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1 |  |  A surface separating different types of rocks is called:
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|  | A) | a chill zone. |
|  | B) | a xenolith. |
|  | C) | a contact. |
|  | D) | none of the above |
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2 |  |  The major difference between volcanic and plutonic igneous rocks is:
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|  | A) | the type of minerals they contain. |
|  | B) | where they solidify. |
|  | C) | their chemical composition. |
|  | D) | all of the above |
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3 |  |  Which is not a fine-grained rock type?
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|  | A) | granite |
|  | B) | andesite |
|  | C) | basalt |
|  | D) | rhyolite |
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 |
4 |  |  By definition, stocks differ from batholiths in:
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|  | A) | elevation above sea level. |
|  | B) | chemical composition. |
|  | C) | shape. |
|  | D) | size. |
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5 |  |  Fragments of country rock that are distinct from the body of igneous rocks in which they are enclosed: |
|  | A) | meteorites |
|  | B) | xenoliths |
|  | C) | exoliths |
|  | D) | lithographs |
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6 |  |  Which of the following minerals is part of Bowen's Continuous Series?
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|  | A) | olivine. |
|  | B) | amphibole. |
|  | C) | biotite. |
|  | D) | plagioclase feldspar. |
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 |
7 |  |  Which of the following minerals is part of Bowen's Discontinuous Series?
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|  | A) | olivine |
|  | B) | biotite |
|  | C) | pyroxene |
|  | D) | All of these are part of Bowen's Discontinuous Series. |
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8 |  |  The difference in minerals among plutonic rocks is caused by:
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|  | A) | different chemical compositions. |
|  | B) | different crystallization temperatures. |
|  | C) | magmatic differentiation. |
|  | D) | all of these. |
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9 |  |  An example of a hot spot where a hot mantle plume is currently lying at a shallow depth beneath the continental crust is:
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|  | A) | Columbia River Plateau. |
|  | B) | Hawaii. |
|  | C) | Mt. Rainier. |
|  | D) | Yellowstone National Park. |
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 |
10 |  |  Basalt is most often associated with what type of plate boundary?
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|  | A) | reversible plate boundaries |
|  | B) | convergent plate boundaries |
|  | C) | transform plate boundaries |
|  | D) | divergent plate boundaries |
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11 |  |  You discover a rock with minerals large enough to be seen containing potassium feldspar, muscovite, and quartz. This is:
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|  | A) | hornblende. |
|  | B) | granite. |
|  | C) | gabbro. |
|  | D) | diorite. |
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 |
12 |  |  Bowen's Reaction Series illustrates relations between:
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|  | A) | temperature, pressure, and viscosity. |
|  | B) | viscosity, temperature, silica content, and volatile content. |
|  | C) | temperature, chemical composition, and mineral structure. |
|  | D) | temperature, viscosity, and mineral composition. |
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 |
13 |  |  The two important criteria used for igneous rock classification are:
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|  | A) | texture and mineral composition. |
|  | B) | temperature and viscosity. |
|  | C) | mineral composition and temperature. |
|  | D) | texture and temperature. |
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 |
14 |  |  Andesite and diorite:
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|  | A) | formed from magma with the same silica content. |
|  | B) | formed from magma with the same temperature. |
|  | C) | contain the same minerals. |
|  | D) | all of these |
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 |
15 |  |  A rock with mineral crystals too small to be seen and low temperature minerals is:
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|  | A) | granite. |
|  | B) | andesite. |
|  | C) | rhyolite. |
|  | D) | gabbro. |
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 |
16 |  |  Igneous rocks that form entirely beneath Earth's surface are said to be:
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|  | A) | platonic. |
|  | B) | plutonic |
|  | C) | extrusive. |
|  | D) | volcanic. |
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 |
17 |  |  Andesite was named for a rock type commonly found:
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|  | A) | in Mayberry, North Carolina. |
|  | B) | in the Andes Mountains. |
|  | C) | in Hawaii. |
|  | D) | in the Rocky Mountains. |
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 |
18 |  |  Igneous processes are those which relate to:
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|  | A) | solidification of magma. |
|  | B) | formation of magma. |
|  | C) | melting of rocks. |
|  | D) | all of these |
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 |
19 |  |  The geothermal gradient of the asthenosphere is:
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|  | A) | always changing as a result of plate tectonics. |
|  | B) | the reverse of the geothermal gradient in the lithosphere. |
|  | C) | less than that of the lithosphere. |
|  | D) | the same as the temperature structure of the lithosphere. |
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 |
20 |  |  Volcanic rocks are ALL:
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|  | A) | Explosive. |
|  | B) | Extrusive. |
|  | C) | Plutonic. |
|  | D) | Intrusive. |
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