Plate Tectonics 3

Plate Tectonics 3

Assessment

Assessment

Created by

Patti Greenfield

Other Sciences

6th - 8th Grade

Hard

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20 questions

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1.

Multiple Choice

1 min

12 pts

The movement of the tectonic plates is caused by

the rotation of the Earth.

convection currents in the Asthenosphere

the gravity of the iron-nickel core.

the Moho discontinuity.

2.

Multiple Choice

20 sec

12 pts

In some areas of the world, like California and Japan, earthquakes are a common occurrence. How can this best be explained?

The strong ocean currents are undermining both areas causing earthquakes.

Both areas are located near the edge of the Pacific Ocean, the unstable sand causes earthquakes.

Both areas are subjected to strong ocean wind and waves that causes earthquakes.

Both areas are on the boundary of active plates, the motion of the plates causes earthquakes.

3.

Multiple Choice

20 sec

12 pts

Media Image

Subduction zones occur on Earth where dense oceanic crust dives under more buoyant continental crust. These boundaries are characterized by a deep ocean trench next to a high continental mountain range, large numbers of earthquakes and volcanoes. All of this is further evidence for the

big bang theory.

theory of plate tectonics.

origin of the species.

theory of natural selection.

4.

Multiple Choice

20 sec

12 pts

There are three types of plate boundaries. Which choice is NOT a type of plate boundary?

convergent

thrust

divergent

transform

5.

Multiple Choice

30 sec

1 pt

Media Image

Observe this diagram of a plate boundary. One statement BEST describes what is happening. It is that

the oceanic crust is melting.

the denser ceanic crust is subducting under the less dense oceanic crust

volcanic islands are forming.

the tectonic plates are moving away from each other.

6.

Multiple Choice

20 sec

1 pt

Media Image

The map in the picture shows tectonic plate boundaries. This map would be useful in predicting the location of future

droughts

hurricanes

earthquakes

tornadoes

cartoon woman

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