plate tectonics
DESCRIPTION
Plate Tectonics. Sea Floor Spreading. Crustal Features. Vocabulary. Plate Boundaries. $100. $100. $100. $100. $100. $200. $200. $200. $200. $200. $300. $300. $300. $300. $300. $400. $400. $400. $400. $400. $500. $500. $500. $500. $500. by: Rebecca McCown. - PowerPoint PPT PresentationTRANSCRIPT
![Page 1: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/1.jpg)
PlateTectonics
PlateBoundarie
s
Sea FloorSpreading
Crustal Features
Vocabulary
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$500 $500 $500 $500 $500by: Rebecca McCown
![Page 2: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/2.jpg)
A. Convection currents of magma in the Earth’s mantle.
![Page 3: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/3.jpg)
C. The Lithosphere – the Earth’s crust that is broken up into huge pieces.
![Page 4: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/4.jpg)
C. At plate tectonic boundaries
![Page 5: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/5.jpg)
C. Asthenosphere
![Page 6: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/6.jpg)
C. A Hot Spot
![Page 7: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/7.jpg)
B. Convergent
![Page 8: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/8.jpg)
A.Divergent
![Page 9: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/9.jpg)
C. Transform boundary
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A. Divergent Boundaries
![Page 11: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/11.jpg)
B. Convergent Boundary
![Page 12: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/12.jpg)
A. Mid-Ocean Ridges
![Page 13: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/13.jpg)
B. They’ll move further apart
![Page 14: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/14.jpg)
C. Sea Floor Spreading
![Page 15: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/15.jpg)
D. Furthest away from the ridge
![Page 16: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/16.jpg)
A. California is located on a plate boundary where plates slide past each other. The San Andreas Fault is a transform boundary.
![Page 17: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/17.jpg)
B. Rift Valley
![Page 18: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/18.jpg)
D. Trench
![Page 19: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/19.jpg)
C. Volcano
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A.Mountain Range
The Himalaya Mountain Range formed because India is
crashing into Asia
![Page 21: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/21.jpg)
B. A Mid Ocean Ridge
![Page 22: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/22.jpg)
D. Sea Floor Spreading
![Page 23: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/23.jpg)
A. Subduction Zone
![Page 24: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/24.jpg)
C. Convection Currents
![Page 25: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/25.jpg)
B. Fault Lines
![Page 26: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/26.jpg)
D. Volcanoes – Magma is coming up at mid-ocean ridges and forming new sea floor. This forms volcanoes all along the mid-ocean ridges.
![Page 27: Plate Tectonics](https://reader035.vdocuments.us/reader035/viewer/2022062217/56814d4f550346895dba8210/html5/thumbnails/27.jpg)
Final Jeopard
y