The distance from the earthquake to the observation point is estimated using the arrival time difference of the P-wave and S-wave information needed to determine the distance from the focus of an earthquake to the seismic receiving station.
The distance from the epicenter of an earthquake to the seismic station is determined by the time difference between the first arrival of the P and S waves. This is known as the S-P interval.
Requires triangulation to determine the exact location. Three seismometers are required. A circle is drawn from each of the three different seismometer sites, with the radius of each circle equal to the distance from that seismic receiving station to the epicenter.
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<span>Air is a very poor conductor of electricity and gets extremely hot when lightning passes through it. weirdly lightning can heat the air it passes through to 50,000 degrees Fahrenheit , or 5 times hotter than the surface of the sun.</span>
England, Wales, Scotland, and Northern Ireland.
Metamorphism (the process called intrusion)
By rename do you mean turn into an improper fraction?
if so, it is because without turning it into an improper fraction, you cannot subtract 3/4 from 1/4 because you would get a negative answer and that would be incorrect
