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refraction
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When a seismic wave crosses a boundary it will change directions it the process of?
refraction
When a seismic waves crosses a boundary it will change directions in the prosses of?
refraction
When a seismic wave crosses a boundary it will change directions in the process of blank?
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.
When a seismic wave crosses a boundary it will change directions in what process?
Refraction
When a seismic wave crosses a boundary it will change directions in the process of?
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.
When a seismic wave crosses a boundary in what process will it change direction?
When a seismic wave crosses a boundary between different materials, it will change direction through a process called refraction. Refraction occurs because seismic waves travel at different speeds in different materials, causing them to bend as they encounter new mediums with varying densities.
What is it called when a seimic waves bounces backward when it reaches a boundary?
When a seismic wave bounces backward when it reaches a boundary, it is called reflection. This phenomenon occurs when the wave encounters a change in medium or boundary, causing it to change direction and return to its source. Reflection is a key process in seismic imaging and is used to map subsurface structures in geophysics.
In which area do seismic waves change dramaticaly?
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.
How can seismic wave be used to infer the presence of the Mohorovicic Discontinuity?
Seismic waves change speed and direction when they encounter changes in the density and composition of rocks. The Mohorovicic Discontinuity marks the boundary between the Earth's crust and mantle, causing seismic waves to abruptly change behavior when passing through it. By analyzing the way seismic waves interact with this boundary, scientists can infer the presence and properties of the Mohorovicic Discontinuity.
The bending of a seismic wave as it crosses a boundary is called?
The bending of a seismic wave as it crosses a boundary is called refraction. This occurs due to the wave changing speed as it moves from one material to another with different properties, causing it to change direction.
In which area do seismic waves change dramatically in speed?
they use vaginas
What divides the mantle and the core?
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
