ultrasonic waves have a frequency greater than 20khz
when an ultrasonic wave meets a boundary between two different mediums it is partially reflected
echo sounding or sonar is the use of ultrasonic waves for detecting obects in deep water or depth
the speed is the speed of sound in water which is 1500 m/s
two types of seismic waves
p-waves
s-waves
p-waves
longitudinal
travel at the speed of sound , twice as fast as s-waves
travels at different speeds through solids and liquids
when seismic waves are produces , the difference in time between the arrival in pwaves and swaves at detectors ca provide evidence of the earth structure
during an earthquake
seismic waves travel out wards in a curved path due to the earths increasing density and depth
p-waves shadow zone (longitudinal)
they are able to travel through the liquid outer core
however , they are refracted at the boundary between the semi-solid mantle and liquid outer core
then they are refracted again at the liquid outer core and solid inner core
these shadow zones are used to determine the size and composition of the inner and outer core
s-wave shadow zones (transverse)
not able to travel through the liquid outer core
this results in a large shadow zone opposite where the earthquake took place
the shadow zone provides evidence for the size of the earths core