A Left-Lateral Strike-Slip Fault is a type of geological fault where two blocks of the Earth's crust slide past each other horizontally. In this faulting mechanism, if you stand on one side of the fault and look across, the block on the opposite side appears to move to the left. This movement occurs due to tectonic forces that cause stress in the Earth's crust. These faults are commonly found at the boundaries of tectonic plates, such as the San Andreas Fault in California. Left-lateral strike-slip faults can lead to earthquakes, as the accumulated stress is released suddenly when the rocks break and slip. Understanding these faults is crucial for assessing seismic risks in affected areas.