Colliding Continents | Naked Science

Andrei Samoylov
13 May 202050:12

Summary

TLDRThis script explores Earth's geological future, predicting dramatic changes due to continental drift. It envisions a time when familiar continents merge into a supercontinent, causing extreme climate shifts and potential mass extinctions. The script delves into Earth's history, from its violent birth to the formation and destruction of supercontinents like Pangaea, driven by plate tectonics. It highlights natural disasters as a consequence of these movements and speculates on the future geological and climatic conditions that might challenge human survival.

Takeaways

  • ๐ŸŒ The Earth's continents are in a constant state of motion and transformation due to tectonic forces, which will continue to shape the planet's surface for billions of years.
  • ๐ŸŒŒ Intergalactic explorers in the distant future may find a vastly different Earth, possibly a single landmass with extreme climates and geological features, due to the ongoing process of continental collision and separation.
  • ๐Ÿž๏ธ Continents are formed and destroyed in cycles, with the current configuration of continents being just a snapshot in a long geological timeline.
  • ๐Ÿ”ฅ The Earth was initially a molten mass, and over time, the cooling and solidification of its surface led to the formation of the first landmasses, including granite as a key component.
  • ๐ŸŒŠ Water, possibly delivered by meteors and asteroids, played a crucial role in the formation of Earth's oceans, which are essential for the development of life and climate.
  • ๐ŸŒ‹ The theory of continental drift, proposed by Alfred Wegener, has been confirmed by evidence such as matching fossils on different continents, indicating that they were once joined.
  • ๐ŸŒˆ Plate tectonics is driven by heat from the Earth's core, causing the movement of continents and the creation of geological features like mountains and ocean trenches.
  • ๐Ÿž๏ธ The formation of continents and their geological features, such as the Grand Canyon and the Alps, are the result of continental collisions and the immense forces involved.
  • ๐ŸŒ The current configuration of continents has a significant impact on global climate and ecosystems, and changes in this configuration will affect the habitability of the planet.
  • ๐ŸŒช๏ธ Natural disasters such as earthquakes, volcanic eruptions, and tsunamis are part of the Earth's natural cycle and are a consequence of the movement of tectonic plates.
  • ๐Ÿ”ฎ Predicting the exact timing of geological events is impossible, but the locations of future volcanic activity and earthquakes can be anticipated based on plate boundaries and historical patterns.

Q & A

  • What is the premise of the video script discussing Earth's future?

    -The video script discusses a future vision of Earth hundreds of millions of years from now, where intergalactic explorers return to find a drastically changed planet with a single giant landmass, massive geological features, and remnants of ancient civilizations.

  • How does the script describe the current continents of Earth?

    -The script describes the current continents as distinct land masses separated by oceans, providing a stable environment with hospitable weather patterns suitable for civilization and city development.

  • What is the role of colliding continents in shaping Earth's geological features?

    -Colliding continents are described as the mightiest force on Earth, responsible for the creation and destruction of geological features, including the formation of mountains, the disappearance of oceans, and the reshaping of landmasses in a cycle of death and rebirth.

  • How did the first land on Earth form?

    -The first land on Earth formed as the heaviest elements like lead and nickel sank toward the center to form a molten core, while lighter elements including oxygen and silicon rose to the surface, erupting in volcanoes and slowly cooling to form patches of crust.

  • What is the significance of granite in the formation of the first continents?

    -Granite is significant because it is less dense than other rocks in the mantle, allowing it to float on the surface and mix with other rocks to form the first continental nuclei, which are the seeds of the first continents.

  • How does the script explain the movement of continents?

    -The script explains that continents are not fixed in place but are constantly moving due to powerful forces deep within the planet, which rip continents apart and then smash them together in an ever-changing cycle.

  • What evidence supports the theory of continental drift?

    -Evidence for continental drift includes the discovery of identical fossils on different continents, which suggests that these continents were once closer together, and the observation of continents moving apart at the mid-Atlantic ridge.

  • How does the script describe the formation of the Atlantic Ocean?

    -The script describes the formation of the Atlantic Ocean as a result of the collision and subsequent separation of the African and South American plates, which created a vast interconnected volcanic mountain range that extends through all the major oceans of the world.

  • What is the role of plate tectonics in the creation of natural disasters?

    -Plate tectonics play a significant role in the creation of natural disasters such as volcanic eruptions, earthquakes, and tsunamis, as the movement and interaction of tectonic plates create stress points and instability at plate boundaries.

  • What does the script suggest about the future of Earth's continents?

    -The script suggests that the continents will continue to move and change, potentially forming a new supercontinent called Pangaea Ultima, which could lead to extreme climate conditions and possibly trigger another mass extinction.

  • How does the script relate the geological history of Earth to the potential future of our planet?

    -The script relates the geological history of Earth by highlighting the continuous cycle of continental movement and change, suggesting that the processes that have shaped Earth over billions of years will continue to do so in the future, potentially leading to the destruction and rebirth of continents and affecting the survival of life on Earth.

Outlines

00:00

๐ŸŒ Future Earth's Drastic Transformation

This paragraph envisions Earth in the distant future, where intergalactic explorers return to find a planet drastically altered from its current state. Continents have merged into a single landmass with immense mountain ranges and glaciers. The once-thriving metropolises are now mere remnants buried under tons of rock. The script introduces the concept of Earth's ever-changing landscape due to the power of colliding continents, which have been shaping and reshaping the planet in a cycle of creation and destruction for billions of years.

05:00

๐Ÿ” The Birth and Evolution of Continents

The script delves into the geological history of Earth, starting from its formation 4.5 billion years ago. It describes the initial creation of the planet from debris, the formation of the Moon, and the intense heat that characterized the early Earth. The process of land formation is detailed, with heavy elements sinking to form the core and lighter elements like oxygen and silicon rising to create the first patches of crust. The challenges faced by the early crust due to asteroid bombardments are highlighted, and the eventual stabilization leading to the formation of the first continents is discussed.

10:02

๐Ÿ“… Geological Time and the Formation of Granite

This paragraph focuses on the role of granite in the formation of the first continents. It discusses the importance of zircon crystals in dating rocks and the process of how these crystals form a natural clock to measure geological time. The granite in South Africa's cup Val region is presented as an ancient remnant of the first continental nuclei. The paragraph also explores the theory that life, specifically photosynthetic organisms, may have contributed to the formation of granite and the growth of the continents.

15:03

๐ŸŒ The Dynamics of Continental Drift

The concept of continental drift is introduced, with the explanation of tectonic plates and their movement powered by heat from the Earth's core. The paragraph discusses the evidence for continental drift, such as identical fossils found on different continents, and the process of plate tectonics that leads to the creation of new land and the destruction of existing land masses. The formation of the Atlantic Ocean and the mid-Atlantic ridge is highlighted as an example of continents being pushed apart.

20:04

๐ŸŒ‹ The Creation and Destruction of Supercontinents

The script discusses the cyclical nature of continental movement, leading to the formation and breakup of supercontinents. It describes the process of how continents drift apart and then collide again to form new landmasses. The history of the supercontinent Val Barra and its eventual destruction by the heat buildup beneath it is detailed. The paragraph also touches on the formation of the next known supercontinent, Rodinia, and the continuous cycle of continental dispersion and collision.

25:06

๐Ÿ›‘ Mass Extinctions and the Formation of Pangaea

This paragraph discusses the formation of the supercontinent Pangaea and its impact on Earth's climate and life. It describes how the formation of Pangaea led to drastic climate changes and may have contributed to one of the largest mass extinctions in Earth's history. The script also details the breakup of Pangaea and the gradual formation of the continents we recognize today, including the separation of South America from Africa and the movement of other landmasses.

30:06

๐Ÿž๏ธ The Geological Features Formed by Colliding Continents

The script explores the geological features created by continental collisions, such as the formation of the Alps and the Himalayas. It explains the process of mountain building as a result of the collision between the African and Eurasian plates, and the formation of the Grand Canyon due to the uplift of the seabed following a plate collision. The paragraph also discusses the impact of these geological events on the planet's climate and ecosystems.

35:08

๐ŸŒŠ The Isthmus of Panama and Global Climate Change

This paragraph discusses the formation of the Isthmus of Panama and its effects on global ocean currents and climate. The joining of North and South America led to a change in the flow of water between the Pacific and Atlantic oceans, potentially triggering an ice age and causing mass extinctions. The script highlights the interconnectedness of continental movements and global climate patterns.

40:09

๐ŸŒ The Future of Earth's Continents and Natural Disasters

The script envisions the future of Earth's continents, predicting the widening of the Atlantic Ocean and the formation of new mountain ranges. It discusses the inevitability of natural disasters such as earthquakes and volcanic eruptions due to plate tectonics. The paragraph also contemplates the potential for future mass extinctions and the resilience of the human species in the face of these geological changes.

45:12

๐ŸŒ‘ The Ultimate Fate of Earth: Pangaea Ultima

In this final paragraph, the script speculates on the far future of Earth, predicting the formation of a new supercontinent called Pangaea Ultima. It describes the potential climate extremes and the geological changes that will reshape the planet's surface. The paragraph concludes with a reflection on the resilience of life and the possibility that humanity may have to leave Earth in search of a new home due to these drastic changes.

Mindmap

Keywords

๐Ÿ’กContinents

Continents are large, distinct landmasses on Earth's surface, separated by oceans. They are a central theme in the video, illustrating the dynamic nature of Earth's geology. The script discusses how continents are not fixed but are constantly moving due to tectonic forces, shaping Earth's landscape and climate over millions of years, as seen in the formation and destruction of supercontinents like Pangaea.

๐Ÿ’กTectonic Plates

Tectonic plates are the theory that Earth's lithosphere is divided into several large slabs that move atop the asthenosphere. The script explains how these plates' movement causes the continents to drift, collide, and sometimes split apart, leading to the creation of geological features like mountains and ocean trenches, and influencing natural disasters such as earthquakes and volcanic eruptions.

๐Ÿ’กContinental Drift

Continental drift is the hypothesis that the continents move across the Earth's surface, first proposed by Alfred Wegener. The video script uses this concept to explain how the continents were once joined together in supercontinents and have since drifted apart to form the current configuration of Earth's landmasses, and how they will continue to change in the future.

๐Ÿ’กSupercontinent

A supercontinent refers to a landmass comprising multiple continents that have come together. The script mentions historical supercontinents like Val Barra, Rodinia, and Pangaea, and speculates about the future supercontinent, Pangaea Ultima, illustrating the cyclical nature of Earth's continents amalgamating and splitting over geological time.

๐Ÿ’กSubduction Zone

A subduction zone is an area where one tectonic plate moves under another and is forced into the mantle due to plate tectonics. The script describes how subduction zones are sites of intense geological activity, leading to the formation of deep ocean trenches and volcanic activity, and are a key process in the recycling of Earth's crust.

๐Ÿ’กMountain Ranges

Mountain ranges are a series of mountains that form a continuous chain. The video script discusses how mountain ranges like the Alps and Himalayas are formed by the collision of tectonic plates, resulting in the uplift of the Earth's crust and creating some of the most dramatic landscapes on the planet.

๐Ÿ’กFossil Record

The fossil record is the collection of all preserved fossils of plants and animals. The script uses the fossil record to demonstrate how scientists can determine the historical positions of continents and the existence of past environments, such as the identification of freshwater organisms' fossils on different continents, supporting the theory of continental drift.

๐Ÿ’กGeological Time Scale

The geological time scale is a system of chronological measurement used by geologists, archaeologists, and other Earth scientists to describe the timing and relationships of events that have occurred during Earth's history. The script references this scale to frame the immense timescales over which continental movements and geological processes occur, such as the formation and breakup of supercontinents.

๐Ÿ’กMantle

The mantle is the layer of the Earth between the crust and the core. It is composed of silicate rocks rich in iron and magnesium. The script explains that the mantle's heat and pressure make it semi-fluid, allowing tectonic plates to move, and that it plays a crucial role in the process of plate tectonics and the formation of geological features.

๐Ÿ’กMass Extinctions

Mass extinctions are events where a significant proportion of the Earth's biodiversity is wiped out. The script refers to the Permo-Triassic extinction event, which is linked to the formation of the supercontinent Pangaea and its subsequent climate effects, demonstrating the profound impact of geological processes on Earth's life.

๐Ÿ’กNatural Disasters

Natural disasters are catastrophic events resulting from natural processes of the Earth. The script discusses how the movement of tectonic plates can lead to earthquakes, volcanic eruptions, and tsunamis, emphasizing that these events are an inevitable part of the Earth's geological cycle and have significant impacts on human societies.

Highlights

Intergalactic explorers in the distant future find Earth drastically changed, with a single giant landmass and signs of ancient civilizations nearly erased.

The Earth's continents are not fixed but constantly moving due to powerful forces within the planet.

The geological future of New York is predicted to be traumatic, with continents like Africa and Europe colliding.

The Earth's current continents are formed through a natural cycle of construction and destruction over billions of years.

The first land masses were small 'rafts' of rock floating on the mantle, which later grew into continents.

Granite, a buoyant rock, played a crucial role in the formation of the first continents.

Zircon crystals within rocks provide a natural clock to date the Earth's earliest geological events.

Early life forms may have contributed to the formation of granite, which in turn created the first continents.

Continental drift was proposed by Alfred Wegener in 1912, based on the discovery of identical fossils across oceans.

Plate tectonics is driven by the Earth's core heat, creating convection currents in the mantle.

The mid-Atlantic ridge is a place where continents are currently being pushed apart, forming new ocean crust.

The formation of supercontinents like Pangaea has significant effects on global climate and can lead to mass extinctions.

The breakup of Pangaea led to the formation of the continents and climate patterns we recognize today.

The collision of continents creates mountain ranges like the Alps and the Himalayas.

The Grand Canyon was formed by the uplift of the land due to continental collision and subsequent erosion by the Colorado River.

The Isthmus of Panama's formation changed global ocean currents and may have contributed to an ice age.

Continents will continue to move, potentially leading to another supercontinent and altering Earth's climate and ecosystems.

In the far future, Earth may become a single landmass again, known as Pangaea Ultima, with extreme climate conditions.

The movement of continents is responsible for many natural disasters, such as earthquakes and tsunamis.

Despite the inevitability of these geological processes, humanity may need to adapt or seek new habitats in the distant future.

Transcripts

play00:09

planet Earth hundreds of millions of

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years in the future

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intergalactic explorers return to their

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home planet in search of signs of

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ancient civilizations they find a planet

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that has changed beyond recognition

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all other familiar continents that we

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know today instead may find a giant

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landmass with huge mountain ranges

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massive frozen snow fields and glaciers

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the once thriving metropolis they seek

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has disappeared a few broken remnants

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are all that remain crushed and buried

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beneath tons of rock

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could this be a future vision of Earth

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naked science asks what forces could

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create such a bleak and barren world and

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investigates how the awesome power of

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colliding continents shapes and reshapes

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our planet in an endless cycle of

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construction and destruction

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[Music]

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[Music]

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our world's fierce

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from space it's easy to see the

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distinctive pattern of land that makes

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up the continents North America South

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America Africa Antarctica Europe Asia

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and Australia giant land masses

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separated by oceans that stabilise the

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environment with hospitable weather

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patterns suitable for civilization and

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cities to evolve and prosper

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[Music]

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now imagine our planet ravaged by storm

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force winds subjected to extremes of

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temperature giant freezes heat waves and

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droughts a world where cities are

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crushed and destroyed where Africa

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tramples New York underfoot and London

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freezes at the North Pole

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the geological future of New York is

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going to be rather traumatic North

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America and Europe are going to collide

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with one another the world as we know it

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will be unrecognizable this is not a

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portrait of the earth after a

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devastating global disaster

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this is how nature will shape our planet

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many millions of years in the future

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this incredible remodeling is just part

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of a natural cycle that has shaped the

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earth for the last 4 billion years and

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will continue to do so until the Sun

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finally destroys its surface once and

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for all

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today our continents may seem solid safe

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and forever fixed in place but they are

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none of those things these great land

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masses are constantly on the move speed

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up the last few billion years and one

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can see the continents sailing across

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the globe powerful forces deep within

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the planet rip the continents apart and

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then smash them together in an

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ever-changing cycle of death and rebirth

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oceans disappear mountains crumble and

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rise again land masses form and reform

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colliding continents are the mightiest

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force on earth when we look at the

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history of planet Earth we see that it

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is full of change changes as part of

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nature and this change continues today

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and will continue into the future

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to understand how the continents shape

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our world we must first travel back in

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time to the very birth of the earth four

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and a half billion years ago the earth

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is created from the debris leftover from

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the formation of the Sun dust and debris

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collide and clumped together once these

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clumps grow into objects about half a

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mile in diameter they create enough

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gravity to attract more material

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slowly these clumps grow into as many as

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20 planets as these new planets orbit

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the Sun they begin to collide one

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collision with the planet theรก--

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which creates the moon obliterates the

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surface of the earth

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the energy from the collision makes the

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earth incredibly hot at around 11,000

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degrees Fahrenheit it's more than seven

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times hotter than the inside of a

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cremation furnace earth is a massive

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molten ball of boiling lava

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this is primeval hell with thousands of

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asteroids and comets bombard our world

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but deep within the planet a process

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starts that will lead to the first land

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the heaviest elements LED and nickel

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synched down toward the center of the

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earth to form a molten core the lighter

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elements including oxygen and silicon

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rise toward the surface where they erupt

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in volcanoes of molten rock slowly the

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Earth's surface cools molten lava

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solidifies to form patches of crust the

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seeds of the first continents

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but even as the first land is born it

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faces a battle to survive

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we were being bombarded by a large

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number of asteroids very early in the

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history of the planet so there's a lot

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of dynamic change from being walloped by

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giant impacts disturbing things geology

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professor Sam bowring is an expert in

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early Earth and the genesis of the

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continents when we had a early crust as

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is an interesting question I suspect

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we've had and we had an early crust from

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day one the question is how long was

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that preserved when the earth was being

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bombarded constantly by asteroids the

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chance of preserving any small chunk of

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that crust was very low the relentless

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bombardment destroys the new planet's

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crust almost as soon as it forms this

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recycling of the surface continues for

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many millions of years but as the flux

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of asteroids began to wane and as the

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earth matured a little bit I suspect the

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early crust lasted a little bit longer

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eventually the barrage from asteroid

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impact slows down the surface of the

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earth continues to cool but the earth is

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missing one vital ingredient oceans

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we're earth goddess water has been a

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controversial topic over the years I

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think most people now think that many

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meteoritic bodies actually contain quite

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a lot of water water carried by meteors

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and asteroids may form the oceans that

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surround the first continents

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the earth 4.4 billion years ago our

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planet is now 150 million years old and

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the first primitive land masses have

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formed they are not like the seven

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instantly recognizable continents of

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today they are just small rafts of rock

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floating on the mantle but now a type of

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rock appears on the Earth's surface that

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will form the nucleus of future

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continents a rock buoyant enough not to

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sink into the bowels of the earth

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granite in South Africa in the cup vowel

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region southwest of Johannesburg

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geologists examine ancient granite that

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has survived the ravages of time these

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are the ancient remains of what some

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people consider to be the first true

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continent we're looking at the relics

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the remnants of the first continental

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nuclei this is one of the oldest but

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certainly the best preserved continental

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nucleus in the world geologist Alex

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kissters studies how granite formed the

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first continents the rocks here are so

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important because they are remarkably

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well-preserved much better than any way

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on on earth and that allows us actually

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to study processes that were involved in

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the formation while these early crustal

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rocks

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kissters is collecting samples to date

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the age of the granite we're joining

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these little rock horse taking them out

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and then sending off their light onto

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the lap to potatoes dating rocks is a

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complex process because over long

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periods of time the minerals can break

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down and reform into new rocks

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scientists look for an ingredient of

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rock that is tough enough to withstand

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the test of time

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the answer is zircon a crystal that is

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made inside molten rock as it solidifies

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even if the rock is destroyed the

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zircons are durable enough to survive

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zircon is an incredibly interesting

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mineral and it incorporates uranium and

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excludes lead and that sets us up to

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have basically nature's time capsule to

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illustrate this process imagine that

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this hourglass is a newly formed circle

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crystal sand in the top represents

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uranium the sand in the bottom

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represents lead over millions of years

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the uranium in the zircon turns into

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lead measuring the relative proportions

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of sand in the top and bottom of the

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glass reveals how much time has passed

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uranium's relentless decay into lead

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gives us a natural clock using this

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technique geologists date this granite

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at three and a half billion years old

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this makes it some of the oldest rock on

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the planet these rocks make up a major

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part of what is known as the cup Val

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Creighton a Creighton is an ancient raft

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of rock light enough to float on the

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mantle and around which a continent will

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grow ancient cratons have also been

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found in the heart of the Australian and

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North American continents the Creighton

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here in cap Val in South Africa

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stretches for four hundred and

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sixty-three thousand square miles it's

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almost twice the size of Texas without

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granite the Creighton and modern

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continental crust wouldn't exist

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granite forms when minerals in the crust

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melt then react with water cool and

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crystallize because it is made of

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lighter minerals granite is less dense

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than other rock in the mantle so it

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floats on the surface and mixes with

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other rocks to form rafts of land the

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cup Val Creighton is not totally built

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from granite the oldest rocks here are

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these amazing pillow lavas exposed along

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the kamati River three and a half

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billion years ago they form under the

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sea as lava emerges from an underwater

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volcanic vent upon contact with water

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the lava immediately gains a solid crust

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which then cracks and oozes additional

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large blobs called pillows these rocks

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are amongst the oldest that we know it

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is basically identical to Pillar laws

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that we see on a recent ocean floor when

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settings like a wide the kamati pillow

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lavas begin their life on the ocean

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floor but are pushed up out of the sea

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to form part of a continent

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but where did the granite come from to

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create it you need the right mix of

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minerals a new theory suggests that life

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itself may have provided the missing

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ingredients it may sound like an

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outlandish idea but there's some

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evidence that living organisms that use

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photosynthesis appeared around the same

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time that the continents began to grow

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3.8 billion years ago scientist suggests

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that early organisms microbes help speed

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up the breakdown of rock emerging at the

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Earth's crust over hundreds of thousands

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of years this rock breaks down into new

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minerals which sink back into the mantle

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deep below the surface they heat up and

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form granitic magma the magma rises into

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the proto continent freezes and forms

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huge solid rafts of granite

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now stabilized the Creighton begins to

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grow forming new baby continents but

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crayons are not the only factors at work

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more powerful forces are building up

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deep within the planet forces that have

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the power to rip apart land masses and

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smash them together changing the face of

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the planet forever four and a half

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billion years ago the earth forms for

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many years it is bombarded by asteroids

play14:49

and meteors

play14:52

[Music]

play14:54

slowly the molten planet cools and small

play14:57

land masses form around crayons of

play14:59

granite rock massive forces from deep

play15:03

within the planet rip apart and smash

play15:06

these small proto continents together as

play15:09

they grow into the large land masses we

play15:12

see today the surface of the earth the

play15:18

crust is made up of a giant jigsaw of

play15:21

interlocking pieces called tectonic

play15:24

plates the separate plates themselves

play15:26

sit on the mantle the layer between the

play15:29

crust and the Earth's core

play15:32

although the mantle is made of rock the

play15:35

heat and pressure deep down mean it's

play15:37

flexible enough to allow the plates

play15:39

above to move up to several inches a

play15:42

year evidence for the theory of

play15:48

continental drift was first proposed in

play15:51

1912 by German scientist Alfred Wegener

play15:56

he noticed that identical fossils were

play15:59

discovered oceans away from each other

play16:03

paleontologist professor Mark McManaman

play16:05

of Mount Holyoke College in

play16:06

Massachusetts is an expert in fossil

play16:09

records begginer noted that a freshwater

play16:13

organism cannot cross a salty sea and so

play16:16

if you find the fossils of a freshwater

play16:17

organism or a land creature on two

play16:20

continents that are now greatly

play16:22

separated by distance they must once

play16:24

have been closer together by identifying

play16:26

like fossils on different continents

play16:29

scientists can map which continents were

play16:31

joined in the past the fossil

play16:34

distributions will tell us where fossils

play16:37

occur and how the continents must have

play16:41

been juxtaposed fossils that are

play16:43

identical but occurring in very

play16:45

different parts of the world imply that

play16:47

the continents have drifted when he

play16:50

first proposed his theory of continental

play16:52

drift begginer was laughed at the idea

play16:56

that continents could actually move was

play16:59

considered preposterous the problem was

play17:02

he didn't know how the continents moved

play17:06

the missing mechanism wasn't discovered

play17:09

until the 1960s plate tectonics is

play17:14

powered by heat plate echinus is being

play17:18

largely driven by the fact that the

play17:21

interior of the earth is much hotter

play17:23

than the surface the temperature at the

play17:27

center of the core is 10,000 degrees

play17:29

Fahrenheit it's as hot as the outer

play17:32

parts of the Sun much of the heat is

play17:34

left over from the collisions and

play17:36

massive bombardment during the early

play17:38

days of the earth the rest comes from

play17:41

radioactive decay of heavy elements in

play17:44

the core heat escaping from the core

play17:46

creates convection currents in the next

play17:49

layer of the earth the mantle the

play17:52

process is like a lava lamp where heat

play17:55

from the bulb at the bottom creates

play17:57

convection currents in the oil pushing

play18:00

the synthetic lava upward the heat melts

play18:05

part of the mantle and sends plumes of

play18:07

magma molten rock rising to the surface

play18:12

it rises between cracks in the plates

play18:16

creating new rock that pushes the plates

play18:19

apart I think that plate tectonics is

play18:25

virtually inescapable on this planet

play18:27

it's an exceedingly efficient way to

play18:29

cool the interior of the earth this

play18:33

formation of new rocks splits apart and

play18:36

separates the plates and the continents

play18:38

sitting on them today the majority of

play18:42

this new rock forms under the sea

play18:44

creating vast interconnected volcanic

play18:47

mountain ranges that extend through all

play18:50

the major oceans of the world

play18:52

one range can clearly be seen at the

play18:54

bottom of the Atlantic Ocean along the

play18:56

mid-atlantic ridge it stretches more

play18:59

than 12,000 miles from a sub-antarctic

play19:02

to the Arctic it comes to the surface in

play19:06

a few places Iceland was created from

play19:09

volcanic lava bubbling up at the

play19:11

junction between the North American and

play19:13

Eurasian plates it's one of the few

play19:16

places on earth that one can actually

play19:18

see continents being pushed apart we are

play19:23

watching here geological structures that

play19:25

you cannot really watch anywhere else

play19:26

it's like a big textbook of geology this

play19:29

is where the Earth's crust is being made

play19:32

pal I nursin professor of geophysics at

play19:35

the University of Iceland monitors the

play19:38

mid-ocean ridge where the continental

play19:40

plates are splitting apart the ridge in

play19:44

Iceland is almost three miles wide on

play19:47

one side is the North American plate on

play19:49

the other side the eurasian plate the

play19:53

rift here grows as new rock forms at its

play19:56

center

play19:56

pushing North America and Europe away

play19:59

from each other the Atlantic Ocean

play20:01

widens and the two continents drift

play20:04

apart eventually the Atlantic could

play20:07

become as big as the Pacific to measure

play20:10

how fast they're splitting a nursin

play20:13

takes Global Positioning System readings

play20:15

at specific points along the plate

play20:17

margin to put the antenna right on top

play20:20

of the point and then we can calculate

play20:22

the exact position of this point in the

play20:25

world respect to the central earth

play20:28

although the ridge appears calm and

play20:31

there's no magma rising to the surface

play20:34

ina syns measurements show that the two

play20:36

continents are drifting apart by around

play20:39

an inch a year so by the end of the

play20:42

century Europe and America will be

play20:44

almost eight feet further apart

play20:47

the movement in Iceland is typical of

play20:50

the processes shaping the continents

play20:52

since their birth 4.4 billion years ago

play20:55

it's part of the great cycle of the

play20:58

Earth's continents the new crust created

play21:01

at the mid-ocean ridge moves away cools

play21:04

and eventually sinks back into the earth

play21:08

when the first proto continents formed

play21:11

there were several interconnecting

play21:12

tectonic plates constantly bumping and

play21:16

grinding against each other pushing the

play21:18

new land over the planet today the earth

play21:22

has over a dozen plates some colliding

play21:25

together some moving apart they are

play21:28

powerful enough to move a continent the

play21:31

size of North America over 3,000 miles

play21:34

in 200 million years that's 15 miles

play21:38

every million years the earth 3.4

play21:44

billion years ago and plate tectonics

play21:46

pushes the proto continents together

play21:48

they combine to form ever larger tracts

play21:52

of land

play21:54

scientist suggests that cratons combined

play21:57

with other crayons to form a

play21:59

supercontinent a huge continuous stretch

play22:02

of land

play22:03

it's called Val Barra scientists are

play22:07

unsure of its exact shape or size as

play22:10

only a few pieces like the crayon in

play22:13

South Africa still remain but Val Boras

play22:16

days are numbered

play22:18

a rising plume of heat is growing

play22:22

beneath it it's about to rip the world's

play22:24

first supercontinent into pieces 2.7

play22:35

billion years ago val barra the world's

play22:39

first supercontinent still dominates the

play22:42

planet but plate tectonics powered by

play22:45

heat from the Earth's core is about to

play22:48

split it apart rock is a good insulator

play22:52

when a continent gets very large the

play22:55

rock traps heat beneath it

play23:00

as it gets hotter and hotter a plume of

play23:04

superheated magma builds up beneath the

play23:06

giant continental mass the temperature

play23:10

continues to rise and pressure in the

play23:12

mantle increases eventually the crust

play23:16

can no longer contain the pressure and

play23:18

the hot lava breaks through ripping the

play23:21

land apart

play23:24

you can see this process happening today

play23:27

in Africa heat from the Earth's core is

play23:30

ripping the continent apart a giant Rift

play23:34

Valley runs from the Red Sea down to

play23:37

Mozambique giant cracks are opening up

play23:40

in the land volcanoes like Kilimanjaro

play23:44

marked spots where molten rock have

play23:47

risen to the surface in the past

play23:51

in ten million years the eastern half of

play23:55

the continent will have split away

play24:00

the molten lava trapped beneath the

play24:02

giant supercontinent of all bara

play24:05

eventually smashes through the surface

play24:07

Rock the continent ruptures into several

play24:10

smaller pieces these bits of land sail

play24:14

across the earth but nobody knows what

play24:18

happens to them or what the planet looks

play24:20

like at this time the earth is entering

play24:23

the dark ages it is over two and a half

play24:26

billion years since it was formed it

play24:29

will be over a billion years before

play24:31

another supercontinent forms

play24:38

the earth is entering a deadly cycle of

play24:42

destruction and rebirth the theory of

play24:46

continental drift suggests that we go

play24:48

through cyclic phases of continental

play24:51

dispersion and then continental

play24:53

collision and the continents then seem

play24:56

to move apart from one another and then

play24:58

collide with one another over a maybe a

play25:01

hundred million year or more timescale

play25:05

when a large continent splits apart the

play25:09

separate pieces travel away from each

play25:10

other

play25:11

pushed by the creation of new land at

play25:13

the ridge between plates because the

play25:16

earth has a constant surface area the

play25:18

same amount of land created must be

play25:21

absorbed into the earth this process

play25:23

happens at subduction zones at the

play25:26

junctions of plates at a subduction zone

play25:29

crust dives down into the mantle to be

play25:32

melted to form new rock when the plate

play25:35

subducts into the earth it brings two

play25:37

pieces of land together when they

play25:40

collide a new supercontinent starts to

play25:43

form

play25:46

it is now 1.1 billion years ago on our

play25:49

timeline and the next known

play25:51

supercontinent has formed its name is

play25:54

rodinia and it holds almost all of the

play25:57

continental rock on the surface of the

play25:59

earth still no one knows exactly what it

play26:02

looked like but at its heart is an area

play26:05

that will eventually become North

play26:06

America 350 million years later the

play26:11

cycle of annihilation and creation

play26:13

starts again as the buildup of heat

play26:16

beneath the surface of the earth tears

play26:18

Rodinia apart when Rodinia splits it

play26:22

forms several smaller continents that

play26:25

for millions of years drift apart and

play26:27

then drift back together again to form

play26:30

Gondwana a supercontinent in the

play26:33

southern hemisphere eventually after

play26:36

several hundred million years Gondwana

play26:38

slowly splits apart

play26:40

plate tectonics pushed the land back

play26:42

together to create the world's last

play26:45

supercontinent it's a huge landmass

play26:49

known as Pangaea

play26:53

all the continents we know today are

play26:55

here join together geologists are able

play27:01

to plot the continents relative

play27:03

positions because 350 million years ago

play27:06

there are numerous species on earth each

play27:09

living in distinct regions this specimen

play27:13

that I have right here is the first

play27:15

trial of light that was ever described

play27:17

from what is now the United States it is

play27:20

exactly the same type of trilobite that

play27:23

occurs on the other side of the Atlantic

play27:25

Ocean in North Africa so we know then

play27:28

that the trello bites in the old and new

play27:31

worlds must have been close together

play27:34

because they're so closely related the

play27:37

fossil records show that North America

play27:39

and Europe rests next to one another the

play27:43

land where New York now sits is next to

play27:45

Morocco in North Africa the Atlantic

play27:48

Ocean does not exist the east coast of

play27:53

South America Nestle's against the

play27:54

western coast of Africa while Australia

play27:57

India and Antarctica are joined to the

play28:00

southeast of Africa if we want to look

play28:06

at a picture of the world 250 million

play28:08

years ago we're gonna look at a world in

play28:10

which a four-footed creature could walk

play28:13

from one end of this landmass to the

play28:14

other Pangaea is one giant continuous

play28:20

landmass

play28:22

it not only makes the world look very

play28:24

different it also has a dramatic effect

play28:27

on climate because much of the land is

play28:33

located far from the sea the climate of

play28:36

the interior changes radically from

play28:38

season to season it gets very hot in the

play28:41

summertime and extremely cold in the

play28:45

winter you don't have the moderating

play28:50

influence of the ocean that we have

play28:51

today so it's a very different world and

play28:54

it's a world that in some ways is is

play28:56

harsher and less hospitable at least to

play28:59

life on land it's thought that the

play29:04

climate change caused by pangaea's

play29:06

formation may have played a role in one

play29:09

of the largest mass extinctions on earth

play29:11

this event known as the per mo Triassic

play29:15

mass extinction wipes out about 90% of

play29:18

all life on Earth

play29:19

it's been called the mother of all mass

play29:22

extinctions I would consider that the

play29:24

formation of Pangaea with its climate

play29:28

worsening effects to be a contributing

play29:31

factor however and not the sole cause of

play29:34

the mass extinction 250 million years

play29:38

ago and the supercontinent of pangaea is

play29:41

breaking up the continents we know and

play29:44

recognize today begin to take shape over

play29:48

the next tens of millions of years South

play29:52

America drifts away from Africa North

play29:55

America away from Europe

play29:59

Australia splits off from Antarctica and

play30:02

heads north to warmer climes the

play30:06

positions of our continents are becoming

play30:08

familiar although they're

play30:09

distinguishable features are not the

play30:13

world's vast mountain ranges the Alps

play30:16

and Himalayas and it's great valleys

play30:18

like the Grand Canyon are yet to form

play30:21

they will emerge out of one of the

play30:24

biggest battles in nature the battle

play30:27

between colliding continents

play30:29

[Music]

play30:35

earth 100 million years ago the

play30:40

continental map of the modern world is

play30:42

gradually becoming recognizable but a

play30:45

battle is still raging between the

play30:47

continents that will change the face of

play30:49

our world forever and create some of the

play30:52

most extraordinary geological features

play30:54

on the planet as the continents move

play30:58

slowly across the earth crust and rock

play31:01

is dragged back down into the earth at

play31:03

subduction zones between the tectonic

play31:05

plates but when continents collide at

play31:09

the plate junctions sometimes there is a

play31:12

battle for supremacy if neither plate

play31:17

will submit and drop down to be consumed

play31:19

by the mantle then both the continents

play31:22

slowly smash and grind into each other

play31:25

these pinch points of continental

play31:28

collision build mountains

play31:30

[Music]

play31:35

the Alps are the largest mountain range

play31:38

in Europe higher than the Rockies the

play31:41

Alps stretch from France in the West

play31:43

through Italy Switzerland and Austria to

play31:47

Slovenia in the east their formation is

play31:51

a direct result of a continental

play31:52

collision between Africa and Europe the

play31:56

story of the Alps begins when the

play31:57

African plate breaks away from the South

play32:00

American plate it starts moving toward

play32:02

Europe without the plate movement there

play32:07

wouldn't be any mountain on this planet

play32:10

professor Gerard Stanley of Lausanne

play32:13

University in Switzerland studies the

play32:15

processes that built the Alps

play32:21

the African and Eurasian plates start to

play32:24

move toward each other trapping a third

play32:27

smaller Iberian plate between them the

play32:30

three plates collide the Eurasian Plate

play32:33

is pushed downward into the mantle

play32:35

chopping off the Iberian plate but รซthis

play32:38

si begins to close as the eurasian plate

play32:43

grinds underneath the African plate it

play32:46

pushes the tether part of the iberian

play32:49

plate 600 miles north and many thousands

play32:53

of feet into the air rocks that started

play32:56

life on the bottom of the ocean end up

play32:59

at the top of the alps what's

play33:05

fascinating to imagine that if you are

play33:07

on top of the Matterhorn you actually is

play33:09

staying on top of africa for geologists

play33:12

africa stops in the alps over the next

play33:19

100 million years the continents

play33:21

continue to smash together new mountain

play33:25

ranges start forming around the globe

play33:27

the largest the Himalayas form as the

play33:31

Indian plate charges northward toward

play33:34

the Eurasian Plate it moves at two

play33:37

inches per year lining up a head-on

play33:40

collision the movement of the Indian

play33:44

plate leads to a clash between two giant

play33:47

continents and creates some of the

play33:50

highest structures ever to exist on

play33:52

earth the incredible power of

play33:58

continental drift not only builds

play34:01

mountains

play34:01

it also sculpts one of the world's most

play34:04

recognizable landmarks the Grand Canyon

play34:08

in Arizona

play34:11

the Grand Canyon is a great scar in the

play34:14

surface of the earth geologist Ron

play34:17

Blakey

play34:18

has been studying the canyon for over 30

play34:20

years it's just a wonderful place to

play34:22

come face to face with planet earth the

play34:28

Grand Canyon is 277 miles long and up to

play34:32

18 miles wide at its deepest it

play34:37

stretches down for over a mile

play34:43

the gorge exposes the interior of the

play34:46

North American continent it's like

play34:48

looking through the pages of a book each

play34:50

layer tells a story about the past

play34:54

[Music]

play34:57

whatever really neat things about Grand

play35:00

Canyon is this we go up the walls of the

play35:03

Grand Canyon since it's like going

play35:04

through a time machine layer upon layer

play35:08

of rock reveal the geological history of

play35:11

North America from present day to two

play35:15

billion years ago the deeper you go the

play35:20

older the rocks by studying the layers

play35:25

Blakey can piece together the history of

play35:27

the canyon he finds some of the most

play35:30

interesting evidence at the very top

play35:33

fossils of ocean creatures Wow this beds

play35:41

the jackpot here what we have is a

play35:43

extraordinary example of a Permian sea

play35:47

floor the most important thing it tells

play35:49

us with respect to the Grand Canyon is

play35:51

that this area had to be near sea level

play35:53

when these rocks formed now it's 7,000

play35:56

feet above sea level in the room of the

play35:58

Grand Canyon so something had to happen

play36:01

either the sea had a fall 7,000 feet and

play36:04

we're pretty sure that didn't happen or

play36:06

this landscape had to be uplifted 7,000

play36:09

feet we're pretty sure that happened 250

play36:13

million years ago the canyon starts to

play36:16

form as a result of a collision between

play36:18

the Pacific and North American plates

play36:21

they collide with such force the North

play36:24

American plate thrusts more than two

play36:27

miles upward what was once seabed rises

play36:31

over a period of 15 million years to

play36:34

form a vast plateau far above sea level

play36:43

it stays that way for millions of years

play36:46

until it is transformed by water erosion

play36:50

[Music]

play36:55

six million years ago several hundred

play36:58

miles south of the canyon plate

play37:01

movements open up the Gulf of California

play37:02

to the sea for the first time small

play37:06

streams in the Rocky Mountains could

play37:08

empty into the ocean so if we're

play37:11

starting a stream at 14,000 feet in the

play37:14

Rocky Mountains and carving down the sea

play37:16

level and the Grand Canyon just happens

play37:18

to be in the way the Grand Canyon is

play37:20

going to get cut out these streams

play37:24

merged to form what is now called the

play37:26

Colorado River it cuts down through the

play37:29

land heading to the Gulf of California

play37:36

it took a river to carve the canyon the

play37:40

water has carved down through the rocks

play37:41

layer by layer by layer removing

play37:44

material out of the canyon and leaving

play37:47

the great void that sits behind me the

play37:49

Grand Canyon is a testament to the

play37:52

awesome power of the continents in

play37:54

shaping our world back on our journey

play37:58

tracing the birth and death of the

play38:00

continents it is now 20 million years

play38:03

ago two and a half thousand miles south

play38:07

of the Grand Canyon another plate

play38:09

collision is about to take place the map

play38:16

of the modern world is almost complete

play38:22

at this time water flowing freely

play38:24

between the Pacific and Atlantic oceans

play38:26

still separates North and South America

play38:29

over many millions of years the Pacific

play38:32

plate begins sliding under the Caribbean

play38:35

plate the pressure causes underwater

play38:38

volcanoes to erupt some explode with

play38:42

such ferocity that they create a range

play38:44

of small islands between North and South

play38:46

America

play38:51

over the next 17 million years ocean

play38:56

currents deposit sediment and gaps

play38:58

between these new islands

play39:02

gradually the sediment builds up and

play39:04

compresses to form land bridges between

play39:07

the islands three million years ago the

play39:12

Isthmus of Panama a narrow strip of land

play39:15

finally joins North and South America it

play39:18

separates the Pacific and Atlantic

play39:20

oceans the flow of water between the two

play39:24

stops and ocean currents must take new

play39:27

routes

play39:28

this causes yet another change in the

play39:31

climate of our planet

play39:32

it changes the movement of warm seas

play39:35

around the globe disrupting weather

play39:38

patterns possibly pushing the planet

play39:40

into an ice age many species are wiped

play39:44

out the continents as we know them today

play39:46

are formed creating the nice hospitable

play39:49

environment for human civilization to

play39:52

evolve and thrive on planet Earth

play39:54

but how long will it last the forces

play39:59

that power plate tectonics are still

play40:01

active and will tear our continents

play40:03

apart once again they will build a new

play40:05

world one that may trigger another mass

play40:09

extinction and push humanity to the

play40:11

brink of annihilation

play40:13

[Music]

play40:18

a view from space reveals Earth's

play40:22

continents as we know them today there

play40:24

are seven in total but some are

play40:26

separated by a political divide rather

play40:29

than a geographical one Africa Eurasia

play40:31

is a super continent comprising of

play40:34

Africa Europe and Asia it stretches from

play40:37

the Siberian plateau in Russia to the

play40:39

Cape of Good Hope in South Africa a

play40:42

spectacular route across three

play40:44

continents incorporating dramatic

play40:46

climate change vivid scenery and diverse

play40:49

cultures however Africa Eurasia isn't

play40:53

the only super continent on the planet

play40:54

because the Panama isthmus links North

play40:58

and South America together they too can

play41:00

be thought of as one vast landmass and

play41:02

if the Bering Strait between Russia and

play41:05

Alaska were to freeze over it would be

play41:08

possible to walk from Cape Horn in South

play41:10

America to the Cape of Good Hope in

play41:12

South Africa a journey of around 25,000

play41:17

miles but this won't always be possible

play41:21

for powerful forces deep below the

play41:23

surface continue to send the continents

play41:26

hurdling across the globe a process that

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started at their birth 4.4 billion years

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ago and one which will continue long

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into their future what we observing at

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the moment is only a snapshot of the

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Earth's global cycle that has been

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undergoing for last four and a half

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billion years probably and will be

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undergoing even if you're not around any

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the global continental cycle has another

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impact on our world it causes many

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natural disasters plate movement creates

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stress points which lead to volcanic

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eruptions as continents split apart

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instability at the plate junctions

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causes earthquakes that rip apart whole

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communities this one on October 8th 2005

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in Pakistan ruled Kashmir killed nearly

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75 thousand people and left up to 3

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million homeless and when plates abduct

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into the earth their death throes

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produced devastating waves the 2004

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Indonesian tsunami is just one

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demonstration of the terrifying power

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unleashed when plates move

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such natural disasters are part of the

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continental cycle and they're not going

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to stop

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plates moving is something we have to

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live with there's nothing we can do

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about it it's going to happen they're

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going to be big earthquakes in

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California there's going to be a lot of

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damage there's going to be loss of life

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in recent years it seems as though

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natural disasters powered by the

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movement of the continents have been on

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the rise but what we are witnessing is

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an increase in awareness rather than an

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increase in the number or severity of

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natural disasters I think what we're

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really seeing here is a very raised

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consciousness of the public with instant

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communication abilities much more

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publicity is given to volcanic eruptions

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and earthquakes we are observers to only

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a very short period of the life of the

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earth if we could monitor earthquakes

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and volcanic activity caused by plate

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movements over millions of years we

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would see a very different picture when

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you look at something over 10 years you

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might have 10 major earthquakes the next

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10 years you might not have any but

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that's not significant it just is

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related to the short period of time that

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you're making the observation at when

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you start looking at hundreds thousands

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and millions of years all that averages

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out it's impossible to predict exactly

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when the next disaster will occur but it

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is possible to predict where it will

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happen the plate boundaries

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map the location of earthquakes and

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volcanoes and they line up with the

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cracks between plates plot where these

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plates will move over the next tens of

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millions of years and the future looks

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bleak for many of the world's cities

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[Music]

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so what will our world look like in the

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future 50 million years from now the

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Atlantic Ocean will widen pushing New

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York further away from North Africa

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meanwhile in the southern hemisphere

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Australia will be on a collision course

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with Southeast Asia and in Europe Africa

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will head north closing the

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Mediterranean Sea a new mountain range

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will form where Italy and Greece once

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stood known as the Mediterranean

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Mountains they will be as big as the

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Himalayas extending from Spain across

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southern Europe through the Middle East

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and into Asia 100 million years in the

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future and the power of continental

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movements will render the surface of the

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earth unrecognizable the Atlantic Ocean

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will continue to widen but a subduction

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zone will form along its western

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shoreline the first sign of it can be

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seen today in the Caribbean the Puerto

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Rico Trench this trench will grow north

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and south along the east coast of North

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and South America

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this vast subduction zone will consume

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the Atlantic Ocean drag in Europe and

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Africa back toward the Americas

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[Music]

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250 million years in the future

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intergalactic explorers returning to

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their home planet will find a world very

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different to the one in their records

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there will no longer be seven continents

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but one gigantic landmass containing

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most of the land on earth they could

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find it a barren frozen world the

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explorers search for the remains of our

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cities but when Europe and America

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collide any cities along the coastlines

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will be gradually destroyed the

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geological future of New York is going

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to be rather traumatic in the long term

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a New York is going to be at the site of

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a continental collision North America

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and Europe are going to collide with one

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another and produce a distinctive suite

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of rocks which will eventually be

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crumpled between the two continents as

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they collide New York and its neighbors

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will be crushed and buried beneath the

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surface leaving no more than a few

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remains in the future geologists will be

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able to find remains of New York City

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trapped in the rocks themselves either

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buildings or plastic bottles or old

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autos and their parts all of these

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things will be incorporated into the

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fossil record and will be recognizable

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to a future geologist who knows what she

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or he is looking for

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because of its similarities to pass

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supercontinents this future land mass is

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called Pangaea Ultima the final Pangaea

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nearly all the land masses in the world

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will be joined together an Gaea Ultima

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will probably experience climate

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extremes freezing winters and scorching

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summers this deadly weather could have

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devastating effects on all life on Earth

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the implications for the human race are

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interesting to speculate about certainly

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the disposition of the continents over

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time will affect Earth's climate and

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that will in turn have an influence on

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which organisms survive which go extinct

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and could be a factor in future mass

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extinctions

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the world we know is inching slowly

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toward its own destruction the processes

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that shape the surface of the earth are

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never going to change we're going to

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have earthquakes we're going to have

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volcanoes we're going to have tsunamis

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and hurricanes regardless of whether

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humans inhabit the planet and so the

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planet will always be here probably

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plate tectonics will operate for the

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foreseeable future or not but even

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Pangaea Ultima might not be the end of

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the story the forces that created it may

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eventually rip it apart and start the

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cycle of death and rebirth again but by

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then the impact of colliding continents

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could have been too much for our species

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with our cities destroyed and the

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climate severe we may have already left

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our planet in search of a safer home

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[Music]

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you

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Related Tags
Continental DriftEarth's FutureGeological CyclePlate TectonicsNatural DisastersClimate ChangeSupercontinentsMass ExtinctionsPlanetary EvolutionGeology Science