Exam 2: Internal Structure of Earth and Plate Tectonics

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Compare and contrast the mantle and crust.

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The crust is the outermost layer of the solid Earth and the mantle lies below the crust and above the outer core.The mantle is nearly 3000 km thick and consists mostly of soft plastic to solid material composed of Fe and Mg-rich silicate minerals with a density of 4.5 g/cm3.The crust is composed of cooler solid rock material,is only several km thick (max.4 km)and is much less dense - 2.8 g/cm3.This density contrast defines their boundaries as marked by the Mohorovicic discontinuity,or Moho.

What would be the correct relationship between the crust and the lithosphere?

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A

Which of the following is TRUE about plate tectonics?

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D

The Hawaiian Islands are an example of

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Which of the following statements about the lithosphere is FALSE?

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Describe the three types of plate boundaries.Identify the types of associated hazards and explain how they are generated.

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The Wadati-Benioff Zone marks the boundary between crust and mantle.

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What is paleomagnetism?

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The Hawaiian emperor chain of volcanic islands are a result of a mantle hotspot that is migrating in an easterly trajectory.

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What is plate tectonics?

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Give a description of the lithosphere,crust,asthenosphere,and mantle and explain the relationships between them.

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The crust of the earth is considered the thinnest layer of the earth.

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The inside of the Earth is composed of layers that have different properties.

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Scientists believe that the inner core of the Earth is

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Briefly describe the Wadati-Benioff Zone.

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The energy for plate tectonics comes from

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At 3000 km thickness,the mantle is the thickest section in the interior of the Earth.

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Explain the concept of convection.Describe how convection may work in the mantle of the Earth.

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Which of the following,forms the thickest layer on the interior of the earth?

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Geologists have samples of rock from the Earth's core.

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