Primary waves and secondary waves (body waves). Love waves and rayleigh waves (surface waves) do not travel through the earth's mantle. Though secondary waves do not go through liquids, the asthenosphere is only a semi-liquid, so secondary waves can still go through it.
Yes, P-waves (primary waves) can travel through the Earth's mantle. P-waves are a type of seismic wave that is capable of propagating through solid, liquid, and gaseous materials. They are the fastest seismic waves and can travel through the mantle, which is the layer between the Earth's crust and core.
Seismic waves are the vibrations from earthquakes that travel through the earths surface and is measured bye the shaking you feel.
When earthquakes occur, scientists measure them using seismographs. Earthquakes produce a number of different types of waves. Some run along the surface of the earth. Some travel through the earth. Those that travel through the earth travel at different speeds. It is possible to create similar waves in a lab and measure how those waves travel through different types of materials. Since earthquakes occur all over the world, it is possible to measure the waves from all angles. Thus, if a wave travels a small distance through the core, scientists can tell by differences in speed what it would be if it traveled through all mantle material. So with the difference in speeds in different types of waves, scientists can figure out what is in the earth's interior.
Seismic waves, generated by earthquakes or artificial sources, travel through the Earth's interior. There are two main types of seismic waves: primary waves (P-waves), which are compressional and can travel through solids and liquids, and secondary waves (S-waves), which are shear waves that can only move through solids. These waves provide valuable information about the Earth's internal structure, helping scientists study its composition and behavior. Their speed and path change depending on the materials they encounter, revealing details about different layers such as the crust, mantle, and core.
Scientists know that (at least part of) the Earth's mantle is made up of solid rock because p-waves can be detected going through it. S-waves can only go through solids and are not able to pass through the parts of the mantle that are "molten".
It's impossible but many scientists and other smart people are working on it. we can tell whats under the earths crust by the vibrations produced through earthquakes ect
Yes, P-waves (primary waves) can travel through the Earth's mantle. P-waves are a type of seismic wave that is capable of propagating through solid, liquid, and gaseous materials. They are the fastest seismic waves and can travel through the mantle, which is the layer between the Earth's crust and core.
Yes, S-waves can travel through the Earth's mantle. They are secondary seismic waves that propagate by shearing the material they pass through, making them able to travel through solid materials like the mantle. However, their velocity and amplitude might change as they move through the different layers of the Earth.
Seismic waves are the vibrations from earthquakes that travel through the earths surface and is measured bye the shaking you feel.
The composition of Earth's interior affects earthquakes by influencing the propagation of seismic waves. The different layers, such as the crust, mantle, and core, have varying densities and properties that impact how seismic waves travel through them. This influences the speed, direction, and intensity of seismic waves during an earthquake.
Measurements of S-waves, which cannot travel through liquid, generated by earthquakes indicate that the outer core is liquid.
When earthquakes occur, scientists measure them using seismographs. Earthquakes produce a number of different types of waves. Some run along the surface of the earth. Some travel through the earth. Those that travel through the earth travel at different speeds. It is possible to create similar waves in a lab and measure how those waves travel through different types of materials. Since earthquakes occur all over the world, it is possible to measure the waves from all angles. Thus, if a wave travels a small distance through the core, scientists can tell by differences in speed what it would be if it traveled through all mantle material. So with the difference in speeds in different types of waves, scientists can figure out what is in the earth's interior.
Earthquakes can only happen in solids. Earthquake waves are a different matter:p-waves can travel through both solids and liquidss-waves can only travel through solidssurface waves (e,g, Rayleigh waves, Love waves) can only travel on the surface of solidsetc.
EVERYTHING! Der der der! Except nothing. Earthquakes cannot travel through space..
earthquake waves travel through the earths crust.
Seismic waves, generated by earthquakes or artificial sources, travel through the Earth's interior. There are two main types of seismic waves: primary waves (P-waves), which are compressional and can travel through solids and liquids, and secondary waves (S-waves), which are shear waves that can only move through solids. These waves provide valuable information about the Earth's internal structure, helping scientists study its composition and behavior. Their speed and path change depending on the materials they encounter, revealing details about different layers such as the crust, mantle, and core.
Seismic waves are produced by earthquakes and travel through the Earth. These waves can be divided into two main types: body waves (P-waves and S-waves) that travel through the interior of the Earth, and surface waves that travel along the Earth's surface.