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Earth's Changing Surface [Types of Faults and Formations]

Authored by Lorraine Montiel

Science

11th - 12th Grade

17 Questions

NGSS covered

Used 37+ times

Earth's Changing Surface [Types of Faults and Formations]
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1.

MULTIPLE SELECT QUESTION

45 sec • 1 pt

The amount of stress determines the type of fault that forms, and we usually categorize that sense of stress in three different ways, select the 3-types of stress categories

Compression

Sheer

Tension

Reverse uplift

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Tensional stress happens at _______ plate boundaries

Convergent

Transfrom

Divergent

Slip-Strike

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Compressive stress happens at ________ plate boundaries

Convergent

Divergent

Transform

Subduction

Tags

NGSS.HS-ESS1-5

NGSS.HS-ESS2-1

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Shear stress is experienced at _______ boundaries; also known as strike-slip faults.

Convergent

Divergent

Transform

Subduction

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a reverse fault?

When compressive stress is applied, squeezing and shortening the terrain

When tension is applied, pulling and elongating. If this material were ductile, it would stretch and get thinner, but brittle rocks will break instead

A strike-slip fault, they don't move in a vertical motion. They are formed horizontal shear stress.

It's your fault, not mine.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is considered a "normal fault"

A strike-slip fault, they don't move in a vertical motion. They are formed horizontal shear stress.

When tension is applied, pulling, and elongating. If this material were ductile, it would stretch and get thinner, but brittle rocks will break instead

When compressive stress is applied, squeezing, and shortening the terrain

Ok, it's my fault not yours.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the Elastic Rebound Theory?

The study of earthquakes

There is energy stored in an object when it is under temporary strain

Potential energy will change to kinetic energy.

Theory that rocks that are strained past a certain point will either fracture, spring back to their original shape or deform in shape.

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