P-waves

E672911

P-waves are primary seismic body waves that compress and expand the material they travel through and are the fastest type of earthquake-generated wave, moving through both solids and fluids.

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Statements (47)

Predicate Object
instanceOf body wave
primary wave
seismic wave
alsoKnownAs compressional waves
longitudinal seismic waves
primary waves
amplitude generally smaller than S-wave amplitude at same distance
arrivalOrder first to arrive at a seismic station
attenuation generally lower attenuation than S-waves
cannotTravelThrough vacuum
category earthquake-generated wave
elastic wave
causes alternating compression and dilation of rocks
comparedToS-waves faster than S-waves
comparedToSurfaceWaves arrive earlier than surface waves
directionality radial from the source in a homogeneous medium
discoveryCentury 19th century
energyType mechanical energy
generatedBy earthquakes
explosions
sudden stress changes in the Earth
governedBy elastic wave equations
hazardRelevance often used for early warning before strong shaking
motionType compression and rarefaction of material
particleMotionDirection parallel to direction of wave propagation
phaseNameInSeismology P
polarization linear
propagationMedium gases
liquids
solids
recordedBy seismometers
recordedOn seismograms
reflection can reflect at boundaries between different materials
refraction can refract when entering media with different velocities
relativeSpeed fastest seismic wave type
speedDependsOn density of the medium
elastic properties of the medium
travelsThrough Earth’s crust
Earth’s inner core
Earth’s mantle NERFINISHED
Earth’s outer core
typicalVelocityInCrust about 5 to 7 km/s
typicalVelocityInMantle about 8 to 14 km/s
usedFor estimating earthquake magnitude
locating earthquake hypocenters
probing Earth’s internal structure
waveType longitudinal wave

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Rayleigh waves comparedTo P-waves