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S-Waves
Because S-waves come to a complete stop in the outer core.
The outer core is a liquid.
The sudden density change from the lower mantle to the outer core causes P-waves (compression or longitudinal waves) to be refracted and S-waves (shear or transverse waves) to be absorbed as the outer core is liquid and so cannot support the propagation of S-waves.
This knowledge is based on the behavior of seismic waves, particularly the behavior of P-waves and S-waves. S-waves are unable to travel through liquids, and this particular wave trait indicates a boundary between the solid mantle and the liquid outer core. As S-Waves do not propagate through the outer core a "shadow" zone is created on the other side of the earth from the source of seismic waves. In this zone no S-waves are detected. The boundary between the inner core and outer core is also detected by a difference in velocities of P-waves. The Earth's magnetic field also originates in the liquid outer core by the movement and currents of molten metal in this layer.
S-Waves
Because the Earth's core is liquid; S-waves can't travel through liquid.
Because S-waves come to a complete stop in the outer core.
The liquid outer core of the Earth's interior refracts p-waves at the boundary with the mantle, and does not carry s-waves.
Scientists suspect that the outer core is liquid because of its interaction with seismic waves. Actually, only one segment of inner earth is theorized to be liquid. This segment is known as the outer core
The outer core is a liquid.
Earth's outer core is liquid because S-waves are not transmitted through this layer
P-waves as they are able to travel through the liquid outer core of the earth, where as S-waves are not.
The sudden density change from the lower mantle to the outer core causes P-waves (compression or longitudinal waves) to be refracted and S-waves (shear or transverse waves) to be absorbed as the outer core is liquid and so cannot support the propagation of S-waves.
This knowledge is based on the behavior of seismic waves, particularly the behavior of P-waves and S-waves. S-waves are unable to travel through liquids, and this particular wave trait indicates a boundary between the solid mantle and the liquid outer core. As S-Waves do not propagate through the outer core a "shadow" zone is created on the other side of the earth from the source of seismic waves. In this zone no S-waves are detected. The boundary between the inner core and outer core is also detected by a difference in velocities of P-waves. The Earth's magnetic field also originates in the liquid outer core by the movement and currents of molten metal in this layer.
No, because to reach the center of the Earth, they need to pass through the outer core. Secondary waves, or S-waves, can't pass through liquids, such as the liquid outer core, so they can't thus even reach the center of the Earth.
S waves can not travel through liquids, the outer core is a liquid, so the S waves can not travel through the outer core. You can also determine that since the outer core is all around the inner core, that the S waves can no travel through the inner core as well.