Oceanic Plate Boundaries: Constructive, Transform, and Destructive
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Oceanic Plate Boundaries: A Comprehensive Look
Constructive Boundaries (Mid-Ocean Ridges)
Constructive boundaries are dorsal oceanic ridges. These are fracture zones where hot mantle material rises to the surface, causing intense volcanic activity. This volcanism produces large volumes of basalt, creating new oceanic crust. Convection currents produce divergent forces (rifting) that tend to separate the two sides of the fracture. Magma rises from within, forming the ridge's relief. The depression between the edges, occupied by the fracture, is called a Rift. In the Rift area, the crust is thin and heavily fractured.
Transform Fault Boundaries
Transform faults are discontinuous, winding ridges. Often, a ridge is interrupted and continues a few miles... Continue reading "Oceanic Plate Boundaries: Constructive, Transform, and Destructive" »