WEBVTT

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You know, I was messing around on my phone the

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other night just scrolling through satellite

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maps. It's a weird habit, I know. Oh, yeah? But

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there's this specific frustration that comes

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with it now. We have this illusion of total knowledge.

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You pull up a view, you scroll over a continent,

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and you think, okay, I see it. I know it's there.

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Right. The Google Earth effect. Yeah. We mistake

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visibility for understanding. Exactly. Just because

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you see a pixelated rock doesn't mean you understand

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its ecosystem. And that is why today's... deep

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dive is, I think, going to be so satisfying because

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we're looking at a place that, despite being

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right there on the map, remains a massive blank

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spot in our actual, you know, our real understanding.

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It is genuinely one of the last true frontiers

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in Southern Africa, a real edge of the map. We

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are heading to the absolute edge, northern Namibia,

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the CUNY region. Specifically, we are trying

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to crack the code of the Bains Mountains. Crack

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the code is a good way to put it. And I say that

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because the sources we've pulled for this, I

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mean, everything from the South African Journal

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of Botany to expedition logs and risk management

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studies, they all paint this place not just as

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a landscape, but as a fortress. That is the perfect

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word for it, a fortress. When you look at the

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geology, it's built like a defensive structure.

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So here's the mission for this deep dive. We

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need to understand how this fortress was built,

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the geology. Then what's trying to kill everything

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inside it, the climate. And then the survivors.

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The survivors. The incredible rare biology and

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the people who actually call this hazardous environment

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home. It's a classic story of adaptation. But

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to get the adaptation, you have to understand

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the pressure first. So let's start with that

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foundation, the geography itself. Because when

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I was reading the data, I kept getting tripped

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up on the terminology. They don't just call it

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a mountain range. No, they don't. They call it

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an escarpment plateau. And for you, the listener,

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trying to picture this. Why is that distinction

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so important? It changes the entire geometry

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of the landscape. I mean, you think mountain

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range. You might picture rolling peaks, maybe

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some valleys, things that undulate. Right. Something

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you can sort of hike up gradually. An escarpment

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is different. It's a shelf. It's a dramatic,

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sudden shift in elevation. A real break in the

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Earth's crust. So we are not talking about a

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gentle slope here. Not at all. In the Banes,

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you're looking at a variance that is, well. It's

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frankly hard to wrap your head around without

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being there. The base is around 700 meters. But

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the plateau itself spikes up to over 2 ,000 meters.

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Wow. That's a vertical gain of 1 ,300 meters.

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That's, what, over 4 ,000 feet? In a really compressed

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distance? That is huge. It is. And that verticality

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defines everything else we're going to talk about.

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It's a barrier. It affects wind, moisture, and

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it certainly affects human access. It's a literal

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wall. And it's not a soft wall, is it? This isn't

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just crumbling dirt or loose scree. The geological

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surveys are really clear. They highlight the

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composition as quartz sandstone. Now, I know

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quartz is hard, but what does that mean for the

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actual scenery? It means durability. Sandstone

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is sedimentary. you know, layers of sand compressed

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over millions of years. But when it's full of

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quartz, it gets tough, incredibly tough. It's

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very resistant to chemical weathering. It doesn't

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just dissolve or melt away like limestone might.

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It fractures. It breaks into these sharp blocks.

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So that explains why the expedition logs keep

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describing it as jagged. It's not smoothing out

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over time. Precisely. Because the rock is so

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hard, it holds these steep vertical faces. It

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allows for deep, narrow gorges that don't just

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collapse on themselves. And that geological toughness

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is, well, it's the only reason the Bains Gorge

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can even exist. Exactly. Let's talk about that

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gorge. Because looking at the maps and the photos,

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it really seems to be the centerpiece of this

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entire region. got this massive block of quartz

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and then the Cune River just slicing right through

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it. The Cune is the lifeblood here. It's the

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border between Namibia and Angola. But its interaction

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with the Bains Mountains is geologically violent.

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Violent. I like that. The river is flowing west.

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It's heading for the Atlantic and it has to get

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past the Zebra Mountains and then slam right

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into the Bains. It sounds like a clash of titans.

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The unstoppable force of the water meeting this

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immovable object. And the water wins. eventually.

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But in the process, it creates this dramatic

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high -velocity transition point. This gorge is

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the river's final major obstacle before it just

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spills out into the Namib Desert. That transition

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really stood out to me. The Bains Mountains are

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essentially the gateway to desolation. They're

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the last stand. Once the river passes the Bains

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Gorge, it enters one of the oldest, driest deserts

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on the entire planet. So the Bains ecosystem

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is effectively an island. An island of high -altitude

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rock. Exactly. Surrounded by arid plains and

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then just... Absolute desert. Speaking of arid,

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we have to talk about the climate. Because one

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of the most striking sources in our stack is

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a paper titled Risk Management in a Hazardous

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Environment. That sets a very specific tone,

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doesn't it? It does. When scientists use words

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like hazardous in the title of a paper, you know

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it is not a vacation spot. It implies that just

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existing there is an achievement. And the rainfall

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data really drives that home. The annual rainfall

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in the Bains is about... 200 millimeters. Which

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is only about 8 inches. 18 inches. For you to

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put that in perspective, that's the threshold

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for being considered semi -arid to arid. It's

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barely enough to sustain scrub vegetation. A

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tropical rainforest might get that in a single

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afternoon. And here, that has to last the whole

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year. The whole year. And yet, and this is the

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paradox that I just love about this place, you

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have this... Bone dry, sun -baked sandstone plateau.

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Getting maybe a cup of water a year. And cutting

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right through its basement is the Cuny River,

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a massive permanent water source. It's a juxtaposition

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of extremes. You have absolute scarcity on the

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peaks and potential abundance down on the gorge.

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But this is key. It's not easy to get to. The

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topography makes it almost impossible. Those

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steep quartz cliffs we just talked about, they

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make that water very, very difficult to access

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if you're up on the plateau. So it's a tease.

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The water is right there, but it's a thousand

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meters down a sheer cliff. Exactly. And this

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contrast, this tension, it creates niches. Biology

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hates a vacuum. If there is a way to survive,

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something will find it. But the life that evolves

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there has to be very, very specific. Extremely

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specific. High altitude, quartz rock, low water,

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intense sun. Which brings us to the flora. I'll

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be honest, when I think biodiversity hotspot,

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I'm thinking, you know, the Amazon or a coral

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reef. A misty jungle, yeah. Not a dry rock pile

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in Namibia, but the Red Data Book of Namibian

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plants says otherwise. The Red Data Book is a

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fascinating thing. It's basically a dossier of

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the most vulnerable and unique life in the country.

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If a plant is in that book, it means it's rare,

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threatened, or endemic. Endemic, meaning it lives

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there and absolutely nowhere else. Right, which

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confirms that the banes act as a refuge. Because

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it's an island habitat, things evolve there in

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total isolation. Let's look at the headliner

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here. Banesia luffifera. I mean, it's in the

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name. You can't get more on the nose than that.

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You really can't. When taxonomists name a genus

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Banesia, They're flagging it as the signature

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species of the entire range. It's a succulent.

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It's adapted to cling to those rocky crevices

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we talked about. What does it take for a plant

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to survive there? It can't just be about needing

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less water. It has to deal with the rock. Oh,

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it's about thermal regulation. It's about root

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systems that can penetrate microscopic cracks

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in quartz to find moisture. And it's about surviving

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insane levels of solar radiation. Panagia has

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solved all those problems. It's built for the

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fortress. And it's not alone. We've also got

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Euphorbia oheva. Now, Euphorbia is a huge family,

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right? I feel like I've seen that name on houseplants.

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You have. Quincetias are Euphorbias. But so are

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these incredible cactus -like succulents all

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over Africa. It's a massive, diverse family.

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But oheva is different. Euphorbia oheva is a

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specialist. It was described relatively recently.

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And it's only found in this specific corridor

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of the Bains and just across the river in Angola.

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That recently part is what blew my mind. We were

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looking at citations from the South African Journal

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of Botany, and the dates on some of these discoveries

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are from the late 2000s. 2008, 2011. In the timeline

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of botanical discovery, that is yesterday. That's

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practically this morning. It just completely

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shatters that Google Earth idea we started with.

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We think we know the world, but here's a distinct

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species of life, and we didn't even give it a

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name until after the first iPhone was already

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out. It speaks to those slang -clueth extinction

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logs you mentioned. The fact that we still need...

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to mount expeditions, capital E tells you everything.

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You don't discover new species in a city park.

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Exactly. You discover them in places that are

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physically hostile to human presence. The difficulty

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that protects the mystery. I like that. And to

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find something like Euphorbia oheva or Abrus

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cacoensis, that's another one, a legume species

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specific to the area, a botanist has to physically

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hike into a zone with no roads. minimal water,

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and vertical cliffs. It makes you wonder what

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else is there. If we found a new euphorbia in

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2011, is there a beetle or a lizard or some kind

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of lichen that we just haven't seen yet? Statistically,

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it's almost a certainty. The Banes are what we

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call a center of endemism. The isolation and

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the unique geology create a laboratory for evolution.

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It's like a mini Galapagos. But instead of an

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ocean, it's surrounded by desert. I want to pivot

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a little bit from the plants to the people, because

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while we're looking at this as a scientific wonderland,

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for the people in the CUNY region, this is home.

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Right. And that brings us back to that paper,

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risk management in a hazardous environment. This

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is such a crucial layer to add. We can't just

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look at the rocks and flowers. This is a lived

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in landscape. Yeah. And that source. discusses

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pastoral societies, people who herd livestock.

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How do you even herd livestock in a fortress

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of courts with eight inches of rain? With incredible

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difficulty and profound traditional knowledge.

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The risk management the paper talks about is

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all about diversification and mobility. You can't

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just stay in one spot. You have to know where

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to go. You have to know where the water is in

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the dry season. You have to know which of those

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obscure plants are good for your goats and which

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ones are poisonous. So the pastoralists are essentially

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practical botanists. They have to be. Their survival

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literally depends on reading the signals of the

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environment. The Bains Mountains might look like

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a barrier to us, but for the local populations,

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they're part of a complex resource map. It redefines

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the word hazardous, doesn't it? It's not just

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dangerous. It's unforgiving of mistakes. That's

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it. Exactly. In a city, if you make a mistake,

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you miss a bus, you forget your wallet. It's

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an annoyance. Yeah, an inconvenience. In the

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Bains, if you misjudge the water reserves or

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the grazing for your herd, the consequences are

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immediate and severe. There is one little detail

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in our research stack that I found kind of funny,

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but also oddly poetic. The main encyclopedia

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entry we found for the Bains Mountains was flagged

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as a stub. Ah, the dreaded stub. For anyone who

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doesn't spend their life on wikis, a stub basically

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means we know this thing exists, but we don't

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have enough information to write a real article

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about it. It's a placeholder. It's a watch this

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space. And I just love the irony. We have terabytes

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of data on, I don't know, the fictional history

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of movie characters. Sure. But for this massive

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2 ,000 meter high geological feature that dictates

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the flow of a major river and hosts unique species.

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We have a stub. You know, I actually find that

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really reassuring. How so? It confirms that the

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world isn't fully consumed yet. The fact that

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the Bains Mountains are a stub means they haven't

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been commodified. They haven't been turned into

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a tourist trap with a paved road and a gift shop.

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They're still wild enough to be unknown to the

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algorithm. Yes. The stub is a badge of honor.

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It means the mountains are still winning. And

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it also highlights the value of the sources we

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do have. That paper on pastoral risk. Those botanical

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descriptions, those are the flickering lights

00:12:18.200 --> 00:12:20.299
in the dark. They're the only reason we aren't

00:12:20.299 --> 00:12:22.259
completely blind to what's happening there. Exactly.

00:12:22.740 --> 00:12:24.720
Without those expeditions, we wouldn't even know

00:12:24.720 --> 00:12:26.559
what to put in the stub. We wouldn't know about

00:12:26.559 --> 00:12:29.220
Banesia. Science is the first step in filling

00:12:29.220 --> 00:12:32.409
in the map. So let's try to synthesize this picture

00:12:32.409 --> 00:12:34.769
we've built of the Hidden Fortress. We have a

00:12:34.769 --> 00:12:38.250
geological anomaly, a massive uplift of hard

00:12:38.250 --> 00:12:41.110
quartz sandstone. Which creates a vertical world

00:12:41.110 --> 00:12:44.549
of cliffs and gorges rising 2 ,000 meters into

00:12:44.549 --> 00:12:46.750
the air. We have a cli - That's the right question

00:12:46.750 --> 00:12:50.889
to ask. Is a Banesia flowering? Is a herd moving

00:12:50.889 --> 00:12:53.769
up the slope? The map can't tell you that. And

00:12:53.769 --> 00:12:55.710
that leads me to a final thought I want to leave

00:12:55.710 --> 00:12:57.990
with you, the listener. We've talked about how

00:12:57.990 --> 00:13:01.419
recent some of these discoveries are. 2011. In

00:13:01.419 --> 00:13:03.779
the grand scheme of things, we just got here.

00:13:03.940 --> 00:13:06.820
We have barely scratched the surface. So if we've

00:13:06.820 --> 00:13:09.960
found entire new species of plants in the last

00:13:09.960 --> 00:13:12.340
decade just by hiking a few of these gorges,

00:13:12.639 --> 00:13:15.600
what is happening on the peaks that no one has

00:13:15.600 --> 00:13:18.139
climbed yet? It's highly probable there are species

00:13:18.139 --> 00:13:21.080
up there. Insects, maybe small reptiles, other

00:13:21.080 --> 00:13:23.980
succulents that have never been cataloged by

00:13:23.980 --> 00:13:26.220
science. So the next time you feel like the world

00:13:26.220 --> 00:13:28.320
is fully explored or that there are no mysteries

00:13:28.320 --> 00:13:31.659
left? Just remember the Banes. Remember, there's

00:13:31.659 --> 00:13:33.659
a fortress of rock in Namibia that is mostly

00:13:33.659 --> 00:13:36.220
just a stub in our collective database. And it's

00:13:36.220 --> 00:13:38.340
perfectly happy staying that way. Yeah. The silence

00:13:38.340 --> 00:13:40.580
of the sandstone doesn't need our approval. Not

00:13:40.580 --> 00:13:42.539
at all. Thanks for taking this trip to the edge

00:13:42.539 --> 00:13:44.480
of the map with us. It's a good reminder that

00:13:44.480 --> 00:13:46.440
there's always more to find. Always a pleasure.

00:13:46.919 --> 00:13:49.379
We'll see you on the next deep dive. Stay curious.
