Seismic waves (infrasound - frequency lower than 20Hz)
• produced by earthquakes
o P-waves are longitudinal, different speeds through solids & liquids
o S-waves are transverse, cannot travel through a liquid
o S-waves are slower than P-waves
o When they reach a boundary between 2 layers, some waves will be
absorbed & some will be refracted (change speed gradually resulting in a curved path)
o These seismic waves are detected using seismometers