An L wave, also known as a Love wave, is a type of surface wave that travels along the boundary between two different media, such as the Earth's crust and mantle. It causes the ground to move in a horizontal, side-to-side motion. L waves are the slowest seismic waves and are responsible for the long, rolling motion felt during earthquakes.
The formula for wave steepness is given as H/L, where H is the wave height and L is the wavelength. This ratio provides a measure of how steep or gradual a wave is as it approaches the shore.
An L wave is a type of surface wave that moves in a horizontal, rolling motion during an earthquake. It is slower than other seismic waves but can cause significant damage due to its side-to-side motion.
Longitudinal waves have compressions and rarefactions, they move parallel to the direction of propagation Transverse waves have peaks and troughs, the mover perpendicular to the direction of propagation l l l l lll l l l l l l l l lll l l l l l lll l l l l l l lll l l - Longitudinal ...... ..... .... ...... ...... ..... ..... .... ..... ...... ..... .... .... - Transverse ..... .... .... .... .... ... .... ......
Wavelength lambda is equated to the ratio of the speed of the wave to the frequency of the wave. So L = c / f Here L the wavelength, c the speed of the wave and f the frequency of the wave
The width of the wave. The wavelength is the distance (in the direction of the wave's propagation) between the top of a wave crest to the top of the next wave crest. The wavelength is the frequency divided by the velocity of the wave. v=f/l l=f/v
p-wave s-wave l-wave
The formula for wave steepness is given as H/L, where H is the wave height and L is the wavelength. This ratio provides a measure of how steep or gradual a wave is as it approaches the shore.
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Wavelength (m)=Wave speed (m/s) /Frequency (Hz)
S-wave stands for : Secondary wave. It comes after the P-wave and goes before the L-wave.
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An L wave is a type of surface wave that moves in a horizontal, rolling motion during an earthquake. It is slower than other seismic waves but can cause significant damage due to its side-to-side motion.
Longitudinal waves have compressions and rarefactions, they move parallel to the direction of propagation Transverse waves have peaks and troughs, the mover perpendicular to the direction of propagation l l l l lll l l l l l l l l lll l l l l l lll l l l l l l lll l l - Longitudinal ...... ..... .... ...... ...... ..... ..... .... ..... ...... ..... .... .... - Transverse ..... .... .... .... .... ... .... ......
Wavelength lambda is equated to the ratio of the speed of the wave to the frequency of the wave. So L = c / f Here L the wavelength, c the speed of the wave and f the frequency of the wave
The width of the wave. The wavelength is the distance (in the direction of the wave's propagation) between the top of a wave crest to the top of the next wave crest. The wavelength is the frequency divided by the velocity of the wave. v=f/l l=f/v
N = 2k/(2pi/L) so k = pi.N/L
L waves are formed when P&S waves reach the surface.