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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.
Seismograph is a long sheet of paper with measurements of seismic activity, (earthquakes, explosions, etcetera). It will look like a long sheet with sgwiggily lines on it. These lines are made by a pen on a weight going back and forth due to the seismic activity which causes every to move about.The amplitude of the sgwiggle lines (height of sgwiggle) is proportional to the strength of the activity, naturally.These can be very helpful around the world because from at least 3 seismographs situated around the world, earthquake origins can be found in order to warn near by civilians and possibly to make evacuations for coasts in cases of sea earthquakes forming tsunamis.
By means of contour lines or spot heights.
Because contour lines show the places with same height above sea level, and if they branched, we should instead use another set of contour lines to show a height difference for the place where they should branch, and another to show the same height for the altitude above sea level as the original supposed branch, as if they branched, it would mean that there was a difference in altitude between them.
Richter Scale .
It indicates that it is greater for a more severe earthquake or for an earthquake close to the seismograph.
It indicates that it is greater for a more severe earthquake or for an earthquake close to the seismograph.
Semogram
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.
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.
The larger the deflection of the indicators (ink pens) the stronger the seismic vibrations that reached the detector.
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.
Contour lines.
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.
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.
Vertical Lines