No, the primary (P) waves arrive first.
P waves arrive first.
P-waves arrive first, followed by S-waves, and then surface waves during an earthquake. This sequence is due to the difference in wave velocities, with P-waves being the fastest and surface waves being the slowest.
P waves (APEX)
No, P-waves are the first seismic waves to arrive at a given location. P-waves are faster than S-waves and can travel through solid and fluid materials, whereas S-waves only travel through solid materials.
No, surface waves are typically the last seismic waves to arrive at a seismic facility. They travel more slowly than body waves (P and S waves) and arrive after the initial shaking caused by the faster body waves.
P waves arrive first.
P waves arrive before S waves during an earthquake, as P waves are faster and can travel through solid rock, while S waves can only travel through solids and are slower. This difference in arrival time can be used to determine the distance of the earthquake epicenter from the seismograph station.
P-waves arrive first, followed by S-waves, and then surface waves during an earthquake. This sequence is due to the difference in wave velocities, with P-waves being the fastest and surface waves being the slowest.
The fastest seismic waves, P-waves, will arrive first at a seismograph station after an earthquake. P-waves are compressional waves that can travel through both solids and liquids, allowing them to arrive at a station before the slower S-waves and surface waves.
P waves (APEX)
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.
Secondary waves.
P waves
No, P-waves are the first seismic waves to arrive at a given location. P-waves are faster than S-waves and can travel through solid and fluid materials, whereas S-waves only travel through solid materials.
seismic waves p-waves ans s waves
No, surface waves are typically the last seismic waves to arrive at a seismic facility. They travel more slowly than body waves (P and S waves) and arrive after the initial shaking caused by the faster body waves.
P waves and S waves. P waves arrive first and make a ripple like effect through the ground and S waves arrive second and make a twisting/circular wave.