Deforming the Earth's Crust

Quiz
•
Science
•
6th Grade
•
Hard
+4
Standards-aligned

Vicki Gripp
Used 309+ times
FREE Resource
20 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
stress
the process by which the shape of a rock changes because of stress
the amount of force per square unit area on a given material
stress that occurs when an object is stretched
stress that occurs when an object is squeezed
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
deformation
the process by which the shape of a rock changes because of stress
the amount of force per square unit area on a given material
stress that occurs when an object is stretched
stress that occurs when an object is squeezed
Tags
NGSS.MS-PS2-2
NGSS.MS-PS2-5
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
compression
the process by which the shape of a rock changes because of stress
the amount of force per square unit area on a given material
stress that occurs when an object is stretched
stress that occurs when an object is sqeezed
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
tension
the process by which the shape of a rock changes because of stress
the amount of force per square unit area on a given material
stress that occurs when an object is stretched
stress that occurs when an object is squeezed
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
folding
both ends of a fold in the Earth's crust are horizontal
downward, trough-like folds in the Earth's crust
upward-arching folds in the Earth's crust
the bending of rock layers because of stress in the Earth's crust
Tags
NGSS.MS-ESS2-2
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
anticlines
both ends of a fold in the Earth's crust are horizontal
downward, trough-like folds in the Earth's crust
upward-arching folds in the Earth's crust
the bending of rock layers because of stress in the Earth's crust
Tags
NGSS.HS-ESS2-1
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
synclines
both ends of a fold in the Earth's crust are horizontal
downward, trough-like folds in the Earth's crust
upward-arching folds in the Earth's crust
the bending of rock layers because of stress in the Earth's crust
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