Convergent boundary+oceanic plate=subduction because the oceanic plate is more dense causing it to subduct down back to the mantle.
When two subducting boundaries come together.
The oceanic plate usually subsides after colliding with a continental plate.
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
When two Continental plates come together, they both collide.This forms 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.
When two subducting boundaries come together.
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
The oceanic plate usually subsides after colliding with a continental plate.
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
Although they aren't common, yes, transform faults can give rise to mountains. Most transform faults take place between oceanic crust, but an easy-to-see example is that of the San Andreas Fault giving rise to the San Gabriel Mountains.
Subduction (where one plate is forced beneath another less dense plate - may occur at oceanic-oceanic and oceanic-continental boundaries), obduction (where oceanic plate is forced over a continental plate) and orogenesis where two continental plates collide and mountains are formed (e.g. the Himalayas).
When two Continental plates come together, they both collide.This forms mountains.
Convergent boundaries are also known as destructive plates. In this region, active volcanic activities, earthquakes, and crustal deformations are always happening.
It is folded and uplifted, or subducted into the mantle, depending on the type of convergent boundary.
Plate movement can cause one of three things: 1. Divergent boundaries: These are boundaries where two plates move apart. A divergent boundary will result in the uprising of magma from the mantle which creates new ocean floor. 2. Convergent boundaries: These occur where two plates move together. When this happens, oceanic lithosphere will be forced under the continental lithosphere, where it will eventually be re-absorbed into the mantle. Another outcome of convergent boundaries is the creation of mountains, which are created when two plates are both forced upward. 3. Transform fault boundaries: These occur when two plates grind against each other with producing or destroying lithosphere.
Neither plate subducts and the crust thickens and uplifts.
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.