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NARRATOR: Flying through space,
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a high-tech view from above
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uncovers a strange expanse
on the surface of Mars.
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CYLITA GUY: This find is potentially
huge for the future of space travel.
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- (beep)
NARRATOR: Cutting-edge technology
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looking down from space
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reveals a centuries-old legend
in Earth's oceans.
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TORRI YATES-ORR: Something
weird is definitely going on here.
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NARRATOR:
NASA probes spot a vast hexagon
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swirling around Saturn's north pole.
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DAN RISKIN: This is honestly one of
the weirdest things in the universe.
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NARRATOR: And satellites capture
a perfect doughnut-shaped lake
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carved into the landscape.
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GUY WALTERS: This is really weird.
So what happened here?
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- (boom)
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NARRATOR:
Everywhere we look on our planet,
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there's evidence of the past.
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In nature.
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In buildings.
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In relics.
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Each holds a mystery
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that technology
now allows us to see from above.
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- (dramatic music)
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NARRATOR:
What new secrets are revealed?
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- (optimistic music)
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NARRATOR: In the 21st century,
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the view from above
has reached ever greater heights...
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..uncovering mysteries
not just on Earth
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but across our solar system.
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As we search for clues on Earth
to solve these cosmic enigmas,
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technology reveals that outer space
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holds answers
to some of our own abiding secrets
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and may even hold the key
to the future of human space travel.
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- (tense music)
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NARRATOR: The Red Planet Mars
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is Earth's
most tempting neighbouring planet.
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DAN RISKIN:
Mars really does feel like
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the next frontier
in space exploration.
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TORRI YATES-ORR: Since the 1960s,
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we've sent probes and orbiters
to explore the planet from above,
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searching for clues
about its history
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and what it can reveal
about planet Earth.
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GEORGE KOUROUNIS: Today, there
are even rovers on the surface,
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and space scientists
are looking forward to the day
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humans can fly a mission to Mars.
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PETER SOROYE: To chase that dream,
scientists investigate
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the Martian surface with the images
and data captured from above
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to find places
where humans could land.
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TORRI YATES-ORR:
A landing site needs to be close
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to major areas of interest,
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including where
signs of alien life could be found
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and any resources
that could support a human mission.
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NARRATOR: And one team
of researchers examining
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a possible Martian landing site
finds something astonishing.
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- (tense music)
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DAN RISKIN: It's amazing.
I mean, you think of Mars,
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you expect this boring desert
of flat, orange nothing.
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But this is stunning.
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NARRATOR: Images
captured of the Martian surface
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reveal an unexpected bright area.
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GEORGE KOUROUNIS: This is wild
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because you just don't expect
anything on Mars to look like this!
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It's just completely
the wrong shape and colour.
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DAN RISKIN: It's not
the jagged black of volcanic rock
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and it's not the red waves
of iron-rich sand dunes.
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So what's happening on Mars
to make these light tones?
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PETER SOROYE:
And this is pretty big.
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It's around six kilometres long
and four kilometres wide.
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That's seven times bigger
than Central Park.
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NARRATOR: Millions of kilometres
further away from the sun,
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in the Kuiper Belt,
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advanced space technology
looking down from above
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may uncover a clue.
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- (intriguing music)
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TORRI YATES-ORR:
In the summer of 2015,
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the New Horizons probe
reached Pluto,
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over nine years
after it was launched from Earth.
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CYLITA GUY:
Until this major milestone,
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the best view we had of Pluto
was from the Hubble Space Telescope.
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So when the first images of
the dwarf planet finally reached us,
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the difference was staggering.
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DAN RISKIN: New Horizons captured
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a huge bright feature
on the side of the planet
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that looks like a heart.
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GEORGE KOUROUNIS:
The size of this is staggering,
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about 16-hundred kilometres across.
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That's over three times longer
than the Grand Canyon.
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NARRATOR: But what is making this
huge light-coloured shape on Pluto?
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PETER SOROYE: Pluto
is over three billion kilometres
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from the sun on average,
making it pretty chilly...
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an unbelievably frigid
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minus 232 degrees Celsius.
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CYLITA GUY:
It's so cold that nitrogen, methane
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and carbon monoxide in its thin
atmosphere can actually freeze.
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DAN RISKIN: And this deep-space ice
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collects on unique terrain.
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Most of the heart
is this massive basin
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that's filled in with a thick layer
of these weird kinds of ice.
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NARRATOR:
Could the bright area on Mars
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be a vast ice field
like Pluto's heart
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and will these secrets bring humans
closer to exploring Mars?
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DAN RISKIN: Mars's atmosphere
is more than 95% carbon dioxide.
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So would it be possible for that
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to solidify into
an ice patch on the surface?
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CYLITA GUY: Mars does sometimes
have ice and frost made of CO2,
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but it doesn't always stick around.
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ROMA AGRAWAL:
Mars isn't as cold as Pluto.
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For carbon dioxide
to stay solid as ice,
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it needs to be pretty cold...
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around negative 125 degrees Celsius.
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GEORGE KOUROUNIS:
At the poles or overnight...
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no problem.
Temperatures can drop to minus 130
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or even minus 150 Celsius
in winter at the poles.
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But when the sun hits...
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everything changes.
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PETER SOROYE: On Earth, we know
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frozen or solid carbon dioxide
as dry ice.
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And if you think about
what happens to that
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when it hits normal temperatures,
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you can start to visualise
what happens on Mars
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every time the sun
starts to warm up the surface.
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DAN RISKIN:
It's something called sublimation.
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It's when something goes
from a frozen solid to a gas
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so fast that it just skips
the liquid stage altogether.
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CYLITA GUY:
And this weird light area on Mars
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is right by the equator.
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While it can get down to below
minus 70 degrees Celsius at night,
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this isn't quite cold enough
for CO2 ice.
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DAN RISKIN: And at noon, It can get
up to a balmy 20 degrees Celsius
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at the surface.
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But even then,
because of the thin atmosphere,
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if you go up just one-and-a-half
metres above the ground,
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you're already
down to zero degrees Celsius.
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- That's far too warm for
any CO2 ice to really stick around.
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GEORGE KOUROUNIS:
So what else could be going on?
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What other clues can we find?
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NARRATOR:
A closer look at the NASA images
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suggests something surprising.
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- (intriguing music)
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TORRI YATES-ORR: This bright area on
Mars is full of geographic features
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that look shockingly familiar.
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NARRATOR:
There may be a clue closer to home
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here on Earth in Iceland.
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GEORGE KOUROUNIS: Iceland is
known as the land of fire and ice -
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and for good reason. It has some of
the world's most active volcanoes
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and some of the largest glaciers.
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NARRATOR: This is Vatnajokull,
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one of the largest ice caps
in Europe.
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DAN RISKIN: This massive
chunk of slow-flowing ice
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covers over
75-hundred square kilometres.
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CYLITA GUY: There is
more to this chilling beauty
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than meets the eye.
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Active volcanoes
are hiding under the ice.
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TORRI YATES-ORR: But
it's the glaciers that hold the clue
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to the strange bright region
on Mars...
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particularly the dramatic
Svínafellsjokull glacial tongue.
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DAN RISKIN:
If you look at the glacier tongue,
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where it hits the sea,
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you can see some cracks in the ice
that are starting to spread outward.
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And if you look at the shapes,
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they look an awful lot
like the ones on Mars.
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CYLITA GUY: There are also bands of
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earth and rock
in these really long wavy piles.
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These are called moraines -
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material
that's either been picked up
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by the sides of the glacier
or pushed together by the front.
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ROMA AGRAWAL: And they create shapes
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nearly identical
to the strange area on Mars.
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GEORGE KOUROUNIS: And this
wasn't the only icy clue in Europe.
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NARRATOR: Around 26-hundred
kilometres to the southeast
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is another stunning ice form,
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high in the Austrian Alps.
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- (tense music)
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NARRATOR:
This is the Pasterze Glacier.
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PETER SOROYE:
Climate change is chasing
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this epic glacier into the past.
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It's been receding since the 1850s.
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100 years ago,
it was over 11 kilometres long.
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Today, it's less than
eight kilometres long,
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and it's dropped in mass
by over 50%.
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- (dramatic music)
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DAN RISKIN: But for now it still
holds clues to the Martian mystery.
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NARRATOR:
Its stunning crevasse-like shapes
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reveal signs of the flow
of water and ice over the terrain.
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DAN RISKIN: Circular crevasses
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with these concentric rings
of cracks
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can happen
when there's water flowing under
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or on top of
or even within the glacier.
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These wear away at the ice,
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and then the ice gets weak spots,
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and when it gets unstable enough,
it collapses.
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- And these cracks
that look like hash marks
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are called
tic-tac-toe crevasses.
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They occur when the glacier ice
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flows on top of a higher area
in the landscape,
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which stresses it
in different directions,
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creating this unique crack pattern.
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TORRI YATES-ORR: And
when you look at them side by side,
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these look uncannily
like the fracture shapes
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on the Martian surface.
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GEORGE KOUROUNIS:
The weird shape on Mars
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has the hallmark features
of a glacier.
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NARRATOR:
Could a glacier be the secret
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to this unexpected feature
on the Martian surface?
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GEORGE KOUROUNIS: If we're able
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to find a source of water,
even if it's frozen ice,
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that would make
further explorations of Mars,
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especially by humans,
so much easier.
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It could change everything.
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DAN RISKIN:
Water could be used for everything,
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from drinking to feeding plants.
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It could even
be converted into rocket fuel.
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NARRATOR: But there's a problem.
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ROMA AGRAWAL: The satellites and
probes that look at Mars from above
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have found
signs of water ice glaciers.
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But there's a key difference.
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DAN RISKIN:
Any glaciers at the surface
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are nowhere near the equator,
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and that is because of sublimation.
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CYLITA GUY:
Water is really unstable on Mars,
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and that's because of
its thin atmosphere.
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The atmospheric pressure
is more than 100 times less
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than here on Earth.
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PETER SOROYE: Because of the
low atmospheric pressure on Mars,
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instead of liquid water
boiling at 100 degrees Celsius,
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like it does on Earth,
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it actually turns into gas
at around ten degrees Celsius.
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Basically, if it's not frozen,
it's boiling or evaporating away.
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TORRI YATES-ORR: So if
it can't be a surface water glacier,
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what's going on?
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NARRATOR: What clues can be found
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by the advanced probes
searching Mars from above?
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TORRI YATES-ORR: The Mars
Reconnaissance Orbiter, or MRO,
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has been flying high above
the Red Planet for over 17 years.
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Packed with high-tech equipment,
it offers a crucial clue.
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ROMA AGRAWAL: When the researchers
looked at the data from the MRO,
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they found that the light area
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was actually a kind of salt.
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- (dramatic music)
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NARRATOR:
But how did this salt appear?
241
00:10:53,280 --> 00:10:54,960
- And how can salt on Mars
242
00:10:55,120 --> 00:10:57,600
make shapes just like those
we see in glaciers here on Earth?
243
00:10:57,760 --> 00:10:59,520
NARRATOR: A mystery whose answer
244
00:10:59,680 --> 00:11:02,640
may still hold the key
to human missions to Mars.
245
00:11:03,840 --> 00:11:05,920
- (dramatic music)
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00:11:06,080 --> 00:11:07,760
- There's a clue on Earth
that provides
247
00:11:07,920 --> 00:11:09,760
the final piece of the puzzle.
248
00:11:09,920 --> 00:11:11,600
- (intriguing music)
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00:11:11,760 --> 00:11:13,960
NARRATOR: Hiding
only a few decades in the past,
250
00:11:14,120 --> 00:11:17,080
in the bright red waters
of Bolivia's Laguna Colorada
251
00:11:17,240 --> 00:11:18,920
is a staggering secret.
252
00:11:19,080 --> 00:11:21,600
GEORGE KOUROUNIS:
The lakes of this region,
253
00:11:21,760 --> 00:11:24,320
in the high plateau
known as the Altiplano,
254
00:11:24,480 --> 00:11:26,280
are extremely salt and form
255
00:11:26,440 --> 00:11:29,200
large and dramatic salt islands
in the brilliant waters.
256
00:11:29,360 --> 00:11:31,320
ROMA AGRAWAL: But in the 1980s
257
00:11:31,480 --> 00:11:33,480
scientists discovered
something incredible
258
00:11:33,640 --> 00:11:36,280
hiding in these salty shells.
259
00:11:36,440 --> 00:11:38,480
Ancient ice.
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00:11:38,640 --> 00:11:42,080
CYLITA GUY: The researchers
believed that this ice was formed
261
00:11:42,240 --> 00:11:44,960
during the Little Ice Age,
which started in the Middle Ages.
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00:11:45,120 --> 00:11:49,320
DAN RISKIN: This thick layer of salt
insulated this ice against melting,
263
00:11:49,480 --> 00:11:52,560
so it could stick around for decades
or even centuries, even though
264
00:11:52,720 --> 00:11:54,480
in the bright sunlight
the summer temperatures
265
00:11:54,640 --> 00:11:56,320
get to, like, 16 degrees Celsius.
266
00:11:56,480 --> 00:11:59,040
PETER SOROYE: And
these aren't just little ice cubes.
267
00:11:59,200 --> 00:12:03,440
These ice-cored salt islands were
as large as 1.5 kilometres across
268
00:12:03,600 --> 00:12:06,200
and seven metres high.
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00:12:06,360 --> 00:12:08,640
TORRI YATES-ORR: It's unknown
if the ice persists to this day,
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00:12:08,800 --> 00:12:10,480
but the hidden ice implies
271
00:12:10,640 --> 00:12:13,000
something staggering
about the shape on Mars.
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00:12:14,200 --> 00:12:17,040
NARRATOR: Could the salt
and the glacial-looking terrain
273
00:12:17,200 --> 00:12:21,520
at this strange bright area on Mars
be a sign of ice hiding below?
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00:12:21,680 --> 00:12:24,880
DAN RISKIN: Experts believe
there is a way this could happen.
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00:12:25,040 --> 00:12:28,520
First, a long time ago,
a Martian volcano could have erupted
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00:12:28,680 --> 00:12:31,440
right next to a water ice glacier.
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00:12:32,480 --> 00:12:34,960
GEORGE KOUROUNIS: The hot ash
would have instantly melted
278
00:12:35,120 --> 00:12:38,200
the top of the ice,
and - as it evaporated away -
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00:12:38,360 --> 00:12:41,720
it would have left a layer of salt
behind, hidden by the dark ash.
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00:12:42,840 --> 00:12:45,760
CYLITA GUY: Eventually, Martian
winds would have blown the ash away,
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00:12:45,920 --> 00:12:47,920
leaving behind
the bright salt layer,
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00:12:48,080 --> 00:12:50,360
which would hold
the shape of the glacier beneath.
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00:12:50,520 --> 00:12:53,640
GEORGE KOUROUNIS: Even though
this isn't 100% confirmation,
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00:12:53,800 --> 00:12:57,280
it's really important because,
if it is there on the surface,
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00:12:57,440 --> 00:12:59,240
that changes everything.
286
00:13:01,800 --> 00:13:03,480
- (tense music)
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00:13:03,640 --> 00:13:05,960
ROMA AGRAWAL: Glaciers
have been found on Mars before,
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00:13:06,120 --> 00:13:10,160
but in the unfriendly and extreme
environments at the Martian poles,
289
00:13:10,320 --> 00:13:12,640
where the icy temperatures
and long winter nights
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00:13:12,800 --> 00:13:15,960
would wreak havoc
on humans and electronics alike.
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00:13:16,120 --> 00:13:18,680
PETER SOROYE:
And at such cold temperatures,
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00:13:18,840 --> 00:13:20,840
simply turning that ice
into liquid water
293
00:13:21,000 --> 00:13:22,720
could be a near-impossible task.
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00:13:22,880 --> 00:13:26,800
CYLITA GUY: But this glacier
is at the much more accessible
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00:13:26,960 --> 00:13:28,960
warm and sunny equator.
296
00:13:29,120 --> 00:13:31,640
And digging through a crust of salt
is going to be far easier
297
00:13:31,800 --> 00:13:35,920
than trying to break up polar ice in
negative 50-degree Celsius weather.
298
00:13:36,760 --> 00:13:39,760
GEORGE KOUROUNIS: If there really is
ice hiding under this salt,
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00:13:39,920 --> 00:13:41,640
it'll be a total game changer.
300
00:13:41,800 --> 00:13:43,520
- (tense music)
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00:13:43,680 --> 00:13:46,960
NARRATOR: This shocking discovery
on Mars is just the beginning.
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00:13:47,120 --> 00:13:48,920
CYLITA GUY: This find is potentially
303
00:13:49,080 --> 00:13:51,000
huge for the future of space travel.
304
00:13:51,160 --> 00:13:54,640
The possibility
of accessible frozen water
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00:13:54,800 --> 00:13:57,520
makes the logistics of a mission
to the Red Planet a little simpler.
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00:13:57,680 --> 00:13:59,600
Mind you, not simple,
307
00:13:59,760 --> 00:14:02,280
but just a little bit easier.
308
00:14:02,440 --> 00:14:05,080
GEORGE KOUROUNIS: What we're seeing
here in this view from above,
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00:14:05,240 --> 00:14:07,000
even though it's on another planet,
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00:14:07,160 --> 00:14:09,840
could change
the direction of human history.
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00:14:15,240 --> 00:14:17,560
NARRATOR: Advanced
satellite technology in space,
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00:14:17,720 --> 00:14:19,400
looking down from above,
313
00:14:19,560 --> 00:14:22,040
captures planet Earth
like never before.
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00:14:22,200 --> 00:14:23,880
- (dramatic music)
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00:14:24,040 --> 00:14:26,840
DAN RISKIN: The US has all kinds
of cutting-edge equipment in space,
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00:14:27,000 --> 00:14:29,240
and a couple of satellites
have something called
317
00:14:29,400 --> 00:14:34,760
the Visible Infrared Imaging
Radiometer Suite, or VIIRS.
318
00:14:34,920 --> 00:14:36,920
CYLITA GUY: It's amazing.
319
00:14:37,080 --> 00:14:39,640
Sensors collect
visible and infrared images,
320
00:14:39,800 --> 00:14:42,600
which can be used to do everything
from predicting the weather
321
00:14:42,760 --> 00:14:46,440
to tracking fires and even
sensing changes in the ocean colour.
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00:14:47,320 --> 00:14:49,320
ROMA AGRAWAL: And crucially,
it has something called
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00:14:49,480 --> 00:14:51,520
the Day Night Band Sensor,
324
00:14:51,680 --> 00:14:53,760
which can see
in very low light conditions
325
00:14:53,920 --> 00:14:57,560
to capture things at night that
we can't see with the naked eye.
326
00:14:58,920 --> 00:15:01,360
NARRATOR:
And this new view from above
327
00:15:01,520 --> 00:15:04,240
captures a long-hidden secret
in the nighttime darkness
328
00:15:04,400 --> 00:15:06,280
of Earth's oceans.
329
00:15:06,440 --> 00:15:09,560
In the summer of 2019,
off the coast of Java,
330
00:15:09,720 --> 00:15:12,280
this technology
reveals an eerie shape
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00:15:12,440 --> 00:15:14,800
emerging
from the black ocean waters.
332
00:15:14,960 --> 00:15:17,320
- (tense music)
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00:15:17,480 --> 00:15:20,120
TORRI YATES-ORR: Something weird
is definitely going on here.
334
00:15:20,280 --> 00:15:22,080
PETER SOROYE:
From the satellite, it looks
335
00:15:22,240 --> 00:15:24,880
so otherworldly and ethereal.
336
00:15:25,040 --> 00:15:27,680
CYLITA GUY: This looks like
an abstract work of art.
337
00:15:27,840 --> 00:15:30,240
I see this glowing cloud
floating in the black.
338
00:15:31,240 --> 00:15:34,000
DAN RISKIN: It's paler than the
city lights on the island of Java,
339
00:15:34,160 --> 00:15:36,920
but it's definitely brighter
than the nighttime ocean should be.
340
00:15:37,080 --> 00:15:39,800
GEORGE KOUROUNIS: It's hard to tell
exactly what's going on here,
341
00:15:39,960 --> 00:15:41,400
but it's huge.
342
00:15:42,680 --> 00:15:44,760
CYLITA GUY:
This shape covers a massive area,
343
00:15:44,920 --> 00:15:47,080
100,000 square kilometres.
344
00:15:47,240 --> 00:15:48,960
That's like the size of Iceland.
345
00:15:49,120 --> 00:15:50,440
- (eerie music)
346
00:15:50,600 --> 00:15:52,440
NARRATOR: This strange vast shape
347
00:15:52,600 --> 00:15:55,840
moves over time
and raises countless questions.
348
00:15:56,000 --> 00:15:58,080
TORRI YATES-ORR: What is causing
349
00:15:58,240 --> 00:16:00,040
this enormous
glow-in-the-dark spectre?
350
00:16:00,840 --> 00:16:03,280
PETER SOROYE: Is this some kind
of weird natural phenomenon
351
00:16:03,440 --> 00:16:05,120
or is it caused by humans?
352
00:16:05,280 --> 00:16:07,240
CYLITA GUY:
How long has it been here?
353
00:16:07,400 --> 00:16:09,640
DAN RISKIN: Is there
any other technology in space
354
00:16:09,800 --> 00:16:12,400
that could offer a hint
as to what we're seeing here?
355
00:16:12,560 --> 00:16:15,440
NARRATOR: Over
8,000 kilometres to the northeast,
356
00:16:15,600 --> 00:16:17,400
off the coast of Siberia,
357
00:16:17,560 --> 00:16:19,240
satellites looking down from space
358
00:16:19,400 --> 00:16:21,160
capture a possible clue...
359
00:16:21,320 --> 00:16:23,080
in the Sea of Okhotsk.
360
00:16:23,240 --> 00:16:27,120
Familiar-looking shapes
swirling in the water.
361
00:16:27,280 --> 00:16:29,000
- (tense music)
362
00:16:29,160 --> 00:16:31,160
CYLITA GUY:
In 2023, NASA captured this,
363
00:16:31,320 --> 00:16:33,000
as thinning ice breaks up
364
00:16:33,160 --> 00:16:35,000
and starts to flow
with the spinning ocean currents.
365
00:16:36,440 --> 00:16:38,320
DAN RISKIN: As sea ice melts,
366
00:16:38,480 --> 00:16:41,080
swirls of white
spin off into the ocean.
367
00:16:41,240 --> 00:16:43,240
Here it covers
hundreds of kilometres.
368
00:16:43,400 --> 00:16:45,400
PETER SOROYE:
These happen here every year,
369
00:16:45,560 --> 00:16:47,360
and sometimes last for months.
370
00:16:47,520 --> 00:16:49,480
It's even appearing
earlier and earlier
371
00:16:49,640 --> 00:16:51,880
as sea ice breaks up sooner,
thanks to climate change.
372
00:16:53,560 --> 00:16:56,240
- This swirling ice,
seen from space,
373
00:16:56,400 --> 00:16:59,400
looks a lot like the shape we see
in the images from around Java.
374
00:17:00,400 --> 00:17:02,880
CYLITA GUY: Does that mean
that forming or melting sea ice
375
00:17:03,040 --> 00:17:05,680
could be behind the mysterious
swirl in the Indian Ocean?
376
00:17:07,080 --> 00:17:09,480
NARRATOR:
Further investigation from above
377
00:17:09,640 --> 00:17:11,320
uncovers some shocking clues.
378
00:17:12,560 --> 00:17:15,600
This isn't the only place this
strange phenomenon appears.
379
00:17:16,680 --> 00:17:20,000
ROMA AGRAWAL: The VIIRS equipment
finds several more instances
380
00:17:20,160 --> 00:17:22,560
of these strange
glowing patches of sea.
381
00:17:23,560 --> 00:17:25,600
NARRATION:
These weird phenomena are spotted
382
00:17:25,760 --> 00:17:27,440
off the coast of East Africa
383
00:17:27,600 --> 00:17:29,520
and in the waters
of Southeast Asia.
384
00:17:29,680 --> 00:17:32,400
DAN RISKIN: And there's something
all of those sites have in common.
385
00:17:32,560 --> 00:17:36,000
They're all
in warm tropical waters.
386
00:17:36,160 --> 00:17:38,080
PETER SOROYE:
That means there's no way
387
00:17:38,240 --> 00:17:41,200
these could be caused
by melting or forming sea ice.
388
00:17:41,360 --> 00:17:45,000
So what else could cause huge
areas of the ocean to get so bright?
389
00:17:46,000 --> 00:17:48,520
NARRATOR: Perhaps
a record-breaking event in Spain
390
00:17:48,680 --> 00:17:50,680
can reveal a clue.
391
00:17:50,840 --> 00:17:52,840
In January of 2020,
392
00:17:53,000 --> 00:17:56,600
the Mediterranean
is hit by a major storm.
393
00:17:56,760 --> 00:17:58,760
- Winter storm Gloria batters Spain
394
00:17:58,920 --> 00:18:01,000
with unparalleled heavy rain,
395
00:18:01,160 --> 00:18:03,120
high winds and blizzards.
396
00:18:03,280 --> 00:18:05,920
NARRATOR: And the quiet
seaside town of Tossa de Mar
397
00:18:06,080 --> 00:18:08,520
faces something staggering.
398
00:18:08,680 --> 00:18:11,440
DAN RISKIN: Storms can cause
something called a storm surge,
399
00:18:11,600 --> 00:18:13,840
where the sea level
rises up higher than normal
400
00:18:14,000 --> 00:18:16,080
and then floods coastal areas.
401
00:18:16,240 --> 00:18:19,320
CYLITA GUY: And Gloria's storm surge
poured more than just water
402
00:18:19,480 --> 00:18:21,480
into the streets of Tossa de Mar.
403
00:18:21,640 --> 00:18:25,280
The town suddenly flooded
with a staggering amount of foam.
404
00:18:25,440 --> 00:18:27,880
- (wind whistles)
PETER SOROYE: Sea foam occurs
405
00:18:28,040 --> 00:18:30,200
all the time,
and all around the globe.
406
00:18:30,360 --> 00:18:33,120
It's made when
the agitation of wind and waves
407
00:18:33,280 --> 00:18:37,000
stirs up the organic material,
pollutants, surfactants
408
00:18:37,160 --> 00:18:40,400
and general bits and bobs
that are found in seawater.
409
00:18:41,280 --> 00:18:43,440
DAN RISKIN: To get sea foam
in these large quantities,
410
00:18:43,600 --> 00:18:45,840
there has to be
a lot of dissolved organic material,
411
00:18:46,000 --> 00:18:48,600
like a big algal bloom,
getting broken down.
412
00:18:48,760 --> 00:18:51,240
And you have to pair that
with choppy ocean waters,
413
00:18:51,400 --> 00:18:53,840
like a big cyclonic storm.
414
00:18:54,000 --> 00:18:56,600
NARRATOR:
Could the churning ocean waves
415
00:18:56,760 --> 00:19:00,520
make a giant island of sea foam
visible from space
416
00:19:00,680 --> 00:19:03,760
or is there something else
hiding in the ocean depths?
417
00:19:03,920 --> 00:19:05,600
TORRI YATES-ORR:
Maybe it's not a sign
418
00:19:05,760 --> 00:19:07,680
of organic material breaking down.
419
00:19:07,840 --> 00:19:10,560
Maybe there's
something alive down there.
420
00:19:10,720 --> 00:19:12,720
- (tense music)
421
00:19:14,640 --> 00:19:16,360
NARRATOR: There may be a clue
422
00:19:16,520 --> 00:19:18,200
in an old maritime legend.
423
00:19:19,200 --> 00:19:22,480
TORRI YATES-ORR: Over centuries,
there have been reports from sailors
424
00:19:22,640 --> 00:19:24,400
of a very weird phenomenon...
425
00:19:24,560 --> 00:19:26,680
something they called "milky seas".
426
00:19:26,840 --> 00:19:28,840
GEORGE KOUROUNIS:
Researchers poring over
427
00:19:29,000 --> 00:19:33,640
ships logs and other historical
records found over 200 reports
428
00:19:33,800 --> 00:19:35,480
of vast stretches of ocean
429
00:19:35,640 --> 00:19:38,000
emitting
a starling white or green glow.
430
00:19:39,200 --> 00:19:41,640
- When those are mapped
alongside the 12 instances
431
00:19:41,800 --> 00:19:43,800
captured by modern satellites,
432
00:19:43,960 --> 00:19:46,160
you can see that
it continues a pattern.
433
00:19:46,320 --> 00:19:50,160
CYLITA GUY: These rare glowing
ocean waters are most often found
434
00:19:50,320 --> 00:19:52,920
in the Arabian Sea
and Indian Ocean.
435
00:19:53,840 --> 00:19:56,120
TORRI YATES-ORR: So are
these ocean hazes seen on satellite
436
00:19:56,280 --> 00:19:58,600
the milky seas of maritime legend
437
00:19:58,760 --> 00:20:00,440
and are there any contemporary
438
00:20:00,600 --> 00:20:02,520
on-the-ground sightings
that could back this up?
439
00:20:02,680 --> 00:20:04,400
- (tense music)
440
00:20:04,560 --> 00:20:07,080
NARRATOR:
In an unbelievable moment of luck,
441
00:20:07,240 --> 00:20:09,760
the vessel Ganesha
happened to pass through
442
00:20:09,920 --> 00:20:12,960
the tail of ocean haze
captured by satellite.
443
00:20:13,920 --> 00:20:17,200
And what they record from
the ocean surface is astonishing.
444
00:20:18,880 --> 00:20:21,520
- The crew described
a vast and steady glow
445
00:20:21,680 --> 00:20:23,800
coming from beneath
the ocean surface.
446
00:20:23,960 --> 00:20:25,960
GEORGE KOUROUNIS:
Even more amazing...
447
00:20:26,120 --> 00:20:27,920
they catch it on camera.
448
00:20:28,080 --> 00:20:30,480
And that gives another huge clue
to what's happening.
449
00:20:31,480 --> 00:20:34,600
CYLITA GUY: The crew see the ocean
glow as a pale white or green
450
00:20:34,760 --> 00:20:36,480
because their perception
of colour is affected
451
00:20:36,640 --> 00:20:38,200
by the dark and moonless night.
452
00:20:38,360 --> 00:20:42,760
The human eye contains two types
of receptor cells - rods and cones.
453
00:20:42,920 --> 00:20:44,600
Cones help us to see colour,
454
00:20:44,760 --> 00:20:48,240
while rods work in low light
to help us see in grayscale.
455
00:20:48,400 --> 00:20:50,440
Cone cells need
lots and lots of light to work,
456
00:20:50,600 --> 00:20:52,720
which is why
colour vision decreases at night
457
00:20:52,880 --> 00:20:54,560
or in other dark conditions.
458
00:20:54,720 --> 00:20:56,520
DAN RISKIN:
But the cameras on the ship
459
00:20:56,680 --> 00:20:58,680
aren't affected
the same way human eyes are.
460
00:20:58,840 --> 00:21:00,840
So they capture the truth.
461
00:21:01,000 --> 00:21:03,520
A glowing, greenish-blue haze
462
00:21:03,680 --> 00:21:05,960
that spreads out for miles.
463
00:21:06,120 --> 00:21:09,760
NARRATOR: It's a critical revelation
and raises the question...
464
00:21:09,920 --> 00:21:13,320
what on Earth can make the ocean
glow from below?
465
00:21:14,200 --> 00:21:17,080
GEORGE KOUROUNIS: There are
some other glowing ocean phenomena
466
00:21:17,240 --> 00:21:18,920
that can give us a clue.
467
00:21:19,080 --> 00:21:20,760
PETER SOROYE:
There are parts of the world
468
00:21:20,920 --> 00:21:22,560
where the impact
of the waves on the shore
469
00:21:22,720 --> 00:21:24,920
can make a magical blue sparkle.
470
00:21:25,080 --> 00:21:27,800
Even the motion of fish or dolphins
swimming in the water
471
00:21:27,960 --> 00:21:30,400
can create the same kind of glow.
472
00:21:30,560 --> 00:21:33,320
- These stunning phenomena
are caused by a type of plankton.
473
00:21:33,480 --> 00:21:36,400
Tiny living things are producing
light with their bodies
474
00:21:36,560 --> 00:21:38,360
through chemical reaction.
475
00:21:38,520 --> 00:21:40,760
They give off light
when they're moved around.
476
00:21:40,920 --> 00:21:44,000
DAN RISKIN: But these creatures
only emit little flashes of light,
477
00:21:44,160 --> 00:21:45,960
so it looks like it sparkles.
478
00:21:46,120 --> 00:21:48,120
That's not what we're seeing
off the island of Java.
479
00:21:48,280 --> 00:21:51,040
So could it be
another form of hidden life
480
00:21:51,200 --> 00:21:53,200
that's making the sea glow?
481
00:21:54,520 --> 00:21:57,520
NARRATOR:
There may be a clue in Northern Iran
482
00:21:57,680 --> 00:21:59,480
where the salty Lake Urmia
483
00:21:59,640 --> 00:22:01,720
makes a statement
visible from space.
484
00:22:01,880 --> 00:22:03,880
PETER SOROYE:
In these satellite images,
485
00:22:04,040 --> 00:22:06,960
you can see that this lake
actually changes colour.
486
00:22:07,120 --> 00:22:08,840
There is nothing subtle about it.
487
00:22:09,000 --> 00:22:11,680
CYLITA GUY: Scientists believe
this stunning colour shift
488
00:22:11,840 --> 00:22:14,120
is caused by
microscopic organisms...
489
00:22:14,280 --> 00:22:16,760
either algae or bacteria.
490
00:22:16,920 --> 00:22:18,880
In very bright and salty conditions,
491
00:22:19,040 --> 00:22:21,560
the algae, Dunaliella salina,
492
00:22:21,720 --> 00:22:25,800
turns from green to red as it
makes these protective chemicals.
493
00:22:25,960 --> 00:22:29,280
DAN RISKIN:
The bacteria, Halobacteriaceae,
494
00:22:29,440 --> 00:22:33,160
actually produce a red pigment
that converts light into energy.
495
00:22:33,320 --> 00:22:35,280
So when they appear
in large enough numbers,
496
00:22:35,440 --> 00:22:37,520
they make the water look red.
497
00:22:38,680 --> 00:22:41,400
PETER SOROYE: Lake Urmia shows us
that there are microscopic creatures
498
00:22:41,560 --> 00:22:44,880
that can change the colour of water
for extended periods.
499
00:22:45,040 --> 00:22:46,720
So could invisible bacteria
500
00:22:46,880 --> 00:22:49,080
be behind
the glowing milky seas as well?
501
00:22:50,080 --> 00:22:51,920
CYLITA GUY:
The latest research suggests
502
00:22:52,080 --> 00:22:55,840
that a bioluminescent bacteria
known as Vibrio harveyi could be
503
00:22:56,000 --> 00:22:58,680
the secret ingredient
behind these milky seas.
504
00:22:59,560 --> 00:23:02,280
DAN RISKIN: The bacteria can thrive
under certain rare conditions,
505
00:23:02,440 --> 00:23:04,200
and when they grow to huge numbers,
506
00:23:04,360 --> 00:23:06,800
they collectively begin to glow.
507
00:23:07,680 --> 00:23:09,960
PETER SOROYE:
Glowing is an adaptation that
508
00:23:10,120 --> 00:23:11,800
in other ocean creatures
can be anything from
509
00:23:11,960 --> 00:23:16,800
a lure for food to a warning to
a means of burning off UV radiation.
510
00:23:16,960 --> 00:23:19,640
NARRATOR: But what's
driving these glowing bacteria
511
00:23:19,800 --> 00:23:21,560
is still a mystery.
512
00:23:21,720 --> 00:23:23,480
CYLITA GUY:
Milky seas are rare enough
513
00:23:23,640 --> 00:23:25,880
that spotting them
and getting to them quickly enough
514
00:23:26,040 --> 00:23:28,680
to test the waters for bacteria
is tricky.
515
00:23:28,840 --> 00:23:30,320
So we won't know for sure
516
00:23:30,480 --> 00:23:32,160
if Vibrio harveyi is the culprit
517
00:23:32,320 --> 00:23:34,000
until more research is done.
518
00:23:34,160 --> 00:23:36,080
NARRATOR: And this maritime legend
519
00:23:36,240 --> 00:23:39,200
may hold hints
of something even more staggering.
520
00:23:39,360 --> 00:23:41,960
TORRI YATES-ORR:
Glowing bacteria may hold a clue
521
00:23:42,120 --> 00:23:44,680
not simply
to Earth's milky seas mysteries
522
00:23:44,840 --> 00:23:47,080
but to life on other planets.
523
00:23:47,240 --> 00:23:49,120
DAN RISKIN:
A lot of people think that
524
00:23:49,280 --> 00:23:50,960
since bioluminescence
works so well
525
00:23:51,120 --> 00:23:53,640
and it's evolved
so many times independently,
526
00:23:53,800 --> 00:23:56,120
it's one of the key things
we should be looking for
527
00:23:56,280 --> 00:23:58,440
when we look
for life on other worlds.
528
00:23:58,600 --> 00:24:02,240
GEORGE KOUROUNIS: With tools like
VIIRS pointed toward outer space,
529
00:24:02,400 --> 00:24:05,920
could we uncover
a milky sea on another planet?
530
00:24:06,080 --> 00:24:09,280
Only time will tell,
but it's a tantalising possibility.
531
00:24:09,440 --> 00:24:11,440
- (dramatic music)
532
00:24:15,120 --> 00:24:17,120
LAUNCH ANNOUNCER: Three, two...
533
00:24:17,280 --> 00:24:19,880
NARRATOR:
In 1997, the Cassini Orbiter
534
00:24:20,040 --> 00:24:22,680
launches into the skies...
- (boom)
535
00:24:22,840 --> 00:24:27,720
..beginning a 3.4-billion-kilometre
journey through space.
536
00:24:27,880 --> 00:24:30,360
- (electronic hiss)
GEORGE KOUROUNIS: Its mission?
537
00:24:30,520 --> 00:24:32,800
An in-depth examination of Saturn...
538
00:24:32,960 --> 00:24:35,040
from above.
539
00:24:35,200 --> 00:24:37,880
DAN RISKIN: As Cassini
comes down over the north pole,
540
00:24:38,040 --> 00:24:40,560
it sees something truly incredible.
541
00:24:41,800 --> 00:24:43,800
CYLITA GUY: This is amazing.
542
00:24:43,960 --> 00:24:46,240
There's what looks like
a perfect hexagon
543
00:24:46,400 --> 00:24:48,400
right at the top of the planet.
544
00:24:48,560 --> 00:24:51,400
DAN RISKIN: This is honestly one of
the weirdest things in the universe.
545
00:24:51,560 --> 00:24:55,960
GEORGE KOUROUNIS: It seems too
geometrically perfect to be real.
546
00:24:56,120 --> 00:24:58,600
And this thing
is unbelievably massive.
547
00:24:58,760 --> 00:25:02,760
Each side is 13,800 kilometres long,
548
00:25:02,920 --> 00:25:06,000
and it's almost
25,000 kilometres across.
549
00:25:06,960 --> 00:25:08,920
- You could fit
almost four Earths in there.
550
00:25:09,080 --> 00:25:10,920
GEORGE KOUROUNIS:
How is it possible to have
551
00:25:11,080 --> 00:25:13,280
what looks to be
a near perfect hexagon
552
00:25:13,440 --> 00:25:15,480
at the north pole of Saturn?
553
00:25:15,640 --> 00:25:17,720
TORRI YATES-ORR:
I mean, what is going on here?
554
00:25:17,880 --> 00:25:20,320
What is this thing made of?
555
00:25:20,480 --> 00:25:22,160
- Why is it there?
556
00:25:22,320 --> 00:25:24,560
GEORGE KOUROUNIS:
Saturn is over a billion kilometres
557
00:25:24,720 --> 00:25:29,720
away from Earth. So how can we
investigate such a distant mystery?
558
00:25:29,880 --> 00:25:32,760
DAN RISKIN: When it comes
to solving mysteries like this,
559
00:25:32,920 --> 00:25:35,320
sometimes you have
to start a little closer to home.
560
00:25:35,480 --> 00:25:37,760
NARRATOR: Could clues
to this strange phenomenon
561
00:25:37,920 --> 00:25:39,600
be found on Earth?
562
00:25:39,760 --> 00:25:41,880
CYLITA GUY:
It seems odd to think about,
563
00:25:42,040 --> 00:25:44,400
but there are actually
naturally occurring hexagons
564
00:25:44,560 --> 00:25:46,360
all over our planet.
565
00:25:46,520 --> 00:25:48,520
PETER SOROYE:
From beehives to snowflakes,
566
00:25:48,680 --> 00:25:53,560
ancient rock formations to the
pinpoint-lenses of dragonfly eyes.
567
00:25:53,720 --> 00:25:56,480
- But why does nature love
this shape so much?
568
00:25:57,640 --> 00:25:59,640
NARRATOR:
Perhaps a clue can be found
569
00:25:59,800 --> 00:26:02,440
in the heights
of Bolivia's Altiplano,
570
00:26:02,600 --> 00:26:06,120
where a vast plain of white
can be seen from space.
571
00:26:06,280 --> 00:26:08,280
- This is the Salar de Uyuni.
572
00:26:08,440 --> 00:26:10,680
It covers
over 10,000 square kilometres,
573
00:26:10,840 --> 00:26:13,000
making it
the largest salt flat in the world.
574
00:26:13,160 --> 00:26:16,000
It's about the same size
as the Big Island of Hawaii.
575
00:26:16,160 --> 00:26:18,160
NARRATOR: And viewed from above,
576
00:26:18,320 --> 00:26:22,520
stunning patterns in these ancient
salts form a familiar shape.
577
00:26:22,680 --> 00:26:25,880
CYLITA GUY: There are hexagonal
formations all across the surface,
578
00:26:26,040 --> 00:26:28,080
around one or two metres across.
579
00:26:28,240 --> 00:26:31,480
TORRI YATES-ORR: But what drives
the salt into the hexagon shapes?
580
00:26:31,640 --> 00:26:34,400
PETER SOROYE:
For years, scientists believed
581
00:26:34,560 --> 00:26:36,440
that the salt
was forming hexagonal ridges
582
00:26:36,600 --> 00:26:39,480
from cracking under
the pressure of contracting.
583
00:26:40,480 --> 00:26:43,360
ROMA AGRAWAL: This is something
that can happen in cooling lava,
584
00:26:43,520 --> 00:26:46,120
and we can see the results
in impressive rock formations
585
00:26:46,280 --> 00:26:48,440
like the Devils Tower in Wyoming
586
00:26:48,600 --> 00:26:50,720
and the Giant's Causeway in Ireland.
587
00:26:50,880 --> 00:26:53,200
CYLITA GUY:
These kinds of shapes form because,
588
00:26:53,360 --> 00:26:55,400
as the lava cools, it contracts.
589
00:26:55,560 --> 00:26:58,080
These contractions
stress the cooling rock,
590
00:26:58,240 --> 00:27:01,240
which cracks,
forming these very efficient shapes.
591
00:27:01,400 --> 00:27:05,280
DAN RISKIN: And that just happens
to be at 120-degree angles,
592
00:27:05,440 --> 00:27:07,560
and those are the angles
that make a hexagon.
593
00:27:07,720 --> 00:27:09,400
- (dramatic music)
594
00:27:09,560 --> 00:27:11,360
PETER SOROYE:
The latest research reveals
595
00:27:11,520 --> 00:27:13,720
the secret behind
the salt flat hexagons
596
00:27:13,880 --> 00:27:16,640
is actually
in the movement of water.
597
00:27:16,800 --> 00:27:19,320
DAN RISKIN:
What's happening at the salt flats
598
00:27:19,480 --> 00:27:22,600
is really happening
in the water underneath the crust
599
00:27:22,760 --> 00:27:24,320
in a phenomenon called convection.
600
00:27:24,480 --> 00:27:27,280
PETER SOROYE: Technically,
convection is just the transfer
601
00:27:27,440 --> 00:27:29,840
of heat across a space
by the movement of a fluid.
602
00:27:30,000 --> 00:27:32,800
CYLITA GUY: The warmer,
less dense parts will rise,
603
00:27:32,960 --> 00:27:36,000
while the cooler, more dense
material will sink down.
604
00:27:36,160 --> 00:27:37,840
NARRATOR: At the surface,
605
00:27:38,000 --> 00:27:40,800
water evaporates
leaving behind ridges of salt
606
00:27:40,960 --> 00:27:45,000
that mirror the patterns of movement
hidden under the surface.
607
00:27:45,160 --> 00:27:47,920
ROMA AGRAWAL: This movement
tends to form polygonal shapes -
608
00:27:48,080 --> 00:27:50,080
and in perfect conditions,
609
00:27:50,240 --> 00:27:52,240
where there's nothing
to interrupt the flow,
610
00:27:52,400 --> 00:27:55,360
convection
loves to make hexagonal patterns.
611
00:27:55,520 --> 00:27:59,840
DAN RISKIN: So, could the same
forces that make hexagons on Earth
612
00:28:00,000 --> 00:28:02,920
be what's happening on Saturn?
613
00:28:03,080 --> 00:28:05,840
CYLITA GUY: But Saturn's skies
aren't made of water.
614
00:28:06,000 --> 00:28:09,720
DAN RISKIN: There isn't even
land on Saturn. It's a gas giant.
615
00:28:09,880 --> 00:28:12,400
CYLITA GUY:
Gas giants are huge planets
616
00:28:12,560 --> 00:28:15,640
made mainly of gases
like helium and hydrogen,
617
00:28:15,800 --> 00:28:18,520
which surround
a comparatively smaller solid core.
618
00:28:18,680 --> 00:28:20,600
TORRI YATES-ORR:
So you've got to wonder
619
00:28:20,760 --> 00:28:22,440
if the same kind
of motion in water on Earth
620
00:28:22,600 --> 00:28:24,280
can happen in gas...
621
00:28:24,440 --> 00:28:26,480
on a much larger scale.
622
00:28:26,640 --> 00:28:29,000
NARRATOR: Perhaps
images from the Cassini Orbiter
623
00:28:29,160 --> 00:28:31,160
can provide a clue.
624
00:28:31,320 --> 00:28:33,680
To the naked eye, Saturn's hexagon
625
00:28:33,840 --> 00:28:35,840
appears pale yellow and blue.
626
00:28:36,000 --> 00:28:38,360
But the bright shades
of the false colour images
627
00:28:38,520 --> 00:28:40,520
taken right above the pole
628
00:28:40,680 --> 00:28:43,920
uncovers depth and details
inside this vast alien shape.
629
00:28:44,080 --> 00:28:45,760
DAN RISKIN: Those different colours
630
00:28:45,920 --> 00:28:48,080
indicate
how deep you are in the hexagon.
631
00:28:48,240 --> 00:28:50,120
The redder colours are lower down,
632
00:28:50,280 --> 00:28:51,960
the blue is higher up.
633
00:28:52,120 --> 00:28:54,160
PETER SOROYE: So we can see
that this isn't just right
634
00:28:54,320 --> 00:28:57,280
at the very top of the atmosphere.
This has some real depth to it.
635
00:28:57,440 --> 00:29:01,120
DAN RISKIN: And crucially, looking
straight down from above like this,
636
00:29:01,280 --> 00:29:04,440
Cassini also shows you
that the hexagon is rotating.
637
00:29:04,600 --> 00:29:07,320
TORRI YATES-ORR: So
how can a perfect shape like this
638
00:29:07,480 --> 00:29:10,000
hold together
in the swirling gaseous atmosphere?
639
00:29:10,160 --> 00:29:13,720
NARRATOR: There may be a clue
hidden in Earth's skies.
640
00:29:13,880 --> 00:29:16,920
DAN RISKIN: Just like in the water
underneath the salt flats,
641
00:29:17,080 --> 00:29:19,400
convection
also happens in the atmosphere.
642
00:29:19,560 --> 00:29:21,560
NARRATOR: Convection is behind
643
00:29:21,720 --> 00:29:24,160
the creation
of clouds and thunderstorms.
644
00:29:24,320 --> 00:29:25,800
- (thunder cracks)
645
00:29:25,960 --> 00:29:28,040
- And it's the key driver
of one of the most powerful
646
00:29:28,200 --> 00:29:30,000
phenomena on Earth...
647
00:29:30,160 --> 00:29:31,960
Hurricanes.
- (wind howls)
648
00:29:32,120 --> 00:29:33,920
NARRATOR:
Could an epic cyclonic storm
649
00:29:34,080 --> 00:29:36,360
be responsible
for Saturn's hexagon?
650
00:29:36,520 --> 00:29:38,280
CYLITA GUY: But there's a problem.
651
00:29:38,440 --> 00:29:40,480
This hexagon
isn't like Earth storms.
652
00:29:40,640 --> 00:29:43,840
NARRATOR:
In 1981, the Voyager II space probe
653
00:29:44,000 --> 00:29:45,800
approaches Saturn,
654
00:29:45,960 --> 00:29:48,120
and this historic view from above
655
00:29:48,280 --> 00:29:51,840
reveals something shocking
when it sees Saturn's north pole.
656
00:29:52,000 --> 00:29:54,800
GEORGE KOUROUNIS:
And what did they find? A hexagon.
657
00:29:54,960 --> 00:29:56,960
CYLITA GUY:
And since that first finding,
658
00:29:57,120 --> 00:29:59,360
when Saturn's tilted just right,
659
00:29:59,520 --> 00:30:01,800
we've even been able
to spot it from Earth.
660
00:30:02,720 --> 00:30:04,640
- This strange shape
has been sitting right here
661
00:30:04,800 --> 00:30:06,480
at Saturn's north pole for decades.
662
00:30:06,640 --> 00:30:08,880
PETER SOROYE:
But how could a cyclone
663
00:30:09,040 --> 00:30:10,680
last for such a long time?
664
00:30:10,840 --> 00:30:12,520
- (dramatic music)
665
00:30:12,680 --> 00:30:15,840
NARRATOR: A clue lies
over 600 million kilometres away,
666
00:30:16,000 --> 00:30:18,000
where a space landmark
667
00:30:18,160 --> 00:30:20,840
on another gas giant stands out...
668
00:30:21,000 --> 00:30:23,920
Jupiter's famous red spot.
669
00:30:24,080 --> 00:30:26,760
DAN RISKIN:
The red spot on Jupiter is iconic.
670
00:30:26,920 --> 00:30:29,920
TORRI YATES-ORR: There have been
records of a red spot on Jupiter
671
00:30:30,080 --> 00:30:31,960
since the 1600s.
672
00:30:32,120 --> 00:30:34,160
And while we can't be totally sure
it's the same one,
673
00:30:34,320 --> 00:30:36,320
it sure looks similar.
674
00:30:36,480 --> 00:30:37,600
- From more modern records,
675
00:30:37,760 --> 00:30:39,440
we know that Jupiter's red spot
676
00:30:39,600 --> 00:30:41,600
is at least 150 years old.
677
00:30:41,760 --> 00:30:45,200
Now, if those 17th century
images are of the same spot,
678
00:30:45,360 --> 00:30:48,680
it could be over 350 years old.
679
00:30:48,840 --> 00:30:51,120
TORRI YATES-ORR:
So is there something about
680
00:30:51,280 --> 00:30:53,040
a gas-planet atmosphere
that can make
681
00:30:53,200 --> 00:30:56,600
these enormous storms
live for decades or even centuries?
682
00:30:56,760 --> 00:30:59,080
PETER SOROYE: Unlike Earth
and other rocky planets,
683
00:30:59,240 --> 00:31:02,640
gas-planet atmospheres can stretch
for thousands of kilometres
684
00:31:02,800 --> 00:31:04,560
before you reach the core.
685
00:31:04,720 --> 00:31:06,880
DAN RISKIN: Basically,
gas giants just don't experience
686
00:31:07,040 --> 00:31:09,360
the same kinds of factors
we have here on Earth
687
00:31:09,520 --> 00:31:13,440
that make our atmosphere
so changeable from day to day.
688
00:31:13,600 --> 00:31:15,280
So if something gets going,
689
00:31:15,440 --> 00:31:17,360
chances are its gonna keep going.
690
00:31:17,520 --> 00:31:19,520
CYLITA GUY: It's an important clue.
691
00:31:19,680 --> 00:31:23,320
But is Saturn's hexagon a cyclonic
storm like Jupiter's red spot
692
00:31:23,480 --> 00:31:25,440
or is there something more going on?
693
00:31:26,480 --> 00:31:28,920
NARRATOR:
A closer look at Saturn's hexagon
694
00:31:29,080 --> 00:31:31,080
reveals something staggering.
695
00:31:31,240 --> 00:31:33,000
GEORGE KOUROUNIS: How crazy is this?
696
00:31:33,160 --> 00:31:35,160
The centre looks like a hurricane.
697
00:31:35,320 --> 00:31:36,720
- (tense music)
698
00:31:36,880 --> 00:31:38,560
DAN RISKIN: This thing's huge.
699
00:31:38,720 --> 00:31:41,640
The eye of this thing
is 2,000 kilometres across.
700
00:31:41,800 --> 00:31:44,400
That's 50 times bigger than
the eye of a hurricane on Earth.
701
00:31:44,560 --> 00:31:47,040
NARRATOR:
But this stunning whirlwind
702
00:31:47,200 --> 00:31:50,200
is only a small piece
of the giant hexagon.
703
00:31:50,360 --> 00:31:54,160
What other hidden forces could be
behind this colossal mystery?
704
00:31:54,320 --> 00:31:57,080
GEORGE KOUROUNIS: With a shape
like this right at the centre,
705
00:31:57,240 --> 00:32:00,000
it sure seems like
there's some potent convection
706
00:32:00,160 --> 00:32:01,840
happening in the atmosphere here.
707
00:32:02,000 --> 00:32:05,200
But could that have any connection
to the whole hexagon?
708
00:32:07,480 --> 00:32:09,480
- (ominous music)
709
00:32:09,640 --> 00:32:12,080
NARRATOR: In 2020,
Harvard scientists investigate,
710
00:32:12,240 --> 00:32:16,520
running a simulation on NASA
supercomputers to test their theory.
711
00:32:16,680 --> 00:32:18,400
CYLITA GUY: One that focused on
712
00:32:18,560 --> 00:32:20,920
the sheer size
of Saturn's atmosphere.
713
00:32:21,080 --> 00:32:23,720
DAN RISKIN: Their model
imagined clouds and winds
714
00:32:23,880 --> 00:32:26,480
going down
to 10% of the planet's radius...
715
00:32:26,640 --> 00:32:29,720
So like 6,000 kilometres deep.
716
00:32:29,880 --> 00:32:32,920
Then they started looking at the
kinds of wind patterns that happen
717
00:32:33,080 --> 00:32:35,080
when you combine
the planet's rotation
718
00:32:35,240 --> 00:32:37,680
and that
really, really deep convection.
719
00:32:38,720 --> 00:32:40,400
- (optimistic music)
720
00:32:40,560 --> 00:32:42,240
CYLITA: Let's remember convection -
721
00:32:42,400 --> 00:32:44,240
hot goes up, cold goes down -
722
00:32:44,400 --> 00:32:47,240
is behind the hexagons
in our salt flats on Earth
723
00:32:47,400 --> 00:32:49,080
and the power behind hurricanes.
724
00:32:50,000 --> 00:32:52,240
- Their 3D model showed
something really amazing.
725
00:32:52,400 --> 00:32:54,400
The thermal convection spontaneously
726
00:32:54,560 --> 00:32:58,320
makes exactly the right kinds
of patterns all over the planet,
727
00:32:58,480 --> 00:33:00,600
including at the pole.
728
00:33:01,880 --> 00:33:05,000
Deep under the surface there are
these vortices, these cyclones,
729
00:33:05,160 --> 00:33:09,400
that kind of pinch the jet stream
into that hexagon shape.
730
00:33:09,560 --> 00:33:12,960
Because those air movements
are deep, they're stable.
731
00:33:13,120 --> 00:33:15,560
So the forms they make
stick around for decades.
732
00:33:15,720 --> 00:33:17,480
GEORGE KOUROUNIS: But this is space
733
00:33:17,640 --> 00:33:20,120
we're talking about.
We can't close the case just yet.
734
00:33:20,280 --> 00:33:22,040
DAN RISKIN:
These are just computer models
735
00:33:22,200 --> 00:33:25,920
based on what we can see from
Cassini and a whole lot of guessing.
736
00:33:26,080 --> 00:33:29,000
If we wanna learn more, we gotta
send a probe right into the hexagon,
737
00:33:29,160 --> 00:33:31,760
and that's probably
at least a few years away.
738
00:33:31,920 --> 00:33:35,480
Until we get
to the ringed planet ourselves,
739
00:33:35,640 --> 00:33:37,840
Earth is gonna be
the only laboratory we have
740
00:33:38,000 --> 00:33:40,240
to learn about how it all works.
741
00:33:40,400 --> 00:33:42,400
- (contemplative music)
742
00:33:47,400 --> 00:33:49,520
NARRATOR:
Far above the Canadian landscape,
743
00:33:49,680 --> 00:33:51,680
satellites looking down from space
744
00:33:51,840 --> 00:33:53,600
spot something uncanny
745
00:33:53,760 --> 00:33:55,760
among the lakes
of Northern Saskatchewan.
746
00:33:56,800 --> 00:33:58,600
PETER SOROYE:
There are over 100,000
747
00:33:58,760 --> 00:34:00,640
lakes and rivers in Saskatchewan,
748
00:34:00,800 --> 00:34:03,760
mainly left behind
by Ice Age glaciers.
749
00:34:03,920 --> 00:34:06,200
- When seen from the skies,
one of these lakes
750
00:34:06,360 --> 00:34:08,120
really stands out.
751
00:34:08,280 --> 00:34:11,080
SHEILA HOFFMAN: There's a body of
water that looks almost like an eye.
752
00:34:11,240 --> 00:34:14,240
It's almost perfectly round and
has an island right in the centre.
753
00:34:14,400 --> 00:34:16,080
CYLITA GUY: Which kind of makes
754
00:34:16,240 --> 00:34:18,040
the whole thing
look like a giant Cheerio.
755
00:34:18,200 --> 00:34:20,640
GUY WALTER:
Now, the lake isn't huge.
756
00:34:20,800 --> 00:34:22,720
It's about
four to five kilometres across
757
00:34:22,880 --> 00:34:25,400
and the island itself
is about two kilometres long,
758
00:34:25,560 --> 00:34:27,600
but it doesn't look normal.
759
00:34:27,760 --> 00:34:29,800
CYLITA GUY: If you think
about the depth of the lake
760
00:34:29,960 --> 00:34:31,720
along with its circular shape
761
00:34:31,880 --> 00:34:34,720
it almost looks like
a crater that's filled with water.
762
00:34:34,880 --> 00:34:38,200
TORRI YATES-ORR: What could have
created such a bizarre formation
763
00:34:38,360 --> 00:34:41,120
and why does it look so different
from the surrounding lakes?
764
00:34:41,280 --> 00:34:42,960
PETER SOROYE:
What forces are capable
765
00:34:43,120 --> 00:34:45,920
of creating
huge circles on the Earth's surface?
766
00:34:46,080 --> 00:34:48,080
- (tense music)
767
00:34:48,240 --> 00:34:50,280
NARRATOR:
A potential clue could be hidden
768
00:34:50,440 --> 00:34:52,440
around 6,000 kilometres away,
769
00:34:52,600 --> 00:34:54,680
in the English village of Hanbury.
770
00:34:54,840 --> 00:34:57,960
From above,
among a patchwork of farm fields,
771
00:34:58,120 --> 00:35:02,120
lies an unexpected
circular crater filled with trees
772
00:35:02,280 --> 00:35:04,600
concealing the heart of a disaster.
773
00:35:05,440 --> 00:35:07,880
GUY WALTERS:
About 80 years ago, in 1944,
774
00:35:08,040 --> 00:35:10,920
the UK is in the home stretch
of the Second World War.
775
00:35:11,080 --> 00:35:12,760
- (artillery fire)
776
00:35:12,920 --> 00:35:14,600
GUY WALTERS:
That's the year that you have
777
00:35:14,760 --> 00:35:18,280
the D-Day landings in Normandy
and the liberation of Paris.
778
00:35:18,440 --> 00:35:20,280
TORRI YATES-ORR:
But in the rural countryside,
779
00:35:20,440 --> 00:35:22,600
hundreds of kilometres
from the front lines,
780
00:35:22,760 --> 00:35:24,880
peace is about to be shattered.
781
00:35:25,040 --> 00:35:26,720
GUY WALTER: On November the 27th,
782
00:35:26,880 --> 00:35:29,720
at 11 o'clock in the morning,
there's this sudden explosion
783
00:35:29,880 --> 00:35:32,560
that shakes
the entire village of Hanbury.
784
00:35:32,720 --> 00:35:34,680
- (explosion)
785
00:35:34,840 --> 00:35:36,720
GUY WALTER:
You've got this double blast
786
00:35:36,880 --> 00:35:39,600
shooting this mushroom cloud
into the sky,
787
00:35:39,760 --> 00:35:43,240
and it flattens everything
in a 13-hundred-metre radius.
788
00:35:43,400 --> 00:35:45,480
TORRI YATES-ORR: The blast leaves
789
00:35:45,640 --> 00:35:47,600
a huge circular crater
on the landscape.
790
00:35:47,760 --> 00:35:51,120
It's around 250 metres across
and about 30 metres deep.
791
00:35:52,280 --> 00:35:55,400
NARRATOR: But what explosive power
is behind this destruction?
792
00:35:56,440 --> 00:35:59,000
Could the answer
be concealed below the surface?
793
00:35:59,920 --> 00:36:01,880
GUY WALTER: What you've got here
is a highly secret
794
00:36:02,040 --> 00:36:04,280
British bomb storage site,
795
00:36:04,440 --> 00:36:06,320
known as RAF Fauld.
796
00:36:06,480 --> 00:36:08,880
And this place stored
absolutely huge amounts
797
00:36:09,040 --> 00:36:11,200
of various explosive munitions.
798
00:36:11,360 --> 00:36:13,920
I mean, this place
was packed to the rafters.
799
00:36:15,160 --> 00:36:18,080
TORRI YATES-ORR:
That's a lot of power in one place,
800
00:36:18,240 --> 00:36:21,280
and if anyone found out about it
that would be a major target.
801
00:36:21,440 --> 00:36:23,880
So did spies discover it
and plan its destruction?
802
00:36:24,040 --> 00:36:25,720
Was it sabotaged?
803
00:36:26,640 --> 00:36:28,320
GUY WALTER:
This is a part of England
804
00:36:28,480 --> 00:36:31,480
that has long been targeted
by Axis air raids,
805
00:36:31,640 --> 00:36:33,320
and the Nazis very quickly claim
806
00:36:33,480 --> 00:36:37,920
that it's one of their V-2 rockets
that has caused this devastation.
807
00:36:38,080 --> 00:36:39,520
- (explosion)
808
00:36:39,680 --> 00:36:41,520
SHEILA HOFFMAN:
But this time, it isn't the Germans.
809
00:36:41,680 --> 00:36:44,520
The investigation revealed
something shocking and tragic.
810
00:36:44,680 --> 00:36:46,560
In the pressure of wartime,
811
00:36:46,720 --> 00:36:48,440
a fatal mistake was made.
812
00:36:48,600 --> 00:36:50,680
GUY WALTER:
It's very likely that someone
813
00:36:50,840 --> 00:36:52,840
mishandled a live bomb.
814
00:36:53,000 --> 00:36:57,120
Now, the thick walls of the mine
prevent an even worse catastrophe,
815
00:36:57,280 --> 00:36:59,560
but what happened was bad enough.
816
00:36:59,720 --> 00:37:03,080
TORRI YATES-ORR: About four million
kilograms of explosives,
817
00:37:03,240 --> 00:37:07,960
including a whopping 500 million
rounds of rifle ammunition, blew up.
818
00:37:08,120 --> 00:37:09,800
- (explosion)
819
00:37:09,960 --> 00:37:12,840
TORRI YATES-ORR: It was one of the
largest explosions ever in the UK.
820
00:37:14,000 --> 00:37:16,160
SHEILA HOFFMAN:
When you see it from above today,
821
00:37:16,320 --> 00:37:18,200
the crater
is filled with trees and plants
822
00:37:18,360 --> 00:37:20,040
and looks quite peaceful and safe.
823
00:37:20,200 --> 00:37:23,200
GUY WALTER:
But the hole in the earth remains,
824
00:37:23,360 --> 00:37:27,360
along with a number of explosives
still buried in those tunnels below.
825
00:37:27,520 --> 00:37:30,920
NARRATOR: Could the
strange-shaped lake in Saskatchewan
826
00:37:31,080 --> 00:37:34,120
be the result
of a World War II era weapon?
827
00:37:34,280 --> 00:37:35,720
GUY WALTER:
While Japan lobbed shells
828
00:37:35,880 --> 00:37:38,520
at a British Columbia lighthouse
in 1942
829
00:37:38,680 --> 00:37:40,800
and Axis forces
hit the St Lawrence River
830
00:37:40,960 --> 00:37:42,800
during the Battle of the Atlantic,
831
00:37:42,960 --> 00:37:44,960
Saskatchewan
was well out of reach.
832
00:37:45,120 --> 00:37:47,800
TORRI YATES-ORR: So
if this weird doughnut-shaped lake
833
00:37:47,960 --> 00:37:50,840
isn't a sign of
some kind of human-made explosion,
834
00:37:51,000 --> 00:37:52,760
what else could be going on?
835
00:37:52,920 --> 00:37:54,600
SHEILA HOFFMAN:
What other forces can make
836
00:37:54,760 --> 00:37:56,720
this kind of unique shape
on the landscape?
837
00:37:56,880 --> 00:37:59,240
Is a powerful natural force
at play here?
838
00:37:59,400 --> 00:38:02,320
CYLITA GUY: There's another
out-of-this world possibility.
839
00:38:03,760 --> 00:38:05,760
- (meteor cracks)
840
00:38:07,080 --> 00:38:10,000
PETER SOROYE: There are a few known
impact craters around Canada,
841
00:38:10,160 --> 00:38:12,440
so it makes sense to think
this could be among them.
842
00:38:14,640 --> 00:38:16,560
NARRATOR:
But when researchers venture
843
00:38:16,720 --> 00:38:18,680
into the wilds of Saskatchewan
to investigate,
844
00:38:18,840 --> 00:38:20,680
they uncover something revealing.
845
00:38:20,840 --> 00:38:23,440
TORRI YATES-ORR: When they examine
the rock of the centre island,
846
00:38:23,600 --> 00:38:26,120
they realise
something strange is going on.
847
00:38:27,160 --> 00:38:30,600
NARRATOR: This isn't like any impact
crater they've ever seen on Earth.
848
00:38:30,760 --> 00:38:32,440
CYLITA GUY: On Earth, you expect
849
00:38:32,600 --> 00:38:34,320
two main kinds of impact craters.
850
00:38:34,480 --> 00:38:36,600
Smaller impacts make simple craters,
851
00:38:36,760 --> 00:38:39,720
which are basically just
these bowl-shaped holes.
852
00:38:39,880 --> 00:38:43,280
Bigger impacts make
something called complex craters.
853
00:38:43,440 --> 00:38:46,040
PETER SOROYE: When
these bigger meteors hit the ground,
854
00:38:46,200 --> 00:38:49,040
it's so big and powerful,
has so much energy,
855
00:38:49,200 --> 00:38:51,800
that solid earth
starts to act like a fluid
856
00:38:51,960 --> 00:38:55,240
and rebounds or splashes up
in the middle of the impact hole,
857
00:38:55,400 --> 00:38:57,480
like when a stone
is thrown into the water.
858
00:38:57,640 --> 00:38:59,920
When that rebound of solid earth
drops back down,
859
00:39:00,080 --> 00:39:02,000
you're left with a central peak.
860
00:39:02,160 --> 00:39:04,640
GEORGE KOUROUNIS: If you look
at the shape of this lake doughnut,
861
00:39:04,800 --> 00:39:07,880
it looks just like
a complex crater filled with water.
862
00:39:08,040 --> 00:39:10,480
That's what the researchers
expected to find.
863
00:39:10,640 --> 00:39:12,320
- (dramatic music)
864
00:39:12,480 --> 00:39:14,680
NARRATOR: But what
they uncover is out of this world.
865
00:39:16,120 --> 00:39:19,120
CYLITA GUY: Basically, the rock here
is the wrong kind of rock.
866
00:39:19,280 --> 00:39:21,320
Whatever this central island is,
867
00:39:21,480 --> 00:39:25,120
it wasn't made by the rebound
you see of a complex crater.
868
00:39:25,280 --> 00:39:27,840
DAN RISKIN: But it can't be
a simple crater either
869
00:39:28,000 --> 00:39:30,640
because the floor and the walls
are too full of debris.
870
00:39:30,800 --> 00:39:32,480
CYLITA GUY:
The researchers realised
871
00:39:32,640 --> 00:39:34,360
they'd seen
something like this before
872
00:39:34,520 --> 00:39:36,520
but not on Earth.
873
00:39:36,680 --> 00:39:38,760
NARRATOR:
The final clue to solve this mystery
874
00:39:38,920 --> 00:39:41,200
can be found
by looking down from above
875
00:39:41,360 --> 00:39:43,520
at our planet's nearest neighbour...
876
00:39:43,680 --> 00:39:45,520
the moon.
877
00:39:45,680 --> 00:39:47,560
PETER SOROYE:
Earth's moon is pockmarked
878
00:39:47,720 --> 00:39:49,920
by countless thousands of craters
879
00:39:50,080 --> 00:39:53,440
from the giant 25-hundred-kilometre
South Pole-Aitken basin
880
00:39:53,600 --> 00:39:58,040
to the microscopic dents found in
moon rocks from the Apollo missions.
881
00:39:59,000 --> 00:40:01,560
- Because of the lack of
atmosphere and plate tectonics,
882
00:40:01,720 --> 00:40:03,520
the moon's craters aren't subject to
883
00:40:03,680 --> 00:40:05,360
the same changes
we see here on Earth.
884
00:40:05,520 --> 00:40:09,240
For example, they don't get hidden
over time by things like water.
885
00:40:09,400 --> 00:40:11,520
As a result,
these craters can tell us
886
00:40:11,680 --> 00:40:15,240
a lot about the history of the
meteoroid strikes that form them.
887
00:40:16,200 --> 00:40:18,200
NARRATOR:
And one type of moon crater
888
00:40:18,360 --> 00:40:20,520
could solve
the mystery in Saskatchewan.
889
00:40:21,360 --> 00:40:24,640
DAN RISKIN: When you look at sort
of medium-size craters on the moon
890
00:40:24,800 --> 00:40:27,400
from like 15 to 42 kilometres
in diameter,
891
00:40:27,560 --> 00:40:29,640
you see something pretty special.
892
00:40:29,800 --> 00:40:32,600
PETER SOROYE: These aren't
bowl-shaped, like simple craters,
893
00:40:32,760 --> 00:40:35,760
but they don't have the central
peak of complex craters either.
894
00:40:35,920 --> 00:40:39,160
DAN RISKIN: Instead, they're
kind of like this in-between stage
895
00:40:39,320 --> 00:40:41,840
where they have some of
the traits of each type of crater.
896
00:40:42,000 --> 00:40:44,120
These are called
transitional craters.
897
00:40:44,280 --> 00:40:45,960
They have flat floors,
898
00:40:46,120 --> 00:40:48,120
one or more terraces or rock slides,
899
00:40:48,280 --> 00:40:50,080
like you'd see in a complex crater,
900
00:40:50,240 --> 00:40:52,120
but with no central peak.
901
00:40:52,280 --> 00:40:53,960
NARRATOR:
But can this happen on Earth?
902
00:40:54,120 --> 00:40:57,640
CYLITA GUY: Transitional craters
form so easily on the moon
903
00:40:57,800 --> 00:41:00,600
because of its lack of atmosphere
and low gravity.
904
00:41:00,760 --> 00:41:03,520
So it's easier for larger objects
to hit more gently.
905
00:41:03,680 --> 00:41:06,640
DAN RISKIN: But with
Earth's atmosphere and gravity,
906
00:41:06,800 --> 00:41:09,640
we don't expect quite
so much of that middle ground.
907
00:41:09,800 --> 00:41:11,960
Anything that would make
a medium hit on the moon
908
00:41:12,120 --> 00:41:14,440
would accelerate
way more in Earth's gravity,
909
00:41:14,600 --> 00:41:16,840
so it would end up being
a big punch, not a medium one.
910
00:41:17,000 --> 00:41:18,680
- (meteor hisses)
911
00:41:18,840 --> 00:41:21,240
CYLITA: Science basically thought
that finding that middle ground
912
00:41:21,400 --> 00:41:24,000
here on Earth
was essentially impossible.
913
00:41:24,160 --> 00:41:27,080
But this discovery
changes everything.
914
00:41:27,240 --> 00:41:28,920
DAN RISKIN:
To find something
915
00:41:29,080 --> 00:41:32,200
that we can confirm
is a transitional impact crater
916
00:41:32,360 --> 00:41:34,160
and to see that
it's in such good shape,
917
00:41:34,320 --> 00:41:36,400
this is groundbreaking.
918
00:41:36,560 --> 00:41:38,360
PETER SOROYE:
But then you've got to ask...
919
00:41:38,520 --> 00:41:40,200
how did the central island form
920
00:41:40,360 --> 00:41:42,200
if not through
the initial space rock impact?
921
00:41:42,360 --> 00:41:44,040
- (dramatic music)
922
00:41:44,200 --> 00:41:46,440
DAN RISKIN: The crater
is about 200 million years old.
923
00:41:46,600 --> 00:41:48,880
So it happened
when the Earth looked very different
924
00:41:49,040 --> 00:41:50,720
from the way it looks today.
925
00:41:50,880 --> 00:41:52,560
CYLITA GUY:
So it's hard to say for sure
926
00:41:52,720 --> 00:41:54,400
what factors created the island.
927
00:41:54,560 --> 00:41:58,000
DAN RISKIN: But the thinking
is that, over millions of years,
928
00:41:58,160 --> 00:42:00,160
wind and rain would have worn down
929
00:42:00,320 --> 00:42:02,840
the edges of the crater
until it was almost flat,
930
00:42:03,000 --> 00:42:05,720
and that central dip
would have filled with sediment.
931
00:42:05,880 --> 00:42:07,880
CYLITA GUY: Then, experts think that
932
00:42:08,040 --> 00:42:11,080
the movement of glaciers over
the land during the last ice age
933
00:42:11,240 --> 00:42:13,080
could have carved up the landscape,
934
00:42:13,240 --> 00:42:15,080
including in this ancient crater.
935
00:42:15,240 --> 00:42:17,240
DAN RISKIN:
Thanks to the melting glaciers,
936
00:42:17,400 --> 00:42:19,800
water would have filled
these new scars in the landscape,
937
00:42:19,960 --> 00:42:23,840
which merged with the crater
to form the lake as we see it today.
938
00:42:24,800 --> 00:42:28,080
NARRATOR: This astonishing
discovery isn't just unprecedented.
939
00:42:28,240 --> 00:42:29,920
CYLITA GUY: It's the chance to study
940
00:42:30,080 --> 00:42:32,880
a phenomena we observe on the moon
right here on Earth.
941
00:42:33,040 --> 00:42:35,960
This is what makes this discovery
even more exciting.
942
00:42:36,840 --> 00:42:39,760
NARRATOR: Another Canadian
impact crater in Labrador
943
00:42:39,920 --> 00:42:42,560
is already hosting
cutting-edge lunar research.
944
00:42:42,720 --> 00:42:45,760
PETER SOROYE: The meteorite
that made the Mistastin Lake crater
945
00:42:45,920 --> 00:42:48,240
left behind rocks
that are almost identical
946
00:42:48,400 --> 00:42:50,920
to ones found all over the moon.
947
00:42:51,080 --> 00:42:54,240
CYLITA GUY: So today NASA
uses the site to train astronauts
948
00:42:54,400 --> 00:42:56,640
for their new moon mission -
Artemis.
949
00:42:56,800 --> 00:42:58,840
DAN RISKIN: And this lake may hold
950
00:42:59,000 --> 00:43:01,080
just as many lunar-style secrets.
951
00:43:01,240 --> 00:43:03,040
CYLITA GUY: It's amazing to me
952
00:43:03,200 --> 00:43:06,120
how much we can learn
about our solar system and beyond
953
00:43:06,280 --> 00:43:08,880
from studying
features right here on Earth.
954
00:43:09,800 --> 00:43:11,680
DAN RISKIN: I think this is cool
because we use the moon
955
00:43:11,840 --> 00:43:13,360
to solve this mystery here on Earth.
956
00:43:13,520 --> 00:43:15,400
But as we do
the research on the ground,
957
00:43:15,560 --> 00:43:18,000
we uncover these secrets that are
gonna help us understand the moon.
958
00:43:18,160 --> 00:43:19,920
- (wind whistles)
959
00:43:20,080 --> 00:43:21,800
- (dramatic music)
960
00:43:21,960 --> 00:43:24,240
NARRATOR: From signs of ice on Mars
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00:43:24,400 --> 00:43:26,320
and stunning shapes on Saturn
962
00:43:26,480 --> 00:43:30,600
to hidden impact craters and
mysterious milky seas on Earth...
963
00:43:30,760 --> 00:43:33,920
some of the grandest mysteries
are discovered from space.
964
00:43:34,880 --> 00:43:37,960
And with the latest technology
looking down from above,
965
00:43:38,120 --> 00:43:40,720
Earth's secrets can reveal
the truth about space
966
00:43:40,880 --> 00:43:43,720
and resolve longstanding riddles
back home.
967
00:43:43,880 --> 00:43:45,880
- (uplifting music)
968
00:43:47,200 --> 00:43:49,880
- I love the fact that
we're learning more and more
969
00:43:50,040 --> 00:43:53,400
about our own backyard
here in the vastness of space.
970
00:43:54,520 --> 00:43:57,560
- And you just know that the next
find is right around the corner.
971
00:44:03,120 --> 00:44:06,080
Subtitles by Sky Access Services
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