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At an oceanic-oceanic convergent plate boundary, two oceanic tectonic plates collide, leading to the subduction of one plate beneath the other. This process creates a deep ocean trench and can result in volcanic activity as the subducted plate melts and forms magma. Over time, this can lead to the formation of volcanic island arcs, such as the Aleutian Islands in Alaska. Earthquakes are also common in these regions due to the intense geological activity.

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What are the 3 subtypes of convergent plate boundaries?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.


What happens in oceanic oceanic convergent boundary?

Either plates gets subducted which is usually the older plate.


What type of boundary forms when an oceanic plate is pushed under a continental plate?

A convergent boundary forms when an oceanic plate is pushed under a continental plate. This process, known as subduction, can result in the formation of deep ocean trenches, volcanic arcs, and earthquakes.


What 3 collisions occur at a convergent boundary?

At a convergent boundary, three types of collisions can occur: oceanic-oceanic, oceanic-continental, and continental-continental. In an oceanic-oceanic collision, one oceanic plate subducts beneath the other, forming a deep ocean trench. In an oceanic-continental collision, an oceanic plate subducts beneath a continental plate, creating volcanic arcs and mountain ranges. In a continental-continental collision, both continental plates crumple and fold, forming high mountain ranges.


What are the three different types of convergent plate boundaries?

The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.

Related Questions

What are the 3 subtypes of convergent plate boundaries?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.


What are the three sub types of convergent plate boundrys?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.


What are the sub-types of convergent plates boundrys?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.


What happens in oceanic oceanic convergent boundary?

Either plates gets subducted which is usually the older plate.


What are the three types of convergent plate boundries?

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


What 3 types of convergent boundaries exist?

The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).


What type of boundary forms when an oceanic plate is pushed under a continental plate?

A convergent boundary forms when an oceanic plate is pushed under a continental plate. This process, known as subduction, can result in the formation of deep ocean trenches, volcanic arcs, and earthquakes.


What 3 collisions occur at a convergent boundary?

At a convergent boundary, three types of collisions can occur: oceanic-oceanic, oceanic-continental, and continental-continental. In an oceanic-oceanic collision, one oceanic plate subducts beneath the other, forming a deep ocean trench. In an oceanic-continental collision, an oceanic plate subducts beneath a continental plate, creating volcanic arcs and mountain ranges. In a continental-continental collision, both continental plates crumple and fold, forming high mountain ranges.


What are the three different types of convergent plate boundaries?

The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.


Oceanic-continental convergent plate boundary.?

In an oceanic-continental convergent plate boundary, an oceanic plate is subducted beneath a continental plate due to differences in density. This process can lead to the formation of deep ocean trenches, volcanic arcs on the continental plate, and earthquakes. The subduction of the oceanic plate can also cause melting of rock, leading to the formation of magma that can erupt as volcanoes on the continental plate.


What happens at a convergent plate boundary between an oceanic and continental plate?

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.


Where is the ocean to ocean plate convergent boundary located on earth?

Oceanic-oceanic convergent lead to the formation of Mariana Trench.