WEBVTT

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Imagine a pocket of land that just completely

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ignores the rules of nature and history. Yeah,

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totally plays by its own rule. Right. Like we're

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talking about a mountain range that somehow operates

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like a secluded island, an ancient forest that

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quietly hid an entire human civilization from

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colonial record keepers. And a geological fortress

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that just magically repels the kind of catastrophic

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megafires that routinely devastate the surrounding

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continent. I mean, it sounds like a setting from

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a fantasy novel, right? It really does. But this

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is a very real place. When you look at the topography

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of Victoria, Australia, you expect the landscape

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to make a certain kind of sense. You expect mountain

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ranges to be these massive, unbroken chains.

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Like giant walls of rock that dictate the weather,

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act as inescapable barriers, all that. Exactly.

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But today we are bringing you a deep dive into

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the Strath bogey ranges Yes, which is a region

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that just shatters all of those expectations

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It really does and for this deep dive We're pulling

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from a really detailed a Wikipedia article covering

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the geography the history and the ecology of

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this incredibly specific area and the kicker

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for you listening This place is sitting just

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150 kilometers northeast of Melbourne, which

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is what? Barely a couple of hours drive from

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a major global metropolis. Yeah, exactly. You

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would naturally assume an area that close to

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a capital city would be completely integrated,

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fully mapped out, tamed by modern infrastructure.

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You'd think so, yeah. But our mission today is

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to explore how this geographically isolated pocket

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has managed to quietly play by its own rules

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for millennia. We are going to look at how it

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shaped a completely unique ecology, how the physical

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landscape itself corrects colonial history, and

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how its violent geological past is actively protecting

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it today. So, okay, let's unpack this. Let's

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do it. To understand any of the strange phenomena

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happening in the Strathboegies, you first have

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to understand the ground you're standing on.

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Technically, this region is a part of the Great

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Dividing Range, that massive continental mountain

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chain we were just talking about. But the Strathbogies

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are fundamentally different because of their

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bedrock. Okay, the bedrock. Yeah. The foundation

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of this entire story is Devonian rock. Specifically,

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a formation known as Strathbogie granodierite.

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Okay, I have to say, Strathbogie granodierite

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sounds like something a supervillain uses to

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build a laser. It does. It really does sound

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like comic book science. Right. But what are

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we actually looking at when we talk about this

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specific type of rock? Well, granodierite is

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a type of coarse -grained rock. It forms deep

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underground when magma cools very, very slowly.

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It's incredibly hard, dense, and uncompromising.

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But it's how that rock was brought to the surface

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that makes this region so fascinating. The southern

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part of the range is this uplifted granite plateau.

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But the northern part, that topography was formed

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by a cauldron volcano. A cauldron volcano. I

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was reading that in the source material and the

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scale of it is almost impossible to comprehend.

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The source describes a cauldron volcano that

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is like 20 to 30 kilometers wide. Yeah, massive.

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And I kept trying to picture a normal mountain

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blowing its top, but that doesn't fit a 30 kilometer

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crater, does it? Not at all. A cauldron volcano

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or a caldera doesn't form from a cone blowing

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its peak outward. It's an implosion. Oh, an implosion.

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OK. Right. Imagine a massive reservoir of magma

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deep beneath the Earth's crust. When that magma

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violently erupts and empties out, the structural

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support for the ground above it simply vanishes.

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So the ground just, it just falls in? Exactly.

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The Earth's crust essentially gives way and swallows

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itself. It collapses inward into the empty chamber

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below. Oh, wow. I mean, it's like a collapsed

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geological souffle, like a sinkhole the size

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of a city. Exactly like that. But on a geological

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scale, accompanied by unimaginable heat and force,

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you're looking at the aftermath of a massive

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collapsed geological event. Which makes the contrast

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with the modern landscape so wild. Oh, absolutely.

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Because if you go to the Strathbogie ranges today,

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you don't see a terrifying smoking crater. The

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topography has smoothed out over millions of

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years into these quiet undulating plateaus that

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are dissected by little stream. Right, it's very

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peaceful now. You do have some prominent peaks.

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I mean, the source mentions Mount Strathboogie

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stands out as the highest point at a 1 ,033 meters.

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And then you have Mount Barrenhead at 832 meters.

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Mount Wombat as well. Yeah, Mount Wombat at 791

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meters and Sugarloaf at 691 meters. But mostly

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it's this rolling granite high country. Right,

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but having a high elevation doesn't automatically

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make a place an island. What turns the Strathboogie

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into an isolated fortress is what borders those

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plateaus. Okay. The range sits to the north of

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the main Great Dividing Range and what completely

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separates it is water, specifically the deep

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valleys of the Goldburn River and the Broken

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River. Now I've heard people compare rivers to

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a moat, but that feels a bit too passive, you

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know? A moat is just standing water. These river

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valleys seem far more structural. That is a really

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crucial distinction. These aren't just streams

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you can casually wade across. These valleys represent

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deep geographic trenches carved over millennia.

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So they're actual physical barriers. Exactly.

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Because the Strathpookies are elevated on this

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granite plateau and entirely bounded by these

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deep river valleys, the ecosystem is physically

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cut off. from the rest of the continent's mountain

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ranges. Wow. A flora and fauna on the plateau

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couldn't easily migrate down across the river

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valleys and up into the Great Dividing Range.

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So the plants and animals were effectively trapped

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on this elevated granite raft. Which forces them

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to evolve in a semi -closed system. The physical

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separation produced completely unique biogeographic

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and ecological patterns. It really is an ecological

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island stranded on the mainland of Victoria.

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So we have this isolated, fortress -like plateau.

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To European eyes in the 1800s, an elevated, heavily

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forested region like that looked like an impenetrable,

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empty wilderness. But the geography was actually

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hiding a completely different reality, one that

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brings us to the first humans to navigate this

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landscape. And this is where the physical environment

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directly challenges the written historical record.

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Oh yes. The Strathbogie Ranges are located squarely

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in Tongarung country. The Tongarung people have

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a history with this landscape that stretches

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back into deep time. Right, and here's where

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it gets really interesting, because the sources

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point out a massive glaring contradiction. They

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do. If you go back and read the documented white

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history of the area, the colonial logs, the diaries,

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the early maps, Those written records generally

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asserted that the mountain range was not often

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frequented by indigenous people. Yeah, the official

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narrative was essentially, there's nothing up

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there, it's too dense, it's too difficult, nobody

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was using this land. And if you only look at

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history through the lens of a colonial record

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keeper, you might believe that. Because the European

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model of habitation relied on highly visible

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markers of ownership. You know, cleared fields,

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permanent wooden structures, fenced off grazing

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land. Right, the stuff they were used to seeing

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back home. Exactly. When early settlers looked

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at the dense, heavily forested table land of

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the Strathbogi's, they didn't see those European

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markers, so they assumed it was a void. But they

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were completely spectacularly wrong. Because

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the physical evidence on the ground tells the

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exact opposite story. The source notes that stone

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artifacts are widely distributed all across the

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Strathbogi table land. Widespread distribution

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is the key phrase there. We aren't talking about

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a single isolated campsite near the edge of the

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range. We are talking about a vast footprint

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of stone tools scattered across the plateau.

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Wow. And you have to picture the environment.

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At the time, this entire table land was once

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a dense, formidable forest. So if you were to

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walk through that table land today and brush

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away the topsoil, you wouldn't find emptiness.

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You would find the silent, physical proof of

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a civilization. Exactly. But how does a colonial

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historian completely miss an entire population

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utilizing a landscape? How does that happen?

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Well, it is a profound example of historical

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bias coming up against hard archaeological evidence.

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The colonists just couldn't read the landscape.

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They were looking for the wrong things. Right.

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They didn't understand the nuanced, complex ways

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the Tungurung people were interacting with that

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forested environment. The widespread presence

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of those stone tools provides irrefutable evidence

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of regular and highly likely seasonal utilization

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of the region. The Tungurung were navigating

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that terrain, utilizing its resources and managing

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the forest in ways the settlers simply couldn't

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perceive. It makes you wonder how much of our

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accepted historical record is just someone looking

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at a complex system and mistakenly writing down

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the word empty. A lot of it, probably. But as

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we move forward chronologically in the sources,

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that supposed emptiness suddenly becomes a very

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loud, very crowded scramble for land. Oh, the

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squatter era. Yes. Once the European settlers

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realized the agricultural potential of the region,

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the isolation of the strath bogeys didn't stop

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them at all. Starting from about 1842, we see

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a massive influx of squatters aggressively pushing

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into the ranges. And the names of these early

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pastoral stations feel like they were pulled

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straight out of a frontier novel. They really

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do. You had Bailey Hill, Strathbogie, Springsay,

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Wombat Hill. Most of those were set up in the

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Rough Hill country. And then you had stations

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like St. Field and Borodoman stretching into

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the edges of the ranges. They were driving in

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sheep and hundreds of cattle trying to force

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this rugged, granite environment to yield a profit.

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There were a few who stayed, like John Gall at

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Wombat Hill, and John Kissick arrived a bit later,

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around 1847. But to give you a sense of the sheer

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audacity and the scale of the greed during this

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period, you really only have to look at the land

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holdings of a single man. William Forlong. Yes.

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By the early 1850s, Forlong had acquired Strathbogie

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and several other pastoral stations in the area.

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Okay, the numbers on this absolutely blew my

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mind. How much land did Forlong actually control?

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According to the records between the early 1850s

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and 1867, William Forlong owned 75 ,000 hectares

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of the Strathbogie region. Wait, 75 ,000 hectares?

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For those more familiar with the imperial system,

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what is that? That is 185 ,000 acres of land.

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185 ,000 acres. For one person in this incredibly

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rugged, steep granite terrain. How do you even

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physically comprehend a property the size of

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a small European nation in the 1850s? You could

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ride a horse for days and never leave your own

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backyard. It's staggering. He really is like

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a modern corporate monopoly. He essentially looked

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at this isolated ecological island and bought

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the entire thing. It was a monopolistic land

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grab, yeah. And it kicked off a brave but incredibly

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intense period of industrialization. The settlers

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were determined to tame the landscape. Right,

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they were building it up. Oh yeah, by the late

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1800s, infrastructure was desperately trying

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to keep pace with the agricultural ambitions.

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A post office opened in Strathbogie. on July

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10th, 1878. And then the ultimate symbol of trying

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to force a landscape to do what you want, the

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dueling butter factories. Oh, yes. I found this

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detail so fascinating. In 1891, a butter factory

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is built at Strathbogie South. And then literally

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the very next year in 1892, a second factory

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is constructed at Strathbogie North. It perfectly

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illustrates the boom mentality of the era. They

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were treating dairy production like a gold rush.

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They were hauling heavy industrial equipment

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up into these gran - Highlands convinced they

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could conquer the topography and turn the region

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into a permanent agricultural powerhouse. But

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the landscape always has the final say, doesn't

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it? It does. Always. Look at the Strathbogie

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region today. A place that once hosted these

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massive 185 ,000 acre pastoral empires and competing

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19th century dairy factories. What is left of

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all that ambition? Very, very little. According

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to the source, today there are no major towns

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in the ranges. There are very few major roads.

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The Strathbogie Township boasts a single general

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store and the nearby Ruffy Township has a place

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called The Pantry. Yep, that's it. That is the

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extent of the metropolis they tried to build.

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It's almost funny. It is, but it brings us right

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back to the geology we discussed at the start.

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How so? The uncompromising geography. You know,

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the steep ridges, the deep river trenches, the

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acidic granite soil ultimately dictated the region's

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fate. It simply wasn't conducive to sustaining

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a sprawling industrialized center. So it pushed

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them out. Exactly. The agricultural boom briefly

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flared up, but the terrain pushed back. It reverted

00:12:39.840 --> 00:12:43.679
to being a quiet, isolated pocket. The landscape

00:12:43.679 --> 00:12:45.960
ultimately tames the settlers, not the other

00:12:45.960 --> 00:12:48.860
way around. Okay, so what does this all mean?

00:12:49.039 --> 00:12:52.500
We have a rugged, isolated plateau that thwarted

00:12:52.500 --> 00:12:55.080
the ambitions of 19th century industrialists.

00:12:55.539 --> 00:12:58.139
But that same uncompromising geography doesn't

00:12:58.139 --> 00:13:01.100
just dictate where humans can build towns. According

00:13:01.100 --> 00:13:03.559
to the sources, it actively protects the region

00:13:03.559 --> 00:13:07.559
from total ecological annihilation. You're referring

00:13:07.559 --> 00:13:10.220
to the fire paradox of the Strathboki's. I am.

00:13:10.419 --> 00:13:12.080
Now, the sources make it clear that the region

00:13:12.080 --> 00:13:15.000
is not somehow magically immune to fire. Given

00:13:15.000 --> 00:13:17.019
the climate, the type of vegetation, and the

00:13:17.019 --> 00:13:19.620
topography, the area likely experienced periodic

00:13:19.620 --> 00:13:22.179
bushfires long before European settlement. Right.

00:13:22.299 --> 00:13:24.360
Fire is a fundamental part of the Australian

00:13:24.360 --> 00:13:26.779
ecology. And there's a documented history of

00:13:26.779 --> 00:13:29.679
more localized fires in recent decades. The sources

00:13:29.679 --> 00:13:31.860
specifically highlight a fire in Strathbogie

00:13:31.860 --> 00:13:34.820
in 1990 and the Longwood East Creighton's Creek

00:13:34.820 --> 00:13:37.980
fire in 2014. So the environment certainly can

00:13:37.980 --> 00:13:40.639
burn. It can. But, and this is the part that

00:13:40.639 --> 00:13:43.039
genuinely stopped me in my tracks. When you look

00:13:43.039 --> 00:13:45.559
at the historical record of the major Victorian

00:13:45.559 --> 00:13:49.220
bushfires, the truly catastrophic, century -defining

00:13:49.220 --> 00:13:52.419
mega -fires that reshaped the entire state, The

00:13:52.419 --> 00:13:55.580
Strathboki ranges just, they dodge them. They

00:13:55.580 --> 00:13:58.179
do. The source lists the years of these mega

00:13:58.179 --> 00:14:03.220
fires, 1851, 1939, 1983, 2003, 2006, and 2009.

00:14:03.820 --> 00:14:05.960
None of those catastrophic events penetrated

00:14:05.960 --> 00:14:08.960
the Strathboki ranges. It is a phenomenal statistical

00:14:08.960 --> 00:14:11.620
anomaly. Right. To survive over a century and

00:14:11.620 --> 00:14:13.820
a half of the most intense fire conditions on

00:14:13.820 --> 00:14:16.639
Earth without suffering a direct hit from a mega

00:14:16.639 --> 00:14:19.460
fire requires more than just luck. That is exactly

00:14:19.460 --> 00:14:21.539
what I'm trying to wrap my head around. How does

00:14:21.539 --> 00:14:24.320
a heavily forested elevated area surrounded by

00:14:24.320 --> 00:14:26.460
some of the most fire prone country on the planet

00:14:26.460 --> 00:14:29.059
manage to evade destruction time and time again?

00:14:29.240 --> 00:14:31.159
Like what is the actual mechanism protecting

00:14:31.159 --> 00:14:33.200
this place? It all comes back to the architectural

00:14:33.200 --> 00:14:35.080
layout of the terrain we established earlier.

00:14:35.139 --> 00:14:37.419
Yeah. Think about what a catastrophic mega fire

00:14:37.419 --> 00:14:39.879
requires to maintain its momentum. Fuel and wind.

00:14:40.379 --> 00:14:43.659
Exactly. It needs continuous unbroken fuel and

00:14:43.659 --> 00:14:46.059
it needs wind funnels to drive that heat forward.

00:14:46.220 --> 00:14:49.139
Now, place that fire into the context of the

00:14:49.139 --> 00:14:51.460
Strathbogie topography. Right, the river valleys.

00:14:51.879 --> 00:14:55.799
The moat. Precisely. A fire raging across the

00:14:55.799 --> 00:14:58.480
plains suddenly hits the deep, sheer trenches

00:14:58.480 --> 00:15:01.679
of the Gulburn or Broken River valleys. Those

00:15:01.679 --> 00:15:04.379
valleys act as massive physical breaks in the

00:15:04.379 --> 00:15:06.899
continuity of the vegetation. Oh, I see. The

00:15:06.899 --> 00:15:09.059
radiant heat struggles to jump that gap with

00:15:09.059 --> 00:15:12.220
the same intensity. And even if embers do cross

00:15:12.220 --> 00:15:15.000
over, they are met with the steep, erratic granite

00:15:15.000 --> 00:15:17.519
ridges of the plateau, which actively disrupt

00:15:17.519 --> 00:15:19.659
the wind patterns that drive the fire forward.

00:15:19.679 --> 00:15:21.980
That makes perfect sense. Yeah, the very geological

00:15:21.980 --> 00:15:24.220
features that created an isolated ecological

00:15:24.220 --> 00:15:26.620
island and frustrated the colonial farmers, they

00:15:26.620 --> 00:15:29.220
act as a structural fortress wall against fire

00:15:29.220 --> 00:15:31.399
behavior. The momentum of the fire is broken

00:15:31.399 --> 00:15:33.820
by the train itself. That is incredible. The

00:15:33.820 --> 00:15:36.340
violence of a collapsing 30 kilometer cauldron

00:15:36.340 --> 00:15:39.519
volcano millions of years ago is quite literally

00:15:39.519 --> 00:15:41.779
acting as a physical shield for the forest today.

00:15:41.860 --> 00:15:44.360
It really is. And speaking of how that ancient

00:15:44.360 --> 00:15:47.320
geology shapes the present, those ancient rocks

00:15:47.320 --> 00:15:49.940
are providing a totally different kind of bounty

00:15:49.940 --> 00:15:52.740
in the modern era. The region might have lost

00:15:52.740 --> 00:15:54.879
its butter factories, but it gained something

00:15:54.879 --> 00:15:57.580
far more sophisticated. the Scraft Bogey wine

00:15:57.580 --> 00:16:00.100
region. Yes. Which compared to the deep time

00:16:00.100 --> 00:16:02.360
we've been discussing is a very recent development.

00:16:02.639 --> 00:16:05.639
It really began taking shape in the mid 1970s.

00:16:05.720 --> 00:16:08.779
Right. The sources credit a pioneer named Dr.

00:16:08.960 --> 00:16:11.340
Peter Tisdall, who planted a new vineyard at

00:16:11.340 --> 00:16:14.460
a location called Ment Helen. And from that initial

00:16:14.460 --> 00:16:18.000
planting, the industry has just flourished. Today,

00:16:18.240 --> 00:16:20.480
there are over 25 vineyards operating in the

00:16:20.480 --> 00:16:22.620
region. And the specific placement of these vineyards

00:16:22.620 --> 00:16:25.100
is key. They're situated at altitudes ranging

00:16:25.100 --> 00:16:29.259
from 100 up to about 650 meters. But altitude

00:16:29.259 --> 00:16:31.620
is only half the equation for a successful cool

00:16:31.620 --> 00:16:33.580
climate vineyard. You have to look at the soil

00:16:33.580 --> 00:16:36.279
profile. The source specifies that these plantings

00:16:36.279 --> 00:16:39.200
are thriving on acidic sandy loams. And where

00:16:39.200 --> 00:16:41.600
do acidic sandy loams come from in an elevated

00:16:41.600 --> 00:16:44.320
plateau? They are the direct result of decomposed

00:16:44.320 --> 00:16:47.340
granite. It all connects perfectly, the Strathoggy

00:16:47.340 --> 00:16:49.740
granotierite we discussed in the very first segment.

00:16:50.080 --> 00:16:53.259
Exactly. Millions of years of that ancient hard

00:16:53.259 --> 00:16:56.120
rock slowly weathering, breaking down, and decomposing

00:16:56.120 --> 00:16:58.639
under the elements until it turns into acidic

00:16:58.639 --> 00:17:02.080
sandy loam. Wow. And that specific soil profile

00:17:02.080 --> 00:17:05.440
is highly sought after by winemakers. Sandy loam

00:17:05.440 --> 00:17:07.779
drains incredibly well, which forces the roots

00:17:07.779 --> 00:17:10.420
of the vines to dig deep and struggle just enough

00:17:10.420 --> 00:17:13.920
to produce highly concentrated, flavorful grapes.

00:17:14.160 --> 00:17:17.339
that unique mineral profile, combined with the

00:17:17.339 --> 00:17:20.319
cooler temperatures at that altitude, is exactly

00:17:20.319 --> 00:17:22.960
what you need to grow the region's main varieties.

00:17:23.240 --> 00:17:26.380
You have Chardonnay, Sauvignon Blanc, Pinot Noir,

00:17:26.559 --> 00:17:29.059
and Shiraz. There's something so poetic about

00:17:29.059 --> 00:17:31.400
that. You have this incredibly violent explosive

00:17:31.400 --> 00:17:34.640
geological origin story, a cauldron volcano collapsing

00:17:34.640 --> 00:17:36.799
in on itself. Right. And the end result millions

00:17:36.799 --> 00:17:39.259
of years later is the perfect soil drainage required

00:17:39.259 --> 00:17:41.740
to sit back and enjoy a world class glass of

00:17:41.740 --> 00:17:44.460
local Pinot Noir. The geology created the island,

00:17:44.480 --> 00:17:46.500
the island preserved the soil and the soil produces

00:17:46.500 --> 00:17:49.380
the wine. It is a perfect synthesis. It forces

00:17:49.380 --> 00:17:51.440
you to realize that the earth beneath our feet

00:17:51.440 --> 00:17:54.279
is never just an inert background stage for human

00:17:54.279 --> 00:17:57.059
events. No, not at all. The bedrock is an active

00:17:57.059 --> 00:17:59.480
participant. It dictates the boundaries of what

00:17:59.480 --> 00:18:02.460
is possible. It truly does. So to wrap up our

00:18:02.460 --> 00:18:05.180
journey today, we started with a Devonian cauldron

00:18:05.180 --> 00:18:08.160
volcano imploding to form a granite island in

00:18:08.160 --> 00:18:11.799
the sky. We looked at how that dense forested

00:18:11.799 --> 00:18:14.279
island held the unwritten history of the Tongarung

00:18:14.279 --> 00:18:16.859
people, proving their presence through thousands

00:18:16.859 --> 00:18:19.140
of scattered stone tools, while the colonial

00:18:19.140 --> 00:18:21.740
record books claim the land was empty. Exactly.

00:18:22.039 --> 00:18:24.539
We watched 19th century squatters attempt to

00:18:24.539 --> 00:18:28.339
conquer that terrain with 185 ,000 acre monopolies

00:18:28.339 --> 00:18:31.299
and dueling butter factories only to be politely

00:18:31.299 --> 00:18:34.000
rejected by the landscape and reduced to a single

00:18:34.000 --> 00:18:36.900
general store in the pantry. And we saw how those

00:18:36.900 --> 00:18:40.779
exact same geological walls act as an impenetrable

00:18:40.779 --> 00:18:43.119
shield against century -defining mega -fires

00:18:43.119 --> 00:18:46.299
while quietly decomposing into the perfect soil

00:18:46.299 --> 00:18:49.099
for cool climate wines. It is a landscape that

00:18:49.099 --> 00:18:51.579
has consistently refused to conform to expectations,

00:18:51.799 --> 00:18:54.160
which leaves you with a pretty profound thought

00:18:54.160 --> 00:18:56.549
to walk away with. We often look at mountain

00:18:56.549 --> 00:18:58.549
ranges and assume we understand them. We think

00:18:58.549 --> 00:19:01.589
of them as these highly visible, permanent, heavily

00:19:01.589 --> 00:19:04.589
mapped things, just giant rocks doing exactly

00:19:04.589 --> 00:19:07.390
what we expect rocks to do. But when you examine

00:19:07.390 --> 00:19:09.990
the Strathbogie Ranges, an ecological island

00:19:09.990 --> 00:19:12.589
that hid an entire civilization's footprint in

00:19:12.589 --> 00:19:15.049
stone and somehow magically deflects catastrophic

00:19:15.049 --> 00:19:18.390
megafires, you have to wonder, what other quiet

00:19:18.390 --> 00:19:20.569
pockets of the world are secretly playing by

00:19:20.569 --> 00:19:22.690
their own rules just waiting for you to look

00:19:22.690 --> 00:19:23.430
a little closer?
