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No, seafloor spreading does not hold the plates in place. Seafloor spreading is a process that occurs at mid-ocean ridges where new oceanic crust is formed and spreads apart. It is driven by the movement of tectonic plates, which are actually responsible for holding the seafloor in place.
Subduction zones are where the seafloor is forced under continental plates.
seafloor
Seafloor spreading occurs at divergent plate boundaries under the ocean.
These plates move around slowly and bump into each other creating mountains, new seafloor, and earthquakes.
two seafloor plates and a seafloor plate and continental plate
Continental plates are massively granitic rock, oceanic plates massively basaltic rock, therefore continental rock is less dense than seafloor rock and has a different chemical and mineralogical composition.
No, seafloor spreading does not hold the plates in place. Seafloor spreading is a process that occurs at mid-ocean ridges where new oceanic crust is formed and spreads apart. It is driven by the movement of tectonic plates, which are actually responsible for holding the seafloor in place.
Subduction zones are where the seafloor is forced under continental plates.
the subduction zone
seafloor
Seafloor spreading occurs at divergent plate boundaries under the ocean.
Deep-ocean trenches are formed where seafloor tectonic plates subduct under continental plates.
Contintal plates
Yes. All of Earth's crust, both on land and on the seafloor, is composed of tectonic plates.
These plates move around slowly and bump into each other creating mountains, new seafloor, and earthquakes.
The region where the seafloor is forced beneath the continental plate is called a subduction zone. When the seafloor descends down it produces a deep-ocean trench.