seismic waves
seismic waves
seismic waves
A seismometer is the instrument used to measure horizontal movements along faults. It records the seismic waves generated by these movements.
The movement of faults produces seismic waves. When an earthquake occurs, it generates three types of seismic waves: P-waves (Primary waves), S-waves (Secondary waves), and surface waves. P-waves are the fastest and can travel through solids, liquids, and gases. S-waves are slower and move only through solids. Surface waves cause the most damage and travel along the Earth's surface.
An earthquake's magnitude is a measure of its strength.
These are known as seismic waves.
Faults DO NOT produce earthquakes, faults are produced by earthquakes. This means that earthquake loci are centered on and along faults. The energy released by an earthquake is the strain energy built up as a result of plate tectonic forces. Some faults move easily and thus no strain energy builds up.
It is the winds, often far out into the oceans, that create waves.
Kinetic energy
The waves of energy that an earthquake produces are called seismic waves. There are two main types: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface.
Waves carry energy in the form of kinetic energy, which is the energy of motion. This energy is transferred through the vibrations and movements of particles in the medium through which the wave travels.
Wind that blows across the water surface.