Aliens of the Deep Page #3
It's just amazing,
We've got this huge,
huge carbonate structure,
Unbelievable,
Copy that.
Right rotator going up, rotator going up.
It's just the hot water just flowing up
and slowly forming stalactites,
Upside-down stalactites are slowly
deposited, millennium after millennium,
So what's interesting
about these
is that you don't necessarily
need plate tectonics,
You need some means for the water
to react with the deep mantle rock,
And then you get
the serpentinization reaction
which produces the heat that drives
the formation of such systems,
It's absolutely phenomenal,
Do you want to go ahead
and proceed to the summit? Over.
Roger that,
- There's warm water up here,
- Yeah,
The vent fluid is just
coming right up out of here,
Wow, This is just amazing,
Our technology is just
at the level now
where we can safely explore
the depths of our own ocean,
- Kinda friable,
- Yeah,
OK,
Yeah! Look at that,
- We got a rock,
- Hey, we got a sample,
Rover One, Rover One,
this is Rover Two, Do you...
- Oh, my goodness, look at that!
- Oh, Christ!
Holy cow,
- OK, stop it, stop it, stop it,
- Kevin. You seeing this?
Look at that thing,
That is absolutely unreal,
See if you can
Roger that,
Oh, my goodness,
Look at that, it's just amazing,
Oh, man, look at this thing,
Look at this thing,
This is incredible,
How can something
like that be alive?
How does a creature like this work?
That is absolutely phenomenal,
Beautiful,
Absolutely beautiful,
See the reticulation inside this thing?
Look at that,
That is amazing,
I have no idea what that is,
- No,
- That's what I love about this stuff,
Every single dive, you're gonna see
something you've never seen before,
And you might even see something
that nobody's ever seen before,
Are you seeing this thing?
Look at this,
This is, like,
the ugliest fish in the world,
Oh, he's got feet! Look, he's got feet,
He's got, like, little toe-socks,
The thing about deep diving is you
always need to expect the unexpected.
Oh, my God,
look at that squid,
Oh, it's massive,
Look, look, look,
Quick, look,
See it?
Absolutely fantastic,
Look at that fish,
You see that guy?
All right, we got us a Dumbo,
Been hoping for this for a while,
What a beautiful animal,
What a beautiful animal, Look at that,
Like a dancer,
What an amazing creature,
God, you could watch this guy all day,
Almost looks like
he's glowing from within,
MIR One, MIR One,
This is Rover Two, Do you copy?
MIR One, MIR One,
do you copy? This is Rover Two.
MIR One, MIR One,
This is Rover Two, Do you copy?
It's intermittent, Jim,
Sometimes yes and sometimes no,
Uh, roger, Mike,
We're seriously low on power
and will have to leave the bottom,
We must go up,
Genya, We must go up,
Oh, he's trying to say something,
about...
He's trying to say...
Look out the porthole,
I can't see him,
Can you call surface?
He's saying, "Up and over"?
Might be,
We need you to contact the surface
that we are ascending,
Can't read it, Zoom in,
Let's see if you can read the sign,
"Contact surface, must surface,"
Understood, We'll contact them right now,
Ares surface comm,
Rover Two leaving the bottom
depth 741 meters,
- So, how was it, Jim?
- We got the goods, We definitely got it,
Ah, that thing is phenomenal,
How you doing?
- What did you see down there?
- Oh, it was just incredible, Just incredible,
There was a huge, um...
Was it a jellyfish?
Some type of gelatinous...
Massive, Like, a meter,
We think that it was feeding
off of the, uh,
off the amphipods and the plankton
and the copepods that were next to...
- Hanging out at the lights?
- Hanging out at the light, yeah,
- How's it work?
- Man, we don't know,
- But it's there, So it's working somehow,
- Exactly,
- Life's pretty cool,
- Yeah, absolutely fantastic,
- Welcome back, Kevin,
- Thanks,
- Team Rover,
- Go team Rover!
My name is Maya Tolstoy,
and I'm a marine seismologist
at Lamont-Doherty Earth Observatory.
I study underwater volcanoes,
and particularly I study the earthquakes
And I'm trying to understand
how the Earth is made,
how the surface of
the planet is formed.
I'm going to be deploying
ocean-bottom seismometers.
Those are instruments
that listen to earthquakes
and other noises on the ocean floor.
In the ocean,
the light only goes so far.
to basically see the bottom of the ocean,
and to see into the ocean crust, the way
that light lets you see on the surface.
We put the instruments over the side of
the ship. They drop, they gather the data.
Normally, I don't have to dive
in order to do my job.
So it was very exciting
to finally see the environment
that I've been working on
for over a decade.
MIR two, copy,
We have a visual on you.
We are inbound.
Roger that,
- Can you see them?
- Yeah, It's out my window,
It looks like a spaceship,
Wow,
That's incredible,
That's like another planet,
It's such
an incredible world down there,
and it's so important
to the formation of our planet.
It's where two thirds
of the surface of our world was created,
and we still know so little about it.
Do you see how
they're all shiny and glassy?
- Oh, yeah, Look at that,
- That shows that it cooled superquickly,
That's just, like, it really turns
to glass, basically, To obsidian, it's called,
Look at that,
And you see how there's
hardly any sediment on it?
That's when it's really fresh,
This is brand-new crust we're looking at,
Wow,
Now, can you just imagine
being down here when this stuff erupts?
Molten rock oozing out
and hitting the freezing cold water,
I just can't imagine it,
It must have been insane,
Must look pretty cool,
For the few seconds before you die,
I miss my son.
He's five months old.
It was such a hard decision
to make to come out here.
But I think it's important to study
one of the most remarkable phenomenon
we've ever discovered
in the oceans.
MIR Two, just keep going
upslope on this heading,
at the top of this sulfide mound, Over,
Roger that,
Wow,
There it is,
All around our world,
running down the middle of the oceans
like seams on a baseball,
are these cracks,
these spreading centers,
where the crust of the planet
Up above,
the sea looks normal.
But two miles down,
it's a violent landscape
where fresh lava flows
out of the crack and freezes into rock.
When the sea water seeps down to the
molten rock just beneath the new crust,
it gets superheated,
far hotter than boiling.
But it can't boil, because of the intense
pressure at the bottom of the ocean.
out of the sea floor.
When the superheated water hits the
freezing ocean, minerals condense out,
forming the chimneys,
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"Aliens of the Deep" Scripts.com. STANDS4 LLC, 2024. Web. 21 Nov. 2024. <https://www.scripts.com/script/aliens_of_the_deep_2475>.
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