At an oceanic-oceanic convergent plate boundary, two oceanic tectonic plates collide, leading to one plate being subducted beneath the other. This subduction creates a trench on the ocean floor and can result in volcanic island arcs, as the subducted plate melts and generates magma that rises to the surface. Earthquakes are also common in these areas due to the intense pressure and friction generated by the colliding plates. Ultimately, this dynamic process contributes to the recycling of oceanic crust and the formation of new geological features.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Either plates gets subducted which is usually the older plate.
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.
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
(A+LS) Convergent Boundary
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Either plates gets subducted which is usually the older plate.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
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-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
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.
A convergent boundry is creating the shiveluch volcano in Russia. The Eurasian plate collides with the Pacific plate
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.
An oceanic plate subducts into the mantle at convergent plate boundaries.
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
At convergent boundaries between oceanic and continental plates, the denser oceanic plate usually subducts beneath the less dense continental plate. This subduction can lead to the formation of deep oceanic trenches, volcanic arcs, and mountain ranges. It can also cause seismic activity such as earthquakes and volcanic eruptions.