convergent boudary
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
Oceanic and continental plates meet at convergent plate boundaries. At these boundaries, the denser oceanic plate is typically subducted beneath the less dense continental plate, leading to the formation of features such as deep ocean trenches and volcanic arcs.
Earthquakes, tsunami's. you name it and it could happen
The basaltic oceanic crust is more dense than the granitic continental crust. Therefore, when the two meet at plate margins, the oceanic crust usually subducts beneath the continental plate.
When oceanic and continental crust meet, a subduction zone is formed where the denser oceanic crust is forced beneath the less dense continental crust. This process typically results in the formation of deep ocean trenches, volcanic arcs, and earthquakes.
If the plates are moving toward each other, the more dense oceanic plate will subduct underneath the less dense continental plate. Mountain ranges and volcanism may result as the water saturated subducting oceanic crust creates molten rock which attempts to rise to the surface.
Volcanic arcs and trenches are commonly produced when the oceanic plate bends downwards. For more details, see the following:When an oceanic plate and a continental plate meet at a convergent boundary, the denser oceanic plate is forced down below the less dense continental plate. This is known as subduction.This forms a deep trench on the ocean bed and the subducted crust containing high proportions of volatiles (i.e. water) melts as it sinks. This magma forces it's way to the surface forming volcanoes.Please see the related link for more details.
Oceanic plates typically subduct beneath continental plates or other oceanic plates at subduction zones. The denser oceanic plate is forced beneath the less dense continental plate, leading to the formation of features such as deep ocean trenches, volcanic arcs, and earthquakes.
It is called a destructive plate boundry...one type of crust is oceanic and the other is continental. when they meet the oceanic crust gets pushed down as it is heavier. the friction caused when it sinks creates huge earthquakes and the crust re-melts and gets forced upwards due to pressure to form a volcano.
It's referred to as a Convergent Boundary If 2 Continental Plates --> Mountains If 2 Oceanic Plates --> Subduction of Heavier (older) Plate If Continental-Oceanic --> Oceanic Plate slides under the Continental Plate (Subduction of Oceanic)
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
No subduction doesn't take place when two oceanic crust meet. When two oceanic crusts meet, it is called a divergent boundary. Crustal features vary such as one like mid-ocean rdges. Subducting takes place when an OCEANIC and CONTINENTAL plate meet not when two oceanic plates meet.