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EARTHQUAKE ENGINEERING
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Epicenter
Geographic point on Earth’s surface directly above the focus
Focus/Hypocenter
Point where fault rupture begins (underground).
Fault Plane
Plane along which rock ruptures and slips.
Dip Angle
Angle between fault plane and horizontal surface.
Strike Angle
Direction of fault line relative to North.
Fault Slip
Relative displacement along the fault plane.
Epicentral Distance
Distance from epicenter to observation station.
Shallow
Focal depth of <70 km (most destructive)
Intermediate
Focal depth of 70–300 km
Deep
Focal depth of >300 km
Foreshocks
Smaller quakes before main shock.
Aftershocks
Smaller quakes after main shock due to stress adjustments
Fault Types
Dip-Slip
Strike-Slip
Oblique-Slip
Dip-Slip
Vertical movement (normal/reverse faults).
Strike-Slip
Horizontal movement (e.g., transform faults).
Oblique-Slip
Combination of both Dip-Slip and Strike-Slip
Body Waves
P-waves (Primary)
S-waves (Secondary)
Surface Waves (most destructive)
Love Waves
Rayleigh Waves
P-waves (Primary)
Longitudinal, fastest (∼6 km/s in solids).
Travel through solids and liquids.
S-waves (Secondary)
Transverse, slower (∼3 km/s).
Travel only through solids.
Love Waves
Horizontal shearing motion.
Rayleigh Waves
Rolling motion (like ocean waves).
Peak Ground Acceleration (PGA)
Key parameter for design.
Attenuation
Dissipation of seismic energy with distance.