They go faster through the inner core than the liquid outer core
Primary waves (P-waves) are the seismic waves that can travel through both solid and liquid materials. They are the fastest seismic waves and can travel through the Earth's interior, passing through both solid and liquid layers.
S-wave (secondary wave) seismic waves do not move through liquid materials. Unlike P-waves (primary waves), which can travel through both solids and liquids, S-waves can only propagate through solid materials due to their shear nature. This characteristic allows scientists to infer the presence of liquid layers, such as the Earth's outer core, based on S-wave behavior during seismic events.
NO! Seismic waves can't travel through space. They are mechanical waves. Mechanical waves require going through mediums and there isn't a medium in space.
If you mean Earth's interior, only longitudinal waves can pass through the liquid parts.
Mechanical waves (like seismic waves) will travel faster through a solid than a liquid.
why can s-wave can't travel but p-waves can
liquid
Solid, because that kind of wave goes fastest through solids
The velocity of seismic waves is controlled by the density and elastic properties of the material through which they travel. Solids tend to have larger elastic modulii than fluids. As the speed of a seismic wave increases as the elastic modulii increase, this means that they tend to travel faster through solids.
They go faster through the inner core than the liquid outer core
They go faster through the inner core than the liquid outer core.
Temperature affects the speed of a wave traveling through a liquid by changing the density and viscosity of the liquid. Generally, as temperature increases, the speed of the wave also increases because warmer temperatures decrease the density and viscosity of the liquid, allowing the wave to travel faster.
Primary waves (P-waves) are the seismic waves that can travel through both solid and liquid materials. They are the fastest seismic waves and can travel through the Earth's interior, passing through both solid and liquid layers.
liquid
Seismic waves travel through Earth's layers at different speeds depending on the density and composition of the materials they encounter. For example, seismic waves travel faster through solid rock than through molten magma or liquid layers. This variation in speed helps scientists to study and understand the internal structure of the Earth.
Sound waves generally travel faster through solids than through liquids. This is because the particles in solids are closer together, allowing for more efficient transmission of seismic waves. In liquids, the particles are more spread out, leading to slower sound wave propagation.