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The Milky Way galaxy is an expansive giant.

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Home to hundreds of billions of stars

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and at least 100 billion planets,

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many of which shine brightly in our own night sky.

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But there are others hiding in plain sight.

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If we gaze at the stars hard enough,

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we can even get lucky and catch a glimpse

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of the fluting remnants of solar system bodies.

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What are these near-Earth objects,

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and could they have played a role in our evolution?

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I look at these objects as tracers

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of the very earliest stages

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of planet formation in the solar system.

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We can study the planets and try to understand

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how they form and evolve.

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But the planets are complicated bodies.

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They have weather and wind and water.

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They have plate tectonics.

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They have volcanism.

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All of these things act to erase

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and reset the surfaces of the planet.

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And that makes it very difficult

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to learn about how the Earth formed

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four and a half billion years ago.

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In contrast, the asteroids are leftover fragments

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of the planet formation process,

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and they've been sitting out in the solar system

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for the past four and a half billion years

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relatively undisturbed.

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And so, by studying these objects,

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we're really able to peer back into the past,

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and understand what the conditions were like

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as planets were forming, both chemically and physically.

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So we have 600,000 of these things to study.

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We can't send a spacecraft to all of them,

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but we can use telescopes here on Earth.

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For a long time, the traditional definition

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of an asteroid and a comet,

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is that an asteroid's a rocky body,

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and that a comet's an icy body that shows activity.

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A comet injects a halo,

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those types of things that we associate with a comet.

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The past 10 or 15 years or so,

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we've started to discover asteroids

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that, for whatever reason, all of a sudden turn on.

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Just like a comet would, they start to show activity.

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They start to show evidence of outgassing,

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loss of volatiles, loss of dust.

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Just like a comet.

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And we now think that there are quite a few processes

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probably responsible for taking some of these objects,

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that we would have classified as asteroid,

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and turning them into comets.

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Collision is one possible way

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of making an asteroid look like a comet.

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If you have an asteroid and collide a body onto its surface,

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that's gonna kick up a big dust cloud

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and, as viewed from Earth,

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we will see an asteroid with a big dust cloud around it

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that looks just like a comet.

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They can be a hazard,

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and we certainly know that near-Earth asteroids

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can and do hit the Earth.

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We have numerous pieces of evidence all over the Earth,

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in the form of impact craters,

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that, in some cases, very large objects have hit the Earth

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and we think that there's a pretty good correlation

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between extinction events

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and impacts from asteroids and comets.

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While the most famous has been the impact

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that potentially killed off the dinosaurs,

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we have evidence of that impact

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off the coast of the Yucatan Peninsula in Mexico,

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but there are numerous others throughout history

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that we think correlate with extinction events

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that we see in the fossil record.

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With that said, though, those events are exceedingly rare.

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Exceedingly rare.

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And they're so rare that I don't stay up at night

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worrying about the next killer asteroid coming along.

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While impact events here on Earth

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are few and far between,

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parts of asteroids and comets

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have reached our planet in the form of meteorites.

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There's a whole host of terminology

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associated with meteors.

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There's meteors, there's meteoroids, there's meteorites.

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Meteors come from a variety of sources.

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Some of them are particles

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that have been released by comets.

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Some of them are dust particles released by asteroids,

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generally formed through collisions.

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So two asteroids collide, and produce a shower of fragments.

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Some of those fragments can make their way to the Earth.

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Before that passage through the atmosphere,

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you could refer to that particle or that rock

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as a meteoroid.

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If that meteor makes its way to the ground,

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then that is when it becomes a meteorite.

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Generally what happens with meteorites,

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is that they will impact the atmosphere

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and as that body passes through the atmosphere

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it undergoes extreme heating and fragmentation effects.

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It fragments into many pieces and those pieces get scattered

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all over what we call strewn field.

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Those pieces can range in size from little dust particles

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all the way up to large blocks.

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The biggest meteorites in the world

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can be the size of rooms.

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In February of 2013, over Chelyabinsk, Russia,

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a modest sized meteoroid or asteroid hit the atmosphere,

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passed through the atmosphere as a meteoroid,

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actually blew up at a relatively high altitude

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and showered down fragments of that material

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onto the surface of the Earth.

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That was not predicted and part of the reason for that

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is that it was a relatively small object,

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about 15 meters in size or so.

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Something that small is hard to detect

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with ground-based telescopes.

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But perhaps more importantly,

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is that it approached from the direction of the Sun.

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If something of that size

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is coming from the direction of the Sun,

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you're not gonna know about it ahead of time,

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unless it's been discovered years previously.

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This amazing fireball, a streak of light

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that appeared in the sky,

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it left behind a vapor trail or a gas trail,

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and people ran to their windows to look at this.

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Several minutes after the fireball,

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the shockwave from that event

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made its way down to the surface,

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and that shockwave blew out windows

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all over this region in Russia

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and it was the shattering of windows

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onto people's faces that were looking out the window

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that caused the greatest amount of injuries in that event.

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So it wasn't necessary there was a large impact crater

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and flash heating or anything like that.

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It was the shock of the fireball.

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This is actually a relatively small piece.

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The largest piece that was recovered

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was maybe half a meter in size.

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It was actually at the bottom of a lake.

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This is actually what we refer to as an ordinary chondrite,

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which is unsurprisingly a fairly ordinary meteorite.

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It's the most common type of meteorite

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that falls on the Earth.

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About 80% of all meteorites fall into this category.

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Well, this meteorite itself formed

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about four and a half billion years ago in the solar system,

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and has been floating around in space since then.

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It probably lived part of its life

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on the surface of a main-belt asteroid.

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At some point that main-belt asteroid was probably impacted

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and fragments were removed from that surface,

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and those fragments then made their way to Earth.

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It impacted and delivered the meteorites to the ground.

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So there's nothing terribly extraordinary about it,

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except for the fact that it has a very specific

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and very well documented impact event associated it with it,

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which is fairly unusual.

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Most of the time these things fall in remote regions,

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where people don't witness the fall.

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But this is the most documented impact in history.

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This is one of the more popular type of meteorites.

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It's called a pallasite.

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This is a mix of gem-quality peridot, or olivine,

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in a matrix of metal.

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And so it's a really striking, beautiful piece,

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and we think that something like this

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probably formed around the core-mantle boundary

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of a large protoplanetary body.

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So just like the Earth has a core, a mantle and a crust

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we think planetary bodies in the solar system

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some of them may have undergone

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a similar differentiation process.

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And so this is a chunk of a core-mantle boundary

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of one of these differentiated protoplanets,

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and obviously that protoplanet has been disrupted

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so that it has been collisionally fragmented into a piece

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that we have now collected as this meteorite.

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Many of them are cut into these slices

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so that you can see the sort of appearance

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and internal texture of the meteorite.

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The last piece here that I'll show

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is a fascinating meteorite.

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This is an iron meteorite.

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It a slice of the iron meteorite.

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Its surface has been etched

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so that you can see these crystallized,

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interleaved pattern of crystals on the surface of it.

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This particular iron meteorite

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has the oldest date of any rock in the solar system,

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and that 4.567 billion years old.

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This rock was probably the first thing

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that formed in the solar system,

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the first planetary body that formed in the solar system

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four and a half billion years ago.

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And there's a really interesting history

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about how we think something like this

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could have formed so quickly.

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It requires very rapid accretion,

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so the body accreted very quickly,

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and because we're looking at iron,

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this is a chunk of iron-nickel metal,

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this is almost certainly the core

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of the differentiated body.

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So you're looking at rapid accretion and differentiation

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in the first few million years of solar system history,

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which is staggering to think

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that such complicated geological processes

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were happening so early in the solar system.

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And it's those bodies that this meteorite represents

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that were the precursors to the Earth

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and the planets in the solar system.

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So it was objects like this

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that were colliding and sticking together

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that ultimately formed and built up the planets.

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So by studying these objects

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we can understand the building blocks and the ingredients

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that went in to form the Earth and set up the conditions

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that make the Earth habitable and sustainable for life.

