L7.2 Tectonic Plate Movement Mechanisms

L7.2 Tectonic Plate Movement Mechanisms

Assessment

Interactive Video

Science

9th - 12th Grade

Medium

Created by

Georgianna Allen

Used 2+ times

FREE Resource

10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What was Alfred Wegener's primary proposal regarding continents?

That continents are fixed in their current positions.

That continents fit together like a puzzle and moved apart over time.

That continents are constantly growing in size.

That continents are slowly sinking into the ocean.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What was the main challenge Alfred Wegener faced with his continental drift theory?

He couldn't explain the composition of the continents.

He couldn't explain how the plates moved apart.

He couldn't explain the age of the continents.

He couldn't explain the types of rocks found on different continents.

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How many mechanisms have scientists proposed to explain the movement of tectonic plates?

Two

Three

Four

Five

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following is NOT one of the proposed mechanisms for tectonic plate movement?

Mantle Convection

Ridge Push

Core Expansion

Slab Pull

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to magma as it rises to the Earth's surface during mantle convection?

It becomes hotter and more dense.

It cools and sinks back down.

It solidifies and stops moving.

It evaporates into the atmosphere.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What causes the "ridge push" mechanism in plate tectonics?

The pulling force of a subducting plate.

The upward movement of cold, dense rock.

The force of newly formed, warmer, less dense rock at mid-ocean ridges pushing older, denser rock away.

The sideways movement of plates due to friction.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary force driving "slab pull" in plate tectonics?

Magnetic forces within the Earth's core.

The buoyancy of oceanic crust.

Gravity pulling a dense, subducting plate into the mantle.

The expansion of magma at mid-ocean ridges.

Create a free account and access millions of resources

Create resources

Host any resource

Get auto-graded reports

Google

Continue with Google

Email

Continue with Email

Classlink

Continue with Classlink

Clever

Continue with Clever

or continue with

Microsoft

Microsoft

Apple

Apple

Others

Others

By signing up, you agree to our Terms of Service & Privacy Policy

Already have an account?