Seismic waves are the invisible pressure movements that travel through the earth after an earthquake or tremor. They can also be generated by humans through underground controlled explosions or shocks and on the surface by heavy seismic machinery impacting the surface of an area.
The pressure waves travel in 2 or more ways, p-waves or push ways travel in a straight line and travel the furthest in all directions, s-waves or shear or shake waves, travel from side to side and travel shorter distances, close to the surface. As each wave reaches a boundary in the sub-strata they bounce back to the surface, where they can be recorded on a seismograph, indicating the strata depths and structures and can aid in the interpretation of geological structures and mineral exploration. Other waves can travel right around the earth and down into the earth, where they are reflected back off of the earth's nickel-iron core, forming a shadow area. By correlating a series of recordings from various surface points, a triangulation can be made indicating the source position of the shock.
The strengths of the shocks are given as degrees on The Richter Scale.
Seismic waves are the forms of energy produced by an earthquake.
Seismic waves.
The seismic wave that travels really fast is the primary or P-wave. P-waves are the fastest seismic waves and can travel through solids, liquids, and gases. They are the first waves recorded on seismographs during an earthquake.
The seismic wave that travels fast and increases its speed with depth is called a primary or P-wave. P-waves are compressional waves that can travel through solids, liquids, and gases, and they are the fastest seismic waves.
body waves
things that can cause seismic waves are earthquackes
A seismic wave travels through the Earth's layers, after a volcano, explosion, or earthquake. Transverse, compressional, longitude, and shear waves are all types of seismic waves after earthquakes.
surface waves
A longitudinal wave vibrates in the same direction that the wave travels. Examples of longitudinal waves include sound waves and seismic waves.
S-waves travel only through solids.
Mechanical waves travel by pushing and pulling on the matter they travel through. Sound waves and seismic waves are examples of mechanical waves.
Primary waves (P-waves) are the type of seismic wave that travels the fastest through rock material. These waves are able to cause rocks to vibrate in the same direction as the waves, resulting in a back-and-forth motion.