The Development of Plate Tectonics

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Physics, Science, Geography
•
11th Grade - University
•
Hard
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7 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What was Alfred Wegener's major contribution to the theory of plate tectonics?
He explained the process of subduction.
He developed the concept of mantle plumes.
He proposed the existence of a supercontinent called Pangaea.
He discovered the mid-ocean ridges.
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How did the study of magnetic minerals contribute to the understanding of plate tectonics?
It helped reconstruct Earth's magnetic field over time.
It proved the existence of Pangaea.
It revealed the presence of underwater volcanoes.
It showed that Earth's magnetic field is constant.
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What did World War II sonar mapping reveal about the ocean floor?
It was covered with thick layers of sediment.
It was entirely composed of basalt.
It contained mountain ridges, trenches, and volcanoes.
It was a flat, featureless plain.
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
According to Harold Hess, what happens to oceanic crust at mid-ocean ridges?
It sinks into the mantle.
It is created and spreads out laterally.
It remains stationary.
It is destroyed by subduction.
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What evidence supported Hess's theory of oceanic crust formation?
The constant position of magnetic poles.
The discovery of magnetic striping.
The presence of thick sediment layers.
The alignment of volcanic islands.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How are seamounts like the Hawaiian Islands formed according to J. Tuzo Wilson?
Due to volcanism from stationary mantle plumes.
By the collision of tectonic plates.
Through the process of subduction.
By the accumulation of sediment.
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the role of transform faults along mid-ocean ridges?
They create new oceanic crust.
They connect ridge segments and accommodate spreading rate changes.
They are sites of intense volcanic activity.
They are responsible for the formation of seamounts.
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