Researchers in Panama have been working to estimate the size of the fault rupture caused by the earthquake that occurred on October 9th. The estimation process relies on empirical relationships developed by Wells and Coppersmith in 1994. These relationships correlate earthquake magnitude with the likely dimensions of the resulting fault break. The analysis aims to better understand the geological impact of the seismic event in Panama. Understanding the rupture dimensions is crucial for assessing potential hazards and future earthquake risks in the region. Further studies will likely refine these initial estimates as more data becomes available from the Panama earthquake. This research provides valuable insights into the scale of the geological disruption triggered by the recent tremor.