Exam 12: Earth S Internal Structure, rock Cycle, and Geologic Time
Exam 1: Introduction to Physical Geography54 Questions
Exam 2: The Geographers Tools172 Questions
Exam 3: Earth-Sun Geometry and the Seasons107 Questions
Exam 4: The Global Energy System145 Questions
Exam 5: Global Temperature Patterns112 Questions
Exam 6: Atmospheric Pressure, wind, and Global Circulation119 Questions
Exam 7: Atmospheric Moisture and Precipitation103 Questions
Exam 8: Air Masses and Cyclonic Weather Systems141 Questions
Exam 9: Global Climates and Global Climate Change176 Questions
Exam 10: Plant Geography153 Questions
Exam 11: The Global Distribution and Character of Soils138 Questions
Exam 12: Earth S Internal Structure, rock Cycle, and Geologic Time124 Questions
Exam 13: Tectonic Processes and Landforms132 Questions
Exam 14: Weathering and Mass Movements130 Questions
Exam 15: Groundwater and Karst Landscapes105 Questions
Exam 16: Fluvial Systems and Landforms125 Questions
Exam 17: Glacial Geomorphology: Processes and Landforms114 Questions
Exam 18: Arid Landscapes and Eolian Processes117 Questions
Exam 19: Coastal Processes and Landforms125 Questions
Exam 20: Population Growth and Environmental Impacts146 Questions
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The subsidence and rebound of the asthenosphere is called isostacy.
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In which of the following are the geologic periods in the correct chronological order?
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At the Grand Canyon,the oldest rocks are found on the lip or rim of the canyon.
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The term sima refers to the composition of the continental crust.
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The three classes of sedimentary rocks are clastic,foliated,and organic.
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The layer of very soft rock within the Earth that allows for isostatic adjustments is the
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The period of time that encompasses all of the Earth history,from its formation to the present,is called __________.
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The time that it takes for half of a radioactive isotope to break down is its
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The process whereby loose rock debris is cemented and compacted to form rock is called
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As a mountain erodes,it also rises so that its roots are not as deep into the Earth.
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