This summative assessment will evaluate your knowledge of Plate Techtonics. Vocabulary, essential questions and concepts will be assessed.
Continental crust
Oceanic crust
Both continental and oceanic crust
Mesosphere
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True
False
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Like a layer cake
Like a jigsaw puzzle
Like a stack of books
Like a model car
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Divergent
Convergent
Transform-fault
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True
False
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Hanging wall
Fault
Footwall
Compression
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Transform fault
Convergent
Divergent
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Drift
Uplift
Bending
Stress
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Divergent boundary
Convergent boundary
Transform fault boundary
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Seismic waves
Sonar
Information from drilling expeditions
Ocean waves
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Mantle
Core
Aesthenosphere
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Transform fault boundary
Divergent boundary
Convergent boundary
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Older
Younger
Darker in color
Prettier
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5 inches per year
50 inches per year
5 centimeters per year
50 centimeters per year
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True
False
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No new magma is formed
Transform boundaries tend to be cooler than convergent boundaries
The oceanic crust is thicker than continental crust
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The asthensophere is divided into plates
The lithosphere is divided into plates
The asthenosphere moves over the lithosphere
The asthenosphere is strong and rigid
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The crust and uppermost mantle
The oceanic and continental crust only
The crust and entire mantle
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Clinometers
Global positioning systems (GPS)
Telescopes
Seismographs
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Oceanic crust is thinner
Oceanic crust has more iron
Oceanic crust has a higher density.
Oceanic crust is older than continental crust
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Seafloor spreading
Subduction
New volcano being formed
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Divergent
Transform-fault
Convergent
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Transform-fault
Convergent
Divergent
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Seafloor spreading
Mid-ocean ridge
Older rocks are at the extreme left and right away from the ridge
The magnetic poles of the ocean crust have reversed several times
This is a convergent boundary
This is a divergent boundary
This is a transform-fault boundary
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