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Good afternoon, and welcome to the
crime pace. But buying me, it

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doesn't podcast. How are you doing
out there? Are you hanging in there?

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Are you okay? If you're in
Texas? Are you braving the heat

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wave? All right? God damn, it's fucking I don't know. It's

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unbelievably hot, and it's making me
feel kind of nuts because I'm trapped inside.

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It's just too hot to go outside. I've been having to water every

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day, I've been having to I
don't know, man, it's just brutal.

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You know. The dogs don't want
to they don't want to go for

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walks no more. You know,
everyone's just losing the will to live.

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Would you rather live in a place
where it freezes for five months or where

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it's so hot for five months that
it makes it really hard to grow things

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and everything just kind of melts?
You know? Do you like the way

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that ultra violet light the grades plastic
and metal and wood when it's one hundred

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and five degrees constantly? People who
selling Arizona are like, shut up.

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It gets hot here South Texas.
The house places where ever lived, you

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know, and it's humid too,
or it can be, but it hasn't

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been this hot for this amount of
time, this extended amount of time in

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June. Anyway, today I got
Nick Zentner on the podcast. For those

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that don't know, Zick, not
Nick pe Zick Nentner. Nick Zentner is

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a geology professor at Central Washington University. He's got a YouTube channel. He

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does a lot of great videos.
He's got a lot of cool lectures,

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really cool humble dude. And we
have a ninety minute conversation about all things

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geology, and it kind of turned
into a two way interview in some ways.

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You know, it was just a
fun conversation, which is the way

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I like to do things. I
definitely wanted to put a lot of subject

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matter in there so that people could
get something out of it. It becomes,

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you know, somewhat semi educational.
But you know, he was asking

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me questions as well, and you
know, it was just kind of shooting

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the ship, just kind of I
guess we were kind of getting to know

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each other as well over the over
the course of the ninety minutes. But

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we talk about a lot of good
things. We talk about, you know,

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what got us both into the phenomenon
of doing what we do and how

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good it feels to share things you
know with other people and for me,

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how good it feels to learn new
things too, which is what I'm always

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doing. So that's the that's the
point of a traveling and seeing new shit

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and uh exploring, you know.
So Uh anyway, Um, I'll cut

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right to the chase. But if
you haven't checked out Nick's YouTube videos,

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I recommend doing so. Nick Zentner, just look him up on YouTube.

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He's also got a podcast, and
uh, we talk about uh, you

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know, basically he talks about,
you know, this theory of of challenging

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the this theory that challenges the conventional
ideology about how the Rocky Mountains were formed

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and what was going on tectonically with
North America over the last two hundred million

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years, and um, we talk
about a lot of things that people.

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I mean, there's a lot of
shit in terms of how certain landmask is

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form in North America that we just
don't know. That geologists just don't know

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yet. There's theories out there,
there's dominant theories, but nothing is certain.

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And sometimes I mean I've noticed this
too when I read about because I'm

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always asking questions, how the fun
did these mountains form, you know,

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what was going on at this point
in time fifty million years ago, a

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hundred million years ago. And in
reading about this stuff, I mean,

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I'll be reading research papers, I'll
be asking geologists I know, and a

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lot of people just don't know.
They really don't. It's like there's theories

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out there, but in terms of
we know certainly, like that where's the

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smoking gun? Like where's the where's
where's the gravity? Readings that show the

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crater using an analogy here in the
Yucatan where you know, the comment that

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caused the KT extinction? Where where
is where's that? You know? For

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where's the where's the you know,
the analogy, where's the smoking gun?

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That kind of smoking gun? For
other land forms across North America that show,

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you know a lot more conclusively how
they formed, And that just doesn't

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exist as uh as you slowly find
out for a lot of land masses.

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So but there's theories and there's a
lot of fun stuff to think about,

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and it's all about just slowly piecing
together the way that you think of the

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land that you live on and and
the mountains you hike in and the deserts

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you enjoy being in. And you
know, etcetera. The other the other

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land masses that you enjoy spending your
time, and the road cuts you drive

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by, the lakes you swim in, et cetera. So, uh yeah,

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it's it was a good conversation and
I certainly learned some new things about

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it too. I did not know. Well, you'll you'll hear the conversation.

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But I think this theory about Rocky
Mountain uplift is pretty cool, and

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we talk about that too. But
we also talk about a whole bunch of

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shit. So if you're not interested
in Rocky Mountain uplift, you'll find something

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else interesting. I'm going to Brazil
in a week. I'm a little not

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stressed out. I'm just packing.
I don't like traveling as much. And

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you know, without a break in
between and and then I guess kill you.

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We might be doing another season to
kill your lan. What else do

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I got going on. I'm gonna
be doing a presentation in New York at

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the Cactus Store again in late September. I'll probably going to Ithaca too,

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surprised they're gonna have me. No, no, Cornell, I'm doing a

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talk at Cornell. They're having my
low browed slob ass do a talk in

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Cornell, which is in Ithaca,
right am I fucking this? I don't

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even know what I'm talking about anymore. Man, I got too much stuff

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I might play. I'm trying to
get these illustrations done for a fucking children's

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book. It's driving me nuts breaking
out the brush doing brush and ink illustrations,

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not just the pen anymore. It's
been kind of a pain in the

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ass. But either way, I'll
be in New York in September and probably

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Chicago in August and part of September, and then I think I'm going to

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Lake Wales Ridge in Florida in October. So either way, Uh, my

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schedule is gonna be a little pack
for the next two months. But if

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you're in those places, I want
to say hi, shoot me an email.

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Uh try to keep it short if
you can, because I won't be

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able to respond in depth at all. And yeah, I hope you're hope

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you're enjoying our New Zealand videos anyway, that's all I got. Enjoy this

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conversation with Nick Zetner, and uh, go fuck yourself by well, I'm

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gonna showing you what it's like or
I'm not gonna shure youttec, you know,

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I mean, I'll think they're shock. They've got a nice shop,

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liberal parts. So then you start
to pack and shutter and quash come out.

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You know, I've seen a couple
of night things. Donail the fourth.

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You're a bunch of hippies twelve each
other. You can come with cholgetting

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to hit left down. They're okay, Nick, are you there? I'm

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here, Joey, thank you man. This is great. Yeah, man,

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I got you know, I got
a giant jug of green tea and

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non alcoholic beer in a bottle to
piss in, so I don't have to

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leave the podcast. So uh so
let's go. So I just I want

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to just start off. I've been
watching your videos for a while. I

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mean, any video where a dude
is talking to me about geology and you

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know there's like a beautiful, you
know, scape of mountains behind them,

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uh is gonna woo me in.
So this is like, and where you're

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based out of You're based out of
Washington and Pacific Northwest. Geology is fascinating.

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I mean, we got volcanism,
we got Missoula floods, we got

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a cool fossil flora up there on
chucking Nut Drive and the what is it

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the racehorse formation up there, and
where's that Bellinghammerson got it? I think

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I think somebody chipped me off because
your video's long go and you were up

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here in the early days. Weren't
you making a couple of like plant fossil

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videos up here in Washington? Yeah, twenty eighteen, Yeah, and someone

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I was up there looking at the
escne fossil floora like fifty million year old

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glip, the strobus and tex odium
and ferns and all kinds of cool shit.

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And then I went to a spot
near what was it, I think

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it was near Spokane or Nachi was
we're near with Natchie, And then there

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was like maya scene like twenty million
year old, fifty million year old you

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know, in volcanic sediments like an
ash beautiful fossil flora. Man, it

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was blew my mind. But uh, well it's been it's been five years.

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You're welcome back anytime. There's all
sorts of cool stuff. You're a

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foreshore Yeah, no, I got
I gotta get back there at some point.

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I just I took a break from
the West Coast because I had spent

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so much time there, and I
needed to see what was out in southeast

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in Texas. Texas is weird,
Texas is cool. Geology, lots of

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limestone, the culture here's a little
rough. I think it's just the Southeast.

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I bitch about it all the time. It's just the car, Like

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there's just this addiction with the car, like America has too much land and

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it doesn't know how to use it
responsibly. And we've just said it,

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We've just everything is just driving like
it's it's so bad for people's health.

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You know, well it is.
And I have been listening to your podcast

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and I'm up on the latest,
and so yeah, I mean you kind

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of you kind of self talk.
I mean, you head down those roads

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and you want to kind of stay
someplace else. But it does seem like

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you're you're heading to that end of
day's type vibe with some of these places

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you've been experiencing. And you know, the beauty of geology is I can

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do back millions of years in time
and kind of be totally removed from the

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whole fac totally. That's that,
and that's anitie. What got me into

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what I found so alluring about geology
in the first place. When I first

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got into it almost twenty years ago, was you know, here was a

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way to zoom out and realize the
bigger picture. And I think, you

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know, it's really uh, that's
kind of freeing for a lot of people

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too, because especially people get caught
up in the I mean, I just

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like to complain. I worked for
the railroad for fifteen years. That's what

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we do. We complain about any
you know, anything Like if there's not

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something to complain about, we find
it. And that's that's fine. I

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just you know, as long as
someone takes themselves with a grain of salt,

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I think it's fine. And also, you know, get stalked on

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some beautiful things. But when I
first got into geology, that was what,

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you know, it was like,
Wow, there's this bigger thing,

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and you know, people can get
get kind of land locked in this myopia

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of just oh, the human world
everything sucks. It's like, there's a

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lot of really cool stuff, and
there's this really cool story out there that's

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billions of years old, that's been
you know it only I mean, to

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be honest, it sounds like I
really only got exciting the last billion years

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or so. But maybe you could
chose my mind on that. You know,

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what was going on in those in
those those oceans two billion years ago,

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you know, just a bunch of
cyanobacterias slowly making oxygen or what.

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I have no idea. I mean, Precambrian has always bored me to tears,

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and I you know, I grew
up in Wisconsin and was taught some

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of that stuff early on, and
I'm like, I think I'm more interested

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in kind of some more dynamic stuff
out here in the Pacific Northwest. So

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in part that's why I'm here.
But yeah, we can talk geology.

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But you know, I'm curious about
you, Joey, and I don't know

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how much your viewers and listeners know
all the gory details about you. But

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yeah, I mean you mentioned you
wanted to talk to geology and maybe why

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I got into making videos and other
things for the public. But I have

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the same curiosity about you too,
So oh god, oh you don't want

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to hear about me? I do. I do the self taught part,

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Like, I have very strong opinions
about universities and how they operate and how

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they don't really serve the ideals that
maybe existed a hundred years ago. Were

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you're truly self taught with not only
the botany but the geology, Like you're

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literally checking out books out of a
public library. Oh yeah, yeah,

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I mean I've got I read textbooks, man, That's what got me.

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I mean the geology I started,
well, I had two classes. One

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they were one was an oceanogriy class, one of geology class. They were

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both kind of the same thing.
The geology class was taught by this sweet

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woman, sweet woman, but she
seemed like she was on Quelus ninety nine

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percent of the time. She was
just you know, she just you could

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tell she didn't want to be there. This passionate had a ton of knowledge,

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monotone. She was like, you
know, like that Ben Stein character

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from that fucking eighties six kind of
one of years. It was like that.

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And then I had this The other
lady was this butch lesbian who was

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just fucking she was awesome. She
was so just fuck, I don't give

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a shit. I do you think
I'm a betching. I want you to

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learn the stuff. And I was
just, you know, I was like,

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oh my god, you're my hero, You're You're amazing. And she

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just taught with such passion, and
she loved it. And she was teaching

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oceanography, which you know, I
wasn't really clear as to what it was.

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I didn't realize it was the study
of the oceans. I kind of

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had it confused with some sort of
like study of marine biology, but it

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was really it was essentially the same
as a geology. Of course. We

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talked gard ocean, a cross coindental
crust, three different rock types, tectonic

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plates, um. You know,
the idea that I think everyone should have

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a tectonic map in their classroom,
you know, like any earth science because

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that's really fuck the geopolitical boundaries.
The tectonic map is really what shows you

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what's going on in the world,
you know, and and why mountains exist

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and and and then it gets into
the biological aspect of biogeography and why there's

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these disjunctions of you know, the
same family, same genus, uh,

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you know, for example, all
the Gondwanan stuff, these these families that

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there's a there's you know, members
in Chile and then there's members in a

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you know, Australia and New Zealand
and nowhere else. And why is that,

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you know, because because of tectonics
because everything used to be connected,

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you know, And so that was
you know that teacher, really, God,

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I wish I should. She's someone
I would love to like send a

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fucking Christmas cards some because she was
just so she had such an impact on

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me. And I was only,
you know, that was I wasn't even

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going to school then, because I
was like, I want to degree.

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I kind of knew it was a
joke. And I was like, I

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got friends who have degrees who are
making shit money and working in coffee shops

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and miserable and kind of regretting that
they got a degree, because I mean,

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you know, so many things in
America have just been turned into a

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business, you know, privatization,
there's the it's like the point of what

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they're offering is not the point of
why they do it anymore. It's the

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point of where they do it is
just to make money, you know,

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whatever essential service. And so I
love the idea of college. I love

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the idea of university. I love
the idea of schooling. But it's just

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too tied to class and it's too
tied to business in this country. And

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that's what's a bummer. If it
was you know, free open access to

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all or like subsidized. I'd be
all for it. But I think part

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of the reason I tend to shit
on higher education so much is one because

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of the yeah, the kind of
classist and elitist nature that it takes some

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times. And I get that people
spend all this money going to school and

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they want validation, but uh,
you know, and there's a lot of

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ego tied. But also it's just
the business as fact. I mean,

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it's just it's been made to be
such a struggle to afford it for so

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many people that it's kind of like
it's kind of seems like kind of a

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scam. I'm not gonna you know, It's like it's like signing up for

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a high interest credit card in many
ways, like now, I'll just wait

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till if I don't have the money, i won't get it. You know,

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I won't buy that thing. I'm
not going to pay twenty percent interest

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for it. That kind of thing. So, yeah, well you're onto

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some stuff here. What you're speaking
about is real. And you know,

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I've been teaching for thirty five years
at a university, and I have seen

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some trends that are not particularly great. And we can go there if you

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want, but do me a favor, Do me a favor and find that

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woman if you can. I mean, when people do take the time,

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you know, years later, decades
later, and say, hey, I

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just want to let you know that
you really left an impression on you.

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It's corny, but it really does
feel good. So oh, yeah,

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you can find her, do that
please? Yeah for sure, man,

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Yeah, I know I really need
to. So anyway, that was I

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just went to college for two semesters
at its City College of San Francisco,

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then dropped out to work for the
railroad, but then continued I was just

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so fascinated by this stuff, continued
to read about it, and then I

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got into botany when I was working
for the railroad, and and I just

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went down a wormhole. I mean, I think it's the same way.

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A lot of people find this stuff
so fascinating and want to know more,

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and and some people just can't sit
very well with the idea of not knowing,

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and so you know, and then
you know, that becomes a nice

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distraction from all the other stuff you
know in life. So anyway, but

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you know, you're you're a big
part of that. And I think you

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know this I'm guessing you know this. It's it's you're a genuine guy.

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You're you're you're coming directly through that
computer screen or however anybody is consuming what

256
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you're doing. You're consistent and you're
genuine, and that's what people need,

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that that the information is there if
you hunt for it on your own.

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But you're you're a real person.
You've taught it, You're you've taught it

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to yourself, and you're communicating it
in your own unique way. And there

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00:17:00,600 --> 00:17:03,799
needs to get a lot more of
that, not just in universities, but

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just in general. And so I'm
really impressed by the tone and how you

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do things, and I hope you
keep going with that. No, well

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thanks a lot, man. Yeah, that that means a lot, especially

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coming from you. I just I
think, you know, my goal at

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this point just to share the stuff
with other people so that you know,

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just just I think just the average
schmuck gets could get a lot out of

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knowing this stuff and viewing the world
through this way. And I think that

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traditionally, you know, many human
societies and you know, we're more in

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tune with the land that they live
on. Whether it was knowing the geology

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or the plants or whatever, and
that offers a sense of fulfillment that we

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can't get in today's consumer society,
where every place in the country is starting

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to look the same, and people
people everywhere it seemed equally miserable and depressed.

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So you know, it's a it's
a nice Yeah. It feels good

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to have a connection to landscapes and
to have that kind of perspective. So,

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you know, geology did for me
when I first learned about things like

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the geologic time scale and plate tectonics. What it did for me what religion

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probably does for some other people.
You know, gives you a sense of

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like, I understand my place.
You know, so well, you're you're

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breaking up just a little bit.
I hope that's not in the recording,

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but it's just let's keep going.
Maybe it'll settle down. No, it'll

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be in the recording. Yeah,
that where if we if we have technical

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difficulties, I could just cut it
out and edit it. But um,

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you know, where I live,
the service isn't so good, so let

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me know. Um good. Well, I want to ask you. I

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want to start asking you. I
guess how did you start making making these

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videos? What inspired you to do
that. Well, um, there's a

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long answer and a short answer.
I guess the short answers. Um.

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I started teaching geology in nineteen eighty
seven. That's a long time ago now,

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and I was just focused on teaching
geology one on one and geology two

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ten and doing the traditional stuff.
And I continue with that, you know,

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thirty years later, I'm still doing
that pretty much every day, and

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I do enjoy it. But when
my kids, three boys, and once

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they became teenagers and didn't want to
spend as much time with me, which

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is thoroughly appropriate, and I had
a little extra time, I knew that

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there was an audience. I'm here
in Ellensburg, Washington, and there's all

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these amazing places that everybody's curious about, and so, you know, I

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knew there was a real intense interest
in specific places, whether it's Mount Rainier

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or Grand Cooley or earthquakes or whatever, it's here, and so people were

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calling my office. This is back
in the day when you would call somebody's

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office or you physically knock on their
office door, and just folks from all

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walks of life that wanted to know
things. So, yeah, when I

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had a little extra time, I
started making TV programs just at the university

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00:19:55,319 --> 00:20:00,400
here, just like Waynes World,
basically local cable TV to people in the

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area. And one thing led to
another where I started doing public lectures and

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00:20:04,240 --> 00:20:08,480
the nets fun into public field trips, and I was really interested in making

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it all free for anybody who wanted
to come, and it kind of grew

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and grew, and so that eventually
got me to YouTube and podcasts and everything

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00:20:17,960 --> 00:20:22,359
else. So it was just an
incremental growth, but it was just an

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intensely satisfying thing to take all this
complicated academic bullshit and find some narratives that

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work for different kinds of people.
And they just kept coming back and word

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of mouth and all that. So
it's been really fun and I continue to

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really enjoy just trying to communicate this
stuff in my own way, similar to

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the way that you're communicating stuff in
your own way. So, but I

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mean, you're obviously really passionate about
it, because a lot of people who

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teach geology, I mean a lot
of teachers in general are not very passionate.

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You know, they just know a
lot that they're not inspired by it.

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It's not what they go to sleep
think and about. You obviously are

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00:21:02,279 --> 00:21:04,160
passionate about it, and it obviously
feels good for you to share that with

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other people, which is something I
experienced too with plants. So and I

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think what you said to about you
know people, you know, people,

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especially in an area we've got public
land, which where I live right now,

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00:21:17,680 --> 00:21:21,400
just here temporarily, there's not a
lot of public land in South Texas,

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Texas in general. Man, but
people get curious about these you know.

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That curiosity is what I see that
curiosity in people, and I'm like,

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ooh, let me get at that, you know, let me let

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me there's my end, you know, because I'm like, this is this

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00:21:34,200 --> 00:21:37,319
is you could this is that's the
spark that could like, you know,

328
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a passion for someone about a certain
subject. And so I think especially with

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geology. You know, we got
public land. You're out hiking around,

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You're looking at road cuts, You're
looking at these weird rock formations. You're

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looking at squiggly lines and cliff sides, and you're like, man, how

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00:21:51,079 --> 00:21:53,799
how did that? How can rocks
bend? Like? How are rocks pliable?

333
00:21:55,480 --> 00:21:59,240
You know? Why? Oh that's
chirt? What is it's formed from?

334
00:21:59,680 --> 00:22:04,400
You know? The microscopic bodies of
these single celled organisms that make essentially

335
00:22:04,440 --> 00:22:07,279
houses out of silica. How does
that work? Like what I don't even

336
00:22:07,279 --> 00:22:11,119
know about those? Oh they're still
around, not that particular species, but

337
00:22:11,119 --> 00:22:15,759
they're still around. Oh, micro
fossils, what's that fossil pollen? Like?

338
00:22:15,799 --> 00:22:18,359
Oh, this stuff? And then
it kind of like blows people's minds,

339
00:22:18,440 --> 00:22:22,519
you know. But but initially start
seeing that road cut or that I

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00:22:22,519 --> 00:22:26,319
always love that John mcfeque quote.
You know, road cuts are church to

341
00:22:26,400 --> 00:22:30,680
geologists. It's so true, it's
so true. But but you know,

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00:22:30,839 --> 00:22:36,000
so I guess that's is that where
you see a lot of people coming to

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you, they're just kind of like, I want to know. I'm hike

344
00:22:37,559 --> 00:22:40,960
in or I'm driving and seeing this
stuff, and I want to know how

345
00:22:41,000 --> 00:22:45,240
it formed. Well, I've evolved
in my thinking just in general. It's

346
00:22:45,279 --> 00:22:49,920
not even geology. I just assumed
once upon a time that everybody was curious.

347
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I just assumed every every person walking
down the street was just a naturally

348
00:22:55,119 --> 00:22:59,240
curious person. As I get older, especially, I realized it's a pretty

349
00:22:59,240 --> 00:23:03,000
small group of people. I think
as kids. As kids, they are,

350
00:23:03,079 --> 00:23:04,839
but as they get older and more
defeated, they're not. They stop

351
00:23:04,920 --> 00:23:08,279
being curious about the world. And
that's a tragic moment when you're not curious

352
00:23:08,319 --> 00:23:11,440
about the world anymore. Like I'll
tell people stuff sometimes and they're like,

353
00:23:11,640 --> 00:23:15,240
uh, and I'm like, I
don't you see how cool it is?

354
00:23:15,279 --> 00:23:18,680
Fuck like look at this, and
they're yeah, yes, oh God,

355
00:23:18,799 --> 00:23:22,400
so you're you're you're tapping into that, and so yes, when I when

356
00:23:22,400 --> 00:23:26,319
I do have people kind of burning
calories to come find me or email me

357
00:23:26,440 --> 00:23:29,839
or whatever, like, Okay,
there's curiosity there, and I am going

358
00:23:29,880 --> 00:23:34,759
to feed off of that. But
then the next step for me is is

359
00:23:34,839 --> 00:23:41,960
not just giving them sex, but
somehow showing them a way that you can

360
00:23:41,000 --> 00:23:45,759
tell a story about these places.
To me, I have found this this

361
00:23:45,839 --> 00:23:51,319
way to communicate geology, which is
just storytelling. I'm taking an road cut,

362
00:23:51,359 --> 00:23:56,079
I'm taking these other places, but
I'm I'm weaving these narrative threads.

363
00:23:56,160 --> 00:24:00,400
That's just my style. And so
instead of coming up with a bunch of

364
00:24:00,480 --> 00:24:03,680
jargon for them or you know,
giving them little factoids they can share with

365
00:24:03,720 --> 00:24:07,279
their neighbors, I mean, I'm
kind of bored with that approach. I

366
00:24:07,279 --> 00:24:11,440
don't want to learn stuff just to
learn it. I want to I want

367
00:24:11,440 --> 00:24:15,599
to dig deeper and see how things
are connected. I guess, yeah,

368
00:24:15,720 --> 00:24:21,880
the context. Yeah, so even
even in the geology research community, I

369
00:24:21,960 --> 00:24:26,759
just see all these individual little postage
stamps of knowledge and their their project,

370
00:24:26,880 --> 00:24:30,759
their research project is, you know, maybe thirty five years of research in

371
00:24:30,839 --> 00:24:34,000
this one little area and it's a
it's a deep well of knowledge. But

372
00:24:36,000 --> 00:24:37,960
come on, man, look next
door, look at the next county over.

373
00:24:38,119 --> 00:24:41,359
Isn't that the same shit? How
come you're not talking about that?

374
00:24:41,599 --> 00:24:45,680
Can't can't we can't? We kind
of broaden things out, So I like

375
00:24:45,839 --> 00:24:49,839
connecting dots as opposed to just spending
all my time at one dot. And

376
00:24:49,880 --> 00:24:53,359
it seems like in the research world
that's the case. And my last thought

377
00:24:53,400 --> 00:25:00,319
there is that I've been at some
Penrose conferences recently where the leading research in

378
00:25:00,359 --> 00:25:04,000
a particular field they're all in the
same rule and half of those folks aren't

379
00:25:04,039 --> 00:25:10,440
curious. They're just reporting their details
and job, their job is done.

380
00:25:10,599 --> 00:25:15,519
And I'm just sitting there like depressed, because like there could be so much

381
00:25:15,559 --> 00:25:21,559
more instead of this little m biotic
way to report their findings. And that's

382
00:25:21,599 --> 00:25:23,160
the end of it. Yeah,
sad man, It kind of makes you

383
00:25:23,200 --> 00:25:26,960
want to slip a couple of tabs
of acid into the you know, the

384
00:25:26,200 --> 00:25:30,480
the coffee pot that they got over
there at the at the table. But

385
00:25:30,519 --> 00:25:33,920
anyway, so what do you So
let's talk about because I want this to

386
00:25:33,960 --> 00:25:36,599
be I want to ask you personal
stuff. I want to not personal,

387
00:25:36,599 --> 00:25:38,759
but like personal about your personal life. But I also want to I also

388
00:25:38,799 --> 00:25:44,799
want to talk about, um,
you know what in terms of getting people

389
00:25:44,880 --> 00:25:48,839
into this, like good elementary,
like someone who's got no concept of geology.

390
00:25:48,839 --> 00:25:51,240
People will write me and they'll say
what should I do? And I'm

391
00:25:51,279 --> 00:25:56,759
like, man, just download you
know, a PDF of Essentials of Geology

392
00:25:56,799 --> 00:26:00,680
textbook on lib gen, or just
buy the text book if you can.

393
00:26:00,759 --> 00:26:03,160
And you know, but no one
that sounds Buying textbooks doesn't sound fun to

394
00:26:03,160 --> 00:26:07,039
people. They're overpriced, and you
know, even reading one on like a

395
00:26:07,039 --> 00:26:10,519
PDF on a tablet, which is
a freeway to do it because a lot

396
00:26:10,559 --> 00:26:12,000
of the stuff is on libgen now, which is like a you know,

397
00:26:12,039 --> 00:26:15,960
way to pirate books, doesn't sound
funny. They want that context. And

398
00:26:17,000 --> 00:26:19,319
so that's what's really I tell people
other things too, them, like get

399
00:26:19,440 --> 00:26:23,720
download the app rocked roc KD.
It's an overlay, it's a geologic map.

400
00:26:23,759 --> 00:26:29,880
Overlay of the entire world. Essentially, some countries have more data than

401
00:26:29,920 --> 00:26:33,119
others, but you know, and
then that'll tell you and learn the three

402
00:26:33,200 --> 00:26:37,279
rock types, learn about plate tectonics, you know, oceanic crust versus condental

403
00:26:37,319 --> 00:26:42,000
crust, subduction zones there how they
create vulcanism, that kind of thing.

404
00:26:42,000 --> 00:26:45,599
What do you think is the best
way? Like, what do you tell

405
00:26:45,599 --> 00:26:48,839
people who are like I want to
learn more? Like, what are some

406
00:26:48,039 --> 00:26:55,720
essentials, essential principles that you that
you try to communicate to people. Well,

407
00:26:55,759 --> 00:26:57,759
that's a tough one. I think
your philosophy is slightly different than by

408
00:26:59,279 --> 00:27:03,920
to me. I think a rookie
needs some sort of guide, some sort

409
00:27:03,920 --> 00:27:11,960
of person. Somebody was the personality
to to kind of put this menu together

410
00:27:11,079 --> 00:27:15,759
for them. So I think you're
a rare person in that case where you

411
00:27:15,799 --> 00:27:18,799
have the patience and the dedication to
sit down with these textbooks empower them through

412
00:27:18,799 --> 00:27:23,000
on yourself. Well, someone guided
me to had I had k weiss my

413
00:27:23,279 --> 00:27:27,160
you know, the teacher. But
after that I started kind of you know,

414
00:27:27,319 --> 00:27:30,319
but yeah, it takes time,
and you I kind of agree with

415
00:27:30,359 --> 00:27:34,200
you. People really do need someone
to show them the initial robes, you

416
00:27:34,240 --> 00:27:38,559
know, right, So you know. In that case, um, you

417
00:27:38,599 --> 00:27:42,559
know, if if somebody's interested in
learning about geology, you know, yeah,

418
00:27:42,559 --> 00:27:48,200
the default is come to our university
or go to your nearest community college

419
00:27:48,200 --> 00:27:51,279
and take a class or two.
And if you're inspired that way to at

420
00:27:51,359 --> 00:27:55,240
least learn the basics with that person, maybe you can do it cheaply.

421
00:27:55,319 --> 00:27:57,920
I mean, I have all my
YouTube stuff, all the geology one on

422
00:27:59,000 --> 00:28:02,319
one classes are all online for free
and all that sort of thing, So

423
00:28:02,359 --> 00:28:06,240
there's ways to do it that way. But I can just answer it from

424
00:28:06,240 --> 00:28:10,160
my own point of view, which
is I did a whole undergraduate degree at

425
00:28:10,160 --> 00:28:15,079
the University of Wisconsin, and I
remember graduating. My family was there,

426
00:28:15,079 --> 00:28:17,839
and I was thinking to myself,
I think I screwed up. I think

427
00:28:17,920 --> 00:28:21,920
I picked the wrong major. I
was graduating with a bachelor's degree in geology,

428
00:28:21,960 --> 00:28:26,599
and I'm pretty sure I picked the
wrong fields. But then I went

429
00:28:26,599 --> 00:28:30,359
to graduate school because I didn't know
what else to do, and I came

430
00:28:30,359 --> 00:28:33,240
out to Idaho and that's when it
all clicked for me, and I became

431
00:28:33,640 --> 00:28:37,720
very, very excited about geology because
I had my own project. It was

432
00:28:37,839 --> 00:28:41,319
personal. I was in charge of
it, as opposed to just kind of

433
00:28:41,319 --> 00:28:45,839
being on the receiving end of all
these lectures. So for me, I

434
00:28:45,920 --> 00:28:52,000
turned the corner when I could actually
design a project, have an advisor that

435
00:28:52,119 --> 00:28:56,680
was really good for me and understood
who I was, what my strengths and

436
00:28:56,720 --> 00:29:00,279
weaknesses were, and then I was
often running and I'm still doing that forty

437
00:29:00,319 --> 00:29:03,559
years later. But to me,
it wasn't the content, It wasn't learning

438
00:29:03,880 --> 00:29:08,359
the basics. That didn't turn it
on for me. That it's connecting it

439
00:29:08,440 --> 00:29:12,480
again that context and finding a way
to make it work for myself. And

440
00:29:12,519 --> 00:29:15,680
I think you've done the same thing
with what you're doing, right, Yeah,

441
00:29:15,759 --> 00:29:19,000
yeah, And I definitely think you
got to have something in front of

442
00:29:19,000 --> 00:29:25,720
you to look at, like a
landscape or a mountain or a road cuts,

443
00:29:26,119 --> 00:29:27,480
you know, because I think especially
because you were you were originally in

444
00:29:27,480 --> 00:29:30,799
Ohio, right, I mean that's
where you were teaching. That's you know

445
00:29:30,920 --> 00:29:34,519
shit, man, I mean from
the Midwest. I'm lucky we had quarries

446
00:29:34,880 --> 00:29:37,920
where I lived that where I lived, I lived southwest of Chicago, in

447
00:29:37,920 --> 00:29:41,960
a suburb that was southwest of Chicago. My mom would drive me in to

448
00:29:41,079 --> 00:29:45,000
the city because she was always going
into the city a lot, and we'd

449
00:29:45,000 --> 00:29:48,359
passed the quarries and she'd tell me
about these limestone quarries. But everything there

450
00:29:48,440 --> 00:29:52,559
was limestone, you know, aside
from these occasional giant boulder that had been

451
00:29:52,599 --> 00:29:56,759
dropped in the middle of a force
somewhere by a glacier, you know,

452
00:29:56,759 --> 00:30:00,920
a granite boulder brought from up north
by a glacier. So it was all

453
00:30:02,000 --> 00:30:04,920
limestone, I think the Silurian or
Devonian or somebody. Either way, you

454
00:30:04,920 --> 00:30:07,160
know, it was that was all
I had. And if I didn't have

455
00:30:07,240 --> 00:30:10,799
that, I wouldn't even be thinking
about what was down there, you know,

456
00:30:10,920 --> 00:30:17,200
beneath all the soil, but totally
but you know, gosh, that's

457
00:30:17,200 --> 00:30:21,680
exactly. Yeah. So that's part
of this story that I was in Wisconsin,

458
00:30:22,119 --> 00:30:25,000
great place, all my family's there, rolling hills, you know,

459
00:30:25,160 --> 00:30:30,079
glaciated drumlins and everything else, moraines. But it wasn't until I moved to

460
00:30:30,160 --> 00:30:36,599
west to Idaho where I could see
all this stuff. And that department at

461
00:30:36,640 --> 00:30:40,559
that time was really field base.
So we had whole classes out in the

462
00:30:40,599 --> 00:30:44,839
field, camping every weekend with the
professors and everything. Of course, it

463
00:30:44,880 --> 00:30:47,960
comes to alive, it comes alive
for me then. So yeah, my

464
00:30:48,000 --> 00:30:52,640
first teaching job was back at Miami
University in Ohio outside of Cincinnati, and

465
00:30:53,400 --> 00:30:56,400
I was nearly married at the time, and my wife was from Idaho,

466
00:30:56,480 --> 00:31:00,720
and and we lasted three years,
and she's like, we got to get

467
00:31:00,720 --> 00:31:03,039
out of here, we got to
get out of here. We got to

468
00:31:03,039 --> 00:31:08,039
get back out to where we belong. And so, yes, the place

469
00:31:08,279 --> 00:31:12,680
is a huge part of it.
And it's not this parallel universe that you're

470
00:31:12,720 --> 00:31:15,799
reading about in a textbook. It's
right out your window. I'm looking at

471
00:31:15,799 --> 00:31:18,119
it right now. I'm looking at
the nash Dash Ridge at the top of

472
00:31:18,119 --> 00:31:23,279
the mount right near so it's all
in your face and you are intimately connected

473
00:31:23,400 --> 00:31:29,240
with it. And back to the
public outreach thing, People, at least

474
00:31:29,640 --> 00:31:34,480
out here and maybe even any place, they have real personal connections to these

475
00:31:34,480 --> 00:31:40,960
places, Like they remember fishing with
their mom and dad on this river in

476
00:31:41,000 --> 00:31:48,160
this canyon twenty years ago. And
now they're hearing something from this geology person

477
00:31:48,680 --> 00:31:52,400
that's just a little morsel. It's
a little it's a little idea, but

478
00:31:52,920 --> 00:31:56,039
they but I'm talking about this place
that they know, and they know it

479
00:31:56,200 --> 00:31:59,759
very very well. It's almost a
member of their family. And so then

480
00:32:00,279 --> 00:32:02,440
of course they're their ears perk up, and they want to know more because

481
00:32:02,839 --> 00:32:07,279
it's not an abstract thing. It's
a place that that's the place that they

482
00:32:07,279 --> 00:32:10,480
couldn't find their phone and and and
you know there's some other mishap, you

483
00:32:10,519 --> 00:32:15,799
know, and and so it's that
kind of intersection between a person's normal life

484
00:32:15,960 --> 00:32:20,319
and this academic life that I can
bring. And it works when you can

485
00:32:20,359 --> 00:32:23,039
connect it with their lives. Yeah, yeah, definitely, I think that's

486
00:32:23,039 --> 00:32:25,839
the That's the big thing is again, people haven't it in front of them,

487
00:32:25,839 --> 00:32:30,039
whether it's a road cut or a
mountain or their favorite hiking trail.

488
00:32:30,759 --> 00:32:34,200
Um. Now, so let's talk
about well, let's I want to talk

489
00:32:34,200 --> 00:32:37,000
about the Farelem plate. We got
to talk about the fair Elm plate,

490
00:32:37,119 --> 00:32:39,440
right, because that's I mean,
that's that's the big one that's dictated so

491
00:32:39,519 --> 00:32:45,400
much of the landscape of North America. But um, I guess, well,

492
00:32:45,480 --> 00:32:50,200
let's just go right to the farelmplate. Where would you Let's tell everyone

493
00:32:50,240 --> 00:32:57,160
about the Farrelm plate and what it's
done for mountain building and for you know,

494
00:32:57,200 --> 00:33:01,480
the current shape of the continent and
everything, um in North America.

495
00:33:01,559 --> 00:33:06,680
Right, I mean where you want
to start? I mean basically, yeah,

496
00:33:06,839 --> 00:33:09,519
I'll start by asking you, how
do you know about the Sharallon plate

497
00:33:09,599 --> 00:33:14,079
and why are you interested in learning
about the Sharon Plate From me, I'm

498
00:33:14,119 --> 00:33:16,920
interested, Well, I'm interested in
the Parlon plate rip because well, I

499
00:33:16,960 --> 00:33:21,359
guess it's it's it's just split up, right, because it's it was.

500
00:33:21,440 --> 00:33:27,240
It was essentially this this piece of
oceanic crust that's subducted beneath, you know,

501
00:33:27,319 --> 00:33:30,279
at an angle beneath the continent,
the Condinal Plate of North America,

502
00:33:30,319 --> 00:33:37,160
you get oceanic crust, which is
heavier generally basalt is what it's composed of,

503
00:33:37,200 --> 00:33:40,039
among other things. Uh. And
that gets recycled roughly every two hundred

504
00:33:40,079 --> 00:33:45,319
million years via plate tectonics, coming
up at spreading boundaries like you have in

505
00:33:45,359 --> 00:33:52,160
the mid Atlantic, and then diving
back beneath the Earth's crust at subduction zones.

506
00:33:52,240 --> 00:33:55,880
And wherever you get subduction zones,
a little ways inland you get volcanoes,

507
00:33:55,920 --> 00:34:01,640
whether it's New Zealand or the Cascades
or Japan, etc. And so

508
00:34:01,799 --> 00:34:06,759
the Fairyland Plate was this piece of
it was a it was a tectonic plate,

509
00:34:06,799 --> 00:34:10,320
a piece of oceanic crust which dived
beneath ended up being fully subducted,

510
00:34:10,679 --> 00:34:15,679
but it was kind of at a
weird um angle, you know, kind

511
00:34:15,679 --> 00:34:20,840
of forming the tail end of a
triangle as it went down. Um.

512
00:34:21,199 --> 00:34:24,960
And so uh is it is it
fully subductive beneath the continental crust? And

513
00:34:24,960 --> 00:34:28,920
then you know you get the Cocoas
plate and what does it want to fuca

514
00:34:29,000 --> 00:34:30,960
to the north. It basically what
was left of it split up into two

515
00:34:31,000 --> 00:34:37,840
other oceanic plates which are still going
beneath the continent. Um. But as

516
00:34:37,840 --> 00:34:40,800
it was going down, it's thought
to have caused all these mountains, this

517
00:34:40,880 --> 00:34:45,039
kind of rumpling of the Earth's crust, all these all these mountains to come

518
00:34:45,119 --> 00:34:49,639
up, um, even as far
away as the you know, Sierra Madre,

519
00:34:49,840 --> 00:34:54,320
Oriental Oriental beneath the you know,
just south of where I am in

520
00:34:54,360 --> 00:34:59,440
Texas, you know. Um,
But I know, I know. Also

521
00:34:59,519 --> 00:35:01,880
there's other theories about what why some
of these mountains have formed. But either

522
00:35:01,920 --> 00:35:05,880
way, I mean, it seems
like no matter what the Paralon plate,

523
00:35:06,519 --> 00:35:09,639
which when did it when did it
fully subduct like thirty million years ago less

524
00:35:09,639 --> 00:35:15,559
than that? Well, yeah,
it's um, there are answers. I'll

525
00:35:15,559 --> 00:35:20,320
give you the answers, but there's
also a new story that kind of is

526
00:35:20,360 --> 00:35:22,760
a revolution and how to view the
history of this Farlon place. Yes,

527
00:35:22,880 --> 00:35:25,679
and I saw your video about that, and that's what I was hoping you

528
00:35:25,719 --> 00:35:30,880
would talk about. Okay, good, By the way, Why did you

529
00:35:30,920 --> 00:35:32,920
invite me to do this? I'm
flattered that you've invited me, Joe,

530
00:35:35,159 --> 00:35:38,800
because I think seeing that video and
and and you wanted to involve No,

531
00:35:38,840 --> 00:35:42,559
I've concept in this series. No, I've been watching you. I've been

532
00:35:42,599 --> 00:35:45,400
watching your videos for uh, you
know a long time. I mean,

533
00:35:45,400 --> 00:35:47,719
we were going to do something together
in March. I just couldn't make it

534
00:35:47,760 --> 00:35:52,280
out there. But oh and oh, I mean I think I thought it'd

535
00:35:52,320 --> 00:35:54,239
be a great conversation. Shit,
it already has been. We're only twenty

536
00:35:54,239 --> 00:35:58,639
eight minutes into it. So that's
why, you know, I think it's

537
00:35:58,880 --> 00:36:00,559
all this stuff is fun to talk
about, and I think putting it out

538
00:36:00,559 --> 00:36:05,400
there in a format that's fun to
listen to for other people, uh,

539
00:36:05,440 --> 00:36:07,000
you know, they gain a lot
of information from it. And that's that's

540
00:36:07,000 --> 00:36:13,360
the main reason, because I think
it's going to be elucidating for other people

541
00:36:13,480 --> 00:36:15,840
to hear, like, oh wow, you know, people who don't know

542
00:36:15,880 --> 00:36:17,880
a lot about geology. Maybe and
maybe they'll, you know, maybe they'll

543
00:36:17,920 --> 00:36:22,679
they'll go home and google what this
ship was. The Fairland plate it's you

544
00:36:22,719 --> 00:36:25,760
know, for example. Okay,
well yeah, let me let me let

545
00:36:25,800 --> 00:36:30,079
me answer your question. I was
chuckling there because this this almost sounded like

546
00:36:30,159 --> 00:36:34,559
you missed the final exam and I
had to call you a get a like

547
00:36:34,639 --> 00:36:38,119
a oral exam to make sure that
you learned the content to the course.

548
00:36:38,639 --> 00:36:43,079
You were kind of breaking it down
for me. It was beautiful. You

549
00:36:43,159 --> 00:36:45,320
did a nice job, by the
way. So yeah, so yeah,

550
00:36:45,360 --> 00:36:52,760
I can basically give the cliff notes
of this lecture that I have on YouTube

551
00:36:52,760 --> 00:36:55,480
called how did the Rocky Mountains form? Question mark, And that's what you

552
00:36:55,519 --> 00:37:00,239
were referring to. So the idea
is that I've been teaching for twenty five

553
00:37:00,320 --> 00:37:05,280
years, this old idea, and
it's still the majority opinion. And the

554
00:37:05,400 --> 00:37:09,800
idea is that when Pangaea started to
break apart, and that's opening the Atlantic

555
00:37:09,800 --> 00:37:15,920
Ocean and having North America start to
split away from Europe and Africa about two

556
00:37:15,000 --> 00:37:21,320
hundred million years ago, that starts
and North America starts drifting west generally,

557
00:37:21,880 --> 00:37:27,679
and there's this huge ocean floor plate
called the Farallon Plate under the waters of

558
00:37:27,679 --> 00:37:30,440
the Pacific. So this is starting
two hundred million years ago. And so

559
00:37:30,559 --> 00:37:36,360
if North America is starting to drift
west and it's a continent, that means

560
00:37:36,400 --> 00:37:40,400
the ocean crust off shore it's going
to start diving to the east beneath this

561
00:37:40,519 --> 00:37:45,559
drifting continent because the ocean crust,
as you said correctly, Joy, that

562
00:37:45,679 --> 00:37:50,679
ocean crust is just fined, but
it's dense and it's basaltic, and so

563
00:37:50,719 --> 00:37:55,800
it's going to want to seduct.
So the old model is the Rocky Mountains

564
00:37:55,840 --> 00:38:04,400
started to develop as a result of
North America drifting west and having this ocean

565
00:38:04,800 --> 00:38:10,920
Farllon plate diving beneath North America to
the east. And at there's still the

566
00:38:10,920 --> 00:38:16,840
old model and the first thing to
develop for this Yerera Nevada Mountains in California.

567
00:38:17,079 --> 00:38:21,079
That's a line of volcanoes. That
was a line of volcanoes. So

568
00:38:21,159 --> 00:38:25,000
like where King's Canyon and Yosemite and
Sekoy are today and the John Near Trail

569
00:38:25,039 --> 00:38:30,239
and Daughter Passed and all that that's
all granted today, but that's where there

570
00:38:30,280 --> 00:38:34,920
was a line of beautiful and Deean
like volcanoes or New Zealand like volcanoes,

571
00:38:34,960 --> 00:38:38,280
where you just were, and that
was because there was a relatively steep angle

572
00:38:38,760 --> 00:38:44,119
to the subduction of the Paarllon plate. And then about eighty five million years

573
00:38:44,119 --> 00:38:49,000
ago, North America is still moving
west. But the model says, suddenly

574
00:38:49,079 --> 00:38:53,920
the angle of the seducting Fallon plate
starts to shallow out, and so those

575
00:38:54,000 --> 00:38:59,599
volcanoes in eastern California shut off and
they crumble away. And that's why we

576
00:38:59,639 --> 00:39:05,679
have editing the Sierra Nevada, and
therefore the mountains to the east, the

577
00:39:05,800 --> 00:39:10,159
Rocky Mountains, start to grow.
But it's the Pherrellon plate that's subducting at

578
00:39:10,159 --> 00:39:16,960
a relatively low angle, and so
it's just kind of causing uplift with this

579
00:39:17,159 --> 00:39:23,559
underlying flat slab subduction of the Pharillon
plate tickling the underbelly. I'm not making

580
00:39:23,599 --> 00:39:30,159
this up of Colorado and Utah and
Idaho. To me, that never sounded

581
00:39:30,280 --> 00:39:34,840
right, but I've taught it for
a long long time. So you make

582
00:39:34,880 --> 00:39:39,119
the rocky mountains not from volcanic activity, but from this shortening the crust and

583
00:39:39,239 --> 00:39:45,880
having pieces of sedimentary layer rock be
shoved to the east or uplifted from below.

584
00:39:45,880 --> 00:39:47,559
In Colorado. How are we doing
so far? Good? I'm yeah,

585
00:39:47,599 --> 00:39:52,679
exactly, this is what I've been
taught and read too. Yes,

586
00:39:52,360 --> 00:39:58,960
So if some of your listeners have
taken a geology class and they did learn

587
00:39:58,960 --> 00:40:02,360
about the Rocky Mountain, that's the
model that they were taught and maybe they'll

588
00:40:02,400 --> 00:40:06,679
go to college this fall. Listeners, if you go to college this fall,

589
00:40:06,719 --> 00:40:09,199
tech geology one on one, nine
out of ten instructors are going to

590
00:40:09,239 --> 00:40:15,880
teach what I just said in some
sort of form. But I'm hip to

591
00:40:15,960 --> 00:40:22,519
this new set of work where there's
something called tomography where you can actually study

592
00:40:22,599 --> 00:40:28,320
earthquake speeds through the crust and through
the mantel, and you can make images

593
00:40:28,360 --> 00:40:31,639
almost like a cat scan of what
it's like underneath North America. Way they

594
00:40:31,679 --> 00:40:37,000
held down there like a thousand kilometers
two thousand kilometers below North America, and

595
00:40:37,119 --> 00:40:44,880
there are slabs of ocean floor that
did not melt when they go underneath a

596
00:40:45,000 --> 00:40:49,760
continent, they continue as an ocean
slab, and the freaking things starts sinking

597
00:40:50,599 --> 00:40:53,880
vertically down through the mantle. And
this technology now exists where you can actually

598
00:40:53,960 --> 00:41:00,320
find those old pieces of ocean floor. So that old model of the Alon

599
00:41:00,440 --> 00:41:05,880
plate making Sierra Nevadas and California and
then making the Rockies was back fifty years

600
00:41:05,880 --> 00:41:12,840
ago, before we had this ability
to basically quote unquote see into the mantle,

601
00:41:14,599 --> 00:41:19,360
I said Toraphy, before the tomography, totally right. I mean that

602
00:41:19,440 --> 00:41:22,440
was at the dawn of plate tectonics. People were just proud of themselves for

603
00:41:22,599 --> 00:41:25,960
realizing that things you're moving around,
well not all we can. We've got

604
00:41:25,960 --> 00:41:30,360
these these magic pair of glasses where
we can see into this mantle. And

605
00:41:30,480 --> 00:41:36,199
you're like, okay, well,
where is this farallon plate that's been diving

606
00:41:36,360 --> 00:41:40,440
eastward underneath North America for two hundred
million years. And the punchline is it's

607
00:41:40,480 --> 00:41:45,639
not down there. There's not even
a hint of it down there. Instead,

608
00:41:45,239 --> 00:41:54,400
there's this slab of formerly subducted ocean
plate material that's a vertical wall underneath

609
00:41:55,559 --> 00:42:01,360
Florida, underneath New York City.
And you're like, well, you're like,

610
00:42:01,400 --> 00:42:06,119
well, wait a minute, I
don't understand what is that thing and

611
00:42:06,239 --> 00:42:09,920
how would that have anything to do
it's forming the Rocky Mountains. The answer

612
00:42:10,039 --> 00:42:15,239
is it's that that vertical slab that's
underneath the east coast today that's like fifteen

613
00:42:15,320 --> 00:42:22,639
hundre kilometers below Orlando, used to
be in the in the Pacific Ocean.

614
00:42:22,199 --> 00:42:27,920
And if you're with me, that
makes sense because North America since Pangaea time

615
00:42:28,000 --> 00:42:30,360
has been drifting west. If we
go back, if we run the clock

616
00:42:30,440 --> 00:42:34,920
backwards and we get North America back
to where it was one hundred and fifty

617
00:42:34,920 --> 00:42:39,119
million years ago, suddenly that stuff
that's underneath Florida is in the Pacific.

618
00:42:39,360 --> 00:42:44,360
I don't know, is that making
sense? Yeah? Yeah, yeah.

619
00:42:44,480 --> 00:42:50,800
So the question then is what is
that vertical slab underneath Florida underneath New York

620
00:42:50,880 --> 00:42:54,679
City. And there's different geometries that
you can play with, but the punchline

621
00:42:54,800 --> 00:43:04,199
is it's probably ocean crust that's sub
did westward instead of eastward. And so

622
00:43:04,239 --> 00:43:09,119
this idea of the Farallon plate subducting
beneath North America for such a long time

623
00:43:10,320 --> 00:43:15,679
is maybe erroneous, maybe never actually
did happen that way. And there's a

624
00:43:15,719 --> 00:43:22,199
whole nother plate that's no longer around
that was subducting beneath a fixed island arc

625
00:43:22,280 --> 00:43:25,960
that North America slammed into. And
I know that's impossible to visualize in just

626
00:43:27,000 --> 00:43:30,079
a few minutes, but that lecture
waits for it if you want to see

627
00:43:30,079 --> 00:43:31,639
it more. It sounds like you
did see parts of it. I did.

628
00:43:31,719 --> 00:43:36,039
Yeah, I remember you talking about
the you know, the them catching

629
00:43:36,079 --> 00:43:39,440
that reading of all this stuff beneath
the east coast, this ocean flard beneath

630
00:43:39,440 --> 00:43:43,679
the east coast. So but I
mean, so basically, what would have

631
00:43:43,679 --> 00:43:46,960
happened was there was a westward subduction
zone before there was an eastward one,

632
00:43:47,079 --> 00:43:53,440
and North America overrode it. And
then what exactly would have happened to the

633
00:43:53,440 --> 00:43:58,559
Farrelon plate. Does that mean that
the Farrelon plate didn't die or does that

634
00:43:58,599 --> 00:44:01,559
mean there was no ferol On plate, Like the Farrellon plate never died.

635
00:44:01,840 --> 00:44:07,239
It's been alive all along inside of
us. You know, you can't kill

636
00:44:07,280 --> 00:44:14,280
the spirit of the far What is
it? What are some possible theories?

637
00:44:14,920 --> 00:44:20,360
Uh, you know where that's true? Of where where it is. I'll

638
00:44:20,400 --> 00:44:23,519
try verbally, but of course the
best way to do it is to do

639
00:44:23,559 --> 00:44:29,760
it kind of graphically. Yeah.
The idea is it's all about the timing.

640
00:44:31,079 --> 00:44:34,880
For those that were able to follow
what I was saying a few minutes

641
00:44:34,920 --> 00:44:38,880
ago, there was a huge collision
about one hundred million years ago, and

642
00:44:39,079 --> 00:44:44,880
that one hundred million year collision that
kicked off the building of the Rocky Mountains

643
00:44:44,920 --> 00:44:49,599
did not involve the Farallon plate with
this new model, but instead it was

644
00:44:50,280 --> 00:44:57,360
a inching closer and closer of a
drifting North America getting closer and closer to

645
00:44:57,480 --> 00:45:01,119
this fixed island arcs. Think like
a b micro continent, like a bunch

646
00:45:01,119 --> 00:45:05,199
of Japan and New Zealand things out
there in the water, but they're not

647
00:45:05,320 --> 00:45:10,079
drifting North America is. So here
comes North America getting closer and closer and

648
00:45:10,119 --> 00:45:17,440
then plowing into this fixed island arc
that starts the Rocky Mountain uplift. There's

649
00:45:17,480 --> 00:45:22,800
no Farallon plate yet. But to
answer your question, Joey ask her one

650
00:45:22,840 --> 00:45:29,559
hundred million years ago, now the
fixed Island and North America are drifting together.

651
00:45:30,760 --> 00:45:35,119
The Rockies are growing. But now
we do have eastward subduction of the

652
00:45:35,119 --> 00:45:39,199
Farallon plate. So the Farallon plate
did exist, but it's a younger story

653
00:45:39,239 --> 00:45:44,400
than previously. Ah okay, so
it was in the island arc just kind

654
00:45:44,440 --> 00:45:50,000
of got a created onto a westward
moving North America like a piece of spackling

655
00:45:50,039 --> 00:45:53,559
putty to a rumba kind of right. Is that a way to think it

656
00:45:53,559 --> 00:45:59,199
works? Yeah, that's one way. My favorite is that there's a moose

657
00:45:59,239 --> 00:46:02,119
in the middle of the road,
and the old buick is heading towards the

658
00:46:02,599 --> 00:46:06,960
moose, and we're gonna, Jesus, we're gonna hit the moose. And

659
00:46:07,000 --> 00:46:09,920
we're just gonna keep rolling. We're
not gonna We're not You're just gonna continue,

660
00:46:09,920 --> 00:46:14,679
and the moose is gonna ride the
hood. Why's it gonna be a

661
00:46:14,719 --> 00:46:15,679
buick? You don't want to do
that too? A buick? You know

662
00:46:15,679 --> 00:46:19,480
how hard it is to find a
buick in Chicago. Me and al Scorch

663
00:46:19,559 --> 00:46:23,960
have been looking for a like a
thoroughly rusted around the wheel wells circa nineteen

664
00:46:24,320 --> 00:46:28,519
eighty nine buick in Chicago. We
can't you know, if he were to

665
00:46:28,599 --> 00:46:30,880
hear that you were talking about a
metaphor of destroying a buck, he would

666
00:46:30,920 --> 00:46:37,039
cry. But either way, the
metaphor works so well. That's it's certainly

667
00:46:37,039 --> 00:46:39,400
interesting as hell, and it would
probably, you know, worth this true.

668
00:46:39,960 --> 00:46:45,800
I might explain a few other things
geological phenomenon in North America as well.

669
00:46:45,840 --> 00:46:49,480
But it's again, it seems so
hard. You know, we don't

670
00:46:49,519 --> 00:46:52,280
have a time lapse the eye.
God, wouldn't it be great? I

671
00:46:52,280 --> 00:46:57,320
always think about this, If you
could have like a fixed satellite one hundred

672
00:46:57,400 --> 00:47:00,920
million years ago and just do a
time lapse video, you know, looking

673
00:47:00,000 --> 00:47:06,920
down and like North America Christ then
just see how this really, you know,

674
00:47:07,039 --> 00:47:10,800
panned out. You'd see the western
interior seaway. You'd see maybe this

675
00:47:10,920 --> 00:47:14,480
island arc that no one knew was
there, that kind of thing. So

676
00:47:15,079 --> 00:47:16,840
but but either way, the Rocky
Mountains, I mean, how how old

677
00:47:16,880 --> 00:47:21,559
are they? I didn't oh wow, oh two hundred saying two hundred and

678
00:47:21,559 --> 00:47:24,760
eighty five million years ago a mountain
building process? Is that right? No?

679
00:47:25,000 --> 00:47:34,679
I don't think so. I mean
generally the Rockies were intensely building less

680
00:47:34,679 --> 00:47:37,880
than one hundred million years ago and
ending about fifty million years yeah, eighty

681
00:47:38,119 --> 00:47:40,400
yeah, I see eighty and fifty
five. I don't know. I don't

682
00:47:40,440 --> 00:47:44,960
know what this two eighty five that's
from the USGS. Oh, maybe that's

683
00:47:45,000 --> 00:47:49,079
ancient. That's that's for geology of
Rocky Mountain National Park. That seems a

684
00:47:49,119 --> 00:47:52,159
little more localized in what it's talking
about. We got we got, we

685
00:47:52,280 --> 00:47:57,119
got problems here. Like you know, you go to different sites, there's

686
00:47:57,159 --> 00:48:01,239
different numbers, there's different research groups. There's old information, there's new information.

687
00:48:02,360 --> 00:48:06,639
It's hard to grab a hold of
something and so that's you know,

688
00:48:06,719 --> 00:48:10,400
when I try to communicate geology,
I say, well, here's here's some

689
00:48:10,559 --> 00:48:16,440
data that everybody in science agrees on. Let's put a story together. But

690
00:48:16,880 --> 00:48:21,840
I'm always careful to say, like, it's based on the data that we

691
00:48:21,920 --> 00:48:24,159
have. And then if I if
I kind of fashion it that way,

692
00:48:24,239 --> 00:48:28,840
then then there's not a lot of
pushback like a wait a minute, I

693
00:48:28,880 --> 00:48:32,480
saw I saw different dates. It's
it's it's such a the Internet is so

694
00:48:34,079 --> 00:48:37,880
powerful but also frustrating as and I'm
sure you know as well. It's just

695
00:48:38,039 --> 00:48:45,360
trying to well, you know,
how to do it beautifully. And it's

696
00:48:45,400 --> 00:48:51,199
it's this it's this local thing that
you can eventually plug into something big.

697
00:48:51,280 --> 00:48:54,480
I think that's that's an undervalued part
of this whole science communication thing. You

698
00:48:54,599 --> 00:48:59,280
take something very very local, like
you're so great with holding things in your

699
00:48:59,280 --> 00:49:05,639
hand in but then you can also
change the scale and say this is symptomatic

700
00:49:05,639 --> 00:49:08,159
of something that's happening across three states, and then you can go bigger and

701
00:49:08,199 --> 00:49:10,719
bigger. And I try to do
the same thing with geology. Yeah,

702
00:49:10,719 --> 00:49:15,039
I mean, I think with a
lot of with a lot of geologic phenomena

703
00:49:15,159 --> 00:49:19,920
and landscapes, and structural geology and
stuff like this. The simple fact is

704
00:49:19,960 --> 00:49:22,239
that a lot of shit we just
don't know for sure. There's there's there's

705
00:49:22,280 --> 00:49:25,440
guesses out there. Like when I
was trying to figure out you know,

706
00:49:27,039 --> 00:49:30,559
one of my favorite mountain ranges in
the world is the Sierra Madre Orientel,

707
00:49:30,960 --> 00:49:34,679
which is, uh, just because
the fucking plants there are incredible. And

708
00:49:34,719 --> 00:49:37,920
you've got these, you know what
were originally horizontal seafloor beds that have now

709
00:49:37,960 --> 00:49:42,920
been flipped up nearly vertical and just
created some of the coolest habitat. I

710
00:49:42,960 --> 00:49:46,119
mean you look at it on like
a Google terrain layer and it looks like

711
00:49:46,119 --> 00:49:52,039
a carpet that's been pushed up against
a you know, a doorframe on a

712
00:49:52,079 --> 00:49:54,360
hardwood floor, you know, and
so that. But I was trying to

713
00:49:54,360 --> 00:49:58,400
look at how this was formed.
I couldn't. I mean I was asking

714
00:49:58,440 --> 00:50:01,039
other geologists too. Yeah, yes, we don't really know. I mean,

715
00:50:01,119 --> 00:50:07,199
obviously there was a compression force from
somewhere, but why did it start

716
00:50:07,599 --> 00:50:10,000
there on the east, you know, like on the east side of those

717
00:50:10,039 --> 00:50:14,360
mountains, Like it looks like the
compression came from the west and then they

718
00:50:14,440 --> 00:50:16,679
hit something on the east and that's
why they built up. You know,

719
00:50:16,679 --> 00:50:21,039
you got that rimpling effect, rumpling
effect, rippling, whatever the hell it's

720
00:50:21,079 --> 00:50:22,559
called, you know, and no
one really know, and I couldn't figure

721
00:50:22,599 --> 00:50:25,880
it out, and I was just
kind of there's there's a theory out there

722
00:50:27,000 --> 00:50:30,320
that seems to hold a lot of
water for the time being, but who

723
00:50:30,360 --> 00:50:32,159
knows. I mean again, we
don't we don't know. There's no there's

724
00:50:32,199 --> 00:50:37,840
no time lapse videography of what happened. Well, you're tapping into something that's

725
00:50:37,880 --> 00:50:42,960
important. It's okay to say the
words I don't know. If somebody asks

726
00:50:43,000 --> 00:50:46,079
you a question, you can say
I don't know, and you can even

727
00:50:47,280 --> 00:50:51,639
zoom it out and say we don't
know. Yeah, to have this.

728
00:50:51,880 --> 00:50:55,599
So it's back to this. You
know, you are genuine, but you're

729
00:50:55,639 --> 00:51:00,840
you're also open and you are embraced
seeing the fact that you are continuing to

730
00:51:00,920 --> 00:51:08,360
learn and being a curious person.
People they want that, students of all

731
00:51:08,400 --> 00:51:14,880
ages, viewers, listeners, they
want to be reassured that there's so much

732
00:51:14,920 --> 00:51:19,960
that is unknown and that's not a
negative, that's a positive. That's exciting.

733
00:51:20,000 --> 00:51:24,000
It hasn't all been figured out for
sure. So these these University Ivory

734
00:51:24,079 --> 00:51:29,239
Tower snobs who just insist that they
have all the answers and the way that

735
00:51:29,320 --> 00:51:35,480
they speak to everybody is from on
high looking down. It infuriates me in

736
00:51:35,519 --> 00:51:42,199
my style and maybe your style as
well. Just rooted in like a reaction

737
00:51:42,320 --> 00:51:45,039
against that, Like I had so
many professors like man, if I ever

738
00:51:45,079 --> 00:51:47,760
teach, I'm not doing what that
fucker's doing up there. Yeah, I

739
00:51:47,800 --> 00:51:52,039
can't even picture that person in the
in the grocery store. They don't do

740
00:51:52,159 --> 00:51:54,119
they even exist in real life.
Well, I think the ego and anything,

741
00:51:54,159 --> 00:51:58,360
the ego and anything takes the fun
out of it. That's not fun.

742
00:51:58,000 --> 00:52:02,519
No one and no one likes that. And what's another note. What's

743
00:52:02,639 --> 00:52:06,599
fun is you know, pondering like
God, how the shit did that happen?

744
00:52:07,000 --> 00:52:09,199
Like how do I love stand staring
at a fucking road cut and being

745
00:52:09,199 --> 00:52:14,119
like, God, damn, how
the fuck did that happen? I trying

746
00:52:14,119 --> 00:52:16,239
to figure this out, like thinking
about it. Someone okay, someone told

747
00:52:16,280 --> 00:52:20,119
me, but I don't know.
I can't envision that, like how does

748
00:52:20,159 --> 00:52:22,159
it? You know, just trying
to find I mean, that's what's really

749
00:52:22,159 --> 00:52:24,719
fun. I mean, that's what
is really Because now you've got a puzzle

750
00:52:24,719 --> 00:52:28,079
in front of you've got a mystery, you got a riddle, and you're

751
00:52:28,119 --> 00:52:31,960
you know, you're trying to understand
things on a scale much grander than yourself

752
00:52:32,000 --> 00:52:37,119
and much longer than your own,
you know, meager human lifespan. And

753
00:52:37,199 --> 00:52:39,760
that's what I think. That's another
part of the you know, the geologic

754
00:52:39,840 --> 00:52:42,920
time scale. Man, I don't
know why they don't teach that shit in

755
00:52:42,960 --> 00:52:45,519
first grade. They really should be. It is It is such a it

756
00:52:45,679 --> 00:52:50,440
is so important and it is what
is the foundation of our entire world.

757
00:52:50,519 --> 00:52:54,280
Like teach, you know, chronological
landmarks along the geologic time scale. When

758
00:52:54,280 --> 00:52:58,639
did plants evolve? When did life
evolve? When did photosynthesis evolved? When

759
00:52:58,639 --> 00:53:01,760
did the ox When did you know
the atmosphere become full of oxygen? What's

760
00:53:01,840 --> 00:53:06,639
what are the oldest fossils of life? You know, three point eight billion

761
00:53:06,679 --> 00:53:10,280
years ago, Great oxygenation, oxygenation
event two billion years ago? Uh,

762
00:53:10,559 --> 00:53:14,760
you know, first few karyotic life
forms one billion years ago, land plants

763
00:53:14,800 --> 00:53:17,599
four hundred and thirty eight million years
ago, Cambrian explosion five hundred you know,

764
00:53:17,639 --> 00:53:21,599
whatever, all that shit that's important. Those are things everyone should know.

765
00:53:22,280 --> 00:53:25,320
You know, it's so fucking and
it just what it does to the

766
00:53:25,360 --> 00:53:30,719
way that you perceive the world is
phenomenal. I mean, it's such a

767
00:53:30,880 --> 00:53:35,280
huge shift from how we perceive the
world now, which is either through no

768
00:53:35,360 --> 00:53:39,760
offense to anybody that's somewhat deranged view
of religion, which whatever religion does for

769
00:53:39,800 --> 00:53:44,119
people on an emotional level, it
does jack shit for people on any kind

770
00:53:44,159 --> 00:53:47,440
of scientific level in terms of understanding
the world. So, you know,

771
00:53:47,480 --> 00:53:52,880
I don't know anyway that's that's undering. You're onto something else. Here's this

772
00:53:52,960 --> 00:53:59,199
is really interesting to me. Thank
you for this. Occasionally somebody will say,

773
00:53:59,280 --> 00:54:00,960
you know, if there's a lot
of feedback on some of the stuff

774
00:54:02,440 --> 00:54:09,039
that they see or hear from me. Occasionally somebody's very precise in their language

775
00:54:09,039 --> 00:54:14,800
and they am reminding me or maybe
helping me see for the first time that

776
00:54:15,840 --> 00:54:23,360
that there's reverence and there's kind of
awe and at the power of all this,

777
00:54:23,880 --> 00:54:29,519
and yeah, the mystery part,
but it's it is almost like tapping

778
00:54:29,559 --> 00:54:34,480
into a religious thing or maybe what
religion was for some people who no longer

779
00:54:34,559 --> 00:54:38,079
than practice, and then they're maybe
subconsciously or something looking for something else to

780
00:54:39,760 --> 00:54:45,159
celebrate in the same sort of way. But yeah, if you're talking about

781
00:54:45,239 --> 00:54:50,519
millions of years, or you're talking
about the energy necessary to lift the Cascade

782
00:54:50,559 --> 00:54:54,480
Mountains or to take some granite in
Mexico and have it now up in British

783
00:54:54,519 --> 00:55:00,920
Columbia. I mean that is awesome
stuff, not in the casual slang,

784
00:55:00,039 --> 00:55:05,519
but like truly like the awe and
the power. Yeah, oh yeah,

785
00:55:05,519 --> 00:55:09,000
it doesn't it doesn't mean. It
does help you see your world in a

786
00:55:09,119 --> 00:55:14,880
in a different way, and oftentimes
it's energizing in a positive way. I

787
00:55:14,920 --> 00:55:19,159
think too. For what's really good
for me when I'm trying to put something

788
00:55:19,199 --> 00:55:22,039
in a video and teach people,
is I have to go back and try

789
00:55:22,079 --> 00:55:28,880
to remember how I thought of the
world before I learned all this stuff versus

790
00:55:28,920 --> 00:55:32,519
now, how did I like?
Because it was just so it just blew

791
00:55:32,599 --> 00:55:37,519
my mind and it took a while
to set in. Whether it's like principles

792
00:55:37,559 --> 00:55:42,840
of monophyletic and polyphyletic in terms of
biology and evolution, in taxonomy, phylogeny,

793
00:55:42,880 --> 00:55:44,880
shit like that, or whether it's
you know, in terms of plate

794
00:55:44,880 --> 00:55:50,719
tectonics and and and you know,
basically, how does it fucking you know,

795
00:55:51,320 --> 00:55:54,440
marine fossil end up ten thousand feet
in the air on the side of

796
00:55:54,480 --> 00:55:58,079
a mountain, you know, it
was I and I have to go back

797
00:55:58,079 --> 00:56:00,719
and be like, okay, well
how would I look kind of questions what

798
00:56:00,880 --> 00:56:04,960
I ask like, why would it
be so hard for me to understand this

799
00:56:05,000 --> 00:56:07,960
initially? Why was it so hard
for me to understand its initially? You

800
00:56:07,039 --> 00:56:13,559
know? And that's what helps me
better communicate this to other people because people

801
00:56:13,800 --> 00:56:15,559
a lot of people don't know the
questions to ask at first. It just

802
00:56:15,719 --> 00:56:20,800
is it's hard, you know,
not everyone knows what questions are going to

803
00:56:20,840 --> 00:56:24,679
get me to the answer I'm looking
for. So, so you started doing

804
00:56:24,719 --> 00:56:29,760
this ten fifteen years ago, it
sounds like I'm just thinking of the videos

805
00:56:29,800 --> 00:56:32,000
now in your YouTube channel. Let's
say, so, how has your style

806
00:56:32,159 --> 00:56:38,360
changed over the years are you are
you doing something totally differently in your mind

807
00:56:38,480 --> 00:56:43,079
than you were ten fifteen years ago? Oh yeah, yeah, oh yeah.

808
00:56:43,119 --> 00:56:45,519
I mean what I've slowly been doing
and I think it probably started in

809
00:56:45,519 --> 00:56:50,239
two thousand and six. That's when
I went to City College of San Francisco

810
00:56:50,320 --> 00:56:52,440
and I was like, you know
what, I don't want to go back

811
00:56:52,440 --> 00:56:57,079
to school because I had gone to
school two years earlier for two years a

812
00:56:57,119 --> 00:57:00,639
few years earlier, and I was
like studying sociology or something that no offense

813
00:57:00,679 --> 00:57:02,960
to any sociology people, but I
thought was kind of lame. And I

814
00:57:04,039 --> 00:57:06,320
was like, Nah, this ain't
it. This isn't the answers I'm looking

815
00:57:06,360 --> 00:57:12,679
for. And so I went back
to school and I'm trying to collect my

816
00:57:12,679 --> 00:57:15,360
thoughts here and there. It was
like two thousand and six, yeah,

817
00:57:15,400 --> 00:57:20,840
and I think like that's when I
began the process that that I've been on

818
00:57:20,960 --> 00:57:25,760
ever since, which is slowly building
paradigm, like a perception of my world.

819
00:57:27,199 --> 00:57:31,280
And by nailing down things like the
chronological landmarks and the geologic time scale

820
00:57:31,360 --> 00:57:36,679
or how evolution works. The evolution
shit was really hard for me to kind

821
00:57:36,679 --> 00:57:38,440
of wrap my head around how certain
things evolve, Like how does the plant

822
00:57:38,480 --> 00:57:44,320
evolve to look like a rock?
How does a rattlesnake, you know,

823
00:57:44,360 --> 00:57:47,280
the same species of rattlesnake like speckled
rattlesnakes in the Mojabi. How does each

824
00:57:47,760 --> 00:57:54,559
different population resemble the type of substrate
that it lives on, you know,

825
00:57:54,599 --> 00:58:00,840
whether it's purple rhyolite or pink granite
or or you know, white. And

826
00:58:00,880 --> 00:58:02,719
it's true, I mean these and
these reptiles, they're not like chameleons.

827
00:58:02,719 --> 00:58:07,440
They can't just shift, you know, they don't change overnight. It takes

828
00:58:07,599 --> 00:58:14,159
generations, you know, of these
things being presumably culled out by hawks that

829
00:58:14,239 --> 00:58:15,360
can detect them. But I mean, you know, how does that kind

830
00:58:15,360 --> 00:58:20,000
of mimicry, that camouflage evolve that
kind of thing. So that's what I've

831
00:58:20,000 --> 00:58:22,920
slowly been doing ever since. I
guess is these questions really popped up in

832
00:58:22,960 --> 00:58:25,800
my mind two thousand and five,
two thousand and six in response to seeing,

833
00:58:27,320 --> 00:58:30,320
you know, railroad cuts when I
was riding freight trains, or just

834
00:58:30,400 --> 00:58:32,960
having questions about the world, realizing
I was a jackaspect that I was ignorant

835
00:58:34,000 --> 00:58:36,440
of a lot of things, and
then slowly being like, you know what,

836
00:58:36,480 --> 00:58:39,559
I'm going to start piecing together my
own perception of the world around me

837
00:58:39,599 --> 00:58:45,320
because I need to know, you
know, the context that I exist in

838
00:58:45,519 --> 00:58:49,400
and all these things around me.
So and that's one thing. But then

839
00:58:50,119 --> 00:58:54,159
having the instincts to start making videos
or to make making programs, that's a

840
00:58:54,199 --> 00:59:00,639
totally different layer on this. So
why the move to the video stuff as

841
00:59:00,639 --> 00:59:06,199
you were continuing to learn, Well, I think I was just sharing stuff

842
00:59:06,239 --> 00:59:09,599
I already knew, and then you
know, in terms of making videos like

843
00:59:09,639 --> 00:59:13,920
that became an inspiration to learn more. Like I still learn a lot like

844
00:59:14,000 --> 00:59:15,440
what you know, I was just
in New Zealand, and I was I

845
00:59:15,480 --> 00:59:20,159
had no idea. They've got,
you know, a few convergent, evolutionarily

846
00:59:20,159 --> 00:59:22,559
convergent traits among the flora over there, the plants over there, that these

847
00:59:22,559 --> 00:59:28,400
plants have evolved in response to these
now extinct nine different species of moas,

848
00:59:28,440 --> 00:59:31,239
these giant flightless birds that were built
like fucking tanks. And the thigh bones

849
00:59:31,239 --> 00:59:35,400
on these things were huge. You
know, they look like cow thigh bones,

850
00:59:36,000 --> 00:59:39,159
the femur or whatever as I think
that's the thigh bones. Anyway,

851
00:59:39,159 --> 00:59:42,960
you get the point. But and
so I had no idea, and so

852
00:59:43,039 --> 00:59:45,119
I just you know, going there, I learned. I mean, I

853
00:59:45,159 --> 00:59:49,119
don't know all this shit already.
I learn as I go, too,

854
00:59:49,159 --> 00:59:51,599
and I'll professionally be learning as I
go, and I'll be learning as I

855
00:59:51,639 --> 00:59:54,440
go till the day I fucking die. And that's what makes life so fun,

856
00:59:54,559 --> 00:59:58,360
you know, that's what makes you
never stop learning. You know,

857
00:59:58,840 --> 01:00:00,880
when you learn a certain thing,
boom, you got you Now you have

858
01:00:01,000 --> 01:00:04,400
this knowledge. Now you share with
other people. But you've got a ton

859
01:00:04,440 --> 01:00:07,360
more to learn yourself still, And
that's the way I guess it's the way

860
01:00:07,360 --> 01:00:09,320
I view the world. So that's
what I've been doing. So that's kind

861
01:00:09,320 --> 01:00:13,440
of what I view my life and
my perception of the world around me as

862
01:00:13,480 --> 01:00:16,519
a puzzle that I'm slowly piecing together, you know. And it started fifteen

863
01:00:16,559 --> 01:00:21,280
years ago. It really started fifteen
years ago, and so and it makes

864
01:00:21,280 --> 01:00:23,519
this stuff endlessly fascinating. There is
you know, now I'm getting into all

865
01:00:23,599 --> 01:00:29,159
kinds of other fields and studying all
kinds of different things that that started with

866
01:00:29,199 --> 01:00:34,400
this one, this one seed that
sprouted. You know, that's attractive,

867
01:00:34,480 --> 01:00:38,840
that's inspiring that you're piecing this together
for yourself. And I don't need you

868
01:00:38,880 --> 01:00:42,519
to lay down in the couch here. As I ask more personal questions,

869
01:00:43,039 --> 01:00:49,800
I was gonna say, what about
this sharing motivated you? You must get

870
01:00:49,840 --> 01:00:54,239
something out of the reaction that you
get from viewer comments or emails or whatever,

871
01:00:54,440 --> 01:00:59,320
like it must feel good it does
for me to put this stuff out

872
01:00:59,360 --> 01:01:02,360
there and then have a bunch of
positive reaction. Is that true for you

873
01:01:02,360 --> 01:01:05,719
too? Yeah? I mean,
yeah, it's it's not them. It's

874
01:01:05,960 --> 01:01:07,400
it's not the comments. Because I
think a lot of people. I think

875
01:01:07,440 --> 01:01:12,920
some people just listen for you know, the comedy or the the fucking Life

876
01:01:12,920 --> 01:01:15,480
cent or whatever. But I think
the most fulfilling thing is, you know,

877
01:01:15,639 --> 01:01:17,679
when you get those emails where you're
like, you change the way I

878
01:01:17,679 --> 01:01:21,119
look at the world, you know, and now I got a job in

879
01:01:21,199 --> 01:01:23,119
botany, and now I'm working at
my local botanic garden, I went back

880
01:01:23,119 --> 01:01:25,960
to school, all this shit.
I mean, that's that's the best that

881
01:01:27,039 --> 01:01:29,440
when I get those, I'm like, fuck yeah, Like that's when I

882
01:01:29,519 --> 01:01:31,320
was That's what I was going for. Like I don't give a fuck about

883
01:01:31,719 --> 01:01:35,880
you know, getting pass on the
back and all that. Uh it feels

884
01:01:35,880 --> 01:01:38,920
good sometimes, but it's what really
does it is the knowing that like you're

885
01:01:39,000 --> 01:01:43,719
slowly changing. In effect, you're
slowly changing the world. You're changing a

886
01:01:43,800 --> 01:01:50,679
culture, very very in a very
minute way, because there's obviously but you're

887
01:01:50,679 --> 01:01:53,679
still getting people to look at the
world in a way that they may not

888
01:01:53,800 --> 01:01:57,440
have looked at it before. And
it's a it's a way that we need

889
01:01:58,039 --> 01:02:00,679
more people to look at the world, especially in this country, which I

890
01:02:00,679 --> 01:02:06,840
feel like is getting increasingly dumber for
whatever reason, you know, But like

891
01:02:07,239 --> 01:02:13,079
you go to other first world countries
and lay people have an innate awareness many

892
01:02:13,079 --> 01:02:16,280
of them do of you know,
their landscapes, their geology, they're they're

893
01:02:16,360 --> 01:02:20,119
they're not even first world country.
They just say first world because that's what

894
01:02:20,159 --> 01:02:23,320
you know, we compare America to
right, although America's sometimes you can call

895
01:02:23,320 --> 01:02:25,519
it a third world country with a
Gucci Bilt, you know, the way

896
01:02:25,559 --> 01:02:30,119
it's going, the erosion of the
middle class here. But that that aside,

897
01:02:30,119 --> 01:02:32,239
I mean, you know, you
go to other places and there's just

898
01:02:32,519 --> 01:02:38,000
common there's just a more general awareness. There's I guess, better education.

899
01:02:38,000 --> 01:02:43,199
I mean, should you hear all
this stuff about how China's directing their you

900
01:02:43,239 --> 01:02:47,159
know, their population to become more
educated. Like there, their pop culture,

901
01:02:47,280 --> 01:02:52,519
their social media, you know,
is different in that regard, and

902
01:02:52,599 --> 01:02:55,559
so I think that's and that's that
leads to a better quality of life and

903
01:02:55,599 --> 01:02:59,400
a better world for everybody. It
really does. Man, you get less

904
01:02:59,440 --> 01:03:02,079
dummies out there, You get less
just you know, unthinking consumers. You

905
01:03:02,119 --> 01:03:08,119
get more conscious people who are and
who also have a tide of their land,

906
01:03:08,119 --> 01:03:10,840
and you know, the fulfillment that
they get from that. I think

907
01:03:10,880 --> 01:03:14,920
it's it's really good for people.
So that's what that's what it feels the

908
01:03:14,920 --> 01:03:17,039
best. Man, Well, you're
doing it. You are, You are

909
01:03:17,079 --> 01:03:22,880
actually doing it, and it may
at times feel like it's a very small

910
01:03:22,960 --> 01:03:25,119
drop in the bucket thing. They're
probably other times when it does feel like,

911
01:03:25,159 --> 01:03:30,000
holy shit, there's a lot of
people here and and they are following

912
01:03:30,039 --> 01:03:32,159
what I'm doing. And you're getting
more and more of those emails that are

913
01:03:32,159 --> 01:03:36,960
saying, uh, you know,
you're a very important person in my life,

914
01:03:37,039 --> 01:03:40,480
Joey, and I changed this and
that about myself because it's you've inspired

915
01:03:40,480 --> 01:03:45,760
me to do x y and Z. Universities are not doing that. Universities

916
01:03:45,800 --> 01:03:51,000
are dinosaurs and they are slowly dying. And I'm doing more and more with

917
01:03:51,079 --> 01:03:53,440
a YouTube channel because I can do
it in my own way. I think

918
01:03:53,519 --> 01:04:00,760
similar to you. And it's it's
that freedom to pursue things and to be

919
01:04:01,000 --> 01:04:10,000
real, nimble and responsive to folks
in real life. Um, that university

920
01:04:10,039 --> 01:04:15,519
setup is just unable. They're unwilling
or unable to recognize some of the stuff

921
01:04:15,599 --> 01:04:17,840
that you're doing. Yeah, it's
it's sad man, I mean, and

922
01:04:17,920 --> 01:04:21,039
I hear a lot of people in
academia, Like most of my friends in

923
01:04:21,079 --> 01:04:24,960
academia, the people that get along
with are actually older, you know,

924
01:04:25,079 --> 01:04:30,039
there they were. I mean,
I've pissed off plenty of plenty of people

925
01:04:30,039 --> 01:04:33,559
in academia too. Surprisingly it's mostly
been the younger people. It's weird,

926
01:04:33,639 --> 01:04:38,159
it's it's but whatever anyway, Um, but I hear a lot of people,

927
01:04:38,920 --> 01:04:43,159
yeah, young, young, young
botany professors are are fans of you

928
01:04:43,480 --> 01:04:45,119
or younger people, yeah, you
know, I think they tend to be

929
01:04:45,159 --> 01:04:48,400
a little bit stiffer in some ways. And humorists. I get plenty of

930
01:04:48,519 --> 01:04:53,880
people that are young botany you know, people in academia who like it too.

931
01:04:53,880 --> 01:04:56,840
But I get I think a lot
of people just don't know how to

932
01:04:56,880 --> 01:05:00,639
take it, and they don't yeah, you know, they don't catch the

933
01:05:00,679 --> 01:05:03,280
humor in it, or maybe they're
from generally more well off background. I

934
01:05:03,280 --> 01:05:05,840
don't know, I have no idea, but I've you know, I've got

935
01:05:05,960 --> 01:05:12,679
friends, a lot of friends who
are actually like older professors you know,

936
01:05:12,760 --> 01:05:15,920
or have been in academia for a
while, who are obviously, you know,

937
01:05:15,079 --> 01:05:19,239
not very stiff, because that doesn't
I don't think anyone, you know,

938
01:05:19,239 --> 01:05:23,400
with a stick up their ass is
going to enjoy my style too much.

939
01:05:23,440 --> 01:05:25,519
But and they've all said the same
thing. I mean, they all

940
01:05:25,599 --> 01:05:28,960
kind of say, yeah, it's
sad, what's happening. It's it's you

941
01:05:28,960 --> 01:05:33,920
know, this this private, intense
privatization, this entrepreneurial this mixing of like

942
01:05:34,079 --> 01:05:40,440
entrepreneurialism with higher academia is really tragic, and you know, we're I don't

943
01:05:40,440 --> 01:05:42,800
know, man, it's just it's
it's sad. But you know, luckily,

944
01:05:43,079 --> 01:05:46,320
for better or worse, there's this
contingent of social media that's coming out

945
01:05:46,320 --> 01:05:49,920
that's getting people more stoked on this
shit. That the amount of social media

946
01:05:49,960 --> 01:05:55,239
accounts I see doing plant stuff now
and not just like can you eat it?

947
01:05:55,400 --> 01:05:58,599
Or is it herbalism? You know, no, no offense to that

948
01:05:58,679 --> 01:06:01,559
stuff, you know, forging,
but but more so just like here's this

949
01:06:01,599 --> 01:06:06,320
plant, here's you know what's talking
about taxonomy, talking about ecology, what

950
01:06:06,400 --> 01:06:11,800
pollinates it? You know, really
cool stuff like bigger picture shit. And

951
01:06:11,840 --> 01:06:14,199
I see a lot more of that
out there now, and I think that's

952
01:06:14,239 --> 01:06:16,039
really cool, because I fucking nature
feels good, man, you know,

953
01:06:16,320 --> 01:06:20,519
and so does geology. Hiking out
and seeing these things and getting an understanding

954
01:06:20,559 --> 01:06:24,519
the world, it feels good.
And I think people are starting to catch

955
01:06:24,519 --> 01:06:30,599
it on so well. It is
inspiring to have folks of all walks of

956
01:06:30,639 --> 01:06:35,559
life have the power and the motivation
to do this kind of non traditional type

957
01:06:35,599 --> 01:06:40,719
stuff. I mean, for my
own story, I stopped at a master's

958
01:06:40,760 --> 01:06:44,360
degree. I did not go on
and get a PhD because I was nervous

959
01:06:44,440 --> 01:06:47,119
about going deeper into that world,
which even as a young person, I

960
01:06:47,159 --> 01:06:51,719
realized was probably not my group.
Like the more you get into it,

961
01:06:51,960 --> 01:06:57,199
the more the suckage increases. I've
got, you know, called Yeah.

962
01:06:58,400 --> 01:07:02,000
So I've managed to kind of be
a neutral party. Basically. I've lived

963
01:07:02,039 --> 01:07:05,679
and worked at a university all of
my life, but I've had one foot

964
01:07:05,679 --> 01:07:09,960
you know, off campus essentially,
and one foot on campus, and I've

965
01:07:09,960 --> 01:07:14,639
been kind of straddling that gray area
between black and white, and it's been

966
01:07:14,679 --> 01:07:19,639
fulfilling. But I've hard wired myself
not to have anybody in the university's system

967
01:07:19,800 --> 01:07:26,679
or in my geology department really understand
what I'm up to. And that became

968
01:07:26,920 --> 01:07:31,000
very clear at the beginning of the
pandemic when I forgot I even had a

969
01:07:31,000 --> 01:07:35,400
YouTube channel. There were just a
couple of hundred subscribers, and I freaked

970
01:07:35,400 --> 01:07:40,280
out in March of twenty twenty because
my calendar was suddenly empty like a lot

971
01:07:40,320 --> 01:07:45,159
of people, and so I started
doing live streams every afternoon from my backyard,

972
01:07:45,440 --> 01:07:48,840
five times a week for like three
months, and there was this you

973
01:07:48,880 --> 01:07:55,199
know, organic kind of whatever worldwide
audience that was there just basically trapped at

974
01:07:55,199 --> 01:07:58,000
home and wanted to be part of
this. And yes it was geology,

975
01:07:58,039 --> 01:08:01,880
but was also just community and everything
out. Ever since that March of twenty

976
01:08:01,920 --> 01:08:10,119
twenty Spring of twenty twenty, I've
ard the university as ash, you know,

977
01:08:11,079 --> 01:08:15,599
so unable to operate like I was
operating back then. And then that

978
01:08:15,679 --> 01:08:18,520
momentum is still going on now.
So yeah, the pandemic for me was

979
01:08:18,520 --> 01:08:27,439
was was a change change of perception
for me, just accelerated by um,

980
01:08:27,640 --> 01:08:32,920
divorce from from that university scene.
Yeah, and I think I want to

981
01:08:32,960 --> 01:08:34,760
I want to. I'm not ready
to let you go yet. I want

982
01:08:34,760 --> 01:08:40,680
to keep talking some geology stuff.
But but um, yeah, I think

983
01:08:40,800 --> 01:08:44,119
universities are not in a lot of
a lot of people in academy are not

984
01:08:44,279 --> 01:08:47,359
very good at science communication. And
I understand why, because they you you

985
01:08:47,439 --> 01:08:50,680
need to feel free to a certain
extent. You got to feel you gotta

986
01:08:50,680 --> 01:08:53,760
be able to cut loose. You've
got to feel, you know, feel

987
01:08:53,840 --> 01:08:57,359
able to chill out, and those
are not settings where you can do that.

988
01:08:57,399 --> 01:09:00,840
You've got reputations to worry about.
You've got in my gonna get fired,

989
01:09:00,880 --> 01:09:02,880
You've got you know, is this
going to be uncouth? That kind

990
01:09:02,920 --> 01:09:05,359
of stuff. So you know,
whereas me, I'm just a slob that

991
01:09:05,680 --> 01:09:09,359
got into this stuff and has been
able to make it work. I don't

992
01:09:09,399 --> 01:09:14,640
have any reputation to live up to
except am I communicating shit in a good

993
01:09:14,640 --> 01:09:16,680
way and making it funny? And
are you learning something? That's That's all

994
01:09:16,680 --> 01:09:19,359
my reputation is about. I don't
have to worry about getting fired, have

995
01:09:19,359 --> 01:09:23,079
to worry about any of this stuff. So for me, it's easy.

996
01:09:23,159 --> 01:09:25,920
I'll keep doing it till it sucks
and it's not fun anymore, or you

997
01:09:25,920 --> 01:09:28,640
know, people get bored. But
but um, you know, and then

998
01:09:28,680 --> 01:09:31,960
I'll do something else. That's a
beautiful thing too. I mean, I

999
01:09:32,000 --> 01:09:35,000
don't know if you're committed to X, Y and Z in the next couple

1000
01:09:35,039 --> 01:09:40,840
of years, but this freedom to
do as much or as little as you

1001
01:09:41,000 --> 01:09:45,119
choose, there's a lot of power
in that that you're that you're not.

1002
01:09:45,239 --> 01:09:47,319
You know, as soon as it
starts to become less fun, you don't

1003
01:09:47,319 --> 01:09:49,960
have to keep slogging away. Yeah. Maybe I don't know. Maybe,

1004
01:09:50,039 --> 01:09:53,920
Joey, maybe you have built an
empire to this point you feel like you

1005
01:09:54,000 --> 01:09:57,319
have to keep the wheels shirted I
at all. No, No, I'll

1006
01:09:57,359 --> 01:10:00,640
just do it. It's got to
be fun or else if it's fuck it.

1007
01:10:00,760 --> 01:10:01,640
You know, it's like any job. I always said that about the

1008
01:10:01,680 --> 01:10:04,880
best thing about having a job is
being able to quit it. It really

1009
01:10:05,039 --> 01:10:09,119
is, you know. So I'm
surprised I lasted at the railroad that long.

1010
01:10:09,159 --> 01:10:11,640
But that was a fun job for
a long time, and you know,

1011
01:10:11,720 --> 01:10:13,279
got a lot of cool stories out
of it. Well, anyway,

1012
01:10:13,359 --> 01:10:15,520
let's move on really quick. How
much time you got, Nick, How

1013
01:10:15,600 --> 01:10:20,880
much time you got? I have
got another half an hour? Yeah,

1014
01:10:20,920 --> 01:10:26,000
oh yeah, we're taking it.
We're taking it, brother. So getting

1015
01:10:26,439 --> 01:10:30,239
back to geology stuff. So what
are the things you got going on there

1016
01:10:30,800 --> 01:10:33,600
in Washington that that you find So
we're luring. I want to talk about

1017
01:10:33,600 --> 01:10:41,800
the volcanism past and present, maybe
touching the Missoula floods. Talk talk about

1018
01:10:42,800 --> 01:10:45,359
some of the fossils, fossil flora, Like what did the climate look like

1019
01:10:45,359 --> 01:10:49,760
because those fossils I was finding in
Winnatchee, you know, I guess they're

1020
01:10:49,880 --> 01:10:53,520
maya scene. They did not look
like plants that grow there. Now.

1021
01:10:53,680 --> 01:10:58,319
I mean, you get a really
really cool snapshot of what that area must

1022
01:10:58,359 --> 01:11:00,399
have looked like. It was probably
a lot warmer twenty million years ago.

1023
01:11:01,399 --> 01:11:09,600
Yes, I keep things fresh,
and I designed it so that every year

1024
01:11:09,680 --> 01:11:12,600
or a year and a half,
I'm onto a completely different thing, and

1025
01:11:12,600 --> 01:11:15,479
then I kind of do a deep
guy. So right now I'm with the

1026
01:11:15,520 --> 01:11:18,159
ice age floods, and I'm learning
about this guy called Jay Harlan Bretts,

1027
01:11:18,640 --> 01:11:23,880
who was a longtime professor at University
of Chicago. He probably lived in a

1028
01:11:23,960 --> 01:11:27,279
suburb not far from your shuburb,
But I don't know Homewood. Is that

1029
01:11:27,520 --> 01:11:30,439
is that it's on a south side? Yeah, there was. I knew

1030
01:11:30,439 --> 01:11:33,439
a couple of punk bands from Homewood
back in the day. They were good

1031
01:11:33,439 --> 01:11:38,520
and had garage shows and stuff.
Yeah, working class suburb of Chicago.

1032
01:11:38,640 --> 01:11:44,920
Yeah. So that's an example where
I'm I'm reading the original Bretts papers from

1033
01:11:44,960 --> 01:11:47,239
one hundred years ago when he was
out here. Every summer in the nineteen

1034
01:11:47,279 --> 01:11:51,800
twenties, you brought University of Chicago
students out on the train and they covered

1035
01:11:51,800 --> 01:11:57,439
this ground on foot. And he
put this story together about a huge flood

1036
01:11:58,279 --> 01:12:03,439
that operated in many channels simultaneously.
Graham Coolly, Moses cool. They've been

1037
01:12:03,439 --> 01:12:08,720
making some videos about it recently.
But I've gone back to his original work,

1038
01:12:09,039 --> 01:12:13,479
and again, it's places that many
of us out here know very well,

1039
01:12:13,520 --> 01:12:16,680
and he was seeing things that have
kind of been lost. The narrative

1040
01:12:16,720 --> 01:12:20,239
of the Missoula floods is a different
story than what he was doing one hundred

1041
01:12:20,319 --> 01:12:25,840
years ago. So I'm currently putting
that together and trying to see his original

1042
01:12:25,880 --> 01:12:29,800
work and then eventually trying to figure
out why we've gotten away from something original

1043
01:12:29,880 --> 01:12:32,279
stuff. So that's younger than two
million years ago, right, right,

1044
01:12:32,319 --> 01:12:35,239
at least? Go ahead, Well, I was gonna ask you, so

1045
01:12:35,319 --> 01:12:39,399
let's give a rundown of what the
Missoula floods were. Basically, it's a

1046
01:12:39,439 --> 01:12:43,399
pretty recent phenomenon, right. The
premise is that during the Ice Age,

1047
01:12:43,399 --> 01:12:45,760
there were these glaciers. One of
them broke. It was a glacial dam.

1048
01:12:45,880 --> 01:12:50,159
It was holding back a lot of
water where somewhere in Idaho or Montana,

1049
01:12:50,199 --> 01:12:55,199
I guess Montana, Missoula, and
then all this water flooded west towards

1050
01:12:55,199 --> 01:13:00,760
the ocean. But it was like
a long in terms of lessman like a

1051
01:13:00,840 --> 01:13:05,119
long event, and it was catastrophic
and drastically reshaped the landscape. Is that

1052
01:13:05,279 --> 01:13:11,920
somewhat correct or what the that's the
conventional narrative. So you're picking up a

1053
01:13:11,960 --> 01:13:15,000
theme for me. I've got a
soft spot for the unconventional. I've got

1054
01:13:15,000 --> 01:13:21,600
a soft spot for the underdocks.
So the traditional story is, yes,

1055
01:13:21,960 --> 01:13:29,359
there were dozens of floods of glacial
Lake Missoula, and there was an ice

1056
01:13:29,479 --> 01:13:33,560
dam in today's northern Idaho that broke, and there was a flood of water.

1057
01:13:33,640 --> 01:13:36,840
We drained glacier Lake Missoula and maybe
a couple of weeks time, and

1058
01:13:36,920 --> 01:13:41,640
that water goes all the way over
Portland and to the Pacific Ocean, and

1059
01:13:41,680 --> 01:13:45,399
then that ice dam reforms. Weird
to me, but whatever reforms in northern

1060
01:13:45,399 --> 01:13:50,159
Idaho, we make another glacier Lake
Missoula. We repeat the story, and

1061
01:13:50,279 --> 01:13:55,960
many of the channels in eastern Washington
between Spokane and my house here in Ellensburg

1062
01:13:56,479 --> 01:14:00,520
got hammered by this water. Okay, that's what I've thought for a long

1063
01:14:00,560 --> 01:14:02,920
time. Now. If you go
back to Bretz's stuff one hundred years ago,

1064
01:14:04,039 --> 01:14:10,279
he's saying the big flooding was not
younger than twenty thousand years ago,

1065
01:14:10,560 --> 01:14:14,920
but the big flooding happened one hundred
thousand years earlier than that, and the

1066
01:14:15,000 --> 01:14:17,720
water was not coming from Montana,
but it was coming from the fucking ice

1067
01:14:17,760 --> 01:14:25,279
sheet itself, which was immediately north
of Grand Cooley Dam. And this concept

1068
01:14:25,319 --> 01:14:30,399
of subglacial flow you can actually have
yoku ups with sudden releases of water from

1069
01:14:30,399 --> 01:14:36,239
an ice sheet itself, was the
story as opposed to this kind of skirting

1070
01:14:36,319 --> 01:14:42,000
of glacial waters along the front of
an ice sheet. So I'm hot on

1071
01:14:42,039 --> 01:14:45,600
this right now because I've got a
bunch of buddies who are working up in

1072
01:14:45,680 --> 01:14:50,680
Canada and they have a beautiful case
for subglacial flow coming down the Okanagan River

1073
01:14:50,800 --> 01:14:59,039
valley and heading towards when at Ye
Washington. But the tribal mentality of the

1074
01:14:59,079 --> 01:15:02,359
ice age floods science has who've been
operating the last fifty years or not letting

1075
01:15:02,359 --> 01:15:06,439
those guys do their things. So
I mean, it's it's that again.

1076
01:15:06,479 --> 01:15:13,079
These narratives are interesting to me,
and yes, I'm happy to lay in

1077
01:15:13,119 --> 01:15:19,039
and lean into a bunch of basic
field observations that support a narrative. But

1078
01:15:19,079 --> 01:15:25,479
if the field observations don't totally support
the general story. Then I start asking

1079
01:15:25,560 --> 01:15:28,479
questions, and much like you,
I don't have to worry about a reputation

1080
01:15:28,560 --> 01:15:30,439
or anything else. I just go, hey, man, I'm just a

1081
01:15:30,479 --> 01:15:33,720
teacher. I'm just asking questions.
Put some stuff out there. They've got

1082
01:15:33,760 --> 01:15:38,840
any leads that can help me with
and this YouTube community and then you know,

1083
01:15:38,880 --> 01:15:42,560
people are starting to go through old
newspaper clippings and other things and we

1084
01:15:43,159 --> 01:15:45,279
piece some stuff together. So that's
the fun for me. That content.

1085
01:15:45,439 --> 01:15:47,800
It's fun. I mean, it's
fun stuff to think about. Either way,

1086
01:15:47,880 --> 01:15:51,319
you know right or not? Who
knows right? And that's that's to

1087
01:15:51,439 --> 01:15:54,880
be determined, you know, as
more evidence comes in. But it's really

1088
01:15:54,880 --> 01:15:58,279
fun stuff to think about. But
I mean, for people that don't live

1089
01:15:58,319 --> 01:16:01,079
in the region, explain, well, I mean something happened. It's evidence

1090
01:16:01,159 --> 01:16:04,680
something happened from looking at the landscape. And for people that don't live in

1091
01:16:04,680 --> 01:16:11,079
the region, what makes it apparent? Like I tell everyone what, you

1092
01:16:11,119 --> 01:16:15,239
know, what is so obvious that
there was a mass movement of water that

1093
01:16:15,279 --> 01:16:18,960
occurred here at some point in the
last you know, a few hundred thousand

1094
01:16:19,079 --> 01:16:28,079
years. Great question. So eastern
Washington have these very thick basaltic lava flows

1095
01:16:28,439 --> 01:16:34,520
Hawaiian lava enormously thick, yeah,
and mantling the top of those lava flows

1096
01:16:34,720 --> 01:16:44,479
is wind blown silt thick soils called
loos l o eess. And so before

1097
01:16:44,560 --> 01:16:49,119
these ice age floods, that loos
mantled this giant lava cake. So it's

1098
01:16:49,119 --> 01:16:53,119
like a German chocolate cake with a
bunch of cocaine on top of them,

1099
01:16:54,359 --> 01:16:59,760
a continuous, you know, blanket
of of cocaine. And so then it's

1100
01:17:00,000 --> 01:17:03,720
obvious that a bunch of water came
through because when you now walk around on

1101
01:17:03,800 --> 01:17:09,840
top of this German chocolate cake,
there's whole parts of the top of the

1102
01:17:09,920 --> 01:17:15,359
cake where all the coke is gone. There's other places where there's a place

1103
01:17:15,399 --> 01:17:17,960
where all the coke is gone,
but there's islands of cocaine in the middle.

1104
01:17:18,399 --> 01:17:23,920
So in other words, there's little
remnants of this former mantle where you

1105
01:17:23,960 --> 01:17:29,279
can see these tear drop little islands
of the lists. And most impressively,

1106
01:17:29,720 --> 01:17:33,640
there's other places where not only is
the cocaine gone, but the three top

1107
01:17:33,760 --> 01:17:39,640
layers of the German chocolate cake are
gone, and they're evidence of waterfalls.

1108
01:17:40,359 --> 01:17:45,319
Where you have this niagara falls like
horseshoe shaped cliff, and you've got giant

1109
01:17:45,399 --> 01:17:48,560
potholes at the bottom of the cliff, and there's piles of gravel that are

1110
01:17:48,560 --> 01:17:53,880
downstream, and so not to bring
a brac to brets, but I will

1111
01:17:53,920 --> 01:17:58,079
again one more time. For a
hundred years ago, Bretz is making maps

1112
01:17:58,079 --> 01:18:00,279
of these features and he's saying,
look, man, this has got to

1113
01:18:00,319 --> 01:18:05,800
be a catastrophic flood of water,
probably just one flood that started quickly and

1114
01:18:06,000 --> 01:18:11,359
ended quickly. And all the experts
of the day said, that's impossible.

1115
01:18:11,479 --> 01:18:15,199
We don't do things catastrophically in geology, Harley, It's got to be gradual.

1116
01:18:15,399 --> 01:18:19,359
So these are just glacial rivers that
are just working their way at different

1117
01:18:19,359 --> 01:18:24,840
places. To Holy bullshit, man, every channel was full of water at

1118
01:18:24,920 --> 01:18:28,279
the same time. I had elevations
of the heads of all these channels.

1119
01:18:28,720 --> 01:18:30,119
You guys are high, by the
way, Have you ever been out here?

1120
01:18:30,479 --> 01:18:33,279
Yeah? Anybody actually been out here? Really quickly, if I could

1121
01:18:33,319 --> 01:18:38,960
just read from minute that dogmatic thinking, that that anti catastrophism thinking is so

1122
01:18:39,039 --> 01:18:43,319
fucking weird to me, Like it
just seems so weird to be so stuck

1123
01:18:43,760 --> 01:18:46,319
to this is the way things have
been slow and gradual. I mean that

1124
01:18:46,359 --> 01:18:49,520
seems almost anti scientifically, you don't
know, like it was. Maybe for

1125
01:18:49,560 --> 01:18:53,760
the majority of the time it's slow
and gradual. A lot of things happen

1126
01:18:53,840 --> 01:18:57,159
that way. But there's also a
lot of evidence for you know, a

1127
01:18:57,239 --> 01:19:00,119
crazy, crazy event, not crazy, but a large been happening over a

1128
01:19:00,159 --> 01:19:06,800
relatively small period of time. We're
back to our theme earlier in this conversation,

1129
01:19:06,920 --> 01:19:13,920
Joe, who's curious and who's open? Not many people even in geology,

1130
01:19:14,000 --> 01:19:17,600
this group think this, this fashions
of the day business. It just

1131
01:19:17,720 --> 01:19:21,239
presides. And so yeah, I
taught geology three fifty one this spring,

1132
01:19:21,319 --> 01:19:27,119
and we're reading these papers with my
students, and I kept adding this subtext

1133
01:19:27,279 --> 01:19:30,640
or this, this context for this
whole thing. The students kept saying,

1134
01:19:30,640 --> 01:19:33,199
look, why these guys are in
science. Isn't that why people go into

1135
01:19:33,319 --> 01:19:39,199
science? This, this, this
curiosity and this this wonder and this on.

1136
01:19:39,479 --> 01:19:42,079
I'm like, well, apparently not
with some of these dudes, Like

1137
01:19:42,640 --> 01:19:45,880
so, yes, it's not just
geology, of course, but this,

1138
01:19:46,199 --> 01:19:54,199
yes, this this clash of the
conventional versus the independent thinkers. It's stunning

1139
01:19:54,319 --> 01:19:57,439
sometimes when you just pull back and
you think about this, that's what happens.

1140
01:19:57,880 --> 01:20:00,600
You round up these stiffies, You
round up the stiffy scientists. You

1141
01:20:00,720 --> 01:20:04,159
make them do taba acid in a
beautiful place, you know, if they're

1142
01:20:04,159 --> 01:20:09,640
geologists, have them do it at
Columbia Gorge, and you just I'm serious,

1143
01:20:09,640 --> 01:20:13,199
man, I mean, I'm half
joking, but you know, Carrie

1144
01:20:13,239 --> 01:20:16,520
Mullis invented PCR. After taking after
take, you're just just a way to

1145
01:20:16,800 --> 01:20:19,880
shape the you know, shake things
up, shake up your view of the

1146
01:20:19,920 --> 01:20:23,640
world. You never know what anyway, Yeah, if anyone wants to look

1147
01:20:23,640 --> 01:20:28,000
this up, type in Google image
search satellite image Missoula floods and you will

1148
01:20:28,039 --> 01:20:33,119
get a good amount of pictures of
what we're talking about. Because it's it's

1149
01:20:33,159 --> 01:20:35,840
pretty cool. I mean, it's
pretty and I love that. I love

1150
01:20:35,880 --> 01:20:39,399
that, fucking you know. I
remember the first time I ever looked at

1151
01:20:39,399 --> 01:20:42,960
a satellite image of Mount Shasta and
I was like, what is this shit?

1152
01:20:43,520 --> 01:20:46,760
That looks like someone knocked over a
jar of black molasses. That's you

1153
01:20:46,760 --> 01:20:50,279
know, coming northwest out of Mount
Shasta. And then I went I was

1154
01:20:50,359 --> 01:20:54,680
like, I don't know where that
is. I piloted trains, prey trains

1155
01:20:54,720 --> 01:20:58,479
through that. That's a massive fucking
lava flow of boulders the size of a

1156
01:20:58,520 --> 01:21:03,079
minivan that I guess are kind of
basalt, but Manches is not a basaltic

1157
01:21:03,079 --> 01:21:08,840
pocano. They're more like black antisite
oriola. Anyway, I know what that

1158
01:21:09,000 --> 01:21:12,920
is. It's an incredible, you
know, eerie landscape. There's only like

1159
01:21:12,960 --> 01:21:16,760
a couple canyon live oak trees,
circus chrysalopis and other things popping up.

1160
01:21:16,760 --> 01:21:19,800
Man Zanita's popping up here and there. But this is like a giant rubble

1161
01:21:19,880 --> 01:21:24,279
field. It takes forever to walk
through. You've got to climb over it.

1162
01:21:25,359 --> 01:21:29,359
And that is all I mean from
the asylam is that looks like liquid,

1163
01:21:29,399 --> 01:21:32,199
Like that's fucking wild, that's insane. Like I just that changes everything

1164
01:21:32,199 --> 01:21:35,319
about the way I think of the
world or my local environment. Now.

1165
01:21:35,319 --> 01:21:41,199
I used to live up there temporarily
near Weed, California and Dunsmere And so

1166
01:21:41,880 --> 01:21:44,640
you know when you when you zoom
out, it's it's that zooming out.

1167
01:21:44,680 --> 01:21:46,840
I always use that those words as
an analogy, that zooming out to get

1168
01:21:46,880 --> 01:21:50,359
a bigger picture. I think that
does people so much good, you know,

1169
01:21:50,439 --> 01:21:54,800
just like with a drone zooming out, slowly zooming out, zooming up

1170
01:21:55,199 --> 01:21:59,279
and looking down and wow, this
is what what happened. It's I don't

1171
01:21:59,279 --> 01:22:02,800
know, man, It's it's really
really cool stuff to think about. You've

1172
01:22:02,840 --> 01:22:08,119
got it. It's the zooming out. And yeah, I mean this place

1173
01:22:08,239 --> 01:22:12,439
is Disneyland for geology. I mean, I'm here on purpose. It's it's

1174
01:22:12,479 --> 01:22:16,159
Ellensburg, Washington at Central Washington University. But within a two hour's drive in

1175
01:22:16,199 --> 01:22:21,800
all directions from this place, I
can get to these cascade volcanoes. I

1176
01:22:21,880 --> 01:22:27,159
can get to the ice sheet from
Canada, and can get to these alpine

1177
01:22:27,199 --> 01:22:30,279
glaciers. I can get to these
exotic terrains, which is what I was

1178
01:22:30,319 --> 01:22:34,039
into a couple of years ago,
where pieces of granite are clearly from Mexico,

1179
01:22:34,279 --> 01:22:39,960
but it's slowly been moved north on
San Andrea's fault like structures, on

1180
01:22:40,039 --> 01:22:42,760
and on and on. And I'm
not even much of a fossil guy,

1181
01:22:43,159 --> 01:22:46,600
said, but the fossil stuff draws
me on on occasion. So yeah,

1182
01:22:46,720 --> 01:22:51,199
it's it's it's unlimited. And you
know, I'm making these video programs now

1183
01:22:51,199 --> 01:22:55,000
with PBS, and the producers are
like, well, I don't know,

1184
01:22:55,039 --> 01:22:58,359
I think we need to go beyond
Washington, don't you like, don't you

1185
01:22:58,399 --> 01:23:00,640
need to extend your reach. You're
gonna rune of ideas. I'm like,

1186
01:23:01,079 --> 01:23:09,760
I could do fifteen seasons worth of
stuff central Washington, and they don't believe

1187
01:23:09,840 --> 01:23:12,399
me. They just don't believe me. I'm gonna come out there, Nick,

1188
01:23:13,199 --> 01:23:15,399
I'm gonna come out there. We're
gonna go out for like a fucking

1189
01:23:15,439 --> 01:23:17,079
week, and I want to film, and I want to film a bunch

1190
01:23:17,079 --> 01:23:20,359
of stuff. I'll let you go
in a little bit. Just one more

1191
01:23:20,439 --> 01:23:25,520
thing. I want to talk about
this basalt, because there have been massive

1192
01:23:25,520 --> 01:23:29,840
basalt flows in the Pacific Northwest,
some of them incredibly thick, like ridiculously

1193
01:23:29,880 --> 01:23:32,159
thick. You're driving through fucking canyons
and you're looking at a slab of basalt

1194
01:23:32,479 --> 01:23:36,039
that's three hundred feet thick, and
it's got the columnter jointing and all that.

1195
01:23:38,039 --> 01:23:42,079
One of the things. I was
in northwest Nevada once, so maybe

1196
01:23:42,119 --> 01:23:45,800
the Southern organ I forget either way, you know, a few hundred miles

1197
01:23:45,800 --> 01:23:50,159
from you, but uh, and
I remember coming upon we might have been

1198
01:23:50,199 --> 01:23:54,920
trespassing, but we were. We
came up upon this two or three foot

1199
01:23:54,960 --> 01:24:01,159
diameter meta sequoia stump that was horizontal
laid down horizontal and was I mean very

1200
01:24:01,239 --> 01:24:08,560
clearly, you know, a redwood
stump um, and you know in this

1201
01:24:08,680 --> 01:24:13,840
layer of volcanic tuff of white ash
and bright above it, well twenty thirty

1202
01:24:13,880 --> 01:24:16,880
feet above it was a layer of
basalt probably I don't ten feet thick,

1203
01:24:17,399 --> 01:24:21,720
that had been dated at according to
the rocked app that I was using,

1204
01:24:21,720 --> 01:24:26,399
they had been dated at like ten
or eleven million years. But this this

1205
01:24:26,520 --> 01:24:29,960
log, this metasin coil log beneath
it, and the layers beneath it.

1206
01:24:30,760 --> 01:24:35,800
Uh, some of it was you
know, totally permineralized at petrified, but

1207
01:24:35,960 --> 01:24:41,000
some of it was had the fucking
fibers were still there, like the fibers

1208
01:24:41,119 --> 01:24:45,119
of this very soft wood. They've
been slightly infused with silica. They had

1209
01:24:45,159 --> 01:24:46,199
a different I have a video up
on it, and I had people in

1210
01:24:46,239 --> 01:24:50,439
the video being like, you dummy, that's that's a that's a fresh redwood.

1211
01:24:50,439 --> 01:24:54,680
That's not you know, that was
probably washed down the river. And

1212
01:24:54,720 --> 01:24:56,720
I was like, what in a
fucking desert? Look at where I am

1213
01:24:56,760 --> 01:25:00,039
and you think there's like a four
foot three foot diameter breast height redwood growing

1214
01:25:00,079 --> 01:25:03,439
anywhere near here? It gets like
complete. It's a dry climate, you

1215
01:25:03,439 --> 01:25:05,960
know, and so I was thinking
about that, and I was like,

1216
01:25:05,960 --> 01:25:09,000
this is I mean, when I
saw that too, I was like,

1217
01:25:09,319 --> 01:25:13,640
I mean, this thing is basically
it didn't fully permnteralize, and it was

1218
01:25:14,359 --> 01:25:19,479
basically just been entombed and preserved perfectly
like it was in a in an herbarium

1219
01:25:19,960 --> 01:25:26,239
with perfect climate control and you know, dehumidifiers in a basement somewhere for twelve

1220
01:25:26,239 --> 01:25:30,159
million years. That's fucking insane.
I mean, that's totally mind blowing.

1221
01:25:30,239 --> 01:25:33,000
So that that was my first experience
with and then I realized, oh yeah,

1222
01:25:33,000 --> 01:25:38,319
basalt, a thick cap of basalt
is probably a really good, uh

1223
01:25:38,560 --> 01:25:42,720
you know, way to preserve preserve
something for that long. But let's talk

1224
01:25:42,760 --> 01:25:45,359
about this baso. Where did all
this basalt come from? Why was it

1225
01:25:45,439 --> 01:25:49,479
not andesite, you know, which
is obviously these different composition you get most

1226
01:25:49,520 --> 01:25:55,000
of the Pacific Northwest volcanoes are andesite, right, they're more andesite and rholite.

1227
01:25:55,279 --> 01:25:59,199
Where did this basalt come from?
Well, there's different chapters. It's

1228
01:25:59,239 --> 01:26:01,920
easy to cut put them in a
blender, as far as ages and also

1229
01:26:02,039 --> 01:26:10,560
chemistries and also tectonic settings. So
the giant lava flows are mostly basalt,

1230
01:26:10,640 --> 01:26:15,039
which is less than fifty percent silica
in the lava, and there are some

1231
01:26:15,119 --> 01:26:18,920
basaltic andesites which interestingly flowed the farthest. Then those are a little bit higher

1232
01:26:18,920 --> 01:26:21,880
in silica, maybe fifty one fifty
two percent, so they were a little

1233
01:26:23,840 --> 01:26:29,520
it's counterintuitive the ones that flowed the
farthest were a little stiffer or higher in

1234
01:26:29,640 --> 01:26:34,840
viscosity, So that doesn't make sense. Number one. But the basic messages

1235
01:26:34,960 --> 01:26:43,880
these giant lavas came out of cracks, and the cracks started to form about

1236
01:26:43,920 --> 01:26:48,000
seventeen million years ago in eastern Oregon. Now that's a little too old,

1237
01:26:48,039 --> 01:26:53,439
about seventeen million, so it's a
little too old for your sequoia if you're

1238
01:26:53,520 --> 01:26:58,760
rock app was correct. But there
is one particular flow called the Ginko lava

1239
01:26:58,800 --> 01:27:03,039
flow that's best exposed pretty close to
where I live. There's a place called

1240
01:27:03,039 --> 01:27:08,479
Ginko Petrified flo State Park, turning
the littletown called Advantage on the Columbia,

1241
01:27:09,199 --> 01:27:16,640
and that particular flow has an incredible
variety of petrified logs in the base of

1242
01:27:16,680 --> 01:27:20,760
the lava. I repeat Joey in
the base of the lava flow, not

1243
01:27:20,840 --> 01:27:25,640
at the bottom in the in the
lower portion of the lava flow. Are

1244
01:27:25,680 --> 01:27:30,000
these logs that were petrified. They're
in amongst these things we call pillow basalts,

1245
01:27:30,000 --> 01:27:33,319
which indicate that there was water present
when that lava flow came in.

1246
01:27:33,960 --> 01:27:41,079
But why why there is redwood next
to sweet gum, next to cypress,

1247
01:27:41,119 --> 01:27:45,399
next to maple, next to oak, next to ginko, all in this

1248
01:27:45,560 --> 01:27:49,000
crazy collection. And the trees don't
Like I'm no botany expert, those trees

1249
01:27:49,039 --> 01:27:51,880
don't grow next to each other,
So why are they all sitting next to

1250
01:27:51,880 --> 01:27:57,199
each other at the bottom of this
incredible lava flow. He's just one of

1251
01:27:57,239 --> 01:28:00,520
the mysteries. And I'm not sure
if that koya or that red WoT down

1252
01:28:00,680 --> 01:28:05,039
where you were is part of this
story or not. But those lavas are

1253
01:28:05,319 --> 01:28:11,359
mysterious to a point. But we
now know that ultimately ties back to the

1254
01:28:11,399 --> 01:28:15,840
Yellowstone hot spot where the Yellowstone Hospital, just like Craters of the Moon in

1255
01:28:15,920 --> 01:28:21,479
Idaho. Yeah, yeah, although
those are very very young, as we're

1256
01:28:21,520 --> 01:28:26,600
just two thousand year old lavas,
But the same idea that there's a heat

1257
01:28:26,640 --> 01:28:31,079
source, that's that's it's tied to
Yellowstone. So it's just another example of

1258
01:28:31,720 --> 01:28:35,640
all this stuff happening here. But
I'll tell you people that loves the geology

1259
01:28:35,720 --> 01:28:42,319
programs from up here sometimes make the
rookie mistake where they don't realize how much

1260
01:28:42,359 --> 01:28:45,720
time is the elapsing between these separate
stories, and so they're kind of putting

1261
01:28:45,760 --> 01:28:54,319
them together and and hijinks ensues.
Yeah, it's yeah, those lava flows,

1262
01:28:54,319 --> 01:28:57,239
and how do you keep something moting
for three hundred miles By the way,

1263
01:28:57,279 --> 01:29:00,680
you've got a lava flow traveling from
a crack and each in Oregon and

1264
01:29:00,720 --> 01:29:04,399
getting all the way to the Oregon
coast beneath those lighthouses. Just physically,

1265
01:29:04,439 --> 01:29:09,079
how does that stuff stay molten?
It's a tough one to answer. There's

1266
01:29:09,079 --> 01:29:12,520
a lot of mystery with most of
this stuff. Yeah. So wait,

1267
01:29:12,560 --> 01:29:15,960
so craters of the Moon, because
I thought I remembered reading that that was

1268
01:29:16,880 --> 01:29:20,279
that was tied to the yellow Stone
hot Spot too. Is that incorrect?

1269
01:29:21,199 --> 01:29:26,399
Well, I did my master's thesis
right there actually when I went to hide

1270
01:29:26,399 --> 01:29:33,279
a host State university. So,
um, there are some there's some normal

1271
01:29:33,319 --> 01:29:40,119
faults in the basin and range,
so Nevada in southern Utah's basin range basin

1272
01:29:40,239 --> 01:29:43,479
range patterned. McFee, you're one
of your favorite authors, wrote about it

1273
01:29:43,560 --> 01:29:46,920
a bunch, So one of those
normal faults crosses the snaker of her plane,

1274
01:29:47,560 --> 01:29:51,600
and the lava of the snake craters
of the Moon is coming up right

1275
01:29:51,640 --> 01:29:57,239
along one of those normal faults.
So it's it's like the crust is already

1276
01:29:57,279 --> 01:30:00,520
cracked due to crustal extension, like
an accordion opening up in southern Idaho,

1277
01:30:01,319 --> 01:30:06,399
and there is some very young,
two thousand year old lava that's coming up.

1278
01:30:08,119 --> 01:30:13,920
But there's no physical tie between those
craters of the Moon lavas and the

1279
01:30:14,159 --> 01:30:17,840
Yellowstone supervolcano that's, you know,
a couple hours drive to the northeast of

1280
01:30:17,920 --> 01:30:23,479
there. Right. Oh god,
I'm man, I'm out of my element

1281
01:30:23,560 --> 01:30:27,560
there. I just it's so.
I mean again, it's the structural,

1282
01:30:27,720 --> 01:30:31,520
the structural geology aspect of this stuff, like the recent vulcanism. Trying to

1283
01:30:31,520 --> 01:30:35,720
figure out where this stuff comes from, why it's there is uh, I

1284
01:30:35,720 --> 01:30:39,119
don't know. It's so cool to
think about. Well, lastly, before

1285
01:30:39,159 --> 01:30:44,520
we go, that the giant three
hundred foot thick slab of basalt near Columbia

1286
01:30:44,600 --> 01:30:46,199
River Gorge. I mean, what, what what do we know about that?

1287
01:30:47,640 --> 01:30:51,399
Well, there's all sorts of cool
things. Two come to mind.

1288
01:30:53,520 --> 01:30:57,039
Sometimes those giant lava flows, if
you look at them on a map,

1289
01:30:57,800 --> 01:31:02,119
they look like maple syrup flowing over
the kitchen table if you spell the body

1290
01:31:02,159 --> 01:31:08,119
of anti viama, and that makes
perfect sense. But in some cases that

1291
01:31:08,319 --> 01:31:15,319
maple syrup starts to narrow down to
just a little finger going across the kitchen

1292
01:31:15,359 --> 01:31:17,359
table, and they're like, well, that's weird. I wonder why it

1293
01:31:17,600 --> 01:31:24,199
channelized like that. Well, the
answer is that lava found a river valley

1294
01:31:25,000 --> 01:31:30,399
and it started flowing just in this
little pencil like pattern because it was filling

1295
01:31:30,520 --> 01:31:34,840
a river valley. So we can
actually using those patterns, figure out where

1296
01:31:34,840 --> 01:31:39,640
the Snake River, where the Columbia
River, where the Clearwater River, where

1297
01:31:39,680 --> 01:31:43,439
the Yakima River used to be at
different snapshots in time. Because we have

1298
01:31:43,560 --> 01:31:48,800
these lava flows channeling down to these
old river valleys and basically filling them up

1299
01:31:48,840 --> 01:31:53,760
with hot lava, that's a cool
thing. The other cool thing is that

1300
01:31:54,399 --> 01:32:00,920
we know that the Cascade Mountains lifted
high after those lava because lava flows are

1301
01:32:00,960 --> 01:32:05,640
at sea level basically to the east
of the Cascades, and those same lavas

1302
01:32:05,680 --> 01:32:10,239
are three thousand feet higher than they
should be up in the walls of the

1303
01:32:10,239 --> 01:32:15,439
Columbia River Gorge. Upstream of Portland, so you can can actually document tectonic

1304
01:32:15,520 --> 01:32:19,720
uplift by taking something that used to
be horizontal and then lifting portions, because

1305
01:32:19,720 --> 01:32:25,720
we know these lavas didn't flow up
three thousand feet of elevation. So it's

1306
01:32:25,760 --> 01:32:29,800
all a lot, a lot of
this geology stuff is pretty basic. You

1307
01:32:29,840 --> 01:32:32,920
know. It doesn't have to be
that hard. It's it's it's it's it's

1308
01:32:33,199 --> 01:32:40,399
logic, it's the power of observation. It's just thinking through possible scenarios.

1309
01:32:40,439 --> 01:32:45,159
But the most the most bright minds
of geology are doing the most hell get

1310
01:32:45,239 --> 01:32:48,479
simple stuff like that guy Breads right
right. I think it's also important too,

1311
01:32:48,479 --> 01:32:54,039
like as we had mentioned before,
like the correlation between silica content,

1312
01:32:54,359 --> 01:32:58,399
you know, the composition of of
a magma of an extrusive igness rock and

1313
01:32:58,439 --> 01:33:01,960
how and how it flows the core
lation between silica content and viscosity or flow.

1314
01:33:02,039 --> 01:33:05,800
Does it flow like water, which
should be the more basalt end of

1315
01:33:05,800 --> 01:33:10,560
the spectrum, or does it flow
more like like a thick tar or molasses

1316
01:33:10,920 --> 01:33:14,680
like uh, like you know,
andesite or rhyolite and stuff. And of

1317
01:33:14,680 --> 01:33:17,039
course how does that change how explosive
a volcano is? You know, if

1318
01:33:17,359 --> 01:33:21,119
it's a basaltic volcano. It's not. You're not getting these as you know,

1319
01:33:21,279 --> 01:33:25,960
big explosive eruptions that are you know, got the mushroom cloud it's if.

1320
01:33:26,159 --> 01:33:29,079
But if it's rhyolite and that stuff
builds up and it doesn't flow that

1321
01:33:29,119 --> 01:33:31,239
well, the gas builds up,
you get a big boom, and it's

1322
01:33:31,239 --> 01:33:34,479
a more dangerous volcano. And so
that's why it's always it's I mean,

1323
01:33:34,520 --> 01:33:39,479
it's so important to even you know, notice the difference, you know,

1324
01:33:39,520 --> 01:33:42,079
even just for lay people. Is
it what type of what type of mac

1325
01:33:42,159 --> 01:33:45,039
what type of rock is this?
It's extrusive igness. Is it more andesite

1326
01:33:45,079 --> 01:33:46,960
or rhyolite or is it basalt?
Okay, well this must have been a

1327
01:33:46,960 --> 01:33:51,479
more gentle eruption. It flowed more, um, it flowed easily, more

1328
01:33:51,520 --> 01:33:55,600
easily, you know that kind of
thing. So that's why I mean,

1329
01:33:55,640 --> 01:33:57,720
for me, I think about that, you know, if I'm driving through

1330
01:33:57,720 --> 01:34:00,920
a canyon like God, some of
those those basalt those are so cool too.

1331
01:34:00,920 --> 01:34:05,000
There's a there's an endemic for Celia
endemic plant that grows that only grows

1332
01:34:05,000 --> 01:34:10,239
and some of those with salt flows
in Washington. Yeah, yeah, but

1333
01:34:10,279 --> 01:34:14,000
other than that not you don't get
you don't get too much endemism with volcanics.

1334
01:34:14,000 --> 01:34:17,600
Well, um, thanks a lot, and uh, maybe this was

1335
01:34:17,680 --> 01:34:21,720
longer than you planned, but I
really appreciate it, and I'm sure others

1336
01:34:21,760 --> 01:34:26,000
will too. I think we had
a good conversation, So thanks a lot

1337
01:34:26,039 --> 01:34:30,000
for making ten. I really enjoyed
talking with you, Joey, And thank

1338
01:34:30,039 --> 01:34:31,600
you for the invitation. This is
a real thrill for me. Yeah,

1339
01:34:31,600 --> 01:34:34,920
man. Yeah, and uh as
soon as I uh, I gotta get

1340
01:34:34,920 --> 01:34:36,760
out there next spring, as soon
as I have time. Yeah, we

1341
01:34:36,840 --> 01:34:41,119
got to do it. So you're
always welcome either way, all right,

1342
01:34:41,159 --> 01:34:44,079
brother, thanks a lot. Nick, appreciate it. Thank you, Joey

1343
01:34:44,199 --> 01:34:45,039
Goode. Think it
