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If the plates are moving at each other from directly opposite directions, the denser oceanic crust will subduct, or slide under the less dense continental crust, eventually melting back into the mantle. The hot gasses and pressure created by the melting process will seek release in the form of a volcano! :D
The lower plate subducts down into the mantle while frictional heating between the plates melts the rock of the plates, creating volcanoes in the upper plate.
Gravity plays a crucial role in the movement of tectonic plates through the process known as slab pull and ridge push. Slab pull occurs when a denser oceanic plate subducts beneath a lighter continental plate, pulling the rest of the plate along with it due to gravitational forces. Ridge push happens at mid-ocean ridges, where newly formed magma cools and creates an elevated landform; gravity causes the elevated lithosphere to slide away from the ridge. Together, these mechanisms help drive the continuous movement of tectonic plates across the Earth's surface.
When a continental plate collides with an oceanic plate, the denser oceanic plate will be subducted beneath the less dense continental plate due to the difference in density. This process can result in the formation of deep ocean trenches, volcanic arcs, and mountain ranges. Additionally, earthquakes and tsunamis can occur as a result of the intense tectonic activity in these zones.
Continental drift happens over millions of years due to the slow movement of tectonic plates. The movement of these plates results in the gradual shifting of continents across the Earth's surface, leading to changes in the positions and shapes of the landmasses over time.
it subducts underneath the crustal plate
If the plates are moving at each other from directly opposite directions, the denser oceanic crust will subduct, or slide under the less dense continental crust, eventually melting back into the mantle. The hot gasses and pressure created by the melting process will seek release in the form of a volcano! :D
The lower plate subducts down into the mantle while frictional heating between the plates melts the rock of the plates, creating volcanoes in the upper plate.
This happens at a plate boundary. The oceanic plate subducts (sinks) under the continental plate, because it is heavier. (the oceanic plate is made of basalt and the continental plate is made of granite.) This happens at a destructive plate margin. it is called this because part if the oceanic plate is destroyed, because it melts as it sinks.
In almost all cases the oceanic plate subducts under the continental plate, creating a trench on the seafloor off the coast and an arch of volcanoes inland on the continent. The lava of these volcanoes has a high water content, making their eruptions very explosive.
The older denser plate subducts
An ocean trench forms Two tectonic plates push against each other. The denser/heavier plate is pushed down under the other plate which is in turn pushed up to create mountains.
Convergent plates are two tectonic plates that are colliding as they move toward each other. There are several types of converging plate boundaries.Oceanic to oceanic plate convergence:Where an oceanic plate collides with another oceanic plate, the more dense plate subducts into the mantle. The subduction results in the partial melting of lithospheric rock above the area of the subduction, causing underwater volcanoes to form. If the volcanoes grow to reach the surface, volcanic arc islands are formed.Oceanic to continental plate convergence:Where an oceanic plate collides with a continental plate, the oceanic plate is subducted due to the fact that it is more dense, which can also cause volcanism and mountain building.Continental to continental plate convergence:Where two continental plates collide, neither subducts into the mantle, the crust is thickened, and mountain ranges are formed from the thickening and uplift.
At a convergent plate boundary between an oceanic and continental plate, the oceanic plate is usually denser and subducts beneath the continental plate. This can lead to the formation of deep oceanic trenches, volcanic arcs on the continental plate, and earthquakes due to the intense pressure and friction. Over time, the oceanic plate can melt and create magma that rises to form volcanic mountain ranges on the continental plate.
When a continental plate collides with an oceanic plate, the denser oceanic plate will be subducted beneath the less dense continental plate due to the difference in density. This process can result in the formation of deep ocean trenches, volcanic arcs, and mountain ranges. Additionally, earthquakes and tsunamis can occur as a result of the intense tectonic activity in these zones.
Under the earth tectonic plates and continental plate is covered in earth crust . movement is happen due to mining andsoil dig due to devolepment purpose.
Part of the lithosphere that comes off when a plate collides into another plate, and is added to it. This often happens when an oceanic plate subducts under a continental plate. As this happens, land masses such as islands are scraped off the top of the subduction plate and added to the overriding plate.