Earthquake, (also known as quake, tremor or temblor) is a weak to violent shaking of the ground produced by the sudden movement of rock materials below the earth’s surface.
Earthquake, a wave-like movement of the earth’s surface and may classified as tectonic or volcanic
Volcanic Earthquake, are produced by movement of magma beneath volcanoes.
Tectonic Earthquakes,
are produced by sudden movement along faults and plate boundaries.
Focus, actual location beneath the surface where the earthquake begins.
Epicenter, point on the earth’s surface located directly above the focus of an earthquake.
Fault, refers to a fracture, fissure, or a zone of weakness where movement has occurred.
A fault divides rock into two fault blocks, the hanging wall and footwall
For any inclined fault, the block above the fault is the hanging wall block, and the block below the fault is the footwall block
Normalslip, dip-slip faults on hich the hanging wall moves down relative to the footwall.
Reverse slip, Also know as thrust. Dip-slip faults on which the hanging wall moves up relative to the footwall.
Classification of STRIKE-slip faults: RIGHT-LATERAL (DEXTRAL) FAULTS and LEFT-LATERAL (DEXTRAL) FAULTS
RIGHT-LATERAL (DEXTRAL) FAULTS, Strike-slip faults across which the block moves to the right.
LEFT-LATERAL (DEXTRAL) FAULTS
Strike-slip faults across which the block moves to the left.
Oblique-slip Fault, Combination of dip-slip and strike-slip fault
Energy released at the source of the earthquake and determined by seismographs.
Magnitude is amount of energy coming from the focus.
Intensity is strength of shaking produced by the earthquake at a certain location
Indicates the perceived effects of the earthquake in an area, which may vary according to what the affected residents may experience and observe.
Seismograph is an instrument that records an earthquake
seismograph
Records intensity, height and amplitude of seismic waves.
seismometer
Instrument that detect seismic waves
sesimometer sensor that detects ground motion
seismogram record of earthquake retrieved from a seismograph
Aftershock, usually weaker earthquakes that follow the main shock of an earthquake’s sequence. Usually occurs soon after major quake. Not all energy gets released during major event
Foreshock, Small quake preceding major quake. Can happen days or possible years before major quake.
SEISMIC WAVES: Body waves and Surface waves
P waves, Parallel and Push-Pull. Compress and Expand. Particles move in same direction as waves. Travel faster than S waves. Can go through liquids and solids
s waves, Perpendicular and Particles move at right angle to waves’ direction. Also called transverse waves. Travel slower than P waves. Travel through solids only
Surface waves: Rayleigh waves and Love waves
Rayleigh waves Travel near the surface of solids. Rayleigh waves include both longitudinal and transverse motions that decrease exponentially in amplitude as distance from the surface increases. There is a phase difference between these component motions.
Love waves (also known as Q waves (Quer: German for lateral)) are surface seismic waves that cause horizontal shifting of the Earth during an earthquake.