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What wave does not pass through liquid outer core?
Transverse waves do not pass through the liquid outer core of the Earth. These waves vibrate perpendicular to the direction of wave propagation, making it unable to pass through the liquid outer core due to its fluid nature.
What waves are refracted and what waves are absorbed by earth's outer core?
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.
Which conclusion is supported by studies of earthquake waves passing through Earth?
Studies of earthquake waves passing through Earth support the conclusion that the Earth has distinct layers with varying densities and composition. This is because seismic waves travel at different speeds and paths as they move through different layers, providing information about the internal structure of the Earth.
How did the scientist to know the outer core is liquid?
Scientists determined that the Earth's outer core is liquid primarily through the study 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. S-waves, which cannot travel through liquids, are absent in the outer core, indicating that it must be in a liquid state. Additionally, the behavior of P-waves, which can travel through both solids and liquids, further supports the conclusion that the outer core is liquid.
How have scientist determined that the outer core of earth is liquid?
Scientists have determined that the outer core of Earth is liquid through seismic wave analysis. By studying the behavior of seismic waves as they pass through the Earth, scientists have found that S-waves are unable to travel through the outer core, indicating that it is liquid. This information has been crucial in our understanding of Earth's structure and dynamics.
What is one way that scientists know the outer core is liquid?
Scientists know the outer core is liquid because S waves, which cannot travel through liquid, are not detected beyond the core. Additionally, seismic waves from earthquakes have shown that P waves slow down significantly when passing through the outer core, indicating it is a liquid layer.
What body wave can't move through the liquid outer core?
S waves cannot travel through the outer core because they can only travel through solids, and the outer core is liquid.
What type of seismic wave travels through earth?
The P-wave is a compression / longitudinal wave and so unlike the S-wave is able to travel through the liquid outer core.
How far beneath the Earth's surface would you have to go before you were no longer passing through rock?
Roughly 2900 kilometers to the boundary between the mantle and the outer core which is a liquid.
Why don't secondary waves move through the outer core?
Because it has been proven that the outer layer is made of liquid and secondary waves do not move through liquid ^~^
What wave does not pass through liquid outer core?
Transverse waves do not pass through the liquid outer core of the Earth. These waves vibrate perpendicular to the direction of wave propagation, making it unable to pass through the liquid outer core due to its fluid nature.
What waves are refracted and what waves are absorbed by earth's outer core?
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.
Which of these describes the earth outer core?
The Earth's outer core is a liquid layer composed mainly of iron and nickel. It is responsible for generating the planet's magnetic field through convection currents. The outer core is situated below the mantle and extends to a depth of about 2,300 kilometers.
Is the outer core liquid true or false?
True. The outer core of the Earth is a layer of liquid iron and nickel that surrounds the solid inner core. It is responsible for generating Earth's magnetic field through convection currents.
Which conclusion is supported by studies of earthquake waves passing through Earth?
Studies of earthquake waves passing through Earth support the conclusion that the Earth has distinct layers with varying densities and composition. This is because seismic waves travel at different speeds and paths as they move through different layers, providing information about the internal structure of the Earth.
What happens when s waves hit the outer core of earth?
S-waves cannot travel through the liquid outer core because it cannot support shear stress. Instead, they are either absorbed or reflected when they reach the outer core boundary, causing a shadow zone on the opposite side of the Earth from the earthquake where these waves are not detected.
How did the scientist to know the outer core is liquid?
Scientists determined that the Earth's outer core is liquid primarily through the study 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. S-waves, which cannot travel through liquids, are absent in the outer core, indicating that it must be in a liquid state. Additionally, the behavior of P-waves, which can travel through both solids and liquids, further supports the conclusion that the outer core is liquid.
