P-waves (Primary) and S-waves (Secondary). Using the difference in time between the arrival of P- and S-waves, you can then determine the distance from the epicenter. Once you've determined the distance from the epicenter of three different stations, you'll be able to triangulate the epicenter (the point where all three circles cross).
No. S waves and P waves are energy waves sent from the epicenter of the earthquake. But they are the part of an earthquake that causes damage.
Triangulation. First, they calculate the time between the first and second - primary and secondary - seismic waves created in an earthquake and use this information to determine how far the seismometer is from the epicenter of the earthquake. A circle is drawn around the seismometer so that it is in the center and the radius is equal to the calculated distance. Using this information from three different seismometers, two more circles are drawn and the intersecting point of the three circles is where the epicenter of the earthquake is located.
can travel only through solids ,slower of the two waves ,distorts or shears rock as it travels though it
theres two kinds of waves that are produced...P-waves and S-waves. its kinda hard to explain the difference between them, but if you google them you can find out more.
TWO
Primary (P) and Secondary (S) waves
No. S waves and P waves are energy waves sent from the epicenter of the earthquake. But they are the part of an earthquake that causes damage.
Scientists have sensors that detect vibrations. When two vibrate from the same cause, they hear it at different times, and the difference can be used to triangulate on the epicenter. They can predict it too a little.
They rub together and send shock-waves outward from the epicenter due to friction between the two plates.
From Science Explorer Prentice Hall Earth Science: " Geologists use seismic waves to locate an earthquake's epicenter. Seismic waves travel at different speeds. P waves arrive at a seismograph first, with S waves following close behind. To tell how far the epicenter is from the seismograph, scientists measure the difference between the arrival time of the P waves and S waves. The farther away an earthquake is, the greater the time between arrival of the P waves and the S waves." Did this help?
3 hours
Triangulation. First, they calculate the time between the first and second - primary and secondary - seismic waves created in an earthquake and use this information to determine how far the seismometer is from the epicenter of the earthquake. A circle is drawn around the seismometer so that it is in the center and the radius is equal to the calculated distance. Using this information from three different seismometers, two more circles are drawn and the intersecting point of the three circles is where the epicenter of the earthquake is located.
can travel only through solids ,slower of the two waves ,distorts or shears rock as it travels though it
primary and secondary waves
theres two kinds of waves that are produced...P-waves and S-waves. its kinda hard to explain the difference between them, but if you google them you can find out more.
Then you would end up with 2 possible locations for the epicenter. You need a 3rd station to confirm the actual location.
TWO