WEBVTT - The Future of Earthquakes

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<v Speaker 1>Brought to you by Toyota Let's go places. Welcome to

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<v Speaker 1>Forward Thinking, Hi, and welcome to Forward Thinking, the podcast

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<v Speaker 1>that looks at the future and says, I feel the

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<v Speaker 1>Earth move under my feet. I'm Lauren voc Obama, and

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<v Speaker 1>I'm Joe McCormick, and our regular host Jonathan Strickland is

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<v Speaker 1>not with us today as having a beautiful vacation. Yes,

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<v Speaker 1>hopefully not along the fault line anywhere, which introduces today's topic,

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<v Speaker 1>which is earthquakes. We after we did our super volcano episode,

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<v Speaker 1>we received a couple of messages, one from Jacob via

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<v Speaker 1>Twitter and one from Matt via Facebook, who both wrote

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<v Speaker 1>in to request an episode about another big disaster, earthquakes. Yeah,

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<v Speaker 1>and not just about what earthquakes are and how they work,

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<v Speaker 1>of course, but seeing as this is Forward Thinking, what

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<v Speaker 1>are we going to do about them in the future?

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<v Speaker 1>Will we ever be able to predict earthquakes and understand

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<v Speaker 1>what causes them, when and where they're going to happen,

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<v Speaker 1>and how to stop them and protect against them? Oh? Sure?

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<v Speaker 1>And especially that protect protect against them thing, because even

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<v Speaker 1>if we can't predict them, how can we prepare ourselves

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<v Speaker 1>better for them? Sure? And I'm sure One of the

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<v Speaker 1>reasons people want to know about earthquakes right around now

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<v Speaker 1>is the grand trailer for this movie that's out this

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<v Speaker 1>summer called San Andreas. Yeah. Yeah, that came out on

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<v Speaker 1>May nine. I believe it features the rock right. It's

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<v Speaker 1>not a grand theft auto movie. It is a movie

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<v Speaker 1>about a big earthquake, in the tradition of other movies

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<v Speaker 1>about big disasters where stuff falls over. Yeah, lots of

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<v Speaker 1>stuff falls over, as it turns out. I have not

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<v Speaker 1>seen this movie. I'm probably not going to, but I

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<v Speaker 1>gotta be honest. I saw the trailer when I was

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<v Speaker 1>in the theater watching Mad Max Fury Road, and it

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<v Speaker 1>was hilarious. I I have to say that I laughed

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<v Speaker 1>through that entire trailer, and I'm not I feel I

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<v Speaker 1>felt kind of bad out it at the time because

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<v Speaker 1>although I knew that those digital people were fine, like, like,

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<v Speaker 1>no digital people were harmed in the making of those

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<v Speaker 1>digital effects shots. Earthquakes are very serious matters, of course,

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<v Speaker 1>right there are terrifying and unpredictable attack upon our placid

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<v Speaker 1>urban lives and and a lot of times they seem

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<v Speaker 1>to come out of nowhere and they can kill thousands

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<v Speaker 1>of people, and so of course earthquakes are worth understanding

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<v Speaker 1>to figure out, not just for the pure science of it,

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<v Speaker 1>but to save lives. Oh of course. Yeah. And and

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<v Speaker 1>the thing, of course about the ground that we stand

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<v Speaker 1>on is that it is not solid at all. Well,

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<v Speaker 1>I mean, i'd say it is solid, but it's not.

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<v Speaker 1>It's not what stationary should we yes, and not just

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<v Speaker 1>in the way that that planet Earth is like a spaceship, uh,

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<v Speaker 1>that the ground is always moving. Earth's crust is made

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<v Speaker 1>up of continent sized slabs of rock called tectonic plates,

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<v Speaker 1>which are constantly moving and rubbing up again to each other,

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<v Speaker 1>pushing over under one another, or moving slightly apart. And

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<v Speaker 1>that's fine, that's great, that's I don't know if that's fine. Yeah,

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<v Speaker 1>it's fine. Well, it's normally on a day to day basis,

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<v Speaker 1>it's usually fine. Um. But sometimes those those edges, those

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<v Speaker 1>faults can crack or slip against each other abruptly, causing

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<v Speaker 1>these very powerful vibrations to shake the edges of those

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<v Speaker 1>plates in in patterns radiating outward from the point of

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<v Speaker 1>that slippery origin. Um. And those vibrations a k a.

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<v Speaker 1>Seismic waves are what we feel as earthquakes. Yeah, I

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<v Speaker 1>was trying to think of a good analogy for how

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<v Speaker 1>earthquakes are created in a at a scale that we

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<v Speaker 1>can experiment with. And I think this sort of works.

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<v Speaker 1>If you put on some rubber soled shoes and then

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<v Speaker 1>try to walk along on say like a hardwood floor

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<v Speaker 1>or like a basketball gym floor, without lifting your feet,

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<v Speaker 1>just scooting your shoes along, well, you'll probably notice if

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<v Speaker 1>or shoe scooting experiences anything like mine, is that for

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<v Speaker 1>a certain length of the slide, the shoe will move

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<v Speaker 1>kind of smoothly, but every now and then it will

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<v Speaker 1>sort of get caught for a second. The forward momentum

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<v Speaker 1>will briefly pause, and then you'll experience a sort of

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<v Speaker 1>sudden jolt forward, sometimes accompanied by the classic vibratory sounds

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<v Speaker 1>of scooting, scoot, And these vibrations you can think of

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<v Speaker 1>as being kind of analogous to what's happening when these

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<v Speaker 1>plates are scooting against each other. Sure, and and researchers

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<v Speaker 1>think that it's a it's a build up of potential

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<v Speaker 1>energy over periods of time that are not, to our

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<v Speaker 1>knowledge predictable yet. Um, but we'll address that question later

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<v Speaker 1>in this episode. Yes, yes, but but earthquakes happen constantly.

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<v Speaker 1>Oh yeah, yeah. The U S Geological Survey estimates that

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<v Speaker 1>as many as one point three million earthquakes happen every year.

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<v Speaker 1>And that's just the ones that are over a two

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<v Speaker 1>point oh on the Richter scale, which is the point

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<v Speaker 1>at which human can feel them. Right, And then it's

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<v Speaker 1>not even just the primary effects of the vibration of

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<v Speaker 1>the ground of the earthquake, right, Earthquakes have lots of

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<v Speaker 1>secondary causes that can become disasters on their own. Oh,

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<v Speaker 1>of course, there's a tsunami, and avalanches and landslides and liquification,

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<v Speaker 1>which is a thing where solid ground starts acting like

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<v Speaker 1>a liquid which uh, and and flooding and you know,

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<v Speaker 1>the collapse of human made structures and the lack of

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<v Speaker 1>resources and the aftermath that ensues and all of these

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<v Speaker 1>terrible things. Of course. Yeah, So we have very good

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<v Speaker 1>reason to want to understand how earthquakes work and what

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<v Speaker 1>we can do about them. So so I figured we

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<v Speaker 1>should start by going back a little bit and looking

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<v Speaker 1>at how our understanding of earthquakes developed over time. Yeah, yeah, what,

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<v Speaker 1>I bet people had some interesting ideas about earthquakes and

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<v Speaker 1>ancient times. Well, you'd be right. So the ancient world,

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<v Speaker 1>of course, experienced plenty of earthquakes, just as many earthqua

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<v Speaker 1>wakes as we do today, and without the scientific framework

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<v Speaker 1>to explain them, they came up with some pretty weird

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<v Speaker 1>and sometimes funny explanations. So religious spiritual magical explanations were

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<v Speaker 1>extremely common all over the world West and the East.

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<v Speaker 1>People sort of explained earthquakes as often as divine punishments

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<v Speaker 1>or divine im portents. Gods were either like giving a

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<v Speaker 1>warning or were angry and issuing punishment. I found this

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<v Speaker 1>one funny example of both the magical explanations given by

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<v Speaker 1>the ancients and some of the practical explanations. And these

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<v Speaker 1>are chronicled in the writings of the Roman historian Ombianus Marcellinus,

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<v Speaker 1>who is a soldier by trade, and he lived during

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<v Speaker 1>the fourth century CE, and he wrote a surviving history

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<v Speaker 1>at the time, and and he he has a little

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<v Speaker 1>discourse on earthquakes, and what he says is that when

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<v Speaker 1>you're talking about earthquakes, quote, in all priests the ceremonies,

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<v Speaker 1>whether ritual or pontifical, care is taken not at such

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<v Speaker 1>times to name one god more than another, for fear

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<v Speaker 1>of impiety, since it is quite uncertain which God causes

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<v Speaker 1>these visitations. I love it. They didn't want to they

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<v Speaker 1>didn't want to assign blame without all the facts. Well

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<v Speaker 1>that's that's good. I mean, you know, that's covering your bass.

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<v Speaker 1>I approve of the hypothesis format of finding knowledge. Sure,

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<v Speaker 1>and then of course you had sort of spiritual or

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<v Speaker 1>supernatural explanations in in the East as well. So like

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<v Speaker 1>some ancient Chinese explanations seem to have read earthquakes again

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<v Speaker 1>as divine punishments importance. But to continue with what our

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<v Speaker 1>historian Marcellinus had to say, this was great because he

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<v Speaker 1>also chronicled what some of the dominant practical explanations of

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<v Speaker 1>the day were. So it wasn't that everybody just had

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<v Speaker 1>this religious explanation. There were also the ancient natural philosophers

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<v Speaker 1>who were like, no, let's figure this out. Truly, something's

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<v Speaker 1>going on under the earth. I mean, Aristotle surely had

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<v Speaker 1>something to say about it. Oh yes, So quoting again

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<v Speaker 1>from Marcellinus, and all of these quotes from Marcellinus are

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<v Speaker 1>from the seedy Youngae translation in English. But as the

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<v Speaker 1>various opinions among which Aristotle waivers and hesitates suggest earthquakes

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<v Speaker 1>are engendered either in small caverns under the earth because

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<v Speaker 1>of the waters pouring through them with a more rapid

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<v Speaker 1>motion than usual, or, as Anaxagoras affirms, they arise from

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<v Speaker 1>the force of wind penetrating the lower parts of the Earth,

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<v Speaker 1>which when they have got down to the encrusted solid mass,

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<v Speaker 1>finding no vent holes shake those portions in their solid

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<v Speaker 1>state into which they have got entrance when in a

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<v Speaker 1>state of solution. And this is corroborated by the observation

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<v Speaker 1>that at such times no breezes of wind are felt

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<v Speaker 1>by us above the ground, because the winds are occupied

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<v Speaker 1>in the lowest recesses of the earth. Oh that's delightful.

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<v Speaker 1>That is that is so delightfully incorrect. I adore that. Yeah. So,

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<v Speaker 1>I think the idea that was being propagated at the

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<v Speaker 1>time by Aristotle and some of the other well not

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<v Speaker 1>at the time by Aristotle, but had previously been propagated

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<v Speaker 1>by Aristotle and then continued to be believed by many

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<v Speaker 1>people was something having to do with the exchange of

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<v Speaker 1>gases like wind and evaporation under the earth. And sometimes

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<v Speaker 1>when like gases or evaporating uh vapors would get trapped

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<v Speaker 1>under the earth, sometimes they'd be released in a big burst. Sure. Sure,

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<v Speaker 1>Although I suppose it is interesting that they were thinking

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<v Speaker 1>about liquids and the motion that propagates in liquids because

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<v Speaker 1>earthquakes are in fact caused by by waves of energy,

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<v Speaker 1>which at their time was analogous. So analogous, which yes,

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<v Speaker 1>that thing. Yeah, but but I'm sure they probably weren't

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<v Speaker 1>quite thinking yet of the idea of propagation of waves

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<v Speaker 1>through rock, which must have seemed imposs of all So,

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<v Speaker 1>as with many subject areas see cosmology and physics and

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<v Speaker 1>plenty of things, Aristotle's ideas held sway for a long

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<v Speaker 1>long time in Europe and in the Islamic world, despite

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<v Speaker 1>the fact that they were super super wrong. Um Like,

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<v Speaker 1>don't get me wrong about Aristotle. I'm not saying he

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<v Speaker 1>was stupid. He was obviously a super smart guy of

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<v Speaker 1>the ancient world. I guess just everybody must have assumed

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<v Speaker 1>he was right about everything. That's what they did. It's

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<v Speaker 1>kind of funny if if you've never done this, like

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<v Speaker 1>look up what Galileo overthrew about Aristotelian physics, and it'll

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<v Speaker 1>just kind of make you wonder, like, how did people

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<v Speaker 1>miss this for so long? It seemed so easy to

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<v Speaker 1>figure out. But anyway, Aristotle's ideas about earthquakes hell were

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<v Speaker 1>very popular until the early modern period in Europe, and

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<v Speaker 1>then some other physical explanations for earthquakes began to take

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<v Speaker 1>hold in some circles, like explanations involving fire and explosive properties.

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<v Speaker 1>Just one example like what if iron is reacting with

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<v Speaker 1>sulfur deep under the ground and this explosive chemical reaction

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<v Speaker 1>is causing earthquakes? Even kind of makes sense because you

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<v Speaker 1>can see like, okay, earthquakes sometimes or happening around fault lines,

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<v Speaker 1>which they didn't know about then, but but around volcanoes

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<v Speaker 1>they certainly knew about, yeah, bingo, and that volcanoes have

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<v Speaker 1>this explosive fiery element. Eventually, however, we started to get

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<v Speaker 1>some more correct ideas about seismology, and according to a

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<v Speaker 1>brief history of seismology given by a Duncan car Agony,

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<v Speaker 1>which was my source on most of this historical stuff,

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<v Speaker 1>one of the main events that seemed to trigger the

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<v Speaker 1>modern era of earthquake research was the Lisbon earthquake of

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<v Speaker 1>seventeen fifty five, which was huge and had crazy effects

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<v Speaker 1>throughout are up, including causing uh Sasia's or Seisha's. I

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<v Speaker 1>believe it's satias, which are standing waves in these enclosed

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<v Speaker 1>bodies of water. So if you've ever seen standing waves

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<v Speaker 1>in water, it's where instead of the waves propagating along

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<v Speaker 1>the surface, they sort of bob back and forth. Looks

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<v Speaker 1>really crazy, especially if you were going to see that

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<v Speaker 1>in like the lake Oh yeah, yeah, or I don't know,

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<v Speaker 1>I'm picturing the scene in Jurassic Park where where the

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<v Speaker 1>the cup of water is just going but but but

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<v Speaker 1>but not like that, just continually bounce back and forth. Yeah,

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<v Speaker 1>I do not want creepy so this so anyway, this

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<v Speaker 1>event caused some writers at the time to sort of

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<v Speaker 1>see the effects of an earthquake as pressure waves propagating

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<v Speaker 1>outward from a source through the elasticity of the rock

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<v Speaker 1>in the Earth's crust, kind of like sound emanates through

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<v Speaker 1>a solid medium. And from this time through the people

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<v Speaker 1>began to study earthquakes more scientifically. But you can kind

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<v Speaker 1>of understand the faculty they would have, because think about it,

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<v Speaker 1>how do you study earthquakes. You can't like cause an earthquake,

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<v Speaker 1>especially not with the technology of the time, and you

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<v Speaker 1>can't predict when they're going to happen to set up

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<v Speaker 1>your equipment, So it was very much an exercise in

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<v Speaker 1>sort of gathering what data you could after the event

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<v Speaker 1>and then trying to sort of do backwards experiments by

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<v Speaker 1>analyzing the data you had available to you, which is

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<v Speaker 1>very difficult to do, oh sure, especially right given the

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<v Speaker 1>technology of the time and the lack of electricity, let

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<v Speaker 1>alone computers and all of that stuff. Although the first

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<v Speaker 1>step I would say was around the mid eighteen hundreds

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<v Speaker 1>when one Robert Mallett actually coined the term seismology. Yeah,

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<v Speaker 1>and he also sort of brought a quantitative approach to

0:13:48.320 --> 0:13:51.040
<v Speaker 1>studying wave propagation through the earth. He was big into

0:13:51.080 --> 0:13:54.320
<v Speaker 1>looking at maps and collecting all kinds of data and

0:13:54.400 --> 0:13:58.640
<v Speaker 1>analyzing it quantitatively. But then, of course, one of the

0:13:58.679 --> 0:14:02.600
<v Speaker 1>big things that's led to modern era of studying wave

0:14:02.679 --> 0:14:06.560
<v Speaker 1>propagation through the Earth has been the development of seismometers

0:14:06.720 --> 0:14:11.640
<v Speaker 1>or seismometers as one might say for some reason. Uh yeah,

0:14:11.880 --> 0:14:17.080
<v Speaker 1>those being machines that detect seismic waves as seism graphs,

0:14:17.200 --> 0:14:20.040
<v Speaker 1>which I think is the more frequently used term in

0:14:20.040 --> 0:14:24.040
<v Speaker 1>in in popular culture at any rate, are our seismometers

0:14:24.080 --> 0:14:27.480
<v Speaker 1>that record those waves, and many seismometers are in fact

0:14:27.480 --> 0:14:30.840
<v Speaker 1>seismic graphs. Yeah, it would obviously not be very helpful

0:14:30.880 --> 0:14:37.160
<v Speaker 1>to detect waves and then forget about them. Uh no um.

0:14:37.280 --> 0:14:41.000
<v Speaker 1>And and actually there's historical records of these from from

0:14:41.440 --> 0:14:44.040
<v Speaker 1>way before the eighteen hundreds. Yeah. I think we don't

0:14:44.240 --> 0:14:48.560
<v Speaker 1>fully understand exactly everything about this ancient one. But the

0:14:48.600 --> 0:14:52.640
<v Speaker 1>idea is that the first mechanical seismometer was created in

0:14:52.840 --> 0:14:56.640
<v Speaker 1>ancient China by the Han Chinese inventor in general all

0:14:56.680 --> 0:15:01.680
<v Speaker 1>purpose genius Chang Hang in the one thirty two CE.

0:15:01.840 --> 0:15:05.280
<v Speaker 1>Oh goodness. And supposedly this device could tell the operator

0:15:05.360 --> 0:15:10.200
<v Speaker 1>from which direction the vibrations of an earthquake originated, and

0:15:10.280 --> 0:15:15.120
<v Speaker 1>even on at least one occasion anecdotally it recorded an

0:15:15.160 --> 0:15:17.800
<v Speaker 1>earthquake that humans could not feel, so it was like

0:15:17.840 --> 0:15:21.120
<v Speaker 1>too faint for humans to know been one. But the

0:15:21.160 --> 0:15:25.280
<v Speaker 1>machine said, hey, there's an earthquake over here. Cool uh

0:15:25.640 --> 0:15:29.360
<v Speaker 1>during that wave of interest wave huh um. In the

0:15:29.440 --> 0:15:34.200
<v Speaker 1>in the eighteen hundreds, um, several mechanical models were produced

0:15:34.240 --> 0:15:38.080
<v Speaker 1>and kind of refined. Um. By nineteen o three we

0:15:38.160 --> 0:15:43.360
<v Speaker 1>saw the first electromagnetic seismometer, and then digital equipment and

0:15:43.360 --> 0:15:46.800
<v Speaker 1>and data processing technology started to be developed around the

0:15:46.880 --> 0:15:50.480
<v Speaker 1>nineteen seventies or so, we could probably do an entire

0:15:50.640 --> 0:15:54.920
<v Speaker 1>like series of episodes about seismometer technology. And maybe that's

0:15:54.920 --> 0:15:56.960
<v Speaker 1>the thing. I'll poke Jonathan and see if he wants

0:15:57.000 --> 0:15:59.240
<v Speaker 1>to do some episodes about about that on tech stuff,

0:16:00.080 --> 0:16:02.960
<v Speaker 1>because there's so much out there and it's it's kind

0:16:03.040 --> 0:16:05.200
<v Speaker 1>of fascinating. Maybe it would be better in video because

0:16:05.240 --> 0:16:07.760
<v Speaker 1>it's a whole lot of like pictures of pendulums working

0:16:07.760 --> 0:16:10.280
<v Speaker 1>in different ways and spring loaded things. Dude, all of

0:16:10.280 --> 0:16:12.880
<v Speaker 1>a sudden, to Jonathan talk about some pendulums do a

0:16:12.880 --> 0:16:15.720
<v Speaker 1>good job, I bet he would. Okay, No, wait, how

0:16:15.720 --> 0:16:20.480
<v Speaker 1>about some related technology? What about technology to measure those

0:16:20.520 --> 0:16:24.320
<v Speaker 1>secondary effects of earthquakes that we're talking about earlier. Yeah,

0:16:24.360 --> 0:16:27.640
<v Speaker 1>there's some I think within the past few decades. UM

0:16:27.680 --> 0:16:32.520
<v Speaker 1>a device called a sonometer. I think I'm saying that correctly.

0:16:33.400 --> 0:16:41.280
<v Speaker 1>Tenometer either way, Uh yes, tsonometer is probably probably the

0:16:41.280 --> 0:16:44.440
<v Speaker 1>correct way of saying that. UM. A sosonometer is a

0:16:44.560 --> 0:16:48.280
<v Speaker 1>thing that detects changes in water pressure way deep within

0:16:48.320 --> 0:16:51.800
<v Speaker 1>the ocean and can transmit that info via satellite to

0:16:51.960 --> 0:16:56.800
<v Speaker 1>warning centers. It's it's a weighted anchor containing sensors attached

0:16:56.920 --> 0:16:59.560
<v Speaker 1>via tether to a boy on the surface that has

0:16:59.640 --> 0:17:03.080
<v Speaker 1>you know, data crunching computer and transmission system, and it

0:17:03.160 --> 0:17:06.119
<v Speaker 1>can give you a few hours of warning, um for

0:17:06.400 --> 0:17:12.200
<v Speaker 1>tsunami activity. Yeah, so super valuable of course, because I mean,

0:17:12.240 --> 0:17:15.720
<v Speaker 1>tsunamis can be especially devastating when you've got that wall

0:17:15.760 --> 0:17:17.840
<v Speaker 1>of water. I don't know if you've ever seen video

0:17:17.880 --> 0:17:20.800
<v Speaker 1>of what that looks like. It's absolutely terrifying. Oh yeah,

0:17:20.920 --> 0:17:27.040
<v Speaker 1>it's completely mind blowing. Um. Also mind blowing, I find um.

0:17:27.119 --> 0:17:31.920
<v Speaker 1>It was basically readings from these early seismometers that led

0:17:31.920 --> 0:17:35.840
<v Speaker 1>scientists to build the modern hypotheses of the makeup of

0:17:35.880 --> 0:17:38.719
<v Speaker 1>the Earth, starting around like nineteen o nine and then

0:17:38.800 --> 0:17:42.159
<v Speaker 1>ranging up through the thirties. That is when we figured

0:17:42.200 --> 0:17:45.000
<v Speaker 1>out that the Earth has a solid core and molten

0:17:45.119 --> 0:17:48.800
<v Speaker 1>stuff and a crust. And that is so recent it's

0:17:48.840 --> 0:17:50.359
<v Speaker 1>it's crazy to me, Like I had, for some reason

0:17:50.400 --> 0:17:52.800
<v Speaker 1>assumed that had happened in like the sixt dreds at

0:17:52.800 --> 0:17:59.480
<v Speaker 1>some point, but nope, yeah, crazy, So go seismology. Good job.

0:18:00.040 --> 0:18:03.040
<v Speaker 1>That's just astonishing like that we had like relativity and

0:18:03.160 --> 0:18:08.000
<v Speaker 1>quantum physics before we had a full understanding of the

0:18:08.000 --> 0:18:10.640
<v Speaker 1>the Earth, right Yeah, And you know, to be fair,

0:18:10.720 --> 0:18:13.639
<v Speaker 1>you can't go that deep into the earth. Um, you

0:18:13.720 --> 0:18:19.760
<v Speaker 1>also can't go the speed a light, Lauren. Maybe you can't, Joe, Okay,

0:18:20.520 --> 0:18:23.560
<v Speaker 1>but uh so. So it's really cool, of course that

0:18:23.600 --> 0:18:26.119
<v Speaker 1>we were learning all of this stuff and and learning

0:18:26.119 --> 0:18:31.159
<v Speaker 1>how to take measurements of earthquakes. But how has all

0:18:31.200 --> 0:18:34.719
<v Speaker 1>of this learning been applied in actually saving lives and

0:18:34.760 --> 0:18:38.400
<v Speaker 1>preventing damage and predicting earthquakes. Well, I think one thing

0:18:38.480 --> 0:18:40.960
<v Speaker 1>we should actually look at first before we talk about

0:18:41.000 --> 0:18:45.520
<v Speaker 1>predicting earthquakes, because that's, as you will learn, quite a

0:18:45.600 --> 0:18:48.600
<v Speaker 1>strange and iffi proposition. But we can at least talk

0:18:48.640 --> 0:18:51.119
<v Speaker 1>about what we can do to our buildings and our

0:18:51.160 --> 0:18:56.199
<v Speaker 1>cities to make them safer in the event of an earthquake. Yeah. Yeah, Um,

0:18:56.240 --> 0:19:01.119
<v Speaker 1>there are a bunch of different concepts of material and

0:19:01.160 --> 0:19:06.600
<v Speaker 1>construction engineering that can help us safeguard our stuff against

0:19:06.680 --> 0:19:09.760
<v Speaker 1>getting super destroyed. Yeah. I remember. I actually saw a

0:19:09.840 --> 0:19:12.240
<v Speaker 1>headline a while back that was it was a piece

0:19:12.280 --> 0:19:14.840
<v Speaker 1>I think in the wake of a recent earthquake that

0:19:14.920 --> 0:19:18.520
<v Speaker 1>said something along the lines of earthquakes don't kill people,

0:19:19.000 --> 0:19:22.720
<v Speaker 1>buildings do. Right. That seems quite true to me. I

0:19:22.720 --> 0:19:25.040
<v Speaker 1>mean that if you're standing in the middle of a

0:19:25.119 --> 0:19:28.119
<v Speaker 1>field and an earthquake, you're gonna get knocked on your butt.

0:19:28.240 --> 0:19:29.920
<v Speaker 1>But you know, I mean, I mean maybe if a

0:19:30.000 --> 0:19:32.600
<v Speaker 1>fault in the earth opens up directly under your feet,

0:19:33.119 --> 0:19:37.160
<v Speaker 1>that would suck. But but basically it just trips you. Sure,

0:19:37.280 --> 0:19:39.679
<v Speaker 1>but when you come into real danger is when you

0:19:39.720 --> 0:19:43.800
<v Speaker 1>are near a structurally unsound building that come toppling over

0:19:43.840 --> 0:19:47.320
<v Speaker 1>and crush you. Yeah, that that is that is much

0:19:47.359 --> 0:19:50.280
<v Speaker 1>worse than falling on your butt on on a galactic scale.

0:19:51.080 --> 0:19:53.880
<v Speaker 1>So what are some of the answers that material science

0:19:53.920 --> 0:19:58.360
<v Speaker 1>and construction engineering have given us. One of the classic

0:19:58.440 --> 0:20:02.919
<v Speaker 1>ones is called base i selation, And this is super

0:20:02.960 --> 0:20:06.760
<v Speaker 1>not a new idea. Um. There's evidence that Iranian architects,

0:20:06.880 --> 0:20:10.920
<v Speaker 1>or pre Iranian architects rather and engineers were purposefully constructing

0:20:10.960 --> 0:20:15.640
<v Speaker 1>buildings with seismic base isolation starting around like five fifty BC,

0:20:16.600 --> 0:20:20.360
<v Speaker 1>So two five years ago folks were working on this. Well,

0:20:20.400 --> 0:20:22.080
<v Speaker 1>I don't know if I should be impressed, because I

0:20:22.119 --> 0:20:27.040
<v Speaker 1>don't know what it is, Okay. Base isolation is constructing

0:20:27.040 --> 0:20:30.560
<v Speaker 1>two separate layers of a foundation for your building, that

0:20:30.640 --> 0:20:33.600
<v Speaker 1>the layer against the ground is solid with the ground,

0:20:34.040 --> 0:20:38.399
<v Speaker 1>and the the secondary layer between the first one and

0:20:38.440 --> 0:20:41.119
<v Speaker 1>your building is solid with the building, but it is

0:20:41.160 --> 0:20:46.200
<v Speaker 1>capable of sliding against the lower foundation. Okay, Um, so

0:20:46.320 --> 0:20:49.800
<v Speaker 1>if the ground shakes, the upper foundation and the building

0:20:50.000 --> 0:20:55.560
<v Speaker 1>remain intact. Yeah yeah, um or I mean like up

0:20:55.600 --> 0:20:57.240
<v Speaker 1>to a certain point. I think that over like a

0:20:57.840 --> 0:20:59.720
<v Speaker 1>eight on the Richter scale, and you're just kind of

0:21:00.000 --> 0:21:03.359
<v Speaker 1>it anyway. But um, but but this is really cool.

0:21:03.840 --> 0:21:06.960
<v Speaker 1>Archaeologists have found structures such as the Tomb of Cyrus

0:21:07.000 --> 0:21:10.360
<v Speaker 1>that have been standing for over two thousand years, partially

0:21:10.600 --> 0:21:14.000
<v Speaker 1>thanks to this type of structural safeguard. Safeguard, Well, how

0:21:14.000 --> 0:21:15.800
<v Speaker 1>did they do it back then? I mean if they

0:21:15.800 --> 0:21:18.640
<v Speaker 1>didn't have like ball bearings and or whatever, I don't

0:21:18.680 --> 0:21:22.080
<v Speaker 1>know what people would actually use today. Giant loose slabs

0:21:22.080 --> 0:21:24.880
<v Speaker 1>of rock is how they did it, basically, Um, like

0:21:24.880 --> 0:21:26.919
<v Speaker 1>like one giant slab of rock for the base and

0:21:26.960 --> 0:21:30.520
<v Speaker 1>a and a secondary unattached slab of rock for the

0:21:30.640 --> 0:21:34.720
<v Speaker 1>secondary base. I can just imagine the ancient Persian conversation

0:21:34.840 --> 0:21:37.639
<v Speaker 1>that like create you know, like you can't have just

0:21:37.760 --> 0:21:41.280
<v Speaker 1>one slab Nope, nope, we need two slabs here because

0:21:41.280 --> 0:21:43.840
<v Speaker 1>then your earthquake comes and what are you going to do?

0:21:43.920 --> 0:21:50.240
<v Speaker 1>You have an exposed Cyrus corpse that would just be rude.

0:21:50.480 --> 0:21:54.320
<v Speaker 1>We don't we can't have that, um modern okay, oh sorry,

0:21:54.359 --> 0:21:56.679
<v Speaker 1>I just want to update. I am impressed. Now that's smart.

0:21:58.160 --> 0:21:59.679
<v Speaker 1>Yeah yeah, well, I mean it shows that they were

0:21:59.680 --> 0:22:02.159
<v Speaker 1>thinking about it, and even thinking about it at that

0:22:02.200 --> 0:22:06.080
<v Speaker 1>point in time was probably pretty impressive. Modern Ly, a

0:22:06.080 --> 0:22:08.760
<v Speaker 1>lot of buildings that are in danger zones will use

0:22:08.880 --> 0:22:14.159
<v Speaker 1>these things called lead rubber bearing pads between the solid

0:22:14.200 --> 0:22:17.560
<v Speaker 1>foundation and the building. And and these pads consist of

0:22:17.600 --> 0:22:21.520
<v Speaker 1>a solid lead core that's wrapped in in alternating layers

0:22:21.640 --> 0:22:28.560
<v Speaker 1>of rubber and steel bands. So vertically speaking, it's super solid. UM.

0:22:28.600 --> 0:22:31.760
<v Speaker 1>Horizontally it's wibbly wabbli right, so it's not going to

0:22:31.880 --> 0:22:35.840
<v Speaker 1>get crushed, but it can shimmy. Yeah there yeah. UM.

0:22:36.119 --> 0:22:39.639
<v Speaker 1>And a newish technology out of a Japanese company called

0:22:39.720 --> 0:22:45.840
<v Speaker 1>Air Dunsion Systems Incorporated UM can temporarily suspend a smallish

0:22:45.880 --> 0:22:48.680
<v Speaker 1>structure like a private home, on a cushion of air

0:22:49.200 --> 0:22:53.280
<v Speaker 1>as a secondary foundation. UM. They work by having these

0:22:53.320 --> 0:22:57.480
<v Speaker 1>seismic sensors in the homes primary foundation detect a coming

0:22:57.560 --> 0:23:01.320
<v Speaker 1>quake and UM when that happened, and a really powerful

0:23:01.600 --> 0:23:03.919
<v Speaker 1>air compressor will activate and feel like a like an

0:23:03.920 --> 0:23:09.040
<v Speaker 1>air bag in the secondary foundation in less than a second. Um.

0:23:09.080 --> 0:23:11.600
<v Speaker 1>And then you know, when when the sensors detect the

0:23:11.600 --> 0:23:14.200
<v Speaker 1>earthquake is over, the compressor switches off and the bag deflates,

0:23:14.280 --> 0:23:18.280
<v Speaker 1>kind of bringing the home back down, um gently onto

0:23:18.320 --> 0:23:21.879
<v Speaker 1>its first foundation. It's only lifting the structure like a

0:23:21.880 --> 0:23:24.960
<v Speaker 1>little over an inch in the air. Maybe so, but

0:23:25.080 --> 0:23:26.359
<v Speaker 1>that can make a difference. But that can make a

0:23:26.400 --> 0:23:29.760
<v Speaker 1>huge difference. Yeah, yeah, so uh kind of inexpensive way

0:23:29.800 --> 0:23:34.479
<v Speaker 1>I suppose of conducting a base isolation on, especially a

0:23:34.520 --> 0:23:37.600
<v Speaker 1>small home. As I read that the company was hoping

0:23:37.640 --> 0:23:40.359
<v Speaker 1>to expand their systems for use in high rises, but

0:23:40.640 --> 0:23:43.320
<v Speaker 1>I haven't been able to find anything more recent about

0:23:43.320 --> 0:23:45.720
<v Speaker 1>what they've been doing, so I don't know. I hope

0:23:45.720 --> 0:23:48.280
<v Speaker 1>they're out there. Yeah, good luck to them. Yeah. Well,

0:23:48.320 --> 0:23:50.640
<v Speaker 1>one of the things that I think is interesting is

0:23:50.920 --> 0:23:56.600
<v Speaker 1>studying the way that the ground actually transfers energy to buildings.

0:23:56.960 --> 0:24:00.400
<v Speaker 1>Oh yeah, because that's really your problem, right, that you've

0:24:00.400 --> 0:24:03.159
<v Speaker 1>got all this energy coming into a rigid structure, and

0:24:03.200 --> 0:24:06.399
<v Speaker 1>how do you dissipate it? Right? But I mean, really,

0:24:06.440 --> 0:24:11.679
<v Speaker 1>the damage that earthquakes cause is because of how efficient

0:24:12.000 --> 0:24:17.359
<v Speaker 1>energy transfer is. Like thanks a lot physics, um, but

0:24:17.359 --> 0:24:21.600
<v Speaker 1>but see any given object has a resonant frequency or

0:24:21.640 --> 0:24:23.760
<v Speaker 1>a group of resonant frequencies. And we've talked about that

0:24:23.760 --> 0:24:26.040
<v Speaker 1>a little bit on the show before. Um it means

0:24:26.080 --> 0:24:29.520
<v Speaker 1>that when when the object vibrates, based on its its

0:24:29.560 --> 0:24:31.960
<v Speaker 1>size and its shape and the materials it's made of,

0:24:32.359 --> 0:24:36.280
<v Speaker 1>it's going to resonate at this specific frequency or group

0:24:36.280 --> 0:24:39.440
<v Speaker 1>of frequencies maybe, And it's really hard to get something

0:24:39.480 --> 0:24:44.160
<v Speaker 1>to resonate at a non resonant frequency. Um So, if

0:24:44.200 --> 0:24:46.960
<v Speaker 1>you if you put mechanical energy into an object the

0:24:47.000 --> 0:24:50.120
<v Speaker 1>way that a seismic wave does, uh, it will vibrate

0:24:50.520 --> 0:24:53.639
<v Speaker 1>just as much as it can, like a whole bunch

0:24:54.160 --> 0:24:58.240
<v Speaker 1>at its resonant frequency, because energy is so efficient like that.

0:24:58.720 --> 0:25:02.320
<v Speaker 1>Um But ut, what if you could get a structure

0:25:02.359 --> 0:25:05.879
<v Speaker 1>to vibrate at a different frequency, at a lower frequency.

0:25:07.040 --> 0:25:09.320
<v Speaker 1>But it's really hard to get an object to do that.

0:25:09.440 --> 0:25:12.680
<v Speaker 1>It just wants to resonate at that one frequency, unless,

0:25:12.720 --> 0:25:15.800
<v Speaker 1>of course, you physically change the object on the fly,

0:25:16.359 --> 0:25:18.640
<v Speaker 1>which is also not really a thing that you want

0:25:18.680 --> 0:25:21.200
<v Speaker 1>to do to a building, or that it's physically possible

0:25:21.480 --> 0:25:23.320
<v Speaker 1>to do to a building. I mean, unless you're like

0:25:23.440 --> 0:25:27.800
<v Speaker 1>magneto or something like that. Um So, how can magneto

0:25:27.880 --> 0:25:30.160
<v Speaker 1>do that. You'd have to be something else right now.

0:25:30.200 --> 0:25:32.040
<v Speaker 1>He could change the shape of a building by way

0:25:32.880 --> 0:25:35.280
<v Speaker 1>by by moving around the steel structures or you know,

0:25:35.359 --> 0:25:36.800
<v Speaker 1>or he could take some of the metal out of

0:25:36.800 --> 0:25:44.639
<v Speaker 1>it put extra metal into it. I'm usually right about magneto, UM,

0:25:45.359 --> 0:25:48.400
<v Speaker 1>but engineers who are not magneto have come up with

0:25:48.920 --> 0:25:53.720
<v Speaker 1>various damper systems. One that's really great for skyscrapers is

0:25:53.840 --> 0:25:57.399
<v Speaker 1>called a tuned mass damper. And in the system you

0:25:57.680 --> 0:26:01.160
<v Speaker 1>suspend like a big old massive ing near the top

0:26:01.240 --> 0:26:03.720
<v Speaker 1>of a skyscraper. UM. It can be held in place

0:26:03.720 --> 0:26:07.240
<v Speaker 1>with like fluid cushions or hydraulics or springs or cables

0:26:07.359 --> 0:26:11.320
<v Speaker 1>or some wacky combination of the above, and UM that

0:26:11.440 --> 0:26:15.280
<v Speaker 1>the mass and the hang of the system is tuned

0:26:15.520 --> 0:26:19.119
<v Speaker 1>precisely to the resident frequency of the building, so that

0:26:19.160 --> 0:26:22.560
<v Speaker 1>when an earthquake hits uh at, the building rocks one

0:26:22.560 --> 0:26:26.440
<v Speaker 1>way and the system rocks in the opposite direction, which

0:26:26.520 --> 0:26:29.640
<v Speaker 1>which helps reduce or kind of balance out the forces

0:26:29.640 --> 0:26:33.439
<v Speaker 1>that are acting on the building, UM, thus preventing damage. Okay,

0:26:33.480 --> 0:26:35.400
<v Speaker 1>I can see. So it's like it's almost like trying

0:26:35.440 --> 0:26:40.160
<v Speaker 1>to create a canceling wave for holding Yeah, exactly. Um. Yeah, yeah,

0:26:40.240 --> 0:26:45.439
<v Speaker 1>it's sort of like noise canceling headphones of earthquakes. Yes, yeah,

0:26:45.480 --> 0:26:47.040
<v Speaker 1>and you can think about it if it if it

0:26:47.080 --> 0:26:51.920
<v Speaker 1>helps with the visualization, it's sort of like a pendulum awesome. Um.

0:26:51.960 --> 0:26:56.440
<v Speaker 1>Another thing that engineers due to help to help prevent

0:26:56.480 --> 0:27:01.240
<v Speaker 1>damage to buildings is by bracing. And it sounds pretty obvious,

0:27:01.359 --> 0:27:03.040
<v Speaker 1>but but but the way that they look at it

0:27:03.119 --> 0:27:06.360
<v Speaker 1>is since most of the ground's movement during an earthquake

0:27:06.480 --> 0:27:11.359
<v Speaker 1>is lateral, engineers can can compensate with incisive elements of

0:27:11.440 --> 0:27:14.639
<v Speaker 1>strength and flexibility throughout a building that are designed to

0:27:14.680 --> 0:27:18.639
<v Speaker 1>kind of spread the forces out evenly across the vertical

0:27:18.720 --> 0:27:22.040
<v Speaker 1>and the horizontal elements of the structure. Um. And and

0:27:22.080 --> 0:27:25.879
<v Speaker 1>things that help with that include like having parallel and

0:27:26.000 --> 0:27:32.080
<v Speaker 1>symmetrical designs, using diagonal trusses against walls, and using a

0:27:32.640 --> 0:27:37.800
<v Speaker 1>moment resisting frames which are uh columns and beams that

0:27:37.840 --> 0:27:41.800
<v Speaker 1>are bendy but have connectors that are rigid, so that

0:27:42.040 --> 0:27:45.800
<v Speaker 1>during an earthquake, UM, the the whole the whole thing,

0:27:45.920 --> 0:27:48.959
<v Speaker 1>the whole frame moves is a single piece. Those elastic

0:27:49.000 --> 0:27:51.960
<v Speaker 1>elements absorbs some of the energy and they can dissipate

0:27:52.040 --> 0:27:55.479
<v Speaker 1>it without causing the building to crack or something right, right,

0:27:55.680 --> 0:27:59.320
<v Speaker 1>it spreads the shock out across the entire structure, reducing

0:27:59.400 --> 0:28:03.200
<v Speaker 1>damage to you one part or Another interesting way to

0:28:03.240 --> 0:28:07.480
<v Speaker 1>approach bracing that I read about was specifically directing the

0:28:07.640 --> 0:28:11.200
<v Speaker 1>energy dissipation or sort of like the damage centric zone

0:28:11.280 --> 0:28:15.520
<v Speaker 1>to a replaceable part of the bracing structure, like like

0:28:15.640 --> 0:28:19.320
<v Speaker 1>a fuse. Yeah, that'd be something like the fuses you

0:28:19.400 --> 0:28:21.160
<v Speaker 1>might have in your house. Well, hopefully you have circuit

0:28:21.200 --> 0:28:24.600
<v Speaker 1>breakers now, but the house that had fuses would have

0:28:24.680 --> 0:28:27.240
<v Speaker 1>You know, if a circuit gets overheated, well it can

0:28:27.280 --> 0:28:28.960
<v Speaker 1>just melt the fuse and that's fine. You can just

0:28:29.040 --> 0:28:31.360
<v Speaker 1>change that out. You've got a box full of them

0:28:31.400 --> 0:28:34.240
<v Speaker 1>and it's no big deal. But in two thousand nine,

0:28:34.280 --> 0:28:37.240
<v Speaker 1>a team led by researchers at Stanford University in the

0:28:37.320 --> 0:28:41.920
<v Speaker 1>University of Illinois successfully tested a building protection design that

0:28:41.960 --> 0:28:45.240
<v Speaker 1>would keep multi story buildings from falling apart, and it

0:28:45.240 --> 0:28:49.160
<v Speaker 1>would help return them to basically standing straight up upon

0:28:49.200 --> 0:28:51.960
<v Speaker 1>the foundation after the shaking is over, so that the

0:28:52.000 --> 0:28:54.920
<v Speaker 1>building doesn't like remain a hazard and then maybe fall

0:28:55.000 --> 0:28:59.200
<v Speaker 1>over afterwards. And they tested this design on a shake table,

0:28:59.320 --> 0:29:01.680
<v Speaker 1>which is sort of what it sounds like, it's this

0:29:02.320 --> 0:29:05.320
<v Speaker 1>huge thing to simulate earthquakes, and it was shown that

0:29:05.360 --> 0:29:08.280
<v Speaker 1>it was capable of withstanding earthquakes with a magnitude up

0:29:08.320 --> 0:29:12.600
<v Speaker 1>to seven, which is pretty serious earthquake. But basically, these

0:29:12.640 --> 0:29:16.040
<v Speaker 1>are steel frames that are designed to reinforce a building

0:29:16.160 --> 0:29:19.400
<v Speaker 1>at the core or along the edge, and they dissipate

0:29:19.480 --> 0:29:23.200
<v Speaker 1>the energy of the earthquake by rocking up and down

0:29:23.240 --> 0:29:27.560
<v Speaker 1>within these cages at the foundations that they actually called shoes.

0:29:27.760 --> 0:29:31.160
<v Speaker 1>They act like shoes, and so running along the vertical

0:29:31.240 --> 0:29:34.800
<v Speaker 1>length of the frames are steel cables or steel tendons,

0:29:34.840 --> 0:29:37.400
<v Speaker 1>which are elastic, so you can think of that kind

0:29:37.400 --> 0:29:39.840
<v Speaker 1>of like having a bunch of rubber bands or like

0:29:39.880 --> 0:29:43.640
<v Speaker 1>those elastic stretcher cables holding your building in place and

0:29:43.680 --> 0:29:47.920
<v Speaker 1>helping return it to an upright position right upon its

0:29:48.000 --> 0:29:52.440
<v Speaker 1>rightful place on the foundation. But at the bottom of

0:29:52.480 --> 0:29:54.959
<v Speaker 1>these frames they had these things that they referred to

0:29:55.080 --> 0:29:59.719
<v Speaker 1>as fuses, And basically the idea is that the fuses

0:30:00.000 --> 0:30:02.760
<v Speaker 1>are the parts of the structure that will absorb the

0:30:02.800 --> 0:30:07.000
<v Speaker 1>most energy and become damaged, and the fuses are designed

0:30:07.040 --> 0:30:10.920
<v Speaker 1>to be replaceable. So if there's an earthquake, it tries

0:30:11.000 --> 0:30:14.920
<v Speaker 1>to channel the energy into this fuse area which will

0:30:14.960 --> 0:30:17.840
<v Speaker 1>be damaged and you'll have to replace it. But that's

0:30:17.880 --> 0:30:22.040
<v Speaker 1>you know, pretty easy to do. Cool. Uh So, so

0:30:22.080 --> 0:30:25.960
<v Speaker 1>these are all ways that we have of preventing damage

0:30:26.000 --> 0:30:28.680
<v Speaker 1>in the case of an earthquake. But but but let's

0:30:28.680 --> 0:30:32.600
<v Speaker 1>say that an earthquake does strike and damage is caused. Um,

0:30:32.600 --> 0:30:36.320
<v Speaker 1>how how are science and technology helping us better deal

0:30:36.400 --> 0:30:39.080
<v Speaker 1>with the aftermath of earthquakes? Well, I know one of

0:30:39.120 --> 0:30:41.680
<v Speaker 1>the things that is going on is something we talked

0:30:41.720 --> 0:30:45.240
<v Speaker 1>about in our very recent episode about radar. Uh yeah, yeah,

0:30:45.280 --> 0:30:49.320
<v Speaker 1>the finder. Yeah. So just to revisit this concept briefly,

0:30:49.960 --> 0:30:54.240
<v Speaker 1>it is a way of using radar technology to locate

0:30:54.440 --> 0:30:59.960
<v Speaker 1>human beings trapped underneath rubble. Uh yeah, microwave radar specific

0:31:00.080 --> 0:31:03.040
<v Speaker 1>lee and it this is radar so sensitive that it

0:31:03.080 --> 0:31:07.040
<v Speaker 1>can detect the tiny palpitations of a human heartbeat through

0:31:07.520 --> 0:31:10.840
<v Speaker 1>up to twenty feet of solid concrete or thirty feet

0:31:10.880 --> 0:31:14.880
<v Speaker 1>of wreckage or a hundred feet of open space. So

0:31:15.440 --> 0:31:18.560
<v Speaker 1>that's a bunch um and uh this is technology that

0:31:18.600 --> 0:31:21.680
<v Speaker 1>I think was developed in out of NASA and and

0:31:21.760 --> 0:31:24.080
<v Speaker 1>it and it worked. And in the recent earthquake that

0:31:24.160 --> 0:31:28.280
<v Speaker 1>happened in a Nepal in India, in april of rescuers

0:31:28.320 --> 0:31:32.960
<v Speaker 1>located at least four living victims under ten ft of rebel. So,

0:31:34.240 --> 0:31:38.880
<v Speaker 1>uh go team Doppler effect. That's awesome. UM. Other things

0:31:38.920 --> 0:31:41.920
<v Speaker 1>that we have actually also touched on in the course

0:31:41.920 --> 0:31:46.480
<v Speaker 1>of this podcast include, um using like robots and drones

0:31:46.800 --> 0:31:50.360
<v Speaker 1>for rescues where it is impractical or unsafe for human

0:31:50.400 --> 0:31:54.200
<v Speaker 1>rescuers to go. Yeah, we've talked about programming cockroach drones

0:31:54.320 --> 0:31:57.480
<v Speaker 1>to find people in in rubble right right, um. And

0:31:57.520 --> 0:32:02.840
<v Speaker 1>also smart infrastructure that can engineers uh as to when

0:32:02.880 --> 0:32:06.200
<v Speaker 1>and where damage has been done, so that hopefully before

0:32:06.360 --> 0:32:10.400
<v Speaker 1>you know, if if a minor shock one year makes

0:32:10.400 --> 0:32:12.240
<v Speaker 1>a crack somewhere in a foundation, that could be a

0:32:12.240 --> 0:32:14.920
<v Speaker 1>problem later. That's a thing that like a sensor could go,

0:32:14.960 --> 0:32:18.080
<v Speaker 1>oh hey, engineers, come, come, pay attention to me, and

0:32:18.120 --> 0:32:21.120
<v Speaker 1>hopefully that gets repaired before a larger quake could bring

0:32:21.160 --> 0:32:24.480
<v Speaker 1>the whole building down. That's what you call a smart city,

0:32:24.880 --> 0:32:29.800
<v Speaker 1>smart city, smart buildings as opposed to all these dumb

0:32:29.840 --> 0:32:33.520
<v Speaker 1>buildings we live in now. Oh yeah, so dumb. But hey,

0:32:33.560 --> 0:32:36.040
<v Speaker 1>what about the big question? How about the elephant in

0:32:36.080 --> 0:32:40.360
<v Speaker 1>the room. Can we predict earthquakes? Can we do it?

0:32:40.400 --> 0:32:42.360
<v Speaker 1>Can we know when and where they're going to happen,

0:32:42.440 --> 0:32:44.640
<v Speaker 1>so that we can get people out of harm's way

0:32:44.640 --> 0:32:48.360
<v Speaker 1>ahead of time. This is I think the main thing

0:32:48.400 --> 0:32:53.800
<v Speaker 1>everybody wants to know, of course, And should we just

0:32:53.840 --> 0:32:57.280
<v Speaker 1>go ahead and say it. The answer is not really Yeah, yes,

0:32:57.600 --> 0:33:01.920
<v Speaker 1>certainly not right now. Um And and a lot of

0:33:01.960 --> 0:33:04.440
<v Speaker 1>a lot of researchers are are doubtful that we ever

0:33:04.720 --> 0:33:09.560
<v Speaker 1>will be Um. The seismology community seems to at large

0:33:09.680 --> 0:33:14.600
<v Speaker 1>be saying we'll probably never be able to determine this. Well,

0:33:14.640 --> 0:33:18.760
<v Speaker 1>I mean we're trying, yeah, Um, like with with earth

0:33:18.840 --> 0:33:22.880
<v Speaker 1>earthquake forecasting, which is studying the history and the present

0:33:22.960 --> 0:33:27.800
<v Speaker 1>configuration of a fault and predicting how likely seismic activity

0:33:28.080 --> 0:33:32.360
<v Speaker 1>is in that area within a given period of time. Um.

0:33:32.400 --> 0:33:35.440
<v Speaker 1>But again, according to a lot of seismologists, it's impossible

0:33:35.480 --> 0:33:40.160
<v Speaker 1>to forecast when earthquakes will happen given what we currently

0:33:40.160 --> 0:33:42.880
<v Speaker 1>know about how earthquakes work. We we haven't found a

0:33:42.920 --> 0:33:46.360
<v Speaker 1>pattern despite all of the data that we've been recording. Sure,

0:33:46.440 --> 0:33:48.720
<v Speaker 1>and despite the fact that we can't say when I

0:33:48.760 --> 0:33:51.400
<v Speaker 1>think we do want to emphasize something you just said,

0:33:51.440 --> 0:33:55.400
<v Speaker 1>which is true, we can with some reasonable degree of

0:33:55.440 --> 0:33:59.760
<v Speaker 1>accuracy say where earthquakes are going to happen, oh yeah,

0:33:59.800 --> 0:34:02.680
<v Speaker 1>and not just I mean like obviously along the fault lines,

0:34:02.880 --> 0:34:05.480
<v Speaker 1>but like along specific sections of a fault line. Yeah,

0:34:05.520 --> 0:34:08.759
<v Speaker 1>so it's not necessarily going to be super specific, like

0:34:08.840 --> 0:34:12.439
<v Speaker 1>telling you, you know in this will be right here.

0:34:12.520 --> 0:34:16.920
<v Speaker 1>But we can generally have a pretty good regionally based

0:34:16.960 --> 0:34:21.759
<v Speaker 1>prediction about earthquakes. Unfortunately, the painful element of it is

0:34:21.800 --> 0:34:25.879
<v Speaker 1>you just never really know exactly where or even roughly win.

0:34:26.880 --> 0:34:29.440
<v Speaker 1>And there's actually a good article in the Washington Post

0:34:29.440 --> 0:34:32.319
<v Speaker 1>about this by the writer Joel Aichenbach, who who talks

0:34:32.360 --> 0:34:35.440
<v Speaker 1>about the frustration of scientists who sort of have this knowledge.

0:34:35.440 --> 0:34:40.160
<v Speaker 1>Like he he talks about how the earthquake scientists predicted

0:34:40.840 --> 0:34:45.040
<v Speaker 1>that Catman Do would be, you know, would be vulnerable

0:34:45.080 --> 0:34:47.839
<v Speaker 1>to an earthquake, that something was coming there, but they

0:34:47.840 --> 0:34:50.960
<v Speaker 1>couldn't say they did in April of this year, and

0:34:51.040 --> 0:34:54.640
<v Speaker 1>they couldn't say when and then when it happens. It's

0:34:54.719 --> 0:34:57.479
<v Speaker 1>just kind of this sense of frustration and like, well,

0:34:57.520 --> 0:35:00.880
<v Speaker 1>I mean, there wasn't that much that we could do

0:35:00.920 --> 0:35:04.759
<v Speaker 1>about it, because I mean, you can't you can't evacuate

0:35:04.800 --> 0:35:09.600
<v Speaker 1>an entire population based on well probably sometimes soon sure,

0:35:09.640 --> 0:35:11.480
<v Speaker 1>I mean unless you were just going to say, well,

0:35:11.520 --> 0:35:14.160
<v Speaker 1>we just shouldn't have a city here. And then on

0:35:14.239 --> 0:35:17.760
<v Speaker 1>top of that, there there can be unknown fault lines

0:35:17.880 --> 0:35:21.360
<v Speaker 1>in places that we're not even you know, really privy to, Like,

0:35:21.440 --> 0:35:24.080
<v Speaker 1>there can be earthquakes in places that surprise us. They

0:35:24.080 --> 0:35:27.719
<v Speaker 1>will happen less often, but they will happen, oh sure.

0:35:27.760 --> 0:35:31.920
<v Speaker 1>And fault lines are not these these straight, perfect map lines.

0:35:32.400 --> 0:35:35.359
<v Speaker 1>They're they're they're very jagged in crooked and can can

0:35:35.400 --> 0:35:38.200
<v Speaker 1>go around to interesting new places that you didn't think

0:35:38.200 --> 0:35:40.239
<v Speaker 1>that they would go. Sure. Yeah. One thing is that

0:35:40.280 --> 0:35:42.120
<v Speaker 1>when you have an earthquake in one place, it can

0:35:42.200 --> 0:35:45.799
<v Speaker 1>dissipate energy that that puts stress on another part of

0:35:45.840 --> 0:35:48.359
<v Speaker 1>the tectonic plate or another part of the fault line

0:35:48.360 --> 0:35:50.920
<v Speaker 1>where you wouldn't have expected an earthquake before. And we

0:35:50.960 --> 0:35:55.000
<v Speaker 1>won't necessarily know what's going to happen until it happens. Though,

0:35:55.400 --> 0:35:59.080
<v Speaker 1>it is worth saying that earthquake forecasting is a real thing.

0:35:59.840 --> 0:36:02.239
<v Speaker 1>I is. Cartography is sort of what you'd call it.

0:36:02.280 --> 0:36:05.120
<v Speaker 1>You can make maps and say, based on what we know,

0:36:05.280 --> 0:36:09.600
<v Speaker 1>earthquakes are more likely to happen in these places within

0:36:09.680 --> 0:36:13.960
<v Speaker 1>a certain long given period of time, right right, Um,

0:36:14.040 --> 0:36:19.640
<v Speaker 1>And there are relatively early warning networks. UM. As digital

0:36:19.680 --> 0:36:27.399
<v Speaker 1>communication technology has improved, UH, seismologists have started constructing these

0:36:27.480 --> 0:36:31.240
<v Speaker 1>these large networks of a whole bunch of highly sensitive

0:36:31.280 --> 0:36:35.000
<v Speaker 1>seismometers that can automatically send out alerts not just to

0:36:35.120 --> 0:36:38.319
<v Speaker 1>researchers but also to the general public and therefore give

0:36:38.719 --> 0:36:42.720
<v Speaker 1>a little bit more warning, maybe seconds, maybe minutes before

0:36:42.800 --> 0:36:46.439
<v Speaker 1>an earthquake strikes. Um. And that's I mean, basically because

0:36:46.440 --> 0:36:50.640
<v Speaker 1>seizemic waves only travel about three miles per second tops,

0:36:50.680 --> 0:36:53.319
<v Speaker 1>and information can of course travel a lot faster than that.

0:36:54.000 --> 0:36:58.080
<v Speaker 1>Your internet is faster than the earthquake. Yeah, yeah, hopefully

0:36:58.080 --> 0:37:02.120
<v Speaker 1>fingers crossed. Um And And it sounds like that's absolutely

0:37:02.160 --> 0:37:04.440
<v Speaker 1>no time at all, but but it's plenty enough to

0:37:04.480 --> 0:37:08.799
<v Speaker 1>save lives of say, construction workers who are in precarious positions,

0:37:08.960 --> 0:37:11.960
<v Speaker 1>or of patients who are undergoing surgery, or of of

0:37:12.000 --> 0:37:15.240
<v Speaker 1>people driving on the road. Um. And it also allows

0:37:15.280 --> 0:37:19.720
<v Speaker 1>emergency responders time to begin to prepare. Yeah, it is certainly,

0:37:19.760 --> 0:37:21.719
<v Speaker 1>I mean, even if it's just having a siren go

0:37:21.840 --> 0:37:25.839
<v Speaker 1>off or something that could potentially be useful. But of course,

0:37:25.840 --> 0:37:29.040
<v Speaker 1>what people really want to know is can we get

0:37:29.120 --> 0:37:32.279
<v Speaker 1>much further ahead of the game and One of the

0:37:32.360 --> 0:37:35.040
<v Speaker 1>big things that often comes up when you hear people

0:37:35.080 --> 0:37:37.920
<v Speaker 1>saying no, I think we can predict earthquakes maybe weeks

0:37:37.920 --> 0:37:41.839
<v Speaker 1>ahead of time. Is animals. Oh right, Yeah, there are

0:37:41.960 --> 0:37:45.640
<v Speaker 1>all of these kind of circumstantial reports of animal behavior

0:37:45.800 --> 0:37:49.560
<v Speaker 1>changing dramatically a week or two before an earthquake. Yeah,

0:37:49.600 --> 0:37:53.400
<v Speaker 1>people have reported this for years, supposedly, according to scores

0:37:53.440 --> 0:37:57.440
<v Speaker 1>of anecdotes, fish, birds, rats, reptiles, I mean, what every

0:37:57.520 --> 0:38:01.000
<v Speaker 1>all kinds of animals start acting we're weird before a

0:38:01.040 --> 0:38:05.560
<v Speaker 1>seismic event strikes. One early record is that the ancient

0:38:05.560 --> 0:38:09.279
<v Speaker 1>Greeks reported that animals, including rats and snakes deserted the

0:38:09.280 --> 0:38:13.200
<v Speaker 1>city of hellicay En mass before a huge earthquake destroyed

0:38:13.200 --> 0:38:17.520
<v Speaker 1>it in the fourth century BC. Weird. But whether or

0:38:17.560 --> 0:38:21.120
<v Speaker 1>not that's true, we would need to verify that it's

0:38:21.160 --> 0:38:26.000
<v Speaker 1>a continuously occurring scientific phenomenon, not necessarily like just something

0:38:26.040 --> 0:38:29.200
<v Speaker 1>that happened once, right, because I mean the behavior of

0:38:29.239 --> 0:38:33.359
<v Speaker 1>for example, rats and snakes is relatively ineffable. I mean

0:38:33.560 --> 0:38:36.560
<v Speaker 1>sometimes they just do stuff. Yeah, sure, I mean, can

0:38:36.640 --> 0:38:41.000
<v Speaker 1>animals really predict earthquakes well in advance? Number one? That

0:38:41.040 --> 0:38:45.160
<v Speaker 1>would be a really useful fact were true. It would

0:38:45.200 --> 0:38:48.440
<v Speaker 1>help us save lives, so it's worth studying. Unfortunately, this

0:38:48.520 --> 0:38:51.080
<v Speaker 1>is one of those weird questions that's just really hard

0:38:51.120 --> 0:38:54.040
<v Speaker 1>to answer. It seems to me, based on my reading,

0:38:54.080 --> 0:38:58.720
<v Speaker 1>that generally most scientists are pretty skeptical about using animals

0:38:58.719 --> 0:39:02.480
<v Speaker 1>to predict earthquakes. Some researchers have claimed to discover links

0:39:02.520 --> 0:39:06.640
<v Speaker 1>between animals and earthquakes, but the larger scientific community seems

0:39:06.680 --> 0:39:11.839
<v Speaker 1>to remain pretty unconvinced. Us Unsurprisingly, one person who likes

0:39:11.880 --> 0:39:16.280
<v Speaker 1>this idea is the biologist and parapsychologist Rupert shell Drake.

0:39:16.560 --> 0:39:19.680
<v Speaker 1>He's expressed fondness for the idea that animals can predict

0:39:19.680 --> 0:39:22.839
<v Speaker 1>seismic activity. Though, if you know anything about this guy,

0:39:23.040 --> 0:39:26.800
<v Speaker 1>shell Drake is one of those interesting people who's very smart,

0:39:26.880 --> 0:39:29.319
<v Speaker 1>but it seems to me just generally in favor of

0:39:30.040 --> 0:39:34.799
<v Speaker 1>whatever ideas are opposed to the mainstream scientific establishment. So

0:39:35.000 --> 0:39:38.680
<v Speaker 1>you know, he's into paranormal phenomenon and he's the guy

0:39:38.680 --> 0:39:43.040
<v Speaker 1>who promotes the concept of the morephic residence. Matter has

0:39:43.040 --> 0:39:47.040
<v Speaker 1>a memory and stuff like that. But there actually are

0:39:47.160 --> 0:39:49.479
<v Speaker 1>some studies that we could look at, Like some people

0:39:49.520 --> 0:39:53.239
<v Speaker 1>have claimed that animals might be using their extra sensory

0:39:53.640 --> 0:39:58.120
<v Speaker 1>auditory capabilities to detect sounds outside the normal hearing range

0:39:58.200 --> 0:40:00.960
<v Speaker 1>or something like that. And some these claims are totally

0:40:01.000 --> 0:40:05.360
<v Speaker 1>believable when they concern animals going nuts directly before an earthquake,

0:40:05.400 --> 0:40:08.560
<v Speaker 1>but not so much weeks before, because if it's right

0:40:08.560 --> 0:40:11.279
<v Speaker 1>before the earthquake strikes, that could be the same kind

0:40:11.280 --> 0:40:15.600
<v Speaker 1>of thing we're talking about with these these Uh yeah, exactly,

0:40:15.760 --> 0:40:18.000
<v Speaker 1>it could be the earliest four shocks are just that

0:40:18.040 --> 0:40:21.840
<v Speaker 1>first pee wave that hits before the subsequent shocks do.

0:40:22.680 --> 0:40:27.200
<v Speaker 1>But I did find one recent study that's I think

0:40:27.200 --> 0:40:29.560
<v Speaker 1>worth sighting, though I think I want to site it

0:40:29.600 --> 0:40:32.919
<v Speaker 1>with caution because it just came out pretty recently, and

0:40:33.000 --> 0:40:35.320
<v Speaker 1>it's one of those things that I don't know. It

0:40:35.640 --> 0:40:40.080
<v Speaker 1>just seems like we would definitely want to get some

0:40:40.320 --> 0:40:43.239
<v Speaker 1>more studies of this kind before we assign too much

0:40:43.239 --> 0:40:46.920
<v Speaker 1>credit to it. But anyway, it was a March study

0:40:46.920 --> 0:40:49.680
<v Speaker 1>in the journal Physics and Chemistry of the Earth Parts

0:40:49.719 --> 0:40:53.880
<v Speaker 1>A B n C by Grant, Rollin and Freund, and

0:40:53.920 --> 0:40:58.239
<v Speaker 1>they claim that disturbances in animal behavior were present in

0:40:58.280 --> 0:41:00.680
<v Speaker 1>the weeks leading up to a tooth As an eleven

0:41:00.680 --> 0:41:04.640
<v Speaker 1>earthquake in the Peruvian Andies. So here's what happened. They

0:41:04.680 --> 0:41:08.880
<v Speaker 1>claimed that they used motion triggered cameras in a national

0:41:09.000 --> 0:41:13.360
<v Speaker 1>park in Peru to measure the extent of wildlife activity,

0:41:13.480 --> 0:41:16.640
<v Speaker 1>like you know, physical wildlife movement in the area, and

0:41:16.640 --> 0:41:19.160
<v Speaker 1>they found that in the three weeks leading up to

0:41:19.239 --> 0:41:24.520
<v Speaker 1>the earthquake, quote, animal activity declined significantly, and there was

0:41:24.560 --> 0:41:28.080
<v Speaker 1>even less activity in the final like seven days before

0:41:28.160 --> 0:41:32.680
<v Speaker 1>the earthquake. Now, the author's explanation for the claimed reduction

0:41:32.719 --> 0:41:36.680
<v Speaker 1>and animal behavior was really interesting. They suggested that it

0:41:36.760 --> 0:41:40.920
<v Speaker 1>was another thing they measured concurrent with this reduction and activity,

0:41:41.000 --> 0:41:46.560
<v Speaker 1>which was an increase in the positive airborne ion injection

0:41:46.719 --> 0:41:51.160
<v Speaker 1>at the ground to air interface. So basically the earth

0:41:51.560 --> 0:41:56.560
<v Speaker 1>injecting positively charged particles positive ions up into the air

0:41:57.000 --> 0:42:00.360
<v Speaker 1>and this disturbing animal behaviors. And they were suggest testing

0:42:00.400 --> 0:42:05.040
<v Speaker 1>that this injection of positively charged ions into the air

0:42:05.160 --> 0:42:08.640
<v Speaker 1>could be a result of some kind of preliminary earthquake

0:42:08.680 --> 0:42:15.520
<v Speaker 1>precursor underground. Huh so so maybe maybe I mean, like

0:42:15.560 --> 0:42:17.600
<v Speaker 1>I said, I want to stress caution with this kind

0:42:17.640 --> 0:42:21.359
<v Speaker 1>of thing, because, uh, it seems to go against what

0:42:21.400 --> 0:42:24.880
<v Speaker 1>we know so far, and it's it just came out recently.

0:42:24.920 --> 0:42:27.680
<v Speaker 1>There might be good reasons for thinking there could be

0:42:27.719 --> 0:42:31.160
<v Speaker 1>problems with this study that we haven't read about yet. Sure. Um,

0:42:31.320 --> 0:42:34.880
<v Speaker 1>I I did read another similar report that was published

0:42:35.040 --> 0:42:38.960
<v Speaker 1>UM from the Open University in the UK via the

0:42:39.080 --> 0:42:44.920
<v Speaker 1>Journal of Zoology back in and Uh they were reporting

0:42:45.040 --> 0:42:48.000
<v Speaker 1>that five days before an earthquake struck struck Italy in

0:42:48.040 --> 0:42:52.879
<v Speaker 1>two thousand, nine of the male toads in a population

0:42:53.360 --> 0:42:57.480
<v Speaker 1>abandoned their breeding site. Uh. Their normal behavior would have

0:42:57.520 --> 0:43:00.600
<v Speaker 1>been to have stayed through the awning, but they just

0:43:00.640 --> 0:43:04.760
<v Speaker 1>kind of up and left. And apparently, um, this behavior

0:43:04.840 --> 0:43:09.440
<v Speaker 1>coincided with ion A sphere disruptions, although the cause of

0:43:09.440 --> 0:43:12.640
<v Speaker 1>those disruptions was not discussed in the report or not

0:43:13.040 --> 0:43:17.200
<v Speaker 1>reported in the report. Yes, yeah, I mean so I

0:43:17.200 --> 0:43:20.480
<v Speaker 1>think that's very interesting. But I guess we again we

0:43:20.560 --> 0:43:24.120
<v Speaker 1>don't really know. Yeah, but two reports does not make

0:43:24.160 --> 0:43:27.880
<v Speaker 1>an appropriate sample for making scientific decisions. Sure, but I

0:43:28.200 --> 0:43:31.959
<v Speaker 1>do think that this is worth studying because if there

0:43:32.080 --> 0:43:34.319
<v Speaker 1>is any truth to the fact that animal behavior can

0:43:34.360 --> 0:43:37.879
<v Speaker 1>predict earthquakes, I mean, the scientists aren't suggesting that they

0:43:37.920 --> 0:43:41.560
<v Speaker 1>have telepathy or something triggering the animal reactions. These triggers

0:43:41.800 --> 0:43:44.800
<v Speaker 1>should be normal physical events that we could design instruments

0:43:44.840 --> 0:43:48.040
<v Speaker 1>to look for. Oh yeah, one that I one possibility

0:43:48.040 --> 0:43:51.040
<v Speaker 1>that I read about was emissions of rate on from

0:43:51.160 --> 0:43:55.720
<v Speaker 1>underground rock UM. Right on being a gaseous decay product

0:43:55.760 --> 0:43:59.120
<v Speaker 1>of uranium which gets trapped in rocks UM, and the

0:43:59.360 --> 0:44:02.680
<v Speaker 1>theory here goes that before an earthquake, kind of pre

0:44:02.840 --> 0:44:07.000
<v Speaker 1>movements underground break apart rocks and release rate on up

0:44:07.040 --> 0:44:10.520
<v Speaker 1>into the soil and water above UM. Since radon is

0:44:10.600 --> 0:44:13.600
<v Speaker 1>radioactive and has a half life of of just like

0:44:13.640 --> 0:44:17.319
<v Speaker 1>three to four days UM, it would be really a

0:44:17.400 --> 0:44:20.480
<v Speaker 1>very useful metric to gather if a connection is in

0:44:20.520 --> 0:44:24.880
<v Speaker 1>fact proven, But uh, no conclusive evidence has been found

0:44:24.920 --> 0:44:28.840
<v Speaker 1>as of yet. So you know, what I'm really thinking

0:44:29.160 --> 0:44:33.480
<v Speaker 1>is if we determine that animals can sense earthquakes, and

0:44:33.520 --> 0:44:36.320
<v Speaker 1>then we can use that to make an earthquake sensing machine,

0:44:37.000 --> 0:44:40.560
<v Speaker 1>and then we can evacuate cities where earthquakes are going

0:44:40.640 --> 0:44:43.759
<v Speaker 1>to happen before they happen. What's going to happen to

0:44:43.760 --> 0:44:46.840
<v Speaker 1>the future of the earthquake disaster movie genre? Oh man,

0:44:47.280 --> 0:44:50.840
<v Speaker 1>They'll all have to be fabulous period pieces. Yeah, Oh

0:44:50.880 --> 0:44:52.799
<v Speaker 1>that's right. The rock will have to put on like

0:44:52.880 --> 0:44:55.680
<v Speaker 1>some like plaid and pretend to be some like grunge

0:44:55.719 --> 0:44:58.759
<v Speaker 1>guy from the nineties when there is an earthquake in California.

0:44:58.920 --> 0:45:02.760
<v Speaker 1>Yeah yeah, or like like a toga of some kind,

0:45:02.960 --> 0:45:05.120
<v Speaker 1>and so that he can run around in a ancient

0:45:05.160 --> 0:45:08.400
<v Speaker 1>Greek or Roman city. Oh yeah, yeah, while all the

0:45:08.480 --> 0:45:14.160
<v Speaker 1>rats and snakes are fleeing. Yeah, you know, like the

0:45:14.239 --> 0:45:16.840
<v Speaker 1>wind and the caverns under the earth. Where is it

0:45:16.880 --> 0:45:21.880
<v Speaker 1>gonna go? She's gonna blow? It would have to be

0:45:21.880 --> 0:45:25.759
<v Speaker 1>Paul Gimi saying that though, Yeah, where's that wind a

0:45:25.800 --> 0:45:31.560
<v Speaker 1>gonna go? How was my Paul impression? But I'm not

0:45:31.640 --> 0:45:34.520
<v Speaker 1>I'm not positive about the quality of either the movie

0:45:34.560 --> 0:45:39.040
<v Speaker 1>that we are hypothesizing or of your Paul Madi impersonation. Well,

0:45:39.080 --> 0:45:44.520
<v Speaker 1>I apologize, No, never apologize for Paul impersonations. They're really

0:45:44.560 --> 0:45:50.200
<v Speaker 1>They're all good. Well, anyway, bringing it back a little bit, well,

0:45:50.480 --> 0:45:52.680
<v Speaker 1>I do think that this is really interesting. And even

0:45:52.719 --> 0:45:54.480
<v Speaker 1>if it turns out to be the case, which a

0:45:54.480 --> 0:45:57.279
<v Speaker 1>lot of seismologists think is the case, that we will

0:45:57.320 --> 0:46:00.920
<v Speaker 1>never be able to predict earthquakes, we can at least

0:46:01.000 --> 0:46:03.439
<v Speaker 1>make our cities better, We can make our buildings better,

0:46:03.520 --> 0:46:06.640
<v Speaker 1>we can do a better job protecting ourselves when the

0:46:06.680 --> 0:46:09.040
<v Speaker 1>earthquakes do strike. And who knows, maybe one day we

0:46:09.080 --> 0:46:11.600
<v Speaker 1>will find out that we can predict him ahead of time.

0:46:11.600 --> 0:46:13.759
<v Speaker 1>Ah yeah yeah. And this isn't even for for new

0:46:13.800 --> 0:46:17.239
<v Speaker 1>cities alone. There are lots of ways that engineers are

0:46:17.280 --> 0:46:20.680
<v Speaker 1>looking at for retrofitting buildings to make them stronger in

0:46:20.760 --> 0:46:25.120
<v Speaker 1>places that we strongly suspect a quake will strike eventually. Yeah,

0:46:25.200 --> 0:46:29.680
<v Speaker 1>so let's look at those seismographic maps and get to work.

0:46:29.880 --> 0:46:33.600
<v Speaker 1>Yeah yeah. Um. So, thank you so much Jacob and

0:46:33.640 --> 0:46:36.319
<v Speaker 1>Matt for for writing in. This has been a fascinating

0:46:36.360 --> 0:46:38.640
<v Speaker 1>thing to research. And we got to watch the San

0:46:38.719 --> 0:46:42.840
<v Speaker 1>Andreas trailer a whole bunch and that was endlessly entertaining.

0:46:43.760 --> 0:46:47.120
<v Speaker 1>So if any of you guys have any other questions

0:46:47.120 --> 0:46:48.600
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0:46:48.640 --> 0:46:51.640
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0:46:52.040 --> 0:46:55.399
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