Exam 6: Sedimentary Rocks the Archives of Earth History
Exam 1: The Dynamic and Evolving Earth70 Questions
Exam 2: Minerals and Rocks70 Questions
Exam 3: Plate Tectonics: a Unifying Theory70 Questions
Exam 4: Geologic Time Concepts and Principles70 Questions
Exam 5: Rocks Fossils and Time Making Sense of the Geologic Record70 Questions
Exam 6: Sedimentary Rocks the Archives of Earth History70 Questions
Exam 7: Evolution the Theory and Its Supporting Evidence70 Questions
Exam 8: Precambrian Earth and Life History the Hadean and the Archean Eon70 Questions
Exam 9: Precambrian Earth and Life History the Proterozoic Eon70 Questions
Exam 10: Early Paleozoic Earth History70 Questions
Exam 11: Late Paleozoic Earth History70 Questions
Exam 12: Paleozoic Life History Invertebrates70 Questions
Exam 13: Paleozoic Life History Vertebrates and Plants70 Questions
Exam 14: Mesozoic Earth History70 Questions
Exam 15: Life of the Mesozoic Era70 Questions
Exam 16: Cenozoic Earth History the Paleogene and Neogene Periods70 Questions
Exam 17: Cenozoic Earth History the Quaternary Period70 Questions
Exam 18: Life of the Cenozoic Era70 Questions
Exam 19: Primate and Human Evolution70 Questions
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The three major depositional environments are ____________________, ____________________, and ____________________.
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(Short Answer)
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continental, transitional, marine,
continental, marine, transitional,
transitional, continental, marine,
transitional, marine, continental,
marine, continental, transitional,
marine, transitional, continental
Compare and contrast the various types of depositional environments in which evaporite deposits form. How do these deposits differ?
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Evaporite deposits may be formed in playa lakes and saline lakes in desert areas. However, these deposits generally are relatively thin and small in areal extent. In contrast, silled (barred) marine basins (see Fig. 3 in the Perspectives section of Chapter 6) commonly are the site of deposition of thick evaporite deposits of salt and gypsum. In some cases, evaporation of large seas that are closed to other oceans and seas may be responsible for thick marine evaporite deposits.
Lagoons and reefs are sites of carbonate deposition.
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(True/False)
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True
Because wind has a limited capacity to transport sediment, wind deposits are poorly sorted.
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Explain how fossils, and especially microfossils, can be used to help determine ancient depositional environments.
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In bioturbation, most of the original sedimentary structures are preserved.
(True/False)
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The most important source rocks for fuels we use today are igneous rocks.
(True/False)
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Compare and contrast the sediments deposited in continental, transitional, and marine environments. Give specific examples of these sediment types and the environments where they commonly form.
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From continent to deep-ocean basin, what is the order of offshore environments?
(Multiple Choice)
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Turbidity currents deposit sediments in ____ beds with ____.
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Prograding d elta deposits differ from turbidity current deposits because ____.
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Rocks above and below a bedding plane may have different physical properties.
(True/False)
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A well-sorted sediment contains particles that are of about the same size.
(True/False)
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Graded beds refer to sedimentary beds that show a decrease in grain size from bottom to top.
(True/False)
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