Final answer:
The three types of convergent plate boundaries are oceanic-continental convergence, oceanic-oceanic convergence, and continental-continental convergence. The three types of mountain building are folded mountains, fault-block mountains, and volcanic mountains.
Step-by-step explanation:
There are three types of convergent plate boundaries: oceanic-continental convergence, oceanic-oceanic convergence, and continental-continental convergence. In oceanic-continental convergence, an oceanic plate collides with a continental plate, resulting in the formation of volcanoes and a trench.
Oceanic-oceanic convergence occurs when two oceanic plates collide, forming volcanic islands. Continental-continental convergence leads to the creation of folded mountains, such as the Himalayas.
As for mountain building, the three types are folded mountains, fault-block mountains, and volcanic mountains. Folded mountains are formed when rock layers are squeezed together, creating folds. Fault-block mountains are created when large blocks of crust are uplifted along faults. Volcanic mountains are formed by the eruption of molten rock onto the surface.