Firstly, there are 3 types of seismic waves. Long Waves, Primary Waves(Longitudinal) and Secondary Waves(Transverse). Long Waves travel quickly along the Earth's crust, the thin outer layer. Primary Waves are longitudinal waves, they can travel both through solids andliquids, so they travel through the crust, the mantle, and the outer core (note that they refract through each layer, as each layer has a different density. Secondary Waves are transverse waves, they can only travel through solids, so they go through the inner and outer mantles, and curve away from the cores.
u can differentiate seismic waves by 1- their movement , 2 - velocity ,
3 - amplitude , period and frequency .
They vary depending upon the densities of the Geologic Formations that they pass through.
Primary and secondary waves.
Seismic waves affect us because they are what causes the motion from an earthquake that destroy buildings and such. The three types of seismic waves are surface waves primary waves also called P-waves and secondary waves also called S-waves.
P-waves are the first seismic waves to arrive at a seismograph station.
Seismic waves are the earths crust vibrating. there are two types of waves P-waves and S-waves (Primary and Secondary) Primary waves travel faster than s waves and can travel through solid and liquid, S-waves can only travel through solids
secondary waves.......... i think
Primary seismic waves travel the fastest.
Primary waves, Secondary waves, and Seismic waves
primary
Primary seismic waves are longitudinal waves. Longitudinal waves can travel through solids, liquids and gasses (although seismic waves are of to low a frequency to normally be heard). Secondary seismic waves are transverse waves and only travel through solids.
Primary wave- (P-waves) travel through solids liquids and gas. push/pull or compress waves. They travel faster and arive at seismic stations first. Secondary waves-(S-waves) travels ONLY through solids. moves side to side. Gets to the seismic stations second. I hope that helps!!
i)surface wave ii)primary wave iii)secondary wave
Primary (P) waves are the fastest. Followed by secondary (S) waves, then surface waves. P waves
Primary and secondary waves.
Seismic waves Types: Primary waves Secondary waves Surface waves
Secondary seismic waves travel slower than primary waves but they are much more destructive. Thus it carries more energy.
Primary waves are the fastest seismic waves originating from an earthquake, traveling at 6 to 7 km per second. Secondary waves travel at about 3.5 km per second.
there both wavesThey are both Seismic wavesThey can both go through solidsThey are both Seismic wavesThey can both go through solidsThey are both Seismic wavesThey can both go through solids