A subduction zone occurs at convergent plate margins where an oceanic plate is going underneath a continental plate or a less dense oceanic plate. A mid-ocean ridge is a divergent plate boundary on the ocean floor with a mountain range and a rift running through the center of it. Sea floor spreading also occurs at mid ocean ridges.
C. subduction zone
Ridge push is a gravitation force that causes a plate to move away from the crest of an ocean ridge, and into a subduction zone. The Slab pull force is a tectonic plate force due to subduction. The difference is the force of motion.
The weight of the uplifted ocean ridge creates a downward force on the oceanic plate, causing it to be pushed towards a subduction zone. As the plate moves, it eventually descends into the mantle at the subduction zone due to gravitational forces, leading to the formation of a deep ocean trench.
a mid oceanic ridge
A subduction zone forms when one oceanic plate is forced beneath another plate. This process can lead to the formation of volcanic arcs, deep ocean trenches, and seismic activity.
No, the Mid Atlantic Ridge is where the two plates are diverging, which creates more oceanic floor.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
Ridges and Rises are uplifts in oceanic crust caused by volcanic eruption in oceans, the difference between a ridge and a rise is of rift valleys, ridges have long valleys and rises do not have any valleys
The sections of oceanic crust on either side of a mid-ocean ridge are moving away from each other due to seafloor spreading. As magma rises from the mantle at the ridge, it solidifies to form new oceanic crust, pushing the older crust outward. This movement is driven by tectonic forces, including mantle convection and the pull of subduction at oceanic trenches. Consequently, the ocean floor is continuously being renewed and expanded.
Its oceanic crust
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Both the ocean trench and mid-ocean ridge are features found on the ocean floor as part of the oceanic crust. They are formed by tectonic processes, with ocean trenches created by the subduction of one tectonic plate beneath another, while mid-ocean ridges are formed by the divergence of tectonic plates, leading to the upwelling of magma and the creation of new oceanic crust.