false. it can measure P waves, S waves and surface waves
The seismograph station closest to the earthquake epicenter would have recorded P-waves first, followed by stations farther away. Since P-waves are the fastest seismic waves, they are the first to arrive at a seismograph station after an earthquake.
The primary waves (P-waves) are the first to reach a seismograph after an earthquake. These waves are faster than other seismic waves and can travel through both solid and liquid materials.
The first waves to arrive at a seismograph station are primary waves, or P waves.
The three types of seismic waves—Primary (P) waves, Secondary (S) waves, and surface waves—travel through the Earth at different speeds due to their distinct physical properties. P waves, which are compressional waves, travel the fastest and arrive first at the seismograph. S waves, being shear waves, move more slowly and arrive after P waves. Surface waves, which travel along the Earth's surface, are the slowest and typically arrive last, resulting in the staggered timing of their detection on a seismograph.
In a seismic event, the waves that reach a seismograph station last are called surface waves. These waves travel along the Earth's exterior and typically have lower speeds compared to the faster primary (P) waves and secondary (S) waves. Surface waves can cause significant ground shaking and damage but arrive after the initial P and S waves.
S waves or P waves
S waves or P waves
p-waves
The seismograph station closest to the earthquake epicenter would have recorded P-waves first, followed by stations farther away. Since P-waves are the fastest seismic waves, they are the first to arrive at a seismograph station after an earthquake.
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.
A seismometer is an instrument used to measure and record ground movements during an earthquake. It detects the vibrations caused by seismic waves and produces a graphical representation called a seismogram.
P-waves are the first seismic waves to arrive at a seismograph station.
P
The different types of waves- s waves p waves or surface waves
p waves and s waves
The primary waves (P-waves) are the first to reach a seismograph after an earthquake. These waves are faster than other seismic waves and can travel through both solid and liquid materials.
The first waves to arrive at a seismograph station are primary waves, or P waves.