The height of the lines traced by a seismograph, known as the seismogram, represents the amplitude of ground motion caused by seismic waves during an earthquake. Larger amplitudes indicate stronger shaking and more intense seismic activity, while smaller amplitudes suggest weaker vibrations. By analyzing these heights, seismologists can determine the magnitude of the earthquake and assess its potential impact.
A map's height lines are called contour lines. These lines connect points of equal elevation above sea level, allowing viewers to visualize the terrain's topography and understand changes in height.
A seismograph is a device that measures and records ground motion during an earthquake or other seismic events. It consists of a ground motion sensor coupled with a recording system to monitor and document seismic waves.
Height lines on a map are called contour lines. These lines connect points of equal elevation, helping to represent the terrain's shape and steepness. By analyzing contour lines, one can determine the elevation changes and the landscape's features, such as hills and valleys.
Earthquakes are measure with a seismograph which indicates the intensity of earth crust´s movements this measurement is call Richter 1 being less intensity and 10 being major intensity.
Most scientists use a machine called a seismograph which has a pen on the end and moves when there is shaking from the seismic waves. It records the shaking on a rotating paper called a seismogram. The up and down lines you see sometimes are drawn by the seismograph.
Richter Scale .
It indicates that it is greater for a more severe earthquake or for an earthquake close to the seismograph.
The height of the jagged lines on a seismograph indicates the amplitude or strength of the seismic waves produced by an earthquake. Larger amplitudes typically correspond to stronger shaking and more powerful earthquakes.
A seismograph is located under the ground. When there is an earthquake, the ground shakes, which also shakes the pen on the seismograph, making it move along the paper, drawing lines. To know how strong the earthquake was, scientist can look on the paper. The bigger the lines, the stronger the earthquake was.
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.
Traced lines may appear closer together due to the speed of the movement, the pressure applied by the person tracing, or the texture of the surface being traced upon. These factors can influence the spacing between lines and create variations in the distance between them.
The zigzag lines recorded on a seismograph are called seismic waves. These waves represent the vibrations of the Earth caused by the release of energy during an earthquake. The different patterns and sizes of the waves help scientists analyze the earthquake's characteristics.
The larger the deflection of the indicators (ink pens) the stronger the seismic vibrations that reached the detector.
Contour lines.
because if the pen vibrated then the seismograph wouldn't work and it would defeat the purpose. the machine only works if the pen is still. if the pen is still the machine will guide it by the heartbeat lines the pen creates.
The name of the line on a map that joins places of equals height is "the contour." Contour lines are lines of equal elevation, whereas isohypse are lines of equal geopotential height.
Contour lines are imaginary lines that join points of equal height. Therefore, say, a 300 metre height contour line can never meet a 400 metre height one.