u figure it out dude
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 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.
Sound waves are longitudinal waves that travel through mediums such as air, while seismic waves are a combination of both longitudinal (P-waves) and transverse (S-waves) waves that travel through the Earth’s interior. Seismic waves are typically caused by geological events like earthquakes, while sound waves are produced by vibrating sources like speakers or instruments.
Your standing on it! P-waves travel faster than S-waves through the Earth. As such the further away a seismometer station is from the epicentre of an Earthquake, the larger the difference between arrival times will be. By the same logic this means that the closer you get to the epicentre, the smaller the difference in arrival time will be until your at the epicentre when the difference will be zero!
Microwaves and sound waves are similar because they are electromagnetic waves. The main difference between the two types of waves is the length of the wave. Sound waves are longer than microwaves.
Difference is in their frequency, audible sound waves is between 12 Hz and 20,000 Hz, Ultrasound waves is any sound that has a frequency beyond the 20,000 Hz limit
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.
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 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.
sound are longitudinal waves while water waves are transverse waves
Sound waves are longitudinal waves that travel through mediums such as air, while seismic waves are a combination of both longitudinal (P-waves) and transverse (S-waves) waves that travel through the Earth’s interior. Seismic waves are typically caused by geological events like earthquakes, while sound waves are produced by vibrating sources like speakers or instruments.
Your standing on it! P-waves travel faster than S-waves through the Earth. As such the further away a seismometer station is from the epicentre of an Earthquake, the larger the difference between arrival times will be. By the same logic this means that the closer you get to the epicentre, the smaller the difference in arrival time will be until your at the epicentre when the difference will be zero!
Microwaves and sound waves are similar because they are electromagnetic waves. The main difference between the two types of waves is the length of the wave. Sound waves are longer than microwaves.
The difference in arrival times of P and S waves.
Pitch refers to how high or low a sound is, determined by the frequency of the sound waves. Volume, on the other hand, refers to how loud or soft a sound is, determined by the amplitude of the sound waves.
The distance between a seismological recording station and the earthquake source is determined from the arrival times of seismic waves at the station. By comparing the arrival times of P-waves and S-waves, seismologists can calculate the distance to the earthquake source using the difference in their arrival times.