Respuesta :
The structure of Earth's deep interior cannot be studied directly. But geologists use seismic (earthquake) waves to determine the depths of layers of molten and ... P-wave and S-wave arrival gives a first estimate of the distance to the earthquake
ANSWER:
- Earthquakes create S and P waves. The P waves are quick and of a larger frequency than S waves.
- P waves arrive at a point first and can go through liquid whereas S waves reach after and they lose quite a bit of their energy while passing liquid media.
- This is on the grounds that S-waves are shear waves and require inelastic or inflexible media for transmission.
EXPLANATION:
- During a quake, there is generally a shadow zone (where there isn't any destruction since S-waves didn't reach) framed right over the focal point of the quake.
- This is because of the fact that the S-waves were not able to travel through the inner core of the liquid of the earth before arriving at the surface. Just P-waves are enlisted in this shadow zone.
- Thus, earthquakes provide indirect evidence about the layers of Earth