During the eighteenth and nineteenth centuries, the \"contracting Earth model\"
ID: 298414 • Letter: D
Question
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 27 (1 point)
...the presence of mountain belts.
Question 27 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 28 (1 point)
...the match of mountain belts across continents.
Question 28 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 29 (1 point)
...the fit of the continents.
Question 29 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 30 (1 point)
...paleoclimate data.
Question 30 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 31 (1 point)
...the location of volcanoes and earthquakes.
Question 31 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
During the eighteenth and nineteenth centuries, the "contracting Earth model" hypothesis attempted to explain the origins of Earth's physical features by assuming that the Earth has been slowly cooling and contracting since its formation. A few scientists still supported the contracting Earth model when Alfred Wegener proposed his continental drift hypothesis in the early twentieth century. While both hypotheses were able to explain the origins of some of the Earth's physical features, they both had limitations as well.
Determine which of the two hypotheses would be able to explain...
Question 32 (1 point)
...why the continents move.
Question 32 options:
Contracting Earth model only
Continental drift hypothesis only
Both the contracting earth model and continental drift hypothesis
Neither the contracting earth model nor the continental drift hypothesis
Save
Question 33 (1 point)
Where are the youngest rocks found on the seafloor?
Question 33 options:
Trenches
Mid-ocean ridges
Along coastlines
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Question 34 (1 point)
At what location is heat flow the greatest?
Question 34 options:
Near oceanic ridges.
New oceanic trenches.
Near transform boundaries.
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Question 35 (1 point)
What happens to the age of the seafloor rocks moving away from a mid-ocean ridge?
Question 35 options:
The rocks get younger.
The rocks get older.
The rock ages do not change.
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Question 36 (1 point)
When it was first proposed, Alfred Wegener's continental drift hypothesis was heavily criticized by earth scientists. What was one of their primary objections to the continental drift hypothesis?
Question 36 options:
Wegener couldn't explain the worldwide distribution of fossil species.
Wegener falsified some of his data to better fit his hypothesis.
Wegener did not offer an explanation for how the continents move.
The continents did not fit together as well as Wegener initially claimed.
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Question 37 (1 point)
What is the proper order of Earth's compositional layers from the interior to the surface?
Question 37 options:
Crust, mantle, core
Mantle, core, crust
Core mantle, crust
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Question 38 (1 point)
What technology allows scientists to precisely measure plate motions?
Question 38 options:
Global seismometers
Global satellite imagery
Global positioning system
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Question 39 (1 point)
The magnetic North Pole migrated northward from 1902-2002. How did magnetic inclination readings in the continental United States change during that period?
Question 39 options:
Inclination became steeper (moved towards the vertical)
Inclination became less steep (moved towards the horizontal)
Inclination remained constant
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Question 40 (1 point)
Which two ideas were combined to form the theory of plate tectonics?
Question 40 options:
Continental drift and Big Bang
Continental drift and the scientific process
Continental drift and seafloor spreading
A)Contracting Earth model only
B)Continental drift hypothesis only
C)Both the contracting earth model and continental drift hypothesis
D)Neither the contracting earth model nor the continental drift hypothesis
Explanation / Answer
27)...the presence of mountain belts.
Answer is: B
Continental drift hypothesis only
Explanation:
Wegener use to support the hypothesis of continental drift observation as Mountain belts match across continental margins.
40) Which two ideas were combined to form the theory of plate tectonics?
Answer is:
c) Continental drift and seafloor spreading
Explanation:
By combining the sea floor spreading theory with continental drift and information on global seismicity, the new theory of Plate Tectonics became a coherent theory to explain crustal movements.
Wegener use to support the hypothesis of continental drift observation as Mountain belts match across continental margins.
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