P-waves

First earthquake arrivals

P-waves are the fastest seismic waves generated by earthquakes, traveling through Earth's interior as compression pulses—the same motion as sound waves through air.

They arrive first at seismograph stations, hence "primary waves." P-waves can travel through solid rock and liquid, unlike the slower S-waves (secondary waves) that follow.

The time gap between P-wave and S-wave arrival helps determine an earthquake's distance and location.

seismic

earthquake

Seismic ground movement

epicenter · focus · seismology · tremor · fault · magnitude · arrival time · velocity · crust · mantle

cardiac

ECG

Cardiac electrical recording

arrhythmia · heartbeat · cardiogram · lead · flutter · fibrillation · pacemaker · cardiac cycle · baseline · morphology

Categories
Opposites
seismic wave type

P-wavesS-waves

Secondary seismic vibrations

wave propagation path

P-wavessurface waves

Oscillations at interface boundaries

Family

wave, seismic wave

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