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Answer:
Fault
ata yung sagut dyan
Explenation:
Recognizing Reverse Faults Reverse fault displacements combine vertical and compressional displacements. Reverse faults typically have a wide range of dip angles. Reverse faults with low dips exhibit a sinuous surface expression over hilly to flat terrain. Reverse fault scarps are often difficult to locate precisely due to widespread landslides which cover the fault trace. Surface fracturing is characterized by folding or distortion and displacements along subsidiary faults and fractures within the hanging wall (Figure 5.12A).