Secondary waves (S wave) is a wave across the intermediate seismic corruption in the. Doyonuphak of the middle movement is perpendicular to the direction of the waves through the. There are both vertical and horizontal. This type of wave is only an intermediary through which solid only. Can not travel through liquids. Secondary waves with approximately 3 – 4 km/sec. Secondary waves, stone was born to khotkhong.
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