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Wehling
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NATS 1003
Syllabus
Topic Outlines
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Topic
15 Large Scale Surface Relief
Topics
15.1 Why are
continents high and oceans low?
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Compare: Compare the general elevations of ocean crust and continental
crust
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Term: isostasy
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Analytical: Compare how objects of the same mass and different materials
float in water
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Analytical: Compare how objects of the same density and different mass
float in water
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Explanation: Using the information of the objects floating in water,
explain why ocean crust is lower and continental crust is higher
15.2 Isostasy
and geologic processes
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Explanation: How do compression forces affect the height and thickness
of the crust?
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Explanation: How do extension forces affect the height and thickness of
the crust?
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Explanation: How does erosion affect the height of the crust?
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Explanation: How does deposition affect the height of the crust?
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Explanation: How does the crust under a glacier and near the glacier
respond when the glacier melts/retreats?
15.3 What
causes sea level changes?
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Explanation: How does the amount of glaciers on the Earth affect sea
level?
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Explanation: How does the total area of ocean basins on the Earth affect
sea level? How does the total area of ocean basins change?
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Explanation: How does the average age of ocean lithosphere on the Earth
affect sea level? How does the average age of ocean lithosphere change?
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