Convection Currents and Seafloor Spreading

Quiz
•
Science
•
8th Grade
•
Hard
+1
Standards-aligned
Lisa Thompson
FREE Resource
25 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
The image shows a mid ocean ridge. What is an important feature of seafloor spreading?
Mid ocean ridges only occur at convergent boundaries.
The convection currents in the core drive the plates apart.
As the plates pull apart, the lava rises to form new crust.
Tags
NGSS.MS-ESS2-1
2.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
In the Atlantic ocean, where is the youngest seafloor located?
Towards the edges, near the eastern and western continents
Towards the middle of the ocean at the mid-ocean ridge
Towards the north and south poles
Young seafloor is located randomly throughout the ocean
Tags
NGSS.MS-ESS2-3
3.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Why does the ocean floor sink beneath the continent at Z?
The ocean floor is less dense than the continent.
The ocean floor is more dense than the continent.
The ocean floor is moving faster than the continent.
The ocean floor is moving slower than the continent.
Tags
NGSS.MS-ESS2-3
4.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Which of the following causes Earth's tectonic plates to move?
Energy from the Sun
Magnetic Pole Reversal
Convection currents in the mantle
Faults in Mountain Ranges
Tags
NGSS.MS-ESS2-3
5.
DROPDOWN QUESTION
1 min • 1 pt
According to the hypothesis of seafloor spreading, molten rock is rising up along the (a)
mid-ocean ridge
deep-sea trench
Tags
NGSS.MS-ESS2-3
6.
MULTIPLE CHOICE QUESTION
1 min • 1 pt
Seafloor spread occurs because....
Plates are smashing together and oozing apart
Magma below the Earth's crust is forced up toward the surface after plates move apart
Maui is trying to break out of his prison
The Earth's magnetic poles are reversing
Tags
NGSS.MS-ESS2-2
NGSS.MS-ESS2-3
7.
MULTIPLE CHOICE QUESTION
1 min • 5 pts
The process that creates new seafloor as plates move away from each other at the mid-ocean ridges
stressing
seafloor spreading
subduction
shearing
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