Weathering Review
Quiz
•
Science
•
1st - 5th Grade
•
Practice Problem
•
Medium
Standards-aligned
Max Rosenfeld
Used 2+ times
FREE Resource
Enhance your content in a minute
11 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
15 mins • 1 pt
These rocks were broken apart from the continuous freeze/thaw of water in the cracks of the rocks. This is an example of:
frost wedging
acid rain
wind weathering
river flowing over and smoothing out the rock
Answer explanation
Frost wedging takes small cracks in rocks and expands them. Each time the ice forms it makes the crack larger.
Frost wedging creates “cracked” rocks as well as destroys roads in many cold climates around the world.
2.
MULTIPLE CHOICE QUESTION
15 mins • 1 pt
How does freezing water cause the weathering of rocks? The freezing water—
Tags
NGSS.MS-ESS2-2
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
The diagrams shows a natural process that weathers rock.
Which statement best explains why this process results in weathering?
Tags
NGSS.MS-ESS2-1
NGSS.MS-ESS2-2
NGSS.MS-ESS2-4
4.
MULTIPLE CHOICE QUESTION
15 mins • 1 pt
__________ is the wearing away or slow breaking apart of rock into smaller pieces.
erosion
earthquakes
deposition
weathering
Tags
NGSS.MS-ESS2-2
5.
FILL IN THE BLANK QUESTION
15 mins • 1 pt
_ is the process of weathered particles moving from one location to another
6.
FILL IN THE BLANK QUESTION
1 min • 1 pt
_ is the process of rocks, sediments and other materials being deposited or settle in a new location due to water, wind, and ice.
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Scientist have theorized that the Kummakivi Balancing Rock resulted from
Through glacial deposition, as the two rocks were balanced on top of one another as glaciers melted.
Through water weathering as the two rocks were previously one, and through rain the middle was broken down and over time two rocks were formed.
Through wind erosion, as strong gust of winds were able to pick up the Kummakivi rock and drop it on top of the bottom rock.
Answer explanation
Large glaciers can move boulders and deposit them in new places.
During the last Ice Age glacial boulders were moved hundreds of mile.
Balancing rocks are usually a boulder that travelled on top of a glacier and deposited in an awkward position
Create a free account and access millions of resources
Create resources
Host any resource
Get auto-graded reports

Continue with Google

Continue with Email

Continue with Classlink

Continue with Clever
or continue with

Microsoft
%20(1).png)
Apple
Others
By signing up, you agree to our Terms of Service & Privacy Policy
Already have an account?
Similar Resources on Wayground
15 questions
Animals wild and domestic
Quiz
•
2nd Grade
12 questions
Mythical Creatures: Big Foot
Quiz
•
3rd Grade
10 questions
Means of Transportation
Quiz
•
1st - 2nd Grade
13 questions
F3 electricity
Quiz
•
3rd Grade
13 questions
FORCE, WORK , AND ENERGY
Quiz
•
3rd Grade
10 questions
Soil Erosion
Quiz
•
5th Grade
12 questions
Magnets
Quiz
•
4th Grade
15 questions
Food
Quiz
•
2nd Grade
Popular Resources on Wayground
10 questions
Honoring the Significance of Veterans Day
Interactive video
•
6th - 10th Grade
10 questions
Exploring Veterans Day: Facts and Celebrations for Kids
Interactive video
•
6th - 10th Grade
19 questions
Veterans Day
Quiz
•
5th Grade
25 questions
Multiplication Facts
Quiz
•
5th Grade
15 questions
Circuits, Light Energy, and Forces
Quiz
•
5th Grade
6 questions
FOREST Self-Discipline
Lesson
•
1st - 5th Grade
7 questions
Veteran's Day
Interactive video
•
3rd Grade
20 questions
Weekly Prefix check #2
Quiz
•
4th - 7th Grade
Discover more resources for Science
15 questions
Circuits, Light Energy, and Forces
Quiz
•
5th Grade
19 questions
Energy, Electricity,Conductors and Insulators
Quiz
•
4th Grade
20 questions
Physical and Chemical Changes
Quiz
•
5th Grade
10 questions
Conductors and Insulators
Quiz
•
4th Grade
22 questions
Light Energy
Quiz
•
5th Grade
20 questions
Weather vs. Climate
Quiz
•
5th Grade
17 questions
Animal and Plant Cells
Quiz
•
5th Grade
10 questions
MOY review 4th grade
Quiz
•
4th Grade
