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Continental Drift and Sea-floor Spreading

Total questions: 10

Worksheet time: 8mins

Name
Class
Date
1.

Who proposed the theory of continental drift?

a)

Harry Hess

b)

Alfred Wegener

c)

Chasity Clary

d)

Principal O'Neal

2.

The theory of continental drift states...

a)

the continents will eventually drift off the side of Earth

b)

the continents drifted onto Earth from other planets

c)

new crust is formed at the mid-ocean ridge

d)

the continents were once one big landmass and slowly moved to where they are today

3.

What is the name of the big landmass that existed before the continents separated?

a)

Gondwana

b)

Laurasia

c)

Pangea

d)

America

4.

Which of the following is evidence of continental drift? Check all that apply.

a)

continents seem to fit together like a puzzle

b)

common fossils across the continents

c)

the sonar map of the seafloor

d)

similar rock types and mountain ranges across the continents

5.

What is the longest mountain range in the world?

a)

Mid-Atlantic Ridge

b)

Himalayas

c)

Rocky Mountains

d)

Appalachian Mountains

6.

Where is the longest mountain range in the world located?

a)

in Africa

b)

in Europe

c)

on the ocean floor

d)

on the moon

7.

The mid-ocean ridge is at what type of boundary?

a)

convergent

b)

divergent

c)

transform

d)

transverse

8.

What is created at the mid-ocean ridge?

a)

a new continent is being created there

b)

a new ocean is being formed there

c)

new islands are being created there

d)

new sea floor is created when the plates pull apart and magma bubbles up from the mantle and cools.

9.

What happens to the old sea floor?

a)

it is recycled back into the mantle at subduction zones.

b)

Nothing happens to the old crust. The Earth is actually getting larger and larger due to the contstant formation of new crust.

c)

it dissolves into the ocean

10.

True or False: Newer crust can be found closer to the Mid-Atlantic Ridge and older crust can be found further from the Mid-Atlantic Ridge.

a)

TRUE

b)

FALSE