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Oceanic ridges are caused by the divergent movement of tectonic plates. As the plates move apart, magma rises from the Earth's mantle to fill the gap, creating new oceanic crust. This process is known as seafloor spreading.
Oceanic Plate.
Plates move away from mid-ocean ridges due to the process of seafloor spreading, which occurs as magma rises from the mantle at the ridge, creating new oceanic crust. As this new crust forms, it pushes the older crust away from the ridge, causing tectonic plates to diverge. This movement is driven by convection currents in the mantle, which create forces that pull the plates apart. Additionally, the cooling and sinking of the oceanic lithosphere further contribute to the movement of plates away from the ridges.
Oceanic rises and ridges exist due to seafloor spreading, a process where magma rises up from the mantle to create new oceanic crust at mid-ocean ridges. As the new crust forms, it pushes the existing crust aside, leading to the creation of oceanic rises and ridges. These features are important parts of plate tectonics and play a key role in the movement of Earth's lithospheric plates.
Submarine landforms created by the movement of oceanic plates include ocean ridges, deep-sea trenches, seamounts, and underwater volcanoes. These features are a result of tectonic processes such as seafloor spreading, subduction, and volcanic activity.
Mid-ocean ridges form at diverging oceanic plates. As the plates move apart, magma rises to fill the space, creating new oceanic crust. This process results in the formation of underwater mountain ranges along the divergent boundary.
Divergent plate boundary movement causes mid-ocean ridges and sea-floor spreading. This occurs when two tectonic plates move away from each other, creating new oceanic crust at the boundary. Magma rises to the surface, solidifies, and forms undersea mountain ranges known as mid-ocean ridges.
Mid-Ocean ridges.
Mid-ocean ridges form where tectonic plates diverge, or move apart. This process allows magma from the mantle to rise to the surface, creating new oceanic crust as it cools and solidifies. The continuous movement of the plates at these ridges contributes to seafloor spreading and the dynamic nature of the Earth's lithosphere.
Faults, graben and mid oceanic ridges.
Mid - ocean ridges
Mid - ocean ridges