
Earth's Changing Surface [Types of Faults and Formations]
Authored by Lorraine Montiel
Science
11th - 12th Grade
NGSS covered
Used 41+ times
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17 questions
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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
Tags
NGSS.HS-ESS1-5
NGSS.HS-ESS2-1
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.
Tags
NGSS.HS-ESS1-5
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.
Tags
NGSS.HS-ESS1-5
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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