Surface waves, specifically Love waves and Rayleigh waves, typically show the highest amplitude on a seismograph during an earthquake. These waves travel along the Earth's surface and cause the most shaking and ground displacement, leading to larger amplitudes being recorded.
Surface waves show the highest amplitudes on a seismograph as they are slower-moving and have longer wavelengths, causing more pronounced shaking of the ground during an earthquake compared to body waves.
A correctly adjusted standardization amplitude will show a clear peak signal with minimal noise, indicating that the instrument is accurately calibrated to the standard reference material. The peak intensity should be consistent and reproducible when the standard is analyzed multiple times.
An oscilloscope would show a loud and high-pitched sound as a waveform with high amplitude and frequency. The amplitude would be tall to represent the loud volume, while the frequency would be closely packed together to indicate the high pitch. The waveform would likely appear as a series of closely spaced, rapid oscillations on the screen.
A diagram that represents high pitch would typically show a waveform with a high frequency, indicating the rapid vibration of the sound wave. The wavelength would be shorter and the amplitude may be smaller compared to a low pitch diagram.
An oscilloscope shows sound as a waveform representing variations in sound pressure over time. The waveform on the screen displays the sound signal's amplitude and frequency, allowing users to visualize and analyze different sound characteristics such as volume, pitch, and duration.
Surface waves show the highest amplitudes on a seismograph as they are slower-moving and have longer wavelengths, causing more pronounced shaking of the ground during an earthquake compared to body waves.
The seismograph for a larger earthquake would show stronger and more prolonged seismic waves compared to a smaller earthquake. The amplitude and duration of the seismic waves recorded by the seismograph would be greater for the larger earthquake.
Several hours after an earthquake, the seismograph would likely show small aftershocks or seismic activity continuing to register on the graph, but with decreasing intensity as time progresses. The initial sharp spikes from the main earthquake would have subsided, leaving a more regular, lower amplitude signal on the seismograph paper.
it writes it with a pen on a roll of paper
it writes it with a pen on a roll of paper
The sundial, the seismograph, kites and acupuncture.
A seismograph records earthquake waves.the correct answer is a seismometer a seismograph is the graph to show the recordings
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The height of the jagged lines on a seismogram indicates the amplitude or size of the seismic waves recorded by the seismograph. Larger amplitudes represent stronger ground motion caused by seismic events, such as earthquakes.
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To read a seismograph and interpret seismic activity accurately, first, understand that a seismograph records ground motion caused by earthquakes. Look at the seismograph's wavy lines, called seismograms, which show the intensity and duration of seismic waves. Identify the P-waves (primary waves) and S-waves (secondary waves) to determine the earthquake's location and magnitude. Compare the seismogram with data from other seismographs to confirm the earthquake's characteristics.
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