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Mars.
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The red planet.
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Many scientists believe
that the first person
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to set foot on its surface
is alive today.
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Perhaps it's you.
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If it is you, then welcome
to your ultimate travel guide.
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Using real images and data,
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we will take you to some of
the most jaw-dropping landscapes
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discovered in our solar system
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right here on Mars.
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We don't have anything like this
on earth.
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Places that may change
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the way you think
about our own world...
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Is there life beyond the earth?
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This is probably one
of the most profound questions
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that's ever been asked
by the human mind.
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...on a journey
that will test the endurance
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of any traveler.
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Traveling to Mars
is not for the faint of heart.
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At the dawn of the
next golden age of exploration,
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here's your quintessential guide
to the martian frontier.
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Oh, it's beautiful.
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Have you ever dreamed about
traveling out of this world?
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My name is Mike Massimino,
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and I turned that fantasy
into a reality
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when I space-walked to repair
the Hubble space telescope.
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Great job, Mike.
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Now as we expand our knowledge
of our solar system
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from Mercury
to the cosmic unknowns,
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I want to take you
on a personal journey to...
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-- Captions by vitac --
www.Vitac.Com
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captions paid for by
discovery communications
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welcome to "the planets."
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I'm Mike Massimino.
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Ever since my space missions,
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I've thought about which planet
in the solar system
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I'd like to visit.
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Hands down, it's Mars.
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So far, humans have only
touched down on our moon,
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but that could change.
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NASA is planning on sending
its first astronaut to Mars
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as soon as 2030,
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but there's a whole lot more
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we need to find out about
our neighbor before we visit.
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The red glow of Mars
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is a constant feature
in our night sky.
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But it's only
when viewed up close
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that this rusty planet
begins to reveal its secrets.
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It promises to wow any visitor
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who just traveled
the seven months it would take
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to get there from the earth
by spaceship.
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Other than our home planet,
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there is no world
we know in such detail.
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That's thanks to the numerous
satellites and rovers
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we've sent there
over the past 50 years.
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And the landscapes
they have looked down upon
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tell astonishing stories.
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Vast plains riddled
with hundreds of thousands
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of craters, deep canyons,
and strange rock formations,
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and views not seen
anywhere on earth.
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We've photographed
every corner of the planet,
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and plans are now under way to
send the first humans to Mars.
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But what does it take
to get there?
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How can we survive
on the surface?
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And where are the best places
to explore?
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For those ready for adventure,
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the best place to start is
a well-known martian landmark --
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Gale crater,
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a vast scar on the planet
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and home to NASA's flagship
rover, curiosity, since 2012.
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The crater itself dwarfs any
similar features here on earth.
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Every day, curiosity
sends back detailed images
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from within the crater.
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This is one of them.
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And here,
at the data science institute,
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professor Sanjeev Gupta is part
of the team studying them.
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This is the crater rim
over here.
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This is 150 kilometers
in diameter.
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It's a really big feature.
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And there,
in this view over here,
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what we can see is mount sharp.
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That's 5 kilometers high.
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That sits in the center of the
crater, so it's really amazing
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'cause you really get
a sense of this mountain
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that's sort of
towering high above us.
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That's a mountain
over 93 miles across
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and over 3 miles high.
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But professor Gupta
isn't simply enjoying the view.
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Today, we know Mars
as a dry, desolate world,
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but some images suggest
that wasn't always the case.
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Gale crater was chosen as
the landing site for curiosity
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after a very lengthy
selection process.
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Orbiters had discovered evidence
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that the rocks
at the base of mount sharp --
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so, the rocks
that we can see over here --
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had evidence for hydration.
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Long before
curiosity left earth,
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satellite images like this
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hinted there was more to
this crater than meets the eye.
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And what's beautiful
in this image
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is that you can see
these canyons or valleys
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carved into the crater rim,
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and this is really suggestive
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that water flowed down
the crater rim
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and eroded these canyons.
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Secondly, we can see
all these beautiful layers here
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that form the base
of mount sharp.
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These layers are enriched
in hydrated minerals.
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So, those are minerals
that contain water.
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Curiosity's mission?
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To follow the elusive trail
of water on Mars.
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So, essentially,
the orbital images
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provide us clues on where to go,
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but we really need
to be on the ground,
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looking carefully at these rocks
from a few meters away,
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and that's why we send rovers
to Mars.
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Once the rover touched down,
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it quickly began picking up
more clues.
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These are actually pebbles
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that are a few centimeters
in diameter.
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What you can see when you look
at the pebble outlines
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is that they have
rounded shapes.
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So they've been,
basically, rounded
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during a transport process.
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And they're too large
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to be moved
and rounded by wind processes,
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and so the only way we can
actually get this rounding
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is by water flow.
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I think it's irrefutable
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that there was once water
flowing at the surface on Mars,
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based on
the geological evidence.
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But even
with its smooth surface,
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Gale crater wouldn't be
the best landing site on Mars.
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So the question remains, where
should you first touch down?
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This canyon is Valles Marineris,
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named after the mariner 9, the
NASA mission that discovered it.
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The scale of the canyon
is breathtaking.
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It is like the Grand Canyon
on earth, but supersized.
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In places, its walls
plunge 6 miles down,
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a unique geological formation
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not matched
anywhere else on the planet.
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And it's thanks to this geology
that this vast canyon system
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makes the ideal landing site
for martian explorers.
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Astrogeologist Dr. Jim rice
is confident in this conclusion.
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He's been involved
in selecting Mars landing sites
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for every NASA mission
since Mars pathfinder in 1994.
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You want something fairly flat,
not too rocky, not too dusty.
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And because we use parachutes
to help slow us down
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in the entry
to the martian atmosphere,
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we're gonna be lower
in elevation.
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And the views while
landing would be jaw-dropping.
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Valles Marineris is a great spot
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because it's basically kind of
like the Grand Canyon here.
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It's like someone has taken --
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a giant surgeon with
a scalpel making an incision
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and opened up the crust
of the planet,
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allowing you to see deeper down,
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and deeper down in geology
is further back in history.
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It's this view inside the planet
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that is the big draw
for Dr. rice,
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but for most of us,
the epic scale alone
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would be enticing enough.
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Now, that canyon
is 10 times longer
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than the Grand Canyon here,
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it's four times deeper,
and about 12 times wider.
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Another way
to think about it is,
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the vast expanse
of this canyon system,
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the length of it would be from
New York City to Los Angeles.
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So that truly is the grand
canyon of the solar system.
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Valles Marineris
would provide the ultimate draw
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for any martian visitor.
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But it's not just the views
that are attractive.
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Touching down inside
Valles Marineris
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could help answer
long-held questions
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about the chasm's formation.
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Images like this,
taken from orbit,
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give us some clues
to its history.
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Once theory
is that ancient volcanoes
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ripped apart the surface,
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creating a rift that running
water continued to carve.
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But only by landing there can
we gather the conclusive proof.
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What you want to do
as a geologist
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is get to outcrop
like we see right here,
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a slab of rock
you can get up and interrogate
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and kind of taste, so to speak,
with your instruments.
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If you're a martian coming to
earth, you'd probably come here,
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because you'd get a good idea
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of the geologic history
of the earth
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from the rim
all the way down to the floor.
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You know, most of these rocks
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record oceans
that came and went,
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mountain chains
that came and went,
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deserts that came and went.
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You know, on Mars,
I think it'd be safe to say
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you'd go back 3, 3 1/2,
maybe even 4 billion years
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at the floor of the canyon
down there.
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I'd go in a heartbeat.
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00:10:07,979 --> 00:10:11,716
Would you take
the chance to travel to Mars?
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Visiting the red planet
is not just about sightseeing.
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Once you get there,
you'll have to survive
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some of the harshest conditions
in the entire solar system.
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Years of hard work and planning
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00:10:28,059 --> 00:10:31,759
went into my missions
to the Hubble space telescope,
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00:10:31,763 --> 00:10:33,793
but preparing to go to Mars
is a whole other story.
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00:10:33,798 --> 00:10:37,335
There'll be
ice-cold temperatures
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00:10:37,335 --> 00:10:39,035
and solar radiation
coming at you from every angle.
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00:10:39,037 --> 00:10:41,937
So to meet these challenges,
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00:10:41,940 --> 00:10:43,940
scientists are coming up
with some useful new tools
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00:10:43,942 --> 00:10:46,242
to help us survive.
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00:10:48,913 --> 00:10:53,913
Mars is a barren world,
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00:10:53,918 --> 00:10:55,718
with its water and atmosphere
long lost to the hands of time.
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00:10:55,720 --> 00:10:59,590
For human space travelers,
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00:10:59,591 --> 00:11:01,321
it would be an absolutely
inhospitable environment.
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00:11:01,326 --> 00:11:04,356
That is why researchers
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00:11:04,362 --> 00:11:08,032
have descended upon
the volcanoes of Hawaii,
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00:11:08,032 --> 00:11:11,632
an environment on earth
that closely matches Mars
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in terms of landscape, at least.
218
00:11:14,405 --> 00:11:17,105
They're trying to figure out
how we can survive
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00:11:17,108 --> 00:11:19,177
on the desolate
and hostile planet.
220
00:11:22,213 --> 00:11:26,483
Michael lye and his team
have designed a space suit
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00:11:26,484 --> 00:11:30,254
to simulate Mars missions
here on Hawaii.
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00:11:30,254 --> 00:11:32,724
Once you land on Mars, you're
basically living in a vacuum.
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00:11:32,724 --> 00:11:34,754
It's got an atmosphere,
but not much.
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00:11:34,759 --> 00:11:37,259
And while you're there,
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00:11:37,261 --> 00:11:39,661
you won't be able to go outside
and breathe naturally.
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00:11:42,734 --> 00:11:45,734
Temperature-wise, it's gonna be
extremely cold many times.
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00:11:45,737 --> 00:11:49,907
And it's generally
a pretty hostile environment --
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00:11:49,907 --> 00:11:52,337
solar flares, U.V. radiation,
Alpha particles,
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00:11:52,343 --> 00:11:53,943
other kinds of radiation
from the sun,
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00:11:53,945 --> 00:11:57,215
as well as cosmic radiation
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00:11:57,215 --> 00:11:59,115
that's coming from all over
the solar system and beyond.
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You have to wear a space suit
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00:12:01,819 --> 00:12:03,649
the entire time
you're on the surface of Mars.
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00:12:05,890 --> 00:12:11,860
Temperatures on Mars
can plummet
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00:12:11,863 --> 00:12:14,732
to below negative-195 degrees
near the poles.
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00:12:14,732 --> 00:12:19,270
Containing virtually no oxygen,
237
00:12:19,270 --> 00:12:23,270
the wispy atmosphere
has a pressure of just 0.6%
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00:12:23,274 --> 00:12:27,812
of what can be found
at sea level here on earth.
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00:12:27,812 --> 00:12:31,712
This is why space suits will be
one of the critical components
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00:12:31,716 --> 00:12:32,884
for any future human missions.
241
00:12:32,884 --> 00:12:35,084
So, you need something
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00:12:35,086 --> 00:12:37,516
to protect you
from essentially exploding
243
00:12:37,522 --> 00:12:39,422
or at least having your skin
all stretched out
244
00:12:39,424 --> 00:12:41,254
and the blood boiling
and getting the bends,
245
00:12:41,259 --> 00:12:43,689
things like that.
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00:12:43,695 --> 00:12:46,564
The way space suits
are designed now,
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00:12:46,564 --> 00:12:49,164
they're mostly
pressurized spacecraft.
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00:12:49,167 --> 00:12:52,367
Essentially, they're almost like
a mini spaceship.
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00:12:56,941 --> 00:13:00,278
Oh, it's beautiful, Mike.
It really is.
250
00:13:00,278 --> 00:13:03,008
Martian visitors will require
a full face helmet,
251
00:13:03,014 --> 00:13:04,682
permanent oxygen supply,
life support,
252
00:13:04,682 --> 00:13:08,982
and electrical systems
253
00:13:08,986 --> 00:13:11,923
just like astronauts on board
the international space station.
254
00:13:11,923 --> 00:13:14,523
But you'll have to look
beyond your space suit
255
00:13:14,525 --> 00:13:18,863
for safety and shelter.
256
00:13:18,863 --> 00:13:22,033
The next location
in our Mars travel guide
257
00:13:22,033 --> 00:13:25,870
is one that could provide
some much-needed refuge
258
00:13:25,870 --> 00:13:29,070
for the weary traveler --
the Tharsis region,
259
00:13:29,073 --> 00:13:31,743
home to some of the largest
volcanoes in the solar system,
260
00:13:31,743 --> 00:13:34,873
including Pavonis Mons.
261
00:13:34,879 --> 00:13:38,149
This may not look like
a typical home,
262
00:13:38,149 --> 00:13:41,819
but buried just beneath
the surface of this volcano
263
00:13:41,819 --> 00:13:44,819
is a unique feature that offers
protection from the elements,
264
00:13:44,822 --> 00:13:47,252
and, remarkably,
similar features
265
00:13:47,258 --> 00:13:49,188
can be found right here on earth
266
00:13:49,193 --> 00:13:51,162
if you know
where to look for them.
267
00:13:54,866 --> 00:13:58,336
We're out here
on an A'a flow in Hawaii.
268
00:13:58,336 --> 00:14:00,236
This lava flow originated
towards the summit of Mauna Loa
269
00:14:00,238 --> 00:14:02,268
and has flowed
about 20 kilometers
270
00:14:02,273 --> 00:14:05,073
towards the ocean here.
271
00:14:05,076 --> 00:14:09,646
But what you don't see
is that this lava flow
272
00:14:09,647 --> 00:14:11,517
is covering a vast network of
lava tubes that is now below us,
273
00:14:14,452 --> 00:14:15,982
and that's
what we want to get to.
274
00:14:15,987 --> 00:14:18,087
Volcanoes are cool
275
00:14:18,089 --> 00:14:20,858
'cause we find them
all over the solar system.
276
00:14:20,858 --> 00:14:23,758
Volcanism
is a fundamental process
277
00:14:23,761 --> 00:14:27,231
for shaping planetary bodies,
for shaping moons,
278
00:14:27,231 --> 00:14:31,001
so the more we can learn about
it, the more we can understand
279
00:14:31,002 --> 00:14:33,371
our solar system
and our universe.
280
00:14:33,371 --> 00:14:36,440
The surface of Pavonis Mons
281
00:14:36,440 --> 00:14:38,570
is riddled with lava tubes
like this,
282
00:14:38,576 --> 00:14:41,946
natural caverns that formed
283
00:14:41,946 --> 00:14:44,916
when the planet
was still volcanically active.
284
00:14:44,916 --> 00:14:48,486
NASA volcanologist
Dr. Brent Garry
285
00:14:48,486 --> 00:14:50,354
has dedicated his career
to understanding these features.
286
00:14:50,354 --> 00:14:54,792
As a lava flow is coming down,
287
00:14:54,792 --> 00:14:57,192
these tube systems can form
underneath a solid crust.
288
00:14:57,195 --> 00:14:59,063
So you'll have a hard crust
on the outside,
289
00:14:59,063 --> 00:15:01,663
and the interior
will be the lava,
290
00:15:01,666 --> 00:15:03,066
the liquid rock
flowing through it.
291
00:15:03,067 --> 00:15:06,097
Think of the London underground.
292
00:15:06,103 --> 00:15:08,403
It's like a subway system
of lava going through there.
293
00:15:08,406 --> 00:15:11,436
And as the lava drains out,
294
00:15:11,442 --> 00:15:13,242
that's when we're left
with these giant cavern systems
295
00:15:15,513 --> 00:15:18,683
that we see here,
that we're inside right now.
296
00:15:18,683 --> 00:15:21,652
Today, Dr. Garry
is using light detection
297
00:15:21,652 --> 00:15:26,422
and ranging technology,
or LiDAR,
298
00:15:26,424 --> 00:15:29,124
to create a 3-d model
of this lava tube in Hawaii.
299
00:15:29,126 --> 00:15:31,156
What we're building
with all the LiDAR scans
300
00:15:31,162 --> 00:15:33,262
is a map of a lava tube.
301
00:15:33,264 --> 00:15:34,964
LiDAR is an optimal system
to use
302
00:15:34,966 --> 00:15:36,234
because it doesn't need
its own light source.
303
00:15:36,234 --> 00:15:38,764
It can see in the dark.
304
00:15:38,769 --> 00:15:42,569
Until we land on the red planet,
305
00:15:42,573 --> 00:15:45,943
mapping lava tubes on earth
is Dr. Garry's best chance
306
00:15:45,943 --> 00:15:47,343
of understanding
their martian equivalents.
307
00:15:52,216 --> 00:15:53,684
This is a map created on one
of his previous expeditions.
308
00:15:53,684 --> 00:15:54,884
Here, we're flying through
309
00:15:54,886 --> 00:15:56,486
one of the collapse pits,
310
00:15:56,487 --> 00:15:59,017
and what we're capturing
311
00:15:59,023 --> 00:16:02,093
is the shape, the dimensions,
312
00:16:02,093 --> 00:16:04,093
the morphology of the whole
entire lava-tube system.
313
00:16:04,095 --> 00:16:05,495
But we're also capturing
the details
314
00:16:05,496 --> 00:16:07,926
of all the different textures
315
00:16:07,932 --> 00:16:11,702
that are on the inside
of the lava tube.
316
00:16:15,139 --> 00:16:19,409
Traveling to Mars
is not for the fainthearted.
317
00:16:19,410 --> 00:16:22,079
You need to be prepared for
a harsh, dynamic environment.
318
00:16:22,079 --> 00:16:25,249
Micrometeorites rain down,
319
00:16:25,249 --> 00:16:31,519
dust storms rage
for weeks at a time,
320
00:16:31,522 --> 00:16:35,422
and radiation levels are up to
250 times higher than on earth.
321
00:16:35,426 --> 00:16:39,726
Lava tubes would provide
much-needed sanctuary
322
00:16:39,730 --> 00:16:43,230
for any travelers weary of
the ferocious martian climate.
323
00:16:46,837 --> 00:16:49,637
And for those
willing to venture outside,
324
00:16:49,640 --> 00:16:52,270
the lava tubes
provide the perfect base
325
00:16:52,276 --> 00:16:54,806
to explore the rest
of the Tharsis region
326
00:16:54,812 --> 00:16:59,112
and its staggering volcanoes.
327
00:16:59,116 --> 00:17:02,686
Home to 12 volcanoes
near the martian equator
328
00:17:02,687 --> 00:17:05,687
and stretching
across 2,500 miles,
329
00:17:05,690 --> 00:17:10,528
the volcanoes here
are record-breaking --
330
00:17:10,528 --> 00:17:16,567
up to 100 times larger
than anything on earth,
331
00:17:16,567 --> 00:17:18,997
including the largest volcano in
our solar system, Olympus Mons.
332
00:17:23,441 --> 00:17:26,141
This would surely be one
of the top tourist attractions
333
00:17:26,143 --> 00:17:31,482
for any traveler visiting Mars.
334
00:17:35,319 --> 00:17:37,388
No trip is complete without
sharing these spectacular sights
335
00:17:37,388 --> 00:17:41,958
with your family and friends,
336
00:17:41,959 --> 00:17:46,529
but a postcard
wouldn't make it home to earth.
337
00:17:46,530 --> 00:17:48,399
Instead, scientists are coming
up with cutting-edge technology
338
00:17:48,399 --> 00:17:51,769
to make sure our loved ones
339
00:17:53,778 --> 00:17:56,347
never miss a moment
of our martian adventure.
340
00:18:00,552 --> 00:18:02,482
Communication to mission control
during space travel is vital.
341
00:18:02,487 --> 00:18:04,255
And for me,
it was also essential
342
00:18:04,255 --> 00:18:05,655
to stay connected to my family.
343
00:18:05,657 --> 00:18:08,257
It was on my second mission
344
00:18:08,259 --> 00:18:11,196
that I sent
the first tweet from space.
345
00:18:11,196 --> 00:18:12,864
And as we prepare
for future missions to Mars,
346
00:18:12,864 --> 00:18:15,533
what about space texting?
347
00:18:15,533 --> 00:18:18,533
Researchers are suggesting
that we try that,
348
00:18:18,536 --> 00:18:22,136
along with some
other groundbreaking methods.
349
00:18:25,176 --> 00:18:30,076
With so many stunning images,
350
00:18:30,081 --> 00:18:34,681
it's easy to forget just
how isolated Mars is from earth.
351
00:18:34,686 --> 00:18:38,423
Intrepid travelers will need a
way to keep in touch with home.
352
00:18:38,423 --> 00:18:41,153
NASA engineer Dr. Kara Beaton
is part of the team
353
00:18:41,159 --> 00:18:43,259
investigating
how future Mars explorers
354
00:18:43,261 --> 00:18:44,429
will be able to communicate.
355
00:18:44,429 --> 00:18:45,697
The shortest journey
356
00:18:45,697 --> 00:18:47,227
that you would have
for a Mars mission
357
00:18:47,232 --> 00:18:49,532
is close to three years.
358
00:18:49,534 --> 00:18:51,903
It's about six months
of transit time there,
359
00:18:51,903 --> 00:18:54,072
and then you need to wait for
about a year or year and a half
360
00:18:54,072 --> 00:18:56,202
on the surface
before you can begin
361
00:18:56,207 --> 00:18:58,007
your return journey
back to earth.
362
00:19:00,245 --> 00:19:02,575
Three years in isolation
363
00:19:02,580 --> 00:19:05,917
with a very small crew
of just a couple people
364
00:19:05,917 --> 00:19:09,287
and limited communication
with family and friends on earth
365
00:19:09,287 --> 00:19:13,787
is a big challenge that NASA
is currently looking into.
366
00:19:15,693 --> 00:19:18,793
Today,
Dr. Beaton and her colleagues
367
00:19:18,797 --> 00:19:20,927
are testing prototype
communications backpacks.
368
00:19:22,767 --> 00:19:24,235
So, because
of the very large distances
369
00:19:24,235 --> 00:19:28,035
between earth and Mars --
370
00:19:28,039 --> 00:19:31,709
anywhere from 35 million
to 225 million miles --
371
00:19:31,709 --> 00:19:36,009
there is a communication delay
between someone talking on earth
372
00:19:36,014 --> 00:19:38,244
to someone on Mars
and vice versa.
373
00:19:38,249 --> 00:19:40,118
So if I were to have
a conversation with you
374
00:19:40,118 --> 00:19:42,918
and I'm on Mars
and you're on earth
375
00:19:42,921 --> 00:19:46,051
and I speak
over a voice comm loop,
376
00:19:46,057 --> 00:19:47,287
it would take anywhere from 4
to 22 minutes to get to you,
377
00:19:47,292 --> 00:19:49,492
and then, for you to respond,
378
00:19:49,494 --> 00:19:51,863
it would take another
4 to 22 minutes
379
00:19:51,863 --> 00:19:54,663
for me to hear that response.
380
00:19:54,666 --> 00:19:56,496
By seeing
how these sorts of delays
381
00:19:56,501 --> 00:20:00,501
impact real fieldwork,
382
00:20:00,505 --> 00:20:03,635
Dr. Beaton and her team
are able to develop solutions.
383
00:20:03,641 --> 00:20:05,571
So, we've come up
with different techniques
384
00:20:05,577 --> 00:20:07,107
for how to best communicate.
385
00:20:07,111 --> 00:20:09,441
So, obviously, voice is one way,
386
00:20:09,447 --> 00:20:12,047
and certainly,
that's a viable option,
387
00:20:12,050 --> 00:20:13,680
but we've also found
that text-messaging is good
388
00:20:13,685 --> 00:20:15,315
because that allows
the crew members
389
00:20:15,320 --> 00:20:17,450
to do something else on the side
390
00:20:17,455 --> 00:20:19,385
while they're waiting
to hear a response.
391
00:20:22,093 --> 00:20:26,130
But in a real Mars mission,
392
00:20:26,130 --> 00:20:29,067
how would you actually send
and receive these messages?
393
00:20:29,067 --> 00:20:32,837
To begin,
you'll need one of these --
394
00:20:32,837 --> 00:20:35,837
a nearly 230-foot
radio telescope.
395
00:20:35,840 --> 00:20:39,210
Richard Stephenson
is a radio engineer
396
00:20:39,210 --> 00:20:41,880
here at the Canberra deep space
communication complex
397
00:20:41,880 --> 00:20:44,980
in Australia.
398
00:20:44,983 --> 00:20:48,620
The deep space network
is capable
399
00:20:48,620 --> 00:20:50,588
of sending and receiving
high-frequency radio signals
400
00:20:50,588 --> 00:20:53,958
billions of miles away,
401
00:20:53,958 --> 00:20:59,228
even to the very edges
of our solar system.
402
00:20:59,230 --> 00:21:03,130
The deep space network has three
complexes around the globe,
403
00:21:03,134 --> 00:21:07,504
and they're spaced around
about 120 degrees apart.
404
00:21:07,505 --> 00:21:10,575
So, as the earth rotates,
we can provide 24/7 coverage
405
00:21:10,575 --> 00:21:14,075
to any of the missions
that we're supporting.
406
00:21:14,078 --> 00:21:16,608
These radio dishes are
our eyes and ears on the planet,
407
00:21:16,614 --> 00:21:18,483
and any information
we get back from Mars
408
00:21:18,483 --> 00:21:20,051
is received right here.
409
00:21:20,051 --> 00:21:23,651
Well, this antenna --
410
00:21:23,655 --> 00:21:26,055
deep space station 43
is our 70-meter antenna.
411
00:21:26,057 --> 00:21:29,157
It's a very heavy-duty antenna.
412
00:21:29,160 --> 00:21:32,930
We're looking at 4,000 tons
of steerable metal.
413
00:21:32,931 --> 00:21:34,961
So regardless of wind, weather,
we can support the spacecraft
414
00:21:34,966 --> 00:21:38,936
that need
to communicate to earth.
415
00:21:38,937 --> 00:21:40,437
As we prepare to send
the first human explorers
416
00:21:40,438 --> 00:21:43,168
to the red planet,
417
00:21:43,174 --> 00:21:44,404
building up a martian
communication infrastructure
418
00:21:44,409 --> 00:21:47,839
is going to be key.
419
00:21:47,845 --> 00:21:49,675
The deep space
network's motto is
420
00:21:49,681 --> 00:21:52,681
"don't leave earth without us."
421
00:21:52,684 --> 00:21:54,914
We're the traffic control
of the solar system.
422
00:21:54,919 --> 00:21:57,219
Thanks
to radio telescopes like these,
423
00:21:57,221 --> 00:22:00,221
strategically positioned
around the globe,
424
00:22:00,224 --> 00:22:01,993
travelers to Mars won't be
isolated from everyone
425
00:22:01,993 --> 00:22:03,493
back on earth.
426
00:22:03,494 --> 00:22:06,631
If you're one of them,
427
00:22:06,631 --> 00:22:11,001
you'll be able to communicate
with your loved ones every day,
428
00:22:11,002 --> 00:22:13,972
waxing lyrical about
the epic wonders you have seen.
429
00:22:13,972 --> 00:22:18,509
These telescopes
will be the sorting offices
430
00:22:18,509 --> 00:22:22,809
for the most spectacular
postcards in the universe.
431
00:22:22,814 --> 00:22:26,984
Despite its stunning landscapes,
Mars has a dark secret,
432
00:22:26,985 --> 00:22:30,355
a history shrouded
in mystery and destruction.
433
00:22:30,355 --> 00:22:33,525
If we are ever going to plan
future expeditions to Mars,
434
00:22:35,031 --> 00:22:38,061
we've got to understand
its violent past.
435
00:22:42,338 --> 00:22:44,868
For the past 50 years,
unmanned spacecraft and rovers
436
00:22:44,874 --> 00:22:46,443
have gathered
incredible images and data
437
00:22:46,443 --> 00:22:48,311
about our elusive neighbor.
438
00:22:48,311 --> 00:22:50,079
But even though
Mars is the planet
439
00:22:50,079 --> 00:22:52,309
that we know the most about,
440
00:22:52,315 --> 00:22:54,245
there's still a lot
to understand
441
00:22:54,250 --> 00:22:58,620
before we consider living there.
442
00:23:01,524 --> 00:23:04,154
This is Orcus Patera crater.
443
00:23:09,532 --> 00:23:11,362
Nearly 250 miles long,
it dwarfs any features nearby.
444
00:23:15,472 --> 00:23:16,772
No one knows quite how
this unusual teardrop crater
445
00:23:16,773 --> 00:23:18,441
was formed.
446
00:23:21,277 --> 00:23:25,815
The latest
in a long line of mysteries,
447
00:23:25,815 --> 00:23:27,645
it will provide an intriguing
stop on any martian adventure.
448
00:23:27,650 --> 00:23:29,580
Mars has a lot of craters.
449
00:23:29,586 --> 00:23:32,616
Most of them are circular.
450
00:23:32,622 --> 00:23:33,922
You can see these craters
40 or 50 kilometers across --
451
00:23:33,923 --> 00:23:35,853
they tend to be circular.
452
00:23:35,859 --> 00:23:37,459
But there are some that are not.
453
00:23:37,460 --> 00:23:40,660
Now, if I were going to Mars,
454
00:23:40,663 --> 00:23:42,332
the one I would like to go to
the most is the whopper.
455
00:23:42,332 --> 00:23:43,932
It looks like a whale.
456
00:23:43,933 --> 00:23:45,233
In fact,
it's called Orcus Patera.
457
00:23:45,235 --> 00:23:46,635
"Orcus" means "whale."
458
00:23:46,636 --> 00:23:48,966
So, there's something odd.
459
00:23:48,972 --> 00:23:51,002
Look at all the other craters.
They're round.
460
00:23:51,007 --> 00:23:52,475
What formed this?
461
00:23:52,475 --> 00:23:54,675
Coming down.
462
00:23:54,677 --> 00:23:56,777
Until we go there ourselves,
463
00:23:56,779 --> 00:24:00,179
our best shot
at answering that question
464
00:24:00,183 --> 00:24:04,383
is to re-create the impact
here on earth,
465
00:24:04,387 --> 00:24:05,887
and professor Peter Schultz
has just the experiment.
466
00:24:05,889 --> 00:24:08,889
Going back.
467
00:24:08,892 --> 00:24:10,092
This is the NASA
Ames vertical gun range,
468
00:24:10,093 --> 00:24:13,123
a unique facility
469
00:24:13,129 --> 00:24:14,998
that simulates high-speed
celestial body impacts
470
00:24:14,998 --> 00:24:17,367
on a small scale.
471
00:24:19,135 --> 00:24:22,335
Today, professor Schultz
472
00:24:22,338 --> 00:24:24,807
is trying to re-create
the Orcus Patera crater.
473
00:24:28,645 --> 00:24:31,275
This is a case of trying
to simulate what happens
474
00:24:31,281 --> 00:24:34,511
when you have
a giant projectile --
475
00:24:34,517 --> 00:24:36,247
an asteroid or even a moon --
collide with Mars.
476
00:24:36,252 --> 00:24:38,652
So, we're gonna try that here.
477
00:24:38,655 --> 00:24:42,855
The target sits
478
00:24:42,859 --> 00:24:44,389
inside a large pressure-
controlled impact chamber.
479
00:24:44,394 --> 00:24:46,262
So, at the chamber,
480
00:24:46,262 --> 00:24:47,962
we can control
the atmospheric conditions.
481
00:24:47,964 --> 00:24:50,594
And we have a projectile
482
00:24:50,600 --> 00:24:52,030
that will be launched
to go through this hole,
483
00:24:52,035 --> 00:24:56,435
this launch tube,
484
00:24:56,439 --> 00:25:00,439
maybe about eight times the
velocity of a speeding bullet.
485
00:25:00,443 --> 00:25:02,412
So now all we have to do
is really lock and load.
486
00:25:04,180 --> 00:25:08,050
Professor Schultz
has rigged the gun
487
00:25:08,051 --> 00:25:11,421
so that it fires at just
15 degrees from the horizontal,
488
00:25:11,421 --> 00:25:13,289
simulating
an oblique meteor strike.
489
00:25:13,289 --> 00:25:16,359
With everything in place,
490
00:25:16,359 --> 00:25:18,089
the final step
is to fire the projectile.
491
00:25:24,567 --> 00:25:27,136
Rolling.
492
00:25:28,338 --> 00:25:30,006
Oh, good!
493
00:25:30,006 --> 00:25:31,336
We got it, we got it,
we got it, we got it.
494
00:25:31,341 --> 00:25:33,441
Let me see, let me see,
let me see.
495
00:25:33,443 --> 00:25:34,643
5.60 kilometers per second.
496
00:25:34,644 --> 00:25:35,644
Well done, sir.
497
00:25:41,784 --> 00:25:43,784
Whoa!
498
00:25:43,786 --> 00:25:46,316
It looks like it worked.
499
00:25:46,322 --> 00:25:47,690
So, instead of getting
a round crater,
500
00:25:47,690 --> 00:25:49,258
we have an oblong crater,
501
00:25:49,258 --> 00:25:52,595
and we have an oblong crater
502
00:25:52,595 --> 00:25:57,665
that has multiple impacts
downrange.
503
00:25:57,667 --> 00:26:01,537
There's a really low rim here,
high rim there, and a shelf.
504
00:26:01,537 --> 00:26:03,667
And it requires
a very low-angle impact,
505
00:26:03,673 --> 00:26:06,803
and I think
that's what's happened on Mars.
506
00:26:10,480 --> 00:26:14,017
The crater is almost
a mirror image of Orcus Patera,
507
00:26:14,017 --> 00:26:18,855
scoured lengthways
across the landscape.
508
00:26:18,855 --> 00:26:20,755
And professor Schultz has
a theory for how it was formed.
509
00:26:23,793 --> 00:26:26,093
A moon going around Mars
is in an orbit,
510
00:26:26,095 --> 00:26:28,364
and eventually,
that orbit decays,
511
00:26:28,364 --> 00:26:31,901
gets closer and closer to Mars.
512
00:26:31,901 --> 00:26:33,331
In fact, the moon Phobos
going around Mars right now
513
00:26:33,336 --> 00:26:36,636
will collide with Mars
514
00:26:36,639 --> 00:26:37,769
in something like 28 million,
maybe 30 million years.
515
00:26:37,774 --> 00:26:40,504
So, when that happens,
516
00:26:40,510 --> 00:26:44,347
it'll come in
at an extremely low angle,
517
00:26:44,347 --> 00:26:46,677
grazing, just like a spacecraft
trying to come in for a landing,
518
00:26:46,683 --> 00:26:47,883
except it's not gonna land
so well.
519
00:26:47,884 --> 00:26:50,784
It's gonna collide
520
00:26:50,787 --> 00:26:55,487
and form a crater
very similar to Orcus Patera.
521
00:26:55,491 --> 00:26:57,721
Mars has
two potato-shaped moons --
522
00:26:57,727 --> 00:26:59,657
Phobos and Deimos.
523
00:26:59,662 --> 00:27:04,801
But Peter's audacious thought
524
00:27:04,801 --> 00:27:09,101
is that there was once another
lost moon orbiting the planet.
525
00:27:09,105 --> 00:27:11,274
The theory makes sense,
but the jury remains out.
526
00:27:15,044 --> 00:27:18,014
Situated close to some
of Mars' largest volcanoes,
527
00:27:18,014 --> 00:27:19,714
other scientists argue
that volcanic forces
528
00:27:19,716 --> 00:27:22,585
could have created the crater
529
00:27:22,585 --> 00:27:25,015
by stretching and compressing
the ground.
530
00:27:28,191 --> 00:27:30,191
If we are to discover
the crater's true origins,
531
00:27:30,193 --> 00:27:33,262
we must go there ourselves,
532
00:27:33,262 --> 00:27:36,362
because it's only
by studying landscapes up close
533
00:27:36,365 --> 00:27:39,702
that we can
fully understand them.
534
00:27:39,702 --> 00:27:43,202
Imagine
standing atop the crater rim
535
00:27:43,206 --> 00:27:47,243
rising a mile
above the surrounding plains,
536
00:27:47,243 --> 00:27:50,780
looking into the depths
of the crater below.
537
00:27:50,780 --> 00:27:53,680
What an incredible
and enigmatic stop
538
00:27:53,683 --> 00:27:57,283
on your adventure across Mars.
539
00:27:57,286 --> 00:28:01,186
Just like preparing
for a trip to a foreign land,
540
00:28:01,190 --> 00:28:04,527
smart packing
will be a must for Mars.
541
00:28:04,527 --> 00:28:08,797
So what should
you fill your suitcase with?
542
00:28:10,358 --> 00:28:13,688
For starters, you may want
to bring a winter coat.
543
00:28:17,865 --> 00:28:19,333
Mars is nicknamed the red planet
because of its crimson color.
544
00:28:19,333 --> 00:28:21,933
But take a closer look,
545
00:28:21,936 --> 00:28:24,736
and you'll see
beautiful white swirls.
546
00:28:24,739 --> 00:28:27,539
Learning more about
these mysterious white ribbons
547
00:28:27,542 --> 00:28:30,042
may unlock the secrets
of how Mars formed
548
00:28:30,044 --> 00:28:32,144
and where it's headed.
549
00:28:34,582 --> 00:28:36,751
Your ultimate
travel guide to Mars
550
00:28:36,751 --> 00:28:39,981
includes marvelous canyons,
551
00:28:39,987 --> 00:28:42,417
the most spectacular volcanoes
in the solar system,
552
00:28:42,423 --> 00:28:43,723
and even underground caves.
553
00:28:43,724 --> 00:28:46,894
But there's no better place
554
00:28:46,894 --> 00:28:49,664
to explore the mysterious
martian landscapes
555
00:28:49,664 --> 00:28:51,732
than at the southernmost reaches
of the planet.
556
00:28:51,732 --> 00:28:56,632
It may be
well off the beaten track,
557
00:28:56,637 --> 00:28:59,367
but the extra effort required
to get there will be worthwhile.
558
00:28:59,373 --> 00:29:02,210
This is
Mars' Southern polar cap,
559
00:29:02,210 --> 00:29:07,310
one of the coldest places
on the planet.
560
00:29:07,315 --> 00:29:08,983
Temperatures here can drop below
minus-248 degrees Fahrenheit.
561
00:29:08,983 --> 00:29:11,913
It's an icy destination
562
00:29:11,919 --> 00:29:14,589
that planetary scientist
Dr. Meg Schwamb
563
00:29:14,589 --> 00:29:17,019
has long held a fascination.
564
00:29:17,024 --> 00:29:18,654
So, we're standing
on a dormant volcano
565
00:29:18,659 --> 00:29:19,927
on the big island of Hawaii.
566
00:29:19,927 --> 00:29:21,657
And so, this is where we have
567
00:29:21,662 --> 00:29:23,292
some of
the world-class telescopes
568
00:29:26,300 --> 00:29:29,570
that are observing
the night sky.
569
00:29:29,570 --> 00:29:33,240
So, I'm really interested
in the south pole of Mars,
570
00:29:33,241 --> 00:29:34,871
and so how that can tell us
more about Mars' past
571
00:29:34,876 --> 00:29:37,044
and its current history.
572
00:29:39,714 --> 00:29:44,614
On a clear night,
the poles of Mars
573
00:29:44,619 --> 00:29:46,519
can even be seen through small
telescopes from here on earth.
574
00:29:48,656 --> 00:29:52,556
Amateur images like these
575
00:29:52,560 --> 00:29:55,830
show the bright ice caps against
the red disk of the planet,
576
00:29:55,830 --> 00:29:59,930
but their true wonder
is only truly revealed
577
00:29:59,934 --> 00:30:05,204
with images taken from orbit.
578
00:30:05,206 --> 00:30:08,406
At over 248 miles wide
and almost 2 miles thick,
579
00:30:08,409 --> 00:30:13,009
the Southern polar cap
is a freezing vision
580
00:30:13,014 --> 00:30:16,751
of swirling white on an
otherwise rusty-colored planet.
581
00:30:16,751 --> 00:30:19,581
Though it may look much like
the south pole on earth,
582
00:30:19,587 --> 00:30:21,055
it has one crucial difference.
583
00:30:21,055 --> 00:30:22,585
So, as you can see behind me,
584
00:30:22,590 --> 00:30:24,659
there's some white
dotting the surface,
585
00:30:24,659 --> 00:30:26,789
and that's actually some snow
left after
586
00:30:26,794 --> 00:30:28,994
from one
of our recent snowfalls.
587
00:30:28,996 --> 00:30:32,166
But on Mars, in the south pole,
588
00:30:32,166 --> 00:30:34,435
there isn't water ice
that's exposed, or snow.
589
00:30:34,435 --> 00:30:37,004
It actually snows
carbon dioxide.
590
00:30:37,004 --> 00:30:40,141
Often referred to as dry ice,
591
00:30:40,141 --> 00:30:42,910
in the martian winter,
this frozen carbon dioxide
592
00:30:42,910 --> 00:30:47,880
blankets the Southern reaches
of the planet.
593
00:30:47,882 --> 00:30:50,012
Come spring, when it melts, it
transforms straight into a gas,
594
00:30:50,017 --> 00:30:52,717
dramatically changing
the landscape
595
00:30:52,720 --> 00:30:54,920
and creating
a remarkable phenomenon.
596
00:30:54,922 --> 00:30:59,192
So, what happens
on the south pole of Mars
597
00:30:59,193 --> 00:31:00,793
is that you have this layer
of semitranslucent ice
598
00:31:00,795 --> 00:31:03,965
on top of the dirt,
599
00:31:03,965 --> 00:31:07,635
and when the sun comes up
in the spring and summer,
600
00:31:07,635 --> 00:31:09,303
the sunlight penetrates through
down to that dirt layer
601
00:31:09,303 --> 00:31:12,940
and heats up.
602
00:31:12,940 --> 00:31:14,440
Because it's warm, the carbon
dioxide ice in contact with it
603
00:31:14,442 --> 00:31:16,842
starts to turn into gas.
604
00:31:16,844 --> 00:31:19,244
And so now you have
a layer of gas
605
00:31:19,246 --> 00:31:23,446
trapped
underneath a layer of ice.
606
00:31:23,451 --> 00:31:26,581
The consequences of
this thaw are quite spectacular.
607
00:31:26,587 --> 00:31:29,557
So, when this gas is trapped
underneath this ice sheet,
608
00:31:29,557 --> 00:31:33,027
it breaks through in any way
it can through the ice.
609
00:31:33,027 --> 00:31:35,627
And when it gets to the surface,
it creates these jets or geysers
610
00:31:35,629 --> 00:31:38,299
on the surface
of the south pole of Mars.
611
00:31:38,299 --> 00:31:39,799
Gas is rushing out
maybe a few meters --
612
00:31:39,800 --> 00:31:44,170
not much further, we think.
613
00:31:44,171 --> 00:31:46,471
But it brings up this dust and
dirt from below that ice sheet.
614
00:31:46,474 --> 00:31:49,474
If I was standing
on the surface of Mars,
615
00:31:49,477 --> 00:31:50,945
you'd see these sort of
dark jets coming up,
616
00:31:50,945 --> 00:31:54,715
and it's the local surface winds
617
00:31:54,715 --> 00:31:57,685
that blow these material
into these dark streaks.
618
00:31:57,685 --> 00:31:59,785
And then, when there's
no more carbon dioxide ice,
619
00:31:59,787 --> 00:32:01,517
it disappears.
620
00:32:01,522 --> 00:32:05,492
Seen from space,
621
00:32:05,493 --> 00:32:08,493
this windblown dust
creates breathtaking landscapes.
622
00:32:08,496 --> 00:32:12,096
But these images
aren't simply pretty.
623
00:32:12,099 --> 00:32:15,969
They tell us
about the martian climate, too.
624
00:32:15,970 --> 00:32:20,170
If we can study how
these geysers form, these jets,
625
00:32:20,174 --> 00:32:23,174
and how the wind
sort of blows these material,
626
00:32:23,177 --> 00:32:24,977
we can learn more
about the martian atmosphere.
627
00:32:24,979 --> 00:32:27,879
This process
is completely alien.
628
00:32:27,882 --> 00:32:31,312
We don't have anything like this
on earth.
629
00:32:34,522 --> 00:32:37,922
These features
disappear each year,
630
00:32:37,925 --> 00:32:40,455
but they leave behind
another wonder in their wake --
631
00:32:40,461 --> 00:32:42,991
the real spiders from Mars.
632
00:32:42,997 --> 00:32:46,867
If we look a little deeper
into these images,
633
00:32:46,867 --> 00:32:48,667
what we find, that when there's
no carbon dioxide ice anymore,
634
00:32:48,669 --> 00:32:50,469
the fans go away.
635
00:32:50,471 --> 00:32:54,071
And what's left
in many of these areas
636
00:32:54,075 --> 00:32:56,805
are these kind of dendritic,
like, spider-like features,
637
00:32:56,811 --> 00:32:58,411
which actually has been
informally dubbed spiders,
638
00:32:58,412 --> 00:33:01,342
or aranea forms.
639
00:33:04,718 --> 00:33:08,188
These erosion channels
meet in a central pit
640
00:33:08,189 --> 00:33:11,289
resembling the body
and long legs of a spider,
641
00:33:11,292 --> 00:33:16,262
legs that can stretch
for hundreds of miles
642
00:33:16,263 --> 00:33:19,263
and can take more than
1,000 martian years to grow.
643
00:33:19,266 --> 00:33:20,634
Explorers lucky enough
to stand at the south pole
644
00:33:20,634 --> 00:33:24,134
during a martian summer
645
00:33:24,138 --> 00:33:26,738
would gaze upon these
alien spider-like features
646
00:33:26,740 --> 00:33:29,740
stretching across the landscape.
647
00:33:29,743 --> 00:33:31,212
They would be offered
a taste of martian weather
648
00:33:31,212 --> 00:33:34,812
and witness the dramatic proof
649
00:33:34,815 --> 00:33:37,445
that Mars is far from
the dead and unchanging planet
650
00:33:37,451 --> 00:33:41,188
that many people assumed.
651
00:33:41,188 --> 00:33:46,258
Mars' icy poles
provide some respite
652
00:33:46,260 --> 00:33:48,690
from the desert landscapes
that cover most of the planet.
653
00:33:48,696 --> 00:33:52,533
And the more adventurous
traveler
654
00:33:52,533 --> 00:33:54,602
may also choose to follow the
elusive trail of liquid water
655
00:33:54,602 --> 00:33:58,339
on the martian surface.
656
00:33:58,339 --> 00:34:00,169
In doing so, they will uncover
the hidden story
657
00:34:00,174 --> 00:34:04,111
of ancient Mars.
658
00:34:04,111 --> 00:34:06,080
Thanks to the curiosity rover,
659
00:34:06,080 --> 00:34:09,280
we now know that Gale crater
660
00:34:09,283 --> 00:34:11,652
was once the site
of an ancient lake.
661
00:34:11,652 --> 00:34:16,522
But where did all the water go?
662
00:34:16,524 --> 00:34:18,654
And how did it shape
the landscape we see today?
663
00:34:18,659 --> 00:34:22,659
To see that, Dr. Gupta
664
00:34:22,663 --> 00:34:26,600
needs to look at Gale crater
3.8 billion years ago,
665
00:34:26,600 --> 00:34:29,170
just after it was formed
by a meteor impact.
666
00:34:30,838 --> 00:34:32,968
So, this is really cool here.
667
00:34:32,973 --> 00:34:36,773
We've got
an augmented reality sandbox,
668
00:34:36,777 --> 00:34:38,707
and so what I'm doing now is,
I'm creating the crater rim.
669
00:34:38,712 --> 00:34:40,542
So, there would have been
a mountain
670
00:34:40,548 --> 00:34:43,617
in the center of the crater
671
00:34:43,617 --> 00:34:46,487
formed
during that impact process.
672
00:34:46,487 --> 00:34:48,556
That forms
the core of mount sharp.
673
00:34:48,556 --> 00:34:52,326
When Gale crater first formed,
674
00:34:52,326 --> 00:34:56,696
it's thought Mars had a much
more substantial atmosphere,
675
00:34:56,697 --> 00:34:59,297
making the planet warmer and,
therefore, wetter than today.
676
00:34:59,300 --> 00:35:01,630
And the water fell across
the planet's surface
677
00:35:01,635 --> 00:35:04,035
as rain and snow.
678
00:35:04,038 --> 00:35:07,338
We've got rain forming
on the crater rim
679
00:35:07,341 --> 00:35:09,710
and then gushing out
into the center of Gale crater
680
00:35:09,710 --> 00:35:11,679
and building up.
681
00:35:11,679 --> 00:35:15,679
As it poured down
into the crater,
682
00:35:15,683 --> 00:35:17,952
its water shaped many
of the features we see today.
683
00:35:20,054 --> 00:35:22,554
Imagine,
if you have heavy rainfall,
684
00:35:22,556 --> 00:35:24,586
rainfall over hundreds of years,
685
00:35:24,592 --> 00:35:26,992
the landscape
gets progressively eroded
686
00:35:26,994 --> 00:35:30,364
and carves
deep canyons and valleys.
687
00:35:30,364 --> 00:35:33,194
The sediment
eroded from those gullies
688
00:35:33,200 --> 00:35:36,100
would have washed
into Gale crater,
689
00:35:36,103 --> 00:35:38,372
forming those river deposits
that we can see so beautifully
690
00:35:38,372 --> 00:35:41,002
in the images
that curiosity takes.
691
00:35:41,008 --> 00:35:45,546
And then the climate changed.
692
00:35:45,546 --> 00:35:47,915
It lost its atmosphere
and became arid and hyper-cold,
693
00:35:47,915 --> 00:35:53,385
and all that water evaporated.
694
00:35:53,387 --> 00:35:57,257
And we were left with a crater
infilled with sediment.
695
00:35:57,258 --> 00:36:00,358
The rusty,
ancient surface of Mars
696
00:36:00,361 --> 00:36:05,631
has enigmatic landscapes
at every turn,
697
00:36:05,633 --> 00:36:08,463
from towering sculpted peaks
to hidden underground caverns.
698
00:36:08,469 --> 00:36:11,538
And if you are one
of the first explorers,
699
00:36:11,538 --> 00:36:16,377
you will need to study
every detail.
700
00:36:16,377 --> 00:36:18,577
Each landmark holds its own
clues to Mars' mysteries,
701
00:36:18,579 --> 00:36:23,249
and there is no greater mystery
702
00:36:23,250 --> 00:36:25,780
than whether life exists
beyond the earth.
703
00:36:25,786 --> 00:36:29,486
As a stranger from earth,
704
00:36:31,151 --> 00:36:34,181
will you be greeted
by martian life when you arrive?
705
00:36:36,290 --> 00:36:38,390
When people meet me
for the first time,
706
00:36:38,392 --> 00:36:40,822
the question
I get asked the most is,
707
00:36:40,827 --> 00:36:42,857
"is there life
somewhere else in the universe?"
708
00:36:42,863 --> 00:36:46,500
And while I don't know for sure,
709
00:36:46,500 --> 00:36:48,569
I love the possibility that life
could exist on other planets.
710
00:36:48,569 --> 00:36:51,738
So how do we find this life,
711
00:36:51,738 --> 00:36:56,338
whether it be past,
present, or future?
712
00:36:56,343 --> 00:36:59,173
There's one scientist that says
the proof is in the salt.
713
00:37:02,082 --> 00:37:03,650
To stand a chance
of finding life on Mars,
714
00:37:03,650 --> 00:37:05,250
it's thought travelers will need
715
00:37:05,252 --> 00:37:07,882
to journey
to a region of the planet
716
00:37:07,888 --> 00:37:10,588
unexplored by landers or rovers.
717
00:37:10,591 --> 00:37:13,521
Perched in the remote
Southern highlands,
718
00:37:13,527 --> 00:37:16,827
Terra Sirenum
is a land of cratered terrain
719
00:37:16,830 --> 00:37:20,467
capped in crystalline
mineral deposits.
720
00:37:20,467 --> 00:37:24,805
It's thought that if we're going
to find signs of local wildlife,
721
00:37:24,805 --> 00:37:26,873
past or present,
then this will be the best spot.
722
00:37:28,842 --> 00:37:32,112
Of all the questions
astrobiology asks,
723
00:37:32,112 --> 00:37:36,182
probably its biggest one is,
is there life beyond the earth?
724
00:37:36,183 --> 00:37:37,983
When we're assessing
whether a planet is habitable,
725
00:37:37,985 --> 00:37:39,315
we're looking
for some basic things.
726
00:37:39,319 --> 00:37:41,719
We need some liquid water
727
00:37:41,722 --> 00:37:45,292
for all those chemical reactions
to happen in,
728
00:37:45,292 --> 00:37:46,922
we need a source of energy, like
sunlight or chemical energy,
729
00:37:46,927 --> 00:37:49,157
and we also need
some basic elements
730
00:37:49,162 --> 00:37:51,592
like carbon and phosphorus.
731
00:37:51,598 --> 00:37:55,768
All those things have
to come together in one place
732
00:37:55,769 --> 00:37:58,099
for life as we know it,
at least, to be able to grow.
733
00:38:01,508 --> 00:38:03,276
Before our first
spacecraft arrived in the 1960s,
734
00:38:03,276 --> 00:38:05,776
the idea of visitors to Mars
735
00:38:05,779 --> 00:38:08,579
setting foot
on a lush, living planet
736
00:38:08,582 --> 00:38:10,412
seemed like
a perfectly reasonable idea.
737
00:38:10,417 --> 00:38:13,247
In the early history of Mars,
738
00:38:13,253 --> 00:38:15,322
the planet would have looked
quite a lot like early earth.
739
00:38:15,322 --> 00:38:17,391
There would have been
liquid water on the surface.
740
00:38:17,391 --> 00:38:19,391
Maybe it would have been warmer.
741
00:38:19,393 --> 00:38:21,893
Perhaps during
that period of time,
742
00:38:21,895 --> 00:38:26,565
it could have sustained biology.
743
00:38:26,566 --> 00:38:28,966
But about 3 1/2 billion years
ago, that water froze up,
744
00:38:28,969 --> 00:38:30,799
and the planet
become what we know today --
745
00:38:30,804 --> 00:38:34,141
pretty much a desert world.
746
00:38:34,141 --> 00:38:37,041
Because of that,
it was never able
747
00:38:37,044 --> 00:38:38,674
to sustain the sort
of evolutionary development
748
00:38:38,679 --> 00:38:41,448
that you can see
around you here.
749
00:38:45,118 --> 00:38:49,288
So we need to look
in places on Mars and on earth
750
00:38:49,289 --> 00:38:50,619
that could give primitive life
a fighting chance.
751
00:38:50,624 --> 00:38:53,193
There are two types of places.
752
00:38:53,193 --> 00:38:55,023
We might look
in briny, salty solutions.
753
00:38:55,028 --> 00:38:57,128
Those brines
could still be liquid
754
00:38:57,130 --> 00:38:59,199
on the surface of Mars today.
755
00:38:59,199 --> 00:39:00,567
And we're looking
at ancient salt deposits.
756
00:39:00,567 --> 00:39:03,497
In those salts,
757
00:39:03,503 --> 00:39:05,872
maybe we might try and look
for signs of past life.
758
00:39:07,541 --> 00:39:10,441
With that in mind,
759
00:39:10,444 --> 00:39:14,114
astrobiologists
like professor Cockell
760
00:39:14,114 --> 00:39:17,451
started searching for the
perfect spot to hunt for life.
761
00:39:20,587 --> 00:39:25,287
And in time,
images taken from orbit
762
00:39:25,292 --> 00:39:27,622
revealed more than 200 places
in the Terra Sirenum region
763
00:39:27,627 --> 00:39:30,797
where thick salt layers exist.
764
00:39:32,999 --> 00:39:37,299
The Terra Sirenum region of Mars
765
00:39:37,304 --> 00:39:39,134
has salt deposits
from ancient ponds and lakes
766
00:39:39,139 --> 00:39:41,839
that essentially evaporated --
767
00:39:41,842 --> 00:39:43,510
the last remnants
of liquid water on Mars.
768
00:39:45,645 --> 00:39:49,583
And these salts in Terra Sirenum
769
00:39:49,583 --> 00:39:52,413
could preserve or record
the existence of life on Mars.
770
00:39:52,419 --> 00:39:53,887
And to support this theory,
professor Cockell
771
00:39:53,887 --> 00:39:57,587
has been investigating some
772
00:39:57,591 --> 00:40:00,560
of the most remote and
inhospitable places on earth.
773
00:40:00,560 --> 00:40:03,660
So, here we've got some samples
from the Negev desert.
774
00:40:03,663 --> 00:40:07,533
Microbes that live in those
environments are very tolerant
775
00:40:07,534 --> 00:40:10,234
of both high temperatures
and extreme dryness.
776
00:40:10,237 --> 00:40:12,737
And then, these microbes
are from a lake in Canada
777
00:40:12,739 --> 00:40:16,609
that has very high
concentrations of sulfate,
778
00:40:16,610 --> 00:40:20,310
similar to the sorts of salts
that we find on Mars.
779
00:40:20,313 --> 00:40:21,782
Finding living
bacteria in places like this
780
00:40:21,782 --> 00:40:25,852
tells Cockell and his team
781
00:40:25,852 --> 00:40:28,352
that Mars-like environments
here on earth can support life.
782
00:40:28,355 --> 00:40:30,985
But that's
only half the picture.
783
00:40:30,991 --> 00:40:35,128
So, this is a sample
from a very extreme environment.
784
00:40:35,128 --> 00:40:36,628
It comes from a kilometer
underground in a salt mine.
785
00:40:36,630 --> 00:40:39,030
This is the sort of sample
786
00:40:39,032 --> 00:40:41,802
you might be able
to find in Terra Sirenum
787
00:40:41,802 --> 00:40:44,802
if you dug
down beneath the surface.
788
00:40:44,805 --> 00:40:48,905
The question is,
could these microbes
789
00:40:48,909 --> 00:40:50,609
also survive under the
conditions on present-day Mars?
790
00:40:50,610 --> 00:40:54,410
We've subjected these microbes
791
00:40:54,414 --> 00:40:57,344
to similar sorts of environments
that you might find on Mars,
792
00:40:57,350 --> 00:40:59,820
so no oxygen,
very low amounts of energy,
793
00:40:59,820 --> 00:41:02,120
very low concentrations
of nutrients.
794
00:41:02,122 --> 00:41:05,759
And in those sorts
of environments,
795
00:41:05,759 --> 00:41:07,489
these microbes can not only
survive -- they can also grow.
796
00:41:07,494 --> 00:41:10,063
What these results show us
797
00:41:10,063 --> 00:41:12,263
is that some of
these salty environments on Mars
798
00:41:12,265 --> 00:41:13,765
may well have been habitable.
799
00:41:13,767 --> 00:41:17,837
It may not look like much,
800
00:41:17,838 --> 00:41:21,538
but this is the closest thing
to life on Mars anyone has seen.
801
00:41:21,541 --> 00:41:23,771
I often joke that
if you send me to Terra Sirenum
802
00:41:23,777 --> 00:41:25,907
with a microscope and a shovel,
803
00:41:25,912 --> 00:41:28,112
I can tell you
within a few hours
804
00:41:28,114 --> 00:41:30,644
whether there's life on Mars.
805
00:41:30,650 --> 00:41:33,520
Astrobiologists
like professor Cockell
806
00:41:33,520 --> 00:41:35,720
are building a case
that the salt plains on Mars
807
00:41:35,722 --> 00:41:38,652
are potentially habitable.
808
00:41:38,658 --> 00:41:41,188
The inquisitive traveler
prepared to dig deep
809
00:41:41,194 --> 00:41:44,194
might just find
some of the local wildlife
810
00:41:44,197 --> 00:41:47,867
sheltered
beneath the subsurface.
811
00:41:47,868 --> 00:41:49,468
It would be the discovery
of the century
812
00:41:49,469 --> 00:41:54,139
and proof that life probably exist
elsewhere
813
00:41:54,140 --> 00:41:55,721
in the universe too,
814
00:41:56,297 --> 00:42:00,721
and it would be the perfect end
to an epic journey.
61393
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