WEBVTT

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What if a single, you know, relatively short

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river in the south of Spain could act as a literal

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time machine? Oh, I love that framing. Right.

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And I don't mean a metaphorical sit on the bank

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and just kind of think about the past kind of

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time machine. Sure, sure. I mean, a physical

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record of the Earth tearing itself open. Yeah,

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literally. A journey taking you from, like, Nine

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million year old geological escape rooms straight

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through to five thousand year old cliffside fortresses

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built by some of Europe's earliest settlers.

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Welcome to the deep dive. We're so glad you're

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here. It really is quite the the intricate journey

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we are mapping out today. It totally is. And

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today's mission is pulling apart a brilliantly

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dense Wikipedia article detailing the Cassin

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River. The Cassin River. Yeah. This is a waterway

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in Andalusia, Spain, down in the province of

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Grenada. But we aren't just doing a rote geography

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lesson today. No, definitely not. The goal is

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to truly understand the underlying mechanics

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of how water acts as the ultimate sculptor, you

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know, of both the earth and human history. Right.

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Because when you look at a river today, standing

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on its banks, it looks, well, permanent. Yeah,

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it really does. It gives the illusion that it

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has always been there, just quietly flowing in

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that exact path. But the Cason River's story...

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is fundamentally one of dramatic violent change.

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It's kind of crazy when you dig into it. What's

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fascinating here is the sheer scale of the river's

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journey from being trapped in a basin to eventually

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carving out a sanctuary for early humans. To

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understand the beautiful, rugged canyon environment

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that exists right now, we actually have to start

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our story at a time when this river couldn't

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go anywhere at all. Nowhere at all? Right. It

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was essentially trapped. OK, let's untack this.

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We have to go way back. Way back. We are looking

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at the Late Tortonian and the Middle and Late

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Tyrolean eras. Geologically speaking, we are

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talking roughly 9 .0 to 5 .3 million years ago.

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A massive stretch of time. Yeah. And during this

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massive stretch of time, the entire Granada Basin

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was what Geologists classify as an endorheic

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basin. That is the the crucial foundational term

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for this whole narrative endorheic And the best

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way I can think to visualize an Andorheic basin

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for you is to imagine a giant, regional -sized

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bathtub. A bathtub, right. But the drain has

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been completely plugged up with a rubber stopper.

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You had rivers flowing in from the eastern mountains

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and rivers flowing in from the southwest, all

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pouring into the central lake in the basin. Pouring

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in, but not leaving. Exactly. There was absolutely

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no exit. Well, the bathtub visual works perfectly

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for the mechanics. scale that up to a terrifying

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degree. Oh, for sure. Imagine if the water evaporating

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from that closed tub left behind thousands of

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tons of heavy, mineral -rich sludge every single

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year. Yeah, that's a lot of sludge. In a closed

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system like that, the water has nowhere to flow

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out to the sea. It evaporates, sure, but all

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the sand, gravel, the loose clays. The heavy

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stuff. Right. The immense volume of sediment

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that those rivers carry down from the surrounding

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mountains, it all just settles at the bottom.

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Millions of years of rivers acting like, I don't

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know, delivery trucks, just dumping earth into

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this locked room, slowly filling it up to the

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brim. It's a landscape defined entirely by deposition.

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It is purely collecting. Just piling up. There

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is no carved terrain. Just an ever thickening

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layer of flat heavy sediment pressing down on

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the earth, but the earth rarely stays static

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forever, you know Eventually, it decides it's

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time for a breakout. A massive structural one.

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As we move out of those eras and into the Pliocene

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and eventually the earliest Pleistocene eras,

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the tectonic plunning of the entire Iberian region

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radically shifts. The Earth is actually moving.

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Exactly. The Earth's crust is moving. Mountains

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are pushing up. And because of this regional

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tilting, the western part of this basin started

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being drained by the Paleo -Casene River system.

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OK. It started pushing north and eventually hooking

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west. But the real game -changer, the mechanism

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that broke the bathtub, was the Janelle River.

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When I was looking into the Janelle River's role

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in this, I was just stunned by the sheer physics

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of it. Oh, it's wild. The Janelle River physically

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changed its course to flow west, linked up with

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the Paleo -Cassine system, and suddenly the entire

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basin flipped from being endorheic to completely

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exorheic. Exorheic. meaning it drains out. Right.

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The drain in the bathtub was violently unplugged.

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Well, the sheer scale of consequence from that

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single hydrogeological event is staggering. It

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flipped a switch in the Earth's mechanics for

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the entire region. It totally did. Think about

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the energy involved. For millions of years, the

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Granada Basin had been passively collecting sediments.

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But once that river system broke out and found

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a downward path to the sea, the flowing water

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gained incredible kinetic power. It's moving

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fast now. Very fast. The basin went from collecting

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sediments to aggressively eroding them. So the

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river stops being a delivery truck dropping off

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dirt and suddenly becomes a massive excavator

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digging it all back up. That's a great way to

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put it. And erosion isn't just water lightly

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touching rock. It's water carrying abrasive sand

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and gravel, acting like liquid sandpaper at high

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speed. Wow! Liquid sandpaper! Yeah. That shift

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from deposition to aggressive erosion is what

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sets the stage for the dramatic landscapes that

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define the region today. The water was now slicing

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straight down through millions of years of that

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soft, accumulated sediment. So this river spends

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millions of years acting like a buzzsaw, creating

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these massive steep drops. Exactly. Geologically,

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that is a violent process, but biologically it

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creates a fortress. Which brings us to the present

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-day geography and the river's most spectacular

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feature. Yes. The word tajos refers to these

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sheer, steep cuts or gorges. And the scale of

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this specific gorge is just breathtaking. Let's

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trace the water from the very top, because the

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contrast between where it starts and where it

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ends up is amazing. It really is night and day.

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The Cansin River originates high up, over a thousand

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meters above sea level in the Sierra de la Almejada.

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The water filters down from these high -altitude

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aquifers made of limestone, shale, and quartzite.

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Which is an important detail. Limestone and quartzite

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act almost like giant natural sponges. Oh, really?

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Yeah, they hold the water and release it slowly

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and consistently. That's why the river can flow

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year -round and continue its work of erosion

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rather than just flashing and drying up. That

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makes sense. It bursts out into the world through

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these wilderness springs with beautifully evocative

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names. You have Agujerio Caliente, Manticana

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Las Gondrinas. Very poetic. They sound perfectly

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serene and they run through these pristine, high

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altitude wilderness areas. The runoff from the

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north face of those mountains eventually collects

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in what is now the Los Bermejales Reservoir.

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But once the water leaves that reservoir and

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heads north, the serene sanctuary vibe abruptly

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ends. It's over. Completely. The underlying geology

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changes and the terrain gets intense. The river

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hits the Tajos de los Bremahalas. Wait, so when

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we say the earth here is made of quaternary sandstones,

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clays, and conglomerates, what kind of rock are

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we actually dealing with? Good question. Is this

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like the crumbly stuff left over from the bathtub

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era? That is exactly what it is. Because these

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were loosely packed sediments from when the basin

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was a giant lake, they lack the solid heat -forged

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crystalline structure of older rocks like granite.

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So they're soft. Very. They are highly susceptible

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to rapid water erosion. So when the newly energized

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river hit this soft quaternary layer, it didn't

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just casually flow over it. It carved it up.

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It dug straight down, almost like a knife. through

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an incredibly dense layer cake. Wow. It created

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this incredibly narrow canyon with sudden, sheer

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100 -meter drops. If you were standing at the

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edge of the Tajos today, you'd be looking down

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a 330 -foot vertical plunge of raw, exposed clay

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and sandstone. It is a harsh, raw, deeply eroded

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environment. And apparently people hike this.

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They do. There is a walking trail through the

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gorge, but it's officially classified as a difficult

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route. You aren't just taking a stroll, you are

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dealing with sections of hanging bridges, literal

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metal ladders bolted directly into the rock face.

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Not for the think of heart. No, and there are

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support ropes you have to grip just to navigate

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the narrowest cuts. Oh, and there is a hilarious

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historical quirk on this trail. Oh, I know what

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you're gonna say. You are hiking through this

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treacherous prehistoric gorge, gripping a rope

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for dear life, and you arrive at a majestic landmark

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known as the Roman Bridge, which, as it turns

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out, was actually built in the 1940s. A slight

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branding error by the local tourism board, perhaps.

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Just a bit. I mean, missing the fall of the Roman

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Empire by roughly 1 ,500 years is quite the stretch.

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It is. But 1940s concrete bridge doesn't have

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the same romantic ring to it when you're marketing

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a rugged adventure trail. It really doesn't.

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but the human infrastructure is really just a

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footnote here. What is truly remarkable about

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this gorge is the natural adaptation happening

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on those sheer walls. The wildlife. Yes. This

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deep, harsh canyon with its 100 -meter vertical

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drop somehow became a thriving, heavily protected

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ecosystem. I mean, how does anything survive

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on a sheer, crumbly clay cliff? There's no ground

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to stand on. By entirely utilizing the verticality.

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The canyon walls offer perfect protection from

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land -based predators that simply cannot navigate

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the drops. You say they'd fall. Exactly. It creates

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an aerodynamic haven. You have an incredible

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array of bird colonies that make their home right

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on the sheer walls, utilizing the updrafts created

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by the narrow gorge. Oh, wow. You have raptors

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soaring through the corridor, common kestrels,

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and the Eurasian eagle owl. scientifically known

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as bubo bubo. The bubo bubo. It thrives here

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because it can nest in the inaccessible crags

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high up and use the narrow river corridor below

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as a concentrated hunting ground. That's brilliant.

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And alongside the massive raptors you have colonies

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of western jackdaws, rock doves, bee eaters,

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barn swallows, and Eurasian crag martens. It

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is a veritable high -rise of avian life. Just

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a wall of birds. Pretty much. Yeah. But it's

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not just birds taking advantage of the verticality.

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The gorge is also navigated by the southeastern

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Spanish Ivex. Wild mountain goats just casually

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defying gravity on a 330 -foot drop. It's amazing

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to watch. They have highly specialized cloven

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hooves with rubbery pads that allow them to grip

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the almost vertical clay and sandstone walls.

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Gripping clay. Yeah, they use the sheer drops

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as a shield against predators. It paints such

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a vivid, almost contradictory picture. You have

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this river that spent millennia violently tearing

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the earth open, destroying the flat landscape.

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But in doing so, it accidentally carved out this

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perfect fortified sanctuary for an entire vertical

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biome. Exactly. And that concept of a fortified

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sanctuary brings us to the human element of the

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Cassian River story. Because wildlife weren't

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the only ones to look at those towering, unscalable

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walls and realize the strategic value of an inaccessible

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fortress. Here's where it gets really interesting.

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We're zooming forward from millions of years

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ago to about 5 ,000 years ago. The Neolithic

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era. The early humans. Early humans look at the

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Tajos de los Bermejales with its sheer cliffs

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and its flowing water, and they decide to move

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right in. Literally into the walls of the canyon.

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Yes. They lived sheltering under the overhanging

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walls. And to me, this isn't just seeking shelter.

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This is a prehistoric high -rise apartment complex.

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That's a really good analogy. They didn't just

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find deep caves to hide in. They found shallow

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natural cavities and overhangs in the canyon

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walls. And they actively built physical dry stone

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walls across the front to enclose them, making

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them into secure elevated homes. They were engineering

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their environment. And think about the brilliant

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strategy of it. You live high up in an enclosed

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rock cavity where no rival group or large predator

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can easily reach you. Right. Because of the drop.

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But you have this conveyor belt of resources.

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Fresh water, fish, hunting grounds flowing right

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past you at the bottom of what is essentially

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a massive natural fortress moat. And the wild

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thing is, you can still see the traces of some

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of these built walls today. You can, but this

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raises an important question about the physical

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logistics of living there. It's a detail that

00:12:26.340 --> 00:12:28.720
is easy to gloss over if you aren't speaking

00:12:28.720 --> 00:12:32.090
about the scale of geological time. Those Neolithic

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dwellings, those high -rise apartments. Today,

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they sit about 10 meters above the present river

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level. 10 meters. That's like over 30 feet in

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the air. Over 30 feet. Lugging water and supplies

00:12:41.429 --> 00:12:45.149
up a 30 -foot sheer cliff every single day sounds

00:12:45.149 --> 00:12:48.970
exhausting, even with ladders. It would be. If

00:12:48.970 --> 00:12:51.250
we connect this to the bigger picture of the

00:12:51.250 --> 00:12:54.509
river's geological history, that constant relentless

00:12:54.509 --> 00:12:56.990
erosion we talked about earlier, we realize the

00:12:56.990 --> 00:13:00.269
canyon floor wasn't 30 feet down 5 ,000 years

00:13:00.269 --> 00:13:02.259
ago. Wait, are you saying the physical river

00:13:02.259 --> 00:13:05.320
was higher up the cliff face? Yes. The river

00:13:05.320 --> 00:13:07.740
was physically much closer to those dwellings

00:13:07.740 --> 00:13:09.620
when the Neolithic people actually lived there.

00:13:09.799 --> 00:13:12.960
Oh, wow. They absolutely built their homes slightly

00:13:12.960 --> 00:13:15.960
elevated for defensive reasons, using stairways

00:13:15.960 --> 00:13:17.740
and ladders to reach them, keeping themselves

00:13:17.740 --> 00:13:21.200
safe. But over the last five millennia, the Cassine

00:13:21.200 --> 00:13:23.360
River just kept doing what it does. Which is

00:13:23.360 --> 00:13:26.110
digging. It kept digging. That is a mind -bending

00:13:26.110 --> 00:13:28.789
concept. So the human history stayed bolted to

00:13:28.789 --> 00:13:31.570
the wall, but the earth itself moved. The river

00:13:31.570 --> 00:13:33.509
literally dropped the floor out from under their

00:13:33.509 --> 00:13:36.929
history. It excavated roughly 30 feet of solid

00:13:36.929 --> 00:13:40.250
quaternary sandstone and clay over 5 ,000 years

00:13:40.250 --> 00:13:42.590
while those abandoned walls just sat up there

00:13:42.590 --> 00:13:44.570
watching the water get further and further away.

00:13:44.669 --> 00:13:47.450
That's so much rock. If you do the math on that,

00:13:47.850 --> 00:13:50.809
it means the river has been carving away about

00:13:50.809 --> 00:13:54.500
two millimeters of solid rock every single year

00:13:54.500 --> 00:13:57.960
since the Neolithic era. Two millimeters a year.

00:13:58.120 --> 00:14:00.620
It is the perfect illustration of water as a

00:14:00.620 --> 00:14:03.620
slow, unstoppable sculptor. And because the river

00:14:03.620 --> 00:14:05.620
was the center of their lives and physically

00:14:05.620 --> 00:14:08.519
closer to their homes, their artifacts naturally

00:14:08.519 --> 00:14:10.820
found their way into the water. They did. Which

00:14:10.820 --> 00:14:13.340
brings us to perhaps the most significant historical

00:14:13.340 --> 00:14:16.120
discovery in this entire area. The Cassine Pot.

00:14:16.440 --> 00:14:19.039
or the Olla de Cacín as it is known in Spanish.

00:14:19.200 --> 00:14:21.620
It's an ancient clay vessel that was found right

00:14:21.620 --> 00:14:24.120
down there in the riverbed. The water had essentially

00:14:24.120 --> 00:14:26.759
swallowed it and held onto it for millennia and

00:14:26.759 --> 00:14:29.009
preserved it. It's such a significant find that

00:14:29.009 --> 00:14:31.149
it was carefully extracted from the gorge and

00:14:31.149 --> 00:14:33.409
is now preserved in the National Archaeological

00:14:33.409 --> 00:14:36.429
Museum in Madrid. Its significance goes far beyond

00:14:36.429 --> 00:14:39.750
simply being an old clay pot. The Oia de Cassin

00:14:39.750 --> 00:14:42.590
is a specific type of artifact known as cardium

00:14:42.590 --> 00:14:45.230
pottery. Okay. And it represents the most southern

00:14:45.230 --> 00:14:47.850
example of this specific pottery found in all

00:14:47.850 --> 00:14:50.929
of Europe. Which begs the question, What exactly

00:14:50.929 --> 00:14:54.149
makes cardium pottery so special to archaeologists?

00:14:54.730 --> 00:14:57.649
Why does this one pot in Madrid matter so much

00:14:57.649 --> 00:14:59.929
to the timeline of human history? Well, cardium

00:14:59.929 --> 00:15:02.330
pottery is named after the Cerastoderma edul,

00:15:02.789 --> 00:15:05.549
which is a type of marine cockle shell. A seashell?

00:15:05.690 --> 00:15:08.350
Yes, a seashell. During the Neolithic period,

00:15:08.769 --> 00:15:11.690
a specific culture of early humans would press

00:15:11.690 --> 00:15:13.929
these cockle shells into the wet clay of their

00:15:13.929 --> 00:15:16.990
pottery to create distinct decorative imprints

00:15:16.990 --> 00:15:19.590
before firing it. It's often called impressed

00:15:19.590 --> 00:15:22.809
wear. But a cockle shell is a marine shell. That's

00:15:22.809 --> 00:15:25.769
a coastal resource. The Cassine River Gorge is

00:15:25.769 --> 00:15:28.149
tucked away inland deep in the rugged mountains

00:15:28.149 --> 00:15:31.490
of Andalusia. Exactly the point. This pottery

00:15:31.490 --> 00:15:33.629
technique originated along the coastlines of

00:15:33.629 --> 00:15:36.159
the Mediterranean. It tracks the maritime expansion

00:15:36.159 --> 00:15:38.639
of early farming cultures. Oh, I see. So when

00:15:38.639 --> 00:15:40.940
archaeologists find a pot stamped with coastal

00:15:40.940 --> 00:15:43.460
shells buried deep inside an inland river gorge,

00:15:43.740 --> 00:15:46.220
it becomes a massive archaeological marker. Proof

00:15:46.220 --> 00:15:48.580
of movement. Right. It proves that these Neolithic

00:15:48.580 --> 00:15:51.000
people didn't just stay on the beaches. They

00:15:51.000 --> 00:15:53.519
migrated inland, navigating these treacherous

00:15:53.519 --> 00:15:56.159
mountain passes. Or they established complex,

00:15:56.320 --> 00:15:58.419
long -distance trade networks with coastal groups.

00:15:58.879 --> 00:16:03.159
That is incredible. These people pushed inland.

00:16:03.289 --> 00:16:06.710
found this violently carved gorge, recognized

00:16:06.710 --> 00:16:09.250
it as a natural fortress, built their ladders,

00:16:09.490 --> 00:16:12.230
set up their high rises, and brought their distinct

00:16:12.230 --> 00:16:14.590
coastal pottery traditions with them. And then

00:16:14.590 --> 00:16:16.909
they left. And then they left. And the river

00:16:16.909 --> 00:16:18.970
just kept cutting deeper and deeper into the

00:16:18.970 --> 00:16:21.309
earth, preserving the traces of their homes high

00:16:21.309 --> 00:16:24.169
up on the canyon walls while burying their pottery

00:16:24.169 --> 00:16:27.129
deep in the riverbed. It truly functions as a

00:16:27.129 --> 00:16:30.149
time machine. The geology and the human anthropology

00:16:30.149 --> 00:16:32.490
are completely intertwined. So what does this

00:16:32.490 --> 00:16:35.179
all mean? We started this deep dive looking at

00:16:35.179 --> 00:16:38.139
the documentation of a river in Andalusia that

00:16:38.139 --> 00:16:41.259
flows north to join the Genual River. On paper,

00:16:41.440 --> 00:16:43.759
it is just another geographical line on a map.

00:16:43.799 --> 00:16:45.720
Sure. But when you really look at the mechanics

00:16:45.720 --> 00:16:48.480
of it... The Cassine River is a living, flowing

00:16:48.480 --> 00:16:50.919
record of the Earth's sheer power and consequence.

00:16:51.440 --> 00:16:54.360
It is the story of an ancient, trapped lake finally

00:16:54.360 --> 00:16:56.759
breaking its boundaries. Unplugging the bathtub.

00:16:57.019 --> 00:17:00.080
Exactly. It's the story of water violently carving

00:17:00.080 --> 00:17:03.019
a 100 meter gorge out of soft clay, dropping

00:17:03.019 --> 00:17:05.799
the floor millimeter by millimeter. And it's

00:17:05.799 --> 00:17:08.279
the story of a defensive sanctuary that kept

00:17:08.279 --> 00:17:11.359
ancient Europeans safe five thousand years ago,

00:17:11.740 --> 00:17:13.859
holding on to their secrets until we were ready

00:17:13.859 --> 00:17:15.950
to find them. It serves as a powerful reminder

00:17:15.950 --> 00:17:18.250
for all of us, the landscapes you drive past,

00:17:18.650 --> 00:17:20.990
the wilderness trails you might hike, even the

00:17:20.990 --> 00:17:24.750
difficult ones with ironically named 1940s concrete

00:17:24.750 --> 00:17:28.509
bridges, they are not static painted backdrops.

00:17:28.509 --> 00:17:32.289
They are active ongoing processes. They are the

00:17:32.289 --> 00:17:34.710
result of millions of years of hidden geological

00:17:34.710 --> 00:17:37.750
drama and ancient human adaptation. The earth

00:17:37.750 --> 00:17:39.849
is still moving. The tectonic plates are still

00:17:39.849 --> 00:17:42.069
shifting and the rivers are absolutely still

00:17:42.069 --> 00:17:44.400
digging. And that leaves us with one final thought

00:17:44.400 --> 00:17:46.539
for you to take away. Think about that constant

00:17:46.539 --> 00:17:48.740
relentless digging. It never stops. The water

00:17:48.740 --> 00:17:50.779
is still rushing down from the high aquifers.

00:17:50.900 --> 00:17:53.259
It is still carving through the rock. If the

00:17:53.259 --> 00:17:55.559
Cassian River has eroded the canyon floor 10

00:17:55.559 --> 00:17:58.200
entire meters deeper since those Neolithic people

00:17:58.200 --> 00:18:00.559
lived there just five thousand years ago, what

00:18:00.559 --> 00:18:02.920
is it carving into right now? That's a great

00:18:02.920 --> 00:18:06.000
question. Upstream, the river cuts through the

00:18:06.000 --> 00:18:09.740
Alpujarid reliefs. These are complex, much older

00:18:09.740 --> 00:18:12.170
mountain structures full of folded rock and and

00:18:12.170 --> 00:18:15.089
hidden history. What undiscovered artifacts,

00:18:15.390 --> 00:18:18.049
what pieces of forgotten human or geological

00:18:18.049 --> 00:18:20.470
history are currently being washed down from

00:18:20.470 --> 00:18:22.589
those high reliefs today? We don't know. Right

00:18:22.589 --> 00:18:25.289
now, entirely hidden beneath the flowing water,

00:18:25.529 --> 00:18:27.450
just tumbling along the bottom of the gorge,

00:18:27.869 --> 00:18:30.009
waiting to be found by whoever wanders the Tajos

00:18:30.009 --> 00:18:32.369
thousands of years from now. The time machine

00:18:32.369 --> 00:18:34.470
is still running, and it's still collecting data.

00:18:34.849 --> 00:18:36.410
Thanks for taking the deep dive with us today.
