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Transverse
vibrations are perpendicular to the direction of energy transfer
longitudinal
vibrations are parallel to the direction of energy transfer.
oscillation
the repeated vibration of particles of points in a medium about a fixed position, with the energy transferred from one point to another
amplitude
the maximum displacement of a point on a wave from its equilibrium
wavelength
the distance between two corresponding points on consecutive waves
frequency
the number of complete oscoillations passing a point per second (hertz)
crest
the highest point of a transverse wave
trough
lowest point of a transverse wave
wave speed
distance travelled by the wave per unit time (m/s)
wave speed equation
Wave speed (m/s) = frequency (hertz) x wavelength (m)
example of transverse waves
water waves, Seismic Waves
example of longitudinal
p- waves, sound waves
reflection
when a wave bounces back from a surface
refraction
change in direction of a wave due to the change in speed when it enters a different medium
diffraction
the spreading out of waves as they pass through a narrow gap or obsticle
diffraction is greatest when
the wavelength is a similar size
The normal
The normal is a line drawn at 90° to the surface at the point where the ray meets the surface.
angle of incidence
the angle between the incident ray and the normal.