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from the late 1500's and into the 1600's was a new focus on science and technology. it was the enlightenment period
I=P/S P=SoundPower S=Surface [W/m^2]
F = ma 360 = 1200a a = 0.3 m/s^s a = (v-u)/t (0.3)*(6) = v - 0 v = 18/10 m/s momentum = mass*velcoity p = m*v p = 1200*(18/10) p = 2160 kg m/s
There are four energy sublevels in the fourth energy levels: 4s, 4p, 4d, and 4f.
The most main two body waves are S wave & P wave
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the simplest metod is the S-P method
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It is a method used by seismologists to find the epicentre of an earthquake based on the difference in arrival times of P and S seismic waves as recorded at seismometer stations. For more information on the method used, please see the related question.
It is a method used by seismologists to find the epicentre of an earthquake based on the difference in arrival times of P and S seismic waves as recorded at seismometer stations. For more information on the method used, please see the related question.
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The first step in this method is to collect several seismograms of the same earthquake from different locations. Then, the seismograms are placed on a time-distance graph. The seismogram tracing of the first P wave is lined up with the P-wave time-distance curve, and the tracing of the first S wave is lined up with the S-wave curve.The distance of each station from the earthquake can be found by reading the horizontal axis. After finding out the distances, a seismologist can locate an earthquake's epicenter.-New Boyz