Plate Tectonic Boundaries: Formation and Destruction of Oceanic Crust
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Divergent Plate Boundaries
Mid-Ocean Ridges
Mid-ocean ridges are high elevations located in the middle of all oceans, with a total length of about 65,000 km. Some peaks of the ridges protrude above sea level, forming volcanic islands. The central part of the ridge consists of a system of fractures that form a large groove called the rift valley. The ridges are crossed by numerous transform faults.
The Genesis of an Ocean
The formation of a ridge (dorsal), and therefore a new ocean, under a continent begins when a hot spot appears. Hot magma from the mantle rises, slightly lifting the lithosphere and forming a dome. The rigid lithosphere then breaks, forming a system of three cracks called a triple point. These cracks, called rifts, continue to... Continue reading "Plate Tectonic Boundaries: Formation and Destruction of Oceanic Crust" »