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Something weird is happening on the planet
Venus. We know that Venus is the

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most earthlike planet in the Solar System, practically our twin sibling, So in

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theory this place should be very familiar
to us. But in reality, Venus

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is so incomprehensibly strange that we still
understand very little about the true nature of

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this planet. So are we looking
at a vision of the future, the

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nightmarish end that awaits all planets,
or is Venus a memory of our past,

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of a time when the Earth itself
was a young, hot volcanic wasteland.

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The real secrets lie beneath the surface
and above the clouds. This is

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the mystery of the planet Venus.
We know that there are many similarities between

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Venus and the Earth. Both planets
are very similar in size and mass,

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they have the same rocky composition,
They orbit in a relatively similar proximity to

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the Sun. But one of these
stranger similarities between the two planets is that

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both both Venus and the Earth have
a young, rejuvenated surface. So what

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do we mean by that? Well, if you look at the surface of

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Mars Mercury or Earth's moon, you'll
find a dense pattern of impact craters.

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These are the remnants of multi billion
year old asteroid impacts that occurred when the

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Solar System was young and still full
of rocky leftovers from the formation of planets

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and moons. The Earth was not
spared from this ancient bombardment. Our surface

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would just be as pockmarked as the
Moon if not for the continuous rejuvenation of

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plate tectonics. The Earth is constantly
recycling mass from the surface down into the

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mantle and creating new land through volcanic
eruptions. The surface of Venus appears to

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tell a similar story. The ancient
battle scars have been wiped away, leaving

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the age old Venusian surface at somewhere
between three hundred million and one billion years

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old. Except Venus does not have
plate tectonics. Instead, it has one

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continuous and stagnant lid of rock that
surrounds the entire globe. So there's no

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easy explanation as to how the entire
planet has been resurfaced in such a relatively

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small amount of time. Even one
billion years on the cosmic scale is fairly

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young. You don't need tectonic plates
to have volcanic activity, and this is

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how we identify that Venus has a
stagnant lid. For a surface. On

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the Earth, active volcanoes are concentrated
along the borders between the tectonic plates,

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while on Venus there are thousands of
volcanoes spread out across the surface in a

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seemingly random distribution. This would indicate
that volcanoes simply spring up at any location

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where the surface crust is thin,
and that their formation is not driven by

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physical movement. We have evidence that
volcanic activity on Venus continues to the present

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day, but this still doesn't fully
explain the re surfacing event. Planets with

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a stagnant lid will have lower overall
volcanic activity than similar planets with tectonic plates.

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On the Earth, volcanoes sweep back
and forth across the surface over millions

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of years, violently reshaping the land
as they go, while on a planet

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like Mars, volcanoes just sit in
the same place for millions of years,

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slowly and steadily erupting until they form
gigantic mountains like Olympus Monds, the highest

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peak in the Solar System. Actually, most of the highest mountains in the

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Solar System are located on Mars.
Thanks to its stagnant lid and stationary volcanoes.

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You would think that a similar thing
would happen on Venus, but that's

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not been the case. It does
have a couple of very tall mountains,

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but overall the surface of Venus is
much closer to Earth than it is to

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Mars, which still leaves us wondering
just what the hell happened here. One

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of the more interesting theories about the
resurfacing of Venus is that it all happened

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fairly abruptly in an explosive global cataclysmic
event. The idea is that the stagnant

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lid of the Venusian surface probably traps
in a lot of pressure underneath the surface,

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and since Venus is pretty close to
the Sun, much closer than Mars,

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there is the likelihood that a lot
of thermal energy could build up inside

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the planet over hundreds of millions of
years, and eventually this pressure is going

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to reach a point where it can't
be contained any longer, releasing as one

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catastrophic global volcanic eruption. If Venus
did burst like an overfilled balloon at some

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point within the past billion years,
this would explain everything that we see on

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the planet today. After the volcanic
pressure release, the planet would cool back

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down into a freshly resurfaced globe.
Unfortunately, this cataclysmic event permanently erased any

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surface evidence of the ancient past on
Venus. When we look at the planet

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Mars, we know that there was
a time when liquid water flowed over the

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surface in ancient rivers, lakes,
and even oceans. If a relatively small

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and cold planet like Mars could support
the necessities of life, then it stands

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to reason that Venus probably could have
done the same. In order to find

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the proof, we need to move
up. We know that the atmosphere on

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Venus is incredibly hostile. We know
that is caused by a runaway greenhouse effect,

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but we're not entirely sure how it
got that way. To begin with,

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the surface pressure of Venus is ninety
two bar. That means the air

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is ninety two times more dense than
what we find at the surface of the

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Earth. The majority of the Earth's
atmosphere is actually composed of nitrogen, one

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of the most common elements in the
known universe. It accounts for around seventy

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eight percent of the air. Oxygen
is only around twenty one percent, and

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the remaining one percent is mostly an
inert noble gas called argone, and zero

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point four percent of the Earth's atmosphere
is occupied by greenhouse gases like carbon dioxide,

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methane, and ozone. Interestingly enough, we know that Venus has around

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the same massive nitrogen in the atmosphere
as Earth does, and there are even

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detectable amounts of molecular oxygen on Venus, but that is all dwarfed by an

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unfathomable amount of carbon dioxide. In
the Venusian atmosphere, it makes up over

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ninety six percent of the total composition
and at ninety two bar of density,

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that is a lot of carbon dioxide. But where does it all come from?

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The Earth manages its own carbon dioxide
through a natural cycle. CO two

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is absorbed by plants, they die, they fossilize, and then plate tectonics

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eventually pull the fossils down deep into
the mantle. Then humans came along and

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started burning the fossils and putting them
straight back into the atmosphere. But that

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likely wasn't the case on Venus,
and it's also not likely that Venus just

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happens to have a massive amount of
excess CO two that the Earth does not.

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As far as we can tell Venus
and the Earth started out as nearly

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identical balls of molten rock. The
chemical composition should be more or less the

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same, meaning that some kind of
natural force moved all of the excess carbon

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from the inside of the planet to
the outside and created the runaway greenhouse effect

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that has superheated the planet's surface.
This could have happened during the planet wide

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cataclysm. That would be a reasonable
explanation, meaning that Venus hasn't actually been

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what it is now for all that
long. Venus is closer to the Sun

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than the Earth, but only by
around thirty percent, which is not enough

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to cause a huge difference in temperature. If you take the excess atmosphere out

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of the equation, the average surface
temperature of Venus would be around seventy degrees

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celsius, which is still too hot, but it's as close to Earth temperature

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as we would ever find anywhere in
the Solar System. In fact, it's

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very likely that there was a time
when the atmospheric conditions of Venus were very

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similar to the Earth, complete with
large amounts of liquid water. Now,

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like we said earlier, any geological
evidence of flowing water is long gone from

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the surface of venus, but the
chemical evidence does remain. This comes in

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the form of an atom called deuterium. Okay, stick with me here.

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Deuterium is an isotope of hydrogen,
which basically means that deuterium is a unique

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variant of hydrogen that is created by
the addition of a neutron inside the core

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of the atom. Typical hydrogen only
has one proton in the nucleus, while

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deuterium has a proton and a neutron
inside the nucleus. This gives utium a

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heavier atomic weight than hydrogen, and
on Earth there is typically one deuterium isotope

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for every six thousand, four hundred
and twenty atoms of hydrogen. Here's the

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payoff. The concentration of deuterium atoms
on venus is significantly higher, meaning that

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at some point there was a massive
amount of hydrogen that dissipated into space and

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left behind its heavier isotope variance.
This is a smoking gun indicator of a

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water boil off event. The water
boiled into steam, and the lightest hydrogen

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atoms in that steam floated all the
way up into the atmosphere and were carried

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away by the solar wind, while
the heavier atoms remained trapped somewhere in between.

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So in this way, when we
look at Venus, we are seeing

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a likely future for the Earth.
We often use Mars as an example of

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a dead planet because its geological activity
has ground to a halt, the atmosphere

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has dissipated, and the average surface
temperature has dropped below freezing. But this

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is more like a planetary coma death
is still to come. We live next

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to a gigantic nuclear fusion reactor that
is gradually increasing in power right up until

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the hydrogen fuel source is depleted.
Our Sun won't explode when it dies,

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but it will expand outward to become
a red giant, which will then eject

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its corona and collapse into a white
dwarf star surrounded by a nebula of matter

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that used to be our solar system. Long story short, In the end,

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everything burns. The Earth will not
go quietly into that good night anyway,

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nihilism aside. Our own planet will
gradually, over billions of years,

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start to look a lot more like
Venus, so we can kind of reverse

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engineer the process. It's likely that
the water boil off comes first. The

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Earth's magnetic field won't last forever.
We're not sure if Venus ever had a

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magnetosphere or if it just dissipated very
early on, which would explain the planet's

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short lifespan. Loss of the magnetic
field allows the atmosphere to thin, end

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hydrogen to escape. Lower atmospheric pressure, combined with a hotter sun, means

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that water evaporates much faster and fails
to recondense into rain. With no water,

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the surface of the Earth gets dry
and stiff, which is probably what

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brings an end to plate tectonics and
causes the outer trust to solidify into a

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stagnant lid. Now, thermal energy
builds up under the sealed crust of the

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Earth until it pops like a balloon, and the entire surface is engulfed in

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volcanic activity, spewing massive amounts of
heavy carbon gas into the atmosphere to form

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dense clouds that cling to the planet. And just like that, the Earth

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five billion years in the future would
be largely indistinguishable from the planet Venus as

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we see it today, unless through
reverse engineering Venus' demise, we can somehow

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figure out how to stop our planet
from sharing the same fate.
