The speed of P wave can be expressed as v= square root ((lambda+2xmobility constant)/density of material). During earthquakes, the value of P lies between 5 and 8 Km/s.
fast
A p wave is the primary or compression wave in a seismic wave. it's wavy
no a p wave is faster than s wave
epicenter. focus. magnitude. and density
The next type of seismic wave to arrive after the P-wave is the S-wave.
A P wave reflects atrial depolarization.
The last bit of your question confused me a little!? :P ... But I think you are referring to the 'The Wave Equation'. Wave Speed (v) in m/s = Frequency (f) in Hz * Wave Length (λ) in m This equation relates the speed of a wave to its frequency and wavelength
yes, their speed is about 60% of the speed of a p-wave through a given material. s-waves are also known as surface waves or secondary waves. they are known as secondary waves because they occur second because of their slower speed.
p-waves which is primary waves
P-Wave
A p wave is the primary or compression wave in a seismic wave. it's wavy
no a p wave is faster than s wave
Speed is not a wave.
epicenter. focus. magnitude. and density
Electromagnetic waves travel the fastest, at the speed of light in a vacuum, 3.0 x 108 m/s.
Both, first the P wave Then the S wave.
The seismic wave has a p and an s component. The s wave is the shear portion, and it speaks to the uplift or dropping of the surface area being affected. This wave travels out like a wave over the surface of water. The p wave is a pressure wave that travels out like a sound wave from a speaker. There is a huge difference, however. With sound, the air is being compressed in front of the speaker, while with a quake, ground is being compressed. The compression wave travels MUCH faster in a solid than in a fluid like air. The p wave in a seismic event will travel almost twice as fast as the s wave, and that means that the s wave will arrive at a seismographic sensor later than a p wave.
The next type of seismic wave to arrive after the P-wave is the S-wave.