Understanding P-Waves and S-Waves #SeismicWaves #PWaves #SWaves #PCS #EarthquakeDetection | abhimanu IAS
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Understanding P-Waves and S-Waves #SeismicWaves #PWaves #SWaves #PCS #EarthquakeDetection | abhimanu IAS
abhimanu IAS. abhimanu IAS · Original audio. Understanding P-Waves and S-Waves #SeismicWaves #PWaves #SWaves #PCS #EarthquakeDetection
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SOLVED: Earthquakes produce several types of shock waves. The most knownare the P-waves (P for primary or pressure) and the S-waves (S forsecondary or shear). In the earth’s crust, the P-waves travel ataround 6.5 km/s, while the S-waves move at about 3.5 km/s. Theactual speeds vary depending on the type of material they are goingthrough. The time delay between the arrival of these two waves at aseismic recording station tells geologists how far away theearthquake occurred. If the time delay is 3
SOLVED: Earthquakes produce several types of shock waves. The most knownare the P-waves (P for primary or pressure) and the S-waves (S forsecondary or shear). In the earth’s crust, the P-waves travel ataround 6.5 km/s, while the S-waves move at about 3.5 km/s. Theactual speeds vary depending on the type of material they are goingthrough. The time delay between the arrival of these two waves at aseismic recording station tells geologists how far away theearthquake occurred. If the time delay is 3
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