360 Km
P-waves hit, followed by S-waves, followed by surface waves.
well if a earthquake happened the best thing to do is to go as far away as possiable from the earthquake
To determine which station was closest to the earthquake, you can analyze the seismic data recorded by each station. By calculating the time difference between the arrival of P-waves and S-waves, you can estimate the distance to the epicenter using the known velocities of these waves. The station with the shortest time difference will be the closest to the earthquake's epicenter. Comparing these distances will help identify the nearest station.
3.5 minutes after the earthquake.
The difference in arrival times of P and S waves.
The distance of the receiving station from an earthquake epicenter can be determined by measuring the arrival times of seismic waves at the station and using that data to calculate the distance based on the known speed of the waves in the Earth's crust. The station can be hundreds to thousands of kilometers away from the earthquake epicenter, depending on the strength of the earthquake and the specific propagation paths of the seismic waves.
P-waves hit, followed by S-waves, followed by surface waves.
Marconi-RCA Wireless Receiving Station was created in 1914.
They need three stations to accurately tell where the location of something is. By measuring the time where it hit one station to the next, they can determine its location through a process called triangulation.
well if a earthquake happened the best thing to do is to go as far away as possiable from the earthquake
To determine which station was closest to the earthquake, you can analyze the seismic data recorded by each station. By calculating the time difference between the arrival of P-waves and S-waves, you can estimate the distance to the epicenter using the known velocities of these waves. The station with the shortest time difference will be the closest to the earthquake's epicenter. Comparing these distances will help identify the nearest station.
Alot.
3.5 minutes after the earthquake.
Far Hills - NJT station - was created in 1914.
Far Eastern Hospital Station was created in 2006.
At least three seismograph-station readings are needed to pinpoint the epicenter of an earthquake. By comparing the arrival times of the seismic waves at different stations, scientists can triangulate the exact location of the earthquake's epicenter.
To accurately pinpoint an earthquake's epicenter, data from at least three recording stations are needed. Each station measures the seismic waves generated by the earthquake, and by calculating the time it takes for these waves to reach each station, seismologists can triangulate the location of the epicenter. The intersection of the circles drawn around each station, based on the calculated distances, indicates the epicenter's location.