How are Fracture Zones formed?

Fracture zones are formed as a result of tectonic activity, primarily along mid-ocean ridges where tectonic plates diverge. As the plates move apart, they create fractures in the oceanic crust, which can extend for thousands of kilometers. Over time, these fractures can become offset by the movement of tectonic plates, leading to the development of linear features known as fracture zones. These zones can also experience seismic activity, as the stress along the faults is released.