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NARRATOR: Everyone likes a vacation
in a warm climate,
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but how about a trip to two planets
that are as hot as hell?
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MAN: If you were walking
on the surface of Mercury
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you would need
one heck of a spacesuit.
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NARRATOR: Mysterious Mercury
appears lifeless and desolate.
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But hidden deep inside
is a clue to a different past.
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MAN: The smallest planet
made out of the densest stuff,
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with the most lunar-like
landscape at its surface.
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And yet generating
a magnetic field.
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NARRATOR: But it's nearby Venus,
goddess of love,
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who will really melt your heart
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and crush your defenses
at the same time.
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MAN: So this is a hell.
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Real hell!
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NARRATOR: Once the twin of Earth,
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something went wrong here,
terribly wrong.
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WOMAN: At some point Venus
had an ocean's worth of water
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that is now gone.
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NARRATOR: What turned Venus
from paradise to pressure cooker?
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Could this really be our future?
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MAN: The ultimate fate of the Earth
is to look like Venus looks today.
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NARRATOR: And here,
on our own doorstep,
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there is possibly the greatest
survival story of all.
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MAN: There is some speculation
that Venus might actually still harbor life,
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even though it is
such a hostile place.
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NARRATOR: There has never been
a better time
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to boldly go where
no human has gone before.
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To follow in the footsteps
of our robot pioneers
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and visit the planets
of the solar system.
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MAN: T minus 40 seconds.
Everything looks good for launch.
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NARRATOR: Ever wanted to be
an astronaut?
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Imagine it was you
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who was heading to the Hot Zone
of the two inner planets.
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Where would you go?
What would you see?
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And how would you survive?
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The latest robotic missions
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have revealed more about these worlds
than ever before.
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Armed with this new knowledge,
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think of this as your personal
travel guide to our near neighbors.
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NARRATOR: As the planet
closest to the sun,
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Mercury is the ultimate
summer vacation.
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Step out of your spacecraft
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and sizzling temperatures
are guaranteed...
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for a day that lasts three months.
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And when the sun finally does set,
the nightlife begins--
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with a unique cosmic light show.
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This is one pockmarked planet
worth taking a closer look at.
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Like our moon, Mercury
is covered in craters.
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BRETT DENEVI: You can't look
at the moon or Mercury
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without seeing impact craters.
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NARRATOR: It's a good thing
Brett Denevi loves a big impact.
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As a member of the imaging team
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on the current Messenger Mission
to Mercury,
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she sees a lot of them.
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DENEVI: What's exciting for me
is | get to be one of the first people
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to see these images of places on the planet
that we've never seen before.
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NARRATOR: Most people come here
to Meteor Crater in Arizona
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to see a big hole in the ground.
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Brett's desires run deeper.
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DENEVI: If you want to study
impact craters on Mercury,
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this is the best place to come.
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| mean, this is the most well preserved
impact crater on Earth.
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It's the closest you're going to get.
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NARRATOR: Wonder what it would be like
to take a stroll on Mercury?
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You can walk around Meteor Crater
in about an hour.
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But on Mercury you wouldn't know
when to stop.
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Craters here stretch
as far as the eye can see.
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MAN: Apollo 11, this is Houston.
Radio check, over.
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NARRATOR: Although no human
has ever set foot on Mercury,
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we have a pretty good idea
of what you would see.
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MAN: We copy you down, Eagle.
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SEAN SOLOMON: If you were walking around
on the surface of Mercury,
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it would look, outwardly,
a lot like the moon.
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NARRATOR: When you step
onto Mercury,
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you step into a world
with no real atmosphere;
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where the sky is as black as night
and ablaze in sunshine.
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And where a drive is an off-road trek
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through at least
a three-billion-year-old battlefield.
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DENEVI: Big craters, small craters,
craters everywhere.
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So that's your first impression
looking at it.
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NARRATOR: Like the moon,
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Mercury took most
of its battering early on.
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A silent witness
to the dawn of time,
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it's been undisturbed
by a single drop of rain
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or breath of wind ever since.
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DAVID PAIGE: For the most part
the surface of Mercury
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has been frozen in time for periods
of billions of years.
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And you may say, "That's boring,"
but not necessarily.
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It's a good thing
because these planets
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such as Mercury and the moon
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preserve a record of what was going on
during this critical early period
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of the solar system's formation.
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And so we can basically study it there,
because it's laying right on the surface.
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NARRATOR: Every stone and crater
of this pockmarked world
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has the potential to gaze back
4.5 billion years.
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But counting these craters
is just the first challenge
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when it comes to revealing
a planet like Mercury.
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DENEVI: It's always
low on the horizon
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so it's hard to point a telescope
at it from Earth.
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It's hard to get into orbit
around Mercury
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because it's so close to the sun.
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NARRATOR: For that reason,
Mercury remains
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one of the most underexplored
planets in our solar system.
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Many aspects, like its geological past,
are a mystery.
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But some things we do know:
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this lonely planet has
a strange sense of keeping time.
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NARRATOR: Once you arrive,
you'll have to reset your watch
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for a time zone like no other.
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DENEVI: It has such an unusual orbit
and rotation period,
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the days and nights
are very strange.
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NARRATOR: A Mercurian year
is just 88 Earth days long,
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thanks to its quick sprint
around the sun.
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But it rotates so slowly,
a single day takes much longer.
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DENEVI: The day on Mercury is
more like half a year on Earth's terms.
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NARRATOR: Although known to us
since ancient times,
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for thousands of years
we had little idea
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what the planet
really looked like.
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NARRATOR: Then, in 1974,
NASA's Mariner 10 sends back
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the first ever glimpses
of its surface.
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NEWSREEL NARRATOR: Pictures
can be transmitted to tracking stations
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and on to the Jet Propulsion Laboratory
in California.
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MARK ROBINSON: Due to Mercury's
slow rotation
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and its elliptical orbit around the sun,
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when it flew by three times
it saw the same half of the planet.
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So we've really only seen
something like 45% of the planet
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at relatively low resolution.
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NARRATOR: Hidden in these fuzzy
black and white postcards
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for over 30 years
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are clues that point to one
of Mercury's biggest puzzles:
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it's been shrinking.
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ROBINSON: Mercury doesn't have
plate tectonics like the Earth does.
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So we know that Mercury's crust
is under a lot of compression.
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00:09:03,443 --> 00:09:08,481
And the only way you can really
do that is if the planet shrank.
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And so you can think of it
as the Incredible Shrinking Planet.
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NARRATOR: As Mariner 10 flies past,
the mystery deepens.
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The spacecraft detects
a vast iron core hidden inside.
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DENEVI: Mercury's core makes up
about 60% of the planet by mass.
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It's about twice as big as Earth's.
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Why would it have such a huge core
for such a small planet?
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00:09:36,943 --> 00:09:39,712
Some people think
there was a huge impact...
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that kind of stripped off
a lot of the planet.
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And now what we're seeing
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is just the remnant
of a once bigger planet.
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NARRATOR: Many questions
about Mercury remain unanswered,
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questions a new mission
will hopefully solve.
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00:10:06,106 --> 00:10:10,210
MAN: Five, four, three,
main engine start,
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two, one and zero,
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00:10:12,579 --> 00:10:17,784
and liftoff of Messenger
on NASA's mission to Mercury.
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NARRATOR: NASA's Messenger spacecraft
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will become the first probe
to orbit Mercury.
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SOLOMON: Getting a spacecraft
into orbit around Mercury
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is difficult for two reasons:
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the sun and the sun.
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The sun as a source of heat
and the sun as a source of gravity.
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NARRATOR: To sneak past the sun,
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Messenger is taking a convoluted route,
flying past the Earth once,
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Venus twice and
Mercury itself three times,
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to arrive in fulltime orbit by 2011.
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ROBINSON: When you get into orbit
you can end up mapping the whole planet
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at fairly high resolution.
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So we will start having
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00:11:07,500 --> 00:11:10,303
a mature and fundamental
understanding of Mercury,
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not only its surface,
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but its whole chemistry
throughout the whole planet.
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From that we can unravel,
to some degree, how it formed.
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NARRATOR: What other secrets
are etched into Mercury's ancient surface?
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Already Messenger has sent back
some curious clues.
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After Messenger's three flybys,
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we've now mapped
more than 90% of the planet.
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Taken from around 124 miles,
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these images are the clearest
to date of Mercury.
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And it's not hard to spot a crater
of epic proportions--
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the result of yet another
titanic collision.
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DENEVI: That's the Caloris Basin,
this impact basin.
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It covers almost three million
square kilometers.
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It's one of the biggest
in the solar system.
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00:12:14,267 --> 00:12:18,304
NARRATOR: The size of Alaska
and California combined,
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whatever created Caloris
almost destroyed the planet.
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ROBINSON: It was something in the order
of 100 kilometers in size.
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It could have been a huge comet
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or it could have been
a very large asteroid.
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It had a catastrophic effect
on the surface.
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NARRATOR: Shockwaves rippled
around the crust,
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buckling it on the opposite side.
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And near the center of the crater
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is another spectacular
geological puzzle--
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that has experts
scratching their heads.
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DENEVI: The Spider is
this really strange feature
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that's in almost the center
of the Caloris Basin.
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00:13:02,915 --> 00:13:03,916
ROBINSON: Oh, the Spider.
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00:13:03,950 --> 00:13:06,286
That really annoys me
when | hear people call it that
192
00:13:06,319 --> 00:13:07,487
โcause it doesn't look
like a spider.
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00:13:07,520 --> 00:13:09,289
How many legs does a spider have?
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00:13:09,322 --> 00:13:10,757
Eight, right?
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00:13:10,790 --> 00:13:13,293
DENEVI: It looks kind of like
a 100-legged spider,
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00:13:13,326 --> 00:13:19,332
but it has all of these
radiating cracks coming out of it.
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00:13:19,365 --> 00:13:22,835
NARRATOR: Whether The Spider is
the result of planetary stretch marks
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00:13:22,869 --> 00:13:27,874
or some obscure cratering process,
no one knows.
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00:13:27,907 --> 00:13:30,843
ROBINSON: It's a fascinating feature.
We don't know how it formed.
200
00:13:30,877 --> 00:13:33,212
It's very tantalizing.
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00:13:36,849 --> 00:13:40,153
NARRATOR: So, for a planet
that appears inactive,
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more has been going on
deep inside Mercury
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than we ever gave it credit for.
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00:13:46,259 --> 00:13:50,430
There's even more occurring
above the surface that can't be seen.
205
00:13:50,463 --> 00:13:55,68
And it involves
the relentless force of the sun.
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00:14:06,646 --> 00:14:09,315
NARRATOR: Like Mercury,
the Earth takes a beating
207
00:14:09,349 --> 00:14:12,218
from the sun's violent temper.
208
00:14:14,53 --> 00:14:17,623
Flares, sun storms
and other solar hissy fits
209
00:14:17,657 --> 00:14:20,259
can cause electronic mayhem
for the satellites
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00:14:20,293 --> 00:14:22,962
that roam above our heads.
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00:14:32,872 --> 00:14:36,42
Fortunately, the Earth is protected
from this radiation
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00:14:36,75 --> 00:14:37,844
by a magnetic shield,
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00:14:37,877 --> 00:14:43,116
a kind of force field generated
by our molten iron core.
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00:14:45,485 --> 00:14:49,188
JAMES SLAVIN: Planetary magnetic fields
shield planets,
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00:14:49,222 --> 00:14:51,391
their surfaces and their atmospheres
216
00:14:51,424 --> 00:14:55,995
from charged particles that are
always coming off the sun.
217
00:14:58,664 --> 00:15:01,00
NARRATOR: The auroras
that light up our polar skies
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00:15:01,33 --> 00:15:04,937
are evidence of our
protective shield at work.
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00:15:06,873 --> 00:15:11,544
Without it, life would not exist here.
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00:15:15,314 --> 00:15:17,383
Visit Mercury and you'll be visiting
221
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the only other planet
in the inner solar system
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00:15:20,186 --> 00:15:22,989
with a magnetic field.
223
00:15:23,22 --> 00:15:27,660
But its very existence
defies explanation.
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00:15:27,693 --> 00:15:31,364
SLAVIN: Now the mystery there
is that in order to have a magnetic field,
225
00:15:31,397 --> 00:15:36,602
you need to have an interior to the planet
that is at least partially molten.
226
00:15:36,636 --> 00:15:39,672
Mercury, one of the smallest
of the planets,
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00:15:39,705 --> 00:15:43,342
would have been expected to really
have frozen all the way through.
228
00:15:43,376 --> 00:15:48,848
And yet we have a relatively strong,
very well defined magnetic field
229
00:15:48,881 --> 00:15:53,920
that appears to have a source
that's located deep in the planet.
230
00:15:56,155 --> 00:15:59,625
NARRATOR: Whatever mechanism
is driving Mercury's magnetic field,
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00:15:59,659 --> 00:16:04,931
it's too weak to protect it
from the full force of the sun.
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00:16:04,964 --> 00:16:09,101
The solar wind buffets
Mercury's thin atmosphere.
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00:16:09,135 --> 00:16:13,973
And in the process,
it puts on a light show.
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00:16:14,06 --> 00:16:16,309
RONALD VERVACK: The reason you'd want
to go to Mercury as a travel destination
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00:16:16,342 --> 00:16:18,211
would be this night-side view,
236
00:16:18,244 --> 00:16:21,747
because it's going to be highly unique
in the solar system.
237
00:16:21,781 --> 00:16:24,350
You have sodium atoms
that are streaming off
238
00:16:24,383 --> 00:16:25,952
and giving off this yellow light.
239
00:16:25,985 --> 00:16:27,720
And so you could almost look
as like you're standing
240
00:16:27,753 --> 00:16:31,991
in a doughnut
of sodium emission.
241
00:16:32,24 --> 00:16:33,759
NARRATOR: With the sunrise
three months away,
242
00:16:33,793 --> 00:16:36,929
you'll have plenty of time to sit back
and take in the view,
243
00:16:36,963 --> 00:16:40,533
framed in a halo of amber light.
244
00:16:42,201 --> 00:16:44,537
VERVACK: In some sense you can get
a very nice light show.
245
00:16:44,570 --> 00:16:49,675
And | know people go to Canada
to look at the northern lights all the time.
246
00:16:49,709 --> 00:16:53,746
And so that would be a reason
to go to Mercury.
247
00:16:53,846 --> 00:16:56,849
MAN: T minus 40 seconds.
Everything looks good for launch.
248
00:16:56,883 --> 00:16:58,351
NARRATOR: Not a night owl?
249
00:16:58,384 --> 00:17:01,53
Then head into the light.
250
00:17:01,87 --> 00:17:03,990
But when you're this close
to a stellar rotisserie,
251
00:17:04,23 --> 00:17:08,60
make sure you pack
plenty of sunscreen.
252
00:17:17,103 --> 00:17:22,141
If you want a suntan, you can't beat
the dusty sands of Mercury.
253
00:17:22,174 --> 00:17:23,910
Stretch out on the ground here
254
00:17:23,943 --> 00:17:27,79
and the sun crackles and fizzes
right above you,
255
00:17:27,113 --> 00:17:33,619
appearing almost three times bigger
in the sky and seven times as hot.
256
00:17:36,88 --> 00:17:38,57
PAIGE: If you were walking
on the surface of Mercury,
257
00:17:38,90 --> 00:17:39,559
you would need
one heck of a spacesuit.
258
00:17:39,592 --> 00:17:44,63
Because if you were in the sun
it would be extremely hot.
259
00:17:44,96 --> 00:17:46,832
You would see
an enormous sun in the sky
260
00:17:46,866 --> 00:17:49,101
that would just
burn you to death
261
00:17:49,135 --> 00:17:52,738
if you spent any time
in it whatsoever.
262
00:17:54,640 --> 00:17:58,477
NARRATOR: The mercury
really climbs on Mercury--
263
00:17:58,511 --> 00:18:03,816
to a toasty 840 degrees Fahrenheit.
264
00:18:03,849 --> 00:18:08,421
That's about twice as hot
as your kitchen oven on full heat.
265
00:18:11,157 --> 00:18:15,761
You'll need a bit more
than SPF 30 sunscreen here.
266
00:18:23,469 --> 00:18:27,406
To escape the heat, you can
always head to the dark side.
267
00:18:27,440 --> 00:18:28,975
But dress warmly.
268
00:18:29,08 --> 00:18:32,78
With virtually no atmosphere
to keep the heat in,
269
00:18:32,111 --> 00:18:38,451
the temperature plummets
to minus 275 degrees Fahrenheit.
270
00:18:42,822 --> 00:18:44,991
And it's here in the freezer
271
00:18:45,24 --> 00:18:48,661
that Messenger will encounter
another puzzle:
272
00:18:48,694 --> 00:18:53,899
Can ice exist on a planet
so close to the sun?
273
00:18:55,201 --> 00:18:58,04
PAIGE: It was only when
the first radar observations
274
00:18:58,37 --> 00:19:02,575
of the surface of Mercury
were obtained back in the '90s
275
00:19:02,608 --> 00:19:05,845
that it was discovered
that Mercury in fact had
276
00:19:05,878 --> 00:19:11,17
what appeared to be polar caps
in these first radar images.
277
00:19:11,50 --> 00:19:13,619
NARRATOR: Some corners
of Mercury's polar craters
278
00:19:13,653 --> 00:19:15,688
are in permanent shadow.
279
00:19:15,721 --> 00:19:18,958
Here, on the most
sun-baked planet of all,
280
00:19:18,991 --> 00:19:24,397
water seems to Survive frozen
in eternal darkness.
281
00:19:25,231 --> 00:19:29,201
PAIGE: The ice is contained in places
where literally the sun never shines.
282
00:19:29,235 --> 00:19:34,106
And so the ice is sequestered
in these dark interiors of craters
283
00:19:34,140 --> 00:19:36,575
at the high latitude regions.
284
00:19:41,47 --> 00:19:44,684
NARRATOR: We found the same thing
on our moon.
285
00:19:44,717 --> 00:19:47,453
In late 2009, the LCROSS mission
286
00:19:47,486 --> 00:19:50,423
crashed a probe
into a deeply shadowed crater,
287
00:19:50,456 --> 00:19:54,293
confirming ice hidden
near the lunar south pole.
288
00:19:54,326 --> 00:19:55,995
Where did it come from?
289
00:19:56,28 --> 00:19:59,98
A comet?
290
00:19:59,131 --> 00:20:04,370
PAIGE: It's very interesting because
we believe that the water in the Earth,
291
00:20:04,403 --> 00:20:07,940
in its atmosphere, in the oceans
and even below the surface
292
00:20:07,973 --> 00:20:09,775
probably came
from a similar source.
293
00:20:09,809 --> 00:20:12,144
And so part of the mystery
of Mercury
294
00:20:12,178 --> 00:20:14,80
is to try to find out
where the water came from
295
00:20:14,113 --> 00:20:18,50
and maybe that might help us find out
where the water on Earth came from.
296
00:20:29,95 --> 00:20:34,800
NARRATOR: It may never be possible
to send a human to Mercury.
297
00:20:34,834 --> 00:20:37,403
But how about a robot...
298
00:20:39,271 --> 00:20:43,242
In 2011, when Messenger
arrives in orbit,
299
00:20:43,275 --> 00:20:47,646
imagine this tough little spacecraft
circling a lonely planet,
300
00:20:47,680 --> 00:20:50,883
a very long way from home.
301
00:20:58,190 --> 00:20:59,592
Move away from the sun
302
00:20:59,625 --> 00:21:03,295
and you'd expect things
to cool down a little.
303
00:21:03,329 --> 00:21:07,466
Venus: the picture
of coolness and calm.
304
00:21:07,500 --> 00:21:11,70
All pale, beguiling
and cloaked by clouds.
305
00:21:11,103 --> 00:21:14,774
But the planet of love
is shrouded in mystery.
306
00:21:14,807 --> 00:21:19,578
Drop beneath her treacherous veil
at your own risk.
307
00:21:24,183 --> 00:21:27,620
Beneath the clouds is the only planet
in the solar system
308
00:21:27,653 --> 00:21:29,922
to rotate backwards.
309
00:21:29,955 --> 00:21:33,459
And it does so very slowly.
310
00:21:35,895 --> 00:21:38,531
The sun, if you could see it,
311
00:21:38,564 --> 00:21:41,801
rises in the west
and sets in the east.
312
00:21:41,834 --> 00:21:45,04
An entire day here lasts
for eight Earth months,
313
00:21:45,37 --> 00:21:48,40
which is longer
than the Venusian year.
314
00:21:50,409 --> 00:21:52,144
BAINES: On Venus you can
walk around the planet
315
00:21:52,178 --> 00:21:54,680
faster than the planet rotates.
316
00:21:56,448 --> 00:21:59,819
NARRATOR: The sky above
is as heavy as it looks--
317
00:21:59,852 --> 00:22:02,988
loaded with CO2.
318
00:22:03,22 --> 00:22:06,525
ELLEN STOFAN: Venus' cloud cover
is mostly made of carbon dioxide.
319
00:22:06,559 --> 00:22:08,627
And on the Earth we have
the same amount,
320
00:22:08,661 --> 00:22:11,263
but it's tied up in rocks
like limestones,
321
00:22:11,297 --> 00:22:12,898
it's tied up in reefs.
322
00:22:12,932 --> 00:22:16,836
On Venus, all that carbon dioxide
is in the air.
323
00:22:16,869 --> 00:22:18,704
NARRATOR: It's the differences
between these worlds
324
00:22:18,737 --> 00:22:21,273
that are so intriguing.
325
00:22:21,307 --> 00:22:24,143
That's because
4.5 billion years ago,
326
00:22:24,176 --> 00:22:29,849
Venus and Earth started out
as planetary twins.
327
00:22:29,882 --> 00:22:31,550
MARK BULLOCK: They were formed
right next to each other,
328
00:22:31,584 --> 00:22:33,485
they're very close to each other
in the solar system,
329
00:22:33,519 --> 00:22:37,22
they have similar sizes.
330
00:22:37,56 --> 00:22:39,158
DAVID GRINSPOON: Not only that,
we now know the planets
331
00:22:39,191 --> 00:22:41,627
were exchanging material early on.
332
00:22:41,660 --> 00:22:45,698
Bits of Earth were falling on Venus,
and bits of Venus were falling on Earth.
333
00:22:45,731 --> 00:22:48,968
So if life started
on any of these worlds,
334
00:22:49,01 --> 00:22:51,704
it may well have spread among them
335
00:22:51,737 --> 00:22:54,373
through these little chips
getting knocked off
336
00:22:54,406 --> 00:22:56,342
from all the impacts
that were happening then,
337
00:22:56,375 --> 00:22:58,277
all the big collisions.
338
00:23:00,346 --> 00:23:02,147
ANNOUNCER: You are there...
339
00:23:02,181 --> 00:23:06,252
on the most exciting, nerve-shattering
journey in the history of man!
340
00:23:06,285 --> 00:23:10,189
NARRATOR: 50 years ago,
it was easy for us to imagine Venus,
341
00:23:10,222 --> 00:23:12,658
closer to the sun
and wrapped in clouds,
342
00:23:12,691 --> 00:23:17,396
to be our scorched tropical sister,
swarming with life.
343
00:23:19,298 --> 00:23:21,133
GRINSPOON: There was
this picture of Venus
344
00:23:21,166 --> 00:23:24,503
as a kind of primitive, steamy Earth,
345
00:23:24,536 --> 00:23:29,408
complete with giant tree ferns
and dinosaurs.
346
00:23:32,912 --> 00:23:37,616
MIKHAIL MAROV: Altogether,
it seemed to us
347
00:23:37,650 --> 00:23:42,788
that it should be, just possibly,
even a populated world.
348
00:23:47,259 --> 00:23:51,363
NARRATOR: In the late 1950s,
the Space Race begins.
349
00:23:51,397 --> 00:23:53,599
While America aims for the moon,
350
00:23:53,632 --> 00:23:57,670
Russia sets its sights
on meeting the neighbors.
351
00:24:05,144 --> 00:24:08,914
MAROV: Venus and Mars
still was in the human dreams
352
00:24:08,948 --> 00:24:16,88
to meet the species
which could be very similar to us.
353
00:24:16,121 --> 00:24:23,295
Venus was even easier
than Mars to reach.
354
00:24:25,898 --> 00:24:29,668
NARRATOR: But landing on Venus
proves surprisingly difficult.
355
00:24:29,702 --> 00:24:32,404
One by one, the Soviet Venera probes
356
00:24:32,438 --> 00:24:36,442
disappear within
the thick Venusian atmosphere...
357
00:24:39,278 --> 00:24:41,13
their last transmissions warning
358
00:24:41,46 --> 00:24:45,751
of a world of inconceivably high
temperatures and pressure.
359
00:24:58,697 --> 00:25:01,200
Persistence and
tough Russian engineering
360
00:25:01,233 --> 00:25:03,302
eventually pay off.
361
00:25:03,335 --> 00:25:08,140
In 1975, the camera
on the redesigned Venera 9
362
00:25:08,173 --> 00:25:12,745
finally penetrates the Venusian veil.
363
00:25:12,778 --> 00:25:18,384
But what it sees is nothing
like the tropical paradise imagined.
364
00:25:23,22 --> 00:25:29,361
This is the first-ever picture taken
from the surface of another planet.
365
00:25:29,395 --> 00:25:31,897
MAROV: And for the first time
it was returned
366
00:25:31,930 --> 00:25:36,502
black-and-white panoramas
of the Venus surface.
367
00:25:36,535 --> 00:25:39,671
These images were
extremely important,
368
00:25:39,705 --> 00:25:44,76
because for the first time
we, human beings,
369
00:25:44,109 --> 00:25:50,416
had a chance to see
with our naked eyes
370
00:25:50,449 --> 00:25:54,853
completely different other world.
371
00:25:54,887 --> 00:25:57,990
We were very much proud of that.
372
00:26:02,194 --> 00:26:05,931
NARRATOR: Seven years later,
Veneras 13 and 14
373
00:26:05,964 --> 00:26:11,503
send back the first color postcards
taken under Venusian skies.
374
00:26:13,172 --> 00:26:19,244
MAROV: It means that standing
on the surface of Venus
375
00:26:19,278 --> 00:26:26,518
you will meet absolutely
incredible situation.
376
00:26:26,552 --> 00:26:32,57
First of all, you will see
not the blue skies.
377
00:26:32,91 --> 00:26:38,997
You will see red skies,
orange in color.
378
00:26:39,31 --> 00:26:41,233
This is a hell.
379
00:26:41,266 --> 00:26:43,01
Real hell!
380
00:26:45,337 --> 00:26:48,240
NARRATOR: Hell is a good description.
381
00:26:48,273 --> 00:26:51,610
This is what it's like to enter
the Venusian underworld;
382
00:26:51,643 --> 00:26:56,582
a volcanic landscape ruled
by crushing pressure and searing heat.
383
00:26:56,615 --> 00:27:00,385
No probe survives here
for much more than a few hours.
384
00:27:00,419 --> 00:27:03,522
And none have ever returned.
385
00:27:10,696 --> 00:27:13,265
What happened to our twin world?
386
00:27:13,298 --> 00:27:17,769
Was Venus always as barren
and hostile as it appears to be?
387
00:27:19,671 --> 00:27:21,607
STOFAN: One of the most intriguing things about
Venus
388
00:27:21,640 --> 00:27:24,276
is that we know that
at some point in Venus' history,
389
00:27:24,309 --> 00:27:27,746
it had an ocean like the one
we have here on Earth.
390
00:27:27,779 --> 00:27:29,715
There have been chemicals
measured in the atmosphere
391
00:27:29,748 --> 00:27:30,983
that tell you at some point
392
00:27:31,16 --> 00:27:35,187
Venus had an ocean's worth
of water that is now gone.
393
00:27:38,457 --> 00:27:39,458
MAN: Atlantis, Houston.
394
00:27:39,491 --> 00:27:42,561
Everything down here
looks real good to us.
395
00:27:42,594 --> 00:27:45,831
NARRATOR: Where did
all the water on Venus go?
396
00:27:45,864 --> 00:27:50,702
And what else lies hidden
under her veil?
397
00:27:50,736 --> 00:27:56,74
WOMAN: Five, four, three, two, one.
398
00:27:56,108 --> 00:28:00,12
We have ignition
and liftoff of Atlantis.
399
00:28:00,45 --> 00:28:03,415
NARRATOR: In 1989,
the space shuttle Atlantis
400
00:28:03,448 --> 00:28:06,618
launches the Magellan probe
toward Venus.
401
00:28:06,652 --> 00:28:08,654
MAN: Roger, roll, Atlantis.
402
00:28:17,229 --> 00:28:19,698
NARRATOR: After a journey
of 15 months,
403
00:28:19,731 --> 00:28:25,37
Magellan uses radar eyes to peer
through the clouds from orbit.
404
00:28:28,106 --> 00:28:31,243
Watching from Earth is Ellen Stofan.
405
00:28:32,778 --> 00:28:34,613
STOFAN: When you have that ability
to pick up an image
406
00:28:34,646 --> 00:28:36,815
and say, "I'm one
of the first three people,
407
00:28:36,848 --> 00:28:38,116
I'm one of the first five people
408
00:28:38,150 --> 00:28:41,820
to ever look at this piece of ground
on another planet."
409
00:28:41,853 --> 00:28:45,591
It's such a sense of awe
and a sense of discovery.
410
00:28:50,629 --> 00:28:56,01
NARRATOR: Magellan's radar
strips away the thick clouds.
411
00:28:56,34 --> 00:29:00,973
For the first time ever,
we see all of Venus laid bare.
412
00:29:06,144 --> 00:29:08,380
Welcome to lava land!
413
00:29:10,382 --> 00:29:12,17
STOFAN: There are volcanoes
of all sizes,
414
00:29:12,50 --> 00:29:15,654
from a kilometer across
to hundreds of kilometers across.
415
00:29:15,687 --> 00:29:17,623
And in that sense
it's not all that different
416
00:29:17,656 --> 00:29:19,558
from some areas on the Earth.
417
00:29:19,591 --> 00:29:20,859
But on the other hand,
418
00:29:20,892 --> 00:29:26,64
it's of course this dry world
with no vegetation at all.
419
00:29:26,98 --> 00:29:31,303
NARRATOR: It's the sheer number
of volcanoes that sets Venus apart.
420
00:29:31,336 --> 00:29:35,73
This is a world that
has been tortured by fire.
421
00:29:35,107 --> 00:29:40,479
Over 1,600 giant volcanoes
puncture its surface.
422
00:29:40,512 --> 00:29:43,782
It's possible some are still active.
423
00:29:46,485 --> 00:29:49,621
[helicopter]
424
00:29:54,192 --> 00:29:56,28
BULLOCK: If we could just hover
like this over Venus
425
00:29:56,61 --> 00:29:59,464
it would probably look
a lot like this.
426
00:29:59,498 --> 00:30:02,901
NARRATOR: Mark Bullock
enjoys spending time on Venus,
427
00:30:02,934 --> 00:30:07,105
at least the version he finds
here on Earth.
428
00:30:07,139 --> 00:30:11,410
BULLOCK: Hawaii has some of
the most spectacular shield volcanoes
429
00:30:11,443 --> 00:30:17,549
that are very similar to the volcanoes
that we see on Venus.
430
00:30:17,582 --> 00:30:22,587
NARRATOR: The huge, gently sloped
volcanoes of Hawaii may be impressive.
431
00:30:22,621 --> 00:30:25,857
On Venus there are at least 150
432
00:30:25,891 --> 00:30:30,329
ranging from this size
to ten times larger.
433
00:30:33,365 --> 00:30:38,136
But the observant visitor may notice
that Venus is missing something.
434
00:30:39,271 --> 00:30:41,440
STOFAN: The whole impact crater
situation on Venus
435
00:30:41,473 --> 00:30:43,975
is really very puzzling.
436
00:30:44,09 --> 00:30:45,177
BULLOCK: With the Magellan images,
437
00:30:45,210 --> 00:30:47,713
we see really a small number
of impact craters.
438
00:30:47,746 --> 00:30:50,482
And it's such a small number,
it's about a thousand.
439
00:30:50,515 --> 00:30:52,584
Because we know the rate
at which impactors come in,
440
00:30:52,617 --> 00:30:54,86
we can actually date the surface
441
00:30:54,119 --> 00:30:58,290
to somewhere between 300 million
and 1 billion years old.
442
00:31:00,158 --> 00:31:03,28
NARRATOR: Sometime
in the recent geological past,
443
00:31:03,61 --> 00:31:07,532
it seems the entire surface of Venus
was remodeled...
444
00:31:07,566 --> 00:31:09,34
and suddenly.
445
00:31:11,803 --> 00:31:14,573
BAINES: The surface geology of Venus
is different than the Earth,
446
00:31:14,606 --> 00:31:15,907
basically because a lack of water.
447
00:31:15,941 --> 00:31:19,845
Water is not lubricating that crust,
so you don't get plate tectonics.
448
00:31:19,878 --> 00:31:23,315
Instead what seems to happen
is that forces inside the planet
449
00:31:23,348 --> 00:31:24,950
are trying to move things around.
450
00:31:24,983 --> 00:31:26,351
But it can't, it's locked.
451
00:31:26,385 --> 00:31:30,255
And then it explodes, very massive,
globally explosive episodes
452
00:31:30,288 --> 00:31:34,192
that happen about every
half a billion to a billion years.
453
00:31:37,662 --> 00:31:40,532
So you would not want to be
on Venus when that happens.
454
00:31:40,565 --> 00:31:42,267
Because once
something gives way
455
00:31:42,300 --> 00:31:45,604
the whole planet might just
basically explode in a sense
456
00:31:45,637 --> 00:31:46,938
and turn itself over
457
00:31:46,972 --> 00:31:51,09
in a very short amount of time
in geological terms.
458
00:31:53,845 --> 00:31:55,747
BULLOCK: Oh, man, look at this!
459
00:31:55,781 --> 00:31:58,717
We can see a river of lava
beneath the surface.
460
00:31:58,750 --> 00:32:01,987
Imagine that this lava
is on Venus.
461
00:32:02,20 --> 00:32:03,655
Probably something
very much like this
462
00:32:03,688 --> 00:32:07,826
occurs either today
or in the recent past.
463
00:32:08,794 --> 00:32:10,395
NARRATOR: No one
can say for sure
464
00:32:10,429 --> 00:32:15,00
if we'll ever see an eruption
like this on Venus.
465
00:32:15,33 --> 00:32:18,403
No one has ever been able
to get this close!
466
00:32:19,404 --> 00:32:22,874
BULLOCK: One of the really exciting
and high level of scientific interest
467
00:32:22,908 --> 00:32:25,577
is whether Venus
is geologically active today.
468
00:32:25,610 --> 00:32:29,714
Because there are reasons to think
that the clouds on Venus only exist
469
00:32:29,748 --> 00:32:33,251
because there is ongoing
geologic activity.
470
00:32:33,285 --> 00:32:35,554
So this is one of
the big secrets of Venus,
471
00:32:35,587 --> 00:32:38,23
it's something that we
want to find out.
472
00:32:38,56 --> 00:32:40,225
NARRATOR: In recent years,
finding the source
473
00:32:40,258 --> 00:32:42,127
of Venus' thick atmosphere
474
00:32:42,160 --> 00:32:47,98
has become surprisingly relevant
for all of us down here on Earth.
475
00:32:47,132 --> 00:32:49,968
BULLOCK: Half a million tons
of sulfur dioxide
476
00:32:50,01 --> 00:32:53,338
spewed into the atmosphere
every year.
477
00:32:56,107 --> 00:32:58,276
BAINES: The whole Greenhouse Effect
was not really recognized
478
00:32:58,310 --> 00:33:01,246
as a Significant effect
to influence planetary climates
479
00:33:01,279 --> 00:33:02,347
until we went to Venus
480
00:33:02,380 --> 00:33:04,549
and found that instead of being
90 degrees Fahrenheit
481
00:33:04,583 --> 00:33:06,17
it was 900 degrees Fahrenheit.
482
00:33:06,51 --> 00:33:07,552
And we said, "Whoa,
what's wrong with this?
483
00:33:07,586 --> 00:33:08,653
Let's learn about this."
484
00:33:08,687 --> 00:33:11,323
And it taught us
about the greenhouse effect.
485
00:33:13,158 --> 00:33:15,160
NARRATOR: The best way
to experience Venus
486
00:33:15,193 --> 00:33:20,98
is to hitch an imaginary ride
on a Soviet Venera probe.
487
00:33:27,405 --> 00:33:30,08
BULLOCK: Well, it would be a wild ride.
488
00:33:31,176 --> 00:33:35,347
NARRATOR: The clouds start
about 40 miles up,
489
00:33:35,380 --> 00:33:38,783
some five times higher
than the Earth's.
490
00:33:41,86 --> 00:33:42,187
BAINES: What are those clouds
made out of?
491
00:33:42,220 --> 00:33:43,388
They're not made out of water,
492
00:33:43,421 --> 00:33:44,789
they're made out of a completely
different substance.
493
00:33:44,823 --> 00:33:47,192
They're made out of sulfuric acid.
494
00:33:47,225 --> 00:33:51,296
Everywhere you go, the atmosphere
is going to try to eat you away.
495
00:33:52,564 --> 00:33:55,166
NARRATOR: As you get deeper,
things heat up.
496
00:33:55,200 --> 00:33:59,938
The thickening atmosphere
allows the sun's heat in, but not out.
497
00:33:59,971 --> 00:34:01,840
It's also getting dense.
498
00:34:01,873 --> 00:34:06,711
So dense, your probe
drops like a coin in water.
499
00:34:06,745 --> 00:34:09,548
BULLOCK: As we descended
we would gradually,
500
00:34:09,581 --> 00:34:12,150
the surface would gradually
appear to us
501
00:34:12,183 --> 00:34:15,287
as if we were approaching
the bottom of the ocean.
502
00:34:23,795 --> 00:34:25,597
NARRATOR: Congratulations,
you've arrived
503
00:34:25,630 --> 00:34:28,967
on the hottest surface
in the solar system!
504
00:34:30,769 --> 00:34:36,975
Here the official temperature
is 870 degrees Fahrenheit.
505
00:34:40,478 --> 00:34:43,14
Day or night, equator or pole,
506
00:34:43,48 --> 00:34:47,352
the searing heat never varies
more than a few degrees.
507
00:34:48,553 --> 00:34:53,625
And it's why we have so few snapshots
from the Venusian surface.
508
00:34:57,429 --> 00:34:58,897
GRINSPOON:
So why is it so hard
509
00:34:58,930 --> 00:35:02,400
to bring scientific instruments
to the surface of Venus?
510
00:35:02,434 --> 00:35:03,969
What about an ordinary camera?
511
00:35:04,02 --> 00:35:05,103
There's plenty of light there.
512
00:35:05,136 --> 00:35:07,906
Why not just send a camera
and take pictures?
513
00:35:07,939 --> 00:35:12,377
I've got my NASA-issued spacesuit here,
my special Venus suit.
514
00:35:12,410 --> 00:35:14,546
And let's take this camera
and send it to Venus
515
00:35:14,579 --> 00:35:16,448
and see what happens.
516
00:35:25,357 --> 00:35:27,892
BULLOCK: Primarily
you don't want to melt.
517
00:35:27,926 --> 00:35:31,296
It's such a hot environment
that all the electronics,
518
00:35:31,329 --> 00:35:34,132
all the power,
all the communications
519
00:35:34,165 --> 00:35:36,868
have to be very rugged.
520
00:35:36,901 --> 00:35:38,903
GRINSPOON:
Oh, that's cool, though!
521
00:35:38,937 --> 00:35:41,506
BULLOCK: Anything mechanical,
anything electronic
522
00:35:41,539 --> 00:35:46,511
is just an enormous challenge
to have it function on the surface.
523
00:35:51,16 --> 00:35:54,352
NARRATOR: And it's not just the heat
that you have to bear.
524
00:35:54,386 --> 00:35:58,23
All that sky above
is really heavy,
525
00:35:58,56 --> 00:36:02,794
pressing in at around 90 times
the pressure on Earth.
526
00:36:02,827 --> 00:36:03,995
STOFAN: When | was
a graduate student
527
00:36:04,29 --> 00:36:05,997
we use to get in conversations
about what would get you first,
528
00:36:06,31 --> 00:36:09,00
the temperature
or the pressure?
529
00:36:09,34 --> 00:36:11,536
It would be pretty simultaneous,
| think.
530
00:36:18,309 --> 00:36:20,612
NARRATOR: To descend
to the surface of Venus
531
00:36:20,645 --> 00:36:25,517
is the same as diving
over half a mile underwater.
532
00:36:26,985 --> 00:36:29,688
PHIL NUYTTEN: It's an enormous pressure,
enormous, crushing pressure.
533
00:36:29,721 --> 00:36:31,623
How do you make things
that withstand,
534
00:36:31,656 --> 00:36:35,827
how do things turn and move
under those huge outside pressures?
535
00:36:35,860 --> 00:36:40,432
Well, that's what the armor
of technology is all about.
536
00:36:40,465 --> 00:36:43,134
The Exosuit, using composite fiber,
537
00:36:43,168 --> 00:36:46,838
strong aluminum alloys
and stainless and titanium
538
00:36:46,871 --> 00:36:48,106
and all these things.
539
00:36:48,139 --> 00:36:50,442
It looks like something
out of Transformers
540
00:36:50,475 --> 00:36:51,910
or out of a comic book.
541
00:36:51,943 --> 00:36:54,546
That's the same kind of suit
that you'd need
542
00:36:54,579 --> 00:36:58,550
on the surface of Venus.
543
00:36:58,583 --> 00:37:02,954
NARRATOR: You'd never guess
the dangers on the ground from orbit.
544
00:37:05,790 --> 00:37:07,592
Except maybe for this:
545
00:37:07,625 --> 00:37:12,630
massive double-barreled storms
hovering above the poles.
546
00:37:12,664 --> 00:37:15,500
BAINES: These, what we call
dipole features, twirling around.
547
00:37:15,533 --> 00:37:17,535
We don't know really what they are.
548
00:37:17,569 --> 00:37:18,570
But the whole feature itself
549
00:37:18,603 --> 00:37:21,239
is only a thousand or two
kilometers across,
550
00:37:21,272 --> 00:37:22,407
it's not very big.
551
00:37:22,440 --> 00:37:25,877
But it has like a figure-eight
type of look to it.
552
00:37:25,910 --> 00:37:29,414
NARRATOR: Believed to be created
by winds that roar around the equator
553
00:37:29,447 --> 00:37:32,550
at speeds up to 230 miles per hour,
554
00:37:32,584 --> 00:37:37,255
these hurricanes can split
into three and even four.
555
00:37:41,793 --> 00:37:44,796
And the wild weather
doesn't end there.
556
00:37:44,829 --> 00:37:48,633
Because the hottest planet
in the solar system even has snow...
557
00:37:48,666 --> 00:37:51,770
but not as we know it.
558
00:37:51,803 --> 00:37:54,239
STOFAN: All of the sudden
in the radar images,
559
00:37:54,272 --> 00:37:56,107
all the mountains go white.
560
00:37:56,141 --> 00:37:59,144
Now that's because there's some kind
of highly reflective coating.
561
00:37:59,177 --> 00:38:00,745
It wouldn't look white to your eyes
562
00:38:00,779 --> 00:38:03,314
if you could actually land
on the surface of Venus.
563
00:38:03,348 --> 00:38:04,549
It might look shiny,
564
00:38:04,582 --> 00:38:07,619
because we actually think it might be
some sort of metallic coating,
565
00:38:07,652 --> 00:38:09,420
almost like a pyrite
or a fool's gold.
566
00:38:09,454 --> 00:38:11,55
So something sparkly,
567
00:38:11,89 --> 00:38:14,425
which to me is even better
than looking at snow.
568
00:38:18,897 --> 00:38:20,765
NARRATOR: These are just
some of the puzzles
569
00:38:20,799 --> 00:38:24,202
that the European Space Agency's
Venus Express,
570
00:38:24,235 --> 00:38:29,107
now in orbit,
is hoping to solve.
571
00:38:29,140 --> 00:38:33,444
As we begin to understand
how carbon dioxide controls our climate,
572
00:38:33,478 --> 00:38:38,116
there's never been a better time
to learn lessons from our neighbor.
573
00:38:40,718 --> 00:38:42,921
HAKAN SVEDHEM: What we're trying
to solve now
574
00:38:42,954 --> 00:38:47,58
with this very, very dense atmosphere,
very complex weather patterns,
575
00:38:47,91 --> 00:38:48,560
with the new data
from Venus Express
576
00:38:48,593 --> 00:38:52,297
we are really learning
by mapping out in three dimensions
577
00:38:52,330 --> 00:38:54,666
how the atmosphere behaves.
578
00:38:57,335 --> 00:38:59,671
NARRATOR: Unprotected
by a magnetic shield,
579
00:38:59,704 --> 00:39:04,409
Venus is still being robbed
of precious water.
580
00:39:04,442 --> 00:39:07,378
Venus Express has seen
how the solar wind
581
00:39:07,412 --> 00:39:10,248
eats away at the atmosphere.
582
00:39:11,716 --> 00:39:13,551
SVEDHEM: We can see
that even today
583
00:39:13,585 --> 00:39:18,857
that actually water is still escaping
in the form of oxygen and hydrogen.
584
00:39:18,890 --> 00:39:20,24
And that's an indication
585
00:39:20,58 --> 00:39:23,494
that there has been water
on Venus in the past.
586
00:39:25,363 --> 00:39:27,899
NARRATOR: Despite
all this scientific effort,
587
00:39:27,932 --> 00:39:33,671
we still don't know what triggered
Venus' diabolical transformation.
588
00:39:35,974 --> 00:39:38,109
STOFAN: People debate over whether
Venus ever had a moon.
589
00:39:38,142 --> 00:39:40,278
If Venus had a satellite
at one point,
590
00:39:40,311 --> 00:39:43,648
could that satellite have eventually
impacted onto the surface
591
00:39:43,681 --> 00:39:46,517
and caused some catastrophe
to happen?
592
00:39:46,551 --> 00:39:49,320
We don't know.
It could have been possibly a factor.
593
00:39:52,857 --> 00:39:54,259
NARRATOR: Perhaps such an impact
594
00:39:54,292 --> 00:39:59,430
explains both the strange calendar
and climate on Venus.
595
00:39:59,464 --> 00:40:02,267
Was it hit hard enough
to flip upside down?
596
00:40:02,300 --> 00:40:05,837
And for its day to be slowed to a crawl?
597
00:40:05,870 --> 00:40:12,76
Was this the moment Venus' climate
was thrown into chaos?
598
00:40:15,79 --> 00:40:17,749
GRINSPOON: If | had to guess,
or | had to bet,
599
00:40:17,782 --> 00:40:20,184
| would say, "Yeah,
Venus did have a life."
600
00:40:20,218 --> 00:40:25,423
And | say that because what we do
understand about life on Earth
601
00:40:25,456 --> 00:40:29,327
is that it started early
602
00:40:29,360 --> 00:40:35,266
and doesn't seem to have required
any extraordinary conditions.
603
00:40:35,300 --> 00:40:38,770
If there was life of our kind,
the organic kind,
604
00:40:38,803 --> 00:40:41,239
on the surface of Venus
a long time ago,
605
00:40:41,272 --> 00:40:45,209
then what happened to that life?
606
00:40:45,243 --> 00:40:48,613
Well, one possibility
is that it just died out.
607
00:40:48,646 --> 00:40:51,716
But there's another possibility
that's a little more exotic,
608
00:40:51,749 --> 00:40:57,355
which is that it may have migrated
up into the clouds.
609
00:40:57,388 --> 00:41:00,358
BAINES: There is some speculation
that Venus might actually still harbor life
610
00:41:00,391 --> 00:41:03,27
even though it is
such a hostile place.
611
00:41:03,61 --> 00:41:04,295
And the reasoning is that,
612
00:41:04,329 --> 00:41:06,664
well, gee, at one time Venus
was like the Earth
613
00:41:06,698 --> 00:41:09,100
in the first two billion years or so
of its history.
614
00:41:09,133 --> 00:41:13,137
So if life were to grab a hold,
maybe life was able to stay ahead
615
00:41:13,171 --> 00:41:15,273
of the environmental disaster
that befell Venus
616
00:41:15,306 --> 00:41:18,09
as the water basically
left the planet.
617
00:41:19,877 --> 00:41:25,49
NARRATOR: Could life really exist
in the clouds of Venus?
618
00:41:29,53 --> 00:41:30,855
The best way to know for sure
619
00:41:30,888 --> 00:41:34,959
is to float into the atmosphere
and find out.
620
00:41:34,993 --> 00:41:37,595
BAINES: Right behind us
is the Valor balloon
621
00:41:37,628 --> 00:41:40,164
which we intend to fly
in the skies of Venus
622
00:41:40,198 --> 00:41:43,01
a couple of years from now.
623
00:41:43,34 --> 00:41:46,37
NARRATOR: Valor will be tackling
the acid clouds of Venus
624
00:41:46,70 --> 00:41:51,509
with a little help
from frying pan technology.
625
00:41:51,542 --> 00:41:52,910
BAINES: There's been
two other balloons,
626
00:41:52,944 --> 00:41:56,247
already launched to Venus
in the mid-1980s.
627
00:41:56,280 --> 00:41:57,415
These were the Vega missions.
628
00:41:57,448 --> 00:41:59,83
There were two separate balloons
629
00:41:59,117 --> 00:42:03,187
that the Russians put
into the atmosphere.
630
00:42:03,221 --> 00:42:06,524
The one thing they knew to do
is put Teflon on that whole balloon,
631
00:42:06,557 --> 00:42:10,94
and the balloons worked perfectly
for two days just as designed.
632
00:42:10,128 --> 00:42:12,797
And so we know that Teflon works.
633
00:42:14,532 --> 00:42:17,835
NARRATOR: Battling violent updrafts
and acid clouds,
634
00:42:17,869 --> 00:42:19,637
these non-stick pioneers
635
00:42:19,670 --> 00:42:22,974
were swept nearly halfway
round the planet.
636
00:42:23,07 --> 00:42:27,111
Kevin expects Valor to go further.
637
00:42:27,145 --> 00:42:30,681
BAINES: We'll circumnavigate the planet,
that is fly around the world of Venus,
638
00:42:30,715 --> 00:42:33,451
not just once but up to five times.
639
00:42:33,484 --> 00:42:37,789
And if we do that, if we accomplish that,
we will by far have the world's record,
640
00:42:37,822 --> 00:42:39,724
actually it's the universal record,
641
00:42:39,757 --> 00:42:42,727
for flight in the skies
of any planet anywhere.
642
00:42:49,667 --> 00:42:53,137
NARRATOR: Underexplored
and unbelievably alien,
643
00:42:53,171 --> 00:42:56,507
the hot zone planets
are finally being recognized
644
00:42:56,541 --> 00:43:00,78
as prime space travel destinations.
645
00:43:01,512 --> 00:43:07,351
Mercury: a planet that's
both freezer and furnace.
646
00:43:07,385 --> 00:43:08,419
DENEVI: As a geologist,
647
00:43:08,453 --> 00:43:11,756
if | could just bring back
one rock, one sample.
648
00:43:11,789 --> 00:43:13,825
| mean, that would increase
our knowledge of Mercury
649
00:43:13,858 --> 00:43:17,462
by, you know, tenfold or something.
650
00:43:18,963 --> 00:43:21,199
ROBINSON: | would like to go
to these polar craters
651
00:43:21,232 --> 00:43:22,633
and figure out what is it.
652
00:43:22,667 --> 00:43:28,39
Even if it's not water, it's something
very unusual and very fascinating.
653
00:43:28,72 --> 00:43:32,810
NARRATOR: And Venus,
our unfortunate twin sister.
654
00:43:32,844 --> 00:43:34,412
BULLOCK: What we'd like to do
is explore the regions
655
00:43:34,445 --> 00:43:36,414
that haven't been explored before.
656
00:43:36,447 --> 00:43:40,384
And so | would pick Alpha Regio here.
657
00:43:40,418 --> 00:43:43,988
That's probably the first place | would go.
658
00:43:44,21 --> 00:43:45,189
BAINES: I'd love to go see
659
00:43:45,223 --> 00:43:48,259
those snow-filled mountain peaks
with metallic snow
660
00:43:48,292 --> 00:43:50,61
and see if we can figure out
what's going on there.
661
00:43:50,94 --> 00:43:51,762
Maybe some new sports
that can be created,
662
00:43:51,796 --> 00:43:54,432
sliding down those metallic snows?
663
00:43:57,602 --> 00:44:00,04
GRINSPOON: And then of course
there's the future story
664
00:44:00,37 --> 00:44:02,206
and what's going to happen to Earth
in the distant future.
665
00:44:02,240 --> 00:44:05,76
And that's another reason
we are really interested in Venus.
666
00:44:05,109 --> 00:44:09,614
Because the ultimate fate of the Earth
is to look like Venus looks today.
667
00:44:13,151 --> 00:44:17,54
NARRATOR: Venus and Mercury:
two planets of wonder
668
00:44:17,88 --> 00:44:21,792
but trapped in their own alien hells.
669
00:44:21,826 --> 00:44:23,728
Perhaps not obvious destinations
670
00:44:23,761 --> 00:44:28,199
to discover more
about our home planet,
671
00:44:28,232 --> 00:44:32,03
but that's the beauty of traveling
the solar system;
672
00:44:32,36 --> 00:44:35,740
it's just full of surprises.
54396
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