Seismic Remote Sensing

Seismic remote sensing is a technique used to study the Earth’s subsurface by analyzing how seismic waves—vibrations that travel through the ground—are generated, transmitted, and recorded. These waves can be triggered naturally (e.g., earthquakes) or artificially (e.g., controlled blasts). By examining how seismic waves behave as they pass through different underground layers, scientists can create detailed images of beneath the surface, helping locate resources like oil and minerals, or understand geologic hazards. It’s a powerful, non-invasive way to explore what's hidden beneath our feet without drilling or excavation.