Reference: Prentice Hall. Use for educational purposes only.
Constructive interference
Destructive interference
Reflection
Refraction
Refraction
Reflection
Interference
Diffraction
Crest
Vibration
Trough
Medium
Vibrate
Compress
Expand
Move
Seismic waves
Standing waves
Transverse waves
Longitudinal waves
Nodes
Crests
Wavelengths
Troughs
Amplitude
Wavelength
Frequency
Speed
Antinodes
Nodes
Hertz
Amps
Their size
How they move
Their shape
Their source
Transverse wave
S waves
Tsunami
P waves
Diffraction
Reflection
Resonance
Refraction
Wave
Medium
Compression
Vibration
Surface waves
Longitudinal waves
Combination waves
Transverse waves
Transverse waves
Surface wave
Primary waves
Secondary waves
Surface waves
Tranverse waves
Standing waves
Longitudinal waves
Destructive interference
Constructive interference
Reflection
Refraction
Vibration
Reflection
Amplitude
Frequency
Transverse waves
S waves
Surface waves
P waves
Inward toward the Earth's core
In all directions
North to south only
Toward the equator only
Constructive interference
Destructive interference
Reflection
Refraction
Longitudinal wave
Transverse wave
Standing wave
Surface wave
How loud the sound is
The amplitude of the waves
How often the sound is repeated
The air temperature
Refraction
Reflection
Resonance
Diffraction
Speed of the wave
Frequency of the wave
Amplitude of the wave
Wavelength of the wave
Earth's crust
Rock
Earth's mantle
Liquids
Nodes
Antinodes
Rarefactions
Compressions
P waves
Longitudinal waves
S waves
Surface waves
Surface waves
S waves
P waves
Transverse waves
Locating pockets of valuable resources underground
Locating gold dust in rivers
Predicting accurately when and where volcanoes will erupt
Measuring tsunamis
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