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Question
Answer in detail:
Explain the concept of the shadow zone.
Answer in Brief
Solution
- The waves which are caused by an earthquake are called seismic waves. There are three types of waves: P-waves, S-waves, and longitudinal waves.
- P-waves can pass through all the mediums while S-wave can pass only through a solid medium.
- Even though P-waves pass through all mediums, they experience refraction as they pass from one medium to the other.
- However, there exist some specific areas where the waves of that earthquake are not reported. Such a zone is called the 'shadow zone'.
- Generally, seismographs located at any distance within 105° from the epicenter, record both P-waves and S-wave. However, beyond 140° P-wave are recorded but not S-waves.
- Thus, the zone between 105° and 140° is identified as the shadow zone for both types of waves.
- The entire zone beyond 105° does not receive S-waves. The shadow zone of S-waves is much larger than that of P-waves.
- The shadow zone of P-waves appears as a band around the earth between 105° and 140° away from the epicenter.
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