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[ENG SUB] [Meeting] The Unit (더 유닛): MelodyDay Yeoeun, Chahee & Yoomin #SUPERBOOT - Duration: 3:21.
Have a melody day!
Hello, we're MelodyDay!
Hello, I'm MelodyDay's leader and main vocalist Yeoeun. Nice to meet you!
Hello, I'm MelodyDay Chahee
Hello~
Hello, I'm Melody's Yoomin. Nice to meet you~
What made you decide to participate in this show?
First of all, there are many things MelodyDay didn't get to show
So we decided on this with the thought of being able to show more through this program
We did have a lot of worries at first
But we couldn't miss out on a good opportunity because of such worries
So we prepared hard and here we are
What were your worries?
My biggest worry was whether I would be able to do well
We worried this might affect us negatively
Because we could be at a disadvantage
We only worked as a team before. And there are many other idols coming on the show...
So somehow...
Afraid you'll be pushed aside?
Yes~
Yes, that can't happen
Because of that, we worried a lot
You said earlier this was a good opportunity. Why do you think that?
Just being able to stand on stage and meet the fans regularly is a good opportunity for us
A chance to do that doesn't come often for us
It's an opportunity to show MelodyDay a bit more on broadcast
So I think it's a great one
Because we really don't promote a lot,
Our fans (??)
But if we're able to come on KBS through this program
The fans would say, "Oh MelodyDay will be on!" and could see us one more time
We could also gain more fans if we get to show our unique colors
So yes~ That's why we decided to come on
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🍀 INTEY SHIATSU FOOT MASSAGER REVIEW - BEST FOOT MASSAGER 👈 - Duration: 6:33.
okay so here is a great gift idea
christmas is coming get it for the person who has everything or thinks that they have
everything you want to try it you're envious she's gonna be as my I didn't
talk to massager maybe next time so this is really relaxing I was out doing yard
work for hours today it's a Saturday and my feet were really hurting and they're
starting to feel better already what you think Trixie you want to try
you want your hi today I have a foot massager to show you it's made by Entei
and I've been using it now for a couple of days and it's working great it's
especially great for those who suffer from foot pain such as plantar fasciitis
not sure I pronounced that right but I have been diagnosed with that in the past
it's very painful and I've learned to control it with certain things like not
going barefoot and wearing inserts shoe inserts this is a product that would
make a great gift for Mother's Day Father's Day Christmas birthdays I think
especially great gifts for men and I say that is because they're very hard
to shop for most of them don't like things like fragrances and jewelry so
this is a shiatsu massager with the kneading function it also has optional
heat and air pressure so there's a timer that toggles between ten twenty and
thirty minutes for any of the functions bayoneting I see their offer on and
that's the shiatsu massaging function
the air pressure goes between f1 and f5 to indicate the level of intensity you
can hear it sounds like a blood pressure cuff and this is really
high-tech okay yeah heating heating is either off or on
so there's a lot of options here for if you you want the heat you don't want the
heat the level of air pressure kneading massaging or none lots of options that
you can individualize this is obviously where you put your feet and I'll show
you that in a minute from the other side so I guess then search your feet here
and see oh let's I'll start with the kneading
it's really good I had
a foot massager are some years ago but it was not didn't have this many functions
or just you put your you just set your feet down on top of it and it kind of
massaged it and I think there might have been a heat option but this is much more
effective as I said this is more high-tech and then I can turn on turn off vignetting
and - on the air pressure okay there guys
so it sounds just like an air pressure or blood pressure cuff okay for your arm
and except you can choose the level of intensity you know how when you're
getting a blood pressure taking it feels good for a few seconds and then it gets
too tight but with this you could you could choose between the different levels and
it really it really helps alleviate foot pain
now I'm going to turn on the kneading with the air pressure
so much that you can individualize the heat the it's um it's really relaxing
this is really great to put on your desk if you sit at a desk whether it's at
home or in an office at work because you can kind of have it out of the way just
set your chair you're sitting anyway why not get a foot massage thanks for
watching
is it your turn yeah my feet better
They do feel better!
-------------------------------------------
Mobile Legends WTF Moments 23 - Duration: 10:53.
If you like my video please subscribe to the channel (Because it's free)
Plz subscribe to my channel to update the latest videos
Thank you so much for watching!
1 subscriber = million pleasure
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Kman夾娃娃 一箭雙鵰！！這也太爽了吧！一次就夾2隻超大娃。柯基、胡蘿蔔超大娃。クレーンゲーム Claw crane UFOキャッチャー#158 - Duration: 3:20.
For more infomation >> Kman夾娃娃 一箭雙鵰！！這也太爽了吧！一次就夾2隻超大娃。柯基、胡蘿蔔超大娃。クレーンゲーム Claw crane UFOキャッチャー#158 - Duration: 3:20. -------------------------------------------
Trailer Animasi Anicraft Part 2 Filler Animasi 4brother | Minecraft Animation Indonesia - Duration: 1:07.
Roman : I Have A Plan..
Animation Anicraft !
Will Be Different !
With Voice Actor !
Blane : What !!
Use Software...
Focuses To..
Story Animation Before 4brother.,
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Basic embroidery stitches | hand embroidery designs for beginners | new blouse models 2018 - Duration: 2:41.
Hand embroidery
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Comprehensive Earth Tectonics and Rock Cycle (Captions Included!) - Duration: 21:33.
Billions of years in the past when the earth was new
there were no rocks.
Earth was a burning hot gooey ball of melted minerals and metals
called magma.
Eventually, as heat drifted into space
Earth's surface cooled.
A thin crust of rock formed over it
like ice over a lake in winter.
The heart of the Earth, it's inner core,
is a solid ball of iron and nickle.
Here, the pressure is so high
it never melts
despite the intense heat of 3,700 degrees Celsius.
The outer core is under less pressure
so it is molten.
This is enclosed by a deep layer of hot rocks
called silicates.
This is the mantle.
And it's 3,000 km thick.
The surface is hard
and forms a solid crust.
If the Earth was a peach,
this crust would be as thin as its skin.
But the Earth's crust is cracked and brittle
like an egg shell.
It's made up of several segments
called tectonic plates.
The plates float on the dense mantle.
Scientists believe that the immense energy of the Earth's inner heat,
sets up convection currents in these rocks,
which move the crustal plates about
but very, very slowly.
I mean, let me just give you an example of this thick viscous flow stuff.
If you take a glass of honey and put it on a pot of warm water
such that it's being heated at the bottom and cooled at the top...
If you just look at it in real time,
it doesn't look like it's moving.
So as you can see, the honey looks
remarkably static.
And then below it, I've added a heat source, which is just
some water -- hot water
so what does our static honey look like
in time-lapse...
But if you add a little more timing to that, then all of a sudden
you can very easily see the convection currents.
And those are the convection currents which are moving around
the tectonic plates.
And these days we directly track that motion
with millimeter precision...
from space.
The common simplified explanation for why tectonic plates are moving,
is that they're carried along on currents in the upper mantle.
Some plates are moving apart.
Some move towards each other.
Other plates just slide past one another.
Converging currents drive plates into each other.
Diverging currents pull them apart.
This is mostly true.
Hot mantle rock rises from the core, and moves along under the crust
until it grows cool and heavy and sinks back down again.
But the plates aren't just passively riding these currents
around like a bunch of suitcases at the baggage claim.
They can't be.
Because some of the plates are moving faster than the currents underneath them.
For example,
the Nazca plate,
a chunk of ocean crust off the west coast of South America,
is cruising eastward, at about 10 cm per year.
while the mantle underneath it, oozes along at just five.
Neither tectonic plates, nor luggage,
can move faster than the belts they're riding on,
unless something else is helping to push or pull them along.
And some of Earth's plates,
it turns out,
are pulling themselves.
When an ocean plate collides with another ocean plate,
or a plate bearing the thick crust of continental land masses,
the thinner of the two plates bends and slides under the other.
As the edge of the sea floor sinks into the mantle,
it pulls on the plate behind it,
the same way a chain dangling further and further off a table
will eventually start to slide.
The bigger the sunken portion of the plate becomes,
the harder in pulls and the faster the remaining plate behind it moves.
What's more,
these chunks of sea floor are actually helping
to drive convection in the mantle beneath them.
Sunken slabs of ocean crust block flowing rock from moving further sideways,
forcing it to turn downwards and sink.
And eventually those slabs get too heavy and break off,
plunging slowly toward the core
and creating a suction force that pulls mantle material along behind them.
The plates are moving very, very slowly.
Less than five centimeters a year.
But over time,
this has added up...
In 1963,
Icelandic fishermen spotted plumes of ash, steam, and lava
shooting out of the sea.
Almost over night,
a new island emerged.
Lava poured out of the earth.
The eruptions didn't stop until four years later.
Within months, birds began to visit, and plants grew.
But what had happened?
At the bottom of the ocean,
two plates of continental crust had slowly moved apart.
Molten rock called magma,
lying below the plates,
oozed up through the cracks.
When it reached the surface,
the magma cooled and solidified,
forming lava.
This gradually built up,
until it broke through the ocean surface, to form an island.
A ridge of lava and mountains has been formed
where the two plates have moved apart.
This runs down the middle of the Atlantic ocean.
These mountains are caused by the collision of two plates of continental crust.
They're called fold mountains
because the layers of different rocks within the Earth's crust,
the strata,
are folded and bent.
Over time,
erosion of the layers can occur at different rates.
producing characteristic jagged rock formations.
There are two kinds of crust:
Continental crust forms the great landmasses of the world.
This is thick.
These rocks are made of ancient lightweight substances like granite.
Some were formed almost 4,000 million years ago.
Oceanic crust,
which lies under the planet's great oceans,
is much thinner.
Oceanic crusts like Basalt,
are heavy and much younger;
one twentieth the age of continental rock.
Volcanoes like Merapi in Indonesia,
are caused by the collision of oceanic and continental plates,
along what is known as a destructive margin.
Over millions of years,
heavier oceanic plate
is being forced down under the lighter continental plate,
creating a trench.
Carrying water and debris with it,
the oceanic plate breaks up under immense pressure.
As it's forced down, it gets hotter and hotter
due to friction,
and because the temperature rises rapidly towards the Earth's center.
Eventually it melts.
and the molten magma rises to form volcanoes some distance from the trench.
Sometimes,
a row of these volcanoes can form an island,
like Java
Millions of years of eruptions,
have made the country very mountainous
and fertile.
These volcanoes release ash and rocks that break down quickly into soil,
producing new supplies of the minerals plants use to grow.
This makes the land very productive.
So what happens within the volcano to make it erupt?
Molten magma from below the Earth's crust,
pushes up into the mountain.
This causes tremors,
and tilt meters can actually detect
how much the mountain is bulging as it fills with magma.
This is thick,
like porridge,
and when it reaches the surface, it solidifies into a hot crumbly plug.
Pressure on the magma builds up and bits fall off all the time.
The plug, or dome, gets too big and top-heavy.
Eventually, it's forced apart.
The liquid rock matter that we see coming out from volcanoes,
is called magma.
When this magma reaches the Earth's surface,
it is known as lava.
The cooling and the solidification of lava at the Earth's surface
result in the formation of extrusive igneous rocks.
They are also known as 'volcanic rocks'.
The cooling and the solidification of magma at a depth within the Earth's crust
result in the formation of intrusive igneous rocks.
So, we have learned that igneous rocks are of two types:
Extrusive igneous rocks,
and intrusive igneous rocks.
It is interesting to know that igneous rocks were the first to be formed.
Some of that original rock formed more than 3 billion years ago,
as Earth was cooling off.
Earth's surface cooled.
A thin crust of rock formed over it, like ice over a lake in winter.
This crust,
made of minerals and metals, cooled from red-hot magma,
was igneous rock.
Igneous rock occurs in many forms.
They vary according to the kind of minerals and metals they're made of,
and how fast they cooled.
Granite cooled slowly under ground over thousands of years.
Obsidian,
which looks like black glass,
cooled quickly.
As did pumice,
which floats in water.
Though varied,
all igneous rock hardened directly from magma.
The second rock of our story,
is sedimentary rock.
Sedimentary rock develops through a long process
that starts with weathering, and ends with lithification.
Weathering breaks down rocks on Earth's surface
through mechanical, chemical, and biological forces.
In mechanical weathering,
heat,
cold,
ice,
wind-blown sand,
and falls,
slowly crack and wear down rocks.
In chemical weathering,
rock dissolves in rain water,
which is slightly acid.
In biological weathering,
plant roots both crack and dissolve rocks.
Weathering occurs slowly,
but old grave stones in cemeteries show what can happen to exposed rock.
Over time,
even huge mountains weather bit by bit,
into sand,
dust,
clay,
and minerals dissolved in water,
and disappear.
200 million years ago,
the Appalachian Mountains were several times their present height.
Where did the mountains go?
They get carried away through erosion.
Wind, and especially water,
moves each bit of mountain rock downhill.
Eventually, eroded rock fills up nearby valleys,
or gets carried away in a river out to sea.
Where rivers flow into the sea, the land either pokes out, or bends inward.
So why do they have innies and outties?
well, an example would be,
during the last ice age,
sea levels fell by over 120 meters.
and rivers cut deeper and deeper valleys to reach the falling seas.
Then, about 18,000 years ago,
warming temperatures began to melt the ice,
and the now rising seas flooded river valleys around the world,
creating giant estuaries
and giving us the 'innie' riddled coast lines we have today.
But when the steady landward march of the seas
finally began to slow about 7,000 years ago,
the coastlines around the mouths of some rivers began to gain back some ground.
The key factor was the sediments that rivers drop
as their currents slow at the entrance to the sea.
Where the sediment supply was big enough and the ocean was calm enough,
the dropped dirt piled up,
eventually forming new land that both lengthened the river and divided it in two.
Dirt would continue to drop out and build up at the mouths of both channels,
splitting the river again,
and again,
and again.
Creating a new lobe of land advancing slowly into the sea.
Wherever they settle, sediments accumulate in layers.
In oceans,
sediment layers may grow higher than our tallest mountains.
Upper sediment layers press down on lower ones.
This helps lithification,
the process that turns sediments into stone.
Sometimes layers get squeezed so hard,
sediment grains get shoved into one another and lock into place.
Other times,
water evaporates from a layer,
and leaves behind minerals that glue together the tightly packed grains.
Either way,
what was once sand, mud, or gravel
becomes sedimentary rock.
Depending on how it formed,
sedimentary rock may be quite hard,
or rather weak and crumbly.
Sedimentary rock may not stay forever where it settled.
Strong forces within Earth,
sometimes push up rock from the bottom of a valley or an ocean
into spectacular peaks and long mountain chains.
Once sedimentary rock,
or any other kind of rock,
gets uplifted,
it undergoes another cycle of weathering.
This story's third chapter tells about metamorphic rock.
Metamorphic means changed.
Metamorphic rock may start as igneous,
sedimentary,
or even another metamorphic rock.
But then somewhere deep underground gets changed by heat and pressure.
There are two types of metamorphism that occur in nature.
The first type is called contact metamorphism,
and the second is called regional metamorphism.
And so I'm gonna show you how contact metamorphism works.
The reason it's called contact, is because it involves
existing rocks coming into contact with really intense heat,
which is generally provided by lava or magma.
So imagine that one day an intrusion of magma
forces its way up through these layers of rock.
Now,
all of the existing rock are gonna be burned by the heat of the magma.
So all along the edge of this magma,
shown here in orange,
you're gonna have rocks that have been burned by the heat of the magma.
That burning causes them to change
or metamorphosize (metamorphose)
into something new.
So anywhere you see the orange,
you're gonna have some metamorphic rock.
This is caused primarily by heat.
But let's talk about the second type,
regional metamorphism.
Now this one is gonna be more from pressure.
So let's imagine that I have a plate boundary here,
a fault, a crack.
and that these two plates are coming together.
So it's a convergent plate boundary.
Well, as you can imagine, in the middle here,
there's gonna be immense, immense pressure,
and that pressure can cause the rocks trapped in the middle
to become metamorphosized. (metamorphosed)
So all along this boundary, you'll find metamorphic rocks.
Again, this is different from contact in that it's not so much about the heat,
it's more about the pressure.
Let's take a look at what we see here.
This is a typical progression of metamorphism that occurs.
Starting with the sedimentary rock shale,
if you add heat and pressure, it will metamorphosize (metamorphose) to slate.
If you add more heat and pressure it will become phyllite.
More, and it will become schist.
Even more, and it will become the metamorphic rock gneiss.
Take a look at that gneiss sample right there,
you'll notice it has bands of minerals.
That's a result of the intense, intense pressure.
What once were flecks of black minerals, are now stripes or layers of it.
Now,
*inhale*
If you were to take gneiss and add additional heat and pressure,
it would likely melt into magma or lava,
and then it would become an igneous rock.
So gneiss is generally the extent of metamorphism that we see.
Even the beauty of metamorphic rock
cannot protect it from the forces of weathering.
If uncovered,
it too will eventually fall as sediments.
It starts long ago, and continues today,
with lots of fire and ice,
mountain peaks and ocean waves,
and more time than we can imagine.
So these are three rocks,
igneous,
sedimentary,
and metamorphic.
Some are as old as can be,
others, as new as today.
In a way,
they're all the same,
because they all started as hardened magma.
But still,
each is different
because rocks can change over long periods of time,
into rocks of another type.
For instance,
Igneous rocks can be broken down through weathering,
and the pieces can form sedimentary rocks.
Igneous rocks can also change into metamorphic rocks
when exposed to heat and pressure
that change them, but don't melt them completely.
If exposed to high enough heat,
they can melt back into magma,
to form new igneous rocks.
Sedimentary rocks
can break down through weathering to form new sedimentary rocks.
They can also be transformed into metamorphic rocks
through the action of heat and pressure.
If they get hot enough,
they can melt into magma
to form igneous rocks.
Metamorphic rocks can break down to form sedimentary rocks.
They can also be converted into different metamorphic rocks
when exposed to heat and pressure.
Like igneous and sedimentary rocks,
metamorphic rocks can melt into magma
to form new igneous rocks.
As you can see,
the interactions between the three main rock types
can take several different paths.
-------------------------------------------
Perman in hindi new episode - Peramn in hindi - Perman latest episode - Duration: 16:15.
For more infomation >> Perman in hindi new episode - Peramn in hindi - Perman latest episode - Duration: 16:15. -------------------------------------------
டாக்டர் மாத்துரு பூதம் எப்படி இறந்தார் தெரியுமா ? அதற்கு யார் காரணம் தெரியுமா ? Tamil Cinema News - Duration: 1:45.
For more infomation >> டாக்டர் மாத்துரு பூதம் எப்படி இறந்தார் தெரியுமா ? அதற்கு யார் காரணம் தெரியுமா ? Tamil Cinema News - Duration: 1:45. -------------------------------------------
Android Application | Bangla Romantic Love sms Collection - Duration: 3:10.
Android Application Bangla Romantic Love SMS Collection
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Dragon Ball Super Episode 114 English Sub CC YouTube - Duration: 19:02.
<i>Dragon Ball Super</i>
Take this!
Son Goku!
You're a nice team!
<i>Kale's powered up!</i>
<i>She unleashes her combos with Caulifla! Comin' right up!</i>
<i>INTIMIDATING PASSION! THE BIRTH OF A NEW SUPER WARRIOR!!</i>
That's...
That insane transformation from before?!
She's gone berserk again!
Amazing! Kale, this is amazing!
This tremendous energy...
Is it that Universe 6 Saiyan, Kale again?
It truly seems that Saiyans cannot be underestimated.
Here's something you should know.
Among those Saiyans, I stand at the top!
How arrogant.
There it is again!
The amazing Super Saiyan!
How huge. What amazing energy!
Kale, I knew you could do it!
You've finally made that power your own!
Can't you recognize me?
I'll get stronger too.
I'll get stronger, and with Sis...
You surpassed your limits...
...and summoned so much power you lost control.
Thanks, Kale.
You're amazing!
You're seriously amazing!
With this power, we can beat Son Goku!
That's my protegee for you.
Maybe I can't beat him alone,
but if we unite our strength, we're the strongest in all universes, right?
You're the only one who can fight by my side, Kale.
You're my precious protegee, and the best friend I've ever had!
Sis...
Let's go, Kale!
Yes, Sis!
Sorry to keep you waiting, Sis.
The main dish is still coming up!
She's not berserk.
She has that power completely under control.
Not only that, but Kale's energy has massively increased!
Okay! Nice, Kale!
You two should be able to beat Son Goku!
I can't stop shakin'. That must be her Saiyan instinct.
Not bad.
I better be careful or this could get messy.
Kale, you got it, right?
Yes! No matter what, I'll follow you, Sis!
That's not it!
Huh?!
We're going together!
If we unite our strength...
We're the strongest in all universes!
That's right!
I understand, Sis! From now on, we'll always be together!
Okay, let's pick things up!
Let's go, Kale!
Yes!
Take this!
C'mon! What's wrong?
You need more vigor!
Nice, Kale! Keep after him!
Okay, Sis!
Lemme pump some spirit into you!
Sorry, Tien. I'm borrowin' your attack.
Solar Flare!
Sis!
Ow!
Son Goku!
Sis was going to hit you!
Why did you dodge it?!
So, who is going to entertain me next?
I can't deal with this guy.
That's enough, Frieza!
Unfortunately for you, I've got you in my sights!
Oh? And you are?
My name is Katopesla!
I'm a Policeman of Justice, protecting the people of Universe 3 from evil!
For those I must protect, I shall unleash the power of my robot suit!
Mode change!
What?!
Now fall off!
Kale, don't go too far ahead!
Yes, Sis!
We're beating this guy together!
You?!
You're the guy who knocked Cabba off!
This is a rather obnoxious arrival, isn't it?
Sorry. Did I interrupt you?
However,
you've brought a rather interesting bonus with you.
I shall be taking these.
Huh? Hey!
Saiyans truly are suitable as playthings.
What?!
This is revenge for Cabba!
Saiyans are so persistent. I hate them!
Hold it. No fair, Frieza.
I was fightin' them.
First come, first served.
Then hurry up and lose so it's my turn.
I don't think so.
Don't get distracted by Frieza.
I'm the one you're fightin', right?
Frieza, hands off, okay?
Very well.
Watching Saiyans crush each other is the perfect show for me.
I shall enjoy the spectacle from above.
You're going nowhere, Frieza!
Observe the true power of my suit!
Mode change!
Whirlwind Speed Mode!
In Speed Mode, I can move 300 times as fast!
I can easily see through your attacks!
Now follow me!
I'll ignore that.
Okay, let's go all-out!
Are you okay by yourself?
You seem pretty confident against the two of us.
I'm not confident at all.
But,
I wanna fight with all I got against you two!
Well said!
Let's go, Sis!
Together with Sis, we're the strongest in all universes!
Right!
Go, Kale!
You're tryin' to create a smokescreen,
but your energy gives you away!
No, it's according to plan.
Great!
Keep him held, Kale!
Yes!
Good, Caulifla <i>san</i> and Kale <i>san</i>! You've got him on the ropes!
You two really are the strongest in all the universes!
Keep it up and knock Son Goku off!
He's completely at a disadvantage.
Dammit! He should have teamed up with Frieza!
Indeed, things look grim like this.
<i>He's disappearing!</i>
Right there!
How's that?!
Well done, Sis!
Of course!
So, this attack won't work anymore.
You're a nice team!
He became Super Saiyan God!
I thought he hadn't fully recovered yet.
That's Goku.
Huh?
No matter how bad things are, He's always exceeded our expectations.
So he's starting with red.
Red or blue, it's all the same!
Let's beat him up!
Well said!
Let's do it!
Yes!
Sis!
Dammit!
Take this!
Nice going, Kale!
Don't be so sure!
What?!
He withstood that?!
Good! Keep it up Goku!
It looks like he really does exert power beyond his limitations.
Well done, Goku <i>san</i>!
He's in a different class from those two Universe 6 Saiyan women!
Then how about times two?!
Hit him from both sides, Kale!
Yes!
It's tracking me! What a pain!
Sis!
Sis! Are you all right?!
Can you move?
Sis!
Both of you did well.
You're both pretty impressive, but your end game needs work.
After the Tournament of Power's over let's do this again sometime.
You think you've won?!
Sis?!
I can... still fight.
Sis!
How pathetic.
Kale.
I told you if we unite our strength, we're the strongest in all the universes, right?
Y-Yes.
Okay.
Take out that thing we got before the tournament.
You mean...
Ka... Me...
Ha... Me...
Ha!
Great! We knocked them both off at once!
Yes, yes, yes, yes! Yes!
Is that...?
You're...?!
Kale and Caulifla make...
...Kefla!
There's the Potara! At last!
I'm the one who lent those to you in the first place.
No need to split hairs!
Pulverize him!
That's...
Listen up!
The items I just gave you are a last resort!
Don't use them lightly!
This isn't really my style.
I said not to use them lightly!
What?!
Cabba, you can have mine.
Mine too.
I don't want them!
Those things are amazing items, all right?
From back then...
The new body and personality born from a Potara fusion...
...are more than the sum of their parts and their power increases tens of times.
Exactly!
See that? A real trump card is saved until the last moment!
Please win, Kale <i>san</i> and Caulifla <i>san</i>!
I mean, Kefla <i>san</i>!
I feel great!
I can feel infinite power bubbling up from deep inside!
It's so massive, I can't sense a limit to her energy.
<i>What's that? I sense an incredible energy near Kakarot.</i>
You're open!
This will be an entertaining fight.
Time to test just how far I can go with this power!
Whoops!
Lame!
<i>Kale and Caulifla fused by using the Potara.</i>
<i>Their new name is Kefla.</i>
<i>Will Goku's Universe 7 be able to win...</i>
<i>...against this powerful enemy, Kefla, and Universe 6?</i>
<i>The universe's fate is at stake in the Tournament of Power.</i>
<i>The time until it ends is 21 minutes.</i>
This is my power!
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