The Andes
The Andes
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.
In Europe: the Alps, in the Americas: the Andes.
A cordillera is a chain of mountains or mountain ranges. The term cordillera is mostly applied to various ranges of the Andes in South America. The structure of cordillera mountains is usually the result of folding and faulting accompanied by volcanic activity.
Mountain ranges have more precipitation on one side than the opposite because as the moist air rises and cools, the water vapor condenses and precipitates. The result is often a dry steppe or even a desert on the one side, and a lush forest or even a rainforest on the opposite side. Examples include the Rockies, the Andes, and the Himalayas.
The Andes
Continental-continental convergence
are the result of continental-continental convergence (:
Continental-continental convergence.
its the himialahs appalicans and albines
Ocean convergence with continental plates result in subduction zone. Oceanic with oceanic plates convergence forms volcanic mountain.
Most of the large mountain ranges formed as a result of continental drift/collision, some of the smaller ranges were formed in other ways.
continental-continental convergence
Continental plate to continental plate collisions.
Typically continental plate convergence will result in an orogeny event, or a mountain building event. As the plates converge, the crust will deform, but there will be no plate subduction, and so continent to continent convergence is not related to volcanism. Large thrust faults are often associated with continental convergence zones as well.
ocean-continent convergence
There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.