Reflection seismology
Reflection seismology is a branch of seismology that uses reflected seismic waves to produce images of the Earth's subsurface. By noting the time it takes for a reflection to arrive at a receiver, it is possible to estimate of the depth of the feature that generated the reflection. In this way, reflection seismology is similar to sonar and echolocation.
Related Topics:
Seismology - Seismic wave - Earth - Sonar - Echolocation
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~ Table of Content ~
| ► | Introduction |
| ► | Applications |
| ► | Outline of the method |
| ► | Environmental impact |
| ► | History |
| ► | Related articles |
| ► | Further reading |
| ► | References |
| ► | External links |
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