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The type of seismic wave that cannot pass through air and liquid is the S-wave, or secondary wave. S-waves are shear waves that require a medium with rigidity to propagate, which means they can only travel through solids. Unlike P-waves (primary waves), which are compressional waves and can move through both solids and fluids, S-waves are unable to transmit through liquids or gases.

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Which type of seismic wave can travel through the interior of the?

If you mean Earth's interior, only longitudinal waves can pass through the liquid parts.


Does not pass through earth's liquid outer core?

S-waves do not pass through Earth's liquid outer core because liquids cannot support the shear stress needed for these waves to propagate. This property helps scientists to understand the composition of Earth's layers by observing which seismic waves are transmitted or blocked.


How do data seismic waves indicate that earths outer core is liquid?

Because since secondary waves cannot pass through liquids or solids, and the waves can't pass thruogh the outer core than that means that the outer core is not soild.


What is divided into 2 sections because of seismic waves?

The Earth's interior is divided into two main sections due to seismic waves: the outer core and the inner core. Seismic waves behave differently when they pass through these layers; primary (P) waves can travel through both solid and liquid, while secondary (S) waves cannot pass through liquids. This behavior helps scientists determine the composition and state of the Earth's inner layers. The distinction between the solid inner core and the liquid outer core is a crucial aspect of geophysical studies.


How did scientist come to know that outer core is liquid?

Scientists determined that the Earth's outer core is liquid through the analysis of seismic waves generated by earthquakes. When these waves travel through the Earth, they behave differently depending on the state of the material they encounter. Primary waves (P-waves) can pass through both solid and liquid, while secondary waves (S-waves) cannot pass through liquids. The absence of S-waves in specific regions indicated that the outer core is liquid, as they did not travel through that part of the Earth.

Related Questions

Which type of seismic wave can only pass through earths mantle?

There is no seismic wave that can only pass through the Earth's mantle. However S-waves can not travel through earth's outer core because it is a liquid.


Which type of seismic wave can travel through the interior of the?

If you mean Earth's interior, only longitudinal waves can pass through the liquid parts.


Does not pass through earth's liquid outer core?

S-waves do not pass through Earth's liquid outer core because liquids cannot support the shear stress needed for these waves to propagate. This property helps scientists to understand the composition of Earth's layers by observing which seismic waves are transmitted or blocked.


How do data seismic waves indicate that earths outer core is liquid?

Because since secondary waves cannot pass through liquids or solids, and the waves can't pass thruogh the outer core than that means that the outer core is not soild.


Which kind of seismic wave cannot pass through water?

The S-wave.


What is the liquid you can not see trough but light go through?

The liquid you cannot see through but allows light to pass through is called opaque. This means that the liquid does not allow visible light to pass through, making it impossible to see through it.


What is divided into 2 sections because of seismic waves?

The Earth's interior is divided into two main sections due to seismic waves: the outer core and the inner core. Seismic waves behave differently when they pass through these layers; primary (P) waves can travel through both solid and liquid, while secondary (S) waves cannot pass through liquids. This behavior helps scientists determine the composition and state of the Earth's inner layers. The distinction between the solid inner core and the liquid outer core is a crucial aspect of geophysical studies.


What are liquid drops or solid particles spread through gas?

A gas cannot easily pass through a liquid or a solid however it can be entrapped in it . If a gas bubble is formed in a liquid it moves upward and escapes out of the liquid. Gas cannot pass through a solid barrier.


Which seismic body wave can penetrate the Earth's core?

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.


How did scientist come to know that outer core is liquid?

Scientists determined that the Earth's outer core is liquid through the analysis of seismic waves generated by earthquakes. When these waves travel through the Earth, they behave differently depending on the state of the material they encounter. Primary waves (P-waves) can pass through both solid and liquid, while secondary waves (S-waves) cannot pass through liquids. The absence of S-waves in specific regions indicated that the outer core is liquid, as they did not travel through that part of the Earth.


Which kind of material through which water cannot pass?

Water cannot pass through tyvek. Water vapor can however but liquid water cannot. Tyvek is high-density polyethylene fiber and is a synthetic material.


How does earth solid inner core effect seismic waves?

The Earth's solid inner core significantly affects seismic waves by changing their speed and behavior as they pass through different layers of the Earth. Primary waves (P-waves), which are compressional, can travel through both solid and liquid, while secondary waves (S-waves), which are shear waves, cannot pass through the liquid outer core. As seismic waves encounter the boundary between the outer core and the inner core, they are refracted and reflected, providing valuable information about the Earth's internal structure and composition. This behavior helps seismologists understand the characteristics of the Earth's layers and the dynamics of seismic events.