
Ocean Floor Features
Quiz
•
Science
•
Professional Development
•
Hard
Standards-aligned
Allison Harig
FREE Resource
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9 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the ocean floor like?
Flat and featureless
Full of mountains and valleys
Covered in sediment
Similar to the surface of the moon
Tags
NGSS.MS-ESS2-3
2.
MULTIPLE SELECT QUESTION
30 sec • 1 pt
How do scientists gather information about the ocean floor?
By traveling to the ocean floor in specialized vessels
By using radio and infrared telescopes
By reflecting sound waves off the bottom of the ocean
By studying underwater volcanoes
Tags
NGSS.MS-ESS2-3
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What causes the topography of the ocean floor to change?
Earthquakes
Plate tectonics
Underwater volcanoes
Tsunamis
Tags
NGSS.MS-ESS2-2
NGSS.MS-ESS2-3
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is formed when two ocean plates move away from each other?
A ridge
A trench
A seamount
A hot spot
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the Mariana Trench?
A deep crack in the ocean floor
A ridge formed by plate movement
A volcano formed at a subduction zone
The deepest part of the ocean
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Where do hot spots occur?
At divergent plate boundaries
At subduction zones
At the edge of the continental shelf
In the middle of tectonic plates
Tags
NGSS.HS-ESS2-3
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are seamounts?
Underwater mountains formed by plate movement
Flat regions of the ocean floor
Volcanoes that form away from plate boundaries
Underwater trenches formed by subduction
8.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the continental shelf?
A large flat region of the ocean floor
The site of sediment build-up
The portion of the continent underwater
The beginning of the continental rise
9.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the continental slope?
A sudden increase in depth at the edge of the continental shelf
A large flat region of the ocean floor
The site of sediment build-up
The beginning of the continental rise
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