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WWW.MY-SUBS.CO

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>> Earth, a unique planet,

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restless and dynamic.

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Continents shift and clash.

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volcanoes erupt. Glaciers grow

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and recede.

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Titanic forces that are

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constantly at work, leaving a

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trail of geological mysteries

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behind.

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In this episode, we investigate

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the formation of The Rockies,

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A North American mountain

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range shrouded in mystery,

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flanked by huge slabs of rocks

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with ancient sea fossils buried

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high in its slopes and crowned

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by jagged peaks that geologists

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believe were once double the

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height they are today.

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Scientists piecing together

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their story uncover evidence of

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massive ice sheets, collapsing

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mountains and explosive

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volcanic eruptions.

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A geological history that

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brings us one step closer to

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understanding how the Earth was made.

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S02x06 The Rockies
Original Air Date on December 22, 2009

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-- Sync, corrected by elderman --
-- for MY-SUBS.com ---

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The Rockies--a majestic

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mountain range towering high

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above the American West.

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It's the longest chain in North

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America and the third longest

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in the world, stretching over

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3,000 miles from New Mexico,

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through Colorado, Wyoming and

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Montana and north into Canada.

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For decades, geologists have

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been puzzled about how this

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giant mountain range rose from

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the plains.

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The investigation begins with a

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specific type of rock.

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>> Here we are in the

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heart of the Rocky Mountains,

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we're in an amazing place to

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begin with, and right here at

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Red Rocks we're in the midst of

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an amphitheatre of rock.

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>> [singing rock music]

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>> 13 miles west of Denver,

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Colorado, two 300-foot-high

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sandstone monoliths slope 45

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degrees into the sky.

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Each is taller than Niagara

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Falls.

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Together, they form the walls of

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a unique musical venue.

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[crowd cheering]

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>> But there is more to these

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rocks than fine acoustics.

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These rocks tell the story of

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how the Rocky Mountains were

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made.

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The story begins with a

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mystery, 8,000 feet high in the

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Colorado Rockies 60 miles

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northwest of Boulder.

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All kinds of strange

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impressions are found in rocks

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scattered over the landscape.

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>> We find more than a hundred

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species of marine animals right

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here at this site. We find

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sharks. We find lobsters,

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crabs. We find beautiful fossil

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clams which are all over the

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place.

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>> These fossils are crucial

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evidence of what existed here

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before The Rockies emerged.

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>> We're sitting at

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about 8,000 feet in the middle

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of the Rocky Mountains.

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And so when these fossils where

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formed, this was below the level

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of the ocean. This was below sea

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level.

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>> This area was covered by a

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vast inland sea.

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It existed for over 30 million

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years and stretched from Utah

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to Missouri and from the Gulf

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of Mexico to the Arctic Sea.

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>> And at this very site,

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it would have been very warm,

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almost tropical, so

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envision maybe a day on the

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beach in Florida or something

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like that.

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>> This warm climate attracted a

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unique type of creature that

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left behind large, round

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imprints in the rocks.

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These fossils would play an

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important part in the

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investigation.

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>> This fossil here is

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a giant fossil Ammonite and

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this animal, this coiled shell

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right here, is a relative of

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modern-day squids.

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So, the closest living relatives

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today are squids, nautiloids,

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octopuses, things like that.

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And so in this big coiled shell

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here, the animal would have

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lived at this end, and its

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tentacles would have stretched

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out right here.

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And this animal is really quite

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remarkable. It's about the size

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of a truck tire, and this is

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incredible because most

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Ammonites aren't this big.

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>> Nowhere else have scientists

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found a greater number of these

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prehistoric creatures than here.

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Miller has come up with a

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theory why so many of them came

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to this area.

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>> We think this particular

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fossil here was a female

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Ammonite. And we think that in

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part because male squids are

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smaller than female squids by a

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lot. So just looking around the

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fossil deposits here, we've

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found a male Ammonite, this

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small one here.

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So compare the size of this guy

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to this very big one here. And

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when we look across this

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landscape, we find mostly these

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big Ammonites. And so we think

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that maybe all these females

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got together to spawn and then

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died after they spawned.

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>> When the Ammonites became

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extinct, the map of North

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America looked completely

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different.

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To the north, the Canadian Rocky

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Mountains already existed.

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To the south, the American

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Rockies had yet to rise.

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The date of the Ammonites'

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extinction holds a key to when

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they first emerged.

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>> These animals died

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about 70 million years ago

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in the middle of the western

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interior seaway. And so we know

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at that time, about 70

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million years ago, that this

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site was below sea level.

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So we know then that the Rocky

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Mountains had to rise from that

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seaway some time after

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70 million years ago.

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>> Today, all that is left from

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the ancient sea floor are these

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fossilized remains high in the

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Colorado Rockies.

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Next, geologists needed to find

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out what pushed the seafloor up.

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The investigation moves to

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these slabs of rock flanking

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the Rockies just outside

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Denver, Colorado.

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They are known as the flatirons,

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and they are part of the same

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formation that make up the Red

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Rocks Amphitheater.

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These slabs of rock are

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unusual, because they contain

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holes--holes that make the

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flatirons appealing to climbers

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and geologists alike.

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>> So when we go

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climbing in the flatirons, we're

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climbing on really nice

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hand-holds, in some cases

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hand-holds that have been

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formed either by the pebbles in

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the rock or by zones of

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fine-grained material that are

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easily removed by erosion, the

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shales and the silt stones.

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Those layers get removed

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leaving a notch for the hands

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to go in, and it makes

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for fantastic climbing.

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>> The holes are a clue as to

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how these strangely tilted

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flatirons were formed.

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>> The layers themselves, the

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different grain sizes in the

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layers, the silt, the sand, the

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pebbles--this tells us that

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these are sedimentary rocks.

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>> Sediments form in water when

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sand and small pieces of rock

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settle on the ground.

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Over millions of years, they get

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compressed into layers of rock.

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Taking a closer look, Lester can

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find out more about the

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surroundings they formed in.

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>> These were not just deposited

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in any kind of sedimentary

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situation, but they were

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deposited in rivers capable of

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transporting big particles and

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busting 'em up as it goes along.

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>> Sheets of sand and gravel

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built up a thick sedimentary bed

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like a layered cake,

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but stream deposits are rarely

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more than a few degrees from

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horizontal.

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>> These rocks--you can see the

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layers and the layers in the

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flatirons behind me--are 60

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degrees.

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>> Something caused these vast

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slabs to be tilted.

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The investigation moves 10

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miles northeast to Flagstaff

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Mountain, located in the outer

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ranges of the Colorado Rockies.

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>> I'm standing here

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right next to a miniature

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flatiron. It's tilted like the

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flatirons at about 60 degrees.

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It's steep. How did it

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get that way if it was

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originally a stream gravel

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deposit?

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>> The answer lies in the darker

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rock underneath.

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It is granite and looks

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completely different to the

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flatiron rock above.

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>> There's no layering

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in this rock, unlike the

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flatiron rock which does have

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layering.

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There's no pebbles in this

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rock, unlike the flatiron rock

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which does have pebbles.

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>> A close-up investigation of

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the granite reveals that it is

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full of minerals.

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This offers another clue to how

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the Rockies emerged.

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>> So I've picked up

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this granite here and taking a

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look at it, I see quartz and

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feldspar and a little bit of

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mica in here, very

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characteristic of a rock like

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this that has cooled from a

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magma, from a liquid rock.

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>> Among the minerals is iron.

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It is responsible for the dark

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color of the rock.

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The precise quantity of iron

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tells scientists the depth at

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which the rock was formed.

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>> So we've taken this

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rock into the laboratory and we

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do the chemistry on this rock,

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and we can actually determine

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that not only did  cool and

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00:09:47,871 --> 00:09:49,639
crystallize at depth, that

288
00:09:49,707 --> 00:09:51,441
depth we can estimate at about

289
00:09:51,542 --> 00:09:56,746
15 miles down.

290
00:09:56,780 --> 00:09:58,581
It's now at the surface. How

291
00:09:58,649 --> 00:10:00,149
did it get here? It's been

292
00:10:00,251 --> 00:10:01,684
pushed up by the rise of the

293
00:10:01,752 --> 00:10:03,219
Rocky Mountains and in doing

294
00:10:03,287 --> 00:10:04,787
so, look what it's done to the

295
00:10:04,855 --> 00:10:06,956
flatiron.

296
00:10:07,057 --> 00:10:08,491
>> Scientists investigating the

297
00:10:08,559 --> 00:10:10,226
Rocky Mountains have found two

298
00:10:10,327 --> 00:10:14,030
clues about their early history.

299
00:10:14,098 --> 00:10:16,032
Ammonites on a site 8,000 feet

300
00:10:16,100 --> 00:10:17,934
high are evidence that the area

301
00:10:18,002 --> 00:10:20,203
was once under the sea.

302
00:10:20,304 --> 00:10:22,305
Traces of iron in granite

303
00:10:22,373 --> 00:10:23,539
is evidence that

304
00:10:23,574 --> 00:10:25,642
rock pushed up from 15 miles

305
00:10:25,743 --> 00:10:26,909
below the surface

306
00:10:27,011 --> 00:10:29,479
tilting the flatirons.

307
00:10:29,546 --> 00:10:31,014
And it didn't just happen here

308
00:10:31,081 --> 00:10:32,482
but along approximately 1,000

309
00:10:32,549 --> 00:10:35,852
miles of the American Rockies.

310
00:10:35,953 --> 00:10:37,387
Geologists now needed to find

311
00:10:37,454 --> 00:10:39,489
out what monumental forces were

312
00:10:39,590 --> 00:10:41,391
responsible for this massive

313
00:10:41,458 --> 00:10:44,059
upheaval.

314
00:10:50,478 --> 00:10:52,179
100 million years ago, most of

315
00:10:52,280 --> 00:10:54,014
North America was covered by a

316
00:10:54,082 --> 00:10:57,451
vVast inland sea.

317
00:10:57,552 --> 00:10:59,286
70 million years ago, the sea

318
00:10:59,354 --> 00:11:02,022
retreated and the Rocky

319
00:11:02,090 --> 00:11:04,191
Mountains began to rise, forming

320
00:11:04,259 --> 00:11:07,194
a great mountain range.

321
00:11:07,295 --> 00:11:08,462
Scientists trying to piece

322
00:11:08,563 --> 00:11:10,564
together their geological past

323
00:11:10,632 --> 00:11:12,199
needed to solve the mystery of

324
00:11:12,267 --> 00:11:18,205
what lifted them up.

325
00:11:18,273 --> 00:11:19,807
A force capable of that amount

326
00:11:19,841 --> 00:11:21,175
of heavy lifting would have to

327
00:11:21,276 --> 00:11:24,378
have been on a global scale.

328
00:11:24,479 --> 00:11:26,080
Geologists believe this force

329
00:11:26,114 --> 00:11:29,884
was caused by plate tectonics.

330
00:11:29,918 --> 00:11:31,518
The Earth's crust is broken up

331
00:11:31,553 --> 00:11:33,354
into a series of interlocking

332
00:11:33,388 --> 00:11:34,989
plates.

333
00:11:35,023 --> 00:11:36,924
These plates are continuously

334
00:11:36,992 --> 00:11:38,726
on the move.

335
00:11:38,827 --> 00:11:40,361
Over millions of years, they

336
00:11:40,428 --> 00:11:42,796
collide and break apart,

337
00:11:42,831 --> 00:11:44,098
forming new continents and

338
00:11:44,199 --> 00:11:45,833
geological features around the

339
00:11:45,901 --> 00:11:47,468
world.

340
00:11:47,535 --> 00:11:49,169
When The Rockies formed, two of

341
00:11:49,204 --> 00:11:50,838
these plates smashed into each

342
00:11:50,906 --> 00:11:52,273
other at the American West

343
00:11:52,374 --> 00:11:53,807
Coast.

344
00:11:53,808 --> 00:11:55,009
>> What we know is

345
00:11:55,110 --> 00:11:56,443
that at the time of this

346
00:11:56,511 --> 00:11:58,178
granite uplift on the western

347
00:11:58,179 --> 00:12:00,714
margin of North America, ocean

348
00:12:00,782 --> 00:12:03,083
crust and oceanic plate was

349
00:12:03,184 --> 00:12:05,085
subducting beneath the North

350
00:12:05,153 --> 00:12:06,654
American plate, and it was doing

351
00:12:06,721 --> 00:12:09,890
so at a high rate of speed.

352
00:12:09,925 --> 00:12:11,926
As such, it was transferring

353
00:12:11,993 --> 00:12:13,694
stress into the interior of the

354
00:12:13,728 --> 00:12:15,329
continent.

355
00:12:15,363 --> 00:12:16,263
>> As the two plates moved

356
00:12:16,364 --> 00:12:17,464
towards each other, they

357
00:12:17,532 --> 00:12:19,700
squeezed the crust.

358
00:12:19,734 --> 00:12:21,168
Over millions of years, it

359
00:12:21,269 --> 00:12:23,070
folded and buckled forming tall

360
00:12:23,104 --> 00:12:24,905
mountains.

361
00:12:24,973 --> 00:12:26,440
This was the birth of the

362
00:12:26,541 --> 00:12:29,009
American Rockies.

363
00:12:29,077 --> 00:12:30,911
But a mystery remained.

364
00:12:30,979 --> 00:12:32,146
How did the collision of two

365
00:12:32,180 --> 00:12:33,647
tectonic plates at the western

366
00:12:33,715 --> 00:12:35,549
edge of North America cause the

367
00:12:35,617 --> 00:12:38,619
rise of the Rockies 500 to 1,000

368
00:12:38,720 --> 00:12:40,454
miles inland?

369
00:12:40,522 --> 00:12:41,355
>> Mountain ranges

370
00:12:41,456 --> 00:12:42,556
that form on the margins of

371
00:12:42,624 --> 00:12:43,791
continents are pretty easy to

372
00:12:43,825 --> 00:12:45,726
explain, or where continents

373
00:12:45,827 --> 00:12:47,061
have collided. Where India

374
00:12:47,095 --> 00:12:48,362
slams into Asia, we get the

375
00:12:48,463 --> 00:12:50,631
Himalayas. Where oceanic crust

376
00:12:50,699 --> 00:12:52,099
dives beneath the continental

377
00:12:52,167 --> 00:12:54,001
margin in the northwest,

378
00:12:54,069 --> 00:12:55,235
the Cascades, or in

379
00:12:55,270 --> 00:12:56,337
South America, the Andes

380
00:12:56,371 --> 00:12:57,604
Mountains.

381
00:12:57,639 --> 00:12:59,440
But these mountains here in the

382
00:12:59,541 --> 00:13:01,141
middle of a continent are much

383
00:13:01,176 --> 00:13:02,443
harder to explain and they've

384
00:13:02,510 --> 00:13:05,446
been an enigma for decades.

385
00:13:05,513 --> 00:13:07,047
>> Only recently geologists have

386
00:13:07,082 --> 00:13:10,684
come up with a plausible theory.

387
00:13:10,719 --> 00:13:12,353
They suspect the Rockies formed

388
00:13:12,454 --> 00:13:14,321
along a line where the crust is

389
00:13:14,356 --> 00:13:15,689
very fragile.

390
00:13:15,724 --> 00:13:16,724
>> What happens when

391
00:13:16,791 --> 00:13:18,092
the continent gets compressed,

392
00:13:18,159 --> 00:13:19,393
especially if there's a weak

393
00:13:19,461 --> 00:13:20,728
zone or a zone that's prone to

394
00:13:20,795 --> 00:13:23,430
buckling, it rises.

395
00:13:23,531 --> 00:13:24,498
That's what's brought this

396
00:13:24,532 --> 00:13:26,900
granite to the surface.

397
00:13:26,968 --> 00:13:29,770
>> Geologists now understood how

398
00:13:29,804 --> 00:13:31,905
the Rockies rose and they had a

399
00:13:31,973 --> 00:13:34,541
date for when it happened,

400
00:13:34,609 --> 00:13:35,709
but what were these early

401
00:13:35,810 --> 00:13:37,344
mountains like?

402
00:13:37,445 --> 00:13:38,612
How do they compare to the

403
00:13:38,713 --> 00:13:40,814
mountains of today?

404
00:13:40,882 --> 00:13:42,182
On a site in The Rockies 70

405
00:13:42,250 --> 00:13:44,184
miles northwest of Denver,

406
00:13:44,252 --> 00:13:47,254
geologists find a clue.

407
00:13:47,255 --> 00:13:48,322
>> The mountains that

408
00:13:48,356 --> 00:13:49,356
we see here today aren't the

409
00:13:49,424 --> 00:13:50,858
mountains that were around

410
00:13:50,892 --> 00:13:52,092
millions of years ago. They're

411
00:13:52,160 --> 00:13:53,260
always evolving. Rivers are

412
00:13:53,261 --> 00:13:54,995
shifting. Peaks are shifting.

413
00:13:55,063 --> 00:13:56,363
It's a very dynamic process.

414
00:13:56,431 --> 00:13:57,364
It's almost as if the mountains

415
00:13:57,432 --> 00:14:00,567
are alive themselves.

416
00:14:00,602 --> 00:14:01,935
>> Miller sets out to estimate

417
00:14:02,037 --> 00:14:03,103
the height of the early

418
00:14:03,138 --> 00:14:04,872
mountains. But how can you

419
00:14:04,939 --> 00:14:06,673
measure something that is no

420
00:14:06,775 --> 00:14:08,409
longer there?

421
00:14:08,510 --> 00:14:10,477
Once more, fossils provide the

422
00:14:10,512 --> 00:14:13,047
evidence he is looking for.

423
00:14:13,114 --> 00:14:14,214
>> What's amazing about

424
00:14:14,315 --> 00:14:15,582
collecting fossils is that

425
00:14:15,650 --> 00:14:16,750
you're really the first person

426
00:14:16,785 --> 00:14:18,052
to see this when you crack open

427
00:14:18,119 --> 00:14:19,486
a rock.

428
00:14:19,554 --> 00:14:20,320
It's the first time it sees

429
00:14:20,388 --> 00:14:21,588
light again after 60 million

430
00:14:21,656 --> 00:14:23,957
years.

431
00:14:24,025 --> 00:14:25,392
>> Miller has uncovered a 60

432
00:14:25,460 --> 00:14:27,127
million-year-old fossilized

433
00:14:27,195 --> 00:14:29,463
leaf.

434
00:14:29,497 --> 00:14:30,597
>> It's from a tree that grew

435
00:14:30,665 --> 00:14:32,566
here just 10 million years after

436
00:14:32,667 --> 00:14:35,502
the Rockies began to form.

437
00:14:35,570 --> 00:14:37,371
And intriguingly, this leaf

438
00:14:37,405 --> 00:14:39,273
holds a clue to the height of

439
00:14:39,307 --> 00:14:41,708
these early mountains.

440
00:14:41,810 --> 00:14:43,177
Or more precisely, it's the

441
00:14:43,244 --> 00:14:45,045
edges of the leaf, known as

442
00:14:45,080 --> 00:14:47,147
leaf margins.

443
00:14:47,215 --> 00:14:48,715
Botanists know that in colder

444
00:14:48,783 --> 00:14:50,250
temperatures, the margins tend

445
00:14:50,318 --> 00:14:52,419
to have more teeth than leaves

446
00:14:52,520 --> 00:14:54,421
that grow in warmer areas.

447
00:14:54,489 --> 00:14:55,689
>> Leaves with teeth

448
00:14:55,790 --> 00:14:57,157
do better in colder climates

449
00:14:57,225 --> 00:14:58,258
because teeth are actually

450
00:14:58,326 --> 00:14:59,526
really advantageous in

451
00:14:59,594 --> 00:15:00,894
ump-starting growth at the

452
00:15:00,962 --> 00:15:02,162
beginning of the growing season.

453
00:15:02,230 --> 00:15:03,330
In this case, you can see this

454
00:15:03,398 --> 00:15:04,598
beautiful fossil leaf here with

455
00:15:04,666 --> 00:15:06,433
teeth, and each of the teeth are

456
00:15:06,534 --> 00:15:07,434
little hot-beds of

457
00:15:07,502 --> 00:15:08,802
photosynthesis. So when that

458
00:15:08,870 --> 00:15:10,437
leaf first comes out of the bud,

459
00:15:10,505 --> 00:15:12,339
it gets a jump-start on leaves

460
00:15:12,407 --> 00:15:15,943
that don't have teeth.

461
00:15:15,977 --> 00:15:17,478
>> Miller uses this information

462
00:15:17,512 --> 00:15:19,213
to find out about the height of

463
00:15:19,247 --> 00:15:21,515
the young Rocky Mountains.

464
00:15:21,583 --> 00:15:22,783
In a simple but powerful

465
00:15:22,884 --> 00:15:24,618
technique, he compares the

466
00:15:24,686 --> 00:15:26,620
number of leaves with teeth to

467
00:15:26,688 --> 00:15:28,322
those without.

468
00:15:28,356 --> 00:15:29,423
>> If you go to a

469
00:15:29,524 --> 00:15:30,424
particular area and you pick up

470
00:15:30,492 --> 00:15:31,959
all the species of leaves that

471
00:15:32,060 --> 00:15:33,227
are there from the trees that

472
00:15:33,328 --> 00:15:34,294
are growing in that area and

473
00:15:34,329 --> 00:15:35,329
you compare the number of

474
00:15:35,430 --> 00:15:36,864
species that have teeth to the

475
00:15:36,965 --> 00:15:38,332
number of species that have

476
00:15:38,433 --> 00:15:39,967
smooth margins, that gives us

477
00:15:40,068 --> 00:15:40,968
some idea of what the

478
00:15:41,035 --> 00:15:42,669
temperature is.

479
00:15:42,704 --> 00:15:44,238
>> So the higher the proportion

480
00:15:44,339 --> 00:15:46,306
of plants with jagged edges

481
00:15:46,341 --> 00:15:47,975
compared to plants with smooth

482
00:15:48,042 --> 00:15:49,510
edges, the colder the

483
00:15:49,611 --> 00:15:51,612
temperature of the site.

484
00:15:51,679 --> 00:15:53,313
And the colder the temperature,

485
00:15:53,414 --> 00:15:55,849
the higher the mountain.

486
00:15:55,884 --> 00:15:56,884
>> So if you

487
00:15:56,951 --> 00:15:58,318
got into a hot-air balloon here

488
00:15:58,386 --> 00:15:59,486
today and you floated straight

489
00:15:59,521 --> 00:16:00,954
up into the atmosphere, the

490
00:16:01,022 --> 00:16:02,156
temperature would decrease in a

491
00:16:02,223 --> 00:16:03,423
aery predictable way. And it

492
00:16:03,525 --> 00:16:05,058
turns out that for about every

493
00:16:05,126 --> 00:16:06,126
mile you go up in the

494
00:16:06,161 --> 00:16:07,227
atmosphere, you lose about

495
00:16:07,328 --> 00:16:09,129
20 degrees fahrenheit.

496
00:16:09,230 --> 00:16:10,564
So if we know how temperature

497
00:16:10,598 --> 00:16:11,865
changes with elevation, we can

498
00:16:11,966 --> 00:16:13,867
back out elevation from those

499
00:16:13,935 --> 00:16:16,703
estimates of temperature.

500
00:16:16,771 --> 00:16:17,971
>> To work out the height of the

501
00:16:18,039 --> 00:16:19,973
early mountain, Miller needs to

502
00:16:20,041 --> 00:16:22,743
compare samples from two areas--

503
00:16:22,777 --> 00:16:24,411
one at the base of the mountain

504
00:16:24,512 --> 00:16:27,047
and one at the top.

505
00:16:27,115 --> 00:16:28,515
Fossils found at the base of

506
00:16:28,583 --> 00:16:30,117
the Rockies near to present day

507
00:16:30,151 --> 00:16:32,219
Denver have an amazing story to

508
00:16:32,287 --> 00:16:34,054
tell.

509
00:16:34,122 --> 00:16:35,689
These ancient leaves are

510
00:16:35,790 --> 00:16:37,858
incredibly similar to plants

511
00:16:37,926 --> 00:16:42,029
growing in the tropics today.

512
00:16:42,063 --> 00:16:43,297
>> So after the Rockies

513
00:16:43,331 --> 00:16:44,831
rose, down in the area of

514
00:16:44,866 --> 00:16:46,300
Denver, it was sub-tropical and

515
00:16:46,334 --> 00:16:48,402
tropical forests. We had palms

516
00:16:48,503 --> 00:16:50,404
and cycads and canopies like we

517
00:16:50,471 --> 00:16:52,673
see in the tropics today.

518
00:16:52,740 --> 00:16:53,941
Up here, we had a forest that

519
00:16:54,008 --> 00:16:55,042
looked probably more like a

520
00:16:55,109 --> 00:16:56,410
forest that grows in North or

521
00:16:56,511 --> 00:16:57,578
South Carolina on the east

522
00:16:57,645 --> 00:17:00,581
coast of the U.S.

523
00:17:00,648 --> 00:17:01,848
>> By comparing the ancient

524
00:17:01,950 --> 00:17:03,317
fossil leaves from the top of

525
00:17:03,384 --> 00:17:04,851
the mountain with fossil leaves

526
00:17:04,953 --> 00:17:06,486
from the foot of the mountain,

527
00:17:06,588 --> 00:17:07,654
Miller has come up

528
00:17:07,689 --> 00:17:12,392
with a surprising conclusion.

529
00:17:12,460 --> 00:17:13,327
>> Turns out that

530
00:17:13,394 --> 00:17:14,695
the fossil leaves here are

531
00:17:14,762 --> 00:17:16,129
predominantly toothed, as

532
00:17:16,231 --> 00:17:17,130
compared to those that are in

533
00:17:17,232 --> 00:17:18,865
Denver, which are predominantly

534
00:17:18,967 --> 00:17:20,133
smooth margined.

535
00:17:20,235 --> 00:17:20,968
And it turns out the ones in

536
00:17:21,035 --> 00:17:22,035
Denver grew in a climate that

537
00:17:22,136 --> 00:17:23,303
was about, on average, about

538
00:17:23,371 --> 00:17:25,138
75 degrees fahrenheit.

539
00:17:25,206 --> 00:17:26,373
The ones up here grew in a

540
00:17:26,407 --> 00:17:27,507
climate that was probably about

541
00:17:27,575 --> 00:17:29,209
50 degrees fahrenheit.

542
00:17:29,310 --> 00:17:30,744
So we know how temperature

543
00:17:30,778 --> 00:17:32,045
changes with elevation. That

544
00:17:32,146 --> 00:17:34,214
means that this site when these

545
00:17:34,315 --> 00:17:35,549
fossil leaves were deposited,

546
00:17:35,583 --> 00:17:37,684
was about a mile higher than

547
00:17:37,752 --> 00:17:38,685
Denver.

548
00:17:38,753 --> 00:17:39,753
Today, it's only half a mile

549
00:17:39,821 --> 00:17:41,588
higher. So, 60 million years

550
00:17:41,656 --> 00:17:42,322
ago, the mountains would be

551
00:17:42,390 --> 00:17:48,629
twice as high as they are today.

552
00:17:48,663 --> 00:17:50,030
>> After the Rockies emerged

553
00:17:50,131 --> 00:17:51,765
from the sea, it took them 10

554
00:17:51,866 --> 00:17:54,301
million years to rise.

555
00:17:54,369 --> 00:17:55,936
60 million years ago, they

556
00:17:56,004 --> 00:17:57,871
reached spectacular heights of

557
00:17:57,939 --> 00:18:00,574
28,000 feet, rivaling the

558
00:18:00,642 --> 00:18:02,109
Himalayas today.

559
00:18:06,781 --> 00:18:08,115
The deep history of the Rocky

560
00:18:08,216 --> 00:18:09,850
Mountains is beginning to take

561
00:18:09,951 --> 00:18:12,953
shape. A weak line in the crust

562
00:18:13,021 --> 00:18:14,955
explains why The Rockies rose

563
00:18:15,023 --> 00:18:18,191
500 to 1,000 miles inland.

564
00:18:18,226 --> 00:18:19,593
Fossil leaves show that the

565
00:18:19,661 --> 00:18:21,194
young Rocky Mountains were once

566
00:18:21,229 --> 00:18:25,032
nearly twice their size.

567
00:18:25,099 --> 00:18:26,266
Half of the rock that formed

568
00:18:26,301 --> 00:18:28,669
them originally has vanished.

569
00:18:28,770 --> 00:18:30,103
Scientists are now trying to

570
00:18:30,138 --> 00:18:31,838
unravel the processes that cut

571
00:18:31,906 --> 00:18:33,674
them down to the size they are

572
00:18:33,741 --> 00:18:35,575
today.

573
00:18:43,625 --> 00:18:45,559
100 million years ago, a vast

574
00:18:45,627 --> 00:18:47,361
inland sea covered the area

575
00:18:47,395 --> 00:18:48,762
where the American Rockies

576
00:18:48,830 --> 00:18:51,198
stand tall today.

577
00:18:51,299 --> 00:18:52,899
70 million years ago, the sea

578
00:18:52,934 --> 00:18:55,035
retreated as The Rockies began

579
00:18:55,103 --> 00:18:58,739
to rise. 60 million years ago,

580
00:18:58,840 --> 00:19:00,073
the Rocky Mountains reached

581
00:19:00,108 --> 00:19:01,575
their pinnacle, towering into

582
00:19:01,643 --> 00:19:04,077
the sky with peaks over 28,000

583
00:19:04,112 --> 00:19:05,912
feet high, rivaling the

584
00:19:06,014 --> 00:19:08,982
Himalayas. Since then, the

585
00:19:09,017 --> 00:19:11,184
entire mountain range has lost

586
00:19:11,252 --> 00:19:14,655
nearly half its height.

587
00:19:14,722 --> 00:19:16,123
Geologists investigating the

588
00:19:16,190 --> 00:19:17,624
history of the Rockies are

589
00:19:17,659 --> 00:19:19,026
trying to discover what

590
00:19:19,093 --> 00:19:20,727
happened to the billions of

591
00:19:20,828 --> 00:19:23,830
tons of rock that went missing.

592
00:19:27,435 --> 00:19:29,369
The investigation starts with a

593
00:19:29,437 --> 00:19:30,737
mystery at the Owl Creek

594
00:19:30,838 --> 00:19:32,005
Mountains in the Wyoming

595
00:19:32,106 --> 00:19:34,441
Rockies.

596
00:19:34,475 --> 00:19:35,642
The mountains are sliced by a

597
00:19:35,710 --> 00:19:37,444
river that has formed a deep

598
00:19:37,478 --> 00:19:40,080
canyon.

599
00:19:40,081 --> 00:19:41,081
>> Well, the Wind River

600
00:19:41,115 --> 00:19:42,616
is very perplexing.

601
00:19:42,650 --> 00:19:43,750
It chose to take a straight

602
00:19:43,818 --> 00:19:45,285
path right through the core of

603
00:19:45,353 --> 00:19:47,454
a major mountain range. This is

604
00:19:47,455 --> 00:19:48,555
not the way that rivers

605
00:19:48,656 --> 00:19:50,557
normally act. Usually they'll

606
00:19:50,625 --> 00:19:51,925
take the easiest route,

607
00:19:51,993 --> 00:19:53,460
which is downhill. But this

608
00:19:53,561 --> 00:19:55,362
river cut right through a major

609
00:19:55,463 --> 00:19:57,097
mountain range and has been

610
00:19:57,198 --> 00:19:58,565
a mystery. It's a very

611
00:19:58,633 --> 00:19:59,900
perplexing issue to early

612
00:19:59,934 --> 00:20:03,637
geologists in the region.

613
00:20:03,738 --> 00:20:05,472
>> This river led to confusion

614
00:20:05,540 --> 00:20:08,008
as early as 1806 when Meriwether

615
00:20:08,109 --> 00:20:10,477
Lewis and William Clark mapped

616
00:20:10,545 --> 00:20:12,079
the area during their famous

617
00:20:12,113 --> 00:20:14,381
expedition to explore uncharted

618
00:20:14,449 --> 00:20:17,017
territory in the west.

619
00:20:17,085 --> 00:20:18,185
When they came to the area

620
00:20:18,286 --> 00:20:20,287
around the Owl Creek Mountains,

621
00:20:20,355 --> 00:20:22,022
they assumed there were two

622
00:20:22,090 --> 00:20:24,291
rivers.

623
00:20:24,359 --> 00:20:25,559
North of the mountain flowed a

624
00:20:25,626 --> 00:20:26,893
river which they named

625
00:20:26,928 --> 00:20:28,462
"Bighorn", thinking it was

626
00:20:28,563 --> 00:20:30,263
different to Wind River in the

627
00:20:30,331 --> 00:20:31,732
South.

628
00:20:31,833 --> 00:20:33,700
But later surveys showed that

629
00:20:33,735 --> 00:20:35,435
the Bighorn and Wind River are

630
00:20:35,470 --> 00:20:37,437
in fact one river that

631
00:20:37,472 --> 00:20:41,541
channeled through the mountain.

632
00:20:41,609 --> 00:20:43,510
Recently, geologists have come

633
00:20:43,544 --> 00:20:45,645
up with a possible answer--an

634
00:20:45,713 --> 00:20:47,547
answer that could also explain

635
00:20:47,648 --> 00:20:49,082
what happened to the once

636
00:20:49,183 --> 00:20:51,885
towering peaks of the Rockies.

637
00:20:51,919 --> 00:20:54,054
They proposed that millions of

638
00:20:54,088 --> 00:20:56,556
tons of rock eroded away,

639
00:20:56,624 --> 00:20:58,091
filled in the valleys, and

640
00:20:58,159 --> 00:20:59,459
covered the lower parts of the

641
00:20:59,527 --> 00:21:00,727
mountains.

642
00:21:00,795 --> 00:21:01,962
It completely changed the

643
00:21:01,996 --> 00:21:04,097
terrain.

644
00:21:04,165 --> 00:21:05,165
>> At one point in

645
00:21:05,233 --> 00:21:06,366
ancient history, the basins in

646
00:21:06,434 --> 00:21:07,467
Wyoming were filled with

647
00:21:07,535 --> 00:21:08,802
sediments that had eroded off

648
00:21:08,903 --> 00:21:09,870
the mountains.

649
00:21:09,904 --> 00:21:11,738
This allowed the river to be at

650
00:21:11,806 --> 00:21:13,006
a higher plain and meander

651
00:21:13,074 --> 00:21:14,174
wherever it wanted to on its

652
00:21:14,242 --> 00:21:17,010
course.

653
00:21:17,078 --> 00:21:18,412
>> As the water flowed, it

654
00:21:18,446 --> 00:21:20,447
carved deep into the sediments

655
00:21:20,515 --> 00:21:23,250
and rock underneath.

656
00:21:23,284 --> 00:21:24,451
>> Eventually, it

657
00:21:24,519 --> 00:21:25,819
cut down a channel into the

658
00:21:25,887 --> 00:21:26,887
mountain and it eventually

659
00:21:26,921 --> 00:21:28,088
excavated right through the

660
00:21:28,156 --> 00:21:31,258
mountain.

661
00:21:31,292 --> 00:21:33,827
>> But this is just a theory.

662
00:21:33,895 --> 00:21:35,695
Now geologists needed to find

663
00:21:35,730 --> 00:21:38,165
proof on the ground.

664
00:21:38,266 --> 00:21:39,966
The search is on for the rock

665
00:21:40,001 --> 00:21:41,501
yhat eroded from the early

666
00:21:41,536 --> 00:21:44,438
Rockies.

667
00:21:44,539 --> 00:21:45,806
The investigation moves to a

668
00:21:45,907 --> 00:21:47,507
series of thousand-foot-tall

669
00:21:47,542 --> 00:21:49,643
hills in the Powder River basin

670
00:21:49,710 --> 00:21:53,346
in Wyoming.

671
00:21:53,448 --> 00:21:55,882
Known as the Pumpkin Buttes,

672
00:21:55,983 --> 00:21:58,084
they stand tall in an otherwise

673
00:21:58,152 --> 00:22:02,255
wide, empty landscape.

674
00:22:02,356 --> 00:22:03,723
Hidden behind the horizon are

675
00:22:03,791 --> 00:22:05,525
the Bighorn Mountains, the

676
00:22:05,626 --> 00:22:09,362
nearest range of the Rockies.

677
00:22:09,430 --> 00:22:10,697
These hills are not formed from

678
00:22:10,731 --> 00:22:13,066
solid rock but a collection of

679
00:22:13,167 --> 00:22:14,334
rubble.

680
00:22:19,040 --> 00:22:20,207
>> This rock, which

681
00:22:20,241 --> 00:22:21,374
we find all over the top of

682
00:22:21,409 --> 00:22:23,210
Pumpkin Buttes in wyoming, is

683
00:22:23,311 --> 00:22:25,278
granite. The closest granitee

684
00:22:25,379 --> 00:22:27,080
find to this area is the Bighorn

685
00:22:27,114 --> 00:22:28,181
Mountains, nearly a

686
00:22:28,282 --> 00:22:31,818
hundred miles to the west.

687
00:22:31,919 --> 00:22:32,986
>> The round shape of the

688
00:22:33,020 --> 00:22:34,721
granite rocks is further proof

689
00:22:34,822 --> 00:22:36,990
that they traveled from afar.

690
00:22:37,091 --> 00:22:39,059
Tumbling downhill in rivers and

691
00:22:39,093 --> 00:22:41,194
kandslides rounded them on

692
00:22:41,262 --> 00:22:42,696
their journey over millions of

693
00:22:42,730 --> 00:22:45,265
years.

694
00:22:45,366 --> 00:22:47,467
This was a crucial step in the

695
00:22:47,535 --> 00:22:49,002
investigation tracing the

696
00:22:49,070 --> 00:22:50,437
missing rock from the early

697
00:22:50,471 --> 00:22:52,639
Rockies.

698
00:22:52,707 --> 00:22:55,709
Rock and cobbles eroded down

699
00:22:55,743 --> 00:22:57,711
from the Bighorn Mountains and

700
00:22:57,745 --> 00:22:59,446
filled up the basin to at least

701
00:22:59,547 --> 00:23:02,015
1,000 feet, the height of the

702
00:23:02,083 --> 00:23:03,283
Pumpkin Buttes.

703
00:23:03,351 --> 00:23:04,284
>> The Pumpkin Buttes

704
00:23:04,352 --> 00:23:06,419
are unique because this used to

705
00:23:06,454 --> 00:23:09,289
be the actual surface level of

706
00:23:09,357 --> 00:23:11,157
the basin itself.

707
00:23:11,192 --> 00:23:13,560
The rest has been eroded away,

708
00:23:13,628 --> 00:23:15,262
a thousand feet of sediment, to

709
00:23:15,363 --> 00:23:18,999
the basin that we see now.

710
00:23:19,100 --> 00:23:20,367
>> But the rubble found here is

711
00:23:20,468 --> 00:23:22,102
nowhere near enough to have

712
00:23:22,169 --> 00:23:26,106
covered the Owl Creek Mountains.

713
00:23:26,173 --> 00:23:27,807
Mclaughlin traveled to Darton's

714
00:23:27,842 --> 00:23:30,076
Peak, 100 miles west in the

715
00:23:30,144 --> 00:23:32,512
Bighorn Mountains.

716
00:23:32,547 --> 00:23:35,181
On a cliff 9,000 feet high, he

717
00:23:35,283 --> 00:23:37,350
finds granitic cobbles that are

718
00:23:37,451 --> 00:23:39,352
strikingly similar to the ones

719
00:23:39,420 --> 00:23:41,254
on the Pumpkin Buttes.

720
00:23:41,355 --> 00:23:43,456
They, too, are from the core of

721
00:23:43,558 --> 00:23:46,960
the Rocky Mountains.

722
00:23:46,994 --> 00:23:47,994
>> The core of the

723
00:23:48,095 --> 00:23:49,095
Rocky Mountains are made

724
00:23:49,163 --> 00:23:50,096
extensively of granite, much

725
00:23:50,164 --> 00:23:51,698
like what you see here.

726
00:23:51,732 --> 00:23:54,000
These are from the Bighorns

727
00:23:54,068 --> 00:23:55,235
that have been transported

728
00:23:55,269 --> 00:23:57,370
down, rolled, and smoothed along

729
00:23:57,438 --> 00:23:58,338
their way to create these

730
00:23:58,372 --> 00:24:02,642
smaller boulders and cobbles.

731
00:24:02,710 --> 00:24:04,277
>> This is strong evidence that

732
00:24:04,345 --> 00:24:05,512
cobbles eroding from the

733
00:24:05,546 --> 00:24:07,347
Rockies filled in the basins

734
00:24:07,381 --> 00:24:09,349
and valleys to at least 9,000

735
00:24:09,417 --> 00:24:11,618
feet, slowly burying the

736
00:24:11,719 --> 00:24:13,153
Mountains under their own

737
00:24:13,220 --> 00:24:14,788
debris.

738
00:24:14,855 --> 00:24:16,222
Where once the mighty Rockies

739
00:24:16,324 --> 00:24:18,758
stood, there was now a gray,

740
00:24:18,859 --> 00:24:20,760
barren plain with only the

741
00:24:20,861 --> 00:24:22,562
peaks of the old mountains

742
00:24:22,597 --> 00:24:27,467
piercing the surface.

743
00:24:27,501 --> 00:24:28,935
The same process has happened

744
00:24:28,970 --> 00:24:31,671
in other mountain chains, too.

745
00:24:31,772 --> 00:24:32,772
There is evidence that the

746
00:24:32,840 --> 00:24:34,774
European Alps were also cut in

747
00:24:34,875 --> 00:24:38,311
half by erosion.

748
00:24:38,379 --> 00:24:40,146
At their base, scientists found

749
00:24:40,214 --> 00:24:42,048
hills formed out of millions of

750
00:24:42,149 --> 00:24:44,150
tons of rock that had cascaded

751
00:24:44,218 --> 00:24:49,022
down and reduced their height.

752
00:24:49,056 --> 00:24:50,924
But the story of the eroding

753
00:24:50,958 --> 00:24:54,761
Rockies wasn't over yet.

754
00:24:54,829 --> 00:24:56,129
After erosion turned the

755
00:24:56,197 --> 00:24:57,931
landscape into a gray cobble

756
00:24:57,965 --> 00:24:59,833
field, another disruption

757
00:24:59,867 --> 00:25:01,568
happened.

758
00:25:01,602 --> 00:25:03,036
Evidence for this is a layer

759
00:25:03,137 --> 00:25:07,140
covering the top of the cobbles.

760
00:25:07,208 --> 00:25:08,208
>> It's very light.

761
00:25:08,275 --> 00:25:09,275
It's very fine-grained.

762
00:25:09,310 --> 00:25:10,677
It's actually a volcanic ash.

763
00:25:10,778 --> 00:25:11,511
As you can see, it's made of

764
00:25:11,579 --> 00:25:12,746
very, very fine-grained

765
00:25:12,780 --> 00:25:14,214
sediments compared to this

766
00:25:14,281 --> 00:25:16,383
boulder conglomerate, which is

767
00:25:16,417 --> 00:25:18,918
made up of big hunks of rock.

768
00:25:18,953 --> 00:25:20,387
It sits directly on top of this

769
00:25:20,454 --> 00:25:21,655
unit, and it was laid

770
00:25:21,689 --> 00:25:24,157
horizontally from mostly ash

771
00:25:24,191 --> 00:25:27,360
fall.

772
00:25:27,461 --> 00:25:28,928
>> This fine-grained ash

773
00:25:28,996 --> 00:25:31,064
suggests huge volcanic eruptions

774
00:25:31,098 --> 00:25:34,067
nearby. They spewed out thick

775
00:25:34,101 --> 00:25:36,336
clouds of hot air, ash, and

776
00:25:36,370 --> 00:25:38,338
volcanic rock, which settled on

777
00:25:38,372 --> 00:25:42,509
the ground. Radiocarbon dating

778
00:25:42,543 --> 00:25:43,877
the rock revealed that it

779
00:25:43,911 --> 00:25:47,781
happened 25 million years ago.

780
00:25:47,815 --> 00:25:49,449
>> Ash was deposited as it came

781
00:25:49,550 --> 00:25:51,351
out of the sky as plumes.

782
00:25:51,419 --> 00:25:52,619
Most of it came from the west

783
00:25:52,653 --> 00:25:54,988
and was deposited in basins

784
00:25:55,056 --> 00:25:56,823
across Wyoming.

785
00:25:56,891 --> 00:25:58,191
>> After the lower Rockies were

786
00:25:58,259 --> 00:26:00,193
buried by their own rock,

787
00:26:00,261 --> 00:26:02,362
volcanic ash settled on top and

788
00:26:02,430 --> 00:26:03,730
covered the area with a thick

789
00:26:03,831 --> 00:26:08,334
white sheet.

790
00:26:08,369 --> 00:26:09,269
>> At the time of

791
00:26:09,336 --> 00:26:10,704
the deepest basin-fill of this

792
00:26:10,738 --> 00:26:12,272
volcanic material, all you would

793
00:26:12,339 --> 00:26:13,640
see in this area would be the

794
00:26:13,708 --> 00:26:15,442
very tops of the peaks exposed.

795
00:26:15,543 --> 00:26:16,443
The rest would be large,

796
00:26:16,510 --> 00:26:20,413
extensive lateral ash sheets.

797
00:26:20,448 --> 00:26:21,915
>> Erosion and volcanism

798
00:26:21,982 --> 00:26:23,283
completely transformed the

799
00:26:23,350 --> 00:26:26,920
terrain and buried The Rockies.

800
00:26:26,987 --> 00:26:28,321
But then over millions of

801
00:26:28,355 --> 00:26:30,724
years, rivers flushed out the

802
00:26:30,825 --> 00:26:32,726
eroded rock.

803
00:26:32,793 --> 00:26:33,827
Most of it is thought to have

804
00:26:33,894 --> 00:26:35,228
ended up in the Missouri and

805
00:26:35,262 --> 00:26:36,796
Mississippi rivers from where

806
00:26:36,831 --> 00:26:40,366
it was transported into the sea.

807
00:26:40,434 --> 00:26:42,068
What's left are the mountains

808
00:26:42,136 --> 00:26:45,238
we see today.

809
00:26:45,272 --> 00:26:46,706
This also confirmed the theory

810
00:26:46,807 --> 00:26:48,174
geologists had about the

811
00:26:48,275 --> 00:26:51,277
formation of Wind River Canyon.

812
00:26:51,345 --> 00:26:52,979
The incredible amount of infill

813
00:26:53,047 --> 00:26:55,682
buried the Owl Creek Mountain.

814
00:26:55,716 --> 00:26:57,450
Wind River flowed on top and

815
00:26:57,518 --> 00:26:59,486
began carving into the mountain,

816
00:26:59,520 --> 00:27:00,954
creating the canyon we see

817
00:27:01,055 --> 00:27:06,593
today.

818
00:27:06,694 --> 00:27:08,061
The investigation into what

819
00:27:08,129 --> 00:27:09,395
happened to the early Rocky

820
00:27:09,497 --> 00:27:11,231
Mountains reveals two major

821
00:27:11,298 --> 00:27:13,399
clues.

822
00:27:13,501 --> 00:27:14,768
Granite found on the Pumpkin

823
00:27:14,835 --> 00:27:16,136
Buttes is evidence that the

824
00:27:16,237 --> 00:27:17,871
early Rockies dumped their

825
00:27:17,938 --> 00:27:21,508
eroded rock into the basins.

826
00:27:21,575 --> 00:27:22,942
Wind River Canyon cutting

827
00:27:23,043 --> 00:27:24,577
straight through the Owl Creek

828
00:27:24,678 --> 00:27:26,146
Mountains is evidence that the

829
00:27:26,213 --> 00:27:27,580
Rockies were buried by their

830
00:27:27,681 --> 00:27:30,784
own debris.

831
00:27:30,851 --> 00:27:32,752
The once mighty Rockies had now

832
00:27:32,853 --> 00:27:34,654
been cut down to nearly half

833
00:27:34,688 --> 00:27:36,689
their original size,

834
00:27:36,757 --> 00:27:39,926
but the story was far from over.

835
00:27:39,960 --> 00:27:40,927
Before they became the

836
00:27:40,961 --> 00:27:42,829
Mountains we know today, they

837
00:27:42,863 --> 00:27:44,364
would have to endure an even

838
00:27:44,465 --> 00:27:45,064
greater assault.

839
00:27:52,803 --> 00:27:54,337
70 million years ago, a great

840
00:27:54,404 --> 00:27:56,706
inland sea disappeared and the

841
00:27:56,807 --> 00:27:58,608
Rocky Mountains emerged from

842
00:27:58,709 --> 00:28:00,810
yhe sea floor.

843
00:28:00,911 --> 00:28:02,245
60 million years ago, they

844
00:28:02,312 --> 00:28:04,080
reached their peak height--

845
00:28:04,147 --> 00:28:07,049
twice what it is today.

846
00:28:07,084 --> 00:28:09,151
Then for millions of years, the

847
00:28:09,253 --> 00:28:10,953
Rockies slowly eroded away to

848
00:28:10,988 --> 00:28:12,888
half their original height

849
00:28:12,990 --> 00:28:14,957
until 3 million years ago

850
00:28:14,992 --> 00:28:16,492
another dramatic chapter in

851
00:28:16,526 --> 00:28:18,427
their story began that would

852
00:28:18,528 --> 00:28:19,629
transform them into the

853
00:28:19,696 --> 00:28:21,964
Mountains we know today.

854
00:28:29,406 --> 00:28:30,873
Geologist and photographer Bob

855
00:28:30,907 --> 00:28:33,175
Anderson takes to the air.

856
00:28:33,243 --> 00:28:34,677
He is looking for clues that

857
00:28:34,711 --> 00:28:36,178
will tell him how the mountains

858
00:28:36,246 --> 00:28:39,448
have evolved.

859
00:28:39,516 --> 00:28:40,950
First, he flies over Boulder

860
00:28:40,984 --> 00:28:45,421
Canyon in the Colorado Rockies.

861
00:28:45,489 --> 00:28:46,889
It is an area that has remained

862
00:28:46,990 --> 00:28:49,225
almost unchanged over millions

863
00:28:49,259 --> 00:28:51,060
of years.

864
00:28:51,094 --> 00:28:52,061
>> So, this is Boulder

865
00:28:52,129 --> 00:28:53,396
Canyon we're flying up right

866
00:28:53,397 --> 00:28:56,399
now and you can see how the

867
00:28:56,433 --> 00:28:59,402
river has incised maybe a few

868
00:28:59,403 --> 00:29:00,970
hundred feet down into

869
00:29:01,038 --> 00:29:02,972
otherwise relatively rolling

870
00:29:03,040 --> 00:29:08,077
terrain.

871
00:29:08,145 --> 00:29:09,078
>> The mountain peaks that

872
00:29:09,146 --> 00:29:10,346
existed on the young Rocky

873
00:29:10,414 --> 00:29:12,315
Mountains were rounded off as

874
00:29:12,349 --> 00:29:14,350
rivers and streams eroded the

875
00:29:14,418 --> 00:29:17,787
rock.

876
00:29:17,888 --> 00:29:19,322
>> It's this rolling terrain

877
00:29:19,389 --> 00:29:22,124
that the landscape looked like

878
00:29:22,159 --> 00:29:23,326
in the aftermath of

879
00:29:23,393 --> 00:29:24,694
the mountain-building event that

880
00:29:24,795 --> 00:29:26,228
ended about 50 million years

881
00:29:26,330 --> 00:29:30,066
ago.

882
00:29:30,133 --> 00:29:31,701
>> But as Anderson climbs higher

883
00:29:31,802 --> 00:29:33,069
to Longs Peaks in the Rocky

884
00:29:33,136 --> 00:29:34,970
Mountain National Park, the

885
00:29:35,038 --> 00:29:37,940
terrain changes.

886
00:29:37,974 --> 00:29:39,342
Instead of rolling hills, there

887
00:29:39,409 --> 00:29:40,776
are rugged mountains with

888
00:29:40,844 --> 00:29:43,212
steep, jagged cliffs.

889
00:29:43,246 --> 00:29:44,413
It's evidence that another

890
00:29:44,481 --> 00:29:47,983
force has been at work.

891
00:29:48,051 --> 00:29:49,585
The most famous of these cliffs

892
00:29:49,619 --> 00:29:51,687
is "the Diamond".

893
00:29:51,788 --> 00:29:53,255
Named for its shape, it's a

894
00:29:53,323 --> 00:29:55,591
vertical wall with a sheer 900

895
00:29:55,692 --> 00:29:57,793
foot drop.

896
00:29:57,861 --> 00:29:59,962
The summit, about 45,000 square

897
00:30:00,030 --> 00:30:02,231
feet, is the same size as a

898
00:30:02,299 --> 00:30:04,934
football field.

899
00:30:04,968 --> 00:30:05,701
>> Well, we're flying

900
00:30:05,769 --> 00:30:08,337
beside Longs Peak, one of the

901
00:30:08,405 --> 00:30:09,972
biggest climbing

902
00:30:10,040 --> 00:30:11,941
challenges in The Rockies.

903
00:30:11,975 --> 00:30:13,509
For a century, it's been a

904
00:30:13,610 --> 00:30:15,511
climbing mecca.

905
00:30:15,612 --> 00:30:17,913
It's a gorgeous intact piece

906
00:30:17,948 --> 00:30:20,483
of rock.

907
00:30:20,550 --> 00:30:22,485
>> This awesome wall is the most

908
00:30:22,552 --> 00:30:24,086
difficult climb in the whole of

909
00:30:24,121 --> 00:30:26,021
the Rockies, and since it was

910
00:30:26,089 --> 00:30:27,490
officially opened to climbers

911
00:30:27,557 --> 00:30:30,259
in 1960 has claimed over 50

912
00:30:30,293 --> 00:30:35,464
lives.

913
00:30:35,499 --> 00:30:36,632
Back on the ground,

914
00:30:36,666 --> 00:30:37,833
Anderson is looking for

915
00:30:37,934 --> 00:30:39,301
evidence that will reveal the

916
00:30:39,369 --> 00:30:40,936
processes that shaped the

917
00:30:41,004 --> 00:30:43,472
jagged peaks.

918
00:30:43,573 --> 00:30:45,741
On a hillside, he finds

919
00:30:45,809 --> 00:30:47,743
mysterious large boulders

920
00:30:47,844 --> 00:30:48,911
scattered across the valley

921
00:30:48,979 --> 00:30:50,379
floor.

922
00:30:50,447 --> 00:30:53,015
[tapping rock]

923
00:30:53,116 --> 00:30:54,550
A closer look uncovers some

924
00:30:54,651 --> 00:30:58,754
secrets about their origin.

925
00:30:58,822 --> 00:30:59,822
>> I'm standing in

926
00:30:59,856 --> 00:31:01,190
front of a rounded boulder that

927
00:31:01,291 --> 00:31:03,392
itself is sitting on a smooth

928
00:31:03,460 --> 00:31:06,462
bedrock outcrop.

929
00:31:06,530 --> 00:31:07,830
Both the boulder and the

930
00:31:07,898 --> 00:31:09,899
outcrop are covered in lichen

931
00:31:09,933 --> 00:31:12,301
here of green to black to

932
00:31:12,369 --> 00:31:15,104
gray colors, and therefore I had

933
00:31:15,205 --> 00:31:16,705
to whack off a piece of the

934
00:31:16,740 --> 00:31:18,641
rock in order to see inside the

935
00:31:18,742 --> 00:31:19,708
rock.

936
00:31:19,743 --> 00:31:20,810
And indeed it is different.

937
00:31:20,844 --> 00:31:22,278
The minerals that I see and the

938
00:31:22,345 --> 00:31:23,913
texture of the rock is

939
00:31:24,014 --> 00:31:25,347
different from the underlying

940
00:31:25,382 --> 00:31:27,016
rock. And therefore the rock is

941
00:31:27,083 --> 00:31:31,554
foreign to this particular site.

942
00:31:31,655 --> 00:31:33,088
>> Anderson searches the ground

943
00:31:33,156 --> 00:31:35,024
for more clues as to how this

944
00:31:35,091 --> 00:31:37,726
massive boulder got here.

945
00:31:37,828 --> 00:31:39,628
Nearby, he finds a smooth

946
00:31:39,729 --> 00:31:41,931
surface with very fine scratch

947
00:31:41,998 --> 00:31:44,633
marks.

948
00:31:44,734 --> 00:31:45,835
>> I'm sitting on a

949
00:31:45,902 --> 00:31:47,470
polished surface. This little

950
00:31:47,537 --> 00:31:49,738
piece right here is smooth to

951
00:31:49,840 --> 00:31:51,674
the touch. And if I look at it

952
00:31:51,741 --> 00:31:53,442
in a certain way that the light

953
00:31:53,477 --> 00:31:55,110
glints off of it just right, I

954
00:31:55,178 --> 00:31:56,178
can see that there are

955
00:31:56,246 --> 00:31:57,746
scratches running in this

956
00:31:57,814 --> 00:31:59,715
direction across the surface.

957
00:31:59,816 --> 00:32:01,083
>> The only force that could

958
00:32:01,184 --> 00:32:02,651
have produced these fine,

959
00:32:02,719 --> 00:32:04,720
parallel scratches on the rock

960
00:32:04,821 --> 00:32:09,358
is ice, and lots of it.

961
00:32:09,426 --> 00:32:11,093
It's a clue that a massive

962
00:32:11,194 --> 00:32:15,464
glacier once filled this valley.

963
00:32:15,532 --> 00:32:16,465
>> And that tells me

964
00:32:16,533 --> 00:32:17,533
that the glacier came

965
00:32:17,634 --> 00:32:18,901
down-valley, came across this

966
00:32:19,002 --> 00:32:22,037
surface and eroded it.

967
00:32:22,072 --> 00:32:23,439
Each one of these scratches

968
00:32:23,507 --> 00:32:25,207
corresponds to a sand grain

969
00:32:25,242 --> 00:32:27,142
embedded in the sole of the ice

970
00:32:27,244 --> 00:32:28,878
that just like sandpaper

971
00:32:28,945 --> 00:32:30,513
smoothes off the surface. So

972
00:32:30,580 --> 00:32:32,248
zillions of sand grains over

973
00:32:32,315 --> 00:32:34,416
thousands of years will have

974
00:32:34,484 --> 00:32:38,120
eroded this surface smooth.

975
00:32:38,154 --> 00:32:39,588
>> As glaciers flowed down the

976
00:32:39,656 --> 00:32:41,690
valley, they picked up rocks

977
00:32:41,758 --> 00:32:43,692
and grit.

978
00:32:43,760 --> 00:32:45,661
The ice pushed down on these

979
00:32:45,695 --> 00:32:46,962
cutting tools with the weight

980
00:32:47,063 --> 00:32:48,864
of over a thousand fully loaded

981
00:32:48,965 --> 00:32:51,600
garbage trucks.

982
00:32:51,701 --> 00:32:53,402
It left scratch marks all over

983
00:32:53,503 --> 00:32:55,404
the Rockies up to 1,000 feet

984
00:32:55,472 --> 00:32:56,972
high.

985
00:32:57,040 --> 00:32:59,241
This is evidence that a massive

986
00:32:59,309 --> 00:33:01,110
wall of ice covered this part

987
00:33:01,177 --> 00:33:02,811
of The Rockies and shaped the

988
00:33:02,846 --> 00:33:04,914
mountains.

989
00:33:05,015 --> 00:33:06,382
The ice ripped out the rock

990
00:33:06,483 --> 00:33:08,183
from the valley walls and left

991
00:33:08,218 --> 00:33:10,452
behind the jagged cliffs and

992
00:33:10,487 --> 00:33:14,924
rugged edges.

993
00:33:14,991 --> 00:33:15,891
>> For the last few

994
00:33:15,926 --> 00:33:17,092
million years, perhaps 3

995
00:33:17,193 --> 00:33:18,394
million years, glaciers have

996
00:33:18,461 --> 00:33:20,462
come and gone from the Rocky

997
00:33:20,530 --> 00:33:22,197
Mountains. And every time they

998
00:33:22,265 --> 00:33:23,832
come across the landscape,

999
00:33:23,900 --> 00:33:25,200
they're capable of eroding that

1000
00:33:25,302 --> 00:33:27,102
landscape at rates that are

1001
00:33:27,170 --> 00:33:29,638
perhaps fractions of an inch

1002
00:33:29,739 --> 00:33:31,907
per year, meaning that over the

1003
00:33:32,008 --> 00:33:35,277
course of one glacial cycle you

1004
00:33:35,378 --> 00:33:38,547
perhaps erode 10, 20 feet

1005
00:33:38,648 --> 00:33:40,649
of rock.

1006
00:33:40,750 --> 00:33:42,451
>> Ice also created the broad

1007
00:33:42,485 --> 00:33:44,286
Canyons.

1008
00:33:44,387 --> 00:33:46,288
With every ice age, new glaciers

1009
00:33:46,356 --> 00:33:48,257
ground their way down v-shaped

1010
00:33:48,291 --> 00:33:49,825
river valleys and turned them

1011
00:33:49,893 --> 00:33:56,065
into broad u-shaped canyons.

1012
00:33:56,099 --> 00:33:56,932
>> For the glacier,

1013
00:33:57,000 --> 00:33:58,367
the whole valley is its

1014
00:33:58,435 --> 00:34:00,469
channel, so any place where the

1015
00:34:00,570 --> 00:34:02,438
glacier touches the wall it's

1016
00:34:02,472 --> 00:34:04,073
capable of eroding it.

1017
00:34:04,174 --> 00:34:05,874
And therefore the walls

1018
00:34:05,942 --> 00:34:07,309
will be made more vertical on

1019
00:34:07,344 --> 00:34:08,877
the edges and be flattened on

1020
00:34:08,979 --> 00:34:10,613
the base, until it gets

1021
00:34:10,680 --> 00:34:12,881
to now a u-shape which then

1022
00:34:12,949 --> 00:34:15,484
propagates downward.

1023
00:34:15,518 --> 00:34:16,986
>> Ice also explains the

1024
00:34:17,053 --> 00:34:20,623
presence of these boulders.

1025
00:34:20,690 --> 00:34:22,057
They hitchhiked at the bottom

1026
00:34:22,125 --> 00:34:23,792
of a glacier down the frozen

1027
00:34:23,860 --> 00:34:25,761
valley.

1028
00:34:25,795 --> 00:34:27,329
When the last ice age came to

1029
00:34:27,430 --> 00:34:29,331
an end and the glaciers melted

1030
00:34:29,432 --> 00:34:31,433
about 10,000 years ago, the

1031
00:34:31,501 --> 00:34:36,772
boulders were left behind.

1032
00:34:36,806 --> 00:34:38,774
Scientists had found two pieces

1033
00:34:38,842 --> 00:34:39,875
of evidence that were

1034
00:34:39,976 --> 00:34:41,210
responsible for the jagged

1035
00:34:41,244 --> 00:34:43,946
looks of the Rockies today.

1036
00:34:43,980 --> 00:34:45,614
A solitary boulder foreign to

1037
00:34:45,682 --> 00:34:47,149
the area could have only been

1038
00:34:47,217 --> 00:34:50,419
transported here by ice.

1039
00:34:50,520 --> 00:34:52,254
Striations showed scientists

1040
00:34:52,288 --> 00:34:53,889
that a glacier at least 1,000

1041
00:34:53,957 --> 00:34:57,326
feet thick covered the Rockies.

1042
00:34:57,360 --> 00:34:58,794
Ice was responsible for the

1043
00:34:58,862 --> 00:35:00,429
dramatic shape of the Rockies

1044
00:35:00,497 --> 00:35:01,964
today.

1045
00:35:02,032 --> 00:35:04,033
But the mountains keep evolving.

1046
00:35:04,067 --> 00:35:05,668
Recently, scientists discovered

1047
00:35:05,702 --> 00:35:07,603
alarming evidence that they may

1048
00:35:07,704 --> 00:35:10,839
collapse into a deep rift.

1049
00:35:20,028 --> 00:35:21,962
For the last 70 million years,

1050
00:35:22,030 --> 00:35:24,131
compression, erosion and ice

1051
00:35:24,232 --> 00:35:25,299
have sculpted the Rocky

1052
00:35:25,333 --> 00:35:26,600
Mountains to their present

1053
00:35:26,668 --> 00:35:28,402
formation.

1054
00:35:28,503 --> 00:35:29,837
But the geology that created

1055
00:35:29,871 --> 00:35:30,771
this impressive

1056
00:35:30,872 --> 00:35:32,973
Mountain range has also the

1057
00:35:33,041 --> 00:35:35,876
potential to destroy it.

1058
00:35:35,977 --> 00:35:38,412
Over the last 25 million years,

1059
00:35:38,479 --> 00:35:40,047
a gigantic rift has been

1060
00:35:40,114 --> 00:35:41,415
opening up at the southern end

1061
00:35:41,482 --> 00:35:43,951
of the Rocky Mountains.

1062
00:35:44,052 --> 00:35:46,420
It stretches over 160,000 square

1063
00:35:46,487 --> 00:35:48,922
miles and is known as the Rio

1064
00:35:48,957 --> 00:35:51,225
Grande Valley.

1065
00:35:51,292 --> 00:35:52,392
Geologists are eager to

1066
00:35:52,427 --> 00:35:54,061
investigate how this giant

1067
00:35:54,128 --> 00:35:55,696
rifting valley could affect the

1068
00:35:55,763 --> 00:36:00,334
future of the Rockies.

1069
00:36:00,401 --> 00:36:01,702
They find their first lead in

1070
00:36:01,769 --> 00:36:03,837
San Ysidro, New Mexico, north

1071
00:36:03,872 --> 00:36:06,473
of Albuquerque.

1072
00:36:06,507 --> 00:36:08,675
The area is dominated by

1073
00:36:08,776 --> 00:36:11,144
bright, yellow, porous rock

1074
00:36:11,212 --> 00:36:14,214
known as travertines.

1075
00:36:14,315 --> 00:36:16,583
Curiously, geologists think

1076
00:36:16,684 --> 00:36:20,587
this rock forms from water.

1077
00:36:20,588 --> 00:36:23,323
>> This water has some unusual

1078
00:36:23,391 --> 00:36:24,591
characteristics, and that is

1079
00:36:24,692 --> 00:36:26,693
this water's capable of

1080
00:36:26,694 --> 00:36:28,295
precipitating, or depositing, a

1081
00:36:28,329 --> 00:36:30,564
new rock called travertine. It's

1082
00:36:30,598 --> 00:36:32,199
kind of like the scale in your

1083
00:36:32,233 --> 00:36:34,835
teapot.

1084
00:36:34,869 --> 00:36:36,103
>> Travertine rock is

1085
00:36:36,137 --> 00:36:38,238
made out of calcite, the same

1086
00:36:38,306 --> 00:36:39,873
material that builds up lime

1087
00:36:39,941 --> 00:36:44,511
scale. These rocks grow very

1088
00:36:44,579 --> 00:36:47,281
rapidly. Some enlarge by a few

1089
00:36:47,315 --> 00:36:49,149
inches per month.

1090
00:36:49,217 --> 00:36:50,217
>> About a liter of

1091
00:36:50,218 --> 00:36:51,919
the water will be able to drop

1092
00:36:51,953 --> 00:36:54,321
out or precipitate a little

1093
00:36:54,389 --> 00:36:56,189
pile of calcite about as big as

1094
00:36:56,190 --> 00:36:58,592
an aspirin tablet.

1095
00:36:58,660 --> 00:37:00,193
>> Like lime scale building up

1096
00:37:00,228 --> 00:37:01,595
in a hot water kettle,

1097
00:37:01,663 --> 00:37:03,664
travertines form around warm

1098
00:37:03,731 --> 00:37:08,502
springs. Measurements confirm

1099
00:37:08,569 --> 00:37:10,003
that water temperature around

1100
00:37:10,038 --> 00:37:12,005
the travertines is roughly 77

1101
00:37:12,040 --> 00:37:15,309
degrees.

1102
00:37:15,410 --> 00:37:16,743
Besides the ability to build

1103
00:37:16,778 --> 00:37:19,413
rock, this hot water has more

1104
00:37:19,480 --> 00:37:23,317
secrets to tell.

1105
00:37:23,384 --> 00:37:24,484
Laura Crossey and Karl

1106
00:37:24,585 --> 00:37:26,453
Karlstrom have a hunch that the

1107
00:37:26,487 --> 00:37:28,555
water is warmed up by heat from

1108
00:37:28,589 --> 00:37:30,958
the Earth's interior, rising up

1109
00:37:31,025 --> 00:37:34,294
through cracks in the rock.

1110
00:37:34,362 --> 00:37:36,129
They form as the rift valley

1111
00:37:36,230 --> 00:37:38,999
pulls apart.

1112
00:37:39,033 --> 00:37:40,934
Climbing down a cave 25 feet

1113
00:37:41,035 --> 00:37:42,302
below the surface, they are

1114
00:37:42,370 --> 00:37:47,574
hoping to find further evidence.

1115
00:37:47,642 --> 00:37:50,377
The water contains microbes.

1116
00:37:50,478 --> 00:37:51,912
They are microscopically small

1117
00:37:51,946 --> 00:37:53,914
organisms.

1118
00:37:53,948 --> 00:37:55,282
Most of them consist of only

1119
00:37:55,316 --> 00:37:57,584
one cell.

1120
00:37:57,652 --> 00:37:58,952
When scientists analyzed their

1121
00:37:59,020 --> 00:38:00,721
genes in the lab, they found

1122
00:38:00,755 --> 00:38:03,223
something remarkable.

1123
00:38:03,291 --> 00:38:04,358
>> What we found in springs like

1124
00:38:04,392 --> 00:38:06,393
this by doing the dna analysis

1125
00:38:06,461 --> 00:38:07,761
is that the microbes that are

1126
00:38:07,862 --> 00:38:10,197
coming up these faults are much

1127
00:38:10,264 --> 00:38:11,832
more like what we find

1128
00:38:11,933 --> 00:38:13,467
at mid-ocean ridges than like

1129
00:38:13,568 --> 00:38:14,768
the rivers and streams we would

1130
00:38:14,836 --> 00:38:18,105
expect in a continental setting.

1131
00:38:18,172 --> 00:38:19,673
>> Mid-ocean ridges are very

1132
00:38:19,741 --> 00:38:21,375
long mountain chains under the

1133
00:38:21,476 --> 00:38:24,378
sea. Just like the rift valley,

1134
00:38:24,479 --> 00:38:26,313
they also form in geologically

1135
00:38:26,381 --> 00:38:28,482
active areas where lava

1136
00:38:28,549 --> 00:38:30,650
constantly erupts and builds up

1137
00:38:30,718 --> 00:38:32,486
new crust.

1138
00:38:32,553 --> 00:38:34,221
Any living organism surviving

1139
00:38:34,288 --> 00:38:36,023
down there has to be able to

1140
00:38:36,124 --> 00:38:39,459
cope with these hot conditions.

1141
00:38:39,494 --> 00:38:41,028
>> The springs here in the

1142
00:38:41,129 --> 00:38:42,462
mid-ocean ridge settings are

1143
00:38:42,563 --> 00:38:43,730
also characterized by

1144
00:38:43,765 --> 00:38:45,365
the upwelling of deep hot fluids

1145
00:38:45,400 --> 00:38:46,933
from within the Earth,

1146
00:38:47,001 --> 00:38:48,802
indicating that these both are

1147
00:38:48,836 --> 00:38:50,470
connected to that deep tectonic

1148
00:38:50,571 --> 00:38:52,205
setting.

1149
00:38:52,273 --> 00:38:53,473
>> The microbes suggest

1150
00:38:53,541 --> 00:38:55,275
deep tectonic forces are at

1151
00:38:55,309 --> 00:38:58,111
work, but there is even more

1152
00:38:58,179 --> 00:39:00,213
compelling evidence.

1153
00:39:00,281 --> 00:39:01,648
Karlstrom and Crossey find an

1154
00:39:01,749 --> 00:39:04,017
unusually high amount of gas

1155
00:39:04,085 --> 00:39:06,119
bubbling up through the water.

1156
00:39:06,187 --> 00:39:07,387
>> These samples are kind of fun

1157
00:39:07,455 --> 00:39:08,755
because it looks like an empty

1158
00:39:08,823 --> 00:39:10,190
glass bottle, but it started out

1159
00:39:10,291 --> 00:39:12,092
full of water. And then we

1160
00:39:12,193 --> 00:39:13,393
filled up--turned it upside-

1161
00:39:13,461 --> 00:39:14,761
down in the water, and the gas

1162
00:39:14,829 --> 00:39:15,929
displaced the water until it's

1163
00:39:16,030 --> 00:39:17,464
full of gas.

1164
00:39:17,565 --> 00:39:18,999
>> A lab analysis identifies the

1165
00:39:19,033 --> 00:39:20,834
gas as helium.

1166
00:39:20,902 --> 00:39:22,569
This is the conclusive evidence

1167
00:39:22,637 --> 00:39:24,271
that deep tectonic forces are

1168
00:39:24,372 --> 00:39:26,073
at work here.

1169
00:39:26,107 --> 00:39:28,742
>> The helium is the most

1170
00:39:28,843 --> 00:39:30,010
interesting gas for us. It's

1171
00:39:30,078 --> 00:39:31,545
the smoking gun of evidence

1172
00:39:31,646 --> 00:39:33,647
for where these fluids

1173
00:39:33,748 --> 00:39:34,848
have come from.

1174
00:39:34,916 --> 00:39:36,450
There's two forms of helium, but

1175
00:39:36,484 --> 00:39:38,819
yt's the helium 3 that we're

1176
00:39:38,920 --> 00:39:40,287
most interested in, and that

1177
00:39:40,388 --> 00:39:42,556
form of helium is only derived

1178
00:39:42,657 --> 00:39:45,192
from the Earth's mantle.

1179
00:39:45,293 --> 00:39:46,359
>> The mantle is a part of the

1180
00:39:46,461 --> 00:39:48,361
Earth's interior 30 miles below

1181
00:39:48,463 --> 00:39:49,663
the surface.

1182
00:39:49,730 --> 00:39:51,064
It is made up of hot, molten

1183
00:39:51,099 --> 00:39:53,300
rock.

1184
00:39:53,367 --> 00:39:55,569
In areas where magma moves up,

1185
00:39:55,636 --> 00:39:57,571
pressure on top of it decreases

1186
00:39:57,638 --> 00:39:59,005
and gases such as helium are

1187
00:39:59,107 --> 00:40:01,374
released.

1188
00:40:01,476 --> 00:40:02,843
They find their way through

1189
00:40:02,910 --> 00:40:04,444
faults and cracks until they

1190
00:40:04,479 --> 00:40:07,914
reach the surface.

1191
00:40:07,982 --> 00:40:10,083
So, helium gas is conclusive

1192
00:40:10,184 --> 00:40:11,918
proof that geological forces

1193
00:40:12,019 --> 00:40:13,186
deep under the Earth are

1194
00:40:13,287 --> 00:40:15,288
building up,

1195
00:40:15,356 --> 00:40:16,656
and the effect it will have on

1196
00:40:16,724 --> 00:40:19,826
the Rockies is devastating.

1197
00:40:19,927 --> 00:40:21,094
>> The Rio Grande rift

1198
00:40:21,162 --> 00:40:22,529
is an area that's

1199
00:40:22,563 --> 00:40:24,464
tectonically active

1200
00:40:24,532 --> 00:40:25,532
in a different way than you

1201
00:40:25,566 --> 00:40:27,200
think of building of mountains.

1202
00:40:27,268 --> 00:40:29,903
This area is the next stage

1203
00:40:29,971 --> 00:40:31,471
in the life sometimes of a

1204
00:40:31,539 --> 00:40:33,106
mountain belt where it starts to

1205
00:40:33,174 --> 00:40:35,809
collapse, it starts to extend.

1206
00:40:35,910 --> 00:40:37,344
>> As hot magma

1207
00:40:37,378 --> 00:40:38,979
surges upwards from 30 miles

1208
00:40:39,013 --> 00:40:40,814
below the surface, it forces the

1209
00:40:40,882 --> 00:40:44,184
area on top to spread.

1210
00:40:44,252 --> 00:40:46,520
The surface stretches and thins

1211
00:40:46,554 --> 00:40:49,789
and opens up a deep chasm.

1212
00:40:49,824 --> 00:40:51,057
As the rift opens, the

1213
00:40:51,092 --> 00:40:53,260
mountains to each side crumble

1214
00:40:53,327 --> 00:40:57,464
into the valley.

1215
00:40:57,532 --> 00:40:58,532
>> You can think of a piece

1216
00:40:58,633 --> 00:41:00,634
of taffy that's being stretched,

1217
00:41:00,701 --> 00:41:02,235
and it might break on the top.

1218
00:41:02,270 --> 00:41:04,538
And those breaks would lower

1219
00:41:04,605 --> 00:41:06,239
pieces of the--they would drop

1220
00:41:06,274 --> 00:41:08,375
down. And then once you have

1221
00:41:08,442 --> 00:41:10,644
what's called a fault valley,

1222
00:41:10,711 --> 00:41:13,146
then the sediments wash in from

1223
00:41:13,181 --> 00:41:14,347
the high mountains. It's an

1224
00:41:14,448 --> 00:41:16,283
immense structure. It's

1225
00:41:16,350 --> 00:41:18,552
about 6 miles deep. It's about

1226
00:41:18,619 --> 00:41:20,086
as deep as Mount Everest is

1227
00:41:20,154 --> 00:41:22,189
high. But when you drive

1228
00:41:22,256 --> 00:41:23,623
across it or you look at it

1229
00:41:23,691 --> 00:41:26,193
from any vantage point,

1230
00:41:26,260 --> 00:41:28,962
you don't see that entire depth

1231
00:41:28,996 --> 00:41:30,163
because it's all been filled

1232
00:41:30,231 --> 00:41:31,164
with sand and gravel

1233
00:41:31,232 --> 00:41:33,166
progressively as the extension

1234
00:41:33,234 --> 00:41:34,534
took place.

1235
00:41:34,635 --> 00:41:36,269
>> Today, the Rio Grande rift

1236
00:41:36,370 --> 00:41:39,072
stretches over 160,000 square

1237
00:41:39,173 --> 00:41:41,374
miles from Mexico in the south

1238
00:41:41,442 --> 00:41:42,809
where it's broadest, to

1239
00:41:42,910 --> 00:41:44,711
Colorado in the north where

1240
00:41:44,812 --> 00:41:46,980
it's only just begun to open up.

1241
00:41:47,048 --> 00:41:48,448
>> This rift is propagating

1242
00:41:48,516 --> 00:41:50,617
northwards into the higher

1243
00:41:50,718 --> 00:41:51,718
Colorado Rockies.

1244
00:41:51,786 --> 00:41:52,686
What's gonna happen to

1245
00:41:52,720 --> 00:41:54,054
Colorado, those mountains will

1246
00:41:54,088 --> 00:41:57,157
probably collapse by rifting,

1247
00:41:57,258 --> 00:41:58,992
as the rift propagates, zippers

1248
00:41:59,093 --> 00:42:00,327
northward. And you can

1249
00:42:00,428 --> 00:42:02,429
visualize that what's

1250
00:42:02,463 --> 00:42:05,165
now in Colorado is more similar

1251
00:42:05,266 --> 00:42:06,800
to what was in New Mexico

1252
00:42:06,867 --> 00:42:08,068
before the Rio Grande rift

1253
00:42:08,135 --> 00:42:09,803
opened and before the mountains

1254
00:42:09,904 --> 00:42:13,173
collapsed.

1255
00:42:13,241 --> 00:42:14,274
>> Looking ahead in the distant

1256
00:42:14,342 --> 00:42:15,408
future, there could be

1257
00:42:15,443 --> 00:42:17,277
challenging times.

1258
00:42:17,345 --> 00:42:19,179
The tectonic forces that created

1259
00:42:19,247 --> 00:42:20,614
the Rockies could eventually

1260
00:42:20,648 --> 00:42:22,983
lead to their destruction.

1261
00:42:23,050 --> 00:42:23,883
>> When we think

1262
00:42:23,985 --> 00:42:24,985
about the great continental

1263
00:42:25,086 --> 00:42:26,953
rifts of East African and Rio

1264
00:42:26,988 --> 00:42:28,088
Grande rift, the question

1265
00:42:28,155 --> 00:42:30,790
arises: Is the continent gonna

1266
00:42:30,858 --> 00:42:32,158
split apart here? If this

1267
00:42:32,226 --> 00:42:33,727
rifting carries on, are we gonna

1268
00:42:33,794 --> 00:42:36,529
have beachfront property right

1269
00:42:36,631 --> 00:42:38,865
here in New Mexico? And the

1270
00:42:38,899 --> 00:42:40,233
realtors are very interested in

1271
00:42:40,268 --> 00:42:42,802
this, but so are the geologists.

1272
00:42:42,870 --> 00:42:44,037
>> The formation of the Rocky

1273
00:42:44,071 --> 00:42:48,675
Mountains is a remarkable story.

1274
00:42:48,709 --> 00:42:50,510
70 million years ago. The death

1275
00:42:50,544 --> 00:42:52,078
ff ancient ammonites marked the

1276
00:42:52,179 --> 00:42:53,713
rise of the Rocky Mountains

1277
00:42:53,814 --> 00:42:57,517
from the retreating inland sea.

1278
00:42:57,618 --> 00:42:59,419
60 million years ago, leaves

1279
00:42:59,520 --> 00:43:01,087
with jagged margins grew on the

1280
00:43:01,155 --> 00:43:02,522
Mountains that were twice as

1281
00:43:02,590 --> 00:43:05,258
high as today.

1282
00:43:05,326 --> 00:43:07,527
10,000 years ago, a solitary

1283
00:43:07,628 --> 00:43:09,162
boulder marked the retreat of

1284
00:43:09,263 --> 00:43:11,064
the last glacier, that sculpted

1285
00:43:11,132 --> 00:43:12,799
the Rockies.

1286
00:43:12,900 --> 00:43:14,267
And helium gas in the Rio

1287
00:43:14,335 --> 00:43:16,503
Grande Valley today is a clue

1288
00:43:16,537 --> 00:43:17,871
that the area deep under the

1289
00:43:17,972 --> 00:43:23,343
surface is active again.

1290
00:43:23,444 --> 00:43:25,045
If rifting continues and the

1291
00:43:25,079 --> 00:43:27,047
Rio Grande Valley widens, the

1292
00:43:27,081 --> 00:43:28,581
area of the Rocky Mountains

1293
00:43:28,616 --> 00:43:31,618
could one day rip apart.

1294
00:43:31,719 --> 00:43:34,254
A new sea would move in, like

1295
00:43:34,322 --> 00:43:35,989
the vast inland sea that

1296
00:43:36,057 --> 00:43:37,957
covered the area 70 million

1297
00:43:37,992 --> 00:43:40,427
years ago.

1298
00:43:40,428 --> 00:43:42,028
The Rocky Mountains, the great

1299
00:43:42,063 --> 00:43:44,431
backbone of North America would

1300
00:43:44,498 --> 00:43:46,966
slowly disappear, and the

1301
00:43:47,034 --> 00:43:50,236
continent would once more split.

1302
00:43:50,304 --> 00:43:52,872
- Living proof that the Earth

1303
00:43:52,907 --> 00:43:54,507
is never at rest.

1304
00:43:54,508 --> 00:44:00,508
-- Sync, corrected by elderman --
-- for MY-SUBS.com ---


