It creates a mountain that might turn into a volcano.
a trench is formed when 2 oceanic plates collide
1. Oceanic trenches. 2. Volcanic islands. 3. Volcanic mountains. and 4. Volcanic arcs.
Oceanic-continental convergence (when an oceanic plate meets a continental plate) & oceanic-oceanic convergence (2 oceanic plates) both involve oceanic plates & subduction. Continental-continental convergence (2 continental plates) involves neither.
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)
earthquakes
the earth is made up of different plates and all the plates are different sizes, shapes and weight. there are 2 types of plates, oceanic and continental. a mountain is formed when 2 continental plates of the same weight collide into each other, it creates a mountain and the oceanic plates underneath them are pused down.
an earth quake happens when two plates meet
convergence
The place where two tectonic plates come together is known as a convergent boundary. At these boundaries, plates may collide, leading to geological phenomena such as earthquakes, mountain formation, or volcanic activity. The interactions can vary depending on the types of plates involved, such as oceanic or continental.
It makes a mountain.
Two major land formations that occur at convergent boundaries are volcanic arcs and mountain ranges. When oceanic and continental plates collide, volcanic arcs are formed due to the subduction of the oceanic plate beneath the continental plate. Alternatively, when two continental plates collide, mountain ranges are formed through the intense compression and folding of the Earth's crust.
Oceanic-continental convergent boundary: Where oceanic plates subduct beneath continental plates, creating deep ocean trenches and volcanic arcs on the overriding plate. Continental-continental convergent boundary: Where two continental plates collide, causing intense folding and faulting to create mountain ranges. An example is the collision of the Indian Plate with the Eurasian Plate, forming the Himalayas.