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Crustal Deformation

Authored by Ashley Elaine

Science

9th Grade - University

NGSS covered

Used 10+ times

Crustal Deformation
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20 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

Media Image

What type of structure is shown in this photograph?

anticline

monocline

syncline

reverse fault

2.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

Media Image

For the fault indicated in the figure, which side is the hanging wall?

Neither A nor B is the hanging wall.

Both A and B are hanging walls.

A is the hanging wall.

B is the hanging wall.

3.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

Media Image

What type of stress formed the structure shown in this figure?

compression

tension

confining pressure

fluid pressure

Tags

NGSS.MS-ESS2-2

4.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

How does a monocline form?

A monocline forms due to tensile stresses when rocks are beginning to flow.

A monocline forms when sedimentary rocks drape above a fault.

A monocline forms under compressional stresses when rocks are just beginning to fold.

A monocline forms as the connection between a syncline and an anticline.

5.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

Media Image

What type of structure is shown in this photograph?

Ayncline

Reverse fault

Normal fault

Joint

Tags

NGSS.HS-ESS1-5

6.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

Media Image

What type of a structure is shown in this figure?

Plunging anticline

Normal fault

Plunging syncline

syncline

7.

MULTIPLE CHOICE QUESTION

30 sec • 5 pts

What is the difference between “joints” and “faults” in rocks?

Faults form first but if the deformation continues, then joints will begin to form in the rock to show that the rock unit is about to break apart entirely.

Joints are fractures that form due to brittle expansion or stretching of rocks, while faults are fractures where the rocks on one side have moved relative to the other side due to many different types of stresses.

Faults are fractures that form due to brittle expansion or stretching of rocks, while joints are fractures where the rocks on one side have moved relative to the other side due to many different types of stresses.

The terms describe the same thing.

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