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Each of the plates may be oceanic or continental. That gives three possibilities:oceanic - oceanicoceanic - continentalcontinental - continental.
The Andes mountains of South America and the Cascade Mountains of North America are some examples of a continental-oceanic plate boundaries.
continental arc
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Three main structures form by convergent boundaries. There are three types of convergent boundaries, oceanic-oceanic, oceanic-continental, and continental- continental. Oceanic to oceanic boundaries form volcanic islands, because the two plates come together, one crust goes under, the other forms a mountain, and the lava from the crust that went under the other one goes through the mountain, making it a volcano. Oceanic- continental convergent boundaries form volcanoes, the continental crust form the mountain, the oceanice goes under and makes the lava that goes up through the mountain and makes a volcano. continental to continental boundaries form mountains. since both crusts are of the same density, they both shoot up and form a mountain.
Each of the plates may be oceanic or continental. That gives three possibilities:oceanic - oceanicoceanic - continentalcontinental - continental.
volcanic mountains
I think its either a Trench or mountains/Volcanoes.
The Andes mountains of South America and the Cascade Mountains of North America are some examples of a continental-oceanic plate boundaries.
continental arc
Convergent oceanic - continental and oceanic - oceanic boundaries.
When two continental plates converge, it results in formation of high mountains such as the Himalayan mountain.
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).
trench
Below are the 3 types of plate boundaries, not collisions. I'm not sure myself what the correct answer is, but I know that this is incorrect.The three are divergent boundaries, convergent boundaries, and transform boundaries.The types of collisions are oceanic-oceanic which create Mt Pinatubi, oceanic-continental which create Mt. St. Helens, continental-continental which create the Himalayas, oceanic-oceanic which create the Ring of Fire and the transform boundary which is like the San Andreas Fault.
The three types of convergent plate boundaries are Oceanic-Oceanic, Continental-Continental, Continental-Oceanic.
Three main structures form by convergent boundaries. There are three types of convergent boundaries, oceanic-oceanic, oceanic-continental, and continental- continental. Oceanic to oceanic boundaries form volcanic islands, because the two plates come together, one crust goes under, the other forms a mountain, and the lava from the crust that went under the other one goes through the mountain, making it a volcano. Oceanic- continental convergent boundaries form volcanoes, the continental crust form the mountain, the oceanice goes under and makes the lava that goes up through the mountain and makes a volcano. continental to continental boundaries form mountains. since both crusts are of the same density, they both shoot up and form a mountain.