Exam 3: Earth Structure and Plate Tectonics

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The outermost solid layer of the Earth that comprises both continental and oceanic crust is called the:

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What do these things have in common: Paleomagnetism, seafloor spreading, Pangaea, Wadati-Benioff zones, transform faults, fracture zones, seamount chains, Pacific hotspots.

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One cubic meter of which of these would weigh the most?

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A boundary in which crustal plates move past one another is called a:

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If two oceanic plates collide at a relatively fast speed, and one is much older and cooler (therefore more dense) than the other, what will happen?

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The hot, partially melted, slowly flowing layer of the earth is called the:

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The Emperor Seamounts were formed:

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Evidence for plate tectonics can be seen in:

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A "mystery" in our understanding of plate tectonics has been, until recently, the nature of the power source capable of moving the plates and the continents embedded within them. Recent evidence indicates the power source to be:

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One piece of evidence that suggests the existence of Pangaea is continuous mountain ranges spanning Australia and Antarctica.

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The oceanic crust is made of basalt.

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The asthenosphere is cooler than the lithosphere.

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The Hawaiian Islands were formed within the last 2 million years under a hot spot that is now inactive.

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Oceanographers believe the breakup of Pangaea occurred about:

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New crust is being generated:

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Buoyancy is the ability of an object to float in a fluid by:

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Why is the inside of the Earth still hot?

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The youngest seafloor rocks are found:

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With the use of radiometric dating, one would expect to find the OLDEST rock to be found:

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Using the Atlantic ocean basin as an example, describe in detail how an ocean basin is formed.

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