The Wellington Fault is a significant geological feature located in the Wellington region of New Zealand. It is a strike-slip fault, meaning that the two sides of the fault move horizontally past each other. This fault is part of the complex tectonic system that shapes the region, influenced by the movement of the Pacific and Australian tectonic plates. The Wellington Fault has the potential to generate earthquakes, which can pose risks to the surrounding communities. Scientists closely monitor this fault to better understand its behavior and to improve earthquake preparedness in the area. The fault runs through urban areas, making it a critical focus for local safety measures and urban planning.