Wiki User
∙ 12y agoP waves (APEX)
Wiki User
∙ 12y agoLets Getrid
a user1
Primary waves (P-waves) arrive first at a seismometer after an earthquake. P-waves are the fastest seismic waves and are able to travel through both solid and liquid layers of the Earth.
Wiki User
∙ 10y agoThe P (primary) waves are the first to arrive.
Wiki User
∙ 9y agoThe P-wave, or primary wave, arrives first on a seismogram.
Wiki User
∙ 7y agoP waves arrive first (think Primary) follow by S waves (secondary)
Wiki User
∙ 13y agoP-waves.
Wiki User
∙ 8y agoP waves
boomybrggs
L waves
P-waves which are a compression or pressure wave are the fastest seismic waves. As they are the fastest they will reach the seismic station before any of the other seismic waves and be recorded first. Seismologists can use the difference between the arrival times of different seismic waves to calculate the distance and ultimately the location of the earthquakes epicentre. For information on this, please see the related question.
Surface waves arrive last at a seismograph station. These waves move along the Earth's surface and are the slowest of the seismic waves, but they can cause the most damage during an earthquake.
Primary (P) waves arrive at distant points before any other seismic waves. They are fastest because they are compressional waves that can travel through both solids and liquids.
The distance between a seismic station and the earthquake epicenter is determined by measuring the time it takes for the seismic waves from the earthquake to arrive at the station. By analyzing the arrival times of the different types of seismic waves (P-waves and S-waves), scientists can triangulate the epicenter location using multiple seismic stations.
The first shock wave of an earthquake is known as the P-wave or primary wave. It is the fastest seismic wave and can travel through both solid and liquid materials. P-waves are responsible for the initial jolt felt during an earthquake.
P waves
A seismometer detects primary waves (P-waves) first. These are the fastest seismic waves and are the first to arrive at a seismometer after an earthquake.
A seismometer is the instrument that measures the density of an earthquake, which is done by detecting and recording the vibrations produced by seismic waves. These measurements help scientists determine the magnitude and intensity of an earthquake.
The P Waves. Then the S Waves.
P-waves which are a compression or pressure wave are the fastest seismic waves. As they are the fastest they will reach the seismic station before any of the other seismic waves and be recorded first. Seismologists can use the difference between the arrival times of different seismic waves to calculate the distance and ultimately the location of the earthquakes epicentre. For information on this, please see the related question.
They are given this name in seismology because they are the fastest travelling of the seismic body waves released by an earthquake. Because they are the fastest, they are detected by seismometer stations first. Hence P for primary wave.
To find an earthquake's epicenter, seismologists use data from three or more seismograph stations to triangulate the location. By analyzing the arrival times of seismic waves at different stations, they can determine the distance to the epicenter from each station. The point where the circles representing the distances intersect is the earthquake's epicenter.
Surface waves arrive last at a seismograph station. These waves move along the Earth's surface and are the slowest of the seismic waves, but they can cause the most damage during an earthquake.
Primary (P) waves arrive at distant points before any other seismic waves. They are fastest because they are compressional waves that can travel through both solids and liquids.
The seismometer records the P and S-wave arrival times. P-waves travel faster through the earth than S-waves and so they arrive at the seismometer station before the S-waves and are recorded by the seismometer first. The difference in arrival time between the two types of seismic wave can be used to calculate the distance of the earthquake's epicentre from the seismometer. This can then be plotted on a map, by drawing a circle with a radius equal to the distance to the epicentre around the seismometer station. This is then repeated for the other two seismometer stations and the point where the three circles intersect is the location of the earthquakes epicentre.
The distance between a seismic station and the earthquake epicenter is determined by measuring the time it takes for the seismic waves from the earthquake to arrive at the station. By analyzing the arrival times of the different types of seismic waves (P-waves and S-waves), scientists can triangulate the epicenter location using multiple seismic stations.
3.5 minutes after the earthquake.