Deck 3: Plate Tectonics
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Deck 3: Plate Tectonics
1
These are areas not connected with plate boundaries but are regions of volcanic activities and are use to monitor the direction and movement of plates are called
A) Divergent plate boundaries.
B) Volcanic areas.
C) Convergent plate boundaries.
D) Hotspots.
A) Divergent plate boundaries.
B) Volcanic areas.
C) Convergent plate boundaries.
D) Hotspots.
D
2
According to plate-tectonic theory,plates of rigid,elastic __________ move over a weak plastic layer below.
A) Lithosphere
B) Asthenosphere
C) Mantle
D) Core
A) Lithosphere
B) Asthenosphere
C) Mantle
D) Core
A
3
Example of the movement of the following plates: continent-ocean; continent-continent; ocean-ocean is best referred to as the
A) Divergent plate boundary.
B) Transform plate boundary.
C) Constructive plate boundary.
D) Convergent plate boundary.
A) Divergent plate boundary.
B) Transform plate boundary.
C) Constructive plate boundary.
D) Convergent plate boundary.
D
4
The magnetic dip preserved in a rock indicates
A) How far east or west of north the rock crystallized.
B) The rock's magnetic latitude at the time that it - crystallized.
C) How deep in the crust the magma crystallized.
D) How far from a spreading ridge the rock has traveled.
A) How far east or west of north the rock crystallized.
B) The rock's magnetic latitude at the time that it - crystallized.
C) How deep in the crust the magma crystallized.
D) How far from a spreading ridge the rock has traveled.
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5
At a convergent plate boundary,
A) Sea floor is produced.
B) High mountains may be built during continent-continent collision.
C) There are very few earthquakes.
D) All of the choices are correct.
A) Sea floor is produced.
B) High mountains may be built during continent-continent collision.
C) There are very few earthquakes.
D) All of the choices are correct.
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6
Divergent plate boundaries
A) Always result in rifts along which new oceanic crust is created.
B) May result in rifts on continents, but may also "fail" or stop, resulting in topographically low areas.
C) Are no longer a potential hazard if they are not actively rifting.
D) Are simple curvilinear features on all ocean floors.
A) Always result in rifts along which new oceanic crust is created.
B) May result in rifts on continents, but may also "fail" or stop, resulting in topographically low areas.
C) Are no longer a potential hazard if they are not actively rifting.
D) Are simple curvilinear features on all ocean floors.
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7
A rock's Curie temperature is the temperature above which it
A) Melts.
B) Begins to flow plastically.
C) Loses its magnetism.
D) Ruptures.
A) Melts.
B) Begins to flow plastically.
C) Loses its magnetism.
D) Ruptures.
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8
The Azores Islands
A) Are remnants of rare rift zone volcanoes.
B) Are part of the Aleutian Island volcanic arc.
C) Are, like Hawaii, formed by a Hot Spot.
D) Are not formed by tectonic processes.
A) Are remnants of rare rift zone volcanoes.
B) Are part of the Aleutian Island volcanic arc.
C) Are, like Hawaii, formed by a Hot Spot.
D) Are not formed by tectonic processes.
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9
Stress tending to pull objects apart is __________ stress.
A) Compressive
B) Tensile
C) Shearing
D) Elastic
A) Compressive
B) Tensile
C) Shearing
D) Elastic
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10
The San Andreas fault is a good example of a
A) Convergent plate boundary.
B) Divergent plate boundary.
C) Transform plate boundary.
D) Hotspot.
A) Convergent plate boundary.
B) Divergent plate boundary.
C) Transform plate boundary.
D) Hotspot.
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11
A ductile material is one that
A) Resists deformation under stress.
B) Conducts electricity well.
C) Readily undergoes plastic deformation.
D) Ruptures easily under stress.
A) Resists deformation under stress.
B) Conducts electricity well.
C) Readily undergoes plastic deformation.
D) Ruptures easily under stress.
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12
Pre-drift reassembly of the continents can be assisted by
A) Polar-wander curves.
B) Matching up the shapes of the corresponding continental margins.
C) Matching up mountain ranges and rock types between once-adjacent continents.
D) All of the choices are correct.
A) Polar-wander curves.
B) Matching up the shapes of the corresponding continental margins.
C) Matching up mountain ranges and rock types between once-adjacent continents.
D) All of the choices are correct.
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13
With increasing distance from an oceanic ridge,
A) The rocks become older.
B) The rocks become younger.
C) The rocks' ages alternate between younger and older.
D) All of the choices; different patterns occur at different ridges.
A) The rocks become older.
B) The rocks become younger.
C) The rocks' ages alternate between younger and older.
D) All of the choices; different patterns occur at different ridges.
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14
Sea floor is formed at spreading ridges and destroyed
A) At divergent boundaries.
B) In transform faults.
C) In subduction zones.
D) By magnetic-field reversals.
A) At divergent boundaries.
B) In transform faults.
C) In subduction zones.
D) By magnetic-field reversals.
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15
Divergent plate boundaries around the world are indicated by
A) Seafloor spreading.
B) Hotspots.
C) Subduction zones.
D) Both seafloor spreading and subduction zones.
A) Seafloor spreading.
B) Hotspots.
C) Subduction zones.
D) Both seafloor spreading and subduction zones.
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16
Oceanic lithosphere
A) Is made of alternating bands of rocks of different compositions.
B) Is made of alternating bands of rocks of two different ages.
C) Records magnetic "stripes" of normally and reversely magnetized rocks.
D) Moves gradually toward the midocean ridges, where it is consumed.
A) Is made of alternating bands of rocks of different compositions.
B) Is made of alternating bands of rocks of two different ages.
C) Records magnetic "stripes" of normally and reversely magnetized rocks.
D) Moves gradually toward the midocean ridges, where it is consumed.
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17
The strength of a rock
A) May depend on how long it has been subjected to stress.
B) Varies with the kind of stress (compressive, tensile or shearing).
C) May be reduced by weathering or fracturing.
D) All of the choices are correct.
A) May depend on how long it has been subjected to stress.
B) Varies with the kind of stress (compressive, tensile or shearing).
C) May be reduced by weathering or fracturing.
D) All of the choices are correct.
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18
A "polar-wander" curve shows
A) How magnetic poles have moved on the earth.
B) How the sea floor has spread.
C) How continents have moved or drifted, relative to the magnetic poles.
D) How polar glacier ice has moved across continents.
A) How magnetic poles have moved on the earth.
B) How the sea floor has spread.
C) How continents have moved or drifted, relative to the magnetic poles.
D) How polar glacier ice has moved across continents.
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19
For most solids,sufficiently increased stress results in
A) Breakage.
B) Rupture.
C) Deformation.
D) Transformation.
A) Breakage.
B) Rupture.
C) Deformation.
D) Transformation.
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20
Fossil remains of this animal proved important to the belief that South America and Africa were once joined,then drifted apart
A) Glossopteris.
B) Ichtyosaur.
C) Crinoids.
D) Mesosaur.
A) Glossopteris.
B) Ichtyosaur.
C) Crinoids.
D) Mesosaur.
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21
The earth's polarity has remained the same since its existence.
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22
In order for continental drift to occur,the continental lithosphere must behave plastically.
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23
Continental drift may explain evidence of past glaciation in regions now located in the tropics,because local climate is strongly controlled by latitude.
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24
Plate boundaries were originally located by a French graduate student who plotted the location of all earthquakes and volcanic eruptions world-wide on a map.
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25
The locations and ages of islands in the Hawaiian Island chain can be used to show
A) The direction of drift of North America.
B) The rate and direction of movement of the Pacific Plate.
C) The size of earthquakes to be expected in the Pacific Ocean.
D) All of the choices are correct.
A) The direction of drift of North America.
B) The rate and direction of movement of the Pacific Plate.
C) The size of earthquakes to be expected in the Pacific Ocean.
D) All of the choices are correct.
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26
An island arc comprising of volcanic islands forms as a result of ocean-ocean convergence.
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27
Stress is the deformation resulting from the application of strain to a rock.
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28
The physical properties of a rock are determined only by grain shapes and sizes and are independent of the kinds of minerals making up the rock.
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29
Because the sea floor is protected from weathering,seafloor rocks are better preserved and generally older than continental rocks.
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30
Rocks may behave differently over the long spans of geologic time than they do in short-term laboratory experiments.
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31
A possible "driving force" for plate motions is
A) Volcanic eruption at hot spots.
B) Shifts in the earth's magnetic field.
C) Convection in the asthenosphere.
D) The weight of subducted continents pulling downward.
A) Volcanic eruption at hot spots.
B) Shifts in the earth's magnetic field.
C) Convection in the asthenosphere.
D) The weight of subducted continents pulling downward.
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32
The idea of continental drift was not proposed until the 1960s,when the first evidence to support it was discovered.
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33
Plates move away from each other by 3.5 cm per year at the mid-Atlantic ridge,for a net growth of 7 cm per year for the width of the Atlantic Ocean.How much wider is the Atlantic Ocean today compared to when Columbus discovered the Americas in 1492?
A) About 40 meters
B) About 400 meters
C) About 4 meters
D) About 4 kilometers (4000 meters)
A) About 40 meters
B) About 400 meters
C) About 4 meters
D) About 4 kilometers (4000 meters)
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34
Rubber bands show elastic behavior until their elastic limit is exceeded; rocks are always brittle.
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35
The remnant magnetism in the rocks is called paleomagnetism.
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36
The Appalachian Mountains of eastern North America were formed by continent-continent collision.Today,these mountains are still being uplifted by the same type of collision
A) The Andes Mountains of South America.
B) The Cascade Mountains of North America.
C) The Rocky Mountains of North America.
D) The Himalaya Mountains of Asia.
A) The Andes Mountains of South America.
B) The Cascade Mountains of North America.
C) The Rocky Mountains of North America.
D) The Himalaya Mountains of Asia.
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37
The asthenosphere is a weak,locally partly molten layer over which lithospheric plates can move.
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38
Hot spots
A) Move along with plates.
B) Can exist under both oceans and continents, but remain stationary as the plate above moves.
C) result in extrusion of volcanic rocks.
D) Both b and c are correct.
A) Move along with plates.
B) Can exist under both oceans and continents, but remain stationary as the plate above moves.
C) result in extrusion of volcanic rocks.
D) Both b and c are correct.
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39
Deep in the crust,at elevated temperatures,rocks may behave plastically and undergo folding or flow.
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40
Brittle behavior in rocks leads to formation of folds.
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41
Plate tectonics are unrelated to the rock cycle and,in fact,has made the rock-cycle concept obsolete.
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42
Seawater interacting with hot sea floor at spreading ridges may produce mineral deposits.
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43
Although convection in the asthenosphere is widely accepted as the cause of plate movements,it may be that the weight of down-going lithosphere in subduction zones pulls the trailing plate behind it.
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44
Rifting occurs at oceanic spreading ridges,but not within continents,because continents are so thick and strong.
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45
Satellite data now allow direct measurement of the rates of plate movement,even though it is slow.
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46
About 200 million years ago,most of the continents were together,forming a "super continent" called Pangaea.
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47
Part of western California is attached to the Pacific Plate,while most of North America belongs to a separate plate.
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48
Earthquakes occur at subduction zones,but volcanoes do not because the subducted lithosphere is pushed deep into the mantle.
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49
The Hawaiian Islands were formed by repeated volcanic eruptions over a hot spot.
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50
The best explanation for the distribution of Glossopteris and Mesosaurus is that they lived when continents on which their fossils are now found were once connected then later were rifted and drifted apart.
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51
Transform faults that offset segments of a spreading ridge are formed because rates of spreading are not constant along any one rift zone so shearing develops when one segment grows faster than another.
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52
It is not possible to estimate rates of plate movement because new rocks are constantly being created from old.
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