Seismic data is typically collected by using a source, such as a sledgehammer striking a metal plate, to generate seismic energy that travels through the subsurface until reaching a series of receivers (called geophones) on the ground surface.
Seismic data is typically collected by using a source, such as a sledgehammer striking a metal plate, to generate seismic energy that travels through the subsurface until reaching a series of receivers (called geophones) on the ground surface.