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shanepitts
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Below is an example problem from my textbook. I don't fathom the highlighted portion where they replace the y variable with x in accordance with fig. 3.6.3?
Please help
Thanks
Please help
Thanks
paisiello2 said:Doesn't figure 3.2.5 explain it?
A seismograph measures distance by recording the vibrations caused by seismic waves that travel through the Earth's interior. These vibrations are detected by a sensor, called a seismometer, which is connected to a pen that records the movement on a piece of paper. The distance between the seismometer and the point of origin of the seismic waves can be calculated based on the time it takes for the waves to reach the seismometer.
A simple seismograph can measure the distance between the seismometer and the epicenter of an earthquake, as well as the distance between the seismometer and the different layers of the Earth's interior. It can also measure the amplitude or intensity of the seismic waves, which is a direct measure of the earthquake's magnitude.
To switch between distance variables on a seismograph, you need to adjust the settings on the instrument. This can usually be done by changing the sensitivity or gain of the seismometer, which determines the scale of the recorded seismic waves. Some seismographs may also have multiple channels that allow you to switch between different distance variables.
Yes, a simple seismograph can accurately measure long distances. However, the accuracy may be affected by factors such as the sensitivity of the instrument and the strength of the seismic waves. In general, a seismograph is most accurate when measuring distances within a few hundred kilometers.
Distance measurements from a seismograph can be used to study earthquakes in various ways. By comparing distance measurements from multiple seismographs, scientists can determine the location and depth of an earthquake's epicenter, as well as the magnitude and intensity of the earthquake. Distance measurements can also be used to study the properties of the Earth's interior, such as the size and composition of different layers, by analyzing how seismic waves travel through them.