The Transverse waves show up second in time, they are slower than the Primary Waves.
S waves, or Secondary waves, are earthquake waves during an earthquake. They crash after P waves ( Primary waves) and are less stronger than surface waves
This is known as an aftershock.
A surface wave is the last seismic wave to arrive after an earthquake.
These are known as aftershocks.
Aftershocks are smaller earthquakes that occur after a larger earthquake in the same area. They are a result of the earths crust near the fault rupture readjusting as a result of the main earthquake (also known as the "main shock").
secondary tissues.
Another name for an earthquake is a seism or a temblor
Longitudinal waves, the result of earthquakes, also known as Primary, or P-Waves, are faster than Transverse (Secondary) Waves.
S waves, or Secondary waves, are earthquake waves during an earthquake. They crash after P waves ( Primary waves) and are less stronger than surface waves
P-waves and S-waves. P waves are known as Primary waves as they have a high velocity and so are recorded at seismometer stations before Secondary or S-waves. P waves may also be known as pressure waves as they are in fact compression or longitudinal waves. S-waves may also be known as shear waves as they are transverse waves.
it is a well known wave that can easily destroy homes depending on its size, a tsunami!
The P-wave which is a form of body wave known as a compression or longitudinal wave.
These are known as the seismic waves or the s waves. They will reach the earthquake location second after the first shock.
Look it The shearing action/force which takes place in y-direction(transverse dirn.)is known as transverse shear...........
A secondary wave causes rocks to vibrate at 90 degrees. This earthquake wave can travel through solids but not through liquids, and causes rock particles to vibrate at right angles to the direction of wave travel.
P-waves and S-waves. P waves are known as Primary waves as they have a high velocity and so are recorded at seismometer stations before Secondary or S-waves. P waves may also be known as pressure waves as they are in fact compression or longitudinal waves. S-waves may also be known as shear waves as they are transverse waves.
We can divide the effects of an earthquake into those known as the primary effects and those known as the secondary effects. Primary effects of an earthquake are those resulting directly from the earthquake itself. These include; buildings collapsing; roads cracking; bridges giving way; shattering of glass and injuries / deaths resulting from these. Secondary effects are those that result from the primary effects. For example ground shaking may result in the cracking of gas and water pipes (primary effects) this can result in severe fires due to explosion from escaping gas and difficulties in putting out fires due to lack of water from burst mains (secondary effects). Other secondary effects include, homelessness, business going bankrupt and closing etc.