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Inside Earth(Earth Layers)
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Inside the Earth The Layers of the Earth! ● Earth Layers The Earth is divided into four main layers. *Inner Core *Outer Core *Mantle *Crust crust mantle core ● ● ● Earth's Layers How are the earth's layers similar to an egg? Shell-crust Egg white-mantle Yolk-core iStockphoto The Crust *This is the layer that we live on The crust of the Earth is broken into many pieces called plates. Two types of crust Continental and oceanic ● Thickness - ~ 5 miles under the oceans ~25 miles under the continents *The crust makes up 1% of the Earth. Outer Core Inner Core -Mantle Crust Indian Ocean Continent of Africa Thickness of the Earth's Crust (km) 30 1.0 30 30. 10 40- 1.0 30 40. 30 40 40 1.0. 1.0 40- 30. 30 30. 40 New Jersey - Crust - ~28 miles 40- 40 45. 30 40 1.0. 30 40 30 10 2 types of crust — The Crust Oceanic (very dense, made of basalt) Continental (less dense, made of granite) Continental crust Oceanic crust Oceanic and Continental Crust Oceanic Crust Continental Crust Montle WHY DOES EARTH HAVE LAYERS? The Two Types of Crust - Oceanic and Continental Characteristic Thickness Composition Geological age Density Elevation Remelted and destroyed Deformed Continental Crust 35-50 km Granite (light) to 3.8 billion B.P. 2.7 Ave. +1,000 m No Yes 33% Current distribution Oceanic Crust 5-12 km Basalt (dark) to 150,000,000 B.P. 3.0 Ave. - 3,000 m Yes No 67% ● ● The Mantle semi- liquid largest layer of the Earth. divided into two regions: the upper and lower sections. Outer Core Diagram not drawn to scale Inner Core Co Cu th Convection Currents in the Mantle Continental cruit Downwelling Suduction 20 Super cold plume Convection Plate miration Super hot plume Mantle Lithophile sements Sidirop Outer Corets Inner Core South Pac Mid-oceanca Convection Currents magma in the mantle rises as it heats up and falls as it cools down. Image By: Colin Salmon, Dorling Kindersley Outer Core The outer core is liquid. * made up of nickel and iron Outer Core Mantle 1400 Miles Thick Liquid Iron & Nickel Inner Crust Core Diagram not drawn to scale ● Inner Core The inner core of the Earth is solid. It has temperatures...
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Alternative transcript:
and pressures so great that the metals are squeezed together and are not able to move. Crust Diagram Courtesy of Dr. Stephen Matins Outer Mantle Inner Mantle Inner Gore Outer Core Physical Structure of the Earth (5 Layers) Lithosphere- rigid outer layer (crust) Asthenosphere- solid rock that flows slowly (like hot asphalt) Mesosphere- middle layer Outer Core-liquid layer Inner Core-solid, very dense 5 Layers of the Earth Lithosphere (crust and upper- most solid mantle) Crust 0-100 km thick To scale Crust Mantle Outer core Inner core Asthenosphere Mesosphere 2,900 km 5,100 km- 6,378 km Liquid Solid Core Mantle Not to scale Ocean Drilling A ship like this is used for exploration below the earth's crust JE We have not drilled below earth's crust - but we have gotten close. Drilling Tools Advanced CORK System are Core Sa Active Heave Co By drilling the sea floor: Establish deep-sea drilling technology Clarify the global environment changes Research in gas hydrate Search for deep biosphere Observe the seismo- genic zone directly Reach the Earth's mantle where human beings have never explored A depth of 2,500m Target depth of 4,000m OCEANIC CRUST 0-20 Ma 20-65 Ma>65 Ma GEOLOGIC PROVINCE Shield Platform Orogen Basin Large Igneous Province Extended Crust U.S. Geological Survey Convection Currents Heat (convection) cells in mantle/asthenosphere Lithosphere rests on asthenosphere Rising heat cells - plates separate Sinking heat cells - plates pushed down into mantle cooler hotter The Driving Force: Convection Currents e Tasa Collection: Plate Tectonics Outer Core (2270 km) Inner Core (1216 km) (100 km) Asthenosphere (600 km) Mantle (2885 km) Oceanic Crust (5 km) Continental Crust (30-40 km) Lithosphere Pull Mantle Core Mantle Core Push Pusih Montle Mantie Core Lithosphere Pull Lithosphere Thermal Plume Core Copyright 1984, by Tasa Graphic Arts, Inc. All rights reserved. By drilling the sea floor: Establish deep-sea. drilling technology Clarify the global environment changes Research in gas hydrate Search for deep biosphere Observe the seismo- genic zone directly Reach the Earth's mantle where human beings have never explored A depth of 2,500m Target depth of 4,000m HOW DEEP HUMANS HAVE DUG F Ti
Inside Earth(Earth Layers)
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This presentation explains what is inside earth and the 4 layers of earth and more!!
~Taffi~
33 Followers
This presentation explains what is inside earth and the 4 layers of earth and more!!
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Inside the Earth The Layers of the Earth! ● Earth Layers The Earth is divided into four main layers. *Inner Core *Outer Core *Mantle *Crust crust mantle core ● ● ● Earth's Layers How are the earth's layers similar to an egg? Shell-crust Egg white-mantle Yolk-core iStockphoto The Crust *This is the layer that we live on The crust of the Earth is broken into many pieces called plates. Two types of crust Continental and oceanic ● Thickness - ~ 5 miles under the oceans ~25 miles under the continents *The crust makes up 1% of the Earth. Outer Core Inner Core -Mantle Crust Indian Ocean Continent of Africa Thickness of the Earth's Crust (km) 30 1.0 30 30. 10 40- 1.0 30 40. 30 40 40 1.0. 1.0 40- 30. 30 30. 40 New Jersey - Crust - ~28 miles 40- 40 45. 30 40 1.0. 30 40 30 10 2 types of crust — The Crust Oceanic (very dense, made of basalt) Continental (less dense, made of granite) Continental crust Oceanic crust Oceanic and Continental Crust Oceanic Crust Continental Crust Montle WHY DOES EARTH HAVE LAYERS? The Two Types of Crust - Oceanic and Continental Characteristic Thickness Composition Geological age Density Elevation Remelted and destroyed Deformed Continental Crust 35-50 km Granite (light) to 3.8 billion B.P. 2.7 Ave. +1,000 m No Yes 33% Current distribution Oceanic Crust 5-12 km Basalt (dark) to 150,000,000 B.P. 3.0 Ave. - 3,000 m Yes No 67% ● ● The Mantle semi- liquid largest layer of the Earth. divided into two regions: the upper and lower sections. Outer Core Diagram not drawn to scale Inner Core Co Cu th Convection Currents in the Mantle Continental cruit Downwelling Suduction 20 Super cold plume Convection Plate miration Super hot plume Mantle Lithophile sements Sidirop Outer Corets Inner Core South Pac Mid-oceanca Convection Currents magma in the mantle rises as it heats up and falls as it cools down. Image By: Colin Salmon, Dorling Kindersley Outer Core The outer core is liquid. * made up of nickel and iron Outer Core Mantle 1400 Miles Thick Liquid Iron & Nickel Inner Crust Core Diagram not drawn to scale ● Inner Core The inner core of the Earth is solid. It has temperatures...
Inside the Earth The Layers of the Earth! ● Earth Layers The Earth is divided into four main layers. *Inner Core *Outer Core *Mantle *Crust crust mantle core ● ● ● Earth's Layers How are the earth's layers similar to an egg? Shell-crust Egg white-mantle Yolk-core iStockphoto The Crust *This is the layer that we live on The crust of the Earth is broken into many pieces called plates. Two types of crust Continental and oceanic ● Thickness - ~ 5 miles under the oceans ~25 miles under the continents *The crust makes up 1% of the Earth. Outer Core Inner Core -Mantle Crust Indian Ocean Continent of Africa Thickness of the Earth's Crust (km) 30 1.0 30 30. 10 40- 1.0 30 40. 30 40 40 1.0. 1.0 40- 30. 30 30. 40 New Jersey - Crust - ~28 miles 40- 40 45. 30 40 1.0. 30 40 30 10 2 types of crust — The Crust Oceanic (very dense, made of basalt) Continental (less dense, made of granite) Continental crust Oceanic crust Oceanic and Continental Crust Oceanic Crust Continental Crust Montle WHY DOES EARTH HAVE LAYERS? The Two Types of Crust - Oceanic and Continental Characteristic Thickness Composition Geological age Density Elevation Remelted and destroyed Deformed Continental Crust 35-50 km Granite (light) to 3.8 billion B.P. 2.7 Ave. +1,000 m No Yes 33% Current distribution Oceanic Crust 5-12 km Basalt (dark) to 150,000,000 B.P. 3.0 Ave. - 3,000 m Yes No 67% ● ● The Mantle semi- liquid largest layer of the Earth. divided into two regions: the upper and lower sections. Outer Core Diagram not drawn to scale Inner Core Co Cu th Convection Currents in the Mantle Continental cruit Downwelling Suduction 20 Super cold plume Convection Plate miration Super hot plume Mantle Lithophile sements Sidirop Outer Corets Inner Core South Pac Mid-oceanca Convection Currents magma in the mantle rises as it heats up and falls as it cools down. Image By: Colin Salmon, Dorling Kindersley Outer Core The outer core is liquid. * made up of nickel and iron Outer Core Mantle 1400 Miles Thick Liquid Iron & Nickel Inner Crust Core Diagram not drawn to scale ● Inner Core The inner core of the Earth is solid. It has temperatures...
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Knowunity was a featured story by Apple and has consistently topped the app store charts within the education category in Germany, Italy, Poland, Switzerland and United Kingdom. Join Knowunity today and help millions of students around the world.
Still not sure? Look at what your fellow peers are saying...
iOS User
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Stefan S, iOS User
The application is very simple and well designed. So far I have found what I was looking for :D
SuSSan, iOS User
Love this App ❤️, I use it basically all the time whenever I'm studying
Alternative transcript:
and pressures so great that the metals are squeezed together and are not able to move. Crust Diagram Courtesy of Dr. Stephen Matins Outer Mantle Inner Mantle Inner Gore Outer Core Physical Structure of the Earth (5 Layers) Lithosphere- rigid outer layer (crust) Asthenosphere- solid rock that flows slowly (like hot asphalt) Mesosphere- middle layer Outer Core-liquid layer Inner Core-solid, very dense 5 Layers of the Earth Lithosphere (crust and upper- most solid mantle) Crust 0-100 km thick To scale Crust Mantle Outer core Inner core Asthenosphere Mesosphere 2,900 km 5,100 km- 6,378 km Liquid Solid Core Mantle Not to scale Ocean Drilling A ship like this is used for exploration below the earth's crust JE We have not drilled below earth's crust - but we have gotten close. Drilling Tools Advanced CORK System are Core Sa Active Heave Co By drilling the sea floor: Establish deep-sea drilling technology Clarify the global environment changes Research in gas hydrate Search for deep biosphere Observe the seismo- genic zone directly Reach the Earth's mantle where human beings have never explored A depth of 2,500m Target depth of 4,000m OCEANIC CRUST 0-20 Ma 20-65 Ma>65 Ma GEOLOGIC PROVINCE Shield Platform Orogen Basin Large Igneous Province Extended Crust U.S. Geological Survey Convection Currents Heat (convection) cells in mantle/asthenosphere Lithosphere rests on asthenosphere Rising heat cells - plates separate Sinking heat cells - plates pushed down into mantle cooler hotter The Driving Force: Convection Currents e Tasa Collection: Plate Tectonics Outer Core (2270 km) Inner Core (1216 km) (100 km) Asthenosphere (600 km) Mantle (2885 km) Oceanic Crust (5 km) Continental Crust (30-40 km) Lithosphere Pull Mantle Core Mantle Core Push Pusih Montle Mantie Core Lithosphere Pull Lithosphere Thermal Plume Core Copyright 1984, by Tasa Graphic Arts, Inc. All rights reserved. By drilling the sea floor: Establish deep-sea. drilling technology Clarify the global environment changes Research in gas hydrate Search for deep biosphere Observe the seismo- genic zone directly Reach the Earth's mantle where human beings have never explored A depth of 2,500m Target depth of 4,000m HOW DEEP HUMANS HAVE DUG F Ti