The San Andreas Fault is one of the most critical geological features in the United States, running through densely populated areas of California and posing a significant earthquake risk. Understanding the precise rate at which different sections of the fault slip is crucial for seismic hazard assessments and for developing effective earthquake preparedness strategies. If this segment is indeed moving faster and more consistently, it could imply a greater likelihood of accumulating stress that leads to seismic events. This research is vital for seismologists, emergency management agencies, and residents living in proximity to the fault, as it may necessitate a re-evaluation of current risk models and building codes. While this study does not provide a timeline for future earthquakes, it contributes valuable data to the ongoing scientific effort to better comprehend and mitigate the impacts of one of the world's most formidable fault systems.