= Fracture zones
{wiki=Category:Fracture_zones}
Fracture zones are significant geological features found on the ocean floor, particularly in the context of plate tectonics. They are characterized by long, narrow regions where the oceanic crust has been broken and displaced due to tectonic activity. These zones are the result of complex interactions between tectonic plates. Key characteristics of fracture zones include: 1. **Orientation**: Fracture zones typically run perpendicular to mid-ocean ridges, which are underwater mountain ranges formed by tectonic plates moving apart.
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