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Geological faults are critical fractures in the Earth's crust that play a significant role in earthquake dynamics. The chapter discusses the definition, causes, and classifications of faults, along with their geometrical and mechanical properties. It emphasizes the importance of understanding faults for effective civil engineering practices, especially regarding risk assessment and infrastructure planning in seismically active regions.
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References
Chapter_21_Geolo.pdfClass Notes
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What we have learnt
Final Test
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Term: Fault
Definition: A fracture in the Earth's crust along which movement has occurred.
Term: Normal Fault
Definition: A type of dip-slip fault where the hanging wall moves downward relative to the footwall.
Term: Reverse Fault
Definition: A fault where the hanging wall moves upward relative to the footwall, typically found in compressive settings.
Term: Thrust Fault
Definition: A low-angle reverse fault that causes significant crustal shortening.
Term: Elastic Rebound Theory
Definition: A theory explaining how stress accumulates in rocks until it exceeds strength, leading to fault rupture and energy release.
Term: Fault Hazard Assessment
Definition: A process used by civil engineers to evaluate the risks associated with fault activity for effective planning and design.