earth’s interior and plate tectonics integrated science ch 12
TRANSCRIPT
![Page 1: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/1.jpg)
Earth’s Interior and Plate Earth’s Interior and Plate TectonicsTectonics
Integrated ScienceIntegrated Science
Ch 12Ch 12
![Page 2: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/2.jpg)
This is how the continents This is how the continents formed….formed….
• http://www.youtube.com/watch?v=TzzGPfVx32M&list=PLABDC7B24FAFE33FD
![Page 3: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/3.jpg)
The Earth is like a parfait, it has layersThe Earth is like a parfait, it has layers
• If you cut the earth in half, it would look very much like a parfait, with different layers and compositions based on density
• The earth has three main layers, the crust, the mantle, and the core
![Page 4: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/4.jpg)
The CrustThe Crust
• We live on this layer• Its is cool, and made of
solid rock• Oceanic crust is thinner
and denser than continental crust.
• The crust is the least dense portion of the earth and only about 12-25 miles thick
![Page 5: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/5.jpg)
The MantleThe Mantle
• Layer of rock that is denser than the crust
• About 1800 miles thick• Outer mantle is solid rock• Inner mantle the rocks
are extremely hot and bendable like gum (plastic)
![Page 6: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/6.jpg)
The CoreThe Core
• The center of the earth
• Made mostly of iron and nickel
• The inner core is solid metal while the outer core is liquid metal
![Page 7: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/7.jpg)
The Earth heats up with depthThe Earth heats up with depth
• At only 2 miles down the temperature increase to 120 F
• The core is much hotter than the mantle
• In the core, temperatures reach over 10,000 F
![Page 8: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/8.jpg)
The earth heats up with depthThe earth heats up with depth
• The earth gets warmer towards the core because it contains so many radioactive isotopes
• These unstable isotopes are constantly breaking down, releasing huge amounts of energy, which in turn heat the earth
![Page 9: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/9.jpg)
How do plates move?How do plates move?
http://www.youtube.com/watch?v=ryrXAGY1dmE
![Page 10: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/10.jpg)
Evidence #1: Evidence #1: The Pangea PuzzleThe Pangea Puzzle
• In the 20th century, Alfred Wegener noticed that eastern S.America fits into western Africa
• He also noticed that several of the other continents fit together like puzzle pieces
• He also found that fossil evidence showed that several of the same organisms are found on continents now separated by oceans
• He theorized that 250 million years ago all the continents combined to form the giant land mass he named pangea
![Page 11: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/11.jpg)
How did this happen?How did this happen?
• The earth’s outer shell, called the lithosphere is made of the crust and upper portion of the mantle.
• This lithosphere is very rigid and consists of 7 large pieces and a few small ones that fit together like a puzzle
• These large pieces are called tectonic plates
![Page 12: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/12.jpg)
Plate TectonicsPlate Tectonics• These plates fit together like puzzle pieces and
move in relation to each other• these plates move away, towards, or alongside each
other• Tectonic plates move about 6 inches per year
![Page 13: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/13.jpg)
Divergent Divergent Plate Boundaries Plate Boundaries
• In some areas, the plates move away from each other
• When this occurs, hot liquid rock called magma rises and cools, forming new lithospheric rock
![Page 14: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/14.jpg)
Convergent Convergent Plate BoundariesPlate Boundaries
• Less dense continental plate floats over more dense oceanic plate• This process is called subduction• As this more dense rock goes down into the mantle, it heats up
and melts• The magma rises and pushes up the crust, forming volcanic
mountains also earthquakes
![Page 15: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/15.jpg)
• Subduction - two plates meet, the more dense plate (oceanic crust), dives beneath the less dense plate (continental crust)
![Page 16: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/16.jpg)
Continental vs. ContinetalContinental vs. Continetal
• Same density so no subduction
• Builds non-volcanic mts.
• Earthquakes
![Page 17: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/17.jpg)
Oceanic vs. OceanicOceanic vs. Oceanic
• Similar density, but subduction anyway
• Earthquakes, trenches,
• volcanic island arcs
![Page 18: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/18.jpg)
Transform Fault BoundariesTransform Fault Boundaries
• These are areas where plates move along side one another
• As plates move, they can cause cracks in the lithosphere called faults
• As plates move along side each other at these faults, the plates cause a great deal of force and create earthquakes
![Page 19: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/19.jpg)
RECAP RECAP
• Divergent Plate Boundaries– Divergent means plates MOVE AWAY from
each other
• Convergent Plate Boundaries– Convergent means plates MOVE TOWARD
each other
• Transform Fault Boundaries– areas where plates move along side one another
• like this or this •
![Page 20: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/20.jpg)
• Earth is made of 3 main layers– Crust- cool, thin, made of rock, 10-25 miles
thick– Mantle, denser than crust, 2500 miles thick,
80% of earth’s volume: inner mantle solid rock, outer mantle bendable gummy rock
– Core- center of earth, made of iron and nickel, made of 2 layers: inner solid metal, outer liquid metal
![Page 21: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/21.jpg)
• Pangea- 250 million years ago all the continents combined to form the giant land mass called Pangea
• Lithosphere (earth’s outer shell) is made of the crust and upper portion of the mantle.
• lithosphere -very rigid and consists of 7 large pieces (called tectonic plates) and a few small ones that fit together like a puzzle
![Page 22: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/22.jpg)
• Plate Tectonics
• These plates fit together like puzzle pieces and move in relation to each other
• these plates move away, towards, or alongside each other
• Tectonic plates move 6 inches per year
![Page 23: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/23.jpg)
Evidence 2: Evidence 2: BiogeographicalBiogeographical
![Page 24: Earth’s Interior and Plate Tectonics Integrated Science Ch 12](https://reader036.vdocuments.site/reader036/viewer/2022062518/56649e685503460f94b645d1/html5/thumbnails/24.jpg)
Final viewsFinal views
• http://www.youtube.com/watch?v=QrQDXnnXOo4&feature=player_embedded#!