Surface waves
Love and Rayleigh waves are also known as surface waves as they travel along the surface of the earth. As the earth's surface is a free boundary, these surface waves have a larger amplitude than P and S (or body waves)which travel through the earth's interior. The amplitude of a wave is related to the amount of energy it has, where high amplitude waves have more energy! This means that the high amplitude high energy surface waves are capable of transferring more energy into structures or other objects on the surface and so can do more damage.
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.
Although surface waves travel more slowly than S-waves, they can be much larger in amplitude and can be the most destructive type of seismic wave. There are two basic kinds of surface waves: Rayleigh waves, also called ground roll, travel as ripples similar to those on the surface of water.
Body waves Body waves and surface waves are the two types of seismic waves formed during great earthquakes. P waves and S waves are called body waves because they travel through the body of the Earth. Surface waves Love waves and Rayleigh waves travel only on the surface of the Earth and cause the most destruction.
surface waves, raleigh waves, and long waves.
The seismic waves that travel along Earth;'s surface are infact known as "surface waves" of which there are two main types - Love and Rayleigh waves.
Rayleigh Waves propagate along boundary between two dissimilar solid media, in a plane perpendicular to the surface and containing the direction of propagation.
Broadly, the surface waves of which there are two main types. The Love and Rayleigh wave. Rayleigh waves have the largest amplitude of the surface waves and so cause the majority of damage.
Love and Rayleigh waves are also known as surface waves as they travel along the surface of the earth. As the earth's surface is a free boundary, these surface waves have a larger amplitude than P and S (or body waves)which travel through the earth's interior. The amplitude of a wave is related to the amount of energy it has, where high amplitude waves have more energy! This means that the high amplitude high energy surface waves are capable of transferring more energy into structures or other objects on the surface and so can do more damage.
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.
Although surface waves travel more slowly than S-waves, they can be much larger in amplitude and can be the most destructive type of seismic wave. There are two basic kinds of surface waves: Rayleigh waves, also called ground roll, travel as ripples similar to those on the surface of water.
Body waves Body waves and surface waves are the two types of seismic waves formed during great earthquakes. P waves and S waves are called body waves because they travel through the body of the Earth. Surface waves Love waves and Rayleigh waves travel only on the surface of the Earth and cause the most destruction.
surface waves can only travel along the surface.
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.
surface waves can only travel along the surface.
They travel through a material medium.
Vibrations travel through the material, just as they would in air. How well they travel through depends on the material.