This report is a primary result of sampling, experimentation and analysis in Sarunageyama Fault, Sangokuyama Fault, Fujioka Fault, Owara Fault and Eniwayama Fault in Japan to measure the geographical era. The measurement of geologic time scale was conducted by the application of geophysic methods, e.g., crushing rocks with mechanical stress and increasing local temperature among sampling plates. Active (positive) faults of Sanka Sanchi regions are regarded as an abundant source of quartz particles in the granite rocks which are determinants used to assess the ESR era.