The Andes Mountains in South America and the Sierra Nevada Mountains in North America are examples of mountain ranges formed as a result of oceanic-continental convergence. The collision of the oceanic plate and the continental plate led to the uplift and formation of these mountain ranges through the process of subduction and crustal compression.
The Andes
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
The Mid-Atlantic Ridge was not the result of continental convergence. Instead, it is a divergent boundary where new oceanic crust is forming as tectonic plates move apart.
The major types of mountains are volcanic mountains, fold mountains, block mountains, and dome mountains. Volcanic mountains are formed from volcanic activity, while fold mountains are created by the folding of rock layers. Block mountains result from the uplifting or faulting of large blocks of the Earth's crust, and dome mountains are formed by the uplift of a circular-shaped area of rock.
Some mountains, like volcanoes or hotspot mountains, form due to volcanic activity, not from the collision of continents. Examples include the Hawaiian Islands, formed by the movement of the Pacific Plate over a hot spot in the Earth's mantle, and Mount Kilimanjaro in Africa, which is a volcanic mountain formed independently of continental collisions.
The Andes
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.
The Andes Mountains in South America and the Cascades Range in North America were formed as a result of ocean-continental convergence. These mountains were created through the subduction of oceanic plates beneath continental plates, leading to the uplift of land and the formation of mountain ranges.
The Himalayan Mountains were formed as a result of the collision between the Indian and Eurasian tectonic plates. This collision forced the Earth's crust to crumple and uplift, creating the massive mountain range that continues to grow taller each year.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
Continental-continental convergence
are the result of continental-continental convergence (:
Continental crust cannot form as a result of oceanic-oceanic convergence. This process typically results in the formation of volcanic island arcs or deep-sea trenches. Continental crust is formed through processes like continental collision and accretion of terranes.
its the himialahs appalicans and albines
The Mid-Atlantic Ridge was not the result of continental convergence. Instead, it is a divergent boundary where new oceanic crust is forming as tectonic plates move apart.
Oceanic-continental convergence occurs in regions where an oceanic plate is subducting beneath a continental plate. Examples of this type of convergence can be found in various locations around the world, such as along the west coast of South America in countries like Chile, Peru, and Ecuador, as well as in regions like the Andes Mountains.
They are about the same age, actually. The Appalachians were formed as a result of the continental collisions that formed Pangaea.