did this as a kid. If you're allowed to play

0:19:56.720 --> 0:19:59.040
<v Speaker 1>in the mud, do you get some little like pie

0:19:59.119 --> 0:20:03.160
<v Speaker 1>crust or little whatever, you know, cups and pans pour

0:20:03.240 --> 0:20:05.960
<v Speaker 1>the mud up, slap the mud together, and then you

0:20:06.000 --> 0:20:08.560
<v Speaker 1>set it in the sun too dry into mud cakes.

0:20:09.440 --> 0:20:11.520
<v Speaker 1>But yeah, it's like if you're pouring it, if you're

0:20:11.560 --> 0:20:14.119
<v Speaker 1>just complete all you know it is completely pouring it

0:20:14.200 --> 0:20:16.920
<v Speaker 1>into the pan, that doesn't really feel like mud. That's

0:20:17.040 --> 0:20:21.199
<v Speaker 1>just like mud water or something that's like on the

0:20:21.240 --> 0:20:23.320
<v Speaker 1>way to mud. But not mud quite yet. The moisture

0:20:23.320 --> 0:20:25.359
<v Speaker 1>still level is too high. And I guess in baking

0:20:25.440 --> 0:20:28.760
<v Speaker 1>you have variations of that as well. Right like you said,

0:20:28.760 --> 0:20:30.960
<v Speaker 1>the sauce is too runny, the batter is too runny,

0:20:30.960 --> 0:20:31.399
<v Speaker 1>et cetera.

0:20:40.840 --> 0:20:42.720
<v Speaker 3>Oh, I think the mudpie test is a good one.

0:20:42.720 --> 0:20:44.960
<v Speaker 3>And you know what, that actually brings me to the

0:20:45.000 --> 0:20:48.280
<v Speaker 3>next thing I want to talk about, which is this

0:20:48.400 --> 0:20:52.520
<v Speaker 3>might be something you've never considered before. Was there a

0:20:52.640 --> 0:20:55.880
<v Speaker 3>time on Earth when it would have been really difficult

0:20:56.280 --> 0:20:59.640
<v Speaker 3>to make a mud pie? I would argue, based on

0:20:59.680 --> 0:21:02.560
<v Speaker 3>some research I've been reading about that, Yes, if you

0:21:02.640 --> 0:21:06.199
<v Speaker 3>go back before five hundred million years ago, go to

0:21:06.200 --> 0:21:09.600
<v Speaker 3>the pre Cambrian period, and you walk around on Earth's

0:21:09.640 --> 0:21:12.880
<v Speaker 3>continents trying to find a place to make a mud pie,

0:21:13.720 --> 0:21:16.240
<v Speaker 3>you're gonna probably strike out. You're gonna be out of luck,

0:21:16.320 --> 0:21:21.960
<v Speaker 3>because there was a time basically before there was mud

0:21:22.160 --> 0:21:25.760
<v Speaker 3>on land on Earth, or before there was very much

0:21:25.840 --> 0:21:28.520
<v Speaker 3>mud to be found on land. So here I want

0:21:28.560 --> 0:21:30.520
<v Speaker 3>to go to an article I was reading in the

0:21:30.640 --> 0:21:34.800
<v Speaker 3>journal Science in the year twenty eighteen by Woodward Fisher,

0:21:34.880 --> 0:21:40.000
<v Speaker 3>who is a Caltech geobiologist. The article is called Early

0:21:40.080 --> 0:21:44.119
<v Speaker 3>Plants and the Rise of mud, and this article is

0:21:44.200 --> 0:21:49.960
<v Speaker 3>primarily summarizing and contextualizing a study that was published by

0:21:49.960 --> 0:21:52.119
<v Speaker 3>a couple of different authors in the same issue of

0:21:52.200 --> 0:21:56.040
<v Speaker 3>the journal Science in twenty eighteen. This article is very

0:21:56.040 --> 0:22:01.840
<v Speaker 3>good in putting these findings in context. So Fisher mentions

0:22:01.880 --> 0:22:05.800
<v Speaker 3>that you know, life on Earth has several times that

0:22:05.840 --> 0:22:12.320
<v Speaker 3>we know about reshaped fundamental geophysical features and processes at

0:22:12.359 --> 0:22:15.360
<v Speaker 3>the Earth's surface. There are ways in which you could

0:22:15.400 --> 0:22:19.960
<v Speaker 3>say that life has fundamentally changed the planet itself, at

0:22:20.040 --> 0:22:22.360
<v Speaker 3>least what's happening on the surface and in the atmosphere.

0:22:22.760 --> 0:22:26.199
<v Speaker 3>So perhaps the first example that will likely come to

0:22:26.240 --> 0:22:30.840
<v Speaker 3>your mind is the oxygenation of the oceans in the atmosphere.

0:22:31.040 --> 0:22:35.440
<v Speaker 3>It was the evolution of photosynthesis in cyanobacteria and other

0:22:35.520 --> 0:22:38.760
<v Speaker 3>life forms that triggered this shift. You know, we didn't

0:22:38.760 --> 0:22:43.479
<v Speaker 3>always have an oxygen atmosphere. Another major geophysical change triggered

0:22:43.520 --> 0:22:47.760
<v Speaker 3>by life that Fisher mentions is the evolution of mineral

0:22:48.000 --> 0:22:53.920
<v Speaker 3>skeletons by life forms, again, particularly algae, and the presence

0:22:53.920 --> 0:22:57.920
<v Speaker 3>of those skeletons change the way that ocean floors are formed,

0:22:57.960 --> 0:23:01.440
<v Speaker 3>and then subsequently the kinds of rock lay that would

0:23:01.480 --> 0:23:05.159
<v Speaker 3>form when they solidified. Over the eons. But this article

0:23:05.240 --> 0:23:09.679
<v Speaker 3>is focused on another discovery of this sort, how the

0:23:09.720 --> 0:23:16.160
<v Speaker 3>evolution of land based plants changed the Earth by affecting mud.

0:23:16.760 --> 0:23:20.159
<v Speaker 3>So the citation for the study here is William J.

0:23:20.320 --> 0:23:24.160
<v Speaker 3>McMahon and Neil S. Davies. The article is called evolution

0:23:24.359 --> 0:23:28.720
<v Speaker 3>of alluvial mud rock forced by early land plants again

0:23:28.880 --> 0:23:34.040
<v Speaker 3>Journal Science, twenty eighteen. So when soil made mostly out

0:23:34.040 --> 0:23:37.480
<v Speaker 3>of clay or silt sized particles gets compacted in the

0:23:37.520 --> 0:23:42.320
<v Speaker 3>ground and lithifies into rock, the resulting rock layer is

0:23:42.400 --> 0:23:45.240
<v Speaker 3>called mud rock, and there are many kinds of mud rock.

0:23:46.480 --> 0:23:50.520
<v Speaker 3>When geologists look for layers of mud rock from the past,

0:23:50.960 --> 0:23:56.000
<v Speaker 3>they notice something interesting. There is extremely little mud rock

0:23:56.240 --> 0:24:01.200
<v Speaker 3>from river bottoms and floodplains before a geologic period in

0:24:01.280 --> 0:24:02.879
<v Speaker 3>the history of the Earth. So if you look in

0:24:02.920 --> 0:24:07.080
<v Speaker 3>the pre Cambrian era or the early Paleozoic era, there's

0:24:07.280 --> 0:24:11.480
<v Speaker 3>very little mud rock on the continents. And I'll do

0:24:11.520 --> 0:24:14.320
<v Speaker 3>a little refresher on the basic geologic timeline of the

0:24:14.920 --> 0:24:18.040
<v Speaker 3>early to mid Palaeozoic, So you've got the Cambrian period.

0:24:18.640 --> 0:24:22.159
<v Speaker 3>This is roughly five hundred million years ago. Before the

0:24:22.160 --> 0:24:27.840
<v Speaker 3>Cambrian period, most life on Earth is small soft and unicellular,

0:24:28.320 --> 0:24:32.360
<v Speaker 3>and then the Cambrian period represents a sort of explosion

0:24:32.440 --> 0:24:36.680
<v Speaker 3>of life, a massive proliferation in the diversity of life forms.

0:24:37.040 --> 0:24:41.119
<v Speaker 3>Life Forms get bigger, more complex, with hard body parts

0:24:41.160 --> 0:24:44.359
<v Speaker 3>that get fossilized. So think of the age of trilobytes

0:24:44.440 --> 0:24:48.080
<v Speaker 3>and anomalicaras. That's a period of like forty or fifty

0:24:48.119 --> 0:24:51.320
<v Speaker 3>million years, roughly five hundred million years ago. And then

0:24:51.359 --> 0:24:54.160
<v Speaker 3>you've got after that the Ordovician period, which is about

0:24:54.200 --> 0:24:56.760
<v Speaker 3>four hundred and eighty five to four hundred and forty

0:24:56.800 --> 0:25:01.320
<v Speaker 3>four million years ago, more diversification of life forms, primarily

0:25:01.359 --> 0:25:05.919
<v Speaker 3>in the ocean, arthropods, molluscs, so forth, and the appearance

0:25:06.080 --> 0:25:09.520
<v Speaker 3>of the very first primitive land plants. Then you've got

0:25:09.520 --> 0:25:12.560
<v Speaker 3>the Silurian period, which is like four forty four to

0:25:12.600 --> 0:25:16.399
<v Speaker 3>four nineteen million years ago. Note that this is separated

0:25:16.400 --> 0:25:21.119
<v Speaker 3>from the previous era by the Ordovisian Silurian extinction event.

0:25:21.160 --> 0:25:25.480
<v Speaker 3>There's often an extinction event separating these periods. This period

0:25:25.560 --> 0:25:30.200
<v Speaker 3>shows diversification in fish and other marine fauna, but it's

0:25:30.240 --> 0:25:34.639
<v Speaker 3>also important because of sort of a terrestrial revolution, the

0:25:34.760 --> 0:25:38.880
<v Speaker 3>terrestrialization of many branches of life. Suddenly a lot more

0:25:38.920 --> 0:25:41.679
<v Speaker 3>is happening on land instead of just in the ocean.

0:25:41.760 --> 0:25:46.760
<v Speaker 3>So you have the evolution of vascular plants and terrestrial fungi,

0:25:47.400 --> 0:25:50.960
<v Speaker 3>and these lead to changes in land ecosystems, including the

0:25:50.960 --> 0:25:55.000
<v Speaker 3>ones we're talking about now. Also, land based arthropods diversify,

0:25:55.160 --> 0:25:57.919
<v Speaker 3>so you get the ancestors of animals like spiders and

0:25:58.000 --> 0:26:02.000
<v Speaker 3>insects and so forth. After that, from like four nineteen

0:26:02.040 --> 0:26:04.160
<v Speaker 3>to three hundred and fifty nine million years ago, you've

0:26:04.200 --> 0:26:07.679
<v Speaker 3>got the Devonian Period, sometimes called the Age of Fishes.

0:26:07.960 --> 0:26:11.560
<v Speaker 3>Obviously there's a lot of fish diversification here, the terrestrial

0:26:11.640 --> 0:26:15.439
<v Speaker 3>revolution continues, and then later in the Devonian period, this

0:26:15.520 --> 0:26:18.240
<v Speaker 3>is the first time that you have the continents covered

0:26:18.320 --> 0:26:21.679
<v Speaker 3>in forests of plants of the kind of things we

0:26:21.680 --> 0:26:25.000
<v Speaker 3>would recognize as trees. But coming back to how this

0:26:25.680 --> 0:26:29.119
<v Speaker 3>geologic timeline relates to mud, So in the Precambrian in

0:26:29.119 --> 0:26:34.120
<v Speaker 3>continuing into the early Paleozoic, there is very little river

0:26:34.520 --> 0:26:38.400
<v Speaker 3>mud rock showing up in the geologic strata. Instead, lithified

0:26:38.520 --> 0:26:42.800
<v Speaker 3>river beds seem to contain sand and gravel, and as

0:26:42.920 --> 0:26:48.320
<v Speaker 3>the Paleozoic era progresses, there is a rise in the

0:26:48.359 --> 0:26:52.280
<v Speaker 3>formation of mud rocks in river deposits, which seems to

0:26:52.320 --> 0:26:56.760
<v Speaker 3>indicate a global change in how sediment gets pushed and

0:26:56.840 --> 0:27:01.320
<v Speaker 3>pulled around by rivers, and this change is associated with

0:27:01.400 --> 0:27:05.119
<v Speaker 3>the colonization of the continents by plant life. There's an

0:27:05.160 --> 0:27:09.560
<v Speaker 3>interesting analogy which is Mars. Mars we believe once had

0:27:09.600 --> 0:27:13.359
<v Speaker 3>flowing rivers, but presumably did not have plants. And it

0:27:13.400 --> 0:27:16.600
<v Speaker 3>also appears that Mars has very little mud rock in

0:27:16.680 --> 0:27:17.760
<v Speaker 3>its river deposits.

0:27:18.240 --> 0:27:21.040
<v Speaker 1>Though we will come back to the topic of mud

0:27:21.080 --> 0:27:23.800
<v Speaker 1>on Mars. Is there mud on Mars? You might ask,

0:27:24.000 --> 0:27:26.960
<v Speaker 1>how we'll tune in to a future episode.

0:27:27.359 --> 0:27:31.720
<v Speaker 3>Mars needs goloshes. Yeah. So the authors of this twenty

0:27:31.720 --> 0:27:34.800
<v Speaker 3>eighteen paper, McMahon and Davies, they wanted to zero in

0:27:34.880 --> 0:27:37.960
<v Speaker 3>on this change in mud rock deposition in Earth's history

0:27:38.000 --> 0:27:41.119
<v Speaker 3>and understand it better. So they were looking at samples

0:27:41.200 --> 0:27:45.480
<v Speaker 3>of rock strata from ancient river beds before and after

0:27:45.640 --> 0:27:48.879
<v Speaker 3>the land plant revolution all throughout this time period to

0:27:49.040 --> 0:27:52.440
<v Speaker 3>measure the relative amount of mud rock corresponding to the

0:27:52.480 --> 0:27:56.920
<v Speaker 3>different eras, and after crunching the numbers, they concluded that

0:27:57.000 --> 0:28:02.040
<v Speaker 3>the fractional portion of mud rock the geologic strata rose

0:28:02.200 --> 0:28:05.119
<v Speaker 3>by more than an order of magnitude an order of

0:28:05.119 --> 0:28:09.280
<v Speaker 3>magnitude is ten times, so more than ten times increase

0:28:09.440 --> 0:28:11.560
<v Speaker 3>in the proportion of mud rock I think in their

0:28:11.600 --> 0:28:14.320
<v Speaker 3>abstract they actually say it was one point four orders

0:28:14.359 --> 0:28:19.240
<v Speaker 3>of magnitude. This is after land plants evolved, so when

0:28:19.280 --> 0:28:24.080
<v Speaker 3>plants colonized land, it made a huge profound change in

0:28:24.320 --> 0:28:29.040
<v Speaker 3>what was happening with sediment, meaning mud, primarily in river

0:28:29.119 --> 0:28:33.959
<v Speaker 3>bottoms and floodplains. The increase in these rocks made out

0:28:34.000 --> 0:28:39.400
<v Speaker 3>of mud began in the late Ordovisian and continuing to

0:28:39.560 --> 0:28:43.480
<v Speaker 3>the beginning of the Silurian, and this does implicate early

0:28:43.600 --> 0:28:47.000
<v Speaker 3>land plants, but it's also interestingly it's earlier than the

0:28:47.040 --> 0:28:51.440
<v Speaker 3>researchers expected to find it, perhaps in part because or

0:28:51.480 --> 0:28:55.120
<v Speaker 3>perhaps their expectations for finding increases in mud rock in

0:28:55.120 --> 0:28:58.600
<v Speaker 3>this period were low, because the earliest land plants here

0:28:58.680 --> 0:29:03.400
<v Speaker 3>were they're really, I think mostly like bryophytes. They're these

0:29:03.480 --> 0:29:07.640
<v Speaker 3>kind of little patchy green things that would resemble mosses

0:29:07.760 --> 0:29:10.520
<v Speaker 3>or liver warts, so you know, we're not talking about

0:29:10.600 --> 0:29:15.120
<v Speaker 3>jungles yet. Vascular plants meaning plants that have tissues that

0:29:15.200 --> 0:29:18.240
<v Speaker 3>allow them to grow tall because they can conduct water

0:29:18.440 --> 0:29:22.280
<v Speaker 3>and mineral nutrients up their stems. They start to appear

0:29:22.360 --> 0:29:26.000
<v Speaker 3>in the late Silurian and early Devonian, but the earliest

0:29:26.040 --> 0:29:28.880
<v Speaker 3>of these plants would only be a few centimeters off

0:29:28.960 --> 0:29:32.200
<v Speaker 3>the ground and could only survive in wet environments. It

0:29:32.280 --> 0:29:35.680
<v Speaker 3>isn't until again the Late Devonian, maybe like three hundred

0:29:35.720 --> 0:29:38.760
<v Speaker 3>and seventy million years ago or so, that you first

0:29:38.800 --> 0:29:42.560
<v Speaker 3>get what we would think of as forests, landscapes thick

0:29:42.680 --> 0:29:47.400
<v Speaker 3>with relatively tall, vascular plants. But according to this research,

0:29:47.520 --> 0:29:51.720
<v Speaker 3>even these earlier phases of puny, little baby plants, little mossy,

0:29:51.840 --> 0:29:55.200
<v Speaker 3>liver warty type things, made a pretty big difference in

0:29:55.280 --> 0:29:58.880
<v Speaker 3>how mud was distributed on the earth. But when you

0:29:58.920 --> 0:30:02.640
<v Speaker 3>get to the later div and then into the Carboniferous period,

0:30:02.920 --> 0:30:05.400
<v Speaker 3>there is an even bigger shift. This is the phase

0:30:05.440 --> 0:30:09.360
<v Speaker 3>where there would again be forests of like impressive woody

0:30:09.440 --> 0:30:13.720
<v Speaker 3>trees with deep root structures, like the things we think

0:30:13.760 --> 0:30:19.280
<v Speaker 3>of as forests today. Rob I'm including an illustrated graph

0:30:19.320 --> 0:30:22.760
<v Speaker 3>with a timeline from this article for you to look at.

0:30:23.120 --> 0:30:26.160
<v Speaker 3>You can see that the amount of mud rock starts

0:30:26.160 --> 0:30:28.520
<v Speaker 3>to go up during the period of like the bryophytes,

0:30:28.600 --> 0:30:32.120
<v Speaker 3>these little primitive land plants, and then it really reaches

0:30:32.280 --> 0:30:35.560
<v Speaker 3>its peak in the era of vascular plants, and especially

0:30:35.600 --> 0:30:39.280
<v Speaker 3>like woody trees and later vascular plants, it seems like

0:30:39.320 --> 0:30:42.800
<v Speaker 3>those deep root systems played a big role in that

0:30:42.880 --> 0:30:46.440
<v Speaker 3>later period. However, I think, to come back on this,

0:30:46.560 --> 0:30:50.000
<v Speaker 3>it's really worth noting that the Earth was not without

0:30:50.280 --> 0:30:54.560
<v Speaker 3>mud as a planet before the proliferation of land plants.

0:30:54.600 --> 0:30:57.560
<v Speaker 3>It looks like land plants played a huge role in

0:30:57.680 --> 0:31:02.320
<v Speaker 3>forming these continental mud rock But there was mud before

0:31:02.400 --> 0:31:05.680
<v Speaker 3>the plants. A sediment of clay and silt sized particles

0:31:05.720 --> 0:31:09.880
<v Speaker 3>has been produced by erosion of surface rocks for billions

0:31:09.920 --> 0:31:12.920
<v Speaker 3>of years. So what appears to have changed with the

0:31:12.960 --> 0:31:17.200
<v Speaker 3>evolution of land plants is that mud started to stay

0:31:17.320 --> 0:31:21.080
<v Speaker 3>on land, to stay on the continents, as opposed to

0:31:21.280 --> 0:31:24.560
<v Speaker 3>just being blown or washed out to sea and settling

0:31:24.560 --> 0:31:28.600
<v Speaker 3>on the seafloor. So the question is why did the

0:31:28.640 --> 0:31:33.240
<v Speaker 3>evolution of plants lead to the retention of mud on land?

0:31:33.360 --> 0:31:37.320
<v Speaker 3>And the article mentions a few ideas. One thing, first

0:31:37.360 --> 0:31:39.560
<v Speaker 3>of all is that the authors say that the presence

0:31:39.560 --> 0:31:42.960
<v Speaker 3>of land plants may actually have helped produce more mud

0:31:43.000 --> 0:31:47.920
<v Speaker 3>particles to begin with, lead to erosion processes that would

0:31:47.920 --> 0:31:51.000
<v Speaker 3>produce more mud. Now, how would plants help produce more

0:31:51.080 --> 0:31:53.800
<v Speaker 3>mud well. For one thing, I was reading this in

0:31:53.840 --> 0:31:58.640
<v Speaker 3>another article that plants with strong root structures actually break

0:31:58.800 --> 0:32:03.040
<v Speaker 3>and crumble large pieces of rock. Those roots can break

0:32:03.120 --> 0:32:06.200
<v Speaker 3>up the rocks physically, crack and break them, but can

0:32:06.240 --> 0:32:09.360
<v Speaker 3>also lead to changes in the chemical composition of soil

0:32:09.480 --> 0:32:13.880
<v Speaker 3>that break down rocks even further into smaller pieces. But again,

0:32:13.920 --> 0:32:17.160
<v Speaker 3>we don't need plants for mud to exist. There's always

0:32:17.200 --> 0:32:20.520
<v Speaker 3>been these mud sized the soil particles. So what other

0:32:20.600 --> 0:32:24.560
<v Speaker 3>changes did plants introduce? Fissure rites quote. It is therefore

0:32:24.680 --> 0:32:28.960
<v Speaker 3>likely that early plants affected the mechanics of flood plain construction.

0:32:29.440 --> 0:32:33.440
<v Speaker 3>For example, the presence of plants on the landscape decreases

0:32:33.480 --> 0:32:37.160
<v Speaker 3>erosion rates, and thus it was long hypothesized that erosion,

0:32:37.240 --> 0:32:42.400
<v Speaker 3>in particular by wind, removed sediment from pre vegetated landscapes.

0:32:42.800 --> 0:32:46.560
<v Speaker 3>Even if mud was deposited on pre vegetated floodplains, its

0:32:46.600 --> 0:32:51.280
<v Speaker 3>removal by erosion might have been efficient. So before there

0:32:51.280 --> 0:32:54.360
<v Speaker 3>were plants on land, it was just too easy for

0:32:54.560 --> 0:32:58.120
<v Speaker 3>small particles of soil to get washed out to the

0:32:58.200 --> 0:33:00.920
<v Speaker 3>sea one way or another. They could get by wind,

0:33:01.240 --> 0:33:03.560
<v Speaker 3>they could get carried along by the flow of water

0:33:03.640 --> 0:33:06.320
<v Speaker 3>after storms and rain, and they would all just end

0:33:06.400 --> 0:33:08.840
<v Speaker 3>up on the floor of the ocean. So it seems

0:33:08.880 --> 0:33:13.320
<v Speaker 3>like plants and their root structures helped prevent small soil

0:33:13.400 --> 0:33:17.680
<v Speaker 3>particles that form mud from escaping into the sea. But

0:33:18.040 --> 0:33:21.239
<v Speaker 3>it doesn't stop there. Plants and the mud that the

0:33:21.240 --> 0:33:27.480
<v Speaker 3>plants retained changed how rivers form, Fisher writes quote. In

0:33:27.480 --> 0:33:31.640
<v Speaker 3>addition to an inhibiting erosion, plants also interact with river

0:33:31.800 --> 0:33:35.479
<v Speaker 3>flows and promote the deposition of fine grained sediment. This

0:33:35.560 --> 0:33:39.480
<v Speaker 3>can help armor river banks and slow their lateral migration.

0:33:39.960 --> 0:33:44.440
<v Speaker 3>Such process might also aid in preserving muddy floodplain deposits,

0:33:45.080 --> 0:33:48.680
<v Speaker 3>so plants might sort of help stabilize the structure of

0:33:48.800 --> 0:33:52.080
<v Speaker 3>rivers and keep the banks from drifting all over the

0:33:52.120 --> 0:33:56.160
<v Speaker 3>place and changing too rapidly, especially during floods, which helps

0:33:56.200 --> 0:34:00.280
<v Speaker 3>protect the mud that gathers in floodplains and keeps it there.

0:34:00.720 --> 0:34:03.880
<v Speaker 1>Fascinating. Fascinating that the plant's kind of corralling the mud

0:34:04.520 --> 0:34:06.800
<v Speaker 1>in many cases. And I think if you've ever been

0:34:06.840 --> 0:34:09.479
<v Speaker 1>in a like especially I'm thinking of like estuary type

0:34:09.560 --> 0:34:15.360
<v Speaker 1>environments that I've visited, Like you see these elaborate root systems,

0:34:15.360 --> 0:34:19.160
<v Speaker 1>You see the mud and the sediment. So that's what

0:34:19.200 --> 0:34:21.000
<v Speaker 1>I'm picturing during all of this.

0:34:21.440 --> 0:34:23.400
<v Speaker 3>Oh yeah, yeah, yeah. And so actually, to help us

0:34:23.440 --> 0:34:26.040
<v Speaker 3>better picture it, I found another great article that's on

0:34:26.120 --> 0:34:29.000
<v Speaker 3>the same subject, that's on this type of research, but

0:34:29.160 --> 0:34:32.920
<v Speaker 3>it includes a lot more context and imagery to help

0:34:33.000 --> 0:34:36.160
<v Speaker 3>us understand it. So this other article was called the

0:34:36.200 --> 0:34:40.520
<v Speaker 3>Origin of Mud from a magazine called Knowable, written by

0:34:40.680 --> 0:34:44.720
<v Speaker 3>a writer named Laura Poppic, published in August twenty twenty,

0:34:45.320 --> 0:34:47.480
<v Speaker 3>and I thought this was interesting. This article starts with

0:34:47.600 --> 0:34:50.600
<v Speaker 3>this anecdote about one of the two authors of that

0:34:50.640 --> 0:34:54.640
<v Speaker 3>twenty eighteen study, the geologist Neil Davies. It starts with

0:34:54.719 --> 0:34:58.200
<v Speaker 3>this anecdote about him picking through a large fossil formation

0:34:58.320 --> 0:35:00.719
<v Speaker 3>from about four hundred and sixty million years ago in

0:35:00.800 --> 0:35:07.120
<v Speaker 3>Bolivia containing just tons of smothered fish fish that all

0:35:07.200 --> 0:35:09.480
<v Speaker 3>seemed to die at the same time. And apparently this

0:35:09.560 --> 0:35:14.360
<v Speaker 3>is not uncommon for marine fossil formations from this period.

0:35:14.400 --> 0:35:19.080
<v Speaker 3>You'd have large numbers of fossil fish living near an

0:35:19.120 --> 0:35:21.960
<v Speaker 3>ancient shoreline that appear to have all died around the

0:35:22.000 --> 0:35:25.920
<v Speaker 3>same time by being choked by mud. So the explanation

0:35:26.000 --> 0:35:29.920
<v Speaker 3>for this is probably that there's all this muddy sediment

0:35:30.320 --> 0:35:33.880
<v Speaker 3>that is suddenly washed into the water into the ocean

0:35:34.000 --> 0:35:36.880
<v Speaker 3>along the shore, possibly by a storm, and then the

0:35:36.880 --> 0:35:40.440
<v Speaker 3>fish underwent death by mud. So this was four hundred

0:35:40.480 --> 0:35:43.720
<v Speaker 3>and sixty million years ago before the proliferation of land

0:35:43.800 --> 0:35:47.880
<v Speaker 3>plants Poppic writes quote magnified this effect globally, and the

0:35:47.960 --> 0:35:51.479
<v Speaker 3>impacts would have been substantial, not just on coastal life,

0:35:51.560 --> 0:35:55.360
<v Speaker 3>but on the landscape of the entire planet. Before plants,

0:35:55.760 --> 0:35:59.359
<v Speaker 3>rivers would have stripped continents of silt and clay key

0:35:59.360 --> 0:36:03.200
<v Speaker 3>constituents of mud, and sent these sediments to the seafloor.

0:36:03.600 --> 0:36:06.880
<v Speaker 3>This would have left continents full of barren rock and

0:36:07.000 --> 0:36:09.040
<v Speaker 3>seas with smothered fish.

0:36:09.400 --> 0:36:11.880
<v Speaker 1>So primordial muddy oceans.

0:36:11.920 --> 0:36:14.520
<v Speaker 3>Yes, especially at least around like where the rivers would

0:36:14.600 --> 0:36:18.759
<v Speaker 3>drain into them, and landscapes with very little mud at all,

0:36:18.840 --> 0:36:20.200
<v Speaker 3>you know, I mean, you can just let your dog

0:36:20.280 --> 0:36:22.040
<v Speaker 3>run all over it and then come inside the house.

0:36:22.040 --> 0:36:22.840
<v Speaker 3>There's no problem.

0:36:23.280 --> 0:36:26.080
<v Speaker 1>Yeah. I keep wondering if a wellsy and time traveler

0:36:26.080 --> 0:36:30.480
<v Speaker 1>would have to bring his Victorian galoshes in visiting this

0:36:30.600 --> 0:36:31.280
<v Speaker 1>time period.

0:36:31.640 --> 0:36:35.120
<v Speaker 3>But of course plants change all of this. Vegetation, especially

0:36:35.160 --> 0:36:40.440
<v Speaker 3>along river banks, gave mud sized particles something to cling to,

0:36:40.960 --> 0:36:43.480
<v Speaker 3>and so the mud stayed on land rather than getting

0:36:43.640 --> 0:36:46.440
<v Speaker 3>washed or blown out to sea. And in the words

0:36:46.520 --> 0:36:49.800
<v Speaker 3>of Neil Davies, this retention of mud on land quote

0:36:49.880 --> 0:36:53.200
<v Speaker 3>fundamentally changed the way the world operates.

0:36:53.960 --> 0:36:54.520
<v Speaker 1>Wow.

0:37:03.920 --> 0:37:06.560
<v Speaker 3>And so there are some examples of how this mud

0:37:06.600 --> 0:37:11.640
<v Speaker 3>revolution changed the continents, changed the world. Essentially, one thing

0:37:11.719 --> 0:37:15.160
<v Speaker 3>is that the geological record reveals that before the evolution

0:37:15.239 --> 0:37:19.319
<v Speaker 3>of plants, earth rivers probably would have looked more like

0:37:19.680 --> 0:37:23.160
<v Speaker 3>the comparison that Poppuic uses is the rivers found around

0:37:23.200 --> 0:37:27.680
<v Speaker 3>the Gravelly Coast of Alaska today, And she describes these

0:37:28.680 --> 0:37:31.279
<v Speaker 3>I'm trying to say, so like, imagine if you've ever

0:37:31.320 --> 0:37:35.239
<v Speaker 3>seen the kinds of branching, braided channels you see as

0:37:35.280 --> 0:37:40.520
<v Speaker 3>a stream flows into the ocean across a sandy beach.

0:37:40.640 --> 0:37:43.200
<v Speaker 3>So not mud, but you've seen like a stream flowing

0:37:43.239 --> 0:37:44.280
<v Speaker 3>over a sandy beach.

0:37:44.800 --> 0:37:45.040
<v Speaker 1>Yeah.

0:37:45.160 --> 0:37:48.640
<v Speaker 3>Yeah. What you'll usually notice is there is not a

0:37:48.800 --> 0:37:53.560
<v Speaker 3>very strong, unified channel. Instead, there's just lots of little

0:37:53.800 --> 0:37:59.240
<v Speaker 3>threads of channels crisscrossing and always changing. This is referred

0:37:59.239 --> 0:38:00.880
<v Speaker 3>to in several sos as I looked at as a

0:38:01.000 --> 0:38:07.240
<v Speaker 3>braided structure of alluvial flow. The introduction of plants seems

0:38:07.239 --> 0:38:10.319
<v Speaker 3>to have changed this by holding mud in place, and

0:38:10.400 --> 0:38:14.960
<v Speaker 3>the mud being sticky would solidify the form of river banks,

0:38:15.360 --> 0:38:19.600
<v Speaker 3>and this led to stable single channel rivers with fixed

0:38:19.640 --> 0:38:23.920
<v Speaker 3>banks and boundaries, rather than these little shrubs of different

0:38:24.000 --> 0:38:27.279
<v Speaker 3>rivulets changing all the time, so you end up with

0:38:27.280 --> 0:38:31.400
<v Speaker 3>the curving, defined s shaped rivers that we see today.

0:38:32.320 --> 0:38:35.480
<v Speaker 3>These rivers are made possible by the presence of mud,

0:38:35.560 --> 0:38:40.040
<v Speaker 3>which is held on land by plants. Now, these changes

0:38:40.080 --> 0:38:44.560
<v Speaker 3>in rivers had all kinds of interesting biological consequences. For example,

0:38:45.160 --> 0:38:48.400
<v Speaker 3>the bins in a river can alter things like the

0:38:48.440 --> 0:38:51.760
<v Speaker 3>temperature and chemistry and the water compared to a straight

0:38:51.800 --> 0:38:55.640
<v Speaker 3>flowing river, which can create different micro environments along the

0:38:55.719 --> 0:38:58.520
<v Speaker 3>river's length, so that gives all kinds of different little

0:38:59.440 --> 0:39:02.960
<v Speaker 3>tiny eco systems and habitats that organisms would have to

0:39:03.000 --> 0:39:07.080
<v Speaker 3>adapt to. But the presence of mud itself is also

0:39:07.200 --> 0:39:11.440
<v Speaker 3>biologically relevant because mud is a habitat, so it takes

0:39:11.600 --> 0:39:16.239
<v Speaker 3>special skills and evolutionary adaptations to live in mud and

0:39:16.360 --> 0:39:19.760
<v Speaker 3>move around and navigate your way through it. For example,

0:39:19.800 --> 0:39:23.239
<v Speaker 3>it takes different types of adaptations for movement for a

0:39:23.280 --> 0:39:26.120
<v Speaker 3>small animal to get through mud than it does to

0:39:26.160 --> 0:39:29.279
<v Speaker 3>get through sand or some other type of surface. And

0:39:30.160 --> 0:39:33.920
<v Speaker 3>Poppy's article consults a geologist at the University of Oxford

0:39:34.320 --> 0:39:37.759
<v Speaker 3>named Anthony Shalito on this subject. I thought this was

0:39:37.760 --> 0:39:41.760
<v Speaker 3>so interesting, so Shaldo says, here, I'm quoting from popic quote.

0:39:41.800 --> 0:39:44.160
<v Speaker 3>To get through mud, and animals such as a worm,

0:39:44.239 --> 0:39:49.680
<v Speaker 3>creates cracks to shuffle through by contracting its body, extending it,

0:39:50.080 --> 0:39:53.719
<v Speaker 3>squeezing water out of the way, and moving forward. This

0:39:53.760 --> 0:39:57.359
<v Speaker 3>is mechanically different from traveling through sand, which requires an

0:39:57.360 --> 0:40:01.680
<v Speaker 3>animal to excavate material out of the way. Chiledo says,

0:40:02.200 --> 0:40:04.880
<v Speaker 3>so early land worms and insects would have had to

0:40:04.920 --> 0:40:08.920
<v Speaker 3>evolve body parts equipped to deal with muckier movements, but

0:40:09.000 --> 0:40:12.360
<v Speaker 3>then in turn the animals that adapt to those muddy

0:40:12.440 --> 0:40:17.400
<v Speaker 3>environments change them because Poppic then sites a paleobiologist from

0:40:17.520 --> 0:40:20.960
<v Speaker 3>Yale named Lydia Tehran who says that you know, like

0:40:21.000 --> 0:40:25.240
<v Speaker 3>these animals living in the muddy soil around river banks,

0:40:25.400 --> 0:40:28.399
<v Speaker 3>they dig in the mud, they excavate the mud, and

0:40:28.600 --> 0:40:32.480
<v Speaker 3>this for one thing, it affects the chemistry of the mud,

0:40:32.760 --> 0:40:35.719
<v Speaker 3>but it also sort of like breaks and loosens it up,

0:40:35.800 --> 0:40:39.160
<v Speaker 3>which allows the mud to further disperse throughout the rivers

0:40:39.200 --> 0:40:42.560
<v Speaker 3>and then also across flood plains, so you know, the

0:40:42.680 --> 0:40:45.920
<v Speaker 3>valleys where rivers form between the higher areas of the land.

0:40:46.440 --> 0:40:49.920
<v Speaker 3>So because you get these single channel s shaped rivers

0:40:49.960 --> 0:40:54.560
<v Speaker 3>with more defined banks, you get these downstream processes that

0:40:54.640 --> 0:40:58.160
<v Speaker 3>lead to the build up of muddy flood plains around them,

0:40:58.800 --> 0:41:02.040
<v Speaker 3>which don't form as easy along the kind of rivers

0:41:02.080 --> 0:41:04.000
<v Speaker 3>you see forming in sand or gravel.

0:41:04.680 --> 0:41:08.480
<v Speaker 1>This is fascinating. I'm looking forward to getting back to

0:41:08.520 --> 0:41:10.919
<v Speaker 1>some of this in our episode that's going to deal

0:41:10.960 --> 0:41:14.960
<v Speaker 1>more with the specifics of some of the animals in

0:41:14.960 --> 0:41:17.840
<v Speaker 1>the world today that make their home on the mud.

0:41:18.239 --> 0:41:21.000
<v Speaker 3>Oh yeah, absolutely. But I love this story because it's

0:41:21.040 --> 0:41:24.160
<v Speaker 3>just one of these amazing examples of how much, you know,

0:41:24.280 --> 0:41:30.520
<v Speaker 3>sometimes we don't stop to appreciate the inner play between

0:41:30.800 --> 0:41:33.600
<v Speaker 3>like earth and water and life, and the way that

0:41:33.640 --> 0:41:37.719
<v Speaker 3>they all are constantly changing each other. That there's this

0:41:37.840 --> 0:41:41.440
<v Speaker 3>like massive, you know, process like the mud revolution caused

0:41:41.480 --> 0:41:45.399
<v Speaker 3>by the evolution of plants on land further gives rise

0:41:45.480 --> 0:41:49.600
<v Speaker 3>to all of these these changes in land based life,

0:41:50.080 --> 0:41:53.319
<v Speaker 3>which helps give give rise to more changes in like

0:41:53.360 --> 0:41:56.920
<v Speaker 3>how mud accumulates and how sediment is distributed in floodplains

0:41:56.960 --> 0:41:59.320
<v Speaker 3>and so forth. So I guess by way of research,

0:41:59.360 --> 0:42:02.640
<v Speaker 3>we have once again and arrived at cliche. But sometimes

0:42:02.680 --> 0:42:05.200
<v Speaker 3>that's how it is. I mean, it's the life and

0:42:05.239 --> 0:42:08.200
<v Speaker 3>the inorganic systems that support life, the surface of the earth.

0:42:08.520 --> 0:42:10.240
<v Speaker 3>It's a web of interactions.

0:42:10.600 --> 0:42:12.839
<v Speaker 1>Yeah, And I think it is easy to sort of

0:42:13.120 --> 0:42:16.040
<v Speaker 1>fall back on just sort of the school textbook mental

0:42:16.080 --> 0:42:21.560
<v Speaker 1>image of fish flops onto a beach, fish flops onto

0:42:21.640 --> 0:42:24.480
<v Speaker 1>some rocks, and now life on earth has begun, you know,

0:42:24.640 --> 0:42:28.720
<v Speaker 1>like sort of not considering mud is this vital realm

0:42:29.320 --> 0:42:32.040
<v Speaker 1>of evolution and transference.

0:42:31.719 --> 0:42:35.359
<v Speaker 3>And human culture and technology, Because this is another thing

0:42:35.400 --> 0:42:39.120
<v Speaker 3>that Poppic gets into in her article, like she quotes

0:42:39.160 --> 0:42:42.759
<v Speaker 3>Woodward Fisher talking about how there are still things that

0:42:43.120 --> 0:42:45.640
<v Speaker 3>we don't fully understand about mud and the way that

0:42:46.040 --> 0:42:49.440
<v Speaker 3>riverbanks work and stuff, and this research could help contribute

0:42:49.440 --> 0:42:52.560
<v Speaker 3>to that, for example, by giving us better ideas of

0:42:52.600 --> 0:42:56.560
<v Speaker 3>how to do river engineering projects like dam construction. You know,

0:42:56.640 --> 0:42:58.799
<v Speaker 3>if you have a better idea of the way that

0:42:59.120 --> 0:43:04.360
<v Speaker 3>vegetation controls the flow of rivers and how the banks

0:43:04.360 --> 0:43:07.520
<v Speaker 3>of the rivers change and respond to flood conditions, you

0:43:07.560 --> 0:43:12.600
<v Speaker 3>could better anticipate and prevent, for example, river engineering failures.

0:43:12.960 --> 0:43:15.040
<v Speaker 3>The example given in the article here is like flooding

0:43:15.480 --> 0:43:18.920
<v Speaker 3>along the Mississippi River. But you know, this is of

0:43:19.040 --> 0:43:21.040
<v Speaker 3>concern to societies all around the world.

0:43:21.440 --> 0:43:24.440
<v Speaker 1>All of this reminds me of that great quote from T. S.

0:43:24.440 --> 0:43:28.080
<v Speaker 1>Eliot from four Quartets quote. I do not know much

0:43:28.120 --> 0:43:30.360
<v Speaker 1>about gods, but I think that the river is a

0:43:30.400 --> 0:43:34.919
<v Speaker 1>strong brown god, sullen, untamed and intractable.

0:43:35.440 --> 0:43:38.359
<v Speaker 3>Well, that's beautiful. And to know that that god may

0:43:38.400 --> 0:43:41.160
<v Speaker 3>have been formed out of many other lesser gods over

0:43:41.200 --> 0:43:45.400
<v Speaker 3>time by the accumulation of mud by plants. Oh, this

0:43:45.520 --> 0:43:47.520
<v Speaker 3>is just a random thing I remembered, but I wanted

0:43:47.520 --> 0:43:49.880
<v Speaker 3>to throw it in quickly. Another interesting thing mentioned in

0:43:49.920 --> 0:43:53.960
<v Speaker 3>that popic article is the idea that once forests are

0:43:53.960 --> 0:43:58.000
<v Speaker 3>formed on land, they can also help contribute to the

0:43:58.760 --> 0:44:01.640
<v Speaker 3>accumulation of mud on the continents because they act as

0:44:01.680 --> 0:44:05.279
<v Speaker 3>a sort of filter for dust and sediment that is

0:44:05.320 --> 0:44:08.000
<v Speaker 3>blown by the wind. So the wind, you know, you

0:44:08.000 --> 0:44:11.520
<v Speaker 3>can imagine it picking up fine grain particles of soil, clay,

0:44:11.560 --> 0:44:15.200
<v Speaker 3>and silt, blowing them around when they're dry, and normally

0:44:15.200 --> 0:44:17.040
<v Speaker 3>they just get blown out to sea. But if there

0:44:17.080 --> 0:44:20.040
<v Speaker 3>are forests, they get stopped by the forests, they get

0:44:20.040 --> 0:44:22.600
<v Speaker 3>stuck in the sort of the sieve of the trees

0:44:22.920 --> 0:44:25.080
<v Speaker 3>they fall to the earth, and then they can accumulate

0:44:25.160 --> 0:44:28.840
<v Speaker 3>and become mud on the forest floor, flow down into

0:44:28.920 --> 0:44:31.800
<v Speaker 3>a river over time with the wash of the rains

0:44:31.840 --> 0:44:34.040
<v Speaker 3>and so forth, and then become new muddy banks.

0:44:34.680 --> 0:44:39.080
<v Speaker 1>It's amazing. Yeah, it's so easy to take mud for granted, because,

0:44:39.080 --> 0:44:40.480
<v Speaker 1>like I say, if you're just coming at it from

0:44:40.520 --> 0:44:42.520
<v Speaker 1>the perspective of someone who wants to go on a

0:44:42.560 --> 0:44:44.880
<v Speaker 1>walk in the woods, and then mud is what happens

0:44:44.920 --> 0:44:49.120
<v Speaker 1>when when something has failed or or conditions are not optimal.

0:44:50.320 --> 0:44:54.120
<v Speaker 1>But this, this look at the MUD's roll in the

0:44:54.120 --> 0:44:56.440
<v Speaker 1>emergence of life and the sort of the construction of

0:44:56.480 --> 0:44:59.400
<v Speaker 1>the world as we know it, Yeah, really really casts

0:44:59.400 --> 0:44:59.600
<v Speaker 1>it in.

0:44:59.560 --> 0:45:03.160
<v Speaker 3>A different But we're by no means done with this topic.

0:45:03.200 --> 0:45:04.840
<v Speaker 3>I think we should wrap it up for today. But

0:45:04.880 --> 0:45:08.320
<v Speaker 3>when we come back, we will be talking about mud

0:45:08.320 --> 0:45:12.080
<v Speaker 3>and warfare, Mud in human civilization, Mud on Mars, mud

0:45:12.080 --> 0:45:15.839
<v Speaker 3>and animal behavior and more mud, monsters. There's all kinds

0:45:15.840 --> 0:45:17.000
<v Speaker 3>of stuff. Yeah.

0:45:17.080 --> 0:45:19.440
<v Speaker 1>Yeah, So this is one of those where we definitely

0:45:19.440 --> 0:45:22.200
<v Speaker 1>don't know how many episodes it'll be, so we can't

0:45:22.200 --> 0:45:23.640
<v Speaker 1>give you a heads up that this is going to

0:45:23.680 --> 0:45:26.560
<v Speaker 1>be two episodes, three episodes, We're just going to have

0:45:26.600 --> 0:45:29.239
<v Speaker 1>to listen to the mud and follow the mud and

0:45:29.320 --> 0:45:32.759
<v Speaker 1>let it take us. Like someone's stepping in it on

0:45:32.800 --> 0:45:34.799
<v Speaker 1>a muddy path. We just got to let it see

0:45:35.120 --> 0:45:38.240
<v Speaker 1>where we go, how far we're going to slide into mud?

0:45:38.680 --> 0:45:39.960
<v Speaker 1>All right, Well, on that note, we're going to go

0:45:39.960 --> 0:45:42.040
<v Speaker 1>ahead and close it out, but we'll be back next

0:45:42.080 --> 0:45:45.000
<v Speaker 1>time with more mud. So just remember that. Our core

0:45:45.000 --> 0:45:47.120
<v Speaker 1>episodes of Stuff to Blow Your Mind publishing the Stuff

0:45:47.120 --> 0:45:50.319
<v Speaker 1>to Blow Your Mind podcast feed on Tuesdays and Thursdays.

0:45:50.680 --> 0:45:52.799
<v Speaker 1>Mondays we do listener mail, Wednesdays we do a short

0:45:52.840 --> 0:45:55.120
<v Speaker 1>form artifact or monster Effect, and on Fridays we do

0:45:55.320 --> 0:45:57.399
<v Speaker 1>Weird House Cinema. That's our time to set aside most

0:45:57.440 --> 0:45:59.960
<v Speaker 1>serious concerns and just talk about a weird film.

0:46:00.480 --> 0:46:04.319
<v Speaker 3>Huge thanks to our excellent audio producer JJ Posway. If

0:46:04.360 --> 0:46:05.840
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0:46:05.960 --> 0:46:08.440
<v Speaker 3>feedback on this episode or any other, to suggest a

0:46:08.480 --> 0:46:10.480
<v Speaker 3>topic for the future, or just to say hello, you

0:46:10.560 --> 0:46:13.319
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0:46:13.360 --> 0:46:21.880
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0:46:21.920 --> 0:46:24.880
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0:46:24.960 --> 0:46:28.799
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