The epicenter.
According to the chart, this earthquake's epicenter was 215 kilometers away. Measure the amplitude of the strongest wave. The amplitude is the height (on paper) of the strongest wave. On this seismogram, the amplitude is 23 millimeters.
No, to find the epicenter of an earthquake, you use the difference in arrival times between the P-wave and the S-wave at a seismograph station. The greater the time difference between the two waves, the farther the earthquake's epicenter is from that particular station. Subtraction is not directly involved in this process.
At the epicenter of an earthquake, both primary (P-wave) and secondary (S-wave) seismic waves are typically generated. P-waves are faster and arrive first, while S-waves are slower and arrive next. These waves cause the ground to shake in different ways, with P-waves traveling through solids, liquids, and gases, while S-waves only travel through solids.
No, the point directly above the focus of an earthquake is called the epicenter. The S wave is one of the types of seismic waves that are generated during an earthquake and move slower than the P wave.
The type of wave that causes the ground to shake in a motion parallel to the focus moving straight away from the epicenter is a primary (P) wave. P waves are compressional waves that travel through the Earth and are the fastest seismic waves. They are the first to be detected by seismographs during an earthquake.
It is because the epicenter decreases their strenght as it is closer to it
The epicenter.
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).
According to the chart, this earthquake's epicenter was 215 kilometers away. Measure the amplitude of the strongest wave. The amplitude is the height (on paper) of the strongest wave. On this seismogram, the amplitude is 23 millimeters.
The tidal wave starts by the moon
No, to find the epicenter of an earthquake, you use the difference in arrival times between the P-wave and the S-wave at a seismograph station. The greater the time difference between the two waves, the farther the earthquake's epicenter is from that particular station. Subtraction is not directly involved in this process.
At the epicenter of an earthquake, both primary (P-wave) and secondary (S-wave) seismic waves are typically generated. P-waves are faster and arrive first, while S-waves are slower and arrive next. These waves cause the ground to shake in different ways, with P-waves traveling through solids, liquids, and gases, while S-waves only travel through solids.
They first collect several seismogram tracings of the same earthquake from different locations. Then the seismograms are placed on a time distance graph. The seismogram tracing of the first p wave is lined up with the p wave time distance curve. The difference from each station from the earth quake can be found by reading the horizontal axis. After finding out the distance, a seismologist can locate an earthquake's epicenter.
This statement is incorrect. The point directly above the focus of an earthquake is called the epicenter, not the S wave. S waves are one type of seismic wave that travel through the Earth's interior during an earthquake.
A circular wave is a type of wave that propagates outwards in all directions from a central point. It is characterized by a wavefront that forms a series of concentric circles expanding outwards. Circular waves are often observed in phenomena such as ripples on water or seismic waves emanating from an earthquake epicenter.
The distance between a seismic station and the earthquake epicenter is determined from the S-P interval, which is the time difference between the time of arrival of the first P wave and the first S wave.