The two main categories of seismic waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the Earth.
The two main categories of seismic waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the Earth.
Surface waves travel more slowly than body waves (P and S); and of the two surface.
Secondary waves and shear waves
p wave comes first s wave comes next and last comes surface wave.
body and surface waves
Body and Surface Waves
The two types of body waves are P-waves (primary waves) and S-waves (secondary waves). P-waves are compressional waves that travel through solids, liquids, and gases, while S-waves are shear waves that only travel through solids.
S-waves are secondary waves that travel slower than P-waves and have a shearing motion perpendicular to their direction of propagation. They cannot travel through liquids and are responsible for causing the most damage during an earthquake.
Body waves are seismic waves that travel through the Earth's interior. They include Primary (P-waves), which are compressional waves that travel through solids, liquids, and gases, and Secondary (S-waves), which are shear waves that only travel through solids. Body waves are responsible for the initial shaking felt during an earthquake.
The two main categories of seismic waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the Earth.
The two main categories of seismic waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the Earth.
The two main categories of seismic waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the Earth.
Waves have wavelength and frequency, which are characteristics that particles do not possess. These properties describe the spacial and temporal characteristics of a wave, defining its behavior and interactions.
Two types of seismic waves are body waves (P-waves and S-waves) and surface waves (Love waves and Rayleigh waves). Body waves travel through the Earth's interior, while surface waves travel along the Earth's surface.
These waves are called boundary waves or interface waves. They are formed due to the interaction of two different media and can exhibit characteristics of both types of waves present at the boundary.
body waves and surface waves