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Jane: This is But Why: a Podcast
for Curious Kids from Vermont

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Public. On this program, we take
questions from curious kids just

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like you, and we find
interesting people who can offer

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some answers. In this episode,
we're going to look far, far

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beyond our field of vision and
think about our solar system.

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There's so much out there to
explore and learn more about,

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and scientists are still
discovering new things all the

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time. So get ready for some
virtual space exploration. While

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it might be more fun to actually
be an astronaut who gets to

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explore space in person, this
way we all get to participate.

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And actually, we're going to go
farther out in the universe than

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any humans have ever been, so
strap in. To orient ourselves,

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our solar system is anchored by
the sun. The sun is the star at

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the center of our solar system.
It's the gravitational force

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that pulls planets toward it.
The eight planets in our system

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orbit or travel around the sun.
We're going to explore those

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eight planets today, and we have
a special guide for our journey.

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John: My name is John O'Meara,
and I am the chief scientist at

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the W.M. Keck Observatory on the
island of Hawaii. I am part of

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the team that helps run one of
the biggest telescopes on the

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planet, the mirror itself is
about 10 meters across, so about

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you know almost 40 feet across,
and and then the dome that it

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sits in this giant structure
that keeps it safe.

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Jane: Can you see some of the
planets through the telescope?

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John: Oh, totally. We we look at
the planets in our solar system

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a lot because because they're so
close by, relatively speaking. I

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mean, they're very far in terms
of how long it would take to fly

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there in an airplane if that
worked. But because they're

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close by, we can watch them
change over time. We like to

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look at Jupiter a lot. We like
to look at Saturn a lot, and

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Uranus and Neptune a lot. The
planets which are closer to the

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sun than us are hard for us to
look at because the sun is so

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bright and because we don't want
to damage the telescope. So we

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don't look at Mercury and Venus
very often, but most of the

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time, it's it's the planets
farther away, and their moons.

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We really like to look at their
moons.

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Jane: I am glad that you can see
the planets from the telescope

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because we called you up to talk
about planets today, because

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kids have a ton of questions
about planets. So we're gonna

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see how many we can get to,
because we have so many. I don't

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know if we can fit it all in, so
we're gonna yeah we're gonna

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make you go rapid fire, John,
but we're gonna make you, we're

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gonna make you work here. So the
first question we have is from

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Chandler.

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Chandler: How did the planets in
our solar system get made?

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Rey: My name is Rey. I'm from
Encinitasts, California. and I'm

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six years old. How do planets
form?

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Maren: Hi, my name is Maren. I'm
nine years old. I'm from

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Westfield, Massachusetts. Where
do planets come from?

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John: Yeah, Chandler asks, and
and and the other folks are

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asking a really, really fun,
fantastic question, and part of

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the reason why it's fun and
fantastic is we kind of know the

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answer, but we don't completely
know the answer. And part of the

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reason why we don't completely
know the answer is because this

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happened billions of years ago
when the solar system formed. So

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the the best model that we have,
the best theory that we have is

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that the sun and the planets
formed out of what we call a

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nebula. A nebula is just a term
for a bunch of gas and stuff.

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And about 5 billion years ago,
that nebula, for some reason,

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started to collapse. It was just
kind of sitting there, and then

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parts of it started to collapse,
and then gravity started to take

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over, and stuff got closer and
closer and closer. And most of

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the stuff became the sun. About
99% of the stuff became the sun,

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but some of the other stuff
formed a disk around the sun,

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mostly of rock and ice and dust
and gas, and that stuff started

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to form into the planets a few
100 million years after the sun

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started to form. And that disk
of stuff, which had millions and

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millions and millions of chunks
in it, billions, 10s of billions

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of chunks, eventually gravity
started to pull those pieces

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together. Stuff started banging
into each other, and over

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hundreds of millions of years,
the planets in our solar system

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formed. But we didn't see this
happen. We weren't there yet,

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but we've used big telescopes on
the ground and in space to see

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this process happening in other
solar systems as they're being

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born, and we can see this disk
of stuff, and we can see it

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start to clump up, and so that
helps reinforce this idea that's

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that's how our solar system
formed. But it's still, you

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know, it's it's still just you
know something that we have to

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keep testing, we have to keep
looking, we have to pick up as

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much material as we can
throughout the solar system,

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whether or not it's a rock on
Mars or it's a chunk of a comet

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or an asteroid. We need to go
out there, look at that

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material, and see if it matches
this idea for how the solar

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system formed.

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Gabby: Hi, my name is Gabby. I'm
six years old. I live in

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Colorado, and my question is,
why are some planets made of gas

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and some planets are not?

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John: If you look at the planets
in the solar system, the ones

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that are closer to the sun are
mostly made of rocks. So Mercury

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is made of rocks. Venus, we
can't see the surface of from

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here because it has really,
really thick clouds. But most of

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it is rocks. Most of the Earth
is rocks. Mars is mostly rocky.

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But then, when you go farther
out in the solar system, like

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Gabby says, there's there's
these giant balls of gas, like

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Jupiter, the biggest planet in
the solar system, Saturn,

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Uranus, Neptune-these are giant
things of gas. Why is that so

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different? And it has to do with
how close the things were to the

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Sun when they formed. When
you're really close to the Sun,

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relatively speaking, it's
hotter. The Sun is brighter when

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you're closer to it, and that
energy doesn't let gas start to

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form into ice and ice to start
capturing more gas. It only lets

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the rocks stick around, and so
in the early parts of the solar

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system, that energy from the sun
only let rocky things start to

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form close by. But when they
were far enough away that they

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could that ice could form. Ice
did form, and ice is really,

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really good at grabbing other
stuff, grabbing other ice or

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other gas. And so, kind of like
when you build a snowman, you

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start to push the snow, and it
starts to glom onto it and get

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bigger and bigger and bigger.
That snowball method is how the

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big gas giants formed out in the
solar system, and they just

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captured all that gas. Now the
other part of the question was

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why? Why does it even happen at
all? And the answer there is

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gravity. The same thing that if
you you know if you jump off of

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a step onto the ground, you
know, gravity is pulling you

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down towards the the center of
the Earth because the Earth has

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a lot of mass, and because you
have mass. And whenever two

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things have mass, they get
attracted to each other by

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gravity. And so, when stuff
started to form, there was more

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and more and more mass, and the
gravity nearby it got stronger

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and stronger, and all of that
stuff held together to keep the

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planets held together. It's the
same as true for the sun. The

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sun isn't rocky at all. It's
mostly gas and very, very hot

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gas, depending on where you are
in the sun. But gravity is

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what's holding it together.

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Jane: So the planets and the sun
are being held together by

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gravity, but they are also
moving in space. Planets orbit

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or travel around the sun in a
kind of oval or elliptical

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pattern. Some orbits are almost
circular, but most are kind of

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stretched-out ovals. The size of
the orbit depends on the

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distance from the planet to the
sun. But Why and how do they do

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that?

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Penny: This is Penny from
Chappaqua, New York. My question

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is: How do planets float in
space?

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Malcolm: Hello, my name is
Malcolm. I live in Seattle,

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Washington. My age is seven. My
question is: How do planets stay

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in place?

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Ruby: My name is Ruby, and I'm
four years old, and I live in

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Seattle, Washington. And my
question is, how do the planets

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get out of the spot?

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Oliver: Hello, my name is
Oliver. I'm seven years old, and

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I'm from Wellington, New
Zealand. And my question is, why

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do planets spin?

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Larry: My name is Larry, and I
am five years old. I'm from Los

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Angeles, California. Why do the
planets rotate?

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John: It goes back to that model
of how we think the solar system

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formed. So when the stuff
started to collapse, it also

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started to rotate. It started to
spin around a little bit. And

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when we look at the disks of
those early solar systems going

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around stars, we see that
they're moving around, kind of

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like a record on a record
player. When you start spinning

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around, the universe likes to
keep you spinning around. So all

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you have to do is start that
rotation. People know this, like

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when they go out ice skating and
and they they put their arms out

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really wide, and if you start to
spin, you you will keep spinning

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because you know you don't have
a lot of friction slowing you

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down on the ice. In space
there's no none of that friction

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at all, so you keep spinning
around and around. But one neat

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thing happens if you pull your
arms in, you start to spin

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faster, and that has to do with
something called momentum and

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and rotational momentum. It's
the energy that's locked up in

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movement. We have movement in
straight lines, which is is

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regular momentum, and rotational
momentum is when you're spinning

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around. If you pull your arms
and you spin faster, here's a

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neat thing: the planets closer
to the sun orbit around the sun

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faster than the planets farther
away from the sun. So the Earth

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takes about a year to go around
the sun, but the planets

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outside, farther outside in the
solar system, take 10s up to

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hundreds of years to go around
the sun.

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Jane: I thought maybe they were
just taking longer to go around

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the sun because they're so much
farther away, but they're

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actually orbiting slower, so
they have a longer path to

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travel to get around the sun,
but they're doing it at a slower

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pace too. It's like the planets
close to the sun are sprinting,

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and the ones farther out are
just taking a nice leisurely

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stroll.

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Oliver: Hi, my name is Oliver.
I'm almost five, and I live in

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St. Louis. And why does space
have so many planets?

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Jeremiah: I'm Jeremiah. I'm six
years old. I'm from Alexandria,

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Virginia, and my question is:
Why does space have so many

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planets?

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John: That's a great question,
and and if if I can I'll answer

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in two different parts because
there's there's a there's a neat

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thing that we're starting to
learn about in astronomy right

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now about planets around other
stars but let me start with the

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solar system. When the solar
system started off there were

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many many many more planets than
there are today and that's

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because the stuff started
falling in together and glomming

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together like snowballs forming
a giant snowman, and some of

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them smacked into each other and
got kicked out of the solar

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system entirely. But over
hundreds of millions of years,

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these things formed into much,
much bigger things, which we now

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call planets. One piece of the
solar system that still kind of

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looks like that early part of
the solar system is called the

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asteroid belt. It's a place
between Mars and Jupiter. If

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you're going away from the sun,
Jupiter's farther away than

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Mars. In between there, there's
all these asteroids, millions of

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them, giant chunks of rock, and
those are leftover material from

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the formation of the solar
system. They didn't quite form

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into a planet, and they didn't
quite get kicked out. And in a

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very, very long time from now,
they'll slowly start getting

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thrown out of the solar system,
or bounce into each other, or

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bounce into Jupiter, or bounce
into Mars, bounce into other

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things. Most of them will get
thrown out. But that process

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over billions of years took us
from hundreds of millions of

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objects into the solar system
into a few dozen that are that

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are now planets or dwarf
planets. The other fun thing is

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that now that we've looked in
detail at other stars, we think

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that almost every star in the
universe has at least one

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planet, and that most stars in
the universe have more than one

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planet. And that's probably a
different discussion for a

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different time. But it's really
neat to know that our solar

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system isn't alone in terms of
having planets.

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Jane: So we don't even know how
many planets there are if we're

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thinking outside our solar
system.

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John: We don't know. That's one
of the things we like to do a

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lot with the telescope here in
Hawaii is is to look for planets

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around other stars and find more
of them and more of them and

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more of them.

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Jane: Do you have a guess?

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John: I have a rough guess, and
the rough guess is that if I if

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I use a trick and say every star
has at least one planet, and if

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I think I know how many stars
there are in our galaxy, which

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is about 200 billion stars, but
notice I said about we don't

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really know we can't count them
one by one we use we use little

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tricks in math to do that, but
that means there are at least

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200 billion planets in the Milky
Way, and we think in the in the

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universe that we can see, we can
see at least a few 100 billion

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galaxies. So now you need to get
out your your your your

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calculator or a piece of paper
and start writing a lot of

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zeros, because if every galaxy
has a couple 100 billion stars,

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and all of those stars have at
least one planet, then we're

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we're we're talking about 200
billion times 200 billion times

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a lot, and so that's a lot a lot
of planets in the in the

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universe.

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Isaac: My name is Isaac from
Saskatchewan, Canada, and I'm 10

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years old. How did humans figure
out about planets?

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Jane: How did humans even figure
out about planets to begin with?

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John: So, planet is that the
word planet in English is

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derived from the Greek language,
but from from way back when.

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That is is is a word that means
wanderer, and when we look up at

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the night sky, and and and and
humans have been really good at

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looking at the night sky since
since there have been humans

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because it's always there,
always there to to see the stars

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and and to look up and and and
and be really interested and

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excited about that. But when you
look up at the stars and you

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look long enough, you'll see
that most of them are stuck in

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the exact same spot they were
the night before, or the week

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before, or the month before. But
you will see some bright things

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move; they wander on the sky,
and so we we call those things

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planets. And human beings, for
for most of history that that

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that that's been recorded, could
only see some of the planets in

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our solar system. Uranus and
Neptune are so far away that we

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can't see them with our eyes and
know that they are planets.

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Then, in about the 1600s, in the
early 1600s, we started to build

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telescopes, and when you build
telescopes, you can look in more

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detail and you can see fainter
things. And that's when we

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really started to study planets
well and understand that some of

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them were made of gas and some
of them were made of rocks.

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Because at the same time as we
were developing telescopes, we

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were developing new types of
physics and chemistry, and all

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the things that you need to tell
the difference between a rock

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and a bunch of gas that's
hundreds of 1000s of millions of

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miles away-stuff that you can't
reach out and touch yet-and then

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we started to build rockets, and
we put robots on rockets, and we

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landed them in places in the
solar system and grabbed that

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stuff and tested those theories.

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Jane: All right, now that we
have some understanding of our

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solar system and how it formed,
we're going to go on that tour

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of all the planets. So get a
drink of water, take a break

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because there's going to be a
lot to get through when we come

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back.

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This is But Why. Today we're
talking with astronomer John

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O'Meara, who helps run one of
the biggest telescopes in the

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world at the Keck Observatory in
Hawaii. All right, John, let's

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talk about specific planets, and
we're going to start with the

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planets closest to the sun and
move outwards. So the planet

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closest to the sun-I know some
of the kids who are listening

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are like shouting it out
already-is Mercury.

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John: Yeah.

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Jane: We don't have any
questions about Mercury. Why do

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00:18:26,745 --> 00:18:28,545
you think that is? We have
questions about every other

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planet. Why isn't anybody
sending us questions about

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00:18:30,555 --> 00:18:33,105
Mercury? Is it really not very
cool?

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John: Mercury's totally cool. I
think part of the issue is we

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haven't sent many spacecraft to
Mercury, so we don't have a lot

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00:18:40,425 --> 00:18:44,280
of pictures of Mercury up close,
like we do for Venus or Mars or

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00:18:44,280 --> 00:18:50,550
the other planets in in close to
us, or Jupiter, or or Saturn or

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Uranus or Neptune. And Mercury's
really close to the Sun, which

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means it's kind of a nasty place
to visit, and it's also hard to

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see with your eyes. There's only
special times of year that you

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00:19:03,690 --> 00:19:07,035
can see Mercury at all because
it's so close to the sun, and

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sun the sun is really bright. So
the sun has to set, and you have

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to have Mercury in special parts
of its orbit to see it at all.

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So I think all those things put
together make you know kind of

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stack the odds against Mercury.
But we have spacecraft that are

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00:19:23,445 --> 00:19:26,655
there now, looking, you know,
starting to to orbit around

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00:19:26,655 --> 00:19:30,060
Mercury and study it, and it's a
really fascinating place because

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how do you have a planet that
close to the sun and still have

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00:19:32,670 --> 00:19:34,500
it around and all that stuff?
It's kind of neat.

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Jane: All right, you sold me on
Mercury. Maybe we'll get some

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00:19:36,950 --> 00:19:40,450
Mercury questions and we'll have
you back. Let's go next. Travel

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00:19:40,570 --> 00:19:41,800
outwards to Venus.

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Rylo: Hi, my name is Rylo. I'm
five years old. I live in

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00:19:45,750 --> 00:19:51,480
Glendale. Why is Venus the
hottest, but it's not closest to

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00:19:51,480 --> 00:19:52,290
the sun?

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00:19:52,330 --> 00:19:56,260
Jane: Why is Venus the hottest,
but not closest to the sun?

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Because you just said Mercury
was closest to the sun.

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John: Yeah, Mercury is really
close to the sun, and it's not

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00:20:02,650 --> 00:20:06,670
as hot. And part of the reason
is that Mercury only has a very,

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very, very tiny atmosphere.
Venus, on the other hand, has a

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00:20:12,280 --> 00:20:17,230
very thick, heavy atmosphere. In
fact, Venus is about the same

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00:20:17,230 --> 00:20:24,145
size as the Earth, but it has an
atmosphere which is 90 times as

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00:20:24,145 --> 00:20:27,805
thick as our atmosphere, and
what do I mean by thick? I mean

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there.

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00:20:27,925 --> 00:20:29,635
Jane: And what do you mean by
atmosphere?

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00:20:29,540 --> 00:20:33,980
John: Yeah, what do I mean by
atmosphere? So you and I are

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00:20:33,980 --> 00:20:36,950
sitting here breathing air, and
the air is mostly made of

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00:20:36,950 --> 00:20:41,180
nitrogen and a little bit of
oxygen, some carbon dioxide, and

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00:20:41,180 --> 00:20:46,310
that air is for a few 100 miles
above the Earth, and it gets

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00:20:46,310 --> 00:20:49,040
less and less atmosphere as you
get farther and farther away

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00:20:49,040 --> 00:20:53,315
from the surface. But that air
has a quantity called pressure,

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Jane: John, you and I have
talked in previous episodes

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and we know we have pressure
because if you take your hand

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and you swipe it through the
air, you can actually feel the

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00:20:57,785 --> 00:21:01,235
wind against your hand, and
that's because there's enough

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00:21:01,235 --> 00:21:06,095
air there to feel that that
material. If you tried to do

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00:21:06,095 --> 00:21:09,995
that on Venus, you would have to
work a lot harder because the

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air is much more dense. It's
almost like water. It's very,

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00:21:14,615 --> 00:21:19,340
very, very dense, and most of
the atmosphere on Venus is made

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00:21:19,340 --> 00:21:24,560
out of carbon dioxide instead of
nitrogen and and oxygen. Carbon

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dioxide is really good at
grabbing heat and keeping it

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00:21:29,780 --> 00:21:34,910
there. A long time ago, it used
to have we we thought think it

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00:21:34,910 --> 00:21:38,030
used to have oceans on its
surface or at least some water,

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00:21:38,645 --> 00:21:43,835
and then something happened to
evaporate that water away and to

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00:21:43,835 --> 00:21:47,255
change the atmosphere, and it
had lots of volcanoes, dumped a

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00:21:47,255 --> 00:21:50,585
lot of carbon dioxide into the
atmosphere, and then that

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00:21:50,585 --> 00:21:54,665
trapped the heat, and this is
this ran away. This this didn't

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00:21:54,665 --> 00:21:59,045
circulate. This kept getting
more and more and more and more,

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00:21:59,045 --> 00:22:02,960
and we call that the runaway
greenhouse effect, and that

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00:22:02,960 --> 00:22:09,980
makes the surface of Venus
hundreds of degrees. It is very

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00:22:09,980 --> 00:22:14,510
very hot. That pressure is very
very high. We've landed a couple

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00:22:14,510 --> 00:22:19,040
of spacecraft on Venus, and
those spacecraft only survived a

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00:22:19,040 --> 00:22:24,020
very short time because it was
so hot and so dense that they

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kind of crushed the spacecraft
after a bit of time, even though

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00:22:27,065 --> 00:22:31,655
we built them to sort to to to
really handle that environment.

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00:22:31,655 --> 00:22:38,375
So we don't completely
understand why that started on

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00:22:38,375 --> 00:22:43,985
Venus, but we understand the
physics of atmospheres to

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00:22:43,985 --> 00:22:48,455
understand once it kicked off
why it it stayed that way, and

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00:22:48,725 --> 00:22:52,010
what's really interesting about
Venus is that the surface is

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00:22:52,010 --> 00:22:55,940
nasty. It rains acid on Venus.
You don't want to be there, I

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00:22:55,940 --> 00:23:01,190
promise. But high up enough, the
atmosphere starts to get thin

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00:23:01,190 --> 00:23:07,310
again, and there's parts of up
and above the clouds in Venus

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which are about the same
temperature as the Earth, and

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you know kind of a nice place to
be. And so we are we are

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00:23:12,035 --> 00:23:37,730
about the Earth's moon and other
things about Earth's atmosphere,

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00:23:14,405 --> 00:23:19,295
building some spacecraft. NASA
is working on two spacecraft

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00:23:19,295 --> 00:23:23,255
that will be launched to Venus
to study those clouds as well as

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00:23:23,255 --> 00:23:27,125
the surface, which we've looked
at before with radar and by

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00:23:27,125 --> 00:23:29,795
landing some stuff on it.

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and we've done a lot of episodes
that kids can listen to about

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00:23:41,420 --> 00:23:43,940
Earth's atmosphere and our moon.
So we're we're not going to

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focus a lot on Earth today, but
I have one question from Eli

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00:23:48,290 --> 00:23:51,830
that we want to share with you
that will help tie us from Venus

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to Earth, which is the next one
out, and then to Mars, which is

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the next planet out.

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Eli: My name is Eli. I'm seven
years old. I live in Cleveland,

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00:24:03,540 --> 00:24:10,260
Ohio. Why is Earth more like
Mars than Venus, its sister

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00:24:10,410 --> 00:24:10,860
planet?

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00:24:11,540 --> 00:24:15,560
John: So the three planets are
very, very different from each

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00:24:15,560 --> 00:24:19,790
other. You're absolutely right,
and part of that difference is

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what we were talking about with
Venus before that it had this

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00:24:22,700 --> 00:24:26,030
this very big change in its
atmosphere that made it really

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00:24:26,030 --> 00:24:29,960
dense and really hot. On the
other hand, we have Earth, which

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we know pretty well, and then we
have Mars, which is very cold

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00:24:34,895 --> 00:24:38,315
relative to Earth, or certainly
relative to Venus, and it

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00:24:38,315 --> 00:24:41,525
doesn't have to do with their
distance from the Sun very much

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00:24:41,525 --> 00:24:45,335
because they're all kind of
close to the sun, roughly the

378
00:24:45,335 --> 00:24:52,175
roughly about the same. The
difference is that Mars had a

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00:24:52,175 --> 00:24:56,555
different kind of event a long
time ago, about a billion years

380
00:24:56,555 --> 00:25:00,920
ago, in which it lost its
atmosphere. It didn't start

381
00:25:00,920 --> 00:25:05,360
rapidly gaining thickness in its
atmosphere like Venus did.

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00:25:05,360 --> 00:25:10,970
Something happened to strip away
a lot of Mars's atmosphere, and

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00:25:10,970 --> 00:25:17,240
that really changed Mars
relative to Earth and Venus.

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00:25:17,240 --> 00:25:20,675
Mars used to have oceans on it.
We we believe this when you look

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00:25:20,675 --> 00:25:23,975
at at the at the surface
features of Mars, and we dug

386
00:25:23,975 --> 00:25:27,365
into a little bit of the surface
of Mars with rovers and other

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00:25:27,365 --> 00:25:32,435
things, we know that Mars
probably had oceans on it and an

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00:25:32,435 --> 00:25:36,605
atmosphere that kept those
oceans from just boiling off and

389
00:25:36,605 --> 00:25:41,135
going off into space. But
something took that atmosphere

390
00:25:41,135 --> 00:25:43,370
away, and this is why studying
planets is so cool. Is because

391
00:25:43,370 --> 00:25:47,690
we don't know yet why these
things happened, but when you

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00:25:47,690 --> 00:25:51,290
stripped away that atmosphere
and the oceans evaporated off of

393
00:25:51,290 --> 00:25:54,800
Mars, Mars still has an
atmosphere, but it's only about

394
00:25:54,800 --> 00:25:59,720
1 percent as thick as the
atmosphere on Earth.

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00:25:59,720 --> 00:26:02,240
Jane: Ooh, hold up for a second.
Let's squeeze in Jamison's

396
00:26:02,240 --> 00:26:03,320
question right here.

397
00:26:03,320 --> 00:26:06,530
Jameson: I live in the United
States of America. I am 10 years

398
00:26:06,530 --> 00:26:10,115
old, and my question is: Why is
Mars so cold?

399
00:26:10,115 --> 00:26:12,815
John: Because the atmosphere
can't trap that heat in and keep

400
00:26:12,815 --> 00:26:13,775
things warm.

401
00:26:13,775 --> 00:26:19,055
Ilina: Hi, my name is Ilinaa.
I'm six years old. I live in

402
00:26:19,715 --> 00:26:25,595
Newtown Square, Pennsylvania.
and my question is why is Mars

403
00:26:25,595 --> 00:26:26,915
red?

404
00:26:27,080 --> 00:26:30,320
John: Mars has this this kind of
eerie reddish color, and the

405
00:26:30,440 --> 00:26:34,430
main reason why it has that
color is because a lot of the

406
00:26:34,520 --> 00:26:40,250
surface on Mars has iron in it,
in the sands, in the rocks, and

407
00:26:40,370 --> 00:26:44,050
and all throughout the surface
has iron in it. But you can say,

408
00:26:44,170 --> 00:26:47,620
well, wait, I have a I have a
cast iron pan at home, and it's

409
00:26:47,800 --> 00:26:52,630
black. Well, it's black unless
you just leave it in water or

410
00:26:52,720 --> 00:26:55,330
leave it out in the air for a
long time, and then it starts to

411
00:26:55,540 --> 00:26:59,830
rust. This is what happens when
oxygen interacts with iron over

412
00:26:59,890 --> 00:27:04,050
a long time: is it turns into
rust, iron oxide, and so the

413
00:27:04,080 --> 00:27:08,220
surface of Mars is that color in
part because the iron started

414
00:27:08,370 --> 00:27:11,940
rusting in the atmosphere of
Mars, leaving it that weird

415
00:27:12,030 --> 00:27:12,540
reddish color.

416
00:27:13,890 --> 00:27:15,420
Jane: Okay, what about dust
storms?

417
00:27:15,630 --> 00:27:22,800
Levin: My name is Levin, and I'm
four years old and live in

418
00:27:22,800 --> 00:27:29,580
Boulder, Colorado. I want to
know more about why dust storms

419
00:27:29,580 --> 00:27:32,040
happen on Mars.

420
00:27:32,150 --> 00:27:35,300
John: We get dust storms on
Earth, like in this in the

421
00:27:35,300 --> 00:27:38,930
Sahara and other deserts. We see
this a lot, where these these

422
00:27:39,050 --> 00:27:42,550
big winds will kick up the sand
into the air, and lots of Mars

423
00:27:42,610 --> 00:27:48,250
is covered in in sand. And the
there are winds on Mars, even

424
00:27:48,250 --> 00:27:51,670
though there's only about 1% the
the atmospheric pressure. There

425
00:27:51,670 --> 00:27:55,750
are still winds there, and when
sometimes the winds can get very

426
00:27:56,050 --> 00:28:00,600
very powerful relative to just a
normal day on Mars, that kicks

427
00:28:00,780 --> 00:28:04,110
up the dust, and then these
these massive dust storms go

428
00:28:04,350 --> 00:28:07,230
through. And so, when you look
at the surface of Mars, you can

429
00:28:07,350 --> 00:28:10,140
see things which are basically
sand dunes, and they were put

430
00:28:10,230 --> 00:28:14,370
there by these by these giant
dust storms. Mars has seasons

431
00:28:14,490 --> 00:28:17,880
like Earth does. When the winds
come, you know, and and you can

432
00:28:18,480 --> 00:28:20,700
pick up the sand, you get these
massive dust storms.

433
00:28:20,880 --> 00:28:23,120
Jane: All right, so we're going
to jump back in our futuristic

434
00:28:23,240 --> 00:28:26,750
spaceship now that can amazingly
go to and from all the planets.

435
00:28:26,780 --> 00:28:29,960
We're going from Mars. How far
do we have to go to get to the

436
00:28:30,020 --> 00:28:31,130
next planet, Jupiter?

437
00:28:31,450 --> 00:28:34,420
John: Well, we have to go pretty
far. So let's use units that

438
00:28:34,420 --> 00:28:38,470
that I like to describe the
solar system because because we

439
00:28:38,470 --> 00:28:43,030
live on Earth, we can say the
Earth is one unit away from the

440
00:28:43,030 --> 00:28:49,000
Sun. Venus is about 0.7 units
away from the Sun, about a

441
00:28:49,000 --> 00:28:53,440
little bit more than half a
unit. Mars is 1.5 units away

442
00:28:53,440 --> 00:28:57,385
from the Sun. You have to go
pretty far now. You have to go

443
00:28:57,385 --> 00:29:01,855
five units away from the Sun to
get to Jupiter, and that's the

444
00:29:01,855 --> 00:29:06,085
big one in the solar system.
That's the biggest planet there

445
00:29:06,085 --> 00:29:11,005
there is in the solar system. It
has most of the material locked

446
00:29:11,005 --> 00:29:15,175
up in it relative to all the
other planets, which is which is

447
00:29:15,175 --> 00:29:17,530
pretty amazing because you know
we think oh Saturn's big yeah

448
00:29:17,530 --> 00:29:22,870
Saturn's big but Jupiter is big,
and Jupiter is kind of was was

449
00:29:22,870 --> 00:29:26,440
very much along with the sun
like a vacuum cleaner for the

450
00:29:26,440 --> 00:29:30,010
solar system. When there was all
that material out in the disk,

451
00:29:30,010 --> 00:29:33,100
if that stuff didn't start to
form into into their own

452
00:29:33,100 --> 00:29:36,940
planets, Jupiter's gravity,
because it's so big and so

453
00:29:36,940 --> 00:29:40,030
massive, helped pick up that
stuff, and that stuff got

454
00:29:40,075 --> 00:29:44,845
incorporated into Jupiter, so it
is a big, giant gas planet. It's

455
00:29:44,845 --> 00:29:49,615
made out of hydrogen and helium,
and we think it has a rocky core

456
00:29:49,615 --> 00:29:55,285
inside of it, but it's it's
huge, and its mass has really

457
00:29:55,285 --> 00:29:59,215
impacted the whole shape of the
rest of the the solar system. It

458
00:29:59,215 --> 00:30:01,675
and the sun are the two big
bullies of the solar system

459
00:30:01,675 --> 00:30:02,935
pushing stuff around.

460
00:30:02,990 --> 00:30:07,730
Griffin: My name is Griffin, and
why is the storm on Jupiter red?

461
00:30:07,730 --> 00:30:10,670
Jane: And maybe you can help
explain for kids who don't know

462
00:30:10,670 --> 00:30:12,230
about Jupiter's storms.

463
00:30:12,780 --> 00:30:17,190
John: Jupiter is made out of a
lot of gas, and Jupiter rotates

464
00:30:17,550 --> 00:30:23,360
pretty fast. So on Earth, we
have these things called

465
00:30:23,420 --> 00:30:27,050
hurricanes or cyclones, and
hurricanes have their shape,

466
00:30:27,170 --> 00:30:30,500
these spirally shapes that are
spinning around because the

467
00:30:30,530 --> 00:30:33,020
Earth is spinning around. It's
it's it's a thing called the

468
00:30:33,080 --> 00:30:37,520
Coriolis effect. Well, Jupiter
is spinning around pretty fast,

469
00:30:38,450 --> 00:30:42,460
and it's a really really big
planet, so it can have

470
00:30:42,610 --> 00:30:46,810
hurricanes. On Earth, our
hurricanes usually only last a

471
00:30:46,900 --> 00:30:51,460
few weeks, maybe a month from
start to finish. The Big Red

472
00:30:51,670 --> 00:30:56,260
Spot has been a hurricane in
Jupiter's atmosphere that's been

473
00:30:56,350 --> 00:31:00,100
around for hundreds of years.
What's really neat, though, is

474
00:31:00,250 --> 00:31:03,000
because we've now got telescopes
that can look at Jupiter all the

475
00:31:03,120 --> 00:31:07,320
time and look at it at and watch
the spot. It's changing its

476
00:31:07,440 --> 00:31:11,100
shape. In fact, it's starting to
get smaller, and so maybe in a

477
00:31:11,160 --> 00:31:15,270
couple 100 years there won't be
that big red spot. Part of the

478
00:31:15,330 --> 00:31:19,110
question was why is it red? The
reason why it's red has to do

479
00:31:19,200 --> 00:31:23,090
with just slight differences in
in the atoms that make up the

480
00:31:23,390 --> 00:31:25,850
atmosphere and slight
differences in the temperature

481
00:31:25,970 --> 00:31:29,930
and the pressure of that, which
can change the relative color of

482
00:31:30,140 --> 00:31:33,890
of that gas. But for me, it's
it's kind of fun to know that

483
00:31:34,400 --> 00:31:36,710
you know for hundreds of years
we've been watching a hurricane

484
00:31:36,800 --> 00:31:37,490
on another planet.

485
00:31:37,670 --> 00:31:38,450
Jane: That is pretty cool.

486
00:31:38,780 --> 00:31:40,690
John: And Jupiter has a couple
of those. There's the big red

487
00:31:40,780 --> 00:31:44,080
spot, but there's a couple of
smaller white spots, and and a

488
00:31:44,170 --> 00:31:47,620
and another smaller red spot.
And then when you look at the

489
00:31:47,920 --> 00:31:50,950
poles of Jupiter, it's it's
really weird because you start

490
00:31:51,010 --> 00:31:54,640
to see shape the shape around
the poles that that look really

491
00:31:54,670 --> 00:31:57,640
neat. It's just Jupiter has all
these storms in its atmosphere

492
00:31:57,700 --> 00:32:00,070
because it's so big and rotating
so fast.

493
00:32:00,610 --> 00:32:04,860
Jane: Well, is its size also
relevant when we think about

494
00:32:05,130 --> 00:32:06,270
Jupiter's moons?

495
00:32:06,510 --> 00:32:11,490
Brandon: Hi, my name is Brandon,
and I'm 10 years old. I'm from

496
00:32:11,490 --> 00:32:15,600
Sydney, Australia. Why does
Earth only have one moon, but

497
00:32:15,600 --> 00:32:18,120
Jupiter has 95 moons?

498
00:32:17,820 --> 00:32:21,582
John: This is a fantastic
question, and and I want to zoom

499
00:32:21,654 --> 00:32:25,995
out and think about the solar
system again for a little bit.

500
00:32:26,067 --> 00:32:30,480
Mercury doesn't have any moons.
Venus doesn't have any moons.

501
00:32:30,553 --> 00:32:35,183
The Earth has one moon. Mars has
two very tiny moons, Phobos and

502
00:32:35,255 --> 00:32:39,668
Deimos, which are kind of like
asteroids. Then you get to the

503
00:32:39,741 --> 00:32:44,226
big giant gas ones, and those
planets have dozens of moons. We

504
00:32:44,299 --> 00:32:48,784
keep finding new moons around
Jupiter and Saturn every time we

505
00:32:48,856 --> 00:32:53,197
look harder. Uranus and Neptune
also have a lot of moons, so

506
00:32:53,270 --> 00:32:57,538
there's something different just
in general about the solar

507
00:32:57,611 --> 00:33:02,024
system, and it has to go back,
it goes back to how that stuff

508
00:33:02,096 --> 00:33:05,713
formed. The rocky planets, the
rocks came together

509
00:33:05,786 --> 00:33:10,127
gravitationally. Snowball effect
made this this big this big

510
00:33:10,199 --> 00:33:14,757
planet. For the big gas giants,
on the other hand, they started

511
00:33:14,829 --> 00:33:18,881
to build up stuff and then
started capturing things into

512
00:33:18,953 --> 00:33:23,294
orbits around them. And those
things, most of them got flung

513
00:33:23,366 --> 00:33:27,996
off, but some of them survived,
and the planets were so big that

514
00:33:28,069 --> 00:33:32,337
the stuff orbiting it with it
got pretty big, big enough to

515
00:33:32,410 --> 00:33:36,895
make moons. So it's kind of like
Jupiter and Saturn and Uranus

516
00:33:36,967 --> 00:33:41,453
and Neptune are like their own
little solar systems because if

517
00:33:41,525 --> 00:33:46,083
you look at the types of moons
closest to Jupiter or closest to

518
00:33:46,156 --> 00:33:50,569
Saturn, they look different than
the moons farthest away from

519
00:33:50,641 --> 00:33:54,982
Jupiter and farthest away from
Saturn. So they're all acting

520
00:33:55,054 --> 00:33:58,744
almost like little solar
systems, and that's just a

521
00:33:58,816 --> 00:34:03,374
that's a leftover feature of how
the whole solar system formed,

522
00:34:03,447 --> 00:34:08,149
and again, we don't know exactly
how this how this works. But the

523
00:34:08,221 --> 00:34:12,345
bigger the planet, the more
stuff it's trying to pull in,

524
00:34:12,418 --> 00:34:16,903
and that's probably why Jupiter
and Saturn have the most moons

525
00:34:16,976 --> 00:34:18,640
in in the solar system.

526
00:34:18,780 --> 00:34:20,810
Jane: All right. Well, since
we're we're already talking

527
00:34:20,810 --> 00:34:24,590
about Jupiter and Saturn. Let's
move from Jupiter to Saturn, the

528
00:34:24,740 --> 00:34:30,530
next one out. And a lot of kids
and adults know one thing about

529
00:34:30,590 --> 00:34:30,950
Saturn.

530
00:34:31,129 --> 00:34:34,099
Christopher: My name is
Christopher. I'm six years old.

531
00:34:34,489 --> 00:34:38,119
I'm from Buckeye, Arizona. Why
does Saturn have rings?

532
00:34:38,900 --> 00:34:43,670
Aaron: My name is Aaron. I live
in Boston, and I'm five years

533
00:34:43,670 --> 00:34:48,710
old. And my question is, why
does Saturn have wings?

534
00:34:48,710 --> 00:34:52,880
Amelia: My name is Amelia. I'm
from Princeton, New Jersey. I'm

535
00:34:52,880 --> 00:35:01,250
six years old, and why does
Saturn have a ring around it?

536
00:35:01,960 --> 00:35:06,730
Libby: Hi. My name is Libby and
I'm nine years old. I live in

537
00:35:06,730 --> 00:35:13,090
Pearland, the United States of
America. Why does Saturn have

538
00:35:13,090 --> 00:35:14,080
rings?

539
00:35:14,180 --> 00:35:18,620
Arjun: Hi, my name is Arjun and
I'm five years old and I live in

540
00:35:19,250 --> 00:35:23,900
Maryland. Why do some planets
have rings?

541
00:35:24,709 --> 00:35:27,769
John: It turns out that all of
the gas giants in the solar

542
00:35:27,919 --> 00:35:33,469
system-Jupiter, Saturn, Uranus,
and Neptune-have rings. Saturn's

543
00:35:33,589 --> 00:35:36,019
rings are big and beautiful and
easy to see, but Jupiter has

544
00:35:36,139 --> 00:35:40,099
rings. Uranus and Neptune-they
they have rings, and we think

545
00:35:40,249 --> 00:35:44,949
that the rings came about
because in the formation of the

546
00:35:44,949 --> 00:35:47,619
solar system, or in the
formation of the planets, or at

547
00:35:47,829 --> 00:35:51,819
some point in those planets'
history, stuff smacked into each

548
00:35:51,939 --> 00:35:54,939
other and pulverized. It hit
each other really hard. So two

549
00:35:55,119 --> 00:35:59,739
things like moons or or giant
chunks of ice bashed right into

550
00:35:59,829 --> 00:36:03,629
each other, made a lot of
debris, but that stuff was

551
00:36:03,809 --> 00:36:08,009
orbiting around the planet, and
so that debris made a disc which

552
00:36:08,189 --> 00:36:11,579
looks like a ring around the
planet. So if you if you got up

553
00:36:11,639 --> 00:36:14,219
really close to Saturn, you know
its rings are made out of pretty

554
00:36:14,399 --> 00:36:19,199
small stuff. It's mostly rocks
and ice, but it's it's small

555
00:36:19,319 --> 00:36:23,239
stuff, and that's because
something pulverized, Saturn's

556
00:36:23,419 --> 00:36:27,769
rings very likely don't look the
same as they did hundreds of

557
00:36:27,799 --> 00:36:31,999
millions of years ago, and they
may eventually go away because

558
00:36:32,149 --> 00:36:34,969
this stuff will start to clump
together again, or fall into

559
00:36:35,029 --> 00:36:38,389
Saturn, or get thrown out. So
that's another neat thing about

560
00:36:38,509 --> 00:36:41,559
about ringed planets is because
they don't always look the same

561
00:36:41,769 --> 00:36:44,739
over time, right? Jupiter has
rings now. It may have had more

562
00:36:44,799 --> 00:36:49,449
impressive rings, or or maybe no
rings at all early on. And it's

563
00:36:49,629 --> 00:36:53,649
it's it's fun to try to figure
out what the history of those

564
00:36:53,799 --> 00:36:58,779
things might be. We don't watch
over short times like a month or

565
00:36:58,869 --> 00:37:03,389
a year or 10 years the changes
in those rings. We have to use

566
00:37:03,839 --> 00:37:08,849
computers to simulate what those
rings look like. It's kind of

567
00:37:08,879 --> 00:37:12,599
like we're playing Minecraft
with the planets, and we put the

568
00:37:12,749 --> 00:37:15,149
rings there, and we tell them,
"Here's how we think gravity

569
00:37:15,269 --> 00:37:19,349
works, and what moons are there.
And then we let a pretend clock

570
00:37:19,409 --> 00:37:23,479
go really fast, and let the the
thing go much much faster than

571
00:37:23,629 --> 00:37:28,309
than it does in in normal time,
and we can test models of of how

572
00:37:28,339 --> 00:37:31,099
the rings formed, what might
happen to them. The same thing

573
00:37:31,099 --> 00:37:34,789
is what we do with the solar
system. So, going back to the

574
00:37:34,909 --> 00:37:36,979
original question, the main
reason why we have rings is

575
00:37:37,039 --> 00:37:39,619
because we believe that stuff
collided with other stuff and

576
00:37:39,649 --> 00:37:41,349
just left a bunch of debris.

577
00:37:42,880 --> 00:37:45,400
Jane: All right, so we're going
from Saturn. We're still

578
00:37:45,550 --> 00:37:50,560
traveling out away from the sun,
and the next planet is Uranus.

579
00:37:51,490 --> 00:37:51,640
John: Yes.

580
00:37:52,570 --> 00:37:53,710
Jane: So we have a question for
you.

581
00:37:54,130 --> 00:37:54,280
John: Okay.

582
00:37:55,089 --> 00:37:58,839
Jane: We're not sure if this
question is an honest question

583
00:37:58,929 --> 00:38:00,099
or said in jest.

584
00:38:00,330 --> 00:38:05,040
Prayun: My name is Prayun, and
my age is five, and I'm from New

585
00:38:05,040 --> 00:38:10,620
Mexico. And my question is, why
is Uranus so gassy?

586
00:38:11,610 --> 00:38:12,240
Jane: What do you think, John?

587
00:38:12,510 --> 00:38:16,050
John: I will do the answer,
assuming that this is this is a

588
00:38:16,050 --> 00:38:19,320
non-un jest question.

589
00:38:19,320 --> 00:38:24,480
Jane: And and I I think a lot of
kids know what the the joke is,

590
00:38:24,480 --> 00:38:28,830
but just to be clear, sometimes
people call when I was a kid. I

591
00:38:28,830 --> 00:38:33,180
think we always called this
planet Uranus, which is another

592
00:38:33,180 --> 00:38:36,510
word for your butt. So why is
your butt so gassy?

593
00:38:36,555 --> 00:38:37,875
John: Why is your butt so gassy?

594
00:38:37,875 --> 00:38:40,125
Jane: Uranus, the planet is
gassy.

595
00:38:40,219 --> 00:38:43,539
John: It is. It's a giant ball
of gas. I could make the jokes

596
00:38:43,599 --> 00:38:46,989
all day, and maybe that's a
different. That's a. That's a

597
00:38:47,049 --> 00:38:50,529
different podcast. But Uranus is
one of those planets that's

598
00:38:50,589 --> 00:38:54,099
really far away from the sun,
and so it built itself up the

599
00:38:54,189 --> 00:38:57,789
same way that Jupiter and Saturn
did, with slightly different

600
00:38:58,509 --> 00:39:01,649
material because it was farther
away from the sun. So if we used

601
00:39:01,709 --> 00:39:04,769
our units, where the Earth is
one unit away, Jupiter is five

602
00:39:04,799 --> 00:39:08,969
units away, Saturn is 10 units
away, Uranus is 20 units away.

603
00:39:09,119 --> 00:39:11,219
So now we're starting to get
really far away from the sun,

604
00:39:11,969 --> 00:39:16,169
and so it was slightly different
gasses that could form ices out

605
00:39:16,199 --> 00:39:20,929
of at colder temperatures, but
it's still the same process that

606
00:39:20,959 --> 00:39:23,059
that ice is really good at
capturing gas.

607
00:39:23,570 --> 00:39:26,570
Jane: All right, thank you for
that. Appreciate it.

608
00:39:26,570 --> 00:39:26,810
John: Sure.

609
00:39:26,810 --> 00:39:30,290
Jane: So after Uranus, we keep
going out. How many units to get

610
00:39:30,290 --> 00:39:30,980
to Neptune?

611
00:39:30,980 --> 00:39:34,910
John: Neptune is another
doubling, if I remember

612
00:39:34,910 --> 00:39:38,450
correctly. So the planets keep
doubling. They're farther away.

613
00:39:38,450 --> 00:39:42,050
It's I think it's about twice as
far away as Uranus is.

614
00:39:42,050 --> 00:39:44,930
Jane: What do we need to know
about Neptune?

615
00:39:44,930 --> 00:39:48,305
John: We need to know that
Neptune is again because it was

616
00:39:48,305 --> 00:39:52,685
so much farther away. We're now
having other types of gasses

617
00:39:52,685 --> 00:39:58,835
form ice. So out there, you can
have a gas which is called

618
00:39:58,835 --> 00:40:04,745
methane on Earth, and methane on
Earth is made by cow farts and

619
00:40:04,745 --> 00:40:09,005
other things in biology, but
methane can also be made

620
00:40:09,050 --> 00:40:12,950
astronomically and geologically.
Methane, when you get it really,

621
00:40:12,950 --> 00:40:16,760
really cold, can form into ice
as well. And so, that far away

622
00:40:16,760 --> 00:40:20,600
from the sun, you know, it's
it's not just water ice; it's

623
00:40:20,600 --> 00:40:25,430
it's mostly nitrogen ice. Like
nitrogen can make ice, methane

624
00:40:25,430 --> 00:40:31,520
can make ice, and it's those
things are are are what might be

625
00:40:31,520 --> 00:40:36,935
the the the seed units that
captured the gas on on to to

626
00:40:36,935 --> 00:40:41,345
Neptune. What's fun about
Neptune and Uranus is they also

627
00:40:41,345 --> 00:40:45,095
have these giant storms, kind of
like the red spot on Jupiter.

628
00:40:45,095 --> 00:40:48,455
When we take very powerful
telescopes, we can see these

629
00:40:48,455 --> 00:40:52,475
storms in the upper atmosphere
of Uranus and Neptune. the The

630
00:40:52,475 --> 00:40:59,420
other interesting thing about
Neptune is that it is one of the

631
00:40:59,420 --> 00:41:04,880
most common sized planets around
other stars. We have things at

632
00:41:04,880 --> 00:41:09,350
around a Neptune size, and so
it's kind of interesting because

633
00:41:09,350 --> 00:41:12,260
it's it's an interesting
representative of of what other

634
00:41:12,260 --> 00:41:15,890
planets around other stars
might, in general, look like if

635
00:41:15,890 --> 00:41:18,665
they were that distance from
their from their star. But we're

636
00:41:18,665 --> 00:41:21,695
getting pretty cold out there.
We've still got a lot of moons.

637
00:41:21,695 --> 00:41:26,645
We've got some rings, but you
know the sun appears much much

638
00:41:26,645 --> 00:41:30,395
fainter. If you were if you were
in orbit around Neptune and you

639
00:41:30,395 --> 00:41:32,945
looked at the sun, you wouldn't
need to put on sunglasses or

640
00:41:32,945 --> 00:41:36,245
squint your eyes. It's now
getting pretty faint, and so

641
00:41:36,245 --> 00:41:38,615
that gives you a sense of how
cold it is out there.

642
00:41:38,869 --> 00:41:42,939
Jane: So Willow has a question
about Neptune that we may need

643
00:41:42,999 --> 00:41:44,439
to do some redirecting around.

644
00:41:44,500 --> 00:41:50,740
Willow: My name is Willow. I
live in Boone, North Carolina,

645
00:41:51,190 --> 00:41:58,510
and I'm five and a half years
old. Why is Neptune too small to

646
00:41:58,630 --> 00:41:59,560
be a planet?

647
00:42:00,520 --> 00:42:04,200
John: Um. So Neptune is a
planet. It's it's too small to

648
00:42:04,500 --> 00:42:09,330
be a gas giant. It's kind of in
this this this transition space,

649
00:42:09,480 --> 00:42:13,020
but it's definitely a planet.
It's just the smallest of the

650
00:42:13,200 --> 00:42:15,600
gas planets in our outer solar
system.

651
00:42:16,110 --> 00:42:18,480
Jane: Well, I was wondering if
Willow was actually thinking

652
00:42:18,660 --> 00:42:23,540
about another object that if we
kept going past Neptune, we

653
00:42:23,720 --> 00:42:30,620
would get to, that was a planet,
and is pretty small, and that's

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00:42:31,070 --> 00:42:31,550
Pluto.

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00:42:31,780 --> 00:42:37,210
Hazel: I'm Hazel. I'm five years
old, and I live in Burlington,

656
00:42:37,210 --> 00:42:40,960
Massachusetts. Why isn't Pluto a
planet anymore?

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00:42:40,960 --> 00:42:46,120
Jasper: My name's Jasper, and
I'm from Lanzhou, China. And I'm

658
00:42:46,120 --> 00:42:53,110
11 years old. My question is,
why isn't Pluto a planet?

659
00:42:53,140 --> 00:42:58,000
John: The only reason that I
think is a good reason to say

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00:42:58,000 --> 00:43:01,270
Pluto isn't a planet anymore is
because we have to come up with

661
00:43:01,270 --> 00:43:07,600
a definition that is consistent
for what we say a planet is, and

662
00:43:07,600 --> 00:43:12,400
our definition for a planet has
a lot to do with its size, but

663
00:43:12,400 --> 00:43:19,165
also to do with its environment.
And Pluto doesn't quite match

664
00:43:19,165 --> 00:43:22,285
those conditions for any of the
other planets in the solar

665
00:43:22,285 --> 00:43:26,575
system, Pluto is is very small
compared to any of the other

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00:43:26,575 --> 00:43:32,035
planets. It has a moon Charon,
which is almost as big as it is.

667
00:43:32,035 --> 00:43:35,335
A while back, astronomers were
struggling with the definition

668
00:43:35,335 --> 00:43:37,975
of a planet because if they
allowed Pluto to remain a

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00:43:37,975 --> 00:43:41,080
planet, then all of these other
things that we were starting to

670
00:43:41,080 --> 00:43:46,570
discover in the solar system,
like Ceres or Makemake, or you

671
00:43:46,570 --> 00:43:48,700
know, there's there are these
things which we call dwarf

672
00:43:48,700 --> 00:43:53,500
planets, which are big relative
to an asteroid, but small

673
00:43:53,500 --> 00:43:58,720
relative to other planets. Pluto
was a lot more like those than a

674
00:43:58,720 --> 00:44:01,360
planet that we would
traditionally call planets. So

675
00:44:01,360 --> 00:44:03,895
we changed the name. We we said
Pluto is no longer a planet;

676
00:44:03,895 --> 00:44:06,895
it's a dwarf planet, and we have
hundreds of dwarf planets in the

677
00:44:06,895 --> 00:44:08,035
solar system.

678
00:44:08,040 --> 00:44:11,340
Jane: John mentioned Ceres and
Makemake, but the other

679
00:44:11,490 --> 00:44:14,280
officially recognized dwarf
planets, other than Pluto, are

680
00:44:14,490 --> 00:44:19,710
Haumea and Eris. So, if there
are five official ones, then why

681
00:44:19,860 --> 00:44:23,660
did John say there are hundreds
in our solar system. Well, he

682
00:44:23,900 --> 00:44:26,570
and many other astronomers
believe there could be hundreds

683
00:44:26,660 --> 00:44:31,610
or even 1000s of dwarf planets
yet to be discovered. Full

684
00:44:31,700 --> 00:44:34,610
planet or dwarf planet? John
says the real question about

685
00:44:34,670 --> 00:44:36,650
Pluto is: Is it awesome?

686
00:44:36,960 --> 00:44:39,330
John: It's totally awesome and
interesting, and we flew a

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00:44:39,330 --> 00:44:43,740
spacecraft past it called the
New Horizons spacecraft, that

688
00:44:43,740 --> 00:44:48,420
saw things we just never seen
before. We saw mountains of

689
00:44:48,420 --> 00:44:52,080
frozen nitrogen, right? A
mountain range of frozen

690
00:44:52,080 --> 00:44:57,480
nitrogen on its surface. We saw
this giant heart-shaped thing of

691
00:44:57,480 --> 00:45:01,125
ice on its surface, and so is it
a planet or not, I don't care.

692
00:45:01,125 --> 00:45:03,945
It's still awesome, and it's and
it's worth studying.

693
00:45:04,360 --> 00:45:06,490
Jane: All right. Well, we're
pretty far out in our solar

694
00:45:06,490 --> 00:45:09,430
system now, and we've talked
about all the planets and the

695
00:45:09,430 --> 00:45:13,450
dwarf planets. So I think we'd
better end it here. But first,

696
00:45:13,450 --> 00:45:16,090
let's turn our imaginary super
fast spaceship back toward

697
00:45:16,090 --> 00:45:20,830
Earth. As always, if you have a
question about anything, have an

698
00:45:20,830 --> 00:45:23,770
adult record you asking it on a
smartphone using an app like

699
00:45:23,770 --> 00:45:26,980
Voice Memos, then have them
email the file to

700
00:45:27,325 --> 00:45:31,315
questions@butwhykids.org. But
Why is produced by Sarah Baik,

701
00:45:31,315 --> 00:45:34,345
Melody Bodette, and me, Jane
Lindholm at Vermont Public, and

702
00:45:34,345 --> 00:45:38,575
distributed by PRX. Our video
producer is Joey Palumbo, and

703
00:45:38,575 --> 00:45:41,695
our theme music is by Luke
Reynolds. If you like our show,

704
00:45:41,695 --> 00:45:44,335
please have your adults help you
give us a thumbs up or leave a

705
00:45:44,335 --> 00:45:47,335
comment on whatever podcast
platform you like to use to

706
00:45:47,335 --> 00:45:51,655
listen to us. It helps other
kids and families find us. Okay,

707
00:45:51,655 --> 00:45:54,310
time to disembark. We're back at
Earth. Thank you for listening

708
00:45:54,310 --> 00:45:57,310
to our tour of the planets.
We'll be back in two weeks with

709
00:45:57,310 --> 00:46:01,420
an all-new episode. Until then,
stay curious.

