A seismogram is a record of an earthquake induced motion at a measuring station as a function of time. Seismograms are usually taken by seismometers. Seisometers record motions in three cartesian axes (x, y, and z), with the z axis perpendicular to the Earth's surface and the x- and y- axes parallel to the surface.
Historically, seismograms were recorded on paper attached to rotatingdrums. Some used pens on ordinary paper. Others used light beams to expose photosensitive paper.
Today, almost all seismograms are recorded digitally to make analysis by computer easier. Seismograms are very important for measuring earthquakes using the Richter scale.