Deck 11: Earths Interior
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Deck 11: Earths Interior
1
Our knowledge of Earth's interior is based on the travel times of seismic body waves.
True
2
The velocities of P- and S-waves depend on the density and elasticity of the rocks through which they travel.
True
3
All else being equal, wave velocities decrease with increasing elasticity.
False
4
P-wave rays are most commonly reflected while S-wave rays are refracted.
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5
The S-wave shadow zone is evidence that the outer core is liquid.
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6
The mantle's density is uniform with depth at any given level.
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7
Seismic tomography uses seismic waves to get a more accurate measurement of Earth's surface shape.
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8
The mantle is more dense than the outer core because the latter is liquid.
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9
With increasing depth and pressure pyroxene changes to peridotite.
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10
A low velocity zone in the mantle indicates that rocks are less elastic due to partial melting.
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11
Increasing pressure with depth causes P-wave velocities to continuously increase into Earth's interior though at different rates.
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12
Kimberlite pipes are composed of materials intruded from as deep as the molten outer core.
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13
Seismic tomography uses X ray waves to analyze Earth's interior.
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14
Gravitational attraction is the same everywhere on Earth's surface.
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15
The geothermal gradient is about 25 C/km near the surface but is higher in areas with recent volcanism.
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16
Isostatic rebound is an alternative explanation for earthquakes.
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17
According the principle of isostasy, a higher mountain range has a deeper root.
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18
If correct, the principle of isostasy implies that mantle behaves as a fluid.
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19
Positive magnetic anomalies are evidence that the subsurface might locally contain iron-bearing minerals.
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20
When a magnetic field reversal occurs, geographic North and South poles also reverse.
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21
Rocks on Earth's surface all have normal polarity.
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22
Geomagnetic reversals are rare events in geological history.
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23
The deepest drill holes extend to approximately
A) 0.15 km
B) 1.5 km
C) 15 km
D) 150 km
A) 0.15 km
B) 1.5 km
C) 15 km
D) 150 km
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24
At a boundary between materials of different density and elasticity, P- and S-waves are
A) reflected
B) refracted
C) reflected and refracted
D) not affected
A) reflected
B) refracted
C) reflected and refracted
D) not affected
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25
Seismic discontinuities permit
A) the recognition of petroleum and ore deposits.
B) the identification of interior structural layers.
C) the identification of differing compositions and properties.
D) B and C
E) all of the above
A) the recognition of petroleum and ore deposits.
B) the identification of interior structural layers.
C) the identification of differing compositions and properties.
D) B and C
E) all of the above
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26
Which of the following is NOT a method by which the density and composition of the core is estimated?
A) the discovery of ultramafic rocks from kimberlite deposits
B) compositions of meteorites
C) experimental behavior of mixtures of various potential elements under high pressures and temperatures
D) the behavior and velocity of P- and S-waves in solids and liquids
E) calculations based on known whole-Earth and crustal-mantle densities
A) the discovery of ultramafic rocks from kimberlite deposits
B) compositions of meteorites
C) experimental behavior of mixtures of various potential elements under high pressures and temperatures
D) the behavior and velocity of P- and S-waves in solids and liquids
E) calculations based on known whole-Earth and crustal-mantle densities
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27
The S-wave shadow zone exists because
A) S waves weaken substantially as they travel through liquids
B) S waves are reflected off liquids
C) S waves do not travel through liquids
D) S waves only travel to a certain depth
A) S waves weaken substantially as they travel through liquids
B) S waves are reflected off liquids
C) S waves do not travel through liquids
D) S waves only travel to a certain depth
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28
The low-velocity zone is important because
A) the rigid lithosphere is buoyed by it.
B) magmas originate in this zone.
C) it flows and so carries the plates above.
D) A and C
E) all of the above
A) the rigid lithosphere is buoyed by it.
B) magmas originate in this zone.
C) it flows and so carries the plates above.
D) A and C
E) all of the above
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29
Which of the following is NOT a method of inferring the composition of the mantle?
A) calculations based on color density values obtained from seismic studies
B) experiments on olivine and pyroxene stabilities at high pressures and temperatures
C) laboratory experiments on the seismic and other physical properties of peridotite
D) peridotite samples from basal oceanic crust and kimberlite pipe deposits
E) laboratory experiments on peridotite's behavior under high pressures and temperatures
A) calculations based on color density values obtained from seismic studies
B) experiments on olivine and pyroxene stabilities at high pressures and temperatures
C) laboratory experiments on the seismic and other physical properties of peridotite
D) peridotite samples from basal oceanic crust and kimberlite pipe deposits
E) laboratory experiments on peridotite's behavior under high pressures and temperatures
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30
The thickness of Earth's crust varies because of
A) variations in composition
B) variations in density
C) variations in temperature
D) A and B
E) all of the above
A) variations in composition
B) variations in density
C) variations in temperature
D) A and B
E) all of the above
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31
P-wave velocities in continental crust are __________in oceanic crust.
A) faster than
B) slower than
C) the same as
A) faster than
B) slower than
C) the same as
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32
The geothermal gradient, about 25°C/km, is generally valid for which of the following situations or uses?
A) to determine the depth at which the rock melts to form the outer core
B) to illustrate that variations in the temperature of the crust are minimal
C) to approximate near surface temperatures
D) to validate models showing increasing wave ray velocities with depth
A) to determine the depth at which the rock melts to form the outer core
B) to illustrate that variations in the temperature of the crust are minimal
C) to approximate near surface temperatures
D) to validate models showing increasing wave ray velocities with depth
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33
Given two objects of the same mass, one at sea level, and the other atop Mount Everest, which has the greater weight?
A) the object on Mount Everest because the distance to the center of Earth, and therefore, the mass of Earth is locally greater
B) the object at sea level because the distance to the center of Earth is least from this elevation
C) the object at sea level because the centrifugal force is greatest at sea level
D) the object on Mount Everest because centrifugal force increases with distance from the center of gravity
E) the object on Mount Everest because the Coriolis effect is strongest at high altitudes
A) the object on Mount Everest because the distance to the center of Earth, and therefore, the mass of Earth is locally greater
B) the object at sea level because the distance to the center of Earth is least from this elevation
C) the object at sea level because the centrifugal force is greatest at sea level
D) the object on Mount Everest because centrifugal force increases with distance from the center of gravity
E) the object on Mount Everest because the Coriolis effect is strongest at high altitudes
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34
Gravitational attraction is variable around the Earth because
A) centrifugal force resulting from rotation varies
B) distribution of earth materials of different densities varies
C) elevation varies
D) A and B
E) all of the above
A) centrifugal force resulting from rotation varies
B) distribution of earth materials of different densities varies
C) elevation varies
D) A and B
E) all of the above
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35
Departures from Earth's expected gravitational attraction would NOT be due to
A) subsurface hydrocarbon resources
B) subsurface metal ore bodies
C) differences in geographic location
D) differences in surface temperature
E) all of the above
A) subsurface hydrocarbon resources
B) subsurface metal ore bodies
C) differences in geographic location
D) differences in surface temperature
E) all of the above
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36
Magnetometers measure the
A) declination of the magnetic field
B) inclination of the magnetic field
C) polarity of the magnetic field
D) strength of the magnetic field
A) declination of the magnetic field
B) inclination of the magnetic field
C) polarity of the magnetic field
D) strength of the magnetic field
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37
Positive magnetic anomalies may result from
A) subsurface iron-bearing deposits
B) extensive basaltic volcanism
C) subsurface salt domes
D) A and B
E) all of the above
A) subsurface iron-bearing deposits
B) extensive basaltic volcanism
C) subsurface salt domes
D) A and B
E) all of the above
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38
Iron-bearing minerals align with the magnetic field when they
A) crystallize from magma
B) cool through the Curie point
C) adjust to plate tectonic movement
D) A and B
E) all of the above
A) crystallize from magma
B) cool through the Curie point
C) adjust to plate tectonic movement
D) A and B
E) all of the above
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39
Departures from the normal strength of Earth's expected magnetic field would NOT be due to
A) variations in iron content of ore bodies
B) lateral variations in rock type
C) differences in surface temperatures
D) buried geologic structures such as salt domes
E) none of the above
A) variations in iron content of ore bodies
B) lateral variations in rock type
C) differences in surface temperatures
D) buried geologic structures such as salt domes
E) none of the above
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40
With___________ , a pro propagating wave is bent; with___________ , the wave is bounced back toward the surface.
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41
A boundary marking a significant change in Earth materials or their properties is called a___________.
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42
The___________ - ___________boundary is a discontinuity that occurs at a depth of 2,900 km below Earth's surface?
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43
The P-wave velocity abruptly ___________at the core-mantle boundary and S-wave velocity goes to zero.
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44
The igneous rock___________ is considered the most likely candidate for representing the composition of the mantle.
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45
The___________ consists of crust and the upper mantle above the low-velocity zone.
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46
Continental crust is generally ___________in composition, while the oceanic crust is generally ___________.
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47
Continental crust has a mineral composition like that of ___________and is known as granitic crust.
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48
P-wave velocities in both continental and oceanic crust abruptly (decrease/increase)___________at their bases, a boundary also known as the___________ ___________.
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49
The of ancient rocks records the strength and direction of Earth's magnetic field at the time of the rocks' formation.
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50
Velocities of P- and S-waves are determined by which two physical properties of the material through which they pass? Explain.
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51
Discuss the contributions of seismic studies to our knowledge of different aspects of geology.
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52
What are two important and very useful differences between P-waves and S-waves? How are they useful?
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53
Why is the core not composed of minerals common on Earth's surface?
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54
How is Earth's magnetism used to explore for natural resources?
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55
Why are science fiction tales of subterranean journeys, such as Jules Verne's A Journey to the Center of Earth, impossible?
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56
Which structural layer of Earth comprises the greatest volume of Earth?
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57
Which structural layer of Earth is the thinnest and least voluminous?
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58
Which structural layer of Earth is liquid?
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59
What are possible rock compositions for the 3 major internal divisions or layers of Earth?
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60
What is the major source of information used in developing this model of Earth's interior?
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61
What are two ways in which the direction of travel of seismic waves can be changed as they travel through different materials?
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62
How are discontinuities located?
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63
Briefly explain why the outer core can be liquid at temperatures of 3,500 - 5,000 °C while the inner core is solid.
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64
What are the major elements comprising Earth's core?
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65
What significant boundary occurs at a depth of approximately 30 km beneath Earth's surface?
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66
How does the depth to the Mohorovicic discontinuity vary?
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67
What does the P- and S-wave low-velocity zone in the upper part of the mantle correspond to closely?
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68
What is the asthenosphere?
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69
How do the low-velocity zone and the asthenosphere differ?
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70
What do discontinuities below the low-velocity zone appear to represent?
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71
What is the transition zone within the mantle?
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72
What are the major minerals which comprise peridotite?
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73
Is Earth's mantle entirely molten? What evidence is there?
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74
What is Earth's mantle?
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75
Why do geophysicists believe the outer core is liquid?
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76
Where is the continental crust thickest?
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77
Where is the continental crust thinnest?
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78
Where is the oceanic crust thinnest?
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79
What is the geothermal gradient?
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80
What is the average geothermal gradient near the surface?
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