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physics
paper 1
waves
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Created by
Crystal Jef
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Cards (12)
wave speed
=
frequency
X
wave length
wave parts
peak
- top
trough
- bottom
amplitude
- height
wavelength
- distance between 2 peaks
transverse wave
oscillates at
90 degrees
to the direction of wave
sound
all
EM spectrum
waves
seismic s-waves
longitudinal waves
oscillations
parallel
to direction of wave travel
sound
seismic p-waves
total internal reflection
angle of incidence
=
angle of refraction
refraction
- change of
direction
/ speed of a wave from one
medium
to another
more
dense
material
ray
slows down
bends
towards
the normal
less dense material
ray
speeds up
bends
away from the normal
ultra sound
-
frequency
above human hearing
above
20,000
hertz
seismic waves
travel through
earth
result of an earthquake / volcanic eruption
seismometre
to detect
understand internal structure of earth
detect earthquakes early
p waves
travel through
solid
/ liquid / gas
longitudinal
fast
s waves
travel only through solids
transverse