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Sejarah evolusi Bumi: Mengisahkan kembali asal usul terbentuknya planet kita | DW Dokumenter

1:25:18EnglishBy DW DokumenterTranscribed Jul 25, 2026
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0:11

Rock.

0:14

They existed long before oceans,

0:17

forests,

0:18

and plants formed.

0:20

Even before the oxygen we breathe.

0:27

Rocks have existed since the beginning of time.

0:30

They are not just hard surfaces on which we stand,

0:35

but also the main figures

0:39

and silent witnesses of

0:40

Earth's long history. The

0:51

stunning rock formations

0:53

hold tales of rebirth,

0:56

violent upheaval,

0:57

and miracles.

0:59

Its existence is often misunderstood,

1:01

even though it is very essential.

1:04

Because it is in this mineral material that the

1:06

origin of life begins. The

1:12

coevolution of rocks and life is

1:14

one of the most fascinating aspects of Earth's history. There

1:19

can be no life without minerals.

1:24

Without rocks, there

1:26

would be no oxygen,

1:28

continents,

1:29

landforms,

1:31

plants, or

1:32

even animals.

1:36

For billions of years,

1:38

minerals and life have been interconnected.

1:41

The relationship developed slowly and steadily. It is

1:44

very important for the survival of the Earth.

1:47

Until one day,

1:48

one species started to interfere.

1:52

At first it didn't feel like it,

1:54

then it developed so quickly.

1:58

Since the beginning,

1:59

humans have needed minerals.

2:02

Over time,

2:03

the relationship became more complicated.

2:11

Within the rocks of the Earth,

2:13

hidden stories of the beginning of life, the

2:15

complex structure of the world,

2:17

and the balance of forces

2:19

that have long shaped life.

2:25

This is the history of Earth.

2:28

Our history.

2:53

One thing we know is that

2:55

our Earth formed about

2:57

4.5 billion years ago.

3:04

Formed from material that previously came from

3:07

exploded stars.

3:15

Throwing minerals,

3:17

ice,

3:17

and other materials into space.

3:30

Earth, the

3:31

solar system,

3:32

did not exist in the beginning.

3:33

What exists is a cloud of dust and gas.

3:42

Mainly hydrogen and helium,

3:44

which combined to form the Sun.

3:50

Stardust is a small mineral particle

3:54

that, due to gravity,

3:55

turns into a larger clump.

3:58

From the size of a fist, a

4:00

basketball, a

4:01

room,

4:02

to hundreds of kilometers.

4:07

And when the rocky planet began to form,

4:10

all of those dust particles

4:12

became the minerals that formed

4:14

planet Earth. The

4:23

early Earth

4:24

formed from an accumulation of small, mineral-rich dust particles,

4:28

all of which originated from stars.

4:31

So fundamentally,

4:33

we are all made of stardust.

4:43

We are all made of stardust.

4:47

This means that

4:48

everything on Earth

4:50

is a legacy of the stars.

4:53

However,

4:54

in its early days, the

4:55

blue planet was very different

4:57

from what it is today.

5:06

Once the Earth

5:07

was a burning ball of fire.

5:10

Molten mass exposed to solar wind

5:12

and meteorite impacts.

5:15

The surface is covered in a sea of

5:17

boiling magma.

5:23

When the Earth was born, it was

5:25

incredibly hot.

5:27

It is estimated that within 30 or 40 million years after it formed, the

5:30

Earth melted.

5:40

In geology,

5:42

the history of the Earth is divided into several eras.

5:45

The first is the Hadean Era,

5:47

inspired by the name Hades.

5:50

At that time the Earth was very hot, with

5:53

almost no crust. It has

5:54

little solid surface

5:56

and a very thin atmosphere.

5:59

The Earth is also covered in magma

6:01

like a mineral hell,

6:03

very uninhabitable.

6:11

Amidst the turmoil of this ancient era,

6:14

a cosmic event occurred,

6:16

which ultimately transformed the Earth.

6:30

The Moon almost certainly

6:32

formed early in Earth's history,

6:35

when a

6:36

Mars-sized planet collided with Earth. The

6:42

material thrown out by the massive collision

6:46

then solidified to form the Moon

6:48

that now orbits us.

7:01

In the beginning,

7:02

the Moon was also a ball of fire like the Earth.

7:06

Shining like a second sun.

7:17

Its existence gradually influenced the development of the Earth,

7:22

until billions of years later,

7:24

creating conditions conducive

7:27

to life.

7:30

This is the

7:31

beginning of a big change.

7:35

As the Earth slowly cooled, its

7:37

elements began to form.

7:45

Gravity pulls heavier materials

7:48

such as iron and nickel toward the center

7:50

to form the Earth's core,

7:53

while lighter materials

7:55

form its mantle.

8:00

In this fragile balance,

8:03

magma solidifies on the surface

8:05

into a dense,

8:06

dark rock called basalt.

8:12

Basalt became the Earth's first crust.

8:19

On top of this crust,

8:20

another process

8:22

that was equally important

8:23

to the Earth's development began to take shape: the

8:26

water cycle.

8:35

As the atmosphere,

8:36

which is filled with a number of gases, begins to cool,

8:39

water vapor begins to condense

8:40

and falls as rain.

9:14

Over time,

9:16

rain formed puddles on the Earth's surface

9:20

and that was the beginning of the formation of the oceans.

9:36

So, in its first 100 million years or so,

9:39

Earth went from something alien

9:42

to something that

9:43

started to look like our home.

9:46

One major difference between early Earth

9:49

and present-day Earth

9:51

is the absence of life.

9:58

With the formation of the Earth's crust and oceans,

10:02

some of the familiar features of Earth

10:04

began to emerge.

10:10

However,

10:11

volcanoes still spew

10:13

lava flows and gas clouds,

10:15

filling the atmosphere

10:16

with carbon dioxide,

10:18

methane,

10:19

and ammonia.

10:25

At the beginning of the Archean Era,

10:28

the water in the oceans may have been green

10:31

due to its high iron content. It is

10:35

in this turmoil of fire,

10:37

water,

10:38

and gas that

10:39

an important chemical process begins.

10:45

The emergence of life on Earth

10:46

remains one of the greatest mysteries.

10:50

However, it is certain that

10:51

the process involves water and rocks.

11:04

There are several theories.

11:06

Life could have arisen on the seabed,

11:08

near hydrothermal vents

11:10

that release hot water

11:12

with a distinctive chemical environment.

11:14

Life could also arise

11:16

on land,

11:17

from small lakes

11:18

or hot springs,

11:20

as Darwin once suggested.

11:26

Life emerged due to the creation of conducive conditions

11:30

involving water,

11:31

temperature,

11:32

and minerals.

11:38

Once life begins,

11:41

it continues to strive to

11:42

maintain its continuity.

11:49

The formation of life

11:51

and how it maintains its continuity

11:55

are two different things.

11:59

Life may have begun many times on the ancient Earth,

12:04

but it did not last long

12:06

and eventually became extinct.

12:07

However,

12:08

at one point,

12:09

life arose.

12:14

Rising from failure over and over again,

12:18

but with enough elements to survive.

12:26

Until one time in the ancient ocean,

12:29

life forms began to develop,

12:33

diversify,

12:34

and slowly adapt.

12:40

They are simple microorganisms

12:43

that are invisible to the naked eye.

12:49

Some of them

12:50

began to harness the Sun's energy

12:53

by capturing light

12:55

and eventually producing oxygen, an

12:58

element that was previously almost insignificant.

13:11

There was a major change on the Earth's surface at that time

13:14

because the oxygen content in the atmosphere, which was initially non-existent,

13:18

increased slightly,

13:20

from 0% to 2%.

13:23

Currently we have 15%.

13:25

This moment is believed to be a

13:27

pivotal point in geological history

13:29

that allowed life to evolve

13:32

and become increasingly diverse

13:34

throughout the rest of Earth's history. The

13:51

Great Oxygenation Event was a

13:53

crucial time when Earth and life interacted in a way that

13:57

transformed both.

14:06

For more than a billion years,

14:09

oxygen produced by photosynthetic bacteria

14:13

was absorbed by the oceans

14:14

and bound in rocks.

14:20

When these natural reservoirs are full,

14:24

oxygen begins to accumulate in the atmosphere

14:27

and slowly changes its composition.

14:35

Over time, the

14:37

ozone layer formed,

14:38

protecting the planet from ultraviolet radiation

14:42

and allowing

14:44

more complex life to emerge,

14:46

including early forms of plankton

14:49

as we know them today.

14:59

To this day,

15:00

this microscopic world

15:03

still provides insights into

15:05

how increasing marine biodiversity is slowly

15:08

changing not only the atmosphere,

15:10

but also the rocks.

15:32

Marine life is the

15:34

focus of this marine biologist's research.

15:38

An ecosystem

15:39

that still plays an important role in

15:41

maintaining the balance of the Earth.

15:46

Amazingly,

15:48

in one liter of seawater,

15:49

there are 10 to 100 billion plankton organisms.

15:53

That far exceeds the human population on Earth.

15:56

Each liter of seawater

15:58

contains up to ten times the Earth's population.

16:11

Plankton,

16:12

ancient Greek for "wanderers",

16:15

live in water and are estimated to make up 98% of marine life.

16:28

However,

16:29

as a research subject,

16:31

plankton is rarely studied. It was

16:38

only in 2009 that the

16:40

Tara Oceans foundation

16:42

launched a four-year study

16:44

specifically to collect data

16:46

on plankton.

16:55

This is the fresh plankton

16:56

we just collected

16:58

with a large net.

16:59

In this invisible world,

17:01

there are many tiny organisms.

17:05

There are viruses,

17:06

which are already quite eccentric in shape,

17:08

like miniature spaceships,

17:11

there are bacteria,

17:11

which are starting to form filaments

17:13

that sometimes gather into colonies,

17:16

and there are more complex cells

17:18

like protists.

17:22

There are also layers of other small animals

17:24

such as jellyfish and the like.

17:26

All these organisms interact in one ecosystem.

17:30

That's what we need to learn today.

17:37

During the expedition,

17:39

researchers identified

17:41

more than 250,000 species of plankton,

17:44

some of which are

17:46

capable of photosynthesis.

17:53

By absorbing carbon dioxide in the ocean,

17:56

plankton help balance the atmosphere

17:59

and form many of the cliffs

18:01

we see today.

18:16

Phytoplankton includes a group called coccolithophores.

18:20

These tiny cells are able to produce tiny calcium discs

18:24

and attach them to the cell membrane.

18:27

This phenomenon is very special.

18:33

Each of these single-celled organisms

18:35

forms a calcium plate

18:37

that looks like a floating rock.

18:39

The function of these plates is very important

18:41

because when they die,

18:42

these organisms sink to the bottom of the sea.

18:48

Over time,

18:49

this process forms deposits that rise out of the water,

18:52

as seen in the English Channel

18:54

and elsewhere.

19:02

Remarkably,

19:03

this simple process changed Earth's history.

19:13

It is amazing

19:15

that many organisms are able to form minerals

19:18

that remain intact when they die.

19:25

Paleontologists

19:27

quickly realized

19:28

that many rocks were made

19:30

from the remains of life.

19:32

Many limestone rocks are formed

19:34

from skeletons that accumulate

19:36

to a thickness of several kilometers.

19:44

Only about 10 or 15% of

19:48

animals have mineralized skeletons,

19:52

but their impact

19:53

on Earth

19:55

and life on it is enormous. The

20:04

limestone here was formed between 180 million years ago.

20:09

This area was once a 300 meter deep sea,

20:12

filled with coccolithophores.

20:15

Their calcium skeletons accumulated over 20 million years.

20:19

So two centimeters every thousand years,

20:21

shaping this landscape.

20:24

This was once the seabed, which was then exposed

20:27

when the strait separating England

20:29

and France was formed.

20:39

Single-celled organisms

20:41

can form mountains.

20:42

It's a testament to how amazing life is

20:45

and how it impacts geology.

20:56

For a long time, the

20:58

ancient oceans were the

21:00

only habitat for bacteria,

21:02

single-celled algae,

21:04

and the first multicellular organisms.

21:07

The emergence of more complex life forms was just

21:10

beginning.

21:14

Conditions for the next phase of evolution

21:17

are formed in shallower,

21:20

light-filled water zones.

21:22

Life has not yet reached land.

21:26

Imagine a time

21:28

500 million years ago

21:29

when there were no plants on land.

21:50

There are only barren rocks.

21:53

It's like heaven for geologists.

21:55

The entire Earth is

21:56

still covered with raw rocks.

22:00

A fact that many people may not

22:02

know is

22:04

that for 90% of Earth's history, there was very

22:08

little land

22:10

covering the surface. It was

22:13

n't until the last 10% of Earth's history that

22:16

deep soil

22:17

developed.

22:19

However,

22:20

there is also much evidence that

22:22

there are diverse species of microbes

22:24

such as bacteria,

22:26

fungi,

22:27

algae,

22:28

and possibly lichens.

22:31

Lichens are the

22:32

result of symbiosis between algae and fungi.

22:36

They are unique

22:37

because they are mini ecosystems.

22:42

Before vascular plants appeared,

22:45

they covered

22:46

much of the Earth's surface.

22:54

Lichens are

22:55

little known

22:57

because their fossil traces are almost non-existent

22:59

due to their fine structure.

23:02

Researchers believe

23:04

they paved the way

23:06

for life on land.

23:10

These tiny organisms

23:11

trigger huge transformations.

23:15

By dissolving rock minerals,

23:18

they promote biological weathering

23:20

and then create soil.

23:27

This marked the beginning of a new phase

23:30

when living organisms

23:31

began to shape the Earth's surface.

23:37

Until now,

23:38

lichens continue to work

23:39

consistently.

23:41

An organism.

23:43

What fascinated this biologist

23:53

I worked as a geologist for 20 years

23:56

studying ancient rocks.

24:00

What caught my attention was the

24:01

lichen growing on it.

24:04

That's what prompted me to switch

24:06

from a geologist to a biologist.

24:13

This granite is mostly

24:15

made of silica,

24:16

visible from the small,

24:18

clear grains here.

24:22

Around it,

24:23

there are large pale white grains

24:25

and a few pink grains.

24:27

It is feldspar,

24:29

which has a high mineral content.

24:31

They contain potassium,

24:32

possibly calcium as well.

24:34

These nutrients are used by lichens

24:36

to help their growth.

24:41

Lichens also dissolve rocks,

24:43

crystals

24:44

and granules,

24:46

then reabsorb nutrients from them.

24:49

They opened this granite.

24:51

They physically weather rocks

24:54

and chemically dissolve them.

24:56

All of these colors are often associated with acids.

24:59

When these acids are released from lichens,

25:02

they can break down

25:04

and dissolve mineral grains.

25:07

Through this process,

25:09

they turn rocks into clay particles.

25:12

These particles can then be carried by wind or rain.

25:16

From there,

25:17

the particles begin to form soil,

25:20

paving the way for other ecosystems to develop.

25:40

Weathering is the most important process on the Earth's surface.

25:46

Lichens

25:47

can be likened to agents,

25:50

although they are small,

25:52

limited,

25:53

and grow very slowly.

26:00

Although it may be underestimated, I

26:03

think

26:05

the role of lichens is very important

26:06

in the history of life on Earth.

26:31

When I saw these rocks and lichens,

26:34

I was amazed that with their size and speed,

26:37

they could break such hard solid objects into particles.

26:44

It's amazing

26:45

that they were able to do that

26:47

so slowly.

26:49

On a scale of millimeters to microns

26:51

over hundreds to thousands of years.

26:55

Those are spatial scale

26:57

and temporal scale.

26:59

Something different

27:00

from everyday human life

27:02

.

27:12

By settling on rocks,

27:14

lichens prepare the ground

27:16

for the emergence of land plants.

27:20

However,

27:21

without the Moon and its gravitational force,

27:24

these plants

27:25

might never have emerged.

27:30

Most life arises from the waters of unstable coastal zones

27:35

and tidal areas. The

27:42

ebb and flow of the ocean

27:43

creates

27:45

alternating wet and dry environments.

27:47

This condition

27:47

requires significant biological adaptation

27:49

.

27:53

It can be assumed

27:55

that creatures living

27:56

in the tidal zone

27:58

must be accustomed to being wet and dry.

28:04

It may be an important factor

28:06

for survival. It was

28:19

in this tidal zone that the

28:22

first aquatic algae, the

28:23

ancestors of land plants,

28:25

began to settle on land.

28:34

To survive here,

28:36

they must be able to adapt

28:38

and protect themselves.

28:42

450 million years ago,

28:45

when land plants began to appear,

28:51

there was a population of algae

28:52

that produced a kind of

28:55

clear coating on their bodies

28:58

to keep them from drying out.

29:10

That was the first step

29:12

in the formation of the forests,

29:15

woodlands,

29:16

and grasslands

29:17

around us today.

29:31

These early primitive plants

29:34

created the conditions

29:35

for life on land.

29:37

They form a cuticle, a

29:39

clear layer

29:40

that helps them

29:42

retain moisture.

29:45

They also have rhizoids,

29:47

which allow them to

29:49

anchor themselves underground.

29:51

They were the

29:52

beginnings of rooted plants

29:54

that forever changed the biosphere

29:57

and the development of ecosystems on Earth.

30:03

It is amazing

30:04

because many plants

30:05

at that time were small in size.

30:08

All these plants

30:10

require nutrients from minerals

30:12

on the Earth's surface.

30:14

So they

30:15

need to interact with the surface

30:17

they grow on.

30:28

The roots penetrate into the soil,

30:31

forming increasingly complex structures.

30:35

They bring new minerals,

30:38

change the soil

30:39

and its movement.

30:42

So,

30:43

this was a very important moment

30:45

when the first land plants appeared

30:47

and began to form their own habitats.

30:56

The evolution of land plants

30:58

changed our planet.

31:02

They transform rocky landscapes

31:04

into green ecosystems.

31:11

Millions of years later,

31:13

animals followed the same evolutionary path.

31:17

From water to land.

31:25

Like plants,

31:27

animals also have to adapt to a completely different world.

31:32

Their bodies are

31:33

no longer supported by water,

31:35

their skin

31:36

dries out from the air,

31:37

and they have to adapt

31:39

to gravity.

31:42

What needs to be known is that

31:45

animal life thrives in the sea.

31:48

All the types of animals we see on land today

31:52

evolved from water.

32:00

To do so,

32:02

they needed to establish a new structure.

32:05

For example, vertebrates.

32:09

All vertebrates that have legs

32:11

like tetrapods that live on land,

32:14

their ancestors were fish.

32:19

Fish have gills,

32:20

not lungs.

32:22

So,

32:23

in order for vertebrates to live on land,

32:26

they had to develop lungs

32:28

and they succeeded.

32:38

Fins also function well in the sea,

32:42

but to walk

32:44

and support oneself on land, a

32:47

complete change in the

32:50

structure of the

32:51

body's skeleton and muscles is required.

32:53

That also happened successfully.

33:16

The interaction between minerals

33:19

and life is

33:20

most clearly seen

33:22

in the way skeletons are formed.

33:32

Minerals are essential

33:34

for life to

33:35

move onto land.

33:37

Without minerals, there

33:38

would be no skeleton

33:39

or shell.

33:53

In tetrapods,

33:54

these changes occur inside the body.

33:57

Their bones,

33:58

which are composed of calcium phosphate

34:00

and carbonate, become denser

34:03

to support their body weight outside the water.

34:13

On the other hand,

34:14

arthropods developed a kind of armor, an

34:17

organic exoskeleton

34:19

that protected them from dehydration and predators,

34:23

while also giving them a strong shell.

34:39

Without these skeletons and armor, the

34:42

first land animals

34:44

would not have been able to explore

34:46

and create new habitats

34:48

by digging

34:50

and breaking down the soil.

35:01

Burrowing animals

35:02

play an important role in

35:04

life activities on Earth.

35:05

They are often overlooked

35:07

because their activities occur underground.

35:13

Such as termites,

35:15

millipedes,

35:16

ants,

35:17

spiders,

35:18

and others.

35:23

Chemically,

35:24

many burrowing animals eat the soil

35:27

which then

35:29

changes the mineral composition.

35:34

Physically,

35:35

burrowing animals have a big impact on the soil

35:38

because they create many interconnected tunnels in the soil

35:41

.

35:43

This pathway allows the soil

35:45

to contain more oxygen

35:48

and water to move more effectively.

35:51

This encourages the creation of new systems in the soil.

35:55

As a result,

35:56

various types of organisms and species are

35:58

encouraged to thrive

36:00

in these new conditions.

36:11

Throughout the history of the Earth it

36:13

can be seen that after the arrival of arthropods on the surface,

36:17

quite a lot of changes occurred.

36:28

The Earth has long been shaped by powerful geological forces:

36:33

volcanism,

36:34

plate tectonics,

36:36

and continental drift.

36:40

However, the emergence of plants and animals,

36:43

now added a new force:

36:46

Life.

36:49

In the intertidal zone,

36:51

species such as sea urchins or sea urchins

36:54

still shape and alter rocks

36:57

and coral reefs to this day.

36:59

For more than 40 years, the

37:01

marine biologist

37:03

has studied the animal's relationship with rocks.

37:11

I see the interaction with the substrate.

37:13

I saw them eroding sandstone

37:16

which produces millions of tons of sediment

37:18

every year.

37:19

I see a long history,

37:21

ecologically and evolutionary.

37:29

Sea urchins have lived in the sea for 450 million years.

37:35

They have extraordinary abilities.

37:38

Slowly and consistently,

37:41

they use their teeth and spines

37:43

to erode the limestone,

37:45

changing the geological dynamics of the seabed.

37:56

When sea urchins settle, they are

37:57

very small in size. The

38:00

spines are small, the

38:01

tube feet are small,

38:02

and the body is small.

38:03

As they grow,

38:04

they develop a structure for feeding

38:07

called Aristotle's Lantern.

38:10

This organ has five teeth that are used

38:13

to scrape small stones when they eat.

38:18

So they scrape off the algae

38:20

with their teeth

38:21

and they swallow it.

38:28

Their spines also shift sand grains

38:31

as they touch the rock surface. This

38:36

combination of teeth scraping the surface

38:40

and spines raking the surface

38:43

continues to wear away at the rock.

38:50

When that happens,

38:51

they create a small hole.

38:53

This process is called bio-erosion.

39:03

In essence,

39:05

sea urchins have a very big role.

39:09

Through bio-erosion,

39:11

they are included in a geological cycle

39:13

that has been going on for thousands of years.

39:20

The sediments they produce are carried deep

39:23

into the ocean and returned to the surface,

39:26

piling up to form the seabed

39:28

and coastlines. This

39:35

slow,

39:37

but crucial, transformation process

39:38

contributed to the formation of continents.

39:43

What amazes me is that the

39:45

sea urchins, which can number in the thousands

39:49

in these niches,

39:50

act like sculptors.

39:52

They are the ones who do bio-erosion.

39:55

And over the years, the

39:57

sheer number of

39:59

bio-erosion-induced coastal sculpting they have created is

40:02

truly remarkable.

40:17

Animals are very active on the Earth's surface.

40:22

They play a role in the formation

40:24

and erosion of rocks in strange,

40:28

but fascinating ways.

40:33

Erosion by animals can be divided into two,

40:37

namely physical erosion and chemical erosion.

40:43

Rockhopper penguins for example.

40:46

They can cause physical erosion

40:48

to the rock surfaces where they nest.

40:56

They can also undergo chemical erosion

40:59

through urine and other forms of interaction

41:01

with surfaces.

41:09

So, animals are really creative

41:12

and destructive towards rocks.

41:21

If there were no sea urchins,

41:23

these rocks would have no shape.

41:27

They are the ones who make those curves,

41:30

gaps,

41:31

and cracks.

41:34

They are such

41:36

fundamental organisms to this system

41:39

that the absence of sea urchins is simply

41:41

unimaginable to me.

41:55

However,

41:56

sea urchins are only a small part of a larger cycle.

42:01

All over the planet,

42:02

there are various invisible forces

42:05

that help turn rocks to dust.

42:10

Not only living things,

42:13

but also wind and water.

42:17

All of this contributes

42:19

to the slow process of erosion,

42:21

which shapes the landscape

42:23

and nourishes the oceans.

42:25

The earth uses everything.

42:28

Rocks that are detached from cliffs,

42:30

destroyed by tides or organisms,

42:33

will become rocks again.

42:36

It is an eternal cycle

42:38

where every grain of sand

42:39

holds the history of the Earth.

42:43

Humans assume the Earth's surface has always been like this

42:46

because we have only seen it during our lifetime. The

42:49

Alps, for example,

42:51

will remain as they are.

42:52

However,

42:53

geologically,

42:54

tens of millions of years ago,

42:56

there was an ocean here.

42:58

Currently there are mountains four thousand meters high

43:01

and in tens of millions of years there will be

43:04

new hills or even plains.

43:05

In other parts of the Earth,

43:07

new mountains or new oceans

43:09

will also appear.

43:16

It is difficult to understand

43:18

that there is a much larger

43:20

and longer cycle that occurred before our lives.

43:23

All these processes

43:24

will continue

43:25

after we are gone.

43:31

Every mineral grain eroded from a mountain

43:35

holds a story of how mountains were formed,

43:38

eroded,

43:39

and buried deep within the Earth,

43:41

only to be replaced by new mountains.

43:44

That is the story of Earth.

43:49

Imagine rock being exposed,

43:51

and then rain,

43:52

wind,

43:53

and ice releasing tiny fragments.

44:07

The mineral grains were washed away by the river to the bottom of the sea.

44:16

The grains then become a thick layer of sediment.

44:24

The pressure there is quite high.

44:26

When buried deeper and piled up with other sediments,

44:31

the pressure and temperature are high enough

44:32

to change the sediment

44:34

into new rock.

44:41

The rock will probably remain on the seabed

44:44

for tens of millions of years.

44:54

Until finally,

44:56

mountains are formed from crushed rocks.

44:59

The sediment rises again,

45:00

lifted by tectonic forces,

45:03

and becomes part of a new mountain.

45:09

They will erode,

45:10

weather,

45:11

enter rivers,

45:13

and start the cycle again over and over again

45:15

for hundreds of millions of years. The

45:27

rock cycle

45:29

has shaped the Earth

45:30

for billions of years.

45:33

Driven by three main factors:

45:35

Water,

45:36

life,

45:37

and plate tectonics, the interactions of which,

45:39

as far as we know,

45:41

only exist on Earth. It

45:47

all started with magma,

45:50

which formed rock,

45:51

which then became the foundation of the Earth.

45:58

Wind and weather cause rocks to erode,

46:02

dissolve,

46:02

break down into small particles,

46:05

and change shape.

46:11

This is the beginning of a long cycle.

46:14

Rivers carry these particles to the ocean,

46:17

where they settle layer by layer.

46:25

Over time,

46:26

these rocks

46:28

solidified into sandstone,

46:30

limestone,

46:31

and other sedimentary rocks

46:33

that formed cliffs,

46:34

plateaus,

46:35

and seabeds.

46:39

Under the pressure of the Earth's crust,

46:41

these rocks change.

46:45

Limestone turns into marble

46:47

and clay into slate.

46:52

Sometimes the changes are more spectacular.

46:57

In the slow movement of tectonic plates,

47:00

sedimentary rocks are also carried deeper

47:04

until they melt and turn back

47:06

into magma.

47:08

This magma fills the volcano

47:10

and starts this eternal cycle all over again

47:12

.

47:17

However,

47:18

this cycle would not be possible

47:20

without water.

47:22

Water seeps deep beneath the Earth's surface,

47:25

hydrating the oceanic crust

47:27

and aiding the sinking of plates into the Earth's mantle.

47:34

This process

47:35

creates mountains and continents,

47:37

while also supplying nutrients

47:39

to the land and oceans.

47:45

This is essential

47:46

for life on Earth.

47:50

This process has existed since the beginning of Earth's history.

47:54

Without the rock cycle,

47:55

Earth would be a different place

47:57

and life would cease to evolve.

48:01

This is what happens on Mars. There

48:04

may have been life there,

48:06

but it could not have survived

48:09

because there was no dynamic rock cycle. The

48:22

rock cycle and the cycle of life are

48:25

interrelated.

48:29

Both have influenced each other

48:31

for billions of years.

48:35

This is an ongoing process that we are not aware of

48:39

and continues to this day.

48:42

Seen from a dust storm in the Namib Desert

48:44

in Namibia.

48:49

There is an amazing process here. This

48:53

process has been observed

48:55

by sedimentologists

48:57

for many years.

49:00

These dust plumes indicate that the

49:03

Earth is alive and functioning well.

49:05

There are geological processes taking place. The

49:12

Namib Desert

49:13

acts as the setting and main character

49:16

of a phenomenon

49:18

that originally originated in the mountains.

49:33

There,

49:34

rain and wind slowly erode the rocks

49:36

into fine dust.

49:40

The dust is then carried by rivers,

49:43

which only appear during the rainy season

49:46

and then dry up again,

49:47

into the desert sand dunes.

49:56

Seasonal rivers

49:57

only flow during the rainy season after heavy storms. The

50:04

river flowed very fast,

50:05

bringing sand and mud with it.

50:10

The mud eventually reaches the dune area

50:12

where the river can no longer flow as fast.

50:19

The river has difficulty flowing fast in this area

50:22

so the mud stops and settles into clay deposits.

50:41

Once the water is gone,

50:42

the wind comes into play.

50:47

The wind pushes the particles

50:50

and carries them across the desert.

50:53

Some of them

50:54

cover very long distances.

50:59

These minerals are flat

51:01

so that when carried by the wind,

51:03

they can be carried for hundreds of kilometers.

51:21

Wind is very important in helping

51:23

clay particles move far out

51:25

to sea,

51:26

where they settle. It

51:32

contains minerals such as iron,

51:35

nitrogen

51:35

and phosphorus.

51:37

So, these clay particles are important

51:39

because they carry energy and nutrients to the ocean.

51:51

If it weren't for the rock cycle,

51:53

Earth would stagnate and die.

52:01

This cycle continuously brings nutrients to the Earth's surface

52:04

and provides new energy reserves

52:07

for life to survive.

52:12

So, the

52:13

rock cycle is an important part

52:16

of Earth and human history.

52:26

Dust storms that carry nutrients to the oceans are important

52:30

because the oceans are iron deficient.

52:35

This iron is

52:36

carried from the continents

52:39

to stimulate microorganisms in the oceans,

52:42

especially plankton and algae such as diatoms.

52:48

They are the basis of the food chain

52:50

around us today.

53:12

Minerals are the source of life.

53:16

Gradually, the

53:17

first organisms

53:19

began to change their environment.

53:27

The emergence of hominins in Africa around seven million years ago

53:31

marked a significant moment.

53:36

Our ancestors

53:37

were tree dwellers

53:39

who ate leaves

53:40

and fruit.

53:42

At one time,

53:44

they left the trees and lived on the ground.

53:50

The move marked the beginning

53:52

of a unique relationship

53:54

with the rock.

54:03

For most of human history,

54:06

we were creatures that walked

54:08

on all fours.

54:10

This is related to our ancestors

54:13

who used to live in trees.

54:20

Occasionally,

54:21

we would stand on our hind legs

54:24

to spot predators further out on the savannah.

54:31

Then, return to stepping on all four feet.

54:34

Over time,

54:36

we become more adept at balancing ourselves

54:39

and begin to learn to walk

54:42

on two legs.

55:00

This allows our hands

55:03

to move more freely,

55:05

both to pick up,

55:07

hold,

55:08

and play

55:09

with the mineral structure

55:11

so that we can make various tools.

55:23

Imagine that first primate

55:25

taking a stone in his hand

55:28

and realizing that

55:29

he could use it.

55:35

Maybe not consciously,

55:38

but it becomes an instinctive action,

55:40

something the hands can do.

55:43

There are tools that can be used to survive.

55:54

In my opinion,

55:56

discovery is an important part

55:57

of primate and human evolution.

56:03

You learn to do something

56:05

that allows you

56:07

to live life more efficiently, be

56:09

safer

56:10

or be able to hunt prey.

56:14

All the benefits of using this stone

56:17

are an advantage. I

56:23

think

56:24

that's how the coevolution between primates and rocks happened.

56:37

From walking upright,

56:40

using tools to discovering fire,

56:43

minerals have always been the foundation of

56:45

human development.

56:48

For millions of years,

56:50

our ancestors explored the world,

56:52

observing

56:53

and conducting various experiments.

57:00

Initially,

57:01

they used unprocessed stones.

57:03

After that,

57:05

they selected certain stones

57:07

and processed them into simple tools.

57:11

Slowly,

57:12

these tools became more and more sophisticated.

57:15

This is the beginning of the Stone Age.

57:20

Another important step was the use of fire,

57:23

which began about 1.5 million years ago.

57:42

These skills changed the

57:44

relationship between early humans and the Earth,

57:46

as new strategies developed

57:49

to maintain their existence.

57:55

The use of fire by humans is

57:57

closely related to stones

57:59

because one way to light it is

58:01

by rubbing two stones together.

58:15

This

58:16

shows the relationship and importance of rocks

58:19

and minerals for humans.

58:25

Flint and pyrite are commonly used to

58:28

produce sparks,

58:30

which fall, for example, on soft mushrooms,

58:32

and then catch fire.

58:33

Once blown out,

58:34

the fire can be easily fanned

58:36

using fine grass.

58:53

The development of the use of fire

58:55

brought enormous changes

58:57

to human history.

59:03

The use of fire

59:04

allowed us to cook

59:07

and paved the way for us

59:10

to consume calories more efficiently.

59:16

Some anthropologists argue that

59:18

brain size also increased.

59:23

In other words,

59:25

the ability to think and reason

59:28

and perhaps the ability to speak

59:31

may emerge from this process.

59:35

So, it can be said that the use of fire

59:39

not only brought benefits such as

59:41

providing security through lighting,

59:44

but also the foundation for the development of

59:47

more complex civilizations,

59:49

including communication and organization.

1:00:12

The warmth and light of the fire

1:00:14

transformed the cave into a place where humans took shelter,

1:00:17

gathered,

1:00:18

and shared stories.

1:00:28

Under the glow of firelight, the

1:00:31

same movements are repeated,

1:00:33

tools are refined,

1:00:35

and knowledge is passed down.

1:00:37

Closer cultural ties are also developing.

1:00:45

Much later, the

1:00:47

same rock walls

1:00:49

were used as canvas

1:00:51

for the first cave paintings.

1:00:54

This is a witness to the beginning of human art.

1:01:00

Through simple figures

1:01:02

and animal forms,

1:01:04

humans tried to describe the world

1:01:07

and immortalize memories

1:01:08

for the first time.

1:01:15

When I look at the pictures on this wall,

1:01:18

it feels like looking at a book left behind by our ancestors.

1:01:31

Various ethnic groups

1:01:32

have lived in southern Africa

1:01:35

for more than 40,000 years.

1:01:37

As traditional hunters and gatherers,

1:01:40

they have a unique understanding of nature.

1:01:45

This is thanks to their ancestors

1:01:47

who immortalized knowledge in the rocks.

1:01:57

This stone tells how my ancestors lived.

1:02:03

What animals they hunted

1:02:05

and how they used them.

1:02:10

They ate their meat,

1:02:13

warmed themselves with their skin and fur,

1:02:17

and made tools from their bones.

1:02:27

Large animals signify potential danger.

1:02:33

Jumping antelopes and bulls

1:02:34

indicate there is food in the area.

1:02:37

This stone tells it all.

1:02:40

They seem to leave messages and instructions

1:02:43

for future generations.

1:02:52

My ancestors couldn't write,

1:02:54

but they could paint on rocks.

1:03:00

That's how I understand my origins.

1:03:18

The stones are like alive.

1:03:21

They witnessed all the changes

1:03:23

that

1:03:26

human culture and history underwent.

1:03:41

Since the first cave paintings,

1:03:43

stone has been a medium for conveying thoughts,

1:03:47

memories,

1:03:48

and traditions.

1:03:50

People immortalized beliefs,

1:03:53

stories

1:03:54

and ways of seeing the world in stone.

1:04:04

Thousands of years later,

1:04:07

Neolithic peoples continued their

1:04:09

special relationship with stone.

1:04:11

The evidence is not only visible on the cave walls.

1:04:15

They also made the landscape a sacred site.

1:04:27

In Carnac, France,

1:04:29

for example.

1:04:30

Large stones were erected

1:04:32

and arranged in rows. It was as if

1:04:40

humans at that time

1:04:42

wanted to tell something through stone.

1:04:49

To this day,

1:04:51

researchers are still trying to solve the

1:04:53

mystery of these stones.

1:05:03

One of them is this archaeologist.

1:05:08

I sometimes just sit looking at the stones

1:05:12

and try to understand them.

1:05:14

I was attracted to them

1:05:16

and felt comfortable.

1:05:32

At Carnac,

1:05:33

more than 3,000 menhirs line

1:05:35

several kilometers,

1:05:38

forming one of the largest megalithic sites

1:05:40

in the world.

1:05:48

People in the Neolithic period probably

1:05:50

chose these stones

1:05:52

because of their durability.

1:05:54

They wanted to leave something lasting

1:05:58

and have a special purpose.

1:06:06

As one walks among these monoliths,

1:06:09

the question arises:

1:06:11

Are these markers of territory,

1:06:13

power,

1:06:14

eternity,

1:06:15

or permanence?

1:06:18

Unfortunately, there is

1:06:19

no inscription to answer that.

1:06:24

Only a few carvings,

1:06:26

pictures

1:06:27

and symbols are indecipherable.

1:06:33

That's probably the hardest part.

1:06:35

Identifying how much symbolism is

1:06:38

hidden here.

1:06:45

Humans have an almost sacred relationship

1:06:48

with the mineral world.

1:06:52

Maybe because our life is so short.

1:06:57

We think in terms of days,

1:07:00

weeks,

1:07:00

months,

1:07:01

and years.

1:07:04

However, rocks and minerals

1:07:06

can last for millions of years.

1:07:11

So,

1:07:12

when humans build sacred monuments,

1:07:15

they become symbols of eternity

1:07:17

because the lifespan of rocks and minerals is

1:07:20

much longer than is known. Their

1:07:28

beauty and durability

1:07:30

make the stones sacred.

1:07:33

Ancient beliefs say that

1:07:35

stones protect us from disaster

1:07:38

or connect us with a

1:07:40

higher power.

1:08:11

During the Neolithic Revolution,

1:08:13

humans demonstrated their dominance over the world.

1:08:19

Hunters and gatherers

1:08:20

settled as farmers

1:08:22

changing the landscape.

1:08:25

Meadows and fields were formed,

1:08:29

villages were built,

1:08:31

and roads were constructed.

1:08:41

The development of metallurgy

1:08:43

around 5,000 BC

1:08:45

changed everything.

1:08:49

Humans were no longer satisfied with stones

1:08:51

so they began mining mineral ores

1:08:54

and extracting raw materials

1:08:56

such as copper,

1:08:57

bronze,

1:08:58

and iron.

1:08:59

This activity revolutionized society.

1:09:04

In the late 18th century,

1:09:07

this trend accelerated: the

1:09:09

Industrial Revolution.

1:09:14

Mined minerals are not only processed,

1:09:17

but their energy is also extracted.

1:09:22

Coal,

1:09:23

followed by oil afterward,

1:09:25

became the foundation of this revolution

1:09:27

that pushed society

1:09:28

into an era of uncontrolled consumption.

1:09:38

Over the centuries,

1:09:40

humanity's relationship with rocks changed drastically.

1:09:44

From what was initially only used as a tool, it is

1:09:47

now extracted from the bowels of the Earth.

1:09:52

Humans evolved into an extractive society

1:09:55

in which Earth's resources were

1:09:57

exploited at an alarming rate

1:10:00

to satisfy material and energy needs.

1:10:08

Extractivism

1:10:10

means mining,

1:10:12

taking

1:10:13

and extracting limited natural resources

1:10:15

.

1:10:26

This happens because the practice

1:10:29

has become the foundation of society. The

1:10:34

luxuries we enjoy,

1:10:37

mobility,

1:10:38

electric lights,

1:10:39

cars,

1:10:41

and plumbing.

1:10:43

All of them originate from extractive societies

1:10:46

and this has various consequences

1:10:49

for the morphology of the planet.

1:10:55

Humans are altering the planet's carbon cycle

1:10:58

with impacts that will be felt

1:11:00

for thousands of years.

1:11:07

Don't think that

1:11:08

the process of taking and burning plant fossils

1:11:11

that have been stored underground

1:11:13

for hundreds of millions of years

1:11:15

has no impact.

1:11:33

The impacts are global warming,

1:11:35

storms and tornadoes.

1:11:37

Droughts may also occur in some areas,

1:11:39

and floods in others.

1:11:45

When the environment changes, the

1:11:47

Earth's reaction also changes.

1:11:49

This will continue to get worse

1:11:51

unless we change the way we treat the Earth.

1:12:01

Humans have become a force in their own right,

1:12:04

shaping a new geological epoch:

1:12:06

the Anthropocene.

1:12:09

For the first time in Earth's history,

1:12:13

humans are interfering with natural cycles,

1:12:15

changing climate,

1:12:17

erosion,

1:12:18

ocean chemistry, and

1:12:19

even rock structure.

1:12:26

We are not only consuming natural resources

1:12:29

at an incredible rate,

1:12:31

but we are also producing new materials

1:12:33

that are buried in geological layers.

1:12:39

Concrete is one of them.

1:12:42

Made from heated lime,

1:12:43

clay

1:12:44

and sand.

1:12:48

Concrete has become the artificial building material of our civilization

1:12:51

that covers the entire world.

1:12:58

Concrete is more efficient,

1:13:00

smoother,

1:13:01

and has less resistance

1:13:04

for humans to walk on,

1:13:06

compared to dirt,

1:13:08

large rocks,

1:13:09

and grass. The

1:13:14

Earth's natural surface

1:13:15

seems to ask us

1:13:17

to continue adapting

1:13:19

to the surrounding conditions.

1:13:26

However,

1:13:26

we lost that

1:13:29

when we covered the Earth with smooth concrete.

1:13:35

In the last 70 years,

1:13:37

humans have produced more than half a trillion tons of concrete.

1:13:42

The equivalent of one kilogram of concrete

1:13:44

for every square meter of the Earth's surface. The

1:13:47

main ingredients of concrete,

1:13:49

sand and gravel,

1:13:51

are made from highly durable minerals.

1:13:54

Minerals that can last

1:13:56

for billions of years.

1:14:00

If humans disappeared,

1:14:04

cities,

1:14:05

highways,

1:14:07

even jet traffic would cease to exist, what would

1:14:12

remain would be a

1:14:14

very unique mineralogical legacy.

1:14:25

In this new geological layer, the

1:14:28

soil layers will completely change.

1:14:31

Concrete will be seen covering the surface of the Earth.

1:14:36

Encrusted with steel,

1:14:37

glass,

1:14:38

ceramics,

1:14:39

and semiconductors.

1:14:45

However, the

1:14:45

most distinctive geological trace of our era

1:14:48

is plastic.

1:14:54

From discarded goods

1:14:56

to invisible nanoplastics,

1:14:59

plastic waste

1:15:00

is everywhere.

1:15:11

These tiny plastic particles

1:15:14

have polluted the soil,

1:15:16

oceans, and

1:15:18

even rainwater.

1:15:23

In some places,

1:15:24

these particles

1:15:25

even blend with natural sediments

1:15:28

due to the hot temperatures.

1:15:30

This new structure is called a

1:15:31

plastiglomerate.

1:15:44

This phenomenon is the

1:15:46

focus of research by

1:15:47

the founder of the

1:15:49

MARE-Madeira research institute.

1:15:57

I think the

1:15:58

plastic crust around the world

1:16:02

is giving us a warning

1:16:04

that we all need to be vigilant.

1:16:16

This global phenomenon

1:16:17

shows how big our footprint on Earth is.

1:16:21

Plastiglomerate was

1:16:22

first discovered in Madeira, Portugal

1:16:25

in 2016

1:16:27

and can now be found in many places:

1:16:30

the Mediterranean,

1:16:31

Peru,

1:16:32

Brazil

1:16:33

and even Japan.

1:16:35

Water currents,

1:16:36

storms,

1:16:37

and waves carry plastic particles

1:16:39

to beaches around the world,

1:16:41

where they become

1:16:43

entangled with rocks. The

1:16:49

first factor is

1:16:51

the waves throwing the plastic

1:16:53

towards the rocks.

1:16:57

Second, we

1:16:58

think it's because the rocks have a specific texture,

1:17:05

and third,

1:17:07

because the temperature of the rocks is very hot.

1:17:11

This can be seen through the melted plastic crust that

1:17:15

sticks to the rock texture. It is

1:17:18

now known that the surface temperature of these rocks

1:17:22

sometimes reaches over 60°C in summer.

1:17:26

We believe that a

1:17:27

combination of three things is the cause: the

1:17:30

mechanical action of the waves,

1:17:32

the temperature,

1:17:33

and the texture of the rocks.

1:17:45

Microplastics are

1:17:46

everywhere.

1:17:50

Whether it's plastic bags

1:17:52

or children's toys, they

1:17:54

all break down

1:17:56

and enter the ecosystem due to ocean waves. The

1:18:02

microplastics are

1:18:03

then eaten by sea creatures.

1:18:07

Often when humans

1:18:09

eat these sea creatures,

1:18:10

microplastics end up in our bodies.

1:18:13

This can be interpreted as

1:18:15

resistance from the mineral world.

1:18:18

Many plastics are carcinogenic,

1:18:21

have chemical effects,

1:18:23

and can disrupt the endocrine system,

1:18:26

altering hormone levels.

1:18:30

Humans have not yet understood all of this well.

1:18:34

So,

1:18:34

it's kind of a big experiment

1:18:36

that we're doing on ourselves,

1:18:39

where we're the guinea pigs

1:18:42

and we don't know what the consequences are.

1:18:57

Plastiglomerate

1:18:58

reflects how aggressive the

1:19:02

profit-oriented petrochemical industry is in the rock cycle.

1:19:05

Leaving traces

1:19:06

down to the deep layers of the Earth's crust.

1:19:10

Rocks that were once formed from cooled lava

1:19:13

or deposited sediment are

1:19:15

now formed by human waste.

1:19:20

We used to believe that

1:19:21

plastic and concrete represented human progress.

1:19:26

In fact,

1:19:27

we leave a questionable trail.

1:19:34

Some might argue that

1:19:36

societies with modern technology

1:19:39

are evidence of progress

1:19:41

from previous societies

1:19:43

that used stone tools.

1:19:48

Actually,

1:19:49

we are not that different.

1:19:52

We still depend on rocks and minerals.

1:19:55

Our technology remains dependent on geology.

1:20:02

In this room alone,

1:20:04

I am surrounded by various minerals that would have been impossible to gather

1:20:09

in one room 100 years ago.

1:20:15

There is lithium in the camera battery.

1:20:18

There is copper on the wall.

1:20:21

Aluminum on this chair. There

1:20:24

may be rare earth metals in computers and cameras.

1:20:30

They come from all over the world,

1:20:33

many of them

1:20:35

from remote mines.

1:21:00

This is a remarkable technological innovation,

1:21:04

but it also demonstrates our

1:21:07

increasing dependence on the material world.

1:21:36

Science shows

1:21:39

that ancient humans had

1:21:41

more respect for the mineral world.

1:21:49

They view minerals in a more animistic way.

1:21:54

They see and recognize

1:21:56

how minerals have life

1:21:59

and play an important role in life on Earth. I

1:22:03

think

1:22:04

we need to go back to that perspective.

1:22:11

Earth has its own history.

1:22:14

Long before our era, the

1:22:16

Earth experienced heat and cold.

1:22:20

Earth also witnessed the formation of oceans and continents.

1:22:25

Over billions of years,

1:22:27

geological forces have shaped the face of the Earth.

1:22:30

Every rock,

1:22:31

mountain,

1:22:32

and valley is the result of a very slow process of change,

1:22:37

which is clearly engraved in the rocks.

1:22:46

However, in

1:22:47

just a moment in history,

1:22:50

everything changed.

1:22:59

A new development is

1:23:01

disrupting the order that has evolved

1:23:04

over billions of years

1:23:06

and shaking Earth's geological balance

1:23:09

at an unprecedented rate.

1:23:13

In just a few centuries,

1:23:16

humanity has exploited its

1:23:18

ancestral heritage from the land.

1:23:21

Now,

1:23:22

in a short time,

1:23:23

we are burning what has been petrified on Earth

1:23:26

for millions of years.

1:23:32

We cover the planet with plastic,

1:23:34

concrete,

1:23:35

and metal.

1:23:37

Creating geological layers

1:23:39

that mark our era as an anomaly

1:23:41

in Earth's history.

1:23:46

If the Anthropocene is called the era of humanity,

1:23:50

then it can also be called the era of consciousness.

1:23:56

Since Homo habilis made tools from stone,

1:24:00

mankind has been inseparable from rocks

1:24:03

to support its life

1:24:05

and make it the foundation of civilization.

1:24:09

Indeed, many members of society

1:24:11

now live in a world of abundance.

1:24:14

Making it difficult for them to imagine scarcity

1:24:17

and only focus on exploiting it.

1:24:22

However,

1:24:23

there is Earth that is telling of its suffering.

1:24:26

We just need to listen.

1:24:30

For those who have been listening to Earth know full well

1:24:34

that our time is running out.

1:24:39

The earth whispers to us.

1:24:42

However,

1:24:43

sometimes we have difficulty hearing it.

1:24:50

It's not about how loud the Earth whispers,

1:24:53

but how quietly. It

1:24:59

took the Earth millions of years

1:25:02

to speak to us.

1:25:06

Therefore,

1:25:07

we must slow down our steps.

1:25:10

We must listen carefully.

1:25:12

The stories that the Earth tries to tell

1:25:15

us through rocks.

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