What Is Reflection In Geology? Reflection is the change in direction of a wavefront at an interface between two different media so that the wavefront returns into the medium from which it originated. Common examples include the reflection of light, sound and water waves. In geology, it is important in the study of seismic waves.
What Is Reflection In Earthquakes? The reflection is the energy or wave from an earthquake that has been returned (reflected) from an boundary between two different materials within the earth, just as a mirror reflects light. What is the difference between reflection and refraction in earthquakes? In seismic reflection method the waves travel downward initially
How Does Seismic Reflection Work? The general principle of seismic reflection is to send elastic waves (using an energy source such as dynamite explosion or Vibroseis) into the Earth, where each layer within the Earth reflects a portion of the wave’s energy back and allows the rest to refract through. What is seismic reflector? A