The time difference between primary (P) and secondary (S) waves becomes larger as the distance traveled by the waves increases. This is because P-waves travel faster than S-waves, so the time delay between their arrivals at a seismometer station increases with distance.
As the distance traveled by the primary and secondary waves increases, the time difference between them also increases. This is because primary waves travel faster through the Earth than secondary waves, resulting in a greater time gap between their arrivals at a given location.
The three main types of seismic waves produced by an earthquake are primary (P) waves, secondary (S) waves, and surface waves. P waves are the fastest seismic waves and travel through solids, liquids, and gases. S waves are slower than P waves and only travel through solids. Surface waves are the slowest and cause the most damage as they move along the Earth's surface.
Surface waves typically cause more damage than primary or secondary waves during an earthquake. They travel along the earth's surface and are responsible for the shaking that can result in building collapse and other structural damage. Primary and secondary waves, while important for seismologists to study, usually do not cause as much damage as surface waves.
The time between P-waves (primary waves) and S-waves (secondary waves) varies depending on the distance from the seismic event. Generally, for an earthquake, the time difference can range from a few seconds to several minutes, with P-waves arriving first, followed by S-waves. The greater the distance from the epicenter, the longer the interval between the two types of waves. Seismologists often use this time difference to determine the location of the earthquake.
Surface waves travel slower than body waves.
Surface waves travel slower than body waves.
Surface waves travel along the Earth's surface, causing most of the destruction during an earthquake. Body waves, on the other hand, travel through the Earth's interior. Body waves include primary (P-waves) and secondary (S-waves) waves, which are faster than surface waves.
The time difference between primary (P) and secondary (S) waves becomes larger as the distance traveled by the waves increases. This is because P-waves travel faster than S-waves, so the time delay between their arrivals at a seismometer station increases with distance.
the secondary wave breaks up
The secondary wave breaks up.
Primary and secondary refer to the order in which they come out, surface waves are called surface because they resonate close to the surface
As the distance traveled by the primary and secondary waves increases, the time difference between them also increases. This is because primary waves travel faster through the Earth than secondary waves, resulting in a greater time gap between their arrivals at a given location.
brings waves to the surface to create a earthquake
Primary Waves, Secondary Waves, and Surface Waves.
Seismic waves Types: Primary waves Secondary waves Surface waves
a surface wave is a earthquake it comes last. It goes Primary waves, Secondary waves, and Surface waves.