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the difference between the arrival of the p-wave and s-wave

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Nelle Mraz

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3y ago

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What is S-P lag time?

the difference between the arrival of the p-wave and s-wave


As the distance from the epicenter increases What happens to the time lag between p and s wave?

As the distance from the epicenter increases, the time lag between P and S waves increases. This is because the P wave, being faster, arrives at the seismograph station sooner than the S wave which is slower. The greater the distance, the more noticeable this time lag becomes.


What is the distance of a station from the epicenter if the s-p lag time is measured to be 35.5 seconds?

The distance of a station from the epicenter can be calculated using the formula: Distance (in kilometers) = (s-p lag time in seconds) × 8, where the 8 represents the speed of seismic waves. So, if the s-p lag time is 35.5 seconds, the distance from the epicenter would be 35.5 × 8 = 284 kilometers.


Does the lag time get shorter or longer the further you get from the epicenter?

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.


What happens to the lag time as distance from the epicenter increases?

It Also Increases


How do you calculate the distance from an earthquake?

The distance from an earthquake epicenter can be calculated using the time difference between the arrival of P-waves and S-waves at a seismograph station. By measuring this time lag and using the known velocity of seismic waves through the Earth's interior, the distance can be estimated. The greater the time lag between the arrival of the P-wave and S-wave, the farther the seismograph station is from the earthquake epicenter.


If the lag time between the arrival of the P waves and the S waves is 5 minutes what is the distance to the epicenter?

To calculate distance to the epicenter, first convert the 5-minute lag time to seconds (5 minutes = 300 seconds). Then divide this by 8 to get the distance in kilometers (P waves travel at approximately 8 km/s). Therefore, the distance to the epicenter would be 37.5 km (300 seconds / 8 km/s).


How are p-and s-waves arrival time differences related to the distance of a city away from an epicenter?

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.


What is the relationship between lag time and distance from an earthquake's epicenter?

The lag time between the arrival of primary (P-wave) and secondary (S-wave) seismic waves increases with distance from an earthquake's epicenter. This relationship is due to the differing speeds at which these waves travel through the Earth's layers. By measuring this lag time, scientists can estimate the distance to the earthquake's epicenter.


What is the difference between an inside lag and an outside lag?

Inside lag is the time to implement (pass) a policy, while outside lag is the time it needs to take effect.


What difference between P-waves and S-waves is used to find an earthquake's epicenter?

The difference in arrival times of P-waves and S-waves can be used to find an earthquake's epicenter. P-waves travel faster than S-waves, so by measuring the time lag between the arrival of the two wave types at different seismic stations, scientists can triangulate the epicenter of the earthquake.


How are p waves and s waves used to find the distance from a seismic station to the epicenter of an earthquake?

By measuring the time difference between the arrival of P-waves and S-waves at a seismic station, seismologists can calculate the distance from the station to the earthquake's epicenter. P-waves travel faster than S-waves, so the greater the time lag between their arrivals, the farther the station is from the epicenter. By using data from multiple stations, seismologists can triangulate the location of the epicenter.