Exam 7: Crustal Deformation and Mountain Building
Exam 1: Introduction to Earth Science108 Questions
Exam 2: Matter and Minerals115 Questions
Exam 3: Rocks: Materials of the Solid Earth120 Questions
Exam 4: Plate Tectonics: a Scientific Revolution Unfolds89 Questions
Exam 5: Earthquakes and Earths Interior90 Questions
Exam 6: Volcanoes and Other Igneous Activity106 Questions
Exam 7: Crustal Deformation and Mountain Building97 Questions
Exam 8: Weathering, Soil, and Mass Movement124 Questions
Exam 9: Running Water and Groundwater134 Questions
Exam 10: Glaciers, Deserts, and Wind100 Questions
Exam 11: Geologic Time102 Questions
Exam 12: Earths Evolution Through Geologic Time129 Questions
Exam 13: The Ocean Floor92 Questions
Exam 14: Ocean Water and Ocean Life74 Questions
Exam 15: The Dynamic Ocean101 Questions
Exam 16: The Atmosphere: Composition, Structure, and Temperature85 Questions
Exam 17: Moisture, Clouds, and Precipitation101 Questions
Exam 18: Air Pressure and Wind97 Questions
Exam 19: Weather Patterns and Severe Storms96 Questions
Exam 20: World Climates and Global Climate Change105 Questions
Exam 21: Origins of Modern Astronomy101 Questions
Exam 22: Touring Our Solar System93 Questions
Exam 23: Light, Telescopes, and the Sun93 Questions
Exam 24: Beyond Our Solar System83 Questions
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Carefully study the illustration below to determine the types. of geologic structures. it shows. 
(Multiple Choice)
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Southwestern North America contains a large area called the Basin and Range province. What is the origin of this name?
(Multiple Choice)
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Burial of rocks increases the confining pressure so that deeply buried rocks are more likely to _______than shallow rocks.
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The Appalachian Mountains may have once been as lofty as the Himalayan- Tibetan Mountain belt is today. Why are they not this high now?
(Multiple Choice)
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Granitic batholiths typically form over time intervals of _______ These are normally formed below the surface of the earth.
(Multiple Choice)
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The Appalachians and Himalaya are a classic collisional mountain belts yet the elevation of the Appalachians mountains is a tiny fraction of the lofty Himalaya. Why are these two collisional mountain belts so different?
(Essay)
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In the interior of continents the earth's crust is typically about 40km thick and the elevation is near sea level. Most earth materials expand when heated, lowering their density. During rifting continental margins are heated but cool as sea floor spreading moves offshore from the continent. Thus, basic isostasy suggests that after rifting, a continental margin will_______ .
(Multiple Choice)
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Use the figure below to answer the following questions.
-In the figure, which of the deformations appears most similar to what might be expected along a transform plate boundary?
(Multiple Choice)
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The Sierra Nevada Mountains of California, and the Teton Mountains of Wyoming, ranges are examples of_______ .
(Multiple Choice)
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An_______ is a thick accumulation of sediments and small tectonic blocks formed of material scraped off subducting oceanic lithosphere at a convergent margin.
(Multiple Choice)
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The below diagram is an example of what plate tectonic setting? 
(Multiple Choice)
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When subjected to a differential stress, a very "brittle" material, like glass, will_______ .
(Multiple Choice)
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In the figure below, which occurred first, the folding or the faulting? Briefly explain your answer.

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Use this figure for the following questions:
The figure above shows a popular area for North American tourists in winter, the Caribbean region. Match the term to the lett the Figure.
-Island arc
(Multiple Choice)
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Use this figure for the following questions:
The figure above is an oblique Google earth image from southwestern North America looking approximately north. The view approximately 50km across. The area is a classic area of normal faulting.
-Topographic basins like the areas labeled B in this figure are called ______.
(Multiple Choice)
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