Essentials of Oceanography 7th Edition by Tom S. Garrison – Test Bank
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Sample Test
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Chapter 03 Indicate whether the statement is true or false. |
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1. Transform faults
are never found at mid-ocean ridges.
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2. There are two types
of plate divergences: divergent oceanic crust and divergent continental
crust.
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3. Convection within
the inner core facilitates continental drift.
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4. Subduction zones
are areas where new seafloor is created.
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5. The asthenosphere
is cooler than the lithosphere.
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6. Density is a
measure of relative heaviness and is defined as mass per unit volume.
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7. The oceanic crust
is primarily made of basalt.
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8. One piece of
evidence that suggests the existence of Pangaea is the discovery of Mesosaurus fossils
in Argentina and Africa, but nowhere else.
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9. The Hawaiian
Islands were formed within the last 2 million years above a hot spot that is
now inactive.
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10. Alfred Wegener was
a polar explorer who suggested that at one time, Earth’s landmasses were
joined into a supercontinent called Pangaea.
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Indicate the answer choice
that best completes the statement or answers the question. |
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11. Geologists believe
that a new ocean basin is forming ____.
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12. Earlier than 200
million years ago, the continents were joined into one supercontinent called
____.
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13. With the
development of radiometric dating, scientists discovered that the oldest
rocks were typically ____.
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14. A cross section of
Earth reveals a layered structure that has different thicknesses and
densities. How do geologists know this?
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15. The Himalayan
Mountains were formed as a result of ____.
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16. What are the
primary components in Earth’s continental crust?
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17. Japan is located
along the Pacific Ring of Fire and experiences many earthquakes. Almost all
of the earthquakes around Japan occur ____.
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18. One cubic meter of
which of these would weigh the most?
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19. The rigid outer
layer of Earth that comprises both continental and oceanic crust is called
the ____.
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20. The magnetic
striping of the seafloor is considered evidence of seafloor spreading and
____.
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21. The mid-ocean
ridges are ____.
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22. California’s San
Andreas fault is which type of plate boundary?
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23. Roughly how fast
do most lithospheric plates move?
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24. Which statement
with regard to hot spots is true?
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25. New crust is being
generated ____.
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26. The largest known
mantle plume is located beneath ____.
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27. What is the
primary reason for the inside of Earth being hot?
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28. A boundary in
which crustal plates slide laterally past one another is called a ____.
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29. About how many
kilometers (miles) is it from the center of Earth to the outer edge of the
outer core?
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30. Which statement is
true with regard to subduction zones?
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31. Scientists believe
the breakup of Pangaea occurred about ____.
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32. Some plateaus,
ocean ridges, ancient island arcs, and parts of continental crust are too
buoyant to be subducted. These are, instead, squeezed and sheared onto the
face of a continent, forming ____.
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33. The youngest
seafloor rocks are found ____.
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34. The Hawaiian
Islands formed as they pass over a hot spot in the middle of the ____.
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35. As early as the
1700s, scientists and observers noticed a remarkable coincidence of shape of
the Atlantic coasts of Africa and ____.
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36. Buoyancy is the
ability of an object to float in a fluid by ____.
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37. The ____ accounts
for 83% of Earth’s volume.
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38. 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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39. If two oceanic
plates collide and one is older and cooler (therefore more dense) than the
other, what will happen?
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40. The hot, partially
melted, slowly flowing layer of Earth is called the ____.
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41. What kind of observational
evidence did Alfred Wegener use to propose his theory of continental drift,
and the idea that the continents were once connected as the single landmass,
Pangaea? |
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42. What is plate
convergence and what types of features are produced from convergence? |
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43. How has the
history of plate movement been captured in residual magnetic fields? |
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44. Using the Atlantic
Ocean as an example, describe in detail how an ocean basin is formed. |
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45. Describe the
mechanism that controls the formation of the Hawaiian Islands. Is this island
chain still actively forming? |
Answer Key
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1. False |
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2. True |
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3. False |
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4. False |
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5. False |
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6. True |
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7. True |
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8. True |
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9. False |
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10. True |
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11. a |
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12. a |
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13. d |
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14. c |
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15. b |
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16. c |
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17. a |
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18. d |
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19. b |
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20. d |
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21. c |
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22. b |
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23. d |
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24. a |
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25. c |
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26. b |
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27. b |
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28. a |
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29. b |
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30. d |
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31. c |
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32. b |
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33. b |
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34. d |
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35. d |
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36. b |
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37. a |
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38. b |
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39. a |
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40. b |
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41. As early as the 1600’s
scientists and observers noticed that the Atlantic shorelines of continents,
particularly South America and Africa, appeared as if they once fit together,
like a puzzle. Sir Ernest Shackleton’s 1908 discovery of coal (the fossilized
remains of tropical plants) in Antarctica suggested that the continent may
have once been located in a warmer part of the world. Other observers noted
that Mountain ranges in Scandinavia, Scotland, and North America, which are
now separated by the Atlantic, were remarkably similar in age, composition,
and structure. Finally, Eduard Suess discovered fossils of the reptile Mesosaurus in
Africa and Argentina, and the seed fern Glossopteris across all of the
southern hemisphere landmasses. If the continents were once joined, these
mountain ranges and bands of fossils would have formed continuous chains.
Wegener compiled all of this information to come up with his theory of
continental drift. |
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42. Plate convergence
happens when lithospheric plates come together. There are three types of
convergence, and they are defined by the composition and density of plates
that are coming together: (1) the convergence of oceanic crust and
continental crust, (2) the convergence of oceanic crust and oceanic crust and
(3) continental crust-continental crust convergence. Because of the density
differences between oceanic and continental crust, different features are
produced. When oceanic crust collides with continental crust, the
heavier oceanic crust subducts beneath the continent, forming a deep trench.
Volcanic mountains also form at these boundaries because subducting ocean
crust partially melts as it plunges downward toward the mantle. The release
of volatile components (such as water and carbon dioxide) from the ocean
crust reduces the melting temperature of the surrounding mantle, forming a
magma rich in dissolved gases. The magma then rises through overlying layers
to the surface, causing volcanic eruptions. Where oceanic crust converges with oceanic crust, the denser
(older and cooler) plate will subduct beneath the lighter plate forming a
trench. The same processes that cause volcanoes to form along ocean-continent
convergent boundaries will occur at ocean-ocean convergent boundaries as
well. However, the resulting volcanoes emerge from the sea floor instead of
the continent. The volcanoes appear in a curve pattern on the overriding
crust. These volcanoes are called “island arcs” when they emerge above sea
level. Lastly, when two plates of continental crust collide, neither
plate will subduct because both plates are of approximately equal density.
The colliding plates, instead, both are compressed, folded, and uplifted, to
form large mountains, such as the Himalayan mountains. |
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43. A compass needle
points to the magnetic north pole because of the persistent magnetic field
caused by the movement of molten metal in the Earth’s outer core. As new
seafloor is produced at spreading centers, the magnetic minerals (which are
naturally occurring in basaltic magma) align with the Earth’s magnetic field.
As the new rock cools and hardens, the orientation of the Earth’s magnetic
field at that particular time is frozen and records information like a fossil
does. Scientists use this information to measure spreading rates and are able
to create detailed charts of the ocean floor dating back about 200 million
years. |
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44. Ocean basins are
formed at divergent plate boundaries where two lithospheric plates pull
apart. The Atlantic Ocean basin began growing around 210 million years ago
when heat from the mantle caused the asthenosphere to expand and rise. This
caused the overlying lithosphere to lift and fracture, forming a rift. As the
lithosphere continued to separate, magma rose to the surface and solidified,
forming a new balsatic ocean floor. Over time, as the ocean basin continued
to grow larger and deeper, water began to collect in the basin, eventually
forming the Atlantic Ocean. |
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45. The Hawaiian
Islands were formed as a result of a hot spot, the surface expression of a
stationary mantle plume. As the Pacific Plate moves in a westerly-
northwesterly direction over the hot spot, the high temperatures and rising
magma from the plume weaken the crust and form a volcano on the ocean floor.
The volcano eventually grows large enough to break the surface of the ocean,
becoming a volcanic island. Because the Pacific Plate is moving, the volcanic
island eventually is carried away from the source of origin, and a new island
forms over the stationary hot spot. Over millions of years, a volcanic island
chain is formed. The Emperor Seamounts north of Hawaii are the oldest
remnants of this island chain, and the island of Hawaii is the youngest. A
new island, Loihi, is currently being formed on the ocean floor, and will
become the next Hawaiian island in about 30,000 years. |
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