The Planet X Report 2017: Photographic Evidence by C'one Dr. Claudia Albers PhDScott & C'one Scott

Author:C'one, Dr. Claudia Albers PhDScott & C'one, Scott [C'one, Dr. Claudia Albers PhDScott]
Language: eng
Format: epub
Publisher: Scott C'one
Published: 2017-11-09T16:00:00+00:00

Figure 6. A vibrating diaphragm (small drum) on one end of the pipe creates alternative compressions, and rarefactions, of air molecules, which travel through the pipe, and are called sound waves.

There are two main types of seismic waves, surface waves and body waves. Surface waves travel along the surface of the ground, and body waves travel in the interior of the earth. Body waves have a higher frequency, and travel faster, than surface waves, and so are picked up first, by a seismograph. There are also two types of body waves: p and s waves. P waves cause rock to be alternatively pushed and pulled, so that you get compressions and rarefactions of molecules, making up the rock, travelling through the rock, just like the sound wave moving through the pipe, in figure 6 above. The other type of body waves is the s waves, and these cause rock molecules to move up and down, at right angles, to the direction of motion of the wave. Both p and s waves are illustrated in figure 7 below.

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