explain secondary wave
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Secondary waves (S-waves) are shear waves that are transverse in nature. Following an earthquake event, S-waves arrive at seismograph stations after the faster-moving P-waves and displace the ground perpendicular to the direction of propagation.
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Secondary waves
Secondary waves or S waves,, are the second waves to arrive during an earthquake. They are much slower than primary waves or P waves and can travel only through solids. It is after studying the trajectory of S waves through the layers of earth, scientists were able to conclude that the earth’s outer core is liquid.
Characteristics of S waves :
- Second waves to hit seismographs.
- They are shear waves.
- Can only move through solids.
- Shake the medium in the direction perpendicular to which they are moving.
S wave formula
β² = μ / ρ
where,
- ⍴ is the density through which the wave propagates
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