Exam 8: The Moon and Mercury: Scorched and Battered Worlds

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Explain how crater counts allow us to estimate the ages of surfaces throughout the solarsystem.

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Almost all we know about Mercury has come from:

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Mercury's smooth plains are most similar to the Moon's:

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The average rate of erosion on the Moon is far less than on Earth because:

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Mercury and the Earth have about the same average density, but Mercury's core is muchlarger, compared to the size of the body.

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Which of these would support the capture theory of the Moon's origin?

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The cores of both Mercury and the Moon consist of solid inner cores surrounded by fluidouter cores.

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Few of the Moon's craters are actually due to volcanism, as was widely thought prior toApollo.

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Caloris is well named, for at every perihelion, it faces the Sun directly.

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A major surprise from space exploration is that ________ exists at the poles of both Mercuryand our Moon.

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From Earth, due to their motions and the fact that the Sun lights only a portion of eachsurface, both Mercury and the Moon:

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The hollows on Mercury are:

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What are the major factors that rule out the co-formation theory for the Moon-Earth system?

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Mercury is very hard to observe from Earth because:

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Which side of the Moon has the thicker crust? Why?

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The high eccentricity of Mercury's orbit probably has nothing to do with Mercury's 3:2 synchof rotation and revolution.

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Why has Mercury traditionally been such a hard planet to observe and study?

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To measure how Mercury spins, astronomers sent ________ to Mercury and used theDoppler shift to determine how fast it was rotating.

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Compare and contrast the interiors of the Moon and Mercury, including how these featuresformed.

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Relate the formation of Mercury's scarps to its differentiation.

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