WEBVTT - Will California fall into the ocean?

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<v Speaker 1>Welcome to Stuff from the Science Lab from how stuff

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<v Speaker 1>works dot com. Hey guys, and welcome to the podcast.

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<v Speaker 1>This is Alison I don't know, the science editor at

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<v Speaker 1>how stuff works dot com. And this is Robert Lamb,

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<v Speaker 1>science writer at how stuff works dot com. And we're

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<v Speaker 1>kicking off with a letter right off the bat. We

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<v Speaker 1>sure are. And this letter comes to you compliments of

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<v Speaker 1>one of Florida Matt and Florida Matt recently wrote us

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<v Speaker 1>saying good morning Alison and Robert. My girlfriend is currently

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<v Speaker 1>going to college where one of her professors told her

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<v Speaker 1>there is a theory that one end that one day

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<v Speaker 1>the Santa's fault will split, plummeting the West Coast into

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<v Speaker 1>the ocean, never to be heard from again. I'm skeptical

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<v Speaker 1>about it, but I wanted to see what you had

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<v Speaker 1>to say. Thanks for your consideration, Love the podcast. Matt. Okay, Well,

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<v Speaker 1>you know this is actually a really popular idea, at

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<v Speaker 1>least I mean in terms of like pop culture references

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<v Speaker 1>to it. Yeah, it's it's out there, like like, were

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<v Speaker 1>you aware of it? Had you had you encountered this

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<v Speaker 1>anywhere in pop culture beforehand? A little bit? Yeah? How

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<v Speaker 1>about you? Yeah, mainly I was familiar with it out

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<v Speaker 1>because of like there's at least one Tool song that

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<v Speaker 1>makes reference to it a lot off of the Autuma album. Okay,

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<v Speaker 1>I'm not familiar with that one. Yeah that was from

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<v Speaker 1>back in uh in high school when that one came out, Uh,

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<v Speaker 1>really good album. But we put the call for Facebook

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<v Speaker 1>two people for people to come in on this y yeah,

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<v Speaker 1>because because I just remembered that one and I was like,

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<v Speaker 1>all right, well, what else is there? Because I know

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<v Speaker 1>it's a really common thing, right so um uh. This

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<v Speaker 1>guy Michael, who I went to high school with, by

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<v Speaker 1>the way, said Michael from high school. He said that

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<v Speaker 1>Jimmy Eats World song Blister had features it. Um. A

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<v Speaker 1>guy named John told us quote escape from l A

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<v Speaker 1>do you even have to ask? Also sometimes my dreams

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<v Speaker 1>Oh all right, so yeah, I guess he doesn't like CALLI. Um.

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<v Speaker 1>Heather Right mentions something called the End of the World.

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<v Speaker 1>It's like a flash cartoon on the internet. Um uh.

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<v Speaker 1>David mentions, uh the stand up comedy of Bill Hicks, um,

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<v Speaker 1>which I think was also referenced on the that Tool album. Um.

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<v Speaker 1>Valerie says, quote, I think there's a rancid song that

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<v Speaker 1>even adds an expletive between fall into the and ocean, So, um,

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<v Speaker 1>all right, I don't know what that expletive could be.

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<v Speaker 1>But and then, and then one of my favorites, Warren

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<v Speaker 1>Zyvon had a song called Desperadoes under the Eaves and

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<v Speaker 1>there's a part in it. I think it's in the

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<v Speaker 1>course where he's like, and if California falls into the ocean,

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<v Speaker 1>like the mystics and statistics say it will, Like that's

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<v Speaker 1>very nice, Robert, Well, thank you. Yeah. So, but that's

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<v Speaker 1>the thing. Do you do the other part of the

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<v Speaker 1>other big Warren Zevon song. Well, the weird thing is

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<v Speaker 1>it's like, do you think that's representative? Yes? And no?

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<v Speaker 1>Like I love that song, but like, you know, you

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<v Speaker 1>go out to karaoke, and I'm always I don't go

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<v Speaker 1>out to kara okay a lot, but when I do,

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<v Speaker 1>I always check out Warren's. Vanni is one of the

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<v Speaker 1>few artists that I like, Like, these are fun songs

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<v Speaker 1>to sing, right, but they almost always will just have

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<v Speaker 1>Werewolves of London, which is really more of us, Like

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<v Speaker 1>he's kind of talking in that song and it's not

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<v Speaker 1>really sung per se as fun as it is. And

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<v Speaker 1>he has so many other songs that are a lot

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<v Speaker 1>more you know, just a lot more fun to sing,

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<v Speaker 1>like Excitable Boy or or Desperadoes under the Eaves, you know.

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<v Speaker 1>So so yeah, and it's and he did so much

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<v Speaker 1>other work. That's great. So Callie and Warren's that's what

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<v Speaker 1>we bring to you today. So let's do a quick

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<v Speaker 1>refresher on earthquakes. Yeah, because that's what we're talking about.

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<v Speaker 1>That's what would cause California too, in theory, fall into

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<v Speaker 1>the ocean. Right now, that California sin that's going on

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<v Speaker 1>in Californization, but no California earthquakes. That's that's what we're

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<v Speaker 1>interested in. I just I was thinking about the Chili Peppers.

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<v Speaker 1>I was trying to think if they had referenced California

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<v Speaker 1>falling into the ocean. That's like, I don't think, I

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<v Speaker 1>guess not. I think I'm not that familiar with their work,

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<v Speaker 1>but I was a huge fan Mother's Milk No Never,

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<v Speaker 1>I mean I knew from the tracks off of it.

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<v Speaker 1>But but anyway, it's like nobody mentioned it on Facebook,

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<v Speaker 1>So alright, Facebook has to be right. So what's an

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<v Speaker 1>earthquake again? You guys know this, you're probably saying it

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<v Speaker 1>with us it's just really when the ground starts shaking

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<v Speaker 1>beneath your feet, and what does that cause? By shaking

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<v Speaker 1>is caused by a sudden motion in the in the

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<v Speaker 1>plates that are all around us in the Earth's cross

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<v Speaker 1>energy waves like moving through the cross. Right. Yeah, it's

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<v Speaker 1>pretty simple explanation. A rock jockey, you might tell you

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<v Speaker 1>something a little different, get a little bit more into detail.

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<v Speaker 1>And where do they happen? Right? So, earthquakes can happen

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<v Speaker 1>anywhere anywhere anywhere, well on Earth. True, it's not just Calie,

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<v Speaker 1>it's not just the famous Ring of Fire. Um. They

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<v Speaker 1>do tend to concentrate in three zones, according to the

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<v Speaker 1>United States Geological Survey. So first one, you guys are

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<v Speaker 1>going to know this one Pacific rim Ak, the Ring

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<v Speaker 1>of Fire, and that's responsible for more than eight percent

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<v Speaker 1>of earthquakes. Yeah, Johnny Cash wrote a song about it,

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<v Speaker 1>right he did. Are you gonna sing that too? Okay? Ah.

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<v Speaker 1>There's another belt called the Alpine and that's a found

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<v Speaker 1>in Indonesia and it kind of trails into the Atlantic.

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<v Speaker 1>And then there's a last belt that tracks the mid

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<v Speaker 1>Atlantic rich and it's underwater, so it's not the big one.

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<v Speaker 1>It's not the ram of Fire. We don't hear a

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<v Speaker 1>whole lot about that one. And it's important to note

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<v Speaker 1>too that you know, earthquakes on TV or the ones

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<v Speaker 1>that you know your friend is likely to tell you about,

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<v Speaker 1>you know, at dinner is something that you feel obviously,

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<v Speaker 1>but you don't always feel them. Sometimes they're so subtle

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<v Speaker 1>that you'd really have to have like some some actual

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<v Speaker 1>seismological you know, equipment to determine them. Yeah. Here in

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<v Speaker 1>Georgia we have them. There was one in August, fifth

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<v Speaker 1>magnitude two point two, so right, probably probably not too detectable.

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<v Speaker 1>The eppy center of that one was close to Millageville. Somehow,

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<v Speaker 1>I don't picture Millageville and Georgia being you know, it's

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<v Speaker 1>like Milan filosity. The earth quake capital isn't now where

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<v Speaker 1>that football scandal just went down. I think it was

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<v Speaker 1>m hm, no idea. Okay, So here's another earthquake term

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<v Speaker 1>that we should mention. Fault. Yes, when you're talking about earthquakes,

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<v Speaker 1>a lot of times you're talking about faults. And so

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<v Speaker 1>here's the quick definition for you, the quick, the quick

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<v Speaker 1>and dirty. It's a fracture, really um and it's a

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<v Speaker 1>fracture in the Earth. On either side of the Earth,

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<v Speaker 1>you're gonna have these blocks of crust and they're moving

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<v Speaker 1>relative to one another, parallel to the fracture. Yeah, it's

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<v Speaker 1>kind of like I always think of it when I

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<v Speaker 1>look at an actual skull, you know, like a human

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<v Speaker 1>skull or a model of the human skull, because they

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<v Speaker 1>don't do it a lot of just staring at real skulls.

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<v Speaker 1>But you know how like the skull is not one bone,

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<v Speaker 1>it's several and you can see the different lines where

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<v Speaker 1>they come together, and that's like the crust of the Earth. Well,

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<v Speaker 1>today we're going to talk mainly about the San Andrea's fault.

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<v Speaker 1>That's the big one, and it's it's really the boundary

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<v Speaker 1>between the North American and the Pacific plates, right, and

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<v Speaker 1>it's visible to the eye and that that's pretty cool

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<v Speaker 1>because most of the big faults aren't. Yeah, this one

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<v Speaker 1>is one you can you can to these really spectacular

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<v Speaker 1>you know, aerial shots of it, and it looks like

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<v Speaker 1>two massive, uh you know, chunks of of the the

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<v Speaker 1>Earth's surface are rubbing against each other and causing it

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<v Speaker 1>kind of looks like scar tissue, like geologic scar tissue,

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<v Speaker 1>and that's kind of what it is. Yeah, it's also

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<v Speaker 1>kind of like a truugh yeah in the earth. Like

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<v Speaker 1>if you've ever seen like Abdullah the butcher's forehead out,

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<v Speaker 1>throw that out to the wrestling fans. That's what it

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<v Speaker 1>looks like. It's like a gritty, starts, hard tissue. Something

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<v Speaker 1>else that's cool about the Santa Jay as well is, um,

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<v Speaker 1>you can literally straddle two plates, right and these these plates,

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<v Speaker 1>these tectonic plates we're talking about, are enormous, right, they

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<v Speaker 1>have a whole lot of land behind them or you know,

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<v Speaker 1>to the right and the left of them, if you're

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<v Speaker 1>going to think about it like that. Um, so near

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<v Speaker 1>the Santa Jeria's fault, you can find you can like

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<v Speaker 1>sit one ft on the North American plate, the other

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<v Speaker 1>foot on the Pacific plate like Hawaii, Japan, all of that.

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<v Speaker 1>So that's really cool. It reminds me of that spot

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<v Speaker 1>in the United States where the four Corners where you

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<v Speaker 1>can yeah yeah, yeah, where it's like, yeah, you get

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<v Speaker 1>all the touristy photos of in this state, right right.

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<v Speaker 1>So the San andre is specifically is a strike slip fault, okay,

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<v Speaker 1>and this is uh, this is where the two plates

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<v Speaker 1>are trying to push past each other. And if they

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<v Speaker 1>pass one another easily, it's no big deal, right, But

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<v Speaker 1>it's when they can't, when the plates are locked, that

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<v Speaker 1>tension builds up and boom, you get a big earthquake,

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<v Speaker 1>like I tend to think of like like if and

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<v Speaker 1>don't do this because you might you know, you don't

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<v Speaker 1>want to damage your enamel. But like when teeth are grinding,

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<v Speaker 1>you know, like grinding your teeth, and if you would

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<v Speaker 1>have put like so much pressure that you couldn't quite

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<v Speaker 1>grind them, you know where it's like earthquake in your mouth. Yeah, exactly.

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<v Speaker 1>That's what comes to mind when when we were looking

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<v Speaker 1>over all this stuff. Yeah, and it's not just a

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<v Speaker 1>strike slip fall. It's a right lateral strike slip. So

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<v Speaker 1>let's let's set this up for you. Let's say you're

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<v Speaker 1>standing on the North American Plate so um, with your

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<v Speaker 1>back to New York, and you're facing the Pacific Plate.

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<v Speaker 1>You're facing the Pacific Ocean. So the plate, the Pacific Plate,

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<v Speaker 1>with look like it's moving to the right. Okay, So

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<v Speaker 1>how much is it moving? That's the big question? Right, Well,

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<v Speaker 1>not not enough to really like you're not gonna notice it,

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<v Speaker 1>like if your house is on the fault line. You're

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<v Speaker 1>not gonna look at and be like, whoa, there is

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<v Speaker 1>a forest there yesterday. Now it's a desert, right, So yeah,

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<v Speaker 1>you're not really going to notice it because it's forty

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<v Speaker 1>six millimeters a year. That's hardly noticeable to us. But

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<v Speaker 1>you get a big great earthquake going on, like the

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<v Speaker 1>earthquake of nineteen o six, and you're gonna have some

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<v Speaker 1>pretty major offsets. So according to the U s G

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<v Speaker 1>S them, there was a road that wound up being

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<v Speaker 1>offset by one feet. Okay, well that's noticeable. It's definitely noticeable. Um,

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<v Speaker 1>the San Andrew's fault has been around for fifteen five

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<v Speaker 1>million years and it's experienced a creep of about miles.

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<v Speaker 1>That's about normal. It sounds like a lot, but yeah,

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<v Speaker 1>it is pretty normal. Yeah. And again we're talking about

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<v Speaker 1>the Pacific plate, the one that's um moving north with

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<v Speaker 1>respect to the North America, and it's got some southern

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<v Speaker 1>California on it, though not all of southern California, just

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<v Speaker 1>like it's like a tasty strip of it, you know. Yeah. Right,

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<v Speaker 1>So the Sant Andreas Fault, we haven't really told you, Um,

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<v Speaker 1>you know, some of its geographics specifics. Yeah, it's what long. Yeah,

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<v Speaker 1>it runs past San Francisco in the north all the

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<v Speaker 1>way up to Mendocino, and then to the south, it

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<v Speaker 1>runs past Los Angeles to the Sultan Sea, so roughly

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<v Speaker 1>echoes the California coastline for much of it, but as

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<v Speaker 1>you amble south along the fault zone, it moves more

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<v Speaker 1>inland and you know, dividing somewhat northern California from southern California.

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<v Speaker 1>Beneath the coast, the fault can reach up to ten

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<v Speaker 1>miles into the ground. Ten miles into the ground, So

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<v Speaker 1>it's deep, it is, and it's a It's another thing

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<v Speaker 1>to keep in mind here when you talk about, well

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<v Speaker 1>California fall into the ocean, is that the fall line

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<v Speaker 1>we're talking about is not like they didn't like put

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<v Speaker 1>the state boundary on the fall line or anything. It's

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<v Speaker 1>like not even close. It's uh, you know, it's a

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<v Speaker 1>good ways off. But I mean some parts of it

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<v Speaker 1>really do separate, you know, California from the ocean. I

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<v Speaker 1>mean it doesn't literally, but if you look at it

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<v Speaker 1>on an aerial of view or just in the geographic

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<v Speaker 1>boundary for sure, out in the northern part of it,

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<v Speaker 1>between California and the sea. But say between California and Arizona. No, No,

0:11:17.320 --> 0:11:19.360
<v Speaker 1>there's no fault line out there. I mean there's there's

0:11:19.400 --> 0:11:22.160
<v Speaker 1>no fault line dividing the two states. So with that

0:11:22.600 --> 0:11:25.600
<v Speaker 1>rather powerful fault line there in California, obviously there have

0:11:25.760 --> 0:11:28.640
<v Speaker 1>been some some pretty powerful earthquakes over time. Right, we're

0:11:28.679 --> 0:11:31.960
<v Speaker 1>talking about thousands of earthquakes occurring in California every year,

0:11:32.360 --> 0:11:34.920
<v Speaker 1>and in the San Andrea's fault zone is responsible for most.

0:11:35.800 --> 0:11:40.800
<v Speaker 1>So the first recorded California earthquake occurred in seventeen sixty nine. Um,

0:11:40.840 --> 0:11:45.000
<v Speaker 1>there was an expedition, the gaspar da Portola Expedition, that

0:11:45.080 --> 0:11:47.800
<v Speaker 1>was camped about thirty miles outside of Los Angeles, and

0:11:47.800 --> 0:11:54.880
<v Speaker 1>they reported it. They reported four severe shocks. Yeah. And

0:11:54.920 --> 0:11:57.040
<v Speaker 1>then the most famous and destructive was, of course the

0:11:57.080 --> 0:12:02.800
<v Speaker 1>ninety six earthquake, and that's technically April. Yeah, sir, this

0:12:02.880 --> 0:12:04.920
<v Speaker 1>was cool. The U. S g. S, as you guys

0:12:04.920 --> 0:12:08.320
<v Speaker 1>probably know, is just this amazing treasure trove of awesome info.

0:12:09.040 --> 0:12:11.960
<v Speaker 1>And um, they had a link to some eyewitness accounts

0:12:11.960 --> 0:12:14.280
<v Speaker 1>from that earthquake, so I wanted to read you part

0:12:14.280 --> 0:12:17.520
<v Speaker 1>of one. This is from John J. Conlin, who was

0:12:17.559 --> 0:12:19.800
<v Speaker 1>seven on the day of the great earthquake. Okay, are

0:12:19.800 --> 0:12:23.040
<v Speaker 1>you going to do this in like an old dude voice? Well, no, seven,

0:12:23.120 --> 0:12:27.600
<v Speaker 1>So well, I guess yeah. Well I'll give it my best,

0:12:27.720 --> 0:12:32.400
<v Speaker 1>my best attempt. Um. Okay. So there was never any

0:12:32.480 --> 0:12:35.280
<v Speaker 1>question in my mind as to the severity of the earthquake.

0:12:35.360 --> 0:12:38.840
<v Speaker 1>At five thirteen on that Wednesday morning, I was awakened

0:12:38.960 --> 0:12:41.160
<v Speaker 1>from a sound sleep by the shaking of my bed

0:12:41.240 --> 0:12:45.320
<v Speaker 1>and the house father heard it. Flossy. Flossy is this

0:12:45.360 --> 0:12:48.120
<v Speaker 1>woman who apparently assisted John J. Conlin's mom in case

0:12:48.120 --> 0:12:51.680
<v Speaker 1>you guys were wondering, So father hearded Flossy, my brother

0:12:51.679 --> 0:12:54.040
<v Speaker 1>and me into a doorway for protection in the event

0:12:54.080 --> 0:12:58.000
<v Speaker 1>the house collapsed. Actually it was only slightly damaged within moments.

0:12:58.080 --> 0:13:00.600
<v Speaker 1>During this period of the city's greatest in emergency, the

0:13:00.640 --> 0:13:03.400
<v Speaker 1>unusual silence of the alarm belt told its own story.

0:13:03.920 --> 0:13:06.560
<v Speaker 1>The system was destroyed, as was the functioning of the

0:13:06.559 --> 0:13:11.440
<v Speaker 1>city's thirty thousand telephones. For once and tragically, so the

0:13:11.520 --> 0:13:14.680
<v Speaker 1>cries of chapped victims for help generally refer to the

0:13:14.679 --> 0:13:18.840
<v Speaker 1>fire department for attention could not instantly activate rescue crews.

0:13:20.080 --> 0:13:23.160
<v Speaker 1>Conlin gives a lot more detail, but he winds up

0:13:23.280 --> 0:13:26.160
<v Speaker 1>ending with May the children of San Francisco or any

0:13:26.200 --> 0:13:29.880
<v Speaker 1>place never again enjoy such an experience as mine. But

0:13:29.920 --> 0:13:32.120
<v Speaker 1>the truth is earthquakes happen all the time, and big

0:13:32.160 --> 0:13:34.920
<v Speaker 1>ones happen all the time, and hundreds of thousands of people,

0:13:36.000 --> 0:13:37.679
<v Speaker 1>you know, wind up losing their lives. And by the way,

0:13:37.679 --> 0:13:40.920
<v Speaker 1>you mentioned standing under the doorway, and the US Geological

0:13:40.960 --> 0:13:43.400
<v Speaker 1>Survey points out that that's a rather, that's an outdated

0:13:43.480 --> 0:13:45.959
<v Speaker 1>notion that was based on the idea that in the

0:13:46.000 --> 0:13:48.960
<v Speaker 1>old days it would shake houses down and at times

0:13:49.000 --> 0:13:51.240
<v Speaker 1>that would be like the reinforced part of the house,

0:13:51.600 --> 0:13:53.160
<v Speaker 1>and so that would that would be some of it,

0:13:53.240 --> 0:13:55.360
<v Speaker 1>that would be what was still standing after the house

0:13:55.400 --> 0:13:57.960
<v Speaker 1>came down. But they say, don't do that. All right,

0:13:58.040 --> 0:14:00.800
<v Speaker 1>good information, Robert, So, I like we've given you guys

0:14:00.840 --> 0:14:02.920
<v Speaker 1>a lot of preamble to the question at hand. The

0:14:03.000 --> 0:14:05.880
<v Speaker 1>question posed in the podcast title is Calli're going to

0:14:05.960 --> 0:14:08.880
<v Speaker 1>fall into the ocean and it will No, No, it's not.

0:14:09.720 --> 0:14:12.040
<v Speaker 1>I read it wrong off the sheet. It's no, it's

0:14:12.080 --> 0:14:15.640
<v Speaker 1>not going to fall into the ocean. What up? Well,

0:14:15.679 --> 0:14:18.560
<v Speaker 1>because well, for several reasons. Well, first of all, it's again,

0:14:18.600 --> 0:14:20.400
<v Speaker 1>like we said, the fault line. Even if the fault

0:14:20.440 --> 0:14:23.560
<v Speaker 1>the fault line could magically have like the super magnitude

0:14:23.640 --> 0:14:27.280
<v Speaker 1>quake that could make the make part of it fall

0:14:27.280 --> 0:14:29.400
<v Speaker 1>into the ocean, it wouldn't be the whole state. And secondly,

0:14:29.760 --> 0:14:32.360
<v Speaker 1>the ocean isn't deep enough. It's not just this you know,

0:14:32.600 --> 0:14:36.120
<v Speaker 1>yawning hole and which we can throw entire states. Yeah,

0:14:36.160 --> 0:14:38.760
<v Speaker 1>it's and you know, you've seen the movie where like

0:14:38.760 --> 0:14:40.960
<v Speaker 1>the earthquake makes a big hole open up and stuff

0:14:41.000 --> 0:14:43.440
<v Speaker 1>falls into it and Superman is to save somebody or

0:14:43.480 --> 0:14:46.600
<v Speaker 1>you know, erroneous but cool. Yeah, Yeah, it's like that

0:14:46.640 --> 0:14:49.240
<v Speaker 1>doesn't happen. That's again we're talking about. Fault lines are

0:14:49.280 --> 0:14:52.200
<v Speaker 1>about things pushing together, grinding against each other, like your teeth.

0:14:52.200 --> 0:14:54.760
<v Speaker 1>You know, it's like they're grinding together, but they're they're

0:14:54.760 --> 0:14:58.040
<v Speaker 1>not opening up and rending the earth asunder. I just

0:14:58.080 --> 0:15:01.640
<v Speaker 1>love saying that rending the earth asunder. It feels very biblical. Yeah.

0:15:01.680 --> 0:15:03.760
<v Speaker 1>I think I used to have, like when was the kid,

0:15:03.760 --> 0:15:05.160
<v Speaker 1>that was like a Bible book and it had a

0:15:05.200 --> 0:15:07.880
<v Speaker 1>picture of somebody being swallowed up by the earth. Yeah,

0:15:07.920 --> 0:15:10.400
<v Speaker 1>so California is not going to be swept up to see,

0:15:11.000 --> 0:15:15.560
<v Speaker 1>but it is moving. It definitely is moving um compliments

0:15:15.600 --> 0:15:17.840
<v Speaker 1>of the two plates bumping up against each other in

0:15:17.880 --> 0:15:21.720
<v Speaker 1>the fault zone and seth Western California is moving slowly,

0:15:22.240 --> 0:15:25.520
<v Speaker 1>very slowly. Two inches per year is one that the

0:15:25.640 --> 0:15:30.160
<v Speaker 1>USGS provided towards Alaska, and it's sliding past central and

0:15:30.200 --> 0:15:34.320
<v Speaker 1>eastern California. And so you know, roughly fifteen million years

0:15:34.320 --> 0:15:38.600
<v Speaker 1>from now or so, Los Angeles and San Franciscan's will

0:15:38.640 --> 0:15:42.920
<v Speaker 1>be neighbors. That's pretty amazing. So the super evolved squid

0:15:43.200 --> 0:15:46.520
<v Speaker 1>that take over and live in Los Angeles, they will

0:15:46.520 --> 0:15:48.840
<v Speaker 1>be right next door to the super evolved cockroaches that

0:15:48.920 --> 0:15:52.400
<v Speaker 1>live in in San Francisco. Indeed, maybe I hope they

0:15:52.440 --> 0:15:58.440
<v Speaker 1>get along. Um Brinkley Seismological Lab is also an agreement

0:15:58.440 --> 0:16:00.840
<v Speaker 1>on this one, both of which are pretty good sources

0:16:00.880 --> 0:16:02.280
<v Speaker 1>for you guys to check out if you're interested in

0:16:02.320 --> 0:16:05.200
<v Speaker 1>exploring this more. And besides which, earthquakes are just really

0:16:05.200 --> 0:16:07.000
<v Speaker 1>interesting and the U s G s it is pretty

0:16:07.000 --> 0:16:08.720
<v Speaker 1>amazing when I guess and stuff, and we have a

0:16:08.760 --> 0:16:11.880
<v Speaker 1>good article on how earthquakes work. Did you work on one? No?

0:16:11.960 --> 0:16:14.480
<v Speaker 1>I did not. Maybe it was the brain. I think

0:16:14.480 --> 0:16:17.000
<v Speaker 1>the brain. I think it may have human at least

0:16:17.000 --> 0:16:19.120
<v Speaker 1>may have co authored that one. Yeah. Yeah, so that's

0:16:19.160 --> 0:16:21.040
<v Speaker 1>the answer to the question. It is moving, but no,

0:16:21.200 --> 0:16:22.960
<v Speaker 1>it's not going to be swept into the ocean because

0:16:23.360 --> 0:16:26.080
<v Speaker 1>the ocean is a landmass in itself, albeit one with

0:16:26.160 --> 0:16:28.400
<v Speaker 1>water on top of it. But it's it's just not

0:16:28.440 --> 0:16:30.720
<v Speaker 1>going to swallow up California. Yeah. I think people love

0:16:30.760 --> 0:16:32.760
<v Speaker 1>it though, because there's you know, people have a lot

0:16:32.840 --> 0:16:37.280
<v Speaker 1>of either hatred towards California. So this is feeling of yeah,

0:16:37.320 --> 0:16:39.440
<v Speaker 1>it should break off and be its own thing or

0:16:39.760 --> 0:16:43.480
<v Speaker 1>or you know, drowned in the ocean. So right, and

0:16:43.480 --> 0:16:46.480
<v Speaker 1>then there's a whole movement in California, you know, between

0:16:47.160 --> 0:16:51.280
<v Speaker 1>northern California and southern California and being a very different mindsets.

0:16:51.320 --> 0:16:53.800
<v Speaker 1>According to some residents, it feels very different in play.

0:16:53.840 --> 0:16:57.080
<v Speaker 1>I mean I just actually just got back from California.

0:16:57.160 --> 0:16:58.920
<v Speaker 1>My wife and I went on a vacation and we

0:16:59.000 --> 0:17:01.440
<v Speaker 1>got to see like Sam Cisco in l A. Took

0:17:01.520 --> 0:17:04.240
<v Speaker 1>us a lot longer to travel between the two you know,

0:17:05.040 --> 0:17:07.520
<v Speaker 1>two cities now than it will millions of years in

0:17:07.520 --> 0:17:10.960
<v Speaker 1>the future. But yeah, it's like like it's it feels

0:17:11.000 --> 0:17:13.639
<v Speaker 1>almost like a different state and it's a huge state. Yeah,

0:17:14.000 --> 0:17:18.040
<v Speaker 1>no doubt. My brother lives in San Franz. Yeah. So

0:17:18.240 --> 0:17:19.879
<v Speaker 1>thanks to Florida Mike for bringing that one to our

0:17:19.920 --> 0:17:23.080
<v Speaker 1>attention and for giving us inspiration for this podcast. Do

0:17:23.119 --> 0:17:28.119
<v Speaker 1>you want to do some listener mail Robert, Yeah, I've

0:17:28.160 --> 0:17:31.720
<v Speaker 1>got some more, UM, and it's a good podcast to

0:17:31.720 --> 0:17:34.240
<v Speaker 1>do this on, since the whole episodes came from a

0:17:34.359 --> 0:17:37.760
<v Speaker 1>listener mail. UM, we received an email and we were

0:17:37.840 --> 0:17:41.879
<v Speaker 1>both excited about this from uh Jenna, also known as

0:17:41.880 --> 0:17:45.399
<v Speaker 1>hookworm Girl by US listeners. I mean we don't call

0:17:45.440 --> 0:17:47.399
<v Speaker 1>her hook well, maybe we did call her girl. I

0:17:47.440 --> 0:17:51.959
<v Speaker 1>think you call um. She's lovely feet, she said us

0:17:51.960 --> 0:17:54.520
<v Speaker 1>a new pictures feet, new picture of her feet, and

0:17:55.000 --> 0:17:58.639
<v Speaker 1>yes they look. It's a complete turnaround from the parasite

0:17:58.640 --> 0:18:03.320
<v Speaker 1>infected uh things we saw before hookworms. You can see

0:18:03.320 --> 0:18:05.920
<v Speaker 1>the hookworm track center and the skin and her feet.

0:18:06.000 --> 0:18:08.160
<v Speaker 1>It was pretty awesome. Yeah, now they look they look

0:18:08.520 --> 0:18:12.000
<v Speaker 1>pedicured and you know, the the toenails are nice, twinkly

0:18:12.080 --> 0:18:15.760
<v Speaker 1>read and I'm very very healthy looking. And so anyways,

0:18:15.760 --> 0:18:17.880
<v Speaker 1>she wrote as in centensis picture and she says, this

0:18:17.960 --> 0:18:21.119
<v Speaker 1>is Jenna from Vancouver. I eat Hookworm Girl. Not to

0:18:21.160 --> 0:18:23.960
<v Speaker 1>be confused with the superhero, although although that might be

0:18:24.000 --> 0:18:26.919
<v Speaker 1>interesting and I agree. I just wanted to let you

0:18:26.920 --> 0:18:29.480
<v Speaker 1>know that I am so tickled pink every time I

0:18:29.520 --> 0:18:32.119
<v Speaker 1>hear my foot mention on your podcast. Here it is

0:18:32.119 --> 0:18:34.720
<v Speaker 1>getting another mention. I never would have dreamed that that

0:18:34.760 --> 0:18:36.919
<v Speaker 1>picture would have made such an impression. How could it not.

0:18:37.480 --> 0:18:40.520
<v Speaker 1>It's pretty gross picture to put your mind at ease,

0:18:40.560 --> 0:18:42.080
<v Speaker 1>I thought I would send you a more recent foot

0:18:42.119 --> 0:18:45.439
<v Speaker 1>picture and thank you again for the great podcast. I

0:18:45.480 --> 0:18:48.040
<v Speaker 1>work in a lab looking for new therapeutic strategies for

0:18:48.160 --> 0:18:51.640
<v Speaker 1>fighting tuberculosis, and sometimes the lack of progress being made

0:18:51.960 --> 0:18:55.000
<v Speaker 1>in antibotic research can be a little terrifying. On this note,

0:18:55.040 --> 0:18:58.200
<v Speaker 1>I would like to suggest a podcast on bacterial phage

0:18:58.240 --> 0:19:01.840
<v Speaker 1>based therapies. Yeah. I did a little research into it

0:19:01.920 --> 0:19:04.320
<v Speaker 1>after she sending her email, and I think we might

0:19:04.359 --> 0:19:06.280
<v Speaker 1>have to cover that. Although we have devoted a little

0:19:06.280 --> 0:19:08.439
<v Speaker 1>bit of time to bacteria recently with the whole quorum

0:19:08.480 --> 0:19:11.399
<v Speaker 1>sensing and the altruistic bacteria. Yeah, we've been hitting the

0:19:11.400 --> 0:19:15.960
<v Speaker 1>bacteria pretty hard. So so yeah, so anyway, thanks thanks

0:19:15.960 --> 0:19:18.600
<v Speaker 1>for letting us know that your your foot is better.

0:19:19.000 --> 0:19:22.240
<v Speaker 1>It's kind of become a u. The third member of

0:19:22.240 --> 0:19:27.000
<v Speaker 1>the podcast, yeahs foot, Josh writes, um, what's up stuff

0:19:27.000 --> 0:19:29.399
<v Speaker 1>from the science Lab. I was just listening to the

0:19:29.440 --> 0:19:32.439
<v Speaker 1>Wow Signal podcast in my car. I'm currently stopped not

0:19:32.520 --> 0:19:35.959
<v Speaker 1>emailing while driving good enough, and it reminded me of

0:19:36.000 --> 0:19:40.680
<v Speaker 1>a SETI phenomenon that a friend of mine caught potentially um.

0:19:40.720 --> 0:19:43.879
<v Speaker 1>It was around and a bunch of my nerdy friends

0:19:43.880 --> 0:19:46.000
<v Speaker 1>and I were enjoying running steady at home on our

0:19:46.000 --> 0:19:48.760
<v Speaker 1>computers as we're all a lot to do, you know,

0:19:48.800 --> 0:19:53.119
<v Speaker 1>and an evening. Uh. Generally, the data packets that you

0:19:53.160 --> 0:19:56.199
<v Speaker 1>would sift through just showed random noise. But for a

0:19:56.200 --> 0:19:58.679
<v Speaker 1>brief period during one day, a friend of mine was

0:19:58.720 --> 0:20:03.120
<v Speaker 1>receiving perfect waves. They were so perfect against the unusual

0:20:03.480 --> 0:20:06.600
<v Speaker 1>randomness that he shot a few emails with screenshots to

0:20:06.680 --> 0:20:09.480
<v Speaker 1>let Setty people know, UH to check check it out.

0:20:09.880 --> 0:20:11.680
<v Speaker 1>A week or so later, he got a cryptic email

0:20:11.720 --> 0:20:16.959
<v Speaker 1>back claiming some unusual interference from something suspicious and was

0:20:17.000 --> 0:20:21.040
<v Speaker 1>told just to disregard it. Perhaps just because this is

0:20:21.080 --> 0:20:23.439
<v Speaker 1>so awesome, this gives me, this is my new favorite

0:20:23.440 --> 0:20:27.720
<v Speaker 1>listener email. Just perhaps just because conspiracies are fun. We've

0:20:27.720 --> 0:20:29.920
<v Speaker 1>always held onto the belief that we just happened to

0:20:29.960 --> 0:20:32.520
<v Speaker 1>see something that they didn't want us to see. They

0:20:32.680 --> 0:20:35.800
<v Speaker 1>in caps all caps. No, I don't think he did

0:20:35.840 --> 0:20:37.800
<v Speaker 1>put it in all caps, but that's how I imagine it.

0:20:38.000 --> 0:20:40.920
<v Speaker 1>Of course, nothing has come of it in the intervening

0:20:40.960 --> 0:20:43.800
<v Speaker 1>eleven years, so who knows. I love your podcast more

0:20:43.840 --> 0:20:45.679
<v Speaker 1>than I can express, and I hastily written email on

0:20:45.720 --> 0:20:48.320
<v Speaker 1>my phone. It keeps me a company for the six

0:20:48.359 --> 0:20:50.200
<v Speaker 1>to eight hours I spend in the car every day.

0:20:50.280 --> 0:20:53.080
<v Speaker 1>Oh man, that's a long time. Please continue doing it forever.

0:20:53.400 --> 0:20:55.239
<v Speaker 1>We will do it at least as long as it

0:20:55.280 --> 0:20:59.119
<v Speaker 1>takes for Los Angeles to be creep right up to

0:20:59.119 --> 0:21:02.680
<v Speaker 1>San Francisco. So I mean, you knows from beyond the grave,

0:21:02.720 --> 0:21:05.280
<v Speaker 1>if you're really locking us in there, well, with all

0:21:05.280 --> 0:21:08.159
<v Speaker 1>that you know science going on, we could, you know,

0:21:08.200 --> 0:21:11.879
<v Speaker 1>we could live forever, Robert and record podcasts for more

0:21:11.960 --> 0:21:14.239
<v Speaker 1>on this and thousands of other topics. Is that how

0:21:14.280 --> 0:21:18.639
<v Speaker 1>stuff works dot Com? Want more house? We hope that's

0:21:17.480 --> 0:21:21.359
<v Speaker 1>a happy in your house. Tell us about cheery sperience

0:21:21.760 --> 0:21:27.360
<v Speaker 1>with earthquakes or um alien signals? Yeah, yeah, And we're

0:21:27.359 --> 0:21:29.919
<v Speaker 1>on science stuff at house to works dot com, and

0:21:30.040 --> 0:21:32.679
<v Speaker 1>of course on social networking. You can find us on

0:21:32.680 --> 0:21:35.560
<v Speaker 1>Facebook We're stuff from the Science Lab, and over on Twitter.

0:21:36.560 --> 0:21:39.439
<v Speaker 1>R l as a tweet master, so we're lap stuff.

0:21:39.840 --> 0:21:42.159
<v Speaker 1>So yeah, that's all we got today. Thanks for listening.