Yahoo Web Search

Search results

  1. Nov 26, 2013 · In this activity, students use an online simulation—Virtual Earthquake—that is accessible through the Earthquakes Living Lab interface, to locate the epicenter of an earthquake by making simple measurement on three seismograms, recordings of an earthquake's seismic waves detected by instruments (seismographs) far away from the earthquake.

  2. earthquake.usgs.gov › earthquakes › mapLatest Earthquakes

    Search Earthquake Catalog Time Zone. Display event dates and times using this time zone.

  3. (slide 10) S-waves (or secondary waves) are another type of body wave, and as the name suggests, are the second fastest type of seismic wave, meaning an S-wave would be the second wave you would feel after an earthquake occurs. In fact, S-waves travel at 60% of the speed of P-waves.

  4. Seismic waves are vibrations in the earth that transmit energy and occur during seismic activity such as earthquakes, volcanic eruptions, and even man-made explosions. There are two types of seismic waves, primary waves and secondary waves.

  5. S-waves, also known as secondary waves, shear waves or shaking waves, are transverse waves that travel slower than P-waves. In this case, particle motion is perpendicular to the direction of wave propagation.

  6. People also ask

  7. We issue bulletins of earthquake activity and maintain an archive of seismological information and records. We use the data we collect to investigate the nature and distribution of earthquake activity and their driving forces, to improve understanding of earthquake hazard.

  1. People also search for