The time between P-waves (primary waves) and S-waves (secondary waves) varies depending on the distance from the seismic event. Generally, for an earthquake, the time difference can range from a few seconds to several minutes, with P-waves arriving first, followed by S-waves. The greater the distance from the epicenter, the longer the interval between the two types of waves. Seismologists often use this time difference to determine the location of the earthquake.
Yes, that is correct. The time difference between the arrival of P-waves and S-waves increases as the earthquake epicenter gets closer to the seismograph. P-waves are faster, so they arrive first, followed by the slower S-waves.
The arrival time difference between p- and s-waves increases with distance from the epicenter. p-waves travel faster and arrive first, followed by s-waves which are slower. The farther a city is from the epicenter, the greater the time lag between the arrival of the two waves.
The arrival time difference between P-waves and S-waves at station 4 would be shorter than at station 3. This is because the further away a seismic station is from the earthquake epicenter, the shorter the time difference between the arrival of P-waves and S-waves. This is due to the faster travel speed of P-waves compared to S-waves.
The time difference between primary (P) and secondary (S) waves becomes larger as the distance traveled by the waves increases. This is because P-waves travel faster than S-waves, so the time delay between their arrivals at a seismometer station increases with distance.
As P-waves travel at a higher velocity than S-waves they arrive at a seismometer station before the S-waves. The difference between their arrival time can be used to calculate the distance from the seismometer station to the epicentre.
Yes, that is correct. The time difference between the arrival of P-waves and S-waves increases as the earthquake epicenter gets closer to the seismograph. P-waves are faster, so they arrive first, followed by the slower S-waves.
False. The closer an earthquake is, the shorter the time difference between the arrival of P waves and S waves. P waves travel faster than S waves, so the time interval decreases as the distance to the earthquake epicenter decreases.
As P-waves travel at a higher velocity than S-waves they arrive at a seismometer station before the S-waves. The difference between their arrival time can be used to calculate the distance from the seismometer station to the epicentre.
The time difference between P waves and S waves increases with distance from the epicenter because P waves, which are primary waves, travel faster than S waves, which are secondary waves. As seismic waves propagate through the Earth, the greater the distance from the epicenter, the longer it takes for the slower S waves to arrive after the faster P waves. This results in a growing time interval between their arrivals, allowing seismologists to determine the distance to the epicenter based on this time difference.
As the distance from the earthquake to the seismograph station increases, the time interval between the arrival of P waves and S waves also increases. This is because S waves travel slower than P waves, so the further distance allows more time for the S waves to catch up and be recorded after the P waves.
The arrival time difference between p- and s-waves increases with distance from the epicenter. p-waves travel faster and arrive first, followed by s-waves which are slower. The farther a city is from the epicenter, the greater the time lag between the arrival of the two waves.
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The lag time between the arrival of P-waves and S-waves generally gets longer the further you are from the earthquake's epicenter. P-waves travel faster than S-waves, so the time difference between their arrivals increases with distance.
The arrival time difference between P-waves and S-waves at station 4 would be shorter than at station 3. This is because the further away a seismic station is from the earthquake epicenter, the shorter the time difference between the arrival of P-waves and S-waves. This is due to the faster travel speed of P-waves compared to S-waves.
They are waves.
The time difference between primary (P) and secondary (S) waves becomes larger as the distance traveled by the waves increases. This is because P-waves travel faster than S-waves, so the time delay between their arrivals at a seismometer station increases with distance.
P-waves (primary waves) are compressional waves that travel faster than S-waves (secondary waves), which are shear waves. This difference in speed allows seismologists to determine the epicenter of an earthquake by analyzing the time difference between the arrival of these two types of waves at seismograph stations. By measuring the time interval between the arrivals of P-waves and S-waves, the distance to the epicenter can be calculated, enabling the pinpointing of its location.