hi
dispersion of water waves generally refers to frequency dispersion, which means that waves of different wavelengths travel at different phase speeds. Water waves, in this context, are waves propagating on the water surface, and forced by gravity and surface tension.
Mechanical waves, such as sound waves, travel through a medium like air, water, or solids. Electromagnetic waves, like light and radio waves, can travel through a vacuum because they do not need a medium to propagate.
P-waves typically arrive first during an earthquake, followed by S-waves, and then L-waves. P-waves are compressional waves that travel fastest through the earth's interior, followed by S-waves which are shear waves. L-waves are surface waves that travel along the earth's crust.
Yes, earthquake waves are the result of the sudden release of energy in the Earth's crust during an earthquake, and they travel through the Earth in various forms such as P-waves, S-waves, and surface waves. When you throw a stone in the water, the concentric rings of waves are known as water surface waves, which propagate along the water's surface and are caused by the displacement of water molecules. Both types of waves involve the transfer of energy through a medium, but they occur in different contexts and mediums.
Surface waves, Secondary waves, Primary waves :) I had this as a science question in school a few weeks ago... hope this helps :) Oh whoops i didnt log in so i did it again.... :) :) :) :) :) :) :)
L waves
Surface waves
l waves are the slowest our waves . They are also called "Long Waves" . They travel along the surface of the Earth . They are the ones that people notice the most .
L waves, or Love waves, are a type of surface wave that travel near the Earth's surface and cause horizontal shaking during an earthquake. These waves are slower than other types of seismic waves but can cause significant damage due to their side-to-side motion.
The speed of seismic waves from fastest to slowest is P waves (primary waves), S waves (secondary waves), and then surface waves. L waves are a type of surface wave, so they are generally slower than both P and S waves.
L waves are formed when P&S waves reach the surface.
Examples of surface waves include water waves on the ocean's surface, seismic surface waves that travel along the earth's surface during an earthquake, and electromagnetic waves that propagate along the boundaries between different materials.
Surface waves are formed when the waves reach the Earth's surface. These waves travel along the boundary between the Earth and the atmosphere, and they can cause both lateral and vertical movements of the ground.
Raleigh waves are surface waves that occur in many types of media, such as water and the Earth's crust. They cause the ground to roll up and down in a wave-like motion during an earthquake. Long waves, or long-period ocean waves, are also surface waves that have longer wavelengths and occur in the ocean due to forces such as gravity and wind.
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
Surface waves occur at the boundary between two different mediums, such as air and water, or air and land. They travel along the interface, transferring energy in the form of ripples or undulations on the surface. Examples of surface waves include ocean waves, seismic waves, and electromagnetic waves.
The different types of waves- s waves p waves or surface waves