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Geology 103 Sedimentology and Stratigraphy Tim Horner Geology Department, CSU Sacramento

SACRAMENTO. STATE. Geology 103 Sedimentology and Stratigraphy Tim Horner Geology Department, CSU Sacramento. Lecture #8: Mass movements, sediment gravity flows Reading assignment: Boggs, 5 th ed., pp. 31-33, 38-41. Types of mass-movements.

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Geology 103 Sedimentology and Stratigraphy Tim Horner Geology Department, CSU Sacramento

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  1. SACRAMENTO STATE Geology 103Sedimentology and StratigraphyTim HornerGeology Department, CSU Sacramento Lecture #8: Mass movements, sediment gravity flows Reading assignment: Boggs, 5th ed., pp. 31-33, 38-41

  2. Types of mass-movements From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Table 2.1, p. 32

  3. Features of a debris flow deposit: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.7, p. 37

  4. Matrix strength supports grains in a debris flow: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.6, p. 33

  5. Grain-to-grain interaction supports grains in a grain flow: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.6, p. 33

  6. Features of a grain flow deposit: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.7, p. 37

  7. Excess pore pressure supports grains in a liquified (fluidal) flow: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.6, p. 33

  8. Features of a liquified (fluidal) flow deposit: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.7, p. 42

  9. Parts of a turbidity current: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.4.1, p. 34

  10. Turbulence supports grains in a turbidity flow: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.6, p. 33

  11. Features of a turbidity flow deposit: From Boggs, Principles of Sedimentology and Stratigraphy, 5th ed., Figure 2.7, p. 37

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