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Ridge push (also known as gravitational slides or sliding plate force) is a proposed driving force for plate motion in plate tectonics that occurs at mid-ocean ridges as the result of the rigid lithosphere sliding down the hot, raised asthenosphere below mid-ocean ridges.
23 sie 2020 · Ridge push – magma rises as the plates move apart. The magma cools to form new plate material. As it cools It becomes denser and slides down away from the ridge. This causes other plates to move away from each other. Slab pull – The denser plate sinks back into the mantle under the influence of gravity. It pulls the rest of the plate along ...
29 gru 2014 · Definition. Plate Driving Forces: The forces that drive the motions of tectonic plates at the surface. Slab Pull: The force exerted by the weight of the subducted slab on the plate it is attached to. Ridge Push: The pressure exerted by the excess height of the mid-ocean ridge.
Although ridge-push/slab-pull is the favored mechanism for plate motion, it’s important not to underestimate the role of mantle convection. Without convection, there would be no ridges to push from because upward convection brings hot buoyant rock to surface.
Ridge push contributes to plate movement by creating a gravitational force that encourages tectonic plates to slide away from mid-ocean ridges. As new oceanic crust forms and elevates the ridge, it creates a slope that aids in this movement.
ridge push: the force due to the buoyancy of the hot mantle rising to the surface beneath the ridge. viscous drag: the force opposing motion of the plate and slab past the viscous mantle underneath or on the side. This force balance is given by: Fridge − push + Fslab − pull − Fviscous − drag = 0.
Ridge push is a geological process that occurs at mid-ocean ridges, where the elevation of the ridge causes a gravitational force that pushes tectonic plates away from the ridge. This phenomenon is significant in the movement of plates within the Earth's lithosphere, playing a key role in plate tectonics and geodynamics.
