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When the P wave strikes the inner core it bends and goes in a different direction.
When the P wave strikes the inner core it bends and goes in a different direction.
When the P wave strikes the inner core it bends and goes in a different direction.
The bent wave paths can be explained if the core is composed of material that is different from the overlying mantle. The P waves bend around the core in a similar way to sound waves being bent around the corner of a building. For example, you can hear people talking from around the side of a building even if you cannot see them.In this way, rather than actually stopping the P waves in the shadow zone, the outer core bends them. --Justin N. K.
The core, with its vibration causes an increase in waves. The shaking elevates the P wavers, also known as the sound waves. Further from the epicenter, the p waves are slower.
P waves are pressure waves that are the inital set of waves produced by an earthquake. Typical speeds are 330 m/s in air, 1450 m/s in water and about 5000 m/s in Granite.
They go faster through the inner core than the liquid outer core.
Primary Waves(P-Waves)
In shadow zone, seismograph does not record signals. For P-wave it is b/w 104-145 degress.These earthquake waves exhibit same properties as other waves like reflection, refraction etc.As core has denser matter so P-waves will bend inward and hences they will form a shadow zone. S-waves don't pass through liquid phase, core. So, shadow zone is larger here.
The P-wave shadow zone is an area on the Earth's surface where seismic P-waves (primary waves) do not arrive after an earthquake. This phenomenon occurs because P-waves can travel through both solid and liquid, but they are refracted (bent) when they pass through the Earth's liquid outer core. As a result, there is a zone, roughly between 104° and 140° from the earthquake's epicenter, where no P-waves are detected, indicating the presence of the liquid outer core. This shadow zone provides crucial evidence for understanding the Earth's internal structure.
These waves are known as p-waves.
P waves are seismic body waves that can penetrate the Earth's core. They are the fastest seismic waves and can travel through both solid and liquid materials, allowing them to pass through the Earth's core.