Scientists use seismometers to determine the location and strength of earthquakes. The seismometer is the device that actually measures the ground shaking. The signal is transfered to a seismograph which plots the data as a squiggly line called a seismogram. Depending on how far away you are and on how strong the earthquake is, the squiggly line can be jagged or barely noticeable. The richter scale was developed so that earthquakes could be compared in an objective way. For example, a medium-sized earthquake might be really devastating if it occurrs near a city while a big earthquake might be no big deal if it happens out in the desert. The richter scale ignores all the "human" effects and allows scientists to determine the amount of energy released by an earthquake. You probably know that it is not a linear scale. For esample, a 4 on the richter scale is not twice as strong as a 2. For each step on the richter scale there is a multiple of 30x the energy released. Therefore a magnitude 3 releases 30 times as much energy as a magnitude 2. A magnitude 4 releases 30 times as much as a magnitude 3 therefore a magnitude 4 is 30 x 30 as strong as a magnitude 2 or 900 times as strong as a magnitude 2!