If I asked you, "What is a planet made of?",
then you'd probably say, "Well, rocks, and iron."
And for the planets of the inner Solar System, like Earth,
close to the heat of the Sun, you'd be right.
But if you head out into the frozen outer reaches of the Solar System,
then even the gases that make up our atmosphere,
so nitrogen and carbon dioxide, and of course water,
are all frozen solid.
And the planets and moons out there, the mountains, glaciers,
and even the crusts of the world themselves are made of that -
solid, frozen, pristine ice.
Ice that, in the extreme conditions we find beyond Earth,
behaves in ways we never imagined possible.
As we've explored the Solar System,
our spacecraft have encountered moons torn apart..
..by great canyons of shifting ice...
..dwarf planets where mountains of solid ice
float across the surface...
..worlds where ice appears to cover one face...
..but leaves the other entirely alone.
And elsewhere, alien aurora hang above the clouds,
all thanks to a strange, newly discovered form of ice.
Even here, on Earth, the behaviour of something
as simple as ice has had, we think, profound consequences,
because without ice's counterintuitive behaviour,
life on our planet may not have survived.
We begin our journey to the ice worlds at the freezing edge
of the Solar System.
Out here, the Sun is so far away, it resembles just another star.
Pluto is so remote that it was only in July 2015 that we had
our first, and to date only, close encounter.
As it flew by, the New Horizons spacecraft sent back
the first close-up images of this mysterious frozen world.
It discovered a great heart-shaped plain 1,000 kilometres across
that dominates one face.
Around the edge of this plain,
mountains made of solid ice tower over Pluto's surface.
And amongst its rugged uplands,
ice was detected in a form no-one ever expected to see on Pluto.
Glaciers.
Flowing rivers of ice on a world so far away,
we expected nothing would be moving.
That's because the temperature here
is only 40 degrees Celsius or so away from absolute zero...
..a temperature at which nothing should move.
And yet New Horizons discovered regions of Pluto
that for all the world look like the frozen reaches of our planet.
So when you fly here over the years, how much does it change?
It changes every day. Yeah? Yeah.
The shape of the glaciers change.
It's never the same.
I'm just imagining flying over Pluto, actually...
..because it looks remarkably similar. Really?
What is the topography like? It's like this.
Same topography, same mountain heights.
That's incredible!
The discovery of Pluto's dynamic icy landscapes came as a huge shock.
It forced us to rethink our understanding of this
so-called dwarf planet.
We're coming in for landing,
so I'll just be talking to the airplane and not you.
I respect that choice.
I've had a lot of landings, but none quite like this.
In fact, none like this at all.
It's the world's most beautiful runway!
Welcome to the glacier, you guys.
Wow!
You know, when we arrived, they said, "Oh, it's zero degrees."
And I thought, "That's great. Zero degrees, it's warm."
Fahrenheit. Zero degrees Fahrenheit. It's about minus 20 up here.
It's just...
And you've got a real sense actually coming in, it looks
frigid and frozen, you know, unmoving, unchanging,
but it's so dynamic.
You can feel it in the wind as you land.
And then, you know, you can see...
You can see the way that everything flows.
Just look at that glacier.
You can almost feel or see it moving.
It looks like a slow-motion river, and indeed it is moving.
It does flow very, very slowly.
And the reason this great mass can grind its way down the valley
is because of the unique properties of the ice from which it's made.
That bright blue ice certainly looks solid.
Immovable.
It's formed by pressure.
So these snowflakes that are falling down
onto the top of the glacier, and over time they build up
and their weight presses down, increasing the pressure,
and you get that particular crystalline structure of ice,
which looks transparent and blue.
But actually, at those pressures and temperatures,
it's not completely solid.
The crystals are sort of arranged in planes,
a little bit like a deck of cards.
And that means that gravity is acting,
trying to slide this whole thing down the valley.
Those planes can slip and slide over each other,
and that allows the whole glacier to move.
You can also get liquid water between the rock and the ice,
and that sort of lubricates the glacier,
and that allows it to slip as well.
So although this looks fixed and immovable, at the conditions
we find on Earth, this can almost behave like a fluid,
sort of sliding very slowly and deforming down the valley.
Glaciers were the last things we expected to see on Pluto.
It's so cold here that we'd expect the ice crystals
to be too brittle to flow.
Nothing should slip, nothing should slide.
Yet that's precisely what these glaciers are doing.
So if they can't be made of water ice, what are they made of?
As New Horizons flew past Pluto,
its detectors picked up an important clue.
These are images of Pluto's surface,
and the colours correspond to different molecules,
different substances that New Horizons detected on the surface.
The purple is methane, the yellow is nitrogen,
and the green is carbon monoxide.
All these gases are frozen solids.
Now, the glaciers on Pluto are primarily made of nitrogen.
Solid nitrogen.
Now, nitrogen is something that we're all familiar with.
It's this stuff. Our air is pretty much made of nitrogen.
So our familiar experience of it is just we can't see it.
But if you cool it down...
..then we can get it pretty easily to turn into a liquid.
Now, if we carried on cooling that down, it would turn into a solid.
Nitrogen freezes at -210 degrees C,
and Pluto's surface temperature, at around -230 degrees,
ensures that glaciers remain solid.
But crucially, the nitrogen ice is just 20 degrees or so
away from its melting point.
That's very similar to the situation here on this glacier.
The glacier is about, well, the air temperature today is about -10,
-20 degrees Celsius. Heat it up by about 20 degrees and it'll melt.
So the temperature difference between the solid nitrogen ice
and the nitrogen gas,
and the solid water ice and the water, is about the same.
That means that, with just a small rise in temperature,
Pluto's nitrogen ice should be able to move.
So the discovery of its glaciers tells us
something remarkable about Pluto.
This tiny world must have a little heat at its core,
a faint warming from radioactive decay,
just enough to gently melt the bottom of these rivers of ice,
sending them on their way down the valley.
I think, for me, there are two lessons
from the exploration of Pluto.
One is that geology finds a way, even so far away from the Sun,
where temperatures are only 40 degrees or so above absolute zero,
pretty much the coldest it can be, there can still be active geology,
particularly where something is close to its freezing point.
In Pluto's case, nitrogen ice.
The second lesson, I think is perhaps even more profound,
is that nature's imagination far exceeds our own.
Nobody expected that they would see such a beautiful, active world
so far away from the Sun on the far icy edge of the Solar System.
The similarities between Earth and Pluto are striking...
..but New Horizons discovered a wonderful difference.
Pluto's glaciers flow through mountains
reminiscent of Alaska's great ranges.
But unlike Mount Denali's granite spires...
..Pluto's mountains are made from frozen water.
But you can't imagine something that big, that high, being made of water.
That's the thing that amazes me. That's crazy!
All water, no rock? Yeah, pretty much, yeah.
And this leads to a surreal twist.
Water ice in the mountains is less dense
than the nitrogen ice in the glaciers.
So in places, we've seen mountains floating on the glaciers,
carried away like icebergs onto the vast ice plain below.
Pluto, a world sculpted by ice.
Leaving Pluto and heading back towards the Sun's glow,
we enter the realm of the ice giants...
..vast gaseous worlds...
..where ice storms rage.
And on the innermost of these planets,
we've discovered a phenomenon eerily reminiscent of home.
Just above Uranus' ice clouds
hang beautiful, ethereal aurora...
..found not at the poles of the planet, as on Earth,
but scattered across its face...
..even around the equator.
So what's creating this beautiful, rare display?
The basic physics of the aurora on Uranus
is the same as the physics of the aurora on Earth.
So the Sun is constantly emitting a rain of high energy
charged particles, which is called the solar wind.
And when those charged particles reach the Earth,
most of them are deflected around the Earth,
harmlessly off into space, by our magnetic field.
Now, the Earth's magnetic field looks very much like the field
around a bar magnet.
I can show you that by sprinkling some iron filings...
..around a bar magnet.
And the iron filings line up with the magnetic field lines.
When the solar wind hits this magnetic field,
most regions of the Earth, it's deflected harmlessly off into space.
But at the poles, those charged particles can become trapped.
And then they can be accelerated down into the upper atmosphere
and hit molecules in the atmosphere, oxygen and nitrogen.
And that can cause those molecules to emit light, to glow.
And that's what, if you're lucky,
you see as the Northern and Southern Lights.
So somewhere, deep inside our planet, lies the equivalent
of that bar magnet.
And, of course, it does, in the form of a hot molten iron core,
spinning away, as the Earth rotates...
..creating electrical currents
and the magnetic field that projects out into space.
But Uranus is different.
The aurora are not found at the poles, and we don't think it has
a molten iron or metallic core to support those electrical currents.
And so the fact that Uranus does have aurora,
and therefore some kind of magnetic field, is a tremendous mystery.
But we do have theories that allow us
to piece together what might be going on.
Imagine diving beyond the clouds of Uranus,
beyond the slushy ice layer that flows around the planet...
..and keep going towards the core.
We enter a region where the pressure approaches several million times
that of Earth's atmosphere...
..and where it's almost as hot as the Sun's surface.
Rather than molten rock or metal, like we find inside our own planet,
we instead find yet more frozen water...
..in a bizarre form of matter known as superionic ice.
Normal water ice has a crystal structure like this.
So the reds are oxygen atoms, the whites are hydrogens,
and you can see that they're bonded together
into this regular crystal lattice.
Within the lattice,
nothing that could carry an electrical current can flow,
so a magnetic field can't be created.
And this is the crystal structure of superionic ice.
The oxygens are still there, bonded together into a crystal,
but now there are hydrogen nuclei, electrically charged protons
that can move freely through the crystal lattice.
That means that this is an electrical conductor.
It's this movement of the protons
that could be contributing to Uranus' magnetic field.
If so, then the superionic ice is, at least in part,
driving the planet's mysterious aurora.
Now, this story is still far from fully understood.
For a long time, this strange form of ice was only a theory.
But then a team pointed one of the most powerful lasers
at a droplet of water
and recreated the conditions that are present deep down inside Uranus,
and, just for a moment, caught a glimpse of superionic ice.
Uranus, a world illuminated by ice.
On the journey between ice worlds, we edge ever closer
towards the Sun, for an encounter with one of the most
thoroughly explored planetary systems of them all.
Saturn's rings are constructed of countless crystals,
ranging in size from just a few microns to vast boulders...
..and all of them made almost entirely from frozen water.
The rings are joined in their orbit by at least 146 moons.
And out towards the edge of the system,
NASA's Cassini probe made one of its most surprising discoveries.
The moon Iapetus resembles a walnut,
with a mountain ridge around its middle.
But that's not its strangest feature.
Back in the 17th century, only about 60 years or so, actually, after
the invention of the telescope, Giovanni Cassini discovered Iapetus.
But he immediately noticed something strange about the moon
as he watched it orbit the planet, because he could see the moon
on one side of the planet, but then on the other side, he couldn't.
Now, being sensible - he was a scientist, after all - he said,
"Well, it's not somehow disappearing.
"There must be another explanation."
And he guessed that one side of the moon must be very bright
and the other side must be very dark.
Now, 300 years later, we sent a spacecraft to Saturn,
bearing his name...
..and we discovered that he was right.
Cassini sent back proof that one side of Iapetus is icy white,
whilst the other looks as if it's been painted black.
So what could be creating such a sharply defined monochromatic world?
It's a tremendous mystery,
but a clue can be found in looking at the line between the two
hemispheres, because there are jet black regions on the surface there
that are also some of the hottest places in the Saturnian system.
Hot is relative, of course.
It's still -140 degrees Celsius on the dark side of the moon.
Now, that's about 20 degrees warmer than the moon's icy face.
And we think that this difference is just enough
to move ice around the moon in a very particular way.
The sunlight falls on that dark surface, as Iapetus rather languidly
rotates, actually, about once every 79 Earth days, and it heats it up.
The water molecules rise up, drift over to the light side,
and then condense, and fall onto the surface, making it brighter
and brighter and brighter, sort of like what's happening here.
So, out there in the Pacific Ocean,
the water is turning into water vapour, drifting over
the cold land, and falling as snow, making the whole surface bright.
On the dark side of Iapetus, ice is warmed
and creates a thin atmosphere of water vapour.
And where this vapour meets the colder, white side of the moon,
it freezes to the surface again, resembling fresh snow...
..maintaining the bright icy white of this hemisphere.
But a mystery remains,
because Iapetus is an ice moon...
..so what is the dark material covering its other face?
In 2009, the Spitzer Infrared Space Telescope discovered this.
This is another ring around Saturn, but it's enormous.
It's one of the largest structures in the Solar System.
This is about 12 million kilometres across.
Later observations from NASA's WISE telescope suggest that
the disc may extend a further 20 million kilometres out into space.
At this vast scale,
Saturn and its more familiar icy rings are barely visible.
It might seem strange that no-one had seen
one of the largest structures in the Solar System until 2009.
The reason is that that ring is very dark and very diffuse.
If you were transported into the ring, you can look around,
and you wouldn't know you were in it.
Spitzer saw it because Spitzer is an infrared telescope,
and so it detected not visible light, but infrared light.
The glow, the heat emanating from the ring.
The giant outer ring is therefore very different
to Saturn's ice rings.
So what is it made of, and where did it come from?
Phoebe is another of Saturn's outer moons,
and each time a passing asteroid gets too close...
..the resulting impact throws dark material out into space.
Over billions of years, numerous impacts have resulted in the
dust from Phoebe spreading around Saturn, forming its vast dark ring.
Iapetus passes through the ring as it orbits,
and so that dark material from the ring
gets deposited on the surface of Iapetus.
This is a really slow process.
Material falls onto Iapetus and increases the size of that
dark layer by about four hundredths of a millimetre every million years.
It's not a bad analogy this, actually.
Some of those sort of dust particles in the ring
are about this size, about the size of a pepper grain.
Some are bigger, a few centimetres across or something,
but it is pretty much stuff like this.
And yet a puzzle remains.
Why half black and half white?
Iapetus spins on its axis once every 79 days
and orbits around Saturn once every 79 days.
It's what's called spin orbit locked. It's like our Moon.
So it always leads with one hemisphere,
as it orbits around Saturn and passes through the ring.
Iapetus, then, is a fluke of nature that exists thanks to
the interaction of two moons within a dark ring,
right at the edge of Saturn's domain.
A world painted by ice.
As we return ever closer to the Sun, ice becomes increasingly rare.
Jupiter has 95 known moons...
..including three large ice worlds.
And one of these is a promising target
in our search for life beyond Earth.
In 2022, NASA's Juno spacecraft flew by Europa and photographed
a world crisscrossed with mysterious red lines.
Grand canyons...
..some 100 metres deep, and tens of kilometres wide...
..in places, coated in a red substance that may be
a newly discovered compound of salt and water.
Juno is the latest NASA mission to fly by Europa
and take detailed photographs of its peculiar, fractured surface.
The canyons on Europa are quite unlike anything seen on Earth...
..or, indeed, anywhere in the entire Solar System.
The markings are geometric.
They form lines that crisscross over the surface,
though what can be causing that pattern?
Europa's surface features are an active area of research, taking NASA
scientists to the frozen reaches of our own planet in search of answers.
This is an image of a region on Europa's surface
called Phaidra Linea.
And you see this feature,
it almost looks like the Grand Canyon on Earth.
It's actually about 50 kilometres across.
A clue to what this is can be seen, if you look at the top line
and the bottom line, and just in your mind's eye,
just draw these together, you'll see that they knit together perfectly.
So this looks like the crust has just spread.
Now, there's only one other place in the Solar System
where we see features like this, and it's here on Earth.
It's caused by plate tectonics.
On Earth, it's the internal heat of the planet as it forces its way
through the crust which is the driving force of plate tectonics.
I mean, no-one expected to see behaviour like this on a moon.
On Europa, it's not molten rock that's driving its plates apart.
Density measurements of the moon suggests
that beneath the thick icy crust lies a different liquid,
a global subsurface ocean of water.
Up to 150 kilometres deep, it may contain two or three times
all the water in Earth's oceans combined.
So how can all that liquid water exist
just below the surface of this frigid ice moon?
The answer lies with two other moons
of Jupiter, with Io and Ganymede.
So here's Jupiter,
and then Io goes around four times...
..as Europa goes around two times, and Ganymede,
farthest out, goes around once.
It's called an orbital resonance.
Four orbits, to two orbits, to one orbit.
That means that these three moons line up periodically
and give each other a gravitational kick,
which means that the orbits don't stay as nice circles.
They're all ellipses.
And that means that tidal effects, just like the tides here on Earth,
stretch and squash the moons, and heat them up.
Now, the effect is strongest for Io,
because that's closest to the giant planet,
and so that turns Io into essentially one giant volcano.
For Europa, further out, that heat melts the ice.
But the energy that goes into Europa from this eccentric,
elliptical orbit around Jupiter, it sort of trickles into the moon.
So it really isn't enough on its own to produce
the very active geology that we see on the surface.
We estimate the surface ice on Europa is somewhere between
10 and 25 kilometres thick.
So whilst the tidal forces are enough for the subsurface ocean
to remain liquid, they're not enough to split apart all this ice.
So to drive the high energy geological processes
we see on the surface of Europa,
then there must be some kind of energy storage in the moon itself.
So I've got two camping stoves here.
These two pans are filled with water,
and it's at the same temperature - zero degrees.
The only difference is that this water has ice in it,
and this has no ice in it,
the only difference when we start the stoves.
This is a thermal camera here cos, you know,
I wouldn't travel without one.
So it will tell us the temperature of the water is rising.
Eight, nine degrees already.
Whereas this one, it's still zero degrees,
even though we're putting all the energy into it.
Here, look!
Ha-ha!
You see that?
So why?
Well, this is a model of ice.
You can see the water molecules here, and here, and here.
And they're bonded together by these longer bonds,
which are called hydrogen bonds.
They're the thing that hold the crystal lattice in place.
And they're pretty strong.
So to melt the ice, you've got to break all these bonds.
You've got to put a lot of energy into it.
So all the energy from this camping stove at the moment is going
into breaking bonds in the ice.
It's not going into making all the molecules
move around faster, which is what temperature is.
So this one is getting hotter and hotter and hotter.
Nothing is happening to this one.
Now, these have been cooking away now, and I'll show you,
I have confidence. I have confidence in physics.
I believe in it.
I would not put my hand in there.
I can see it'd be a stupid idea. But there...
There you go. Physics works.
It's actually freezing.
Now reverse that idea, reverse that argument.
What happens, then, when I freeze water,
when I turn it from a liquid to a solid?
I get all that energy back out again,
huge amounts of energy as the bonds form.
And this is what we think may be happening on Europa.
The subsurface ocean is warmed by tidal forces from Jupiter
and its moons...
..storing energy.
Then, thanks to its elliptical orbit,
as Europa periodically cools, the ice begins to freeze...
..releasing the stored energy.
The volume of the icy crust grows as it freezes...
..increasing the pressure...
..until the entire canyon is cleaved apart...
..and briny water from the ocean below surges up
through the cracks...
..where, bathed in Jupiter's intense radiation...
..it turns red.
You're actually very familiar with this process.
If your pipes burst in your house because they freeze,
where does the energy come from to burst the pipes?
It comes from water freezing into ice.
Europa is far more dynamic than we'd imagined.
And it's this dynamism that makes it a tantalising target...
..in our search for life under the ice.
At its simplest, life needs three things...
..water, energy, and the right chemical ingredients.
Europa has the first two in abundance...
..but the chemistry for life is missing.
But fortunately, Europa is not alone.
Orbiting close by, Io has the missing ingredients
we believe necessary for life in abundance...
..erupting into space in enormous quantities around Jupiter.
Here's where the story gets even more wonderful,
because the volcanoes of Io are constantly producing chemicals,
materials, that rain down onto the frozen surface of Europa,
but if it wasn't for the geology, then they'd be separated forever
from the ocean below by 10 or 20 kilometres of ice.
But that active geology creating the plate tectonic-like behaviour
can bring those materials, those chemicals, into the ocean.
And then we have all the conditions
we think are necessary for the origin of life.
So Europa's dynamic surface
may form part of an extraordinary ecosystem...
..one that stretches from one moon to another.
And work is already under way to send robotic probes
into that distant icy ocean.
It would be a profound discovery to find life on Europa,
but it would also be profound if we didn't,
because everything we think we know about the origin of life, all
the ingredients that are necessary, seem to be present on Europa,
so if we go there and send a cryobot into the oceans of Europa
and find nothing at all, then it may be far more likely that we are alone
for millions or even billions of lightyears in every direction.
Europa, a world completely encased in ice,
couldn't exist much closer to the Sun...
..because just a little closer in lies the Solar System's ice line.
Cross it and temperatures become too warm
for ice to stay frozen for long.
When comets fall inwards towards the Sun,
some of the ice they carry is transformed into water vapour...
..forming tails that streak through space for hundreds of kilometres.
Inside the ice line, then, ice is rare.
But there are places where it can hold on at the margins.
Most of the ice on the surface of Mars is held at the poles.
Here, NASA's Mars Reconnaissance Orbiter has captured
these extraordinary images of a strange phenomenon
that takes place on the southern ice cap...
..dark spider-like formations that we think are being formed
as the seasons turn.
During the winter, it gets so cold on Mars
that the carbon dioxide in its thin atmosphere freezes...
..creating crystals of dry ice that fall as snow on the pole.
Snowfall on Mars is nothing like snowfall on Earth.
Every winter, between three and four trillion tonnes
of carbon dioxide freezes out onto the surface.
That's about 15% of the entire Martian atmosphere.
And then, in the springtime, everything changes.
As the Sun returns in the spring, the ground is warmed...
..and the frozen carbon dioxide vaporises in an instant,
from solid to gas,
geysers of gas, that lift dark Martian dust high into the air.
And it's this dust, as it settles, that's causing the fan-like
spidery marks that we've seen from orbit.
From Mars, it's just a short hop to our own world...
..and Earth too has permanent ice caps at its poles.
But there the similarity ends.
If an alien astronomer got a powerful telescope
and pointed it at our Solar System,
they would immediately see there's something interesting
and very rare about the third planet from the Sun, about Earth,
because they'd see a place like this, a place with mountains
covered in snow, and flowing rivers, and clouds, and rain.
It's a place where water exists in all three of its phases,
solid, liquid, and gas at the same time.
And that's extremely unusual.
Let me show you what I mean.
So I'm going to draw what's called a phase diagram for water.
It has pressure there
and temperature along here.
The Earth sits at one atmosphere pressure,
so atmospheric pressure there.
And it sits at around zero degrees Celsius, give or take.
So the Earth exists somewhere in this region here.
I'm going to draw a line.
I'll tell you what it is after I've drawn it.
So these two lines mark out the region of pressure and temperature
where water can be either a solid, a liquid,
or a gas, or vapour.
And the Earth is here.
Little tiny range where you can have solid, liquid, and vapour.
Mars sits somewhere around here.
So that means that on Mars, water can either be frozen as a solid,
or it can be a vapour,
but it can never be a liquid cos the atmospheric pressure is too low.
Pluto sits around here,
-230 degrees, where water can only be a solid,
frozen hard as steel, building the mountains of Pluto.
On the other hand, Uranus sits somewhere over here
at millions of times atmospheric pressure
and extremely high temperatures.
And there, we get these strange structures of ice,
the superionic ice.
So Earth sits in a very narrow range of temperature
and pressure where water can exist in all three phases.
And that's what makes the Earth unique,
certainly in our Solar System,
and perhaps for hundreds or even thousands of light years beyond.
It's this that allows
a complex ecosystem to exist on the surface of our planet.
Earth's snow-covered mountains,
great oceans...
..rivers...
..and storm clouds can only exist together
thanks to the rare and very narrow temperature and pressure range
that our planet enjoys.
And that's surely necessary for complex life to have emerged
on just one of the Solar System's ice worlds.
But there is one more twist to our story of ice,
a strange property of the everyday ice with which we are so familiar.
Ice on Earth has the unusual property that it floats
on its own liquid.
It's due to that complicated crystal structure
with all those hydrogen bonds.
Now, there are times in Earth's history
when the planet almost froze solid.
But because ice floats, there was always a bit of liquid water
at the base of the ocean, and life could cling on in that liquid.
That means that there has been an unbroken chain of life
for 3.8 billion years, culminating in us.
So next time you stick a few ice cubes in your drink,
just pause for a second and give a thought to the wonder of ice.
The three key ingredients that you need for life are,
number one, liquid water, two, a source of energy,
and three, various chemical elements that we associate with life.
And we think that Europa has all of these ingredients.
Juno has deepened our knowledge of Europa,
but the mission is due to end in 2025.
While we are yet to find any evidence of life on Europa,
it's clear that this icy moon is worth a closer look.
Sam Howell is part of a NASA team scoping a hugely ambitious attempt
to explore the moon and its subsurface oceans
in search of that elusive proof.
It's all a guess until you go swimming in it,
but we're building this picture up where we understand
how salt water and rock interact on Earth, and the chemistry
that produces, which is likely important to the emergence of life.
How are we going to prove that?
We're launching the Europa Clipper mission, and that will,
in the early 2030s, arrive at Jupiter and orbit Jupiter,
surveying the entirety of the world.
Europa Clipper is the first dedicated mission to Europa.
And, in fact, it's the first dedicated mission to any icy moon.
Europa Clipper is set to launch
from the Kennedy Space Center in October 2024.
And we have a payload of ten instruments that are going to
work together to characterise Europa's icy surface,
its ocean, what their compositions are, and to figure out
if Europa has environments that could support life.
Any time you're anywhere near Jupiter, it's really dangerous.
These high energy particles that are zipping around
can hit your spacecraft and damage it.
And that's one of the big challenges facing Europa Clipper.
And it's not just the spacecraft
that must survive Jupiter's onslaught.
We know that this intense radiation,
that's bad for life as we know it, life as we are,
but maybe life on Europa doesn't mind it too much.
But what's more likely is that the thick layers of ice
that are at Europa's surface shield life in the subsurface ocean.
We think that the icy crust is 18 miles thick,
but Europa Clipper will tell us more.
I'm really excited about learning about Europa's plumes.
I think they could be the key to sampling the subsurface ocean.
We'll figure out if there are traces or ideas of life in those plumes,
and that's something we're going to be able to do
with this amazing spacecraft.
Clipper will only ever survey Europa from afar,
but future missions are being developed that, one day,
may land on the surface and explore beneath the ice.
There is no ice on this planet that behaves like the surface of Europa.
There, the ice is so thick and so hard
that the upper few miles are like concrete or rock.
What we really look at are ways to pack enough heat
into a cylindrical probe
so that it can melt all the way to that ocean, but can also carry
along the scientific payload with us that we want to use to explore.
So is this recording video now? Yes, absolutely.
Ah... Oh, yeah.
I don't know if you've ever seen yourself on camera before,
but there you go. Ha-ha! Hello!
We're just going to deploy it there, right into the hole, and...
..good luck.
And then there we go, we're down in the lake.
We're looking around the interface of the ice
and water just beneath us.
Finding life on Europa would be extraordinarily profound,
because it's almost guaranteed that that would be
a separate instance of an origin of life.
So Europa could teach us a lot about how life begins
across the universe.
Next time...
..a powerful force creating oddball worlds...
..of bizarre shapes...
..and hidden secrets.
These are the Solar System's Strange Worlds.