One of the earlier methods of measuring earthquake magnitude came from the “Richter Scale”, which uses a basic logarithmic formula where every magnitude level is 10 times the previous level. It relied on the amplitude measurements provided by a local seismograph. It’s not widely used anymore due to it’s impracticality for larger magnitude earthquakes and it’s development mainly meant for Southern California geography. \[M_L = log_{10}({A \over A_0})\] where A = amplitude measured by a local seismograph and the \(L\) in \(M_L\) denotes local magnitude scale