The Andes mountains of South America and the Cascade Mountains of North America are some examples of a continental-oceanic plate boundaries.
The three possible combinations would be continental-continental, continental-oceanic, and oceanic-oceanic.
Oceanic-continental convergent boundary, Oceanic-oceanic convergent boundary, and Continental-continental convergent boundary.
Meteor impacts in the ocean basins
Oceanic to oceanic- one plate sinks under the other Oceanic- Continental ocean crust sinks under the other
continental slope
Continental- continental collisions, Continental-oceanic collisions,and Oceanic-oceanic collisions
The three possible combinations would be continental-continental, continental-oceanic, and oceanic-oceanic.
The three possible combinations would be continental-continental, continental-oceanic, and oceanic-oceanic.
The three possible combinations would be continental-continental, continental-oceanic, and oceanic-oceanic.
Oceanic-continental convergent boundary, Oceanic-oceanic convergent boundary, and Continental-continental convergent boundary.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
Meteor impacts in the ocean basins
Continental-continental, Oceanic-oceanic and Oceanic-continental convergent boundaries.
1. oceanic-continental 2. oceanic-oceanic 3. continental-continental
Convergent plate margins are characterized as collision zones between plates and may involve continental to continental crust, continental to oceanic crust, or oceanic to oceanic crust. Those that involve oceanic crust result in subduction of the more dense plate into the Earth's mantle. Continental to continental plate collisions result in uplift of the surface features and mountain building and the margin may eventually become welded together.
Oceanic-Oceanic.
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).