Plate Tectonics

Plate Tectonics

7th Grade

35 Qs

quiz-placeholder

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Plate Tectonics

Plate Tectonics

Assessment

Quiz

Science

7th Grade

Hard

NGSS
MS-ESS2-3, MS-ESS2-2, MS-ESS2-1

+4

Standards-aligned

Created by

Amanda Gunnell

Used 28+ times

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35 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where in Earth do convection currents happen?

In the mantle.

Inner core.

At the crust.

Outer core.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

At some plate boundaries, one of the tectonic plates moves under the other plate.


What is this process called?

Reduction.

Subduction.

Convection.

Induction.

Tags

NGSS.MS-ESS2-3

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Movement of Earth's tectonic plates appears to be caused by...

light from the moon.

temperature differences in Earth’s inner core.

temperature differences in Earth’s mantle.

light from the sun.

Tags

NGSS.MS-ESS2-3

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of these is most responsible for the motion of the tectonic plates that make up Earth's crust?

Light from the moon.

Light from the sun.

Temperature differences in Earth’s mantle.

Temperature differences in Earth’s inner core.

Tags

NGSS.MS-ESS2-3

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a tectonic plate?

A large chunk of the ocean floor.

A large chunk of crust and upper mantle.

A large chunk of the lower mantle.

A large chunk of Earth below a continent.

Tags

NGSS.MS-ESS2-2

NGSS.MS-ESS2-3

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the difference between continental crust and oceanic crust?

Continental crust is thinner.

Oceanic crust moves easily. Continental crust does not move.

Continental crust moves easily. Oceanic crust does not move.

Oceanic crust is thinner.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

In a convection cell, what happens at the lower mantle?

Rock gets warmer and stays at the same level.

Rock gets colder and rises.

Rock gets colder and stays at the same level.

Rock gets warmer and rises.

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