A Right-Lateral Strike-Slip Fault is a type of fault where two blocks of the Earth's crust slide past each other horizontally. When observing the fault, if you stand on one side and look across, the block on the opposite side appears to move to the right. 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. They can lead to earthquakes when the stress builds up and is suddenly released. Understanding these faults is crucial for assessing earthquake risks in affected regions.