Science
Hoodoo and the Sh*tpots
In this episode of 'Geology on the Rocks,' hosts Jamie and Brian welcome special guest Kenneth J. Lazara for a lively discussion on science communication and Arizona geology. The episode fea...
Hoodoo and the Sh*tpots
Science •
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Interactive Transcript
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cup of makeup.
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What?
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That's not from the audience!
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I'm like,
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I don't want everything you say.
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Alright, welcome everyone to another episode of Geology on the Rock.
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You won't stop audio shop for all things rocks and rocking out.
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A brief overview of this evening's episode will include the intros and
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helloes, maybe a little new news question mark.
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Yes, yes, yes.
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So our main discussion will dive into science communication and Arizona
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geology.
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So between the bars of our main discussion will present to you another
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mineral minute.
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And before signing off, we will close things out with a little segment of
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that freaking rocks.
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That freaking rocks.
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Okay, so a big thank you to all of our listeners out there for allowing us to be
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played between your earballs and for spinning your time with us each week,
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months, years, whatevs.
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So if you would like to reach out to us, whether it be for episode ideas,
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questions you're wanting questioned or just to tell us about all the times we
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are wrong, you can reach out to us at Geology OTR at gmail.com or you can find us
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on the Instagram's geology on the rocks podcast.
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So it does look like as if things are squared away over here.
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So without further ado to all of you over there, I am your geology daddies.
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I am your host.
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I'm your hostie, woe'sty Jamie Whammy, the geology, geology daddy,
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wacky.
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And I'm your fancy, fancy Brian Gaggins.
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Say it like you mean it.
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Yes.
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I'm colluvial car.
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No, you know,
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come on.
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Come on.
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Come on.
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Little bit.
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Okay.
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Hot carless.
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All y'all are kidding me.
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Okay.
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So anyways, and this is geology on the rocks.
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Wow.
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All right.
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Well, hello everyone.
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Hi, episode 48.
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Okay.
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We're not cheers and yet.
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No.
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Okay.
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So, but we have something special for all of you listeners today.
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Let me queue up the music.
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And we welcome the one, the only one can only the Pasano from the old neighborhood.
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The beast from the
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Izano.
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Pisano, the kintanix.
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Kinley's are.
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Oh, fuck yeah.
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Fuck yeah.
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Slay up.
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So that was a personal request.
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This was a rib hintless by Slayers.
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I've always wanted to be introduced.
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I've always wanted to be introduced to Slayer.
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Yeah.
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You guys made better reality.
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We did.
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We were talking about when we were trying to find the song.
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We were like, it's like a WWE intro walk up song.
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It is.
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For real.
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Well, yeah.
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Thanks for coming on finally.
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Like James.
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I'm a big fan of Bobbibui.
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Bobbibui of big fan of you guys.
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Listen to you guys.
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I'm actually a listener before I ever even encountered you.
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Well, fun there.
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That's awesome.
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That's awesome.
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It's cool.
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Like that's how you make my long,
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too scared to fly travel work trips in the work trip.
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A little more powerful sometimes.
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Sometimes.
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Yeah.
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That's kind of like how Carly got started.
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She was like, she listened and then like, I don't know.
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It happened to be that she lived here.
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Yeah.
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And that's one thing led to another.
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So for our listeners out there, why don't you tell them just a little bit about who
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you really are?
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I don't know if you're actually you.
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Like we wouldn't know that.
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But unless your real name is Kintonix.
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But yeah.
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So that and also what you do and perhaps maybe what's your favorite sandwich?
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All right.
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Well, in a nutshell, I am Kenneth J.
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Lazara.
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The second.
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But you call me.
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Frickin Ken Ken.
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And I did my, I did a degree in geology at SUNY,
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Sony broke, uh, Sony broke University, Long Island, New York.
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Oh, makes sense.
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Why hear the accent now that you mentioned it?
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Yeah.
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He's on.
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Oh, you're going to, you're going to hear, you're going to get it.
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Don't worry.
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Uh, wow.
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What else?
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Favorite mineral mineral.
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It shouldn't be.
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It really should not be.
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But my favorite mineral is a rose.
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Really?
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Out of all of the minerals.
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Isn't it out of all, right?
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Well, the reason, uh, I mean, it's just so satisfying.
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You know, you look at this lush, deep, you know, pink thing.
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Yeah.
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And it's just so satisfying.
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And I actually, in my last girlfriend, I proposed to her with a piece of rose
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quartz that I found, uh, myself on top of a volcano.
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Under, under a solar eclipse.
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No.
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Okay.
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Well, now everyone looks back.
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Well, she still said no.
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Oh, well, that sucks.
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She's, well, that is, I guess, foreshadowing for proposing with rose quartz.
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Well, I mean, she was a flight attendant, right?
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Okay.
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I'm scared to fly and she scared of commitment.
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Oh, so there you go.
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Hey, old story.
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Anyway, is there a story behind the, the flight fright?
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Uh, not a happy one.
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Oh, well, we don't have to do it.
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I was in, I was in New York, you know, on 9 11.
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Oh, oh, no.
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Well, yeah, there you go.
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I have a really bad habit of bringing up that thing.
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Like, what did I do last time?
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I don't know.
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Oh, no, it was the levy breach.
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Oh, yeah, you're talking about your insensitivity to those who live in a floodplain.
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Yeah, it doesn't, they don't matter.
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That is not what I said for the record.
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Oh, we have it on record.
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Well, okay.
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No, yeah, that was a crazy time.
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I remember you.
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That was a, though the, the students I teach, like they were not, I guess, really conscious
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or aware of really, guess, the severity of 9 11.
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So it's kind of weird.
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It's kind of like our understanding, maybe of like Pearl, what harbor meant to our parents or grandparents?
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Absolutely.
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So it's absolutely.
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I hear the old timers talk and it's the same thing dynamic.
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Yes, we're the old timers now.
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But yeah, I know that.
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Ooh, yeah.
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I have a, and then plus, I don't know, there's a whole bunch of stuff in the news over the
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past week of how a Southwest flight, how a bird got caught in the engine during takeoff
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and the cabin filled with smoke.
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What?
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And they had to make an emergency.
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It happens all the time.
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Oh, what was the smoke in the cabin?
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I learned a lot of stuff, you know, spending five years with my last girlfriend, you know,
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there's like near what they call near miss, but it's like every day.
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Oh my God.
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Oh, Jesus.
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I'm done.
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I'm running and now I hate it.
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No, but then recently last week someone died from turbulence.
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Oh, okay.
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Well, you know, extreme turbulence.
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I mean, like, Carly and I are more like.
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They, they, they dropped like four months and telling you and hit her head and they love telling
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you, oh, it's just turbulence.
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It won't hurt you.
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Guess what?
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Now there's a one in a billion chance as well.
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Yeah.
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Well, I think the stat is you're still the odds of dying is one in 11 million.
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I'm still better than driving.
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Yeah.
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You know what?
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You know what?
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There's no fender benders.
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You tap a bumper up there.
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You don't just pull over.
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Oh, yeah.
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That is a true point.
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So it's Carly looks fucking terrified.
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Like, but I was just talking about this in one of my classes about risk and like talking
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about that kind of like the rationalization or I guess lack there of like, yeah, whenever
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we remember one plane crash, just 300 people died, but like the risk of like 300 car accidents
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with one people dying is it the same?
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Yeah, no, it's, but also like risk.
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So humans in general are overconfident.
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We will always say a probability is more or we'll, we'll mess that up.
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So we don't actually really have a good idea of how likely something is.
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And then also with that, so someone in a similar situation as you, you think your odds are
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better or more positive than someone else probably having worse luck.
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So you are a geologist and you're working out in Arizona.
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What kind of stuff do you do out there?
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I am in environmental consulting.
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I am a geologist in title, which really doesn't mean much more than sophisticated outdoorsy
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beer drinker.
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Yeah.
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But yeah, I do a lot of stuff with groundwater monitoring, modeling.
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What's your favorite pose?
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You know, park your back.
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Make it look like a duck lip.
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Make the kissy face.
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Oh my God.
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Okay, then lastly, our intrusive questions.
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What is your drink of choice?
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Wait, no, he didn't answer my sandwich question.
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Oh, yeah, I really want to know.
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My favorite sandwich.
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I think one of their names was Christine and the other was Rita.
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That was good.
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Are those hurricanes?
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I mean, maybe.
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Hurricane Rita.
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That was a bit after Katrina.
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Yeah, yeah.
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Little bit of monsoon.
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That's good.
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That's good.
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Okay.
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So, yeah, your drink of choice tonight, because you know, this is geology on the rocks.
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However, none of us may be Carly's on the rocks.
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No, none of us are on the rocks tonight.
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But we're emotionally.
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We're emotionally.
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We're emotionally.
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I'm on the rocks tonight.
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You know, lately I go to the store.
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The only thing I see in the beer aisle.
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I see a couple other bullshit, Budweiser, whatever.
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It's the rocket fuel, fucking IPA.
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All right.
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That's Brian.
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Right up right.
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I don't know what it is.
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I like IPA.
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Don't get me wrong.
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I enjoy it now and again.
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But I don't see why we need to stock the shelves.
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30 different brands of it.
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Hold on.
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I don't get it.
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I got something for that.
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Here we go.
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Yeah.
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Bring us.
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No need's IPA.
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We do need them, but we don't need a full aisle of IPAs.
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I've been going through an amber phase.
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Okay.
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So I've been fucking knocking back multiple times of amber.
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You know, that's right.
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Excellent.
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I made up.
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I made up red tonight.
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I am drinking a Ganafe brewing company out of New Mexico.
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Oh, yeah.
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Seven K IPA.
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Seven K.
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That's awesome.
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We had some of their stuff there.
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James.
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Oh, yeah.
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We're on that rooftop.
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Oh, yeah.
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That's fun.
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Yeah.
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Down in Las Vegas, New Mexico.
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Oh, no.
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What's it got?
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It was Las Vegas, New Mexico.
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No, no.
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We went to Santa Fe.
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Okay.
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Yeah.
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Well, I went drinking.
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I think you were with me.
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Maybe.
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I'd rather all squandering around.
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Well, I'm having a double half-life by Manhattan Brewing Project.
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And I'm having a car box.
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Love Street Blonde.
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They're local brewery, right?
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Carly.
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Yeah.
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So is this one.
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And Carly's.
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I'm having a raceling.
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So fancy.
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Is that what I have?
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Yeah.
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A reason.
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Okay.
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I called Carly.
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I was like, they don't have a raceling at the store.
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And then I walked and realized I'd fucking stand right in front of it.
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Okay.
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All right.
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It is, what time is it now?
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It's time for triple junction and mu moves.
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Yeah.
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So for triple junction fanfare, we, I don't think we've done this in a while.
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So Brian, you take the, you take the brunt of all of this or you're the, the chatty one.
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I'm actually the chatty one.
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But just a few fanfare notes.
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We enjoy the engagement with the fans.
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So igneous bliss and the CSU LA mineralogy class.
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Like they said, they listen to us.
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The UCSB Geofolks, Kavi from Australia, Rebecca, I forgot.
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Like the last, she gave us a bottle of whiskey.
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Oh.
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That we drink already.
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I'm Danielle with Daniela with UTSA, GSA, and geologically speaking.
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And you, a few trepisodes with Trey and local listeners Anna, I think recently.
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Yeah.
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Just crazy.
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And also shout out to Jessica Martin, she runs the GM Geofotos Instagram page, but she
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gave me some sand, very kind of her.
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But I'm using it for a research project I'm doing.
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And that's crazy.
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She was like, I'll go ahead.
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Sorry.
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They're, they're freaking awesome.
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That dude, geologically speaking.
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Oh, I know.
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They're in geofotos.
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I met Geo speaking in California and Stan Cometti last year, October 21.
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He fucking bad ass.
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He was listening, you're fucking bad ass.
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Sorry.
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He is though, because like, he just, like, I don't know.
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I don't understand how someone can understand that much of the geology.
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Like I, I mean, I think I know a little bit, but I get out in the field and I'm like,
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what?
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And then what I was going to say, and I, but we've probably talked about this before.
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But the J and Geofotos, she was once my student, the physical geology.
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Yeah.
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So it's crazy.
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And now she's at UTA.
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Yes.
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Working under the guy.
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I'm going to study under.
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So it's like, yeah, so, yeah.
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So I guess we went through it.
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We do have fans and all that.
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We're going to try to do something nice for our listeners and provide some job posts.
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I mean, I'm not going to call through them.
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I, I, that's up for you guys.
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If you're interested in a job to really seek it out and see what it's about, but thanks
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to rock girls only, don't know their name.
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But yeah, they had, they have a few jobs that they had mentioned, and I'll make sure and
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get those up soon.
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And then we also throwing around maybe like a, like a networking event or not.
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Or just kind of like a meet and greet.
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Hopefully that could lead into something like a local geology community.
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Yeah.
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Go do field trips and just meet other geologists.
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I met a geologist today who graduated from UTA in 1974.
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Wow.
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Who is it?
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You know, it is Angela's nephew's grandfather.
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Oh, okay.
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And he was talking about, well, a mailbox money.
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Okay.
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And then obviously, Kentonix, like, right?
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We, I mean, no, we wouldn't be having this episode if it wasn't through the Instagram
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and his listening.
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So, yeah, man.
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Yeah.
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And the audience would like to see more fun videos starring James and Brian created by
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Carly.
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Okay.
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So the audience has asked for this.
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Has it really?
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They have.
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Is this like a personal behind the screen, like an iron door, the audience?
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It sounds like this is like Brian, what I'm, what I'm hearing when she says this and what
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I'm visioning in my head is that we need to make a calendar.
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I have, I mentioned that to Ken.
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I said, we should, he should do a geology.
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What would it, I don't know what that was, but it was like a sexy mangeologist.
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Like, oh, I thought you met like a calendar.
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Like we should actually schedule things.
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Oh, we do have that.
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Don't we?
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I thought we did.
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No, I meant like a, yeah, like if you want, I thought I was going to get to do my arch
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back and back.
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Oh, yes.
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I just, I can envision like photoshopping myself into different landscapes for the different
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months.
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Oh my God.
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Yes.
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He's a lot of them.
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No, it just came to me.
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Oh, okay.
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All right.
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Well, I think it's now time for one of my favorite segments.
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Oh, but the fault factoid segment.
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Oh, yeah.
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So, so Ken, you had an idea.
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I can give you, I'm in a unique position here to give you direct feedback.
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Oh, yeah.
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Instead of you, instead of you having to wait for emails from your ungrateful listeners,
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you've got one right here.
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I'm grateful.
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I like this.
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That's so good.
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I suggest you, is that you guys are two mineralogy patrologists.
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You need to throw in some, you need to throw in some structure.
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Okay.
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A fault, fault factoid segment.
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Fault.
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Fault.
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Fault.
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Let's see, but like the, the sound it makes as it slips.
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Oh, that was really dirty.
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You pick a fault somewhere in the world.
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Okay.
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You just, you just got, you just got this relative motion.
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It's likely potential for whatever magnitude or click.
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It's effect on regional morphology.
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You know, there's a lot you can do.
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In a minute, you could fill a minute easily.
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See, this is a lot.
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I was just thinking of like, okay, this is a normal fault.
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The fault, the hanging wall moves down relative to the full wall.
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No, but that's a good idea.
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That's a good idea.
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That's even, that's more just a random fault throughout the world.
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I like it.
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And we called it not my fault.
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Yeah.
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Oh, so good.
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There you go.
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Okay.
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All right.
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We're going to write that down.
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Write that down.
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Okay.
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Well, then I, we will go into, and please, Ken, at any time, if you have anything to say
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about any of the new news, please feel free to, I guess just fit in.
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Get in where you fit in.
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So this is trying to be as rude as possible.
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I hope so.
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So new news, article one.
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So I know we've talked about this before, but it's about Earth's inner, inner core.
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And there was a new paper that was released.
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And then the scientific American talked about it in February of 2023.
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So it's about the paper discussing the possibility of having to potentially, it has the potential
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for us to reimagine our understanding of the Earth's core, right?
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I guess more on the physical side, right?
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Because if it's the chemical differentiation, it's just core.
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Yeah.
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I agree.
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But okay.
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So recent research suggests that the Earth's inner core may have an inner core of its own.
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So the inner most part of the inner core is believed to be a solid sphere made of iron
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and nickel, but scientists have now found that this region may have a distinct inner core.
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And this new research proposes that the inner core of the Earth may consist of two layers
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with the outer layer being made up of the iron, nickel alloy.
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And the inner one actually being made up of different materials that may have higher melting
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points than the outer core.
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And then the scientists suggest that the second layer could be composed of various materials
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such as iron, carbon, and silicon.
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But more research is needed to determine the exact composition, right?
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Because we don't have a way to actually look into it.
spk_0
So the research suggests that the Earth's inner core may have an inner core, and was
spk_0
based on the analysis of seismic waves, which are just the vibrations that travel through
spk_0
the Earth's interior.
spk_0
And then the seismic waves are produced by earthquakes and other sources, and they provide
spk_0
scientists with information about the structure and composition.
spk_0
And by studying how the seismic waves propagate through the inner core scientists confer properties
spk_0
of its density and elasticity.
spk_0
And in this case, they analyze the seismic waves that had traveled through the inner core
spk_0
and found that they exhibited a certain pattern of polarizations, which could be explained
spk_0
by the existence of the inner inner core with different properties than the outer part
spk_0
of the inner core.
spk_0
And then the hypothesis will still require further investigation and testing through
spk_0
a range of techniques.
spk_0
However, this discovery of the inner core with the Earth's inner core could have significant
spk_0
implications for our understanding of the planet's magnetic field and the processes that
spk_0
drive it.
spk_0
And then the scientists in the study also believe that the motion of the liquid, iron,
spk_0
in the outer core generates Earth's magnetic field, but the inner core is believed to play
spk_0
a role in regulating the magnetic field's strength and stability.
spk_0
So by better understanding the inner core's structure, scientists begin insight into how
spk_0
the Earth's magnetic field has evolved over time and how it may change in the future.
spk_0
Wow.
spk_0
Yeah, I saw there was a huge buzz about that last month.
spk_0
Interesting that, I mean, it makes sense, like all the iron, carbon, and silicon, I think
spk_0
that makes a lot of sense, considering what the asteroid belt's composed of.
spk_0
spk_0
So if there, maybe that's just the early stage of formation and, you know, I don't know.
spk_0
Like, I'm not a planetary geologist.
spk_0
It makes sense to me.
spk_0
I don't.
spk_0
Yeah.
spk_0
I believed you.
spk_0
Well, I don't like the music played while I thought.
spk_0
Oh, yeah, if you get this one.
spk_0
Oh, the thing that strikes fear the most is that there are no notes here.
spk_0
I just have a picture to go off of.
spk_0
So last week I talked about an observation made of certain insects that would fling their
spk_0
pee at super propulsive velocity with their stylus.
spk_0
Yes.
spk_0
Well, I'm going to continue this.
spk_0
I do that over time.
spk_0
Of course you do.
spk_0
Okay.
spk_0
Well, this lady, like wrote this bug guy, this is an entomologist.
spk_0
Entomologist.
spk_0
Yeah.
spk_0
Hold on, hold on, hold on, hold on.
spk_0
So I don't look at entomology ever, right?
spk_0
Yeah.
spk_0
So this is just really weird.
spk_0
We always hear those stories like is Facebook listening, right?
spk_0
So I just yesterday, no, I don't look up entomology.
spk_0
Anything, right?
spk_0
Me and my niece were talking about it yesterday in person because she's like super into
spk_0
entomology and she's part of the entomology club at her school and talking about that.
spk_0
And she found all these bugs.
spk_0
The first ad that pulls up on my Facebook is join this entomology group.
spk_0
Wow.
spk_0
And I was like, whoa, they got the word.
spk_0
I'm like, that's super weird.
spk_0
There's nothing in my search that will face that to it.
spk_0
Not cool.
spk_0
That's why I don't have a Facebook.
spk_0
Not really.
spk_0
Well, not necessarily.
spk_0
Is that why?
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Maybe.
spk_0
I don't know.
spk_0
Well, so this lady, this week, I want to talk about a lady that found a beetle that honestly
spk_0
looks like a mix of a tardigrade and like an assassin bug.
spk_0
But she was like, hey, like, he just has a really weird end to him.
spk_0
And she wrote this entomologist.
spk_0
And he discovered that it's this one type of beetle called a tortoise beetle.
spk_0
The reason it looks so odd is it has this rear appendage.
spk_0
And the whole shabang is called a fecal shield.
spk_0
And so basically this larva of this beetle, it starts shedding its own skin and it's poop,
spk_0
which I guess is called frass.
spk_0
And so, assassin frass.
spk_0
And it basically has this thing called an anal fork that it's where it's where it's
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served.
spk_0
Is that for eating ass?
spk_0
It's got to be, right?
spk_0
That's good.
spk_0
Oh, I'm like, well, yeah.
spk_0
And so, yeah, anal fork, start fresh.
spk_0
That's like a great slogan for, never mind.
spk_0
Okay.
spk_0
That's my, that's my happy metal banding.
spk_0
It's it.
spk_0
Awesome.
spk_0
Well, okay.
spk_0
So basically, they figured out that this beetle will armor itself with its poop.
spk_0
And that's how it wards off other predators because like spiders and ants because they can
spk_0
tell when there's poop and they don't really want to mess with that.
spk_0
Fair.
spk_0
So there you go.
spk_0
It works.
spk_0
It even works among our feet.
spk_0
I think it probably does.
spk_0
Yeah.
spk_0
Like, bring out the poo.
spk_0
Once I bring out the poo, all my enemies run.
spk_0
And let's throw into that.
spk_0
Did you, did you do that or did I do that?
spk_0
I just put that in there.
spk_0
Okay.
spk_0
Okay.
spk_0
I know what the hell your door is.
spk_0
There it is.
spk_0
There's the armored poop.
spk_0
Wow.
spk_0
Yeah.
spk_0
It's not very good.
spk_0
What a cutie.
spk_0
That does, I mean, other than the load of shit on its back.
spk_0
Is that the fork?
spk_0
That's gotta be.
spk_0
That's the shield.
spk_0
Oh.
spk_0
That's the poop shield.
spk_0
Okay.
spk_0
There's my life science update.
spk_0
All right.
spk_0
Do I get the music too?
spk_0
Yeah.
spk_0
Yeah.
spk_0
Let's do this.
spk_0
Build to last.
spk_0
Oh.
spk_0
Okay.
spk_0
I think this was gonna be one of our...
spk_0
In honor of Women's History Month, I'm gonna share this story that I've read from
spk_0
MPR about Emerald Mining in Columbia.
spk_0
So the gist of it is that Emerald Mining used to be very dangerous.
spk_0
I mean, Columbia.
spk_0
And there were Columbian families and they were fighting for control, all that stuff.
spk_0
And there were accidents, you know, in the mines, all that good stuff.
spk_0
So in the article, it doesn't say who, like, what organization or whatnot.
spk_0
But someone asked this guy working at the US Embassy in Columbia to get some foreign
spk_0
investors going.
spk_0
And then those investors helped change it.
spk_0
Helped change it.
spk_0
So instead of like having an open mine, so there were accidents and then it polluted
spk_0
nearby waters.
spk_0
Okay.
spk_0
So it's an open mine not having an open mine.
spk_0
Correct.
spk_0
Yeah.
spk_0
Yeah.
spk_0
So now there are tunnels.
spk_0
You can go down into the tunnels, several meters deep.
spk_0
So now it's eco-friendly.
spk_0
But the great part about all of it in addition to all the happy things is that this Columbian
spk_0
Emerald Mining area is now a pioneer for bringing women into the workforce.
spk_0
So there are several women geologists there, several women doing the mining.
spk_0
So I just thought that was really cool.
spk_0
And I'm sure there's more conflict and other things going on that the article didn't
spk_0
mention.
spk_0
But in the article, it did say like women used to be like, you know, like women on a ship,
spk_0
bad luck, dangerous.
spk_0
You can't have them anywhere near here.
spk_0
And now it's like one of the big places in Columbia hiring women.
spk_0
So that's cool.
spk_0
Yeah.
spk_0
No, it is.
spk_0
And then I'm sure like that industry will have the growth, you know, I guess when you
spk_0
introduce women into an industry like, I don't know, but he sure that it's.
spk_0
Yeah.
spk_0
So I think that's awesome.
spk_0
And I also love me some good barrel.
spk_0
Oh, yeah.
spk_0
Emerald too.
spk_0
Variation of barrel.
spk_0
No, thanks for that, Carly.
spk_0
And yeah, so anytime Brian.
spk_0
Yeah.
spk_0
I really want to make sure that I hope that the future is very equality based.
spk_0
And I think we're at least to like where I'm working.
spk_0
It's there, but that is not the case everywhere and we need to improve.
spk_0
Okay.
spk_0
So we have Ken on here, Ken Tonics.
spk_0
And I just want to say I actually think I found your page before maybe before you found
spk_0
hours.
spk_0
I'm not sure.
spk_0
But I just remember seeing, you know, these outstanding landscape photos and of geology.
spk_0
And I was like, okay, well, I kind of looked into it.
spk_0
And then I didn't get.
spk_0
I was like, oh my God, this is hilarious.
spk_0
And so I realized that there, I couldn't tell if this was, you know, just this guy's
spk_0
page that, you know, he was just doing this because he liked it.
spk_0
Or if it was a science communication thing.
spk_0
And I don't know if that's how it ended up, but it seems to be a really successful thing
spk_0
for you.
spk_0
But I do want to do something.
spk_0
I want to read one of your posts on here.
spk_0
If that's okay.
spk_0
Oh, yeah.
spk_0
Mind your, mind your plosives.
spk_0
Okay.
spk_0
All right.
spk_0
And this one I think is actually about, yeah, from Crater Mountain.
spk_0
So there's this area.
spk_0
Can you read it in your Brian voice?
spk_0
What's my Brian voice?
spk_0
You know, the one I need to read.
spk_0
I know the one you're about to read.
spk_0
Yeah.
spk_0
Like laughing to myself.
spk_0
Exactly.
spk_0
All right.
spk_0
Stories that Brian reads from Ken Tonics.
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There you go.
spk_0
Instagry.
spk_0
I give the credit.
spk_0
What?
spk_0
My feed is the best geology blog on Instagram.
spk_0
True yet is.
spk_0
But don't worry.
spk_0
I'm humble about it.
spk_0
There's something here for all of you, even the snobs who pretend I don't exist because
spk_0
I'm better, stronger, faster, wielding some of the most dazzling kung fu that they've
spk_0
ever witnessed.
spk_0
but it can be our little secret that I said,
spk_0
tiktotic shit, traveling can't get tenure geologist,
spk_0
talking trash about people, A. Cleachay 101,
spk_0
regurgitating crappologist.
spk_0
Here is where it's at.
spk_0
Owens Valley, at least I think,
spk_0
has the coolest feature I've ever seen in my entire life.
spk_0
An oblique normal ride lateral fault
spk_0
offsetting quaternary of the flows,
spk_0
which issued forth from crater mountain in the background.
spk_0
Dude, here is the proof you need.
spk_0
You can't glue fault shut.
spk_0
Duck tape won't solve this one.
spk_0
Okay, crater mountain is part of the greater
spk_0
big pine volcanic field,
spk_0
and which here is erupted basalt
spk_0
in basaltic andesite lava onto the floor of Owens Valley.
spk_0
The Owens Valley fault last ruptured about 7.9 million years ago
spk_0
back in, nope, sorry, 7.9 magnitude back in 1872,
spk_0
producing about 18 to 20 feet of offset
spk_0
with normal and right lateral movement over 30 miles.
spk_0
Dude, how far is this from the San Andreas fault?
spk_0
Like a couple of hundred miles,
spk_0
including entire sear and avadas,
spk_0
and still the stress on the earth here
spk_0
is mostly lateral.
spk_0
Dude, this is the transition zone
spk_0
between the tiktonant regime of the San Andreas
spk_0
and the basin and range province.
spk_0
Such a thing is the product of strained partitioning.
spk_0
In other words, the San Andreas fault is not weak enough
spk_0
to accommodate all the movement between the North American
spk_0
plate and the Pacific plate.
spk_0
In addition, the sear and avada mountains are mostly granite.
spk_0
I really like this part.
spk_0
Granite is a mesh of interlocking crystals,
spk_0
and it really, which really does not want to break.
spk_0
Thus, the real plate boundary is much more diffuse.
spk_0
Some even think that this is the site of the plate boundary
spk_0
and the San Andreas fault will become deactivated.
spk_0
Dude, welcome to the best geology blog on Instagram.
spk_0
Give me my price.
spk_0
Boom, boom.
spk_0
And so I read these things and I was like, man,
spk_0
I actually just learned a lot from reading that.
spk_0
And I'm not a student,
spk_0
and I still learned a ton from that.
spk_0
But it was hilarious.
spk_0
And so I immediately gravitated that to that.
spk_0
So did you mean for this to take off
spk_0
or was this just a...
spk_0
If you were to dig way deep into my first few posts
spk_0
on Instagram, it was just kind of,
spk_0
here's me hiking, here's fucking food on meeting.
spk_0
You know, there was just nothing to it.
spk_0
But I started meeting and it blew my mind
spk_0
because I didn't know there were more of us.
spk_0
I started meeting other geologists on there.
spk_0
I think the first person I met is Susan Laura.
spk_0
She goes by geologists on board.
spk_0
And we started talking shop about this and that.
spk_0
We met up a few times over the years.
spk_0
And I started really getting into it.
spk_0
And it's really started.
spk_0
All right, so I'm doing slightly more
spk_0
than just looking at half naked Brazilian women all day.
spk_0
I'm not.
spk_0
I'm actually using social networking to social networks.
spk_0
So I'm meeting with professors, other hikers,
spk_0
other photographers.
spk_0
Everybody who can possibly be remotely connected
spk_0
to thing that I do.
spk_0
And with all the travel that I do,
spk_0
I have people across the country.
spk_0
In December, I met up with somebody
spk_0
over at the Everglades National Park.
spk_0
You know, I met people in Seattle.
spk_0
I met the guy who co-authored
spk_0
or he was probably the principal author
spk_0
of the roadside geologist, Washington.
spk_0
Wow.
spk_0
It's been a tremendously enabling feature for me
spk_0
to just keep staying involved,
spk_0
and keep going, and keep learning.
spk_0
Mostly I would say it's,
spk_0
I'm not making money doing this.
spk_0
It's mostly just for my satisfaction, you know,
spk_0
what I want to do in my life.
spk_0
It enables me to make my contribution, you know,
spk_0
because the space is working environmental control.
spk_0
I'm not inventing any of this stuff.
spk_0
I'm not discovering this stuff,
spk_0
but I'm more or less thinking,
spk_0
here's this cool thing I found,
spk_0
I just thought, you know.
spk_0
No, right.
spk_0
And what I want to say when I hear in that is too,
spk_0
is like, it's, you're not,
spk_0
this is, it's not passive, right?
spk_0
So like, you can be a passive recipient
spk_0
of this information, but someone is just passively
spk_0
taking this in, being like,
spk_0
these are cool pictures,
spk_0
and I'm learning something,
spk_0
but like on your end,
spk_0
it's very active and engaging, right?
spk_0
So you're actually, it's a meaningful,
spk_0
I guess medium, like what you're doing, right?
spk_0
I mean, I guess what we're all doing in all of this too
spk_0
is the engagement is equally as important
spk_0
as the content that's being created.
spk_0
Right.
spk_0
And I would say that my speed,
spk_0
probably half art, half science,
spk_0
like, you know, I'm dealing with as much photography
spk_0
as I am hard data.
spk_0
I guess I got that influence for my mom with an artist,
spk_0
my dad was a physics professor,
spk_0
and me, I'm just kind of like,
spk_0
toward my best brain, my right brain, you know,
spk_0
a cub war,
spk_0
and the reason these posts are so long,
spk_0
because I only ever post one up on the elliptical machine.
spk_0
spk_0
Wow.
spk_0
Oh my god.
spk_0
I run about an hour a day,
spk_0
and it's most fucking boring thing on earth.
spk_0
So I spend my time writing these long,
spk_0
you know, long-winded posts,
spk_0
and I try, you know, I try to make it fun,
spk_0
try to make it sort of obnoxious, funny,
spk_0
but sort of factually accurate.
spk_0
Yes, you could say I'm like the good will hunting
spk_0
of geology, I don't know.
spk_0
No, yeah, and I think it's trouble.
spk_0
And I would say to that,
spk_0
like I think humor is a very big important part of,
spk_0
like kind of, with all of that,
spk_0
because Brian and I, we gave a talk, right?
spk_0
And we talked about like the humor that we bring in
spk_0
with kind of the podcast to make it not.
spk_0
So I mean, make it more relatable and tangible,
spk_0
and I don't know,
spk_0
then just the coldness that sometimes you get
spk_0
from reading an article, right?
spk_0
How can we interject ourselves into it a little bit more?
spk_0
And maybe inspire a new generation of someone
spk_0
that maybe didn't even think about geology or science
spk_0
in such a way.
spk_0
Yeah, and we're not all lab coats and...
spk_0
Yeah, well, science doesn't say the most,
spk_0
it's not true.
spk_0
I know.
spk_0
But I think that it,
spk_0
what I like about science communication,
spk_0
because it can be something you,
spk_0
like there are people that only do that,
spk_0
but it can be a hobby that you're still being helpful
spk_0
while entertaining yourself,
spk_0
and learning and sharpening your tools, right?
spk_0
Because I think, you know,
spk_0
there may be someone that reads your post,
spk_0
can or listens to one of our episodes,
spk_0
it's like, you know what?
spk_0
I've been thinking about whether or not to do geology.
spk_0
I think I'm starting to see that maybe that's something
spk_0
I want to do or not.
spk_0
Maybe they're like,
spk_0
fuck no, I'm not doing that.
spk_0
Look at these.
spk_0
Yeah.
spk_0
There's people, there's a lot.
spk_0
I get what I get a lot of,
spk_0
are people who went into something else,
spk_0
but they absolutely loved geology.
spk_0
spk_0
And so, you know,
spk_0
they're sitting there miserable,
spk_0
and they're office doing accounting.
spk_0
Well, they, you know, they read my post,
spk_0
and they have questions.
spk_0
I get a lot of really good feedback from those people.
spk_0
Yeah.
spk_0
So, one of my favorite people to meet up with,
spk_0
in person is undergrad,
spk_0
because they're just so into it.
spk_0
So, you know, period.
spk_0
spk_0
That, yeah, no less cocky good God.
spk_0
Like, I don't know about you,
spk_0
but dealing with other like industry geologists,
spk_0
it's just like,
spk_0
or what's worse as engineers,
spk_0
but they're just fucking cocky.
spk_0
And it's like, okay,
spk_0
well, who's dick is bigger at this site?
spk_0
And it's like,
spk_0
you all gotta cut this out.
spk_0
Well, you're is on.
spk_0
That's the mentality though.
spk_0
You're like, no.
spk_0
Yeah.
spk_0
But that's the mentality.
spk_0
And it's just like,
spk_0
here we fucking go again.
spk_0
Like, you can see the guy that walks out.
spk_0
The women are usually cool.
spk_0
And they're like,
spk_0
being fucking helpful,
spk_0
and actually entertaining the problem that we need to solve.
spk_0
And there's always this fucking asshole
spk_0
that walks out on the field.
spk_0
And he's just like,
spk_0
all right,
spk_0
like who's gonna challenge me?
spk_0
It's like,
spk_0
motherfucker.
spk_0
But yeah, no, you, you,
spk_0
the interesting thing is like,
spk_0
another overlap is like,
spk_0
with the podcast and undergraduate geology students,
spk_0
like that's who it seems like.
spk_0
It does seem like.
spk_0
It's like,
spk_0
yeah, that and other creators.
spk_0
Well, I was, yeah,
spk_0
I was just gonna say like,
spk_0
just to speak to it all from my end,
spk_0
because I'm kind of on the other end of it all.
spk_0
And like I had mentioned,
spk_0
you know, I read that one book,
spk_0
and it just got me crazy thinking about geology,
spk_0
and then stumbled upon you guys,
spk_0
and then there's posts like Kins
spk_0
that just keep that curiosity and imagination just going.
spk_0
And so I think to me,
spk_0
that's one of the cool things about it.
spk_0
And like you said,
spk_0
you just keep learning.
spk_0
You're a continual learner.
spk_0
Yeah, I would say that as much as I am speaking,
spk_0
I'm probably learning,
spk_0
tenfold that amount.
spk_0
Yeah, yeah, same.
spk_0
Well, Ken, so you do this for fun
spk_0
while you're doing other field work, is that correct?
spk_0
Yeah, so I travel a lot for work.
spk_0
I'm frequently in Southern California,
spk_0
New Mexico, like I said,
spk_0
I've been to Seattle twice last year.
spk_0
I went to my end Florida.
spk_0
I'm all over the place.
spk_0
I was even in New York, Alabama, all over.
spk_0
And so I'm a big time hyper.
spk_0
And that's really where it becomes possible to do all this.
spk_0
Everywhere I go, I look up, you know, local hikes that I can do.
spk_0
And I always bring my everywhere I go,
spk_0
I bring my car, you know, half the time I do this.
spk_0
I don't even know what I'm looking at when I'm there.
spk_0
I just take a million pictures.
spk_0
And then I start looking it up, you know,
spk_0
when I get home and try to see if I can correlate
spk_0
what I've shot with, you know,
spk_0
what is documented for the region.
spk_0
I feel like that's a very nice thing that, like you've just said,
spk_0
because it kind of lets, you know,
spk_0
let's say those undergrads that are listening,
spk_0
you don't have to know everything right away.
spk_0
Yeah, man, I don't know anything.
spk_0
You know, I find out that's the more I know,
spk_0
the less understanding I have or I have more understanding.
spk_0
But it also enables you,
spk_0
averagingologists to make an unbiased observation, right?
spk_0
So you're sitting there, you're looking at these, you know,
spk_0
cross-bending structures that have some laminar feature on them.
spk_0
And you can sort of ponder it, put it together in your head
spk_0
and then prove or disprove yourself
spk_0
when you're looking up the data later.
spk_0
Or maybe you disagree, maybe you disagree
spk_0
with the technical report, you know?
spk_0
Yeah, and I think that's a good thing for listeners too.
spk_0
I mean, that are interested in geology
spk_0
or are young budding geologists,
spk_0
it's like, look at something,
spk_0
but try to come up with like three or four different explanations
spk_0
to explain it again.
spk_0
Is there are multiple ways to arrive at it?
spk_0
And, you know, the more that you can like tease out,
spk_0
like kind of like, well, this could be a possibility,
spk_0
this could be a possibility.
spk_0
You're honing your skills on what it could be indifferent.
spk_0
You're allowing yourself to allow for the possibility
spk_0
of it being more than just one way.
spk_0
Yeah, and also like, no matter even if you decide not to go
spk_0
a certain path with explaining something,
spk_0
whatever explanation is,
spk_0
you should write down these linear thoughts.
spk_0
Like, what did you start observing at the beginning
spk_0
and then what were your interpretations?
spk_0
What did you, you know, cross stuff out,
spk_0
like make a note, oh, no, I'm not going this path
spk_0
because X, Y, whatever.
spk_0
There is no way that you go out in the field
spk_0
and you're already going to answer the questions right then.
spk_0
So you need all of that background,
spk_0
you're cognitive awareness the entire time.
spk_0
There is a lot, a lot of data to work over
spk_0
before you make any, any decision about anything that it is.
spk_0
Absolutely.
spk_0
That's why the project's budget people for longer than a day.
spk_0
Right. Like, yep.
spk_0
Yeah, so would you say that this is something like you'd like
spk_0
to pursue further?
spk_0
So let's say someone like offers you, I don't know,
spk_0
a social media contract and you know,
spk_0
other such things?
spk_0
Yes, like they will say, okay, like let's say,
spk_0
REI comes to you and they're like, okay,
spk_0
put as you do your geology stuff, put this backpack
spk_0
in one of your posts.
spk_0
Would you do that?
spk_0
Like drop your job.
spk_0
Uh, you know, I'm kind of, I've been,
spk_0
I have been approached for different
spk_0
than you advertise this for that.
spk_0
And I feel like I will just hemorrhage my story.
spk_0
I feel like the authenticity of my feed is, you know,
spk_0
I'm doing this as a genuine person with genuinely no
spk_0
selfishness.
spk_0
I think that if I were to somehow attract the attention
spk_0
of some professor out there who thinks I would be a good candidate
spk_0
for, you know, a graduate role, you know, please reach out
spk_0
to me.
spk_0
Outside of that, I really, you know, I'm gainfully employed.
spk_0
I'm looking at my house hunting right now.
spk_0
I'm not, I'm not hurting for, you know, petty cash
spk_0
to sell somebody a fucking backpack.
spk_0
Yeah, I don't, I don't think REI is going to buy your house.
spk_0
Maybe you could blossom.
spk_0
I mean, you could blossom in like,
spk_0
I, and another thing is, another thing is national,
spk_0
national geographic doesn't return my phone call.
spk_0
Oh, but there was, I don't know.
spk_0
Your photo of the ship pot is pretty damn good.
spk_0
So, yeah.
spk_0
So, yeah, I know like your call for a graduate school,
spk_0
like I just want to just again throw it out there.
spk_0
If anybody is knows anybody, how to get to Antarctica,
spk_0
like I'm more than willing to sell myself
spk_0
all together.
spk_0
Yeah, I can't.
spk_0
So I need to get on a research project with somebody.
spk_0
Cool.
spk_0
Are boats safer than planes?
spk_0
I don't know.
spk_0
I have to be better.
spk_0
You have to take an airplane to get,
spk_0
I think South America or Australia to take a ship there.
spk_0
But anyways, let me know if anybody's going.
spk_0
Okay, so while I'm not going to ask you to marry me, Ken,
spk_0
but so can you, so you do have a backpack?
spk_0
You said a text break.
spk_0
So, because I'm married to Brian, obviously,
spk_0
and he's right in front of you.
spk_0
But so you're a photographer.
spk_0
So can you explain just a little bit about your process
spk_0
of setting up your shot?
spk_0
So like there's a, do you have an idea that you have
spk_0
and try to capture that?
spk_0
Because I know this is a silly question
spk_0
that you said that you go hiking, you bring your camera.
spk_0
But do you see something and then try to capture that moment
spk_0
if that makes sense?
spk_0
Or is it a, I guess, somewhere in between?
spk_0
And then also will follow up to that would be
spk_0
like the camera setting.
spk_0
So, you know, like the, the shit, like the,
spk_0
it's foreign language to me.
spk_0
Like when you talk about like the ISO, the lens,
spk_0
focal depth, exposure, blah, blah, blah, blah.
spk_0
So it's impressive like the, the outcome.
spk_0
Because you have to envision it's at some point
spk_0
in setting up shots, I heard is important.
spk_0
That's like, you're asking him to give us secrets.
spk_0
No, no, no, no, no.
spk_0
That's like, hey, what reverb setting
spk_0
are you using on this track?
spk_0
Well, I mean, like that shit's foreign language to me.
spk_0
Like if I could, I'd do that.
spk_0
I would do it.
spk_0
But like, well, you don't make it into like your exact settings.
spk_0
But is it, do you have it set up in your head?
spk_0
How you want it to be?
spk_0
Or is it just kind of like, I'm gonna capture it.
spk_0
And it is, it is 100% unique for every situation.
spk_0
Okay.
spk_0
But there are, there are some constant.
spk_0
I never, I don't care how, how shitty it turns out.
spk_0
I will never shoot above ISO 100.
spk_0
Because the higher you bump that ISO up,
spk_0
the more draining the image gets.
spk_0
Okay.
spk_0
So is that, can you tell for the non-camera people,
spk_0
like me, what the hell in ISO is?
spk_0
And ISO, institutional standards or something, I don't know.
spk_0
It's an international standard for the cameras
spk_0
sensitivity to light.
spk_0
So increasing that enables you to collect more light,
spk_0
but not as a function of, you know, the lens view.
spk_0
So it just increases the, the sensors sensitivity to light,
spk_0
not the amount of light.
spk_0
So a lot of times you lose data in the form of greening
spk_0
that you start kicking up.
spk_0
A lot of wildlife photographers, you know,
spk_0
because animals are moving around a lot.
spk_0
And they have to shoot at super fast,
spk_0
shutters, we'll tend to kick up the ISO
spk_0
and do some noise reduction post processing
spk_0
to get that sharp image.
spk_0
But I'm photographing fucking rock.
spk_0
I don't need to deal with, I don't need to deal with,
spk_0
you know, ISO.
spk_0
So I keep it at 100.
spk_0
That's a pretty standard number for photography.
spk_0
Yeah, because I'm, oh no, yeah, because like,
spk_0
then would you keep it, I guess, you would lengthen
spk_0
that to if you were, or I guess that would be the,
spk_0
how long you keep it open, like the,
spk_0
those nighttime photographers where they get like the,
spk_0
you can get the movement of them.
spk_0
You keep it on a tripod or something, I don't know.
spk_0
The problem with that, and this is the downside
spk_0
of what I do it is because I'm hiking.
spk_0
A lot of times, a lot of times I just don't take my tripod
spk_0
because I just don't want to carry it.
spk_0
I don't want to wait.
spk_0
If I'm doing a short thing, then the,
spk_0
and you know, absolutely, if I'm trying to do milky way
spk_0
or, you know, stars and stuff like that,
spk_0
yeah, you definitely need a tripod from that.
spk_0
I also shoot in a, a, a setting that we call exposure bracket.
spk_0
So my camera, when I press the,
spk_0
the picture button, it shoots a five round burst of photos
spk_0
at different shutter speeds.
spk_0
So there'll be one super fast shutter speed,
spk_0
and there'll be one super slow shutter speed.
spk_0
And what I do is I take it to my computer later,
spk_0
I merge all those five pictures into one,
spk_0
and it enables me to get much greater control
spk_0
over the shadows in the highlights.
spk_0
So you don't have this big white blotch
spk_0
that, you know, blows out one side of the photo.
spk_0
You have nice, you know, visible shadows,
spk_0
or, and it presents you from getting these black, you know,
spk_0
useless shadows while you have, you know,
spk_0
nice detail and clouds.
spk_0
So it enables me to work on every aspect of the image
spk_0
of all in one shot.
spk_0
Yeah.
spk_0
So you're basically creating the mean
spk_0
out of your sample set.
spk_0
That's kind of cool.
spk_0
Right.
spk_0
Yeah.
spk_0
So, so you're doing this.
spk_0
Sometimes I, what I picture is,
spk_0
I know you do this while hiking,
spk_0
but I'm thinking you're like a rogue theology employee
spk_0
and you're like, I'm gonna take pictures while that work.
spk_0
So I, and so it spawned me darn.
spk_0
Yeah, and I went to, I do.
spk_0
Yeah, you're terrible at your travel.
spk_0
Yeah, mine are like on my iPhone and the normal one.
spk_0
So, but I want to know, you and I are both,
spk_0
at least part of the time, field geologist.
spk_0
What's the worst field disaster that you either caused?
spk_0
We'll scratch that.
spk_0
Witnessed.
spk_0
Yeah, witness.
spk_0
Let's go with witness.
spk_0
I won't throw you under the bus.
spk_0
Well, one of the jobs, the last job I had before my current job,
spk_0
we were doing groundwater injections
spk_0
through either monitoring or dedicated injection well,
spk_0
meaning we're pumping solutions into the aquifer.
spk_0
Yeah.
spk_0
And a lot of times you have the well that you don't have
spk_0
the right fitting to hook up to them.
spk_0
I hope your injection closes up to them.
spk_0
You have to use what they call a packer.
spk_0
Okay, yeah, I know what it's called.
spk_0
Right, so a packer is this inflatable bladder
spk_0
that you lower to a certain depth in the well and inflate it
spk_0
and you start injecting, you know, throw it
spk_0
and it prevents everything from coming up out of the way.
spk_0
Because you're forcing everything to go into the formation.
spk_0
So, we were just named the co-worker,
spk_0
fucking asshole, by the way.
spk_0
We were going to go ahead and name drop him?
spk_0
Sure.
spk_0
I told him, don't fuck Steven,
spk_0
don't fuck Steven.
spk_0
Don't get me wrong, we're still friends.
spk_0
We still go out for beers, but we're in the trailer.
spk_0
That's good, sir.
spk_0
That's awesome.
spk_0
We're in the trailer monitoring, you know, pressure,
spk_0
flow rate, you know, how much it has left in the tank
spk_0
before we make the new tank of solutions.
spk_0
And also in the pressure just dropped almost to zero.
spk_0
We went down to like 20 PSI and we were injecting it.
spk_0
60, yeah, that was good.
spk_0
So we just, we did this thing where we just look at each other.
spk_0
Didn't have to say we're run out there.
spk_0
And then we just see this fucking balloon coming up
spk_0
out of the well, inflating, inflating.
spk_0
And this is like half inch rubber, okay?
spk_0
So this thing, and we had it set, you know,
spk_0
our cut off or on the air compressor was like 60 PSI,
spk_0
but we're not getting 60 PS.
spk_0
There's no limit.
spk_0
So this thing is just inflating, inflating,
spk_0
and then she says to me, this is why he's an asshole.
spk_0
He says to me, go turn off the compressor.
spk_0
Compressor's sitting there right next to this thing
spk_0
that's blowing up.
spk_0
Sorry.
spk_0
Sorry.
spk_0
Turn around.
spk_0
I said to him, mother fucker, you go turn around.
spk_0
For real?
spk_0
Turn off a split second later.
spk_0
Wow.
spk_0
Boom.
spk_0
We exploded.
spk_0
Let me tell you something.
spk_0
The biggest piece that we found was like the size
spk_0
of a fingernail.
spk_0
Huh?
spk_0
There were holes in the fucking wall.
spk_0
I was just gonna, right now it,
spk_0
there's the vegetation, all the vegetation surrounding
spk_0
the well, like, like, boom.
spk_0
It was like, go turn off the compressor.
spk_0
What the fuck?
spk_0
Wow.
spk_0
Okay, that's pretty bad.
spk_0
So I have a rubber joke.
spk_0
Oh yeah.
spk_0
What do condoms and rattlesnakes have in common?
spk_0
I don't fuck with either.
spk_0
You've literally told this joke.
spk_0
So I gotta tell my rubber joke that I've said
spk_0
directly after you've told that joke.
spk_0
What did the condoms say when it flew across the room?
spk_0
Or wait, why?
spk_0
Sorry.
spk_0
Why did the condom fly across the room?
spk_0
It was pissed off.
spk_0
I know them.
spk_0
spk_0
I'm not wrong.
spk_0
I'm not wrong.
spk_0
Did your bug friends tell you that joke?
spk_0
They tell me lots of things.
spk_0
Jesus.
spk_0
Oh yeah.
spk_0
That's pretty bad.
spk_0
Yeah, intense.
spk_0
Oh my God.
spk_0
All right, so I think before we go any further,
spk_0
we should appease the, what do you call them?
spk_0
Australians.
spk_0
Well, I don't know.
spk_0
I'd pay the sponsor.
spk_0
Oh yeah, we got it.
spk_0
So this is where we're going to insert a sponsor.
spk_0
Bip, bip.
spk_0
And now we're going to do a little bit of mineral.
spk_0
Oh yeah.
spk_0
Mineral minutes.
spk_0
Mineral.
spk_0
Mineral.
spk_0
Mineral.
spk_0
Mineral.
spk_0
spk_0
Mineral.
spk_0
All right.
spk_0
So this week's mineral mineral is brought to you by the new
spk_0
and improved titanium silver gold anti-mony,
spk_0
anti-mony, soulful salt, thunder bayite.
spk_0
Thunder bayite's chemical formula is TI-AG3AU.
spk_0
AU3SV7S.
spk_0
spk_0
Oh, I got it.
spk_0
Thunder bayite is black in color.
spk_0
And also a straight splack.
spk_0
And...
spk_0
AAH!
spk_0
AAH!
spk_0
AAH!
spk_0
AAH!
spk_0
Oh God.
spk_0
Thunder bayite has a hardness of three.
spk_0
The hardness scale.
spk_0
Hmm, that thunder now.
spk_0
Yeah, basically.
spk_0
Thunder bayite has no observable cleavage
spk_0
and has an irregular to uneven fracture.
spk_0
Right, and thunder bayite has a density of 5.693
spk_0
grams per cubic centimeter.
spk_0
And that is calculated.
spk_0
Thunder bayite is weekly anyostrophic.
spk_0
And I stro-
spk_0
And I stro-
spk_0
And I stro-
spk_0
And I stro-
spk_0
And I stro-
spk_0
And I stro-
spk_0
There's gonna be words later on.
spk_0
And I don't wanna say.
spk_0
To light blue rotation, tense.
spk_0
Oh!
spk_0
Thunder bayite has weak cleocroism
spk_0
and appears gray in the busted light.
spk_0
Reflective percentages for the forecom-
spk_0
Commissioned on order meteorology wavelengths.
spk_0
AR.
spk_0
AR.
spk_0
AR, men.
spk_0
AR, max, AR.
spk_0
37.9.
spk_0
38.4.
spk_0
4.
spk_0
171.1 nanometers.
spk_0
35.336.
spk_0
548.3.
spk_0
There's 33.934.4.
spk_0
586.6 nanometers.
spk_0
And 32.5652.3 nanometers respectively.
spk_0
I want you to repeat.
spk_0
What does that mean?
spk_0
Oh no.
spk_0
Thunder bayites mean of five electron micropros-
spk_0
Analyses gave silver.
spk_0
14.9116.
spk_0
Um, are you 27.4022?
spk_0
Titanium.
spk_0
Titanium 9.379.
spk_0
Antimony.
spk_0
Antimony.
spk_0
I like Antimony.
spk_0
SB.
spk_0
30.39.84.
spk_0
And silver.
spk_0
Silver.
spk_0
Silver.
spk_0
spk_0
You already said silver.
spk_0
Silver.
spk_0
8.61.7 for a total of 100.9.
spk_0
0.09.
spk_0
0.09.
spk_0
Um, percent.
spk_0
Wait, percent.
spk_0
Wait, percent.
spk_0
Corresponding on the basis of a total of 20 atoms to...
spk_0
Don't worry about that.
spk_0
Don't sing that.
spk_0
So Thunder Bayite is part of the tri-clinic crystal system.
spk_0
And in the crystal class of one, aka, padeal.
spk_0
He's like, let me give it easy.
spk_0
I'm like, tell.
spk_0
Because I edit it.
spk_0
You don't, don't read that one.
spk_0
Come on.
spk_0
I was just being a dick.
spk_0
He could do it.
spk_0
I know he can.
spk_0
All right.
spk_0
Here we go.
spk_0
Thunder Bayite's base group is p1 with the 8.0882.
spk_0
5.
spk_0
Uh, b equals 7.8492.
spk_0
5.
spk_0
d equals 20 point 0.0781.
spk_0
Thanks for your thanks.
spk_0
Thanks for your thanks.
spk_0
Thanks for your time.
spk_0
Oh, thanks for your time.
spk_0
And 9.
spk_0
Alpha equals 9.2.518, 5.
spk_0
Beta equals 93.7395.
spk_0
Gamma equals 90 point 0.086 degrees.
spk_0
Those are all the three.
spk_0
I know.
spk_0
We don't know.
spk_0
B equals 1, 2, 7, 0.739.
spk_0
And the Z-clinic is that cubic?
spk_0
Oh, that's volume.
spk_0
It's an extreme.
spk_0
You don't know how to hyper.
spk_0
We don't hyper here.
spk_0
Z equals 2.
spk_0
And that's where I said, mal, give me something else.
spk_0
Thunder Bayite's 5 strongest powder diffraction lines.
spk_0
D and angstrom.
spk_0
What?
spk_0
That's a capital I.
spk_0
I over I zero.
spk_0
And then fuck this up.
spk_0
What is HK?
spk_0
Oh, I know what HK is.
spk_0
I do know.
spk_0
I'm not going to go into that.
spk_0
That's the crystallography stuff.
spk_0
This is all crystallography.
spk_0
Yeah, our 4.04 on the 1.00 and 2.00 plane.
spk_0
3.92.
spk_0
I don't know.
spk_0
That is 80 point.
spk_0
Yeah, we got a lot of numbers here.
spk_0
And then it ends with the number seven.
spk_0
Thunder Bayite's type locality is from the Himalow gold deposit.
spk_0
Bomby, township, thunder bay district, Ontario, Kanada.
spk_0
I'll be there on Thursday.
spk_0
I'm going to Canada.
spk_0
We'll get some gold.
spk_0
I'm going to Alberta.
spk_0
Oh, Bayite is associated with other minerals such as arousa, thyme, arousa, thyme, and
spk_0
calcite.
spk_0
Calcite, really?
spk_0
Yeah, right.
spk_0
Like we said all that shit and we throw out calcite.
spk_0
Next we see ICO, right?
spk_0
The next one.
spk_0
Thunder Bayite.
spk_0
It's related to some of these minerals.
spk_0
Mugrite.
spk_0
Mugrite?
spk_0
Susan are great.
spk_0
Vidalite.
spk_0
Baroscovite.
spk_0
Brut.
spk_0
Archi-Basite.
spk_0
Cammy and I.
spk_0
Rayberite.
spk_0
Boot.
spk_0
Bootie and I.
spk_0
Bunny and I.
spk_0
And spulite.
spk_0
Maybe I said spulite.
spk_0
spk_0
Spulite.
spk_0
Stay tuned.
spk_0
Stay tuned for next week's spulite.
spk_0
spk_0
spk_0
spk_0
spk_0
spk_0
We're going to get into the little bit more of the technical side.
spk_0
So the geology of Arizona.
spk_0
So the main technical part of the show will be discussing just a smidge of the geology of the Wild West state of Arizona.
spk_0
Yeah.
spk_0
And we're going to forget about the maybe, maybe the Graham Canyon.
spk_0
So you know the most famous geologic feature, maybe ever.
spk_0
I love Graham Crackling.
spk_0
But I know.
spk_0
You know that's every time I've said the Graham Canyon, I say it as Graham Canyon.
spk_0
And that's from the Rugrats.
spk_0
Oh, really?
spk_0
Yeah.
spk_0
So, but Arizona is home to several active volcanoes, including the San Francisco volcanic field in northern Arizona.
spk_0
Which is a member of that on our table.
spk_0
Hell yeah, we do.
spk_0
And then we have the meteor crater that is one of the best preserved impact craters on earth that formed over 50,000 years ago.
spk_0
That's a matter of matter.
spk_0
Yeah, it's over a mile diameter, right?
spk_0
Yeah.
spk_0
It's huge.
spk_0
And then also what people might not know is that there is a petrified forest national park that is home to one of the largest and most colorful concentrations of petrified wood.
spk_0
So in the world from trees that are estimated to be get this 225 million years old and preserved, you know, through the the silica rich groundwater that's flowed through it.
spk_0
And then one more thing about the silica rich groundwater geologists from the area.
spk_0
Yeah.
spk_0
This is just.
spk_0
spk_0
The interesting thing about that is that it's volcanic ash.
spk_0
Okay.
spk_0
This is a fairly distant from where it erupted from and it ended up settling there.
spk_0
A silica does dissolve in groundwater.
spk_0
It's very slow.
spk_0
So you have these logs that were sitting there buried in river mud and the ash settled on top.
spk_0
It dissolved and it percolated through and remember mud does not want to transmit water.
spk_0
Mud wants the whole water.
spk_0
It will transmit extremely slowly.
spk_0
So this is like having something like this is like winning geological lottery.
spk_0
It's a pretty amazing place.
spk_0
Well, having the geodid the the Grand Canyon too.
spk_0
Yeah.
spk_0
Oh yeah.
spk_0
And then also the geologic lottery.
spk_0
You all have one of the largest copper deposits in the world and is so it's also home to the beautiful dessert landscape of the sonoran deserts.
spk_0
But enough for me.
spk_0
We want to know more about here from you because we're obviously not in Arizona.
spk_0
spk_0
So we have this real deal like we're saying an Arizona based geologist here.
spk_0
So we've just maybe I assume all of us have been there.
spk_0
Have you been to Arizona, Carly?
spk_0
Carly is not yet.
spk_0
Have you?
spk_0
Yeah.
spk_0
Okay.
spk_0
So you've been.
spk_0
And so it's it's quite a feat to even drive through that state.
spk_0
Can I remember not understanding the geologic history of that?
spk_0
I don't know why I passed over that one.
spk_0
I focused on it.
spk_0
But let's just like flat.
spk_0
You think it is.
spk_0
No, you're not.
spk_0
And you're like you get out there and it's like, okay, either I'm crazy.
spk_0
There's a million tough cones here.
spk_0
And I don't know what's going on.
spk_0
Why here in Arizona?
spk_0
So I'm really curious.
spk_0
I'm just can to know about your favorite Arizona geologasms, if I may say like the things that are like like you know you just you really latch on to those as far as what you would want to tell people about.
spk_0
And so maybe we can hear about a few of them.
spk_0
But wait, real quick.
spk_0
Can we get that all I am known for is quick.
spk_0
Yes.
spk_0
Can we get the big one?
spk_0
Not the big one out of the way.
spk_0
Big one.
spk_0
So everyone like everyone everyone from America has written to us about this.
spk_0
They want to know about the Grand Canyon.
spk_0
Grand.
spk_0
Yeah, I was reading a post on what you know a little.
spk_0
What are they called?
spk_0
Is it a post?
spk_0
Do you think it's a post?
spk_0
Yeah, I was reading blog.
spk_0
Yeah, one of those.
spk_0
And you wrote something about structural lows and without having them there, there wouldn't be a grand.
spk_0
So that I thought that was really, really interesting.
spk_0
But in general, if you want to talk about the Grand Canyon or if you want to talk about that.
spk_0
Yeah.
spk_0
Take it from here.
spk_0
Ken.
spk_0
The show's yours.
spk_0
All right.
spk_0
Well, you have you know the great on conformity, which separates the separates the two Pete sandstone,
spk_0
which is like basically a Cambrian beach about the ocean and approached over the land after a very long period of erosion,
spk_0
which is probably attributed to a global glacial event in the protozoic.
spk_0
But is that associated with snow worth and no, were you thinking after that?
spk_0
Yes.
spk_0
Oh, they think that snow wall earth caused the erosion that led to the great conformity.
spk_0
So basically you have in the, the Grand Canyon is an incision into the Kaibad plateau,
spk_0
which rises above the Colorado plateau.
spk_0
The Colorado plateau is a region of the Rocky Mountains that everything kind of uplifted at the same rate.
spk_0
So there's very little structural deformation.
spk_0
There's some monocline, some uplift here in there.
spk_0
But the Kaibad plateau really stands even higher above all of that.
spk_0
And it seems to have at least on the east and inside of the canyon.
spk_0
It seems to have risen along this fault line.
spk_0
It's called the butte fault.
spk_0
Now in the protozoic, this was a normal fault.
spk_0
And it dropped all of those pre Cambrian sedimentary sequences, you know, base formations,
spk_0
how caught high formations.
spk_0
There's a hundred of them.
spk_0
It dropped those to a fairly deep burial depth where they were sort of rapidly buried and protected for a long time.
spk_0
But the fault, it remained as a weakness.
spk_0
So during the Laramide Arrogion, you know, pretentious Rocky Mountains building events, the fault reversal orientation and uplifted,
spk_0
or it helps uplift the Kaibad plateau.
spk_0
And it acted as sort of a blind, you know, reverse fault.
spk_0
So the fault didn't break through all the layers that came, you know, during the Paleozoic, you know,
spk_0
the Red Wall line zone, the Hermit formation, Kaibad, all these layers that diskake that stood on top of it.
spk_0
And instead of breaking through all of that, it just sort of worked it up along these huge monocline complex,
spk_0
a monocline that's a fold that has one one limb.
spk_0
So it's not an apex or a dipping fold, which is kind of flat, you know, in the landscape.
spk_0
Yeah, so it's a good way to put it.
spk_0
Yeah, they're associated with the like deep seated faults at reverse and then you just have the overlying strata over it on one side,
spk_0
kind of down, or you get warped.
spk_0
And you can actually see that from one point, it's supposed coming up this week, I have a whole bunch of pictures of it.
spk_0
You can see the monocline that missed the Kaibad plateau above the college.
spk_0
And do I tell my embarrassing story or what?
spk_0
I do want you to and actually let's hold that for one second, because I want to talk about there's a lot.
spk_0
The Grand Canyon is used by a certain like the creationist, right, as a, as an example of rapid erosion, canyon formula.
spk_0
And I don't get it, but the interesting story about that is they use the Grand Canyon and they actually use a canyon here in Texas that was formed in 2002.
spk_0
So just think about that for a second in one day.
spk_0
And it was actually they don't realize it was a spillway event at a dam.
spk_0
And they say that this thing dissected 200 meters in one day.
spk_0
What does that mean about the Grand Canyon?
spk_0
And the reason they dissected that is the spillway fucking flew, right?
spk_0
You had a bunch of flow over that and you have a 200, 200 meter displacement fault.
spk_0
That's why that happened.
spk_0
But my thing about what you're talking about, yeah.
spk_0
And so what I'm talking like what I'm thinking about what you just said is your mentoring pro-rezoic normal faults, like this stuff is fucking billions of years old, right?
spk_0
And so do you think that you know are these, I don't know if you've looked into any of this stuff.
spk_0
I was told by a family member that I had to watch a DVD, yeah, DVD about the Grand Canyon, how is less than 6,000 years old?
spk_0
And so my thing is like, are they are thinking about that?
spk_0
And so the question, here's a thing, they have this thing they call creation science.
spk_0
It's not science.
spk_0
Science is going out, going out in the world collecting data and creating a model.
spk_0
Creation science is going out in the world with your model and fitting your data to it.
spk_0
So yeah, extremely biased.
spk_0
It's not just that they think the Grand Canyon is 6,000 years old.
spk_0
They think the whole earth is that.
spk_0
Yeah.
spk_0
And I have a unique insight into this because I was on a date with this girl that I met in this hiking group that I was in.
spk_0
And I'm just standing there on the rim of the canyon.
spk_0
I'm like, there's the great, great, and the four-rear, there's a breast-y-pipe and the radioactive breast-y-pipe and the red, red-bow-aligned stone.
spk_0
Look down there, that's the coclino sandstone and the math of deserts, 300 million years ago.
spk_0
And the GU separates 1.8 billion years.
spk_0
She goes, you really think the earth is that old?
spk_0
Oh, no.
spk_0
I just looked at her and I'm like, well, look here, there's truffle shells and we're at 8,000 feet elevation.
spk_0
There's a fucking show.
spk_0
It was a year, yeah.
spk_0
And she says, oh, that's just the way they cut the rock.
spk_0
That's how the...
spk_0
You're not lying.
spk_0
Dude, there is this thing on YouTube.
spk_0
And this...
spk_0
Like, I remember watching this like before I ever even thought about pursuing geology, right?
spk_0
And this person made videos about they said paleontologist secretly craft.
spk_0
Like, what was that shit that we used to do in elementary school?
spk_0
Paper mache.
spk_0
They make paper mache fossils and then go and inject them in the earth while they're digging so that it looks like they're pulling out.
spk_0
It's like what for say?
spk_0
Yeah, for say.
spk_0
Faking made her say that.
spk_0
Well, that's really good.
spk_0
I didn't really...
spk_0
Did you really go to college?
spk_0
I went to a state in school.
spk_0
I just wonder, like, do they just just miss that?
spk_0
And they're like, hey, well, I don't want to talk about that.
spk_0
You know, I...
spk_0
They have an answer for everything.
spk_0
Yeah.
spk_0
They're big.
spk_0
The zoom the whole flat earth is just dying.
spk_0
You know.
spk_0
Right.
spk_0
You don't even need to pay attention to that.
spk_0
Right.
spk_0
That's really good.
spk_0
I mean, we could talk about the Grand Canyon as an entire episode, but we wanted to get some more stuff, you know, from you about why Arizona is cool.
spk_0
Why people should go visit?
spk_0
Why do they should go hike there, right?
spk_0
So we...
spk_0
Well, something I wanted to say is we have dinosaurs, dinosaur bones and nice or tracks and Texas.
spk_0
Yeah.
spk_0
But I feel like that's not really the same ones that you have in Arizona.
spk_0
I was hoping maybe we could talk about that.
spk_0
What are your...
spk_0
What are yours preserved in, Brian?
spk_0
Uh, mudstone, limestone, uh, shaman...
spk_0
Oh, limestone, limestone, not moral.
spk_0
Not f...
spk_0
Oh, that's your favorite.
spk_0
God damn it.
spk_0
Moral.
spk_0
Is it a buddy lime or is it a liby mud?
spk_0
God damn it.
spk_0
Well, not moral.
spk_0
That's for 50.
spk_0
It's not 50, 50.
spk_0
Fitty, fitty, fitty.
spk_0
It's not that.
spk_0
It's not.
spk_0
Uh, but the Glenrose formation.
spk_0
Right?
spk_0
That's a big one.
spk_0
Um, and that's where...
spk_0
I've been there.
spk_0
Yeah.
spk_0
Uh, and it's not...
spk_0
There's, like, it's not really that far from it.
spk_0
We have the lateral equivalent up here and that's the Goodland.
spk_0
Um, we have the Goodland and then there's...
spk_0
If you go a little, like, the basal, Cretaceous sands, also have it and the Pallucsi formation.
spk_0
Um, but they're all Cretaceous stuff.
spk_0
So dinosaurs were a little different.
spk_0
Like, we have the Tranosaur, right?
spk_0
And the, like, the other therataceous.
spk_0
Yeah, but I think you have some older stuff.
spk_0
I'm a little bit of a griff.
spk_0
You guys have some older stuff that we have.
spk_0
We have visibly absent in Texas altogether.
spk_0
Exactly.
spk_0
And we don't really...
spk_0
We may have a little bit, but that's...
spk_0
We have...
spk_0
I can not honestly tell you, Triassic Jurassic.
spk_0
Uh, the boundary is probably somewhere within a hundred feet of section up or down.
spk_0
Of this formation.
spk_0
It's called the Moanave formation.
spk_0
Uh, now the Moanave is sort of blood-brain, uh, lecusteryan, which means like, you know, river, river stilts and sands.
spk_0
That interfinger, you know, with...
spk_0
I love fingering.
spk_0
I love interfingering stuff.
spk_0
Hell yeah.
spk_0
The best.
spk_0
So long.
spk_0
The interfingered quiver.
spk_0
Like with the fog.
spk_0
The...
spk_0
The Winggate formation, which is purely aolean desert.
spk_0
So basically, you had this fairly temperate.
spk_0
Uh, it was dry, you know, the rivers and the...
spk_0
The floods would be ephemeral.
spk_0
Yeah.
spk_0
But...
spk_0
You had a stable landform if you had aolean stuff.
spk_0
Right.
spk_0
And then, you know, the Winggate, the...
spk_0
The...
spk_0
The sand sea of the Winggate was crotch on it and you treat, you know, over time.
spk_0
So long story short, you had the...
spk_0
Shortly lived, uh, pools of water adjacent, probably adjacent to rivers, the...
spk_0
Overbank, uh, flooding event, that.
spk_0
Like in the Lion King, when they're at the waterhole?
spk_0
Yeah, it's like a waterhole.
spk_0
But it was like a dinosaur, uh, fucking mosh pit.
spk_0
There are hundreds.
spk_0
It's a hundred way to put that.
spk_0
There's hundreds of tracks.
spk_0
And the tracks over print other tracks.
spk_0
And then you can follow one.
spk_0
You can measure their stride length.
spk_0
And you can determine when walking, running.
spk_0
That's so cool.
spk_0
And that really, it's like so many tracks.
spk_0
Yeah.
spk_0
Now, the thing about this place, it's located just outside to the city.
spk_0
It's on Navajoway.
spk_0
Now, I have nothing against Navajo people.
spk_0
They're deeply beautiful and cultured.
spk_0
Uh, this site does not seem to have any significant to them.
spk_0
It's not part of their, you know, spiritual realm, uh, whatever they have.
spk_0
So what you get there are these guys that are just kind of down on their luck.
spk_0
They're just trying to make a few bucks and they pretend that it's the park.
spk_0
They pretend that they're torrid.
spk_0
Yeah.
spk_0
So they, you pull up to it and they start demanding money and they're going to give you a tour.
spk_0
You know, I always get some of the sheep up because, you know, why not?
spk_0
And then they take you out there on the field with the tracks.
spk_0
And they tell you, oh, this one is a velocity after this one is a turbulent source track.
spk_0
This one is dilapidated.
spk_0
Like, yeah, I saw a Jurassic Park too.
spk_0
Yeah.
spk_0
Those are critacious.
spk_0
Right.
spk_0
spk_0
Yeah.
spk_0
And, you know, you just kind of nod.
spk_0
If you say so, I just kind of pay them to go away, you know, yeah.
spk_0
So you can even determine the dinosaurs behavior.
spk_0
You can see how they slip in the mud.
spk_0
The mud with, let's start sliding all over the place.
spk_0
Yeah.
spk_0
It's awesome.
spk_0
You can see how they pivot on their feet when they change direction.
spk_0
Do you think there was like some kind of thing going on that they were all running in the same
spk_0
direction or like we said, like a watering hole, they all just congregated at.
spk_0
It just seems less the remarkable thing about this place is that it seems to be that there
spk_0
are multiple animals there at all times.
spk_0
Big ones, little ones, and there's no sign of aggression.
spk_0
There's no inference of thrashing every single track that I've measured is walking at a casual
spk_0
pace.
spk_0
And there has to have been up to, you know, 10, 15 of these guys there at once based on the way the track
spk_0
is over.
spk_0
A lot of this comes from conversation.
spk_0
I have to name drop something.
spk_0
A lot of this comes from conversation I have with a really remarkable radiant young woman
spk_0
who's doing a TVC technology, technology is a study of trace boxes.
spk_0
The popples of things that are alive, not dead.
spk_0
Her name is Jen.
spk_0
If you know Jen, she's a badass.
spk_0
That's awesome.
spk_0
Yeah.
spk_0
And so interesting that it was a peaceful place.
spk_0
I guess I can say that in a way.
spk_0
Did you see like evidence of like youth, like youth, dinosaurs, there's tiny, there's tiny little tracks.
spk_0
They're all pheropods.
spk_0
Oh wow.
spk_0
You think of pheropods as these sort of menacing thrashing, you know, savage, you know, animals,
spk_0
but there are little tiny tracks, next big tracks.
spk_0
I wonder if it's young.
spk_0
I don't really know.
spk_0
I'm not there.
spk_0
Is there like sleeping place or something?
spk_0
I don't know.
spk_0
No, I wonder if it was mothers with children.
spk_0
Yeah.
spk_0
I don't know.
spk_0
Make me think.
spk_0
So cool.
spk_0
Well, hey, feel free to take me when I'm out there.
spk_0
Next month, I've got two field trips.
spk_0
So they finally pushed them all to April.
spk_0
Okay.
spk_0
Well, I got another question for you about Arizona.
spk_0
What is Arizona State mineral?
spk_0
And where can I find it?
spk_0
Turquoise.
spk_0
Turquoise.
spk_0
Turquoise.
spk_0
Turquoise.
spk_0
You'll find it, you know, all the mind of the copper mine, have it in some percentage.
spk_0
I've seen a whole lot of it.
spk_0
We have mine clients at my job.
spk_0
They gave me a big chunk of rock that has that blue green color to it.
spk_0
And it's either $10,000 worth of turquoise or a $30 worth of copper oxide.
spk_0
Yeah.
spk_0
That's what I was wondering.
spk_0
spk_0
There's a lot of copper out there that can look like turquoise.
spk_0
But I mean, even so, it's still cool.
spk_0
You're gorgeous.
spk_0
Yeah.
spk_0
I love turquoise.
spk_0
But I like the copper minerals.
spk_0
I do too.
spk_0
So for sake of time, we're going to, I would like to really talk about vulc...
spk_0
...canism because that was the big wow factor for me in Arizona, right?
spk_0
spk_0
I guess I just didn't expect that.
spk_0
I don't know why.
spk_0
And so maybe we could talk about why it's there, maybe the last volcanic episode,
spk_0
or maybe it's still going.
spk_0
I think there's a couple of active...
spk_0
Yeah, that's right.
spk_0
...acto volcanoes.
spk_0
So like the big ones that happened.
spk_0
And then there's a very specific one we would love to talk about.
spk_0
I think you know what it's called.
spk_0
So the most recent years we're talking about the sand-based system of volcanic...
spk_0
Yeah.
spk_0
That's like the east of the Grand Canyon kind of, but it's by Flagstaff, right?
spk_0
Yeah.
spk_0
Now it's just right.
spk_0
Flagstaff is in the field.
spk_0
Yeah.
spk_0
Okay.
spk_0
So for reference, I have a basalt sample.
spk_0
And there's lots of olivine phenocrystinate.
spk_0
But I got it from the...
spk_0
I think it's called the Oak Creek Fault on 89 South going to Sedona.
spk_0
spk_0
You can see it.
spk_0
You take 89 South and you...
spk_0
It may be 89A or whatever.
spk_0
But the freaking valley just opens up.
spk_0
It's tight.
spk_0
And then you're seeing all these sandstones.
spk_0
And then there's a freaking...
spk_0
I know. Carly's like Brian.
spk_0
Can you talk less?
spk_0
Anyways.
spk_0
But then you see the basalts up top of all the red sandstones.
spk_0
You see this dark black gray.
spk_0
And it's all faulted.
spk_0
It's like what the fuck are acting as a protective cap?
spk_0
So as the ball came out of the way and it's so easy to roll that colorful red white sandstone.
spk_0
It's gorgeous.
spk_0
No, you're right.
spk_0
But so I do want to tell people if you're ever in Arizona near Flagstaff, everyone seems to go there.
spk_0
And it's a nice town.
spk_0
But take that road because you're like literally I'm driving in like I did the quintessential like...
spk_0
Like pulled off.
spk_0
I can see the fault.
spk_0
I saw the basalts and I was like I'm fucking getting a sample.
spk_0
And there was construction but I didn't care.
spk_0
And I pulled off and probably caused a mess.
spk_0
I don't care.
spk_0
That's how many we found them.
spk_0
I'll send you chords.
spk_0
So the last eruption in the San Francisco field was less than I think less than a thousand years ago.
spk_0
And that's that sunset crater which was a huge part of a huge fish erosion.
spk_0
So you can go there.
spk_0
You can see the basalt flows.
spk_0
The cojole is still glassy.
spk_0
Oh wow, really?
spk_0
The viscosity.
spk_0
Yeah.
spk_0
Wow.
spk_0
The outer most millimeter of the flow loads are still glassy.
spk_0
So you can see the flow structure.
spk_0
You can see where archery, congealed lava, glee, stuff through this.
spk_0
Pretty wild.
spk_0
Can you see that from Ariel?
spk_0
Like is it black?
spk_0
Because I've seen stuff in New Mexico and I'm like there's fucking new basalt there.
spk_0
Yeah.
spk_0
Yeah, go to sunset crater and Google Maps or whatever.
spk_0
You'll see it.
spk_0
It looks like hell.
spk_0
Sunset crater.
spk_0
Yeah.
spk_0
Very cool.
spk_0
So within that range because there's a really big volcano there, but then there's a ton of these little cones, right?
spk_0
Yeah, they get their tops blown off.
spk_0
But there's one that's aptly named that I want to let you introduce.
spk_0
So there is this particular about 900 foot tall, conical shape.
spk_0
Well did glue to make.
spk_0
So now what glue to make is sort of you know, it contrasts with all the cones around it.
spk_0
Most of the cones there are very eroded because it's just loose fender.
spk_0
Yeah.
spk_0
And you know, rained on for the past 70,000 years.
spk_0
But this guy is holding up because it speared a hotter, shatter wad that collected around the rim and they were still molten when they landed.
spk_0
So in a particular cone, it retains its original shape.
spk_0
It's much harder to erode.
spk_0
It was named the shit pot.
spk_0
After this wild west rancher, one of the first well, you know, the first western murderer who stole land, whatever you want to call it, went in there, ranch cattle, and he had this thing on his property.
spk_0
He thought it just looked like a chamber pot that had spilled over because there's a large, uh, flow that extends, you know, a couple miles to the north outside of it.
spk_0
So he said, yeah, it looks like a shit pot.
spk_0
So the shit pot is a welded, a glutinant, uh, well, you know, composed of basaltic and a little more silica than just a fault.
spk_0
And the enigma to it is the flow issuing forth from the shit pot to the north has a slightly different composition.
spk_0
I think it's a little more mafic.
spk_0
If I remember, it could be wrong about that.
spk_0
I would expect it to be, maybe you like, maybe I might have that backwards.
spk_0
I might have that backwards.
spk_0
It might be more solicit.
spk_0
Yeah, like more of a day site in the site.
spk_0
But, you know, they don't know if it's a flank eruption or an eruption that was subsequently, you know, buried over by further cone development.
spk_0
Yeah, I like the little bit.
spk_0
Well, I like the descriptor of the shit pot having a spattery basaltic and decide like for the better than the battered.
spk_0
Yeah, yeah, right.
spk_0
I usually get and decide and say usually on an active margin kind of thing.
spk_0
But that's why Arizona is so.
spk_0
Yeah, well, you know, it's moving up through all, you know, look at the grand canyon, moving up to all of that.
spk_0
Yeah, I was thinking, when, when, what, you know, yeah, was this like 70,000 years old?
spk_0
That's what it's called.
spk_0
This particular one is about 70 K based on potassium.
spk_0
Yeah, which is, yeah, there's some, there's some problems with that because there's like apparently there's an abundance of argon.
spk_0
Right.
spk_0
So you, you can then do, I'm sure they have done it and we just have to look it up, right?
spk_0
But it's like you do potassium argon, but then you do the argon argon to get.
spk_0
Arr.
spk_0
So yeah, that's, I love the volcanism there and it's really cool.
spk_0
Like we have that sample here on the, on the table.
spk_0
One of the most striking pictures that you have, then I, I guess I recently saw, it's, it's a magmatite and then there's some like relic lava flows.
spk_0
What do you say?
spk_0
Relic.
spk_0
Okay, relic.
spk_0
It's what I say relish.
spk_0
I don't know.
spk_0
Oh, something's like real, real, real dicked.
spk_0
Before we dive into that particular outcrop, let's, let's talk about magmatites a little bit because they're weird, right?
spk_0
I've confused them with nice, nice, like rocks.
spk_0
Nice.
spk_0
Yeah.
spk_0
And anyone that's not just a fucking pro magmatite petrologist would not maybe get it.
spk_0
So they're beautiful rocks.
spk_0
They have properties of both igneous and metamorphic rocks.
spk_0
They were first named by Jacob Johan Sederlom of Health Sinky Finland in 1907.
spk_0
Yeah.
spk_0
The patrologist, they worked for the geological society of China.
spk_0
I've never heard of the geological society.
spk_0
Yeah, we're tied literally names mixed rock in blue.
spk_0
Whoa.
spk_0
In the group.
spk_0
Yeah.
spk_0
So, side note, good old Sederlom was responsible for the names and studies of other geological oddities.
spk_0
These names, which I will now butcher, such as John Tien, set away.
spk_0
Jotnian, Jotnian.
spk_0
Um.
spk_0
spk_0
Yeah.
spk_0
Mermikites.
spk_0
Mermikites.
spk_0
And the famous Rapa Kiwi.
spk_0
Yeah.
spk_0
Good.
spk_0
Right.
spk_0
Which some have been dated back to the late Arcan.
spk_0
Wow.
spk_0
Mermikites are those weird, were me.
spk_0
Like they definitely look weird.
spk_0
Right.
spk_0
Where the courts, their inner growth into usually a sodic plagio clays.
spk_0
So like albiet or illegal clays.
spk_0
And then they're usually associated with tectonic deformation.
spk_0
They're not the same thing as that the macmatic inner growth textures like ingranapherec rocks.
spk_0
Okay.
spk_0
Yeah.
spk_0
So, the Mermikites in Arizona are typically associated with the formations of the Yavapai and the Maratzal originic belts.
spk_0
Which are the what?
spk_0
The Maratzal.
spk_0
The Maratzal originic belts were at the mobile, the mobile mountain belts, which were formed during the process.
spk_0
The Proterozoic era between 1.8 and 1.4 billion with a bee years ago.
spk_0
And these belts were formed during the process of subduction in which one tectonic plate is forced beneath another.
spk_0
Not to insult anybody's intelligence, but this causes an intense amount of pressure that leads to the formation of these metamorphic rocks.
spk_0
And then the Mermikites here have an almost, would you say extreme, nice, agbanding texture?
spk_0
They sure look like that.
spk_0
So, there's these Lucasome layers, Lucas thematic layers of quartz, feltsbar, and then you have other light-colored minerals like muskivite.
spk_0
spk_0
Yeah.
spk_0
Yeah.
spk_0
Yeah.
spk_0
And Luka.
spk_0
Lucasome.
spk_0
Lucasome.
spk_0
spk_0
Lucasome.
spk_0
Lucasome is just a fancy way to describe light-colored layers.
spk_0
But then these layers alternate with darker melanosomic layers that have minerals.
spk_0
Yeah, that one he said, that have minerals such as biotite and various amphiboles.
spk_0
Amphiboles, like corn blend, I can say that.
spk_0
Probably some pyroxines depending on what the parent rock is.
spk_0
Mermikites, they can be, for me, tricky to interpret in the field because I would say, oh, that's a folded nice, because I'm a dumbass.
spk_0
But actually, the Luka-cratic minerals, they have igneous textures, which means they have formed in a multiple,
spk_0
from molten magma, right?
spk_0
Mermikites.
spk_0
So that has been melted in that sense.
spk_0
And the Mafic minerals, so you have the alternate melanosomic layers, they have metamorphic textures.
spk_0
So James, Ken, Carly, how do we make sense of this?
spk_0
Why are the textures differentiated between the light and dark bands in these rocks?
spk_0
Oh, gee, maybe it has something to do with the melting point of the rock.
spk_0
I would think so.
spk_0
Maybe we could talk about that.
spk_0
We could talk about how these things form.
spk_0
Yeah, I know all about this. Don't worry, guys.
spk_0
So they are formed by anatexes.
spk_0
Oh, anatexes.
spk_0
I love anatexes.
spk_0
And it's a character.
spk_0
Oh, my God.
spk_0
Anatexes.
spk_0
We have a new character.
spk_0
I could be anatexes.
spk_0
You could be.
spk_0
Thank God.
spk_0
Or in simpler terms.
spk_0
I'm patina.
spk_0
And I'm anatexes.
spk_0
I'm anatexes, y'all.
spk_0
I'm patina.
spk_0
You sound so real.
spk_0
Oh, I'm from the south.
spk_0
I'll have you know.
spk_0
Well, we're going to talk about how the, like, we're going to talk about the 13th and it's
spk_0
like southern, how you like, Georgia, and it is a slow down version of a British accent.
spk_0
So if you speed up their accent, it turns into a British accent.
spk_0
Yeah, you're right.
spk_0
And we're not here nor there.
spk_0
Anyway, so in simpler terms, it's just partial melting of igneous rocks.
spk_0
Right.
spk_0
And so Brian put in a note saying, hey, write something about this.
spk_0
So I'm going to, I'm going to put on my, uh, my professor, a glasses.
spk_0
I hope you've got bowens.
spk_0
So basically what we got here is the, the temperature and solidis and liquidis and formation
spk_0
for mineral species are in more factors that determine the conditions required for anatexes
spk_0
to occur and the composition of the resulting magma.
spk_0
Right.
spk_0
So anatexes is the process by which the rocks are partially or completely melted to form
spk_0
magma.
spk_0
So the temperature and liquidis and solidis information for mineral species can be the,
spk_0
can be relevant to anatexes because of the temperature at which a rock begins to melt,
spk_0
i.e. the solidis temperature.
spk_0
And that is dependent on the minerals, um, present in the rock and the melting points.
spk_0
So for example, if a rock contains a lot of quartz, which has a high solidis, solidis,
spk_0
temperature, um, of about 400 to 650 degrees Celsius, the rock will require high temperatures
spk_0
to start melting.
spk_0
On the other hand, um, if rocks contain a lot of ampable, which has lower solidis temperatures
spk_0
of 708 degrees Celsius, it will begin to melt at lower temperatures like ductal quartz.
spk_0
That is a, ductal quartz is ductal at what?
spk_0
750.
spk_0
I think my wording was confusing.
spk_0
No, I, I mean, because lower temperatures, I associate 460 and higher temperatures are
spk_0
700, 800 solidis.
spk_0
But I think what this solidis temperature is crystallization.
spk_0
Okay.
spk_0
Okay, so it's opposite.
spk_0
Okay, so then furthermore, the liquidis temperature of the mineral species present and
spk_0
the rock also plays a role in anatexes.
spk_0
Hi, you know, hey.
spk_0
Um, so liquidis temperature is the temperature at which the mineral begins to melt completely
spk_0
and the rock starts to become more homogenous in composition.
spk_0
So if the temperature of the rock continues to increase beyond the liquidis temperature,
spk_0
the rock will melt completely in form magma.
spk_0
Um, so not sure if that relates, but Brian asked me to insert some information about
spk_0
this.
spk_0
So, right.
spk_0
So quartz liquidis temperature, 17, 13 degrees Celsius in the slotted solidis temperature,
spk_0
400, 600 degrees Celsius, whereas pyroxenes, 12 or 13, 15C and 800,000 C. So, respectively.
spk_0
Well done.
spk_0
Yeah.
spk_0
So that was a, I don't know how that relates to anything.
spk_0
No, it does because that explains what we're seeing, right?
spk_0
So, the more mafic minerals don't melt at these temperatures that these like the, your,
spk_0
your felsic feldspars, like your sodium rich and your potassium rich feldspars.
spk_0
Okay, but you, when you say, okay, felsic, right?
spk_0
Yeah, you didn't say mafic.
spk_0
So your felsic minerals are going to melt at a lower temperature.
spk_0
Yeah.
spk_0
Like your quartz, your muskivites.
spk_0
No, in your case.
spk_0
What?
spk_0
I'm just not, not KK.
spk_0
Not KK.
spk_0
Not KK.
spk_0
So, potassium.
spk_0
Yeah.
spk_0
So, anything like that is going to melt at a lower temperature.
spk_0
You're, you're more mafic, you're iron and your magnesium rich minerals, like pyroxenes
spk_0
and your biointite and your infoboles.
spk_0
Infoboles.
spk_0
Some infoboles are going to melt at a higher temperature.
spk_0
And so you have these bands that are completely malt.
spk_0
I don't know.
spk_0
Can't maybe help me out, but I think of these as like, there's minerals that have formed
spk_0
only during complete melting of that particular, like that melting point.
spk_0
And then they re, they crystallize.
spk_0
But the mafic bands have then re crystallized possibly because they haven't fully melted.
spk_0
We don't have, maybe you don't reach a temperature of plus 1300 degrees centigrade.
spk_0
And so that's why you have this differentiation.
spk_0
You have the light colored black, the mafic bands.
spk_0
Yeah.
spk_0
But yeah, you have that differentiation.
spk_0
Yeah.
spk_0
I would say if anything, the darker, the mafic minerals are more, I mean, they're not solid.
spk_0
They're more like a tappy, you know.
spk_0
They're like plastic almost.
spk_0
They're plastic ductile, you know, they're able to accommodate, you know.
spk_0
Oh, yeah, you're right.
spk_0
Shifts and mass and you know, they're able to flex and then they're just.
spk_0
Right.
spk_0
And that's why you see the metamorphic textures in those.
spk_0
So you see more foliation in that layer, but in the light color layers, you just see a crystalline.
spk_0
Yeah.
spk_0
So Ken, we, in these magma tites, we see like this nice, like banding, but it's not really
spk_0
nice.
spk_0
It's actually something else.
spk_0
And we see something, we see a lot of folds that are really weird.
spk_0
What's going on there?
spk_0
Tegmatic folding.
spk_0
So it contrasts a little bit to a magma tight because magma tight things are melting, things
spk_0
are ductile, but to form tegmatic folds, which are extremely tight, rounded, you know,
spk_0
they look like folded folds.
spk_0
It looks like they look like spaghetti.
spk_0
Yeah.
spk_0
You drop a noodle along the floor and it's sort of warped over itself.
spk_0
A tegmatic fold is formed in an environment where everything is just sort of ductile.
spk_0
So probably in some of the later stages of deformation and happiness, what I would
spk_0
do.
spk_0
Yeah, I agree.
spk_0
And it tells a lot of history of the rockets and you have this boundary.
spk_0
spk_0
You might have just, I'm going to make this really simple.
spk_0
So you'll 100 meters away, 500 meters away, you might have a granitic pluton.
spk_0
And then you have this magma tight.
spk_0
And then you go, you know, a thousand meters away and you have a very well developed
spk_0
nice.
spk_0
It just, that's the gradation.
spk_0
I call it a gradation.
spk_0
I don't know if that's correct, but I just think of this great, maybe a gradient is a
spk_0
better way to say that.
spk_0
A gradient in heat flow across the basement.
spk_0
Yeah.
spk_0
And that's the way I think of it.
spk_0
And I've missed it before, I'll be honest.
spk_0
I have looked at a rock that was a magma tight and I've called it a nice, a folded
spk_0
nice and it's not correct.
spk_0
For sure.
spk_0
I think that it comes down to the textures, which you can't really maybe see in the field
spk_0
you need to take a thin section and do the work.
spk_0
Well, I hate them most often.
spk_0
I think the most often and meta-terbidite.
spk_0
Yeah, because of that.
spk_0
Because of how they're differentiated in deposition.
spk_0
You've got the sandy stuff at the bottom.
spk_0
You've got the muddy stuff at the top.
spk_0
Muddy stuff, no, much faster and it deforms much faster.
spk_0
No, yeah.
spk_0
And meta-terbidite is just in general interesting AF.
spk_0
But I say that we invite you back for another episode soon to get into this in more detail.
spk_0
Well, we all, because we want to get into why Metallica sucks.
spk_0
And I feel like that we can't not talk about that.
spk_0
But I think we should talk about that.
spk_0
So what I'm doing is, it's why the geology that is there is there.
spk_0
So that's a full episode.
spk_0
But also we need to talk about faulty San Andreas and then the subsequent 14.
spk_0
So what if we brought on geologically speaking and you at the same time?
spk_0
At the same time.
spk_0
We could do that.
spk_0
I'll see you then.
spk_0
We could do that.
spk_0
We could set that up.
spk_0
We could set that up.
spk_0
And but I do want to do that freaking rock.
spk_0
Because we, James and I don't like Metallica and we want to talk about that.
spk_0
But we want to talk about thrashable too.
spk_0
And we don't want to rob our listeners of all of the fantastic geological knowledge that
spk_0
you have.
spk_0
We're going to do this then, Ken.
spk_0
One second.
spk_0
We're just going to do this.
spk_0
Okay.
spk_0
So this is our towards the end.
spk_0
We do it with that freaking rocks.
spk_0
And I noticed that you in there, and I'm not going to go into this long description that
spk_0
I talked about thrash metal.
spk_0
But I did see an important note in there that maybe you're not a fan of Metallica, eh?
spk_0
Yeah.
spk_0
Well, a lot of us who were, look, Metallica, you were talking me 25 years ago.
spk_0
I would have never thought it would ever see.
spk_0
But Metallica fucking sucks.
spk_0
They betrayed their fans.
spk_0
They started suing their fans.
spk_0
They did.
spk_0
Let me tell you something.
spk_0
I bought that fucking master puppet album like five times because my tape deck ate the
spk_0
tape to thin.
spk_0
I remember what tape decks were, eh?
spk_0
I know I know I'm dating myself right now, but I date myself once a day.
spk_0
We had this evolution of thrash and Metallica was at the forefront of it.
spk_0
Okay.
spk_0
So you had the mid 80s.
spk_0
Right.
spk_0
Yeah.
spk_0
All these guys started coming out and playing with like really intensity rhythms and double
spk_0
bass drums.
spk_0
And you know, it was sort of the bellian thing.
spk_0
I used to walk down the street with my Metallica shirt on.
spk_0
She'd come up and go, hey man, you love slayer.
spk_0
But I'm like, yeah.
spk_0
Like do you love Satan?
spk_0
spk_0
I did.
spk_0
I had to do something.
spk_0
I was paying for a long time and I had to come back.
spk_0
Sorry.
spk_0
So you had the big four.
spk_0
You had the big four.
spk_0
You had Megadeth Metallica and Stratford players.
spk_0
Right.
spk_0
Those were your quintessentials.
spk_0
Then you have the other guys.
spk_0
You have Mads and Badass, Death Metal bands like Cannibal Corps and all those nut job
spk_0
B.S.I.D.
spk_0
You know, is Metallica and Thrash Metal?
spk_0
It was.
spk_0
They were like the Godfather's.
spk_0
They went from practically inventing freshmen.
spk_0
Yeah.
spk_0
They transitioned it from popular metal at the time.
spk_0
I remained.
spk_0
Due to priests, clothing, hook, those guys.
spk_0
They were just, they were just plain metal.
spk_0
They were great.
spk_0
They're awesome.
spk_0
Did you know there's metal?
spk_0
But Thrash Metal came out and started really introducing speed and action.
spk_0
And it was a little bit of attitude and you know, all new brand of.
spk_0
Like Blaspies.
spk_0
They're belly-ish.
spk_0
Yeah.
spk_0
Yeah.
spk_0
So.
spk_0
Did you know there's, so you said, Clothing Huff, that is a, a distortion pedal that is now
spk_0
sold and it's like, it's, it rips.
spk_0
Is it terminus?
spk_0
Like the, I don't know.
spk_0
I, no, no, no, it's not terminus.
spk_0
I thought it was um, Electrohomonics.
spk_0
Maybe it's not.
spk_0
But they, it just rips.
spk_0
It's this nasty pedal.
spk_0
And so that's the boy's thought of, well, no, the rat, the rat pedal is a, that's the
spk_0
format for a lot of really heavy distortion pedals.
spk_0
And I think the Clothing Huff uses that.
spk_0
But I always thought Thrash was like, like just noise core stuff that I'm, I'm way off
spk_0
right now.
spk_0
Um, yeah.
spk_0
But wait, what about like boys in the hood area?
spk_0
I want to hear about that.
spk_0
All right.
spk_0
So almost overnight, my hometown went from Rift Chain, Metal Shirts, uh, Spice Rift
spk_0
End, and, and, and Chains in your pocket to, uh, Fila, Tommy Hill figure, but all that,
spk_0
all that baggy shit.
spk_0
And like the Metal Hat error just seems like it's fucking vanished.
spk_0
And there was only like a handful of, you know, die harder left.
spk_0
And then, top of that, Metallica started, you know, second, going after, going after
spk_0
their fans for the whole master thing.
spk_0
Oh my God.
spk_0
So Metallica, Metallica, like Thrash was already falling out of favor and Metallica hammered
spk_0
it, you know, the number one that changed the music.
spk_0
It's fine.
spk_0
You know, we want to make it to know the dollars who the hell to blame you.
spk_0
But when it started going after fans, it really is.
spk_0
Yeah, it's not going to go well.
spk_0
It was like the death note.
spk_0
Thrash.
spk_0
Yeah.
spk_0
Yeah.
spk_0
So should like the whole master thing.
spk_0
spk_0
Once Cliff Burton, their case is died.
spk_0
Uh, yeah, that's history.
spk_0
Pretty much feel that deal.
spk_0
It seems like it's almost as if Cliff was meeting and going.
spk_0
You never think that about a band member, like, right?
spk_0
Like someone behind the scenes that does a lot.
spk_0
And they, when they're gone, it's like, I think of weasers first two albums.
spk_0
They're bassist.
spk_0
Like, they're, they show completely different.
spk_0
They're from the green album and on.
spk_0
Green album on different bassist.
spk_0
Pinkerton forever.
spk_0
Pinkerton and blue album.
spk_0
Yeah, blue album is so good.
spk_0
Yeah.
spk_0
But this is a little bit before that.
spk_0
This is a long bit of it.
spk_0
No, it's not.
spk_0
It's only 10 years.
spk_0
Well, like, so Thrash now.
spk_0
So what's Thrash look like now?
spk_0
Who can listen to like a threat?
spk_0
They can make us see.
spk_0
There are some modern, really fucking badass Thrash band going on.
spk_0
Yeah.
spk_0
Yes, who is title angels?
spk_0
They're out of Europe.
spk_0
Why do they have that?
spk_0
They have those attitude, you know, rift with the holding notes.
spk_0
And they're singing.
spk_0
And they're singing.
spk_0
You know, you got another one called Dust Bolt.
spk_0
They're freaking awesome.
spk_0
And you got these guys called Thrash or Wolf.
spk_0
And these guys have been around for a while.
spk_0
But I call them modern because it's, you know, post 90s.
spk_0
They have a lot of stuff.
spk_0
The bulk of their albums.
spk_0
And the post year 2005.
spk_0
And of course, there's a land of God.
spk_0
But they're more like group metal and Thrash.
spk_0
Right.
spk_0
They're still badass.
spk_0
They're like my favorite.
spk_0
Do you want to, I'm going to play just a second of Thrash or Wolf's 2022 March 18th.
spk_0
Yeah.
spk_0
They, they debuted something.
spk_0
This is what it sounds like.
spk_0
Thrash metal.
spk_0
They are watching nothing because of crushing the street.
spk_0
But they don't dance in the world.
spk_0
The doctors and pastors and brothers will definitely be jumping in front.
spk_0
But you can see that.
spk_0
Dude, we're all making like orc faces.
spk_0
Oh, yes.
spk_0
Everyone else.
spk_0
That is awesome.
spk_0
But it's like high tempo.
spk_0
It's like the energy.
spk_0
It's high energy.
spk_0
Yeah, I like that.
spk_0
Yeah.
spk_0
Um, so something I would like to do if we have at that freaking rocks when we talk about
spk_0
music.
spk_0
I'd like to make a playlist of that particular episode.
spk_0
So maybe this episode is all fucking shit pot.
spk_0
Shit pot.
spk_0
That's the beard organ.
spk_0
Shit pot.
spk_0
Thrash.
spk_0
That's what it is.
spk_0
And so it can't like all invite you to it.
spk_0
Well, I'll invite all of you to the playlist and we make it and we get people in the listen
spk_0
to like what the everyone's in it.
spk_0
There it is.
spk_0
I was there is.
spk_0
Yeah.
spk_0
That sounds like.
spk_0
Hammett.
spk_0
Like that's the Hammett style weed right there.
spk_0
Yeah, you can see the influence of early slayer early Metallica.
spk_0
Early Metallica for sure.
spk_0
Yeah.
spk_0
That's right.
spk_0
The vocals are very slayer, right?
spk_0
Like, yeah.
spk_0
Yeah.
spk_0
Maybe later slayer.
spk_0
Yeah.
spk_0
Very cool.
spk_0
Well, all right.
spk_0
Well, this is successful.
spk_0
This was this was great.
spk_0
We're going to seriously.
spk_0
No, we're going to have to do it again and do it soon.
spk_0
So let's get like if you're cool with having a co co co co host.
spk_0
But so we're going to have to do a follow up episode because we'll obviously see two short
spk_0
and two hours wasn't enough to cover it.
spk_0
What?
spk_0
Let's hear this one.
spk_0
This one's bad.
spk_0
That was not shocked.
spk_0
Yeah.
spk_0
We would technology limits.
spk_0
Could end up talking like for another two hours, but then it's just a terrible edit for
spk_0
on my end.
spk_0
Yeah.
spk_0
Yeah.
spk_0
But we can definitely next time we'll talk about we actually I think the volcanism part
spk_0
is not we have not really discussed that.
spk_0
No, we do volcanisms and the fault faults like structural geology of the Arizona, but
spk_0
the San Andreas because you've filmed you've.
spk_0
You know guys, if you want to have me on as a recurring.
spk_0
Oh, no.
spk_0
Even if it's even if it's a short thing that we do, every other week.
spk_0
See there's some fucking fault facts.
spk_0
So there we go.
spk_0
The bad facts.
spk_0
He said he said it's not my fault.
spk_0
It's not my fault with Ken.
spk_0
Hey, that's not a bad idea.
spk_0
We just call you up.
spk_0
We need to know about this fault.
spk_0
Well, there's a little thing.
spk_0
But yeah.
spk_0
So I'm in not running out of time because it's rapidly.
spk_0
I'm talking like 30 seconds.
spk_0
So I'm just going to go ahead and do this like unfortunately.
spk_0
Be safe to what you love and fuck everybody else.
spk_0
Oh, while fucking everybody else.
spk_0
Fuck everyone.
spk_0
That wants you to fuck them.
spk_0
Yeah.
spk_0
No one else.
spk_0
Sex with them because sex is not dangerous.
spk_0
You're not a fuck people.
spk_0
They do not want you to fuck.
spk_0
Great time, guys.
spk_0
I'm sorry.
spk_0
I'm sorry.
spk_0
I'm sorry.
spk_0
But until next time, please wrap up.
spk_0
Until we want to remind you to be cool.
spk_0
Stay tuned and keep it on the rocks.
spk_0
Woo!
spk_0
We did it, guys.
spk_0
Oh, oh, oh.
spk_0
Oh, oh.
spk_0
You