WEBVTT - How Earthquakes Work

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<v Speaker 1>Brought to you by the reinvented two thousand twelve camera.

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<v Speaker 1>It's ready. Are you welcome to Stuff you should know

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<v Speaker 1>from house Stuff Works dot Com. Hey, and welcome to

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<v Speaker 1>the podcast. I'm Josh Clark. With me is Charles W.

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<v Speaker 1>Chuck Chuckers. I love you, Bryant, you're saying that or

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<v Speaker 1>that's my middle name. I love everybody. Sure, I'm in

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<v Speaker 1>high spirit city, Chuck. Things are moving, stuff is taking place,

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<v Speaker 1>things are coming to. Fruition is out of nowhere because

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<v Speaker 1>you were not feeling this way, like literally seconds before

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<v Speaker 1>we recorded. I don't know what you're talking about. Wow,

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<v Speaker 1>I'm in brass, dude. You can turn it on. You

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<v Speaker 1>know why, Chuck? Why? I can tell because you're drinking

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<v Speaker 1>your little energy drinking. Yes, I would call it an

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<v Speaker 1>energy soda, be little dream sailor. That was Yeah, you

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<v Speaker 1>really like that podcast? Into it? I thought it was good.

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<v Speaker 1>My favorite part was when we mentioned the doctor in Berkeley,

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<v Speaker 1>when you said, um boom or around or something like that. Yeah,

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<v Speaker 1>that's funny. Yeah, thanks, I thought um. I liked all

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<v Speaker 1>the nose breathing I did in that podcast. For some reason,

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<v Speaker 1>we just sit around talk about our whole podcast Hey, Chuck, Hey, Josh,

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<v Speaker 1>you did some time out in l A right. Yeah. So, um,

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<v Speaker 1>I know that you met Matthew McConaughey. You left that

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<v Speaker 1>story and uh keep for Sutherland's driver. Yeah, and him.

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<v Speaker 1>I saw him in the grocery store too, with his driver,

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<v Speaker 1>No with How did you know it was him that

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<v Speaker 1>a bucks? Some blonde babe actually got you? Um it

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<v Speaker 1>was Keith for Southernlandon. I mean it's unmistakable got you.

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<v Speaker 1>Um he's breathing, mouth breathing behind me in line. We're

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<v Speaker 1>gonna get in trouble one day for that. I know

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<v Speaker 1>he's a hot head too. He just got suited. He

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<v Speaker 1>like hit a photographer somebody did he really? Yeah? So

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<v Speaker 1>watch watch your back. Plus he knows his way around

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<v Speaker 1>a gun, Yes he does, and he's ruthless, as I

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<v Speaker 1>understand it from what I've seen on TV. I know

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<v Speaker 1>what you're about to ask me about Los Angeles. I

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<v Speaker 1>know you do, because we're doing how earthquakes work. So Chuck,

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<v Speaker 1>let's just cut to the chase, shall we. I have

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<v Speaker 1>never felt an earthquake out there, nor have I. I

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<v Speaker 1>was out there for four years, dude, and I was

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<v Speaker 1>there when earthquakes happened, and I never realized it and

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<v Speaker 1>felt anything. Friends of mine will be like, dude, did

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<v Speaker 1>you feel that this morning? Yeah? No, I have no idea.

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<v Speaker 1>Did they use a lot of that um honey that

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<v Speaker 1>comes in the Little Bear? Yes? Did they? They did, dude,

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<v Speaker 1>that's what they say. And Kelly Chuck, I've never experienced

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<v Speaker 1>an earthquake either. The closest um thing to an earthquake

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<v Speaker 1>story I have involves earthquake proofing. Let's hear it. Remember

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<v Speaker 1>my friend Hippie Rob, Hippy Rob did a little time

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<v Speaker 1>out in Uh, I'm so a fan of the honey Bear. Yeah, yes,

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<v Speaker 1>oh yeah, Hippy Rob did a some time out in

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<v Speaker 1>San Quentin. Actually really yeah, here's the thing. He was

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<v Speaker 1>not looking forward to doing San Quentin, I imagine, um.

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<v Speaker 1>And he finds out that right when he gets there

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<v Speaker 1>that um, he and all the other relatively light off

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<v Speaker 1>enders are going to be moved to Fulsome prison, which

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<v Speaker 1>was undergoing earthquake proofing construction. Right, so they were going

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<v Speaker 1>to keep all the light offenders at Folsome and then

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<v Speaker 1>move all the light offenders at San Quentin over to Folsom.

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<v Speaker 1>And then they moved all like the murderers and rapists

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<v Speaker 1>and peder asks to uh that we're at San Quentin.

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<v Speaker 1>Fo over to San Quentin. Wow, that's my earthquake story.

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<v Speaker 1>Good for Falsome. So Hippie Rob got off easy. He

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<v Speaker 1>was with light offenders in Falsome? Did he Did they

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<v Speaker 1>actually have to work on the earthquake proofing where they

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<v Speaker 1>put the work or was it just go? I don't

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<v Speaker 1>think so. Would you trust the guy named Hippie Rob

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<v Speaker 1>to earthquake proofs your prison? Would not? I wouldn't either.

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<v Speaker 1>So let's talk about earthquakes. Let's do it. Can I

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<v Speaker 1>you want a little history? I did some extra research.

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<v Speaker 1>Let's hear it. So before nineteen fifteen, we didn't really

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<v Speaker 1>have much of a conception of what was going on

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<v Speaker 1>geologically with with the continents, right? Was it just anyone's

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<v Speaker 1>gas at that point? Yeah? I think you or I

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<v Speaker 1>could have come up with adequate theory. We'd be like

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<v Speaker 1>ghosts or something like that. Um, but the ghosts was

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<v Speaker 1>not an acceptable explanation for a guy named Alfred Wegner. Uh,

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<v Speaker 1>he's a German clearly because his last name because with

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<v Speaker 1>a W, but I pronounced it with a V, which

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<v Speaker 1>is a dead giveaway for a German is a German,

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<v Speaker 1>right um. So Wagner Um was actually an astronomer by training,

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<v Speaker 1>but he was fascinated with geology, and he became increasingly

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<v Speaker 1>fascinated when he found out that there had been fossils

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<v Speaker 1>identical plant in animal fossils found um on the let's see,

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<v Speaker 1>that would be the east coast of South America and

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<v Speaker 1>the west coast of Africa. And at the time, the

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<v Speaker 1>predominant theory was that there were land bridges that were

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<v Speaker 1>now under water and that's how these species would have

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<v Speaker 1>gotten together. Wegner he thought, I don't know that that's

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<v Speaker 1>entirely true, and he also noted that Africa kind of

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<v Speaker 1>looked like it could fit into South America. Interesting point.

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<v Speaker 1>So he started thinking about it and think about and

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<v Speaker 1>he realized that some he he postulated about three million

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<v Speaker 1>years ago, all of the continents were hooked together, which

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<v Speaker 1>he called one big, stinking massive land right in Greek,

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<v Speaker 1>that would be Pangaea. And uh so Pangea starts to

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<v Speaker 1>break apart, and basically Wevegner uh postulated that the the

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<v Speaker 1>continents were in fact still drifting. He thought that they

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<v Speaker 1>were basically plowing along the ocean, and it was due

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<v Speaker 1>to centrifugal force and title movement. And title movement, it

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<v Speaker 1>makes sense for the time. It's back in UM. He

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<v Speaker 1>was right about the continents drifting. We know that, but

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<v Speaker 1>not with the centrifugal force the title movement. One of

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<v Speaker 1>his rivals calculated that UM, for the tides to move

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<v Speaker 1>a continent, that that kind of force would actually stop

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<v Speaker 1>the rotation of the Earth in less than twelve months.

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<v Speaker 1>So that wasn't it. But he was right about the

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<v Speaker 1>continents drifting. UM. He was pretty much ridiculed during his lifetime.

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<v Speaker 1>But in the nineteen fifties and sixties, as we got

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<v Speaker 1>more and more acquainted with UM, the the actual ridges

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<v Speaker 1>along the plates, uh, they figured out that Vegner had

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<v Speaker 1>been right. The continents were in fact drifting, not in

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<v Speaker 1>the way he thought. Right, go, go Vegner, that's the

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<v Speaker 1>history lesson. That's good. And I didn't know that. I know,

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<v Speaker 1>I told you it was extra research. And that's continental

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<v Speaker 1>drift theory. Right. Once we figured this out that actually

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<v Speaker 1>the what is that the lithosphere, the surface of the

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<v Speaker 1>Earth which all these different plates make up, are actually

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<v Speaker 1>moving along the atheneos sphere, which is this layer of

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<v Speaker 1>rock that Actually it is a lubricantant behaves like a

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<v Speaker 1>liquid because of the heat and pressure, right, right, So

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<v Speaker 1>it's the goop in between the plates that's kind of

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<v Speaker 1>cushioning everything. Right. And we figured this out. I didn't,

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<v Speaker 1>You didn't, but you know, geologists did. Um and we

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<v Speaker 1>once we figured it out, we realized that that explains

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<v Speaker 1>all sorts of stuff like volcanoes, um, trenches, yes, mountains

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<v Speaker 1>under ocean, uh, bridges under the ocean. But most importantly

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<v Speaker 1>this podcast, it also explains Yeah, volcanoes, plate tectonics, earthquakes.

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<v Speaker 1>It's good stuff. Earthquakes, no volcanoes, Okay, tsunami. Well so wait,

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<v Speaker 1>we're gonna switch mid podcast and do how volcanoes work.

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<v Speaker 1>Let's just make it up. Yeah, it really does. It

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<v Speaker 1>explains earthquakes, uh, and it all makes sense. And I

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<v Speaker 1>love plate technico tectonics. Who doesn't, you know, just the

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<v Speaker 1>thought of our earth. I don't know. Stuff like this

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<v Speaker 1>makes me feel insignificant in a good way, that that

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<v Speaker 1>you know, we're kind of on this earth humans and

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<v Speaker 1>we think we're all that, but we're really pit the

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<v Speaker 1>whim of whatever the Earth decided to do. There was

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<v Speaker 1>something going on at the core that we didn't know

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<v Speaker 1>about right now, and all of a sudden everything started

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<v Speaker 1>going haywire. We'd be powerless. Oh yeah, so I kind

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<v Speaker 1>of like that insignificant feeling occasionally. I mean we're powerless

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<v Speaker 1>to you know, baseball size hail. Yeah exactly, you know,

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<v Speaker 1>let alone the movement of continents. Yeah, you want some stats, Josh, Chuck,

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<v Speaker 1>I knew you'd bring those up. There are actually many, many,

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<v Speaker 1>many earthquakes all the time. Uh, you just don't feel

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<v Speaker 1>them all. They don't get attention if you don't feel them,

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<v Speaker 1>and they don't get attention if they're not where people are,

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<v Speaker 1>which a lot of them are as well or away

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<v Speaker 1>from people. Uh, there's one earthquake every eleven seconds, Josh.

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<v Speaker 1>That's eight thousand per day, about three million per year. Actually,

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<v Speaker 1>the U S Geological Survey maintains the site Chuck um

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<v Speaker 1>that has like updated earthquake activity around the world. Did

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<v Speaker 1>you know about, let's see, six hours ago, there was

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<v Speaker 1>a six point seven earthquake UM in Papua New Guinea. Dude, Really,

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<v Speaker 1>that's big. It's a pretty cool sit Anything over seven

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<v Speaker 1>is the major scale is a big time major. Yeah,

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<v Speaker 1>we'll get to the Richter scale and if you don't

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<v Speaker 1>give it away. So, yeah, that many earthquakes is a lot,

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<v Speaker 1>but you don't feel them if they're if they're must

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<v Speaker 1>them are deep underground, right or in uninhabited areas exactly,

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<v Speaker 1>And so unless it's in a may your city or

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<v Speaker 1>something and killing folks, it's not gonna make the news.

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<v Speaker 1>But speaking of killing folks, have got one more stat

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<v Speaker 1>I like this one. One point five million people have

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<v Speaker 1>died from earthquake related activity in the last hundred years alone.

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<v Speaker 1>And you know, earthquakes get a really bad rap, chuck,

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<v Speaker 1>because really most of those debts are attributed to you know,

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<v Speaker 1>collapse structures or tsunamis or mud slides generated by the

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<v Speaker 1>earthquake exactly. The earthquake just opens up, the earth opens up,

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<v Speaker 1>and he swallowed into it like the movies, except in Superman.

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<v Speaker 1>Yeah remember that. Yeah, he reversed it. That dude flying

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<v Speaker 1>very fast, and he liked the Lex Luthor's girlfriend doing

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<v Speaker 1>so too. He did crickets, Josh, I think we should

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<v Speaker 1>get back to tectonics. Okay, let's talk about plates under

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<v Speaker 1>the earth and what can happen. Basically when these things

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<v Speaker 1>meet up. The two plates meet up, right, which where

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<v Speaker 1>they where two plates meet is of it's a fault, right, right.

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<v Speaker 1>You probably heard of the San Andrea's fault line in California,

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<v Speaker 1>very famous. Fault faults are where most earthquake earthquakes happen.

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<v Speaker 1>I keep on say volcanoes, it's so weird. So, uh,

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<v Speaker 1>what happens when plates get together is they can do

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<v Speaker 1>a couple of things. They can move apart from each other. Uh.

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<v Speaker 1>In that case, the magma comes out, Magma turns into

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<v Speaker 1>lava that cools and hardens, and then it kind of

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<v Speaker 1>reforms as part of the structure. So we should he

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<v Speaker 1>uses through and then makes it more solid, right, and

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<v Speaker 1>then it cools and you have a new land mass form.

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<v Speaker 1>Exactly right. We should also probably point out here to

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<v Speaker 1>any um people who believe in the hollow earth theory

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<v Speaker 1>that we're discussing this based on the notion that the

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<v Speaker 1>Earth's core is molten. Okay, yeah, sure, so go ahead

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<v Speaker 1>and chuck disclaimer there. What kind of fault was that

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<v Speaker 1>that you just described? Well, no, that wasn't a fault.

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<v Speaker 1>That's just what happens when the plates move apart. When

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<v Speaker 1>the plates pushed together one oftentimes one will go underneath

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<v Speaker 1>the other. Like they'll meet up and then one will

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<v Speaker 1>slide onto the other one and it dissolves basically at

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<v Speaker 1>that point. And the final thing josh Ish the plates

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<v Speaker 1>can slide against each other, so they just kind of

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<v Speaker 1>pass in the night, basically, just kind of moving by

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<v Speaker 1>each other very slowly. And all these different things that

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<v Speaker 1>I'm talking about where these plates meet, that is where

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<v Speaker 1>we get to the faults. Right there, there's four kinds, right,

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<v Speaker 1>the S and D. There's four kinds that can they

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<v Speaker 1>either go vertically or horizontally. As far as the faults

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<v Speaker 1>are concerned, You've got the normal fault and the reverse fault.

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<v Speaker 1>Those are vertical faults, right, So the normal fault is

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<v Speaker 1>where the plates actually move away from one another. The

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<v Speaker 1>reverse fault is where they moved together, right, And then

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<v Speaker 1>you have ones that that move horizontally, which I think

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<v Speaker 1>the San Andrea's fault is is a horizontal fault. Is

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<v Speaker 1>it a thrust fault? I think it's either a thrust

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<v Speaker 1>fall or strike slip fault. Okay, so it's basically the

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<v Speaker 1>same thing, except along along horizontal lines rather than vertical. Right,

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<v Speaker 1>But no matter which way they're moving, they can be

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<v Speaker 1>moving apart, moving together horizontally or vertically. UM. All fault

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<v Speaker 1>lines are basically where plates are still pressing together very tightly, right,

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<v Speaker 1>and when when they pressed together, they're eventually going to

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<v Speaker 1>get locked because of friction, right, But the pressure is

0:12:09.720 --> 0:12:11.839
<v Speaker 1>still going. They still want to move. So all this

0:12:11.960 --> 0:12:15.560
<v Speaker 1>potential energy is being built up, and as it builds

0:12:15.559 --> 0:12:19.360
<v Speaker 1>and builds and builds, the pressure eventually overcomes the resistance

0:12:19.600 --> 0:12:22.280
<v Speaker 1>and all of a sudden you have a slip. It breaks,

0:12:22.480 --> 0:12:25.880
<v Speaker 1>it does, and that's that's actually the epicenter of the

0:12:25.920 --> 0:12:28.360
<v Speaker 1>focus of the earthquake where that happens right there. That

0:12:28.440 --> 0:12:30.679
<v Speaker 1>is the key, that is what an earthquake is, Yes,

0:12:30.960 --> 0:12:34.480
<v Speaker 1>is when the initial fault break or more that happened

0:12:34.520 --> 0:12:38.040
<v Speaker 1>later on occur. We really paid that out in a

0:12:38.160 --> 0:12:41.680
<v Speaker 1>dramatic fashion, didn't we. Yeah, it didn't feel that dramatic

0:12:41.679 --> 0:12:43.320
<v Speaker 1>to me. It will when we listen to that, maybe

0:12:43.440 --> 0:12:48.160
<v Speaker 1>because I know the ending, so chuck right, they can't

0:12:48.160 --> 0:12:52.520
<v Speaker 1>believe you gave it away. So fault zones, that's that's

0:12:52.520 --> 0:12:55.280
<v Speaker 1>where there's lots of faults together connected, right. Yeah, So

0:12:55.320 --> 0:12:57.640
<v Speaker 1>one of those one of those faults slipping one of

0:12:57.679 --> 0:13:00.360
<v Speaker 1>that UM a place where the potential energy you turns

0:13:00.400 --> 0:13:04.080
<v Speaker 1>kinectic all of a sudden can actually trigger um faults,

0:13:05.040 --> 0:13:08.040
<v Speaker 1>or it can actually trigger movement along other faults that

0:13:08.080 --> 0:13:11.320
<v Speaker 1>are connected those fault zones you mentioned, right, That's why

0:13:11.400 --> 0:13:14.480
<v Speaker 1>earthquakes often happen in a series. It's more than more

0:13:14.520 --> 0:13:17.800
<v Speaker 1>than one, right, and they almost always happened along the faults.

0:13:17.840 --> 0:13:20.880
<v Speaker 1>But I know that very uh one, very famous earthquake

0:13:20.960 --> 0:13:25.000
<v Speaker 1>in eighteen eleven and eighteen twelve, which I didn't Did

0:13:25.040 --> 0:13:28.240
<v Speaker 1>that happen in like December thirty one, in January one

0:13:28.440 --> 0:13:31.680
<v Speaker 1>or what? I don't know. That's a good point twelve

0:13:32.000 --> 0:13:34.520
<v Speaker 1>one long earthquake. Yeah, it would be. We'll find out

0:13:34.559 --> 0:13:36.800
<v Speaker 1>about that. But that occurred in the middle of a plate,

0:13:36.840 --> 0:13:39.000
<v Speaker 1>in the middle of the North American continental Plate, which

0:13:39.000 --> 0:13:41.040
<v Speaker 1>is odd at the time, but it was They found

0:13:41.040 --> 0:13:44.440
<v Speaker 1>out later that deep beneath the earth that was in

0:13:44.480 --> 0:13:47.720
<v Speaker 1>fact a six hundred million year old fault zone. So yeah,

0:13:47.800 --> 0:13:50.440
<v Speaker 1>there you have it. Yeah, so it's it's some way

0:13:50.520 --> 0:13:55.560
<v Speaker 1>or another there's a fault zone involved. Indeed, so chuck um,

0:13:55.600 --> 0:13:58.760
<v Speaker 1>we actually have a way to measure earthquakes. We measure

0:13:58.800 --> 0:14:03.600
<v Speaker 1>them through their seismic waves, right, make waves, which seismic

0:14:03.600 --> 0:14:06.600
<v Speaker 1>waves are the energy that radiates from their focus and

0:14:06.720 --> 0:14:09.640
<v Speaker 1>it it acts as a wave much like a wave

0:14:09.880 --> 0:14:12.200
<v Speaker 1>in water, right, like if you were to throw sound

0:14:12.240 --> 0:14:14.800
<v Speaker 1>waves rock and a pond, that kind of thing. There's

0:14:14.880 --> 0:14:18.440
<v Speaker 1>there's two different types of waves, two major types of waves.

0:14:18.600 --> 0:14:22.280
<v Speaker 1>You have body waves and you have surface waves. So

0:14:22.360 --> 0:14:25.000
<v Speaker 1>let's talk about body waves first. Yes, they move through

0:14:25.040 --> 0:14:27.080
<v Speaker 1>the inside of the earth, the inner part of the earth. Right.

0:14:27.320 --> 0:14:29.160
<v Speaker 1>And well there's two different kinds of it's primary and

0:14:29.160 --> 0:14:33.600
<v Speaker 1>secondary body waves waves, pea waves or s waves. It's

0:14:33.640 --> 0:14:38.040
<v Speaker 1>easy to remember mnemonic induction and lucid dreaming, etcetera. Right.

0:14:38.080 --> 0:14:41.360
<v Speaker 1>They travel about one to five miles per second. The

0:14:42.880 --> 0:14:46.280
<v Speaker 1>pea waves too. Yeah, and they're actually they can move

0:14:46.360 --> 0:14:49.840
<v Speaker 1>through solid liquid or gas. Yes, they cannot be stopped. No,

0:14:50.000 --> 0:14:51.680
<v Speaker 1>so they can actually go from one end of the

0:14:51.680 --> 0:14:54.080
<v Speaker 1>Earth to the other. Well, they do too every time.

0:14:54.120 --> 0:14:56.080
<v Speaker 1>Isn't that correct? I don't know. I think that's what

0:14:56.120 --> 0:15:00.040
<v Speaker 1>it says. We'll find out. Uh. And these these the

0:15:00.640 --> 0:15:03.840
<v Speaker 1>pea waves, actually they affect the stuff that they're moving,

0:15:03.880 --> 0:15:07.680
<v Speaker 1>like say, rock horizontally, so it shakes back and forth

0:15:08.000 --> 0:15:10.920
<v Speaker 1>on a horizontal plane. Okay, And like you said, they're

0:15:10.960 --> 0:15:13.120
<v Speaker 1>the fastest, so they get there first. But I got

0:15:13.160 --> 0:15:15.520
<v Speaker 1>the impression that they caused the least amount of damage.

0:15:16.080 --> 0:15:19.000
<v Speaker 1>Then you have secondary waves, right, secondary body waves. Yeah,

0:15:19.040 --> 0:15:22.440
<v Speaker 1>that's the problem. Well, they're the first problem because they

0:15:22.680 --> 0:15:27.840
<v Speaker 1>displaced rock perpendicularly to the direction of the wave. Right.

0:15:28.120 --> 0:15:32.120
<v Speaker 1>So you remember the movie Tremors, So you remember the

0:15:32.200 --> 0:15:35.560
<v Speaker 1>worms going underground and it was displacing dirt up on

0:15:35.640 --> 0:15:39.080
<v Speaker 1>the Earth's surface. Same thing. That's like, that's like a

0:15:39.080 --> 0:15:41.360
<v Speaker 1>secondary wave and s wave. I love that you're quoting

0:15:41.360 --> 0:15:48.320
<v Speaker 1>tremors are scientific? Backup. I love that one. You It's

0:15:48.440 --> 0:15:53.720
<v Speaker 1>great spread ward classic. So so actually that was Kevin Bay. Yeah,

0:15:53.760 --> 0:15:55.160
<v Speaker 1>that was such a good one. It's probably one of

0:15:55.160 --> 0:15:59.280
<v Speaker 1>my top five. Yeah. Um, so let's let's talk about

0:15:59.320 --> 0:16:02.480
<v Speaker 1>surface waves you want, Well you should actually just say

0:16:02.480 --> 0:16:05.080
<v Speaker 1>real quick though, that they don't travel through solid material,

0:16:05.920 --> 0:16:11.120
<v Speaker 1>the secondary so they stopped liquid the liquid Earth's core,

0:16:12.040 --> 0:16:14.840
<v Speaker 1>or if you believe in hollow war theory, they would

0:16:14.840 --> 0:16:18.120
<v Speaker 1>stop when it became hollow because it doesn't travel through

0:16:18.120 --> 0:16:21.160
<v Speaker 1>gas apparently either, right, Yeah, they would stop at the

0:16:21.160 --> 0:16:24.640
<v Speaker 1>temple of Doom. Yeah, according to dollarwar theory. Can we

0:16:24.680 --> 0:16:28.560
<v Speaker 1>talk about surface waves yet? Yes, we're there. Let's see it.

0:16:28.680 --> 0:16:31.200
<v Speaker 1>They're like more like the waves in a body of water, right,

0:16:31.400 --> 0:16:33.680
<v Speaker 1>they move the earth up and down. Did you see

0:16:33.720 --> 0:16:36.360
<v Speaker 1>some of the pictures in this article. This is a

0:16:36.440 --> 0:16:39.760
<v Speaker 1>really cool article for pictures. There's actually a page, picture

0:16:39.800 --> 0:16:44.800
<v Speaker 1>page of nothing but earthquake aftermath pictures and they're cool

0:16:44.960 --> 0:16:47.640
<v Speaker 1>interactive things too. When you talk about the plate shifting,

0:16:48.080 --> 0:16:51.360
<v Speaker 1>some animations you can click on. Did you see the

0:16:51.360 --> 0:16:54.840
<v Speaker 1>one with the railroad tracks? What was that, Peru? I

0:16:54.840 --> 0:16:57.400
<v Speaker 1>don't remember. There's a picture in this article of railroad

0:16:57.400 --> 0:17:02.280
<v Speaker 1>tracks that um basically just make a perfect s because

0:17:02.480 --> 0:17:05.200
<v Speaker 1>of the surface waves that hit it during an earthquake. Well,

0:17:05.200 --> 0:17:08.159
<v Speaker 1>and the crops that shifted to that being in a

0:17:08.200 --> 0:17:10.119
<v Speaker 1>straight line, they had the wave in them. Yeah, so

0:17:10.160 --> 0:17:12.320
<v Speaker 1>that's all due to surface waves. Surface waves are the

0:17:12.320 --> 0:17:14.720
<v Speaker 1>ones that caused the most damage as far as we're concerned.

0:17:15.040 --> 0:17:17.439
<v Speaker 1>If you're like, you know, a mole man or something,

0:17:17.720 --> 0:17:20.480
<v Speaker 1>you're probably going to be more afraid of secondary body

0:17:20.480 --> 0:17:24.040
<v Speaker 1>waves up top side. We're afraid of, you know, the

0:17:24.600 --> 0:17:26.960
<v Speaker 1>surface waves. The l waves are long waves is what

0:17:27.000 --> 0:17:29.760
<v Speaker 1>they're called as well, top top dwellers that we are, right,

0:17:29.800 --> 0:17:32.360
<v Speaker 1>so they caused the worst damage, and because they move

0:17:32.400 --> 0:17:34.160
<v Speaker 1>the earth up and down, like you said, a wave,

0:17:34.280 --> 0:17:37.800
<v Speaker 1>a water wave in the ocean, Yeah, exactly, which we don't.

0:17:37.840 --> 0:17:42.960
<v Speaker 1>We don't build our buildings generally to withstand wave like motion. No. Well,

0:17:43.000 --> 0:17:45.440
<v Speaker 1>they've done a lot of work though, to build buildings

0:17:45.440 --> 0:17:47.600
<v Speaker 1>that can rock back and forth and move a little

0:17:47.640 --> 0:17:51.399
<v Speaker 1>bit and have the foundation shift. It's called earthquake. What

0:17:51.480 --> 0:17:55.080
<v Speaker 1>we were talking about reinforcement. Sure, some of my apartments

0:17:55.080 --> 0:17:58.160
<v Speaker 1>in l A actually had were reinforced. You could tell,

0:17:58.160 --> 0:17:59.800
<v Speaker 1>like in the walls they would have these bars running

0:17:59.840 --> 0:18:01.920
<v Speaker 1>up in stuff. But yeah, as far as in the

0:18:02.040 --> 0:18:05.880
<v Speaker 1>Japan's on like the cutting edge of of earthquake proofing

0:18:05.920 --> 0:18:08.359
<v Speaker 1>of everything. Yeah, yeah, a lot of earthquakes in Japan.

0:18:08.480 --> 0:18:16.400
<v Speaker 1>Huh Yeah, and robots and volcanoes. Where are we now, Josh?

0:18:16.440 --> 0:18:18.159
<v Speaker 1>You want to talk about Richter scale yet or I

0:18:18.200 --> 0:18:21.520
<v Speaker 1>think that's the inevitable conclusion. So, Josh, the Richter scale

0:18:21.560 --> 0:18:24.960
<v Speaker 1>is uh, as most people know, records a magnitude of

0:18:24.960 --> 0:18:29.240
<v Speaker 1>the earthquake. Um. It's logarithmic, so that means that the

0:18:29.359 --> 0:18:32.119
<v Speaker 1>whole number jump means it increases tenfold. So a six

0:18:32.720 --> 0:18:34.800
<v Speaker 1>on the Richer scale is actually ten times as powerful

0:18:34.840 --> 0:18:37.600
<v Speaker 1>as the five, and the nine times as powerful as

0:18:37.600 --> 0:18:40.760
<v Speaker 1>the seven. How about that. Yeah, that's serious business. And

0:18:41.160 --> 0:18:43.760
<v Speaker 1>what the Richer scale does is it measures that that

0:18:43.920 --> 0:18:49.080
<v Speaker 1>wave amplitude of the seismic energy of a quake. And um,

0:18:49.160 --> 0:18:51.000
<v Speaker 1>so that's the one you always hear about, Like I

0:18:51.040 --> 0:18:52.840
<v Speaker 1>talked about that one in Pepua, New Guinea was a

0:18:52.920 --> 0:18:55.520
<v Speaker 1>six point seven, right, which is large. Anything below a

0:18:55.600 --> 0:18:58.200
<v Speaker 1>three generally doesn't get much attention. This is just a

0:18:58.200 --> 0:19:02.400
<v Speaker 1>little tremor my micro quake. It's kind of hard to say.

0:19:02.520 --> 0:19:05.640
<v Speaker 1>And that's the that's the vast majority of earthquakes or

0:19:06.000 --> 0:19:08.560
<v Speaker 1>three year less. Right. Yeah, you won't see anything below four.

0:19:08.600 --> 0:19:10.200
<v Speaker 1>You won't see a lot of damage going on. But

0:19:10.280 --> 0:19:13.720
<v Speaker 1>anything seven and above is a pretty serious business. And

0:19:13.720 --> 0:19:17.560
<v Speaker 1>then the record is a nine point five. I looked

0:19:17.560 --> 0:19:22.320
<v Speaker 1>this up nineteen sixty Chile. Right, you're ready for some

0:19:22.359 --> 0:19:24.920
<v Speaker 1>stats of my own? Look at you. I mean, imagine

0:19:24.920 --> 0:19:29.200
<v Speaker 1>at nine point five on the Richter's kill it's immense. Um,

0:19:29.320 --> 0:19:34.080
<v Speaker 1>there were sixteen hundred and sixty five people killed, three

0:19:34.080 --> 0:19:40.880
<v Speaker 1>thousand injured, in two hundred thousand homeless in Chile alone, um,

0:19:40.920 --> 0:19:44.520
<v Speaker 1>along with five hundred and fifty million dollars in damage

0:19:44.560 --> 0:19:49.760
<v Speaker 1>property damage nine sixty. So that's ninety that's the impression

0:19:49.800 --> 0:19:53.720
<v Speaker 1>I have you. Um, it created a tsunami that killed

0:19:53.800 --> 0:19:56.440
<v Speaker 1>sixty one people and caused seventy five million dollars with

0:19:56.520 --> 0:19:59.200
<v Speaker 1>the damage all the way in Hawaii, you're kidding, And

0:19:59.320 --> 0:20:01.680
<v Speaker 1>in Japan and there were a hundred and thirty eight

0:20:01.680 --> 0:20:05.399
<v Speaker 1>deaths and fifty million dollars worth of damage. Yeah, and

0:20:05.440 --> 0:20:07.280
<v Speaker 1>it just kind of goes on from there. You know,

0:20:07.280 --> 0:20:10.240
<v Speaker 1>what they said about that eighteen ten slash eleven earthquake

0:20:10.920 --> 0:20:14.320
<v Speaker 1>in Missouri was that they could the church bells in

0:20:14.359 --> 0:20:18.080
<v Speaker 1>Boston rang from the from the reverberation. I know that's nuts. Yeah,

0:20:18.160 --> 0:20:21.560
<v Speaker 1>I want to verify that. But big old earthquake right there.

0:20:22.240 --> 0:20:24.240
<v Speaker 1>So what you're talking about though, with the assessing the

0:20:24.320 --> 0:20:28.400
<v Speaker 1>damage that is actually the Mercali scale, the damage done

0:20:28.400 --> 0:20:31.560
<v Speaker 1>by the earthquake, which has figured out many days or

0:20:31.600 --> 0:20:34.119
<v Speaker 1>weeks later, not like the Richter scale. I call that

0:20:34.240 --> 0:20:40.000
<v Speaker 1>the y us God scale, right. Yeah, it's it's described

0:20:40.040 --> 0:20:43.600
<v Speaker 1>in Roman numerals up to twelve, which you can also

0:20:43.680 --> 0:20:47.000
<v Speaker 1>say is x I I and x i I is

0:20:47.040 --> 0:20:51.679
<v Speaker 1>where there um is evident structural damage. The ground is

0:20:51.680 --> 0:20:55.040
<v Speaker 1>opened up, sure like in the movies. Yeah. Um, and

0:20:55.400 --> 0:20:58.520
<v Speaker 1>there's been at least the tsunami or mudslide or some

0:20:58.560 --> 0:21:01.760
<v Speaker 1>other disaster. Yeah, my brother felt the earthquake when he

0:21:01.800 --> 0:21:05.960
<v Speaker 1>was in l A. Did he look handsome and much

0:21:05.960 --> 0:21:09.040
<v Speaker 1>more exciting things happen to him out there? His He

0:21:09.040 --> 0:21:10.879
<v Speaker 1>he said it felt like a buzzing, like a real

0:21:10.960 --> 0:21:12.639
<v Speaker 1>loud buzzing, and then he looked at his closet and

0:21:12.640 --> 0:21:15.600
<v Speaker 1>the clothes were shaking, and you know it's over then,

0:21:15.720 --> 0:21:17.080
<v Speaker 1>you know, as soon as you realize what's going on,

0:21:17.119 --> 0:21:19.600
<v Speaker 1>it's over. Yeah. I read about the nineteen o six

0:21:19.640 --> 0:21:22.960
<v Speaker 1>San Francisco earthquake. They said that the sensible duration of

0:21:23.000 --> 0:21:26.520
<v Speaker 1>the earthquake it was a minute really, which I imagine

0:21:26.520 --> 0:21:29.480
<v Speaker 1>probably felt like an hour, killed three thousand people. Well,

0:21:29.520 --> 0:21:31.359
<v Speaker 1>that's that just goes to show you the kind of

0:21:31.359 --> 0:21:34.119
<v Speaker 1>devastation if it only takes sixty seconds to wreak, that

0:21:34.160 --> 0:21:37.920
<v Speaker 1>kind of havoc what's going on and fires that broke

0:21:37.920 --> 0:21:45.680
<v Speaker 1>out after buildings collapsing, very scary stuff. So, Chuck, Well,

0:21:45.720 --> 0:21:48.320
<v Speaker 1>we can't predict earthquakes. We do need to close with that.

0:21:48.440 --> 0:21:51.679
<v Speaker 1>I think. Okay, they've come a long way and determining

0:21:52.000 --> 0:21:55.320
<v Speaker 1>the the epicenter, and they can predict after shocks pretty

0:21:55.320 --> 0:22:01.240
<v Speaker 1>well now, and they can say, hey, do you to history,

0:22:01.560 --> 0:22:03.680
<v Speaker 1>you you're likely to have an earthquake because we think

0:22:03.720 --> 0:22:06.320
<v Speaker 1>things are moving in your area. The plates may be moving,

0:22:06.359 --> 0:22:08.840
<v Speaker 1>but they can't accurately say when it's gonna happen. Yeah.

0:22:08.880 --> 0:22:12.320
<v Speaker 1>I remember being a little kid, and I think some

0:22:12.359 --> 0:22:14.840
<v Speaker 1>scientists came out and said, there's going to be a

0:22:14.880 --> 0:22:20.120
<v Speaker 1>massive earthquake and you know San Francisco or California that's

0:22:20.160 --> 0:22:22.600
<v Speaker 1>going to basically cause the state to break off. That's

0:22:22.600 --> 0:22:25.000
<v Speaker 1>a pretty fun thing. But they couldn't They couldn't say

0:22:25.000 --> 0:22:26.760
<v Speaker 1>when it was gonna happen. They said within the next

0:22:26.840 --> 0:22:30.680
<v Speaker 1>X number of decades. Scare a student day at your school. Yeah,

0:22:30.800 --> 0:22:32.920
<v Speaker 1>so if you have any relatives in California, they will

0:22:32.960 --> 0:22:36.000
<v Speaker 1>likely die. And I do have relatives in California too,

0:22:36.440 --> 0:22:39.640
<v Speaker 1>you did at the time. I still do. Hey, Aunt Barbe, Okay, yeah,

0:22:40.080 --> 0:22:43.320
<v Speaker 1>Aunt Barbe, Aunt Barbe, cousin just me and cousin Wolf

0:22:43.640 --> 0:22:47.680
<v Speaker 1>along with cousin Peter, cousin John, and I think that's

0:22:47.760 --> 0:22:51.920
<v Speaker 1>it out there. Oh and uh aunt Donna. Wow, yeah,

0:22:52.320 --> 0:22:56.160
<v Speaker 1>well they live in California. Wolf he actually you want

0:22:56.160 --> 0:22:58.119
<v Speaker 1>to know a wolf he story. This may or may

0:22:58.160 --> 0:23:00.320
<v Speaker 1>not make it in the final version. But I'll tell you, Chuck,

0:23:00.960 --> 0:23:05.560
<v Speaker 1>um cousin. Wolfe was born Eric Wolf right his first

0:23:05.640 --> 0:23:08.119
<v Speaker 1>middle name. When he was like eleven or twelve, he

0:23:08.160 --> 0:23:11.320
<v Speaker 1>decided he preferred the name wolf more. So he got

0:23:11.320 --> 0:23:13.879
<v Speaker 1>his parents permission and went down to the Clerk of

0:23:13.920 --> 0:23:17.040
<v Speaker 1>Courts and changed his name to Wolf Eric and he's

0:23:17.040 --> 0:23:21.600
<v Speaker 1>been Wolfie ever since. That's pretty funny. What a guy. Uh.

0:23:21.680 --> 0:23:24.120
<v Speaker 1>And then, um, I guess we already kind of talked

0:23:24.119 --> 0:23:28.879
<v Speaker 1>about building construction. Is when the uniform building putt came about,

0:23:28.920 --> 0:23:31.399
<v Speaker 1>and it's it's a set of standards basically two people

0:23:31.440 --> 0:23:34.199
<v Speaker 1>have to follow now, right, whether you're in fulsome prison

0:23:35.000 --> 0:23:40.520
<v Speaker 1>San Quentin, Japan, you gotta follow certain standards. Sure, oh yeah,

0:23:40.600 --> 0:23:44.640
<v Speaker 1>especially Chile. So that's earthquakes in a nutshell. And we're

0:23:44.680 --> 0:23:47.240
<v Speaker 1>not doing this one again unless they figure out that

0:23:47.280 --> 0:23:52.480
<v Speaker 1>the continental drift theory was complete rubbish, right yeah. Oh,

0:23:52.520 --> 0:23:54.719
<v Speaker 1>and also we should probably tell people, Chuck, there's an

0:23:54.800 --> 0:23:57.960
<v Speaker 1>article on how to survive an earthquake at how stuff

0:23:57.960 --> 0:24:00.800
<v Speaker 1>works dot com. You can type of five earthquake in

0:24:00.800 --> 0:24:03.320
<v Speaker 1>the handy search parts, save yourself a few keystrokes and

0:24:03.440 --> 0:24:05.720
<v Speaker 1>that will bring that right up. Good idea. And also

0:24:05.880 --> 0:24:08.040
<v Speaker 1>you can just type in earthquakes and I will also

0:24:08.119 --> 0:24:10.840
<v Speaker 1>bring up the how earthquakes work article with all those

0:24:10.880 --> 0:24:19.240
<v Speaker 1>super cool pictures. Right, yeah too, listener mail buddy, Okay, Josh,

0:24:19.240 --> 0:24:24.280
<v Speaker 1>I'm just gonna call this sleep paralysis deluge. It was

0:24:24.320 --> 0:24:27.840
<v Speaker 1>a deluge, wasn't it. Yeah, last well, it will be

0:24:27.920 --> 0:24:29.640
<v Speaker 1>last week now, a couple of weeks ago, probably when

0:24:29.640 --> 0:24:32.240
<v Speaker 1>this is released. We had a listener bail from drowsy

0:24:32.320 --> 0:24:36.359
<v Speaker 1>Dug in Oregon who had the pick suit man. He

0:24:36.560 --> 0:24:40.400
<v Speaker 1>was awake but couldn't move and very frightened and apparently

0:24:40.440 --> 0:24:42.280
<v Speaker 1>everyone on the face of the earth, and this is

0:24:42.320 --> 0:24:46.880
<v Speaker 1>sleep paralysis. But us and I had heard of sleep paralysis, uh,

0:24:47.200 --> 0:24:48.840
<v Speaker 1>never done a whole lot of research on it, but

0:24:49.080 --> 0:24:52.360
<v Speaker 1>rest assured we will do an episode on this now.

0:24:52.760 --> 0:24:55.480
<v Speaker 1>So here's the delusion of paper cup chuck. Yeah. Well,

0:24:55.480 --> 0:24:57.280
<v Speaker 1>I also want to say I did not respond to

0:24:57.320 --> 0:25:00.439
<v Speaker 1>any of those emails, and I am very sorry, but

0:25:00.480 --> 0:25:02.479
<v Speaker 1>we got literally over a hundred of them and I

0:25:02.520 --> 0:25:04.520
<v Speaker 1>just didn't have time. But it did read them, so

0:25:05.280 --> 0:25:08.040
<v Speaker 1>no offense people. And out of all the emails we

0:25:08.119 --> 0:25:12.240
<v Speaker 1>got about that one from medical and psychological professionals, I

0:25:12.320 --> 0:25:16.080
<v Speaker 1>went with Madeleine, our new thirteen year old fan because

0:25:16.119 --> 0:25:18.159
<v Speaker 1>hers was so good. Hey, guys that just listen to

0:25:18.200 --> 0:25:21.199
<v Speaker 1>your podcast with Drowsy Doug. It sounds like what happens

0:25:21.200 --> 0:25:23.360
<v Speaker 1>to me. I would be laying in bed and wake up.

0:25:23.760 --> 0:25:26.720
<v Speaker 1>Unfortunately I'm too lazy and tired to get up. But

0:25:26.800 --> 0:25:29.600
<v Speaker 1>then I would see things out of this world. Like

0:25:29.720 --> 0:25:32.719
<v Speaker 1>one time I woke up and I was too tired

0:25:32.720 --> 0:25:34.679
<v Speaker 1>to get up, and I saw it seems to be

0:25:34.680 --> 0:25:37.920
<v Speaker 1>a common thing, And I saw in my huge half

0:25:37.920 --> 0:25:42.240
<v Speaker 1>a sofa sized mirror my sister. Half her body was

0:25:42.320 --> 0:25:44.199
<v Speaker 1>in the mirror, frozen while the rest of her was

0:25:44.240 --> 0:25:48.800
<v Speaker 1>bending and moving around on my dresser. Awesome. Another time

0:25:48.840 --> 0:25:52.040
<v Speaker 1>I saw army guys getting pulled onto my roof. Please

0:25:52.080 --> 0:25:53.919
<v Speaker 1>don't give me any cures for this, because I like

0:25:54.040 --> 0:25:57.640
<v Speaker 1>seeing Navy seal guys climbing to my roof. So that's

0:25:57.680 --> 0:26:00.320
<v Speaker 1>from Madeleine, and Madeleine sounds like you my have a

0:26:00.320 --> 0:26:03.480
<v Speaker 1>little case of sleep paralysis. But as long as there's

0:26:03.520 --> 0:26:06.720
<v Speaker 1>no pig suited people or don't worry faces, we'll follow

0:26:06.760 --> 0:26:09.719
<v Speaker 1>up with the podcast on this and condition. And a

0:26:09.720 --> 0:26:11.280
<v Speaker 1>lot of people sounds like they have it. Actually a

0:26:11.280 --> 0:26:13.160
<v Speaker 1>lot of people that run in Yeah, they're right there

0:26:13.160 --> 0:26:17.120
<v Speaker 1>with Doug. Keep making these promises, don't you. Yeah, we'll

0:26:17.160 --> 0:26:20.040
<v Speaker 1>do it all right. Well, if you want to basically

0:26:20.160 --> 0:26:22.960
<v Speaker 1>boss chucking me around and get us to do a podcast,

0:26:23.480 --> 0:26:27.359
<v Speaker 1>send us your ideas to stuff podcast at how stuff

0:26:27.359 --> 0:26:34.439
<v Speaker 1>works dot com. For more on this and thousands of

0:26:34.480 --> 0:26:37.800
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0:26:37.880 --> 0:26:40.680
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0:26:40.720 --> 0:26:45.800
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