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∙ 12y agoFalse. The closer you are to the epicentre, the smaller the time difference between the arrival of P and S-waves.
Wiki User
∙ 12y agoYes, 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 difference between the arrival times increases as the distance from an earthquake epicentre increases as S-waves travel more slowly than P-waves so the greater the distance the further they lag behind.
The time difference between the arrival of P waves and S waves at a seismograph station is used to determine the distance of an earthquake's epicenter. By measuring this time lag and knowing the speed at which each wave travels through the Earth's interior, scientists can calculate the distance the waves traveled to reach the station. The farther apart the arrival times of P and S waves, the greater the distance of the epicenter from the station.
No, to find the epicenter of an earthquake, you use the difference in arrival times between the P-wave and the S-wave at a seismograph station. The greater the time difference between the two waves, the farther the earthquake's epicenter is from that particular station. Subtraction is not directly involved in this process.
A magnitude 6 earthquake emits roughly 31 times more energy than a magnitude 5 earthquake. The magnitude 6 quake will also have a maximum seismic wave amplitude of ten times the magnitude 5 earthquake.
The magnitude of a 9.2 earthquake is 1000 times greater than a 6.3 earthquake. This is because every 1-point increase on the Richter scale represents a tenfold increase in amplitude, meaning a 3-point difference represents 10x10x10 = 1000 times difference in magnitude.
The time difference in arrival between P and S waves can help determine the distance to an earthquake epicenter. For each second of difference, the earthquake is roughly 7.5 kilometers away. So, a time difference of, for example, 10 seconds would indicate the earthquake is approximately 75 kilometers away.
The difference between the arrival times increases as the distance from an earthquake epicentre increases as S-waves travel more slowly than P-waves so the greater the distance the further they lag behind.
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.
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.
Using the difference in their arrival times and an estimate of their velocity of propagation you can calculate the distance of the earthquake epicentre from the seismometer recording station. If you do this from three or more different seismometer stations you can triangulate it's position. For more information please see the related question.
The time difference between the arrival of P waves and S waves at a seismograph station is used to determine the distance of an earthquake's epicenter. By measuring this time lag and knowing the speed at which each wave travels through the Earth's interior, scientists can calculate the distance the waves traveled to reach the station. The farther apart the arrival times of P and S waves, the greater the distance of the epicenter from the station.
No, to find the epicenter of an earthquake, you use the difference in arrival times between the P-wave and the S-wave at a seismograph station. The greater the time difference between the two waves, the farther the earthquake's epicenter is from that particular station. Subtraction is not directly involved in this process.
A 7.0 earthquake is much stronger and more destructive than a 5.0 earthquake. The energy released by a 7.0 earthquake is about 1,000 times greater than that of a 5.0 earthquake. This means that a 7.0 earthquake can cause more severe damage to buildings and infrastructure.
The Richter magnitude scale is a base-10 logarithmic scale of the shaking amplitude. This means that a difference of 1 in the scale is equivalent to a 10-fold increase in amplitude. So the difference in amplitude between a mag 8 and a mag 4 earthquake is 104.
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.
A magnitude 6 earthquake emits roughly 31 times more energy than a magnitude 5 earthquake. The magnitude 6 quake will also have a maximum seismic wave amplitude of ten times the magnitude 5 earthquake.
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