Everything You Need to Know About Planet Earth

Kurzgesagt – In a Nutshell
4 Aug 201407:22

Summary

TLDRThis script explores the origins and composition of Earth, from its formation 4.6 billion years ago from remnants of dead stars to its current state. It delves into the violent early history, the creation of the Moon, and Earth's cooling process that led to the emergence of water and life. The script also describes the Earth's structure, from the crust to the core, and the importance of its magnetic field. It touches on the atmosphere's layers and the human perspective, highlighting our brief existence in the grand scheme of Earth's history.

Takeaways

  • 🌍 Earth is the only known home to all lifeforms in the universe, with an age about one-third that of the universe itself.
  • 🌗 Earth's composition includes a heavy metal core, a lighter surface crust, and a thin atmosphere, with vast oceans and diverse landscapes.
  • 💥 Earth was formed around 4.6 billion years ago from the remnants of dead stars, through a process that took 10 to 20 million years.
  • 🌕 A massive collision with an object about the size of Mars led to the creation of the Moon, which is unusually large relative to Earth.
  • 🔥 Initially, Earth was a hot and chaotic planet with a toxic atmosphere, seas of lava, and constant asteroid impacts.
  • 💧 Earth cooled down, allowing water from its interior to reach the surface, forming clouds and eventually oceans as more water was delivered by asteroids.
  • 🌊 Today, Earth's surface is 71% water and 29% land, with the majority of water being saline, and a small fraction being fresh and accessible.
  • 🌳 The cooling of Earth led to the formation of a thin crust, under which hot rock movements cause plate tectonics, shaping the planet's geography.
  • 🏞️ Plate tectonics result in the formation of mountains like Mt. Everest and deep trenches like the Mariana Trench, despite their relative smallness in Earth's cross-section.
  • 🌐 Earth's core, especially the outer core of liquid iron and nickel, generates a magnetic field that protects the planet from high-energy particles.
  • 🌌 The atmosphere consists of several layers, including the troposphere where weather occurs, the stratosphere with the ozone layer, and the thermosphere where the International Space Station orbits.
  • 🕊️ Humans have existed for only 200,000 years, a tiny fraction of Earth's history, and we inhabit a thin, moist layer on this small, wet rock we call home.

Q & A

  • What is the estimated age of Planet Earth in relation to the universe?

    -Planet Earth is about 1/3 the age of the universe.

  • How was Earth formed according to the script?

    -Earth was created from the remnants of dead stars that collected in a giant, dirty gas cloud, which later formed an accretion disk and led to the formation of planets.

  • What significant event occurred during the early formation of the solar system that impacted Earth?

    -A giant object, about as big as Mars, collided with Earth, causing a violent impact that could have destroyed it if the object had been more massive.

  • How was the Moon formed in relation to Earth?

    -Materials from Earth were smashed out into orbit due to a collision and formed the Moon, which is the largest satellite in relation to its planet in the solar system.

  • What drastic change occurred on Earth that led to the formation of its surface?

    -Earth cooled down, and water from the inside of the Earth wandered to the surface, rained down, vaporized, and became clouds, leading to the formation of the surface crust.

  • What percentage of Earth's surface is covered by water?

    -71% of Earth's surface is covered by water, while 29% is land.

  • What is the composition of Earth's fresh water?

    -Fresh water is composed of 69% ice and snow, 30% ground waters, and about 1% in lakes and rivers, with a very small part bound in living things.

  • What is 'Plate Tectonics' and how does it affect Earth's surface?

    -Plate Tectonics is the process where the crust of Earth, consisting of separate giant plates, moves around, creating mountains or deep trenches when they meet or crumble.

  • How thick is Earth's crust on average, and what is the deepest hole ever drilled by humans?

    -Earth's crust is about 50 kilometers thick on average, with variations between 5 and 70 kilometers. The deepest hole ever drilled by humans is 12.262 kilometers deep.

  • What are the main layers of Earth's interior from the crust to the inner core?

    -The main layers of Earth's interior are the crust, mantle (upper and lower), outer core, and inner core.

  • What is the significance of Earth's magnetic field and how is it related to the core?

    -Earth's magnetic field diverts high-energy particles from the Sun and other sources, providing a stable environment with less radiation impact. It is related to the core where large electrical currents flow in complicated patterns, creating a magnetic field through a system known as the Dynamo.

  • How long have humans, in their present form, been around in the context of Earth's history?

    -Humans, in their present form, have been around for 200,000 years, which is 0.004% of Earth's history.

Outlines

00:00

🌏 The Formation and Composition of Earth

This paragraph delves into the origins and makeup of our planet, Earth. It describes Earth as a celestial body that is about 1/3 the age of the universe, with a composition of a metal core, a crust, and an atmosphere. Earth's creation is traced back to 4.6 billion years ago from a gas cloud formed by remnants of dead stars. The process of planet formation through accretion, which took 10 to 20 million years, is highlighted, along with a significant event where a Mars-sized object collided with Earth, leading to the formation of the Moon. The paragraph also touches on Earth's early conditions, the cooling process, and the emergence of water, leading to the current distribution of water and land. It concludes with an explanation of plate tectonics, the structure of Earth's interior, and the presence of Earth's magnetic field, which shields the planet from high-energy particles.

05:01

🌌 Earth's Atmosphere and Human Existence

The second paragraph focuses on Earth's atmosphere, detailing the composition of air and the layers of the atmosphere that are vital for human life. It explains the Troposphere as the weather layer, the Stratosphere with the ozone layer, the Mesosphere as the coldest place on Earth, and the Thermosphere where space begins. The paragraph also describes the Ionosphere, aurora phenomena, and the International Space Station (ISS). It emphasizes the Exosphere, which merges with outer space, and the relative insignificance of human existence, spanning only 200,000 years, or 0.004% of Earth's history. The summary concludes by reflecting on human life as a part of the universe's ongoing cycle of creation and destruction.

Mindmap

Keywords

💡Planet Earth

Planet Earth refers to our home planet, the only known place in the universe that supports life. It is the central focus of the video, illustrating the planet's composition, history, and the life-sustaining environment it provides. The script describes Earth's features such as its oceans, atmosphere, and landforms, emphasizing its uniqueness and importance in the cosmos.

💡Accretion Disk

An accretion disk is a structure formed when particles in a gas cloud come together under gravitational attraction, leading to the creation of celestial bodies like planets. In the script, the formation of Earth is described as beginning with the development of an accretion disk from the remnants of dead stars, highlighting the process that led to the birth of our planet.

💡Plate Tectonics

Plate tectonics is the geological process involving the movement of Earth's lithosphere, which is composed of tectonic plates. The script explains that this process is responsible for the formation of mountains and trenches, such as the Himalayas and the Mariana Trench, and is ongoing, shaping the Earth's surface over time.

💡Mantle

The mantle is a layer of Earth between the crust and the core, consisting of silicate rock and extending about 2,900 kilometers in thickness. The script distinguishes between the upper and lower mantle, describing the mantle's role in supporting the lithosphere and the asthenosphere, which contributes to plate tectonics.

💡Outer Core

The outer core of Earth is a liquid layer composed mainly of iron and nickel, with a thickness of approximately 2,266 kilometers. The script mentions the high temperatures within the outer core, which range from 4,000℃ to 5,700℃, and its significance in generating Earth's magnetic field.

💡Inner Core

The inner core is the central, solid part of Earth, made primarily of an iron-nickel alloy. With a radius about 70% that of the moon, the script notes its slow growth at a rate of about 1mm per year and its extremely high temperatures, comparable to the surface of the Sun.

💡Magnetic Field

Earth's magnetic field is an invisible force that protects the planet from high-energy particles and solar radiation. The script explains its importance in maintaining a stable environment on Earth, although the exact mechanisms behind its creation remain somewhat mysterious, being related to the movements within the Earth's core.

💡Atmosphere

The atmosphere is the layer of gases surrounding Earth, which includes nitrogen, oxygen, argon, and other trace gases. The script describes the different layers of the atmosphere, such as the troposphere where weather occurs, the stratosphere with the ozone layer, and the thermosphere where the International Space Station orbits.

💡Water Cycle

The water cycle is the continuous movement of water on, above, and below the surface of the Earth. The script explains how water from the Earth's interior reached the surface, evaporated to form clouds, and was brought to the planet by asteroids, ultimately covering 71% of the Earth's surface in water.

💡Fresh Water

Fresh water is a vital resource for life, making up only 2.5% of all water on Earth. The script details that most of this fresh water is in the form of ice and snow, with a smaller portion as groundwater, and an even smaller fraction in lakes and rivers, emphasizing the scarcity and importance of this resource.

💡Aurora Borealis

The aurora borealis, also known as the Northern Lights, is a natural light display in the Earth's sky, predominantly seen in the high-latitude regions. The script mentions the aurora borealis as a phenomenon occurring in the thermosphere, illustrating the beauty and complexity of Earth's atmospheric interactions with solar particles.

Highlights

Planet Earth is the only known home of life in the universe, with an age about 1/3 that of the universe itself.

Earth's composition includes a heavy metal core, lighter surface crust, and a thin atmosphere, with vast oceans, fertile plains, and magnificent mountains.

The Earth was formed 4.6 billion years ago from the remnants of dead stars that collected in a giant, dirty gas cloud.

The process of planet formation through accretion from small particles to larger objects took 10-20 million years and is still not well understood.

A violent collision with an object about the size of Mars during the early, chaotic solar system led to the formation of the Moon, Earth's largest satellite relative to its planet.

After the collision, Earth was a hot, hellish place with lava seas and a toxic atmosphere, but it eventually cooled, allowing water to emerge from the interior and rain down.

Millions of asteroids contributed to Earth's water supply, with the total volume of water on Earth being a small fraction of the planet's size.

71% of Earth's surface is water, with 97.5% being saline and only 2.5% fresh water, most of which is in the form of ice and snow or groundwater.

The Earth's crust, which humans live on, is a thin layer about 50 kilometers thick, with the deepest human-made hole being only 12.262 kilometers deep.

Plate tectonics, the movement of Earth's crustal plates, is responsible for the formation of mountains and trenches, including the highest (Mt. Everest) and deepest (Mariana Trench) places on Earth.

The mantle, a silicate rocky shell about 2,900 kilometers thick, consists of the upper and lower mantle, with the upper part including the viscous lithosphere and the asthenosphere.

Earth's outer core is a liquid layer of iron and nickel, with temperatures ranging from 4,000℃ to 5,700℃, and the inner core is a solid iron-nickel ball with a radius about 70% that of the Moon.

The inner core is slowly growing at an estimated rate of 1mm/year, and the Earth's magnetic field, generated by the dynamo effect in the core, protects the planet from high-energy particles.

The Earth's atmosphere, composed mainly of nitrogen, oxygen, argon, and trace amounts of other gases, has distinct layers including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.

The troposphere, where weather occurs, is the lowest layer of the atmosphere and is on average 12 kilometers thick, while the stratosphere contains the ozone layer that shields us from harmful UV radiation.

The mesosphere is the coldest place on Earth with an average temperature of -85℃, and the thermosphere marks the beginning of space at about 80 kilometers above the surface.

The exosphere is the outermost layer of the atmosphere, extending up to 10,000 kilometers and merging with outer space where atoms and molecules are sparse.

Humans, in their current form, have only existed for 200,000 years, which is a mere 0.004% of Earth's history, emphasizing our relatively recent arrival on this ancient planet.

Transcripts

play00:00

Planet Earth is the home of every lifeform,

play00:02

known to us, in the universe.

play00:05

Its age is about 1/3 of the age of the universe

play00:07

and, admitted,

play00:09

It is a thing of beauty.

play00:11

a slightly squashed fair with a heavy metal core,

play00:14

and a lighter surface crust,

play00:15

wrapped in a thin sliver of sweet air to breathe,

play00:18

with vast oceans,

play00:20

fertile plains,

play00:21

magnificent mountains,

play00:23

fresh water rivers, streams, lakes and aquifers,

play00:26

orbiting a star which warms us,

play00:28

and gives us energy.

play00:30

But how did our home come in to existence,

play00:32

and what's it made of?

play00:41

4.6 billion years ago,

play00:43

Earth was created from the remnants of dead stars,

play00:46

that collected in a giant, dirty gas cloud.

play00:49

The gas cloud became denser in its center,

play00:51

and formed an accretion disk.

play00:53

small particles started clumping together,

play00:56

and building larger and larger objects,

play00:58

until they form the objects we call "Planets" today.

play01:01

This process took 10 to 20 million years,

play01:04

and is still not very well understood.

play01:07

At about this time, when the solar system was young and chaotic,

play01:10

a giant object, about as big as Mars,

play01:12

collided with our home.

play01:14

The impact was violent,

play01:16

and if the object had been more massive,

play01:18

it might have destroyed Earth.

play01:20

Materials from Earth were smashed out into orbit,

play01:22

and formed the Moon,

play01:24

which is the biggest satellite in relation to its planet in the solar system.

play01:28

At this time, Earth was a hot hell,

play01:30

constantly being hit by asteroids,

play01:33

with seas of lava,

play01:34

and a toxic atmosphere.

play01:36

But something was about to change drastically.

play01:38

Earth cooled down.

play01:40

Water from the inside of the Earth

play01:42

wandered to the surface and rained down on Earth,

play01:45

only to vaporize again and become clouds.

play01:48

Millions of asteroids brought more and more water to our planet.

play01:52

All the water on Earth has about this volume compared to Earth.

play01:57

Today,

play01:58

the surface of Earth is 71% water,

play02:00

and 29% land.

play02:02

97.5% is saline water,

play02:05

while only 2.5% is fresh water.

play02:08

The Fresh water is 69% ice and snow,

play02:11

30% are ground waters,

play02:13

and only about 1% make up the remaining ground waters.

play02:17

But even this small part is mostly frozen.

play02:20

Only a tiny part of our water is actually lakes and rivers.

play02:23

and an even tinier part is bound in living things.

play02:27

So, gradually the Earth cooled down,

play02:30

and the surface formed a thin crust.

play02:32

But inside the earth, hot rock continue to swirl about,

play02:35

moving the crust from below and breaking it apart.

play02:39

This process is called "Plate Tectonics",

play02:41

and is happening right now.

play02:43

We'll make a whole video about it in the future.

play02:46

For now,

play02:47

let's just say that the crust of Earth consisted of

play02:49

separate giant plates that move around.

play02:51

As they meet, they crumble, and create mighty mountains.

play02:55

OR:

play02:55

violently plunge back down, deeper into Earth,

play02:57

creating deep trenches.

play03:00

That's the way the highest place on Earth was formed: Mt.Everest,

play03:03

and the deepest: the Mariana Trench.

play03:05

From our perspective,

play03:07

Earth's mountains and trenches are mighty indeed,

play03:10

but when you look at the Earth in cross-section,

play03:12

you can see how tiny they actually are.

play03:15

The part we stand on is the crust,

play03:17

which is about 50 kilometers thick,

play03:18

though it can vary between 5 and 70 kilometers

play03:22

By the way,

play03:22

the deepest hole ever drilled by man

play03:24

is 12.262 kilometers deep.

play03:27

After the crust, comes the mantle.

play03:29

It's a silicate rocky shell,

play03:30

and about 2,900 kilometers thick.

play03:33

The mantle consists of the upper mantle, and the lower mantle.

play03:37

The upper mantle has different regions, too.

play03:39

It's upper part, which is viscous and carries the crust,

play03:42

is called the "Lithosphere."

play03:44

After that, there comes the "Asthenosphere,"

play03:46

which consists of less mobile, mostly solid material.

play03:50

The lower mantle reaches deep down to the outer core of Earth.

play03:54

Earth's outer core is a liquid layer of iron and nickel,

play03:57

about 2,266 kilometers thick.

play04:00

Temperatures vary from 4,000℃(7,232℉)

play04:03

to 5,700℃(10,292℉).

play04:06

And in the center, is the inner core.

play04:09

It's mostly solid,

play04:10

a ball made of an iron-nickel alloy.

play04:12

with a radius of about 1,200 kilometers.

play04:15

70% of the size of the moon,

play04:17

and about the temperature of the surface of the Sun.

play04:20

It is slowly growing

play04:21

at an estimated rate of about 1mm/year.

play04:25

Now, for some respective,

play04:27

this small layer of crystallized melt products of former molten mantle,

play04:31

is where we live.

play04:33

Then, there's Earth's magnetic field.

play04:36

It's an invisible phenomenon

play04:38

that diverts high energy particles coming from the Sun and other sources,

play04:41

allowing for a stable environment

play04:43

with comparatively little radiation impact on Earth.

play04:46

But why is it there?

play04:48

Actually, we don't really know a terrible lot about that.

play04:51

We know, it has something to do with the core of Earth.

play04:54

Inside this metal sphere,

play04:56

large electrical currents flow in complicated patterns.

play04:59

They cause a magnetic field,

play05:01

that sort of stabilizes itself according to the laws of electrodynamics.

play05:05

This entire system is called the "Dynamo."

play05:08

But, don't let us fool you into thinking we have it all figured out.

play05:12

Speaking of breathtaking information,

play05:14

what about the airy stuff that surrounds us?

play05:17

By volume,

play05:19

dry air consists mostly of Nitrogen,

play05:21

Oxygen,

play05:22

Argon,

play05:23

Carbon,

play05:24

a variable mount of water vapor,

play05:25

and small amounts of other gases.

play05:28

Humans are very dependent on the lowest layer of the atmosphere:

play05:31

the Troposphere - Where the weather is.

play05:34

It's 12 kilometers thick on average.

play05:36

Above that is the Stratosphere,

play05:38

which is where the ozone layer protects us

play05:40

from the sun's most aggressive type of light.

play05:42

Above that is the Mesosphere - the coolest place on Earth,

play05:46

with an average temperature around -85℃(-121℉).

play05:50

At about 80 kilometers up, the Thermosphere starts.

play05:54

The transition to space is a fluent one, without clear borders.

play05:57

but humans decided that space starts here.

play06:00

At about 100 kilometers, Earth stops, and space begins,

play06:03

though the atmosphere extends a bit further.

play06:06

In this region, we find the Ionosphere,

play06:09

the aurora borealis,

play06:10

and the ISS,

play06:12

and the outermost layer is the Exosphere,

play06:15

stretching up to 10,000 kilometers.

play06:18

It merges fluently with outer space,

play06:20

where there's no atmosphere at all.

play06:22

The atoms and molecules in this area are so far apart,

play06:25

that they can travel hundreds of kilometers

play06:27

without colliding with each other.

play06:29

OK.

play06:30

Humans, in their present form,

play06:32

have only been around for 200,000 years.

play06:35

- that's 0.004% of Earth's history.

play06:39

Not long, really.

play06:40

And, here we are now,

play06:41

living in a thin, moist layer on a small, wet rock.

play06:45

We call this rock: Earth.

play06:48

It is the product of the universe's deepest workings,

play06:50

the result of a constant process of creation and destruction,

play06:54

happening all of the universe, all the time,

play06:57

helped by chance,

play06:59

the laws of the universe and random events,

play07:02

we are really lucky.

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Related Tags
Earth FormationPlanetary ScienceGeological HistorySolar SystemPlate TectonicsAtmospheric LayersMagnetic FieldHydrosphereCrust DynamicsAstrobiologyCosmic Events