Mohorovicic Discontinuity
they use vaginas
The total energy in a seismic wave remains constant as the wave grows larger. The energy is spread out over a larger area, resulting in lower energy concentration at any specific point.
When a seismic wave is reflected, it will bounce off a boundary between different materials and change direction. This can cause the wave to be redirected back towards its source or continue traveling in a different direction.
It is called seismic wave reflection. When a seismic wave encounters a boundary between different materials with contrasting density or rigidity, some of the wave energy is reflected back towards the source.
When a seismic wave crosses a boundary between different materials, it may undergo reflection, refraction, or diffraction. Reflection occurs when the wave bounces off the boundary, while refraction causes the wave to change speed and bend as it enters a different material. Diffraction causes the wave to spread out as it encounters an obstacle or edge.
they use vaginas
Seismic waves can change dramatically when they encounter boundaries between different geological materials with contrasting densities and elastic properties, such as the crust-mantle boundary or the core-mantle boundary. These changes in seismic wave behavior are key in helping scientists study the internal structure of the Earth.
Stress waves
refraction
refraction
The total energy in a seismic wave remains constant as the wave grows larger. The energy is spread out over a larger area, resulting in lower energy concentration at any specific point.
A seismograph can locate a seismic wave.
Seismic wave
The fastest wave is the electromagnetic wave. Of the seismic waves, the P-wave is the fastest seismic wave.
You need a shotgun and shoot the wave and that's how you stop a seismic wave
When a seismic wave is reflected, it will bounce off a boundary between different materials and change direction. This can cause the wave to be redirected back towards its source or continue traveling in a different direction.
When a seismic wave crosses a boundary, it will change directions in the process of refraction. This occurs because the wave travels at different speeds in different materials, leading to a bending of the wave path as it enters a new medium. The extent of this change in direction depends on the properties of the materials involved, such as density and elastic properties.