@Rickoshay75,
Quote:
Earthquake scientists can't see what is is going on below the surface,
, they actually HEAR what is going on, and this is done by uing software that connects several seismic stations together. Thats how we can tell epicenters, hypocenters, magnitudes nd critical angles.
We can also measure the earths core by how signals are attenuated at various stations.
And rgman is correct, seismographs record all sorts of noise including explosions at quarries (or buildings coming down after planes hit em).
One of my old field stations where I was mapping a major aquifer by seismics was set up in a tornado cellar an (not to mention how it picked up tornadoes ina certain radius, but also it could let me know when the 3;$5 M freight train passed through the town. (This was in Tennessee.
Ever wonder why we prefer to use analog data recording for seismic data?