Thunder + fiber-optic cabling used for seismic imaging
Source ↗
👁 0
💬 0
Most of what we know about the Earth's interior comes from observing seismic waves. These travel at somewhat different speeds depending on the details of the rock they're moving through—whether it's solid or semi-molten, how much water is present, whether it's fractured or solid material, and so on. Get enough data from enough seismic events, and you can start piecing together a picture of what's present at different depths below the surface.
In many cases, we can get this data from naturally oc
In many cases, we can get this data from naturally oc
Comments (0)