Exam 17: Earths Interior and Geophysical Properties

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The average density of the Earth is 2.7 gm/cm3.

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Oceanic crust is _____ continental crust.

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Because _____ can be accurately calculated, the size and shape of the core can be determined.

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A cavity or body of low-density material causes a _____ pull on a gravity meter relative to average crust.

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The upper mantle consists of _______.

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Seismic tomography uses earthquake waves and computers to study cross sections of the mantle.

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Recently, geologists have been analyzing ____ generated by tidal friction, ocean waves, and storms to gain an even more detailed image of the crust and upper mantle.

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The average temperature increase in the shallow crust (the geothermal gradient) is about ______ degrees C per kilometer.

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The force of gravity between two objects decreases as the square of the distance between the objects increases.

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The Moho separates the crust from the mantle.

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One widely accepted hypothesis is that the Earth's magnetic field is created by electric currents within the ______.

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A gravity meter can be used to explore for metallic mineral deposits.

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Geologists think that the asthenosphere is molten.

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The study of ancient magnetic fields is called ____.

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The presence of an S-wave shadow zone implies that the Earth's core is liquid.

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The ____ is the transition zone at the core-mantle boundary.

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High _____ is usually an indication of a magma body or still-cooling pluton near the surface.

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The rock record for tens of millions of years indicates that the Earth's magnetic field ____.

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The boundary that separates the crust from the mantle is the ____.

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Detailed images provided by _____ suggest that the mantle is heterogeneous, probably due to variations in temperature, composition, and density.

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